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+{"event_id": 1065296, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-10 21:11:00", "end_date_time": "2023-01-10 23:11:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side  Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported a mudslide on SR 41 at Road 415 in Coarsegold.", "ts_dict_index": [12, 13, 14]}
+{"event_id": 988991, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2021-12-14 13:14:00", "end_date_time": "2021-12-14 16:14:00", "narrative": "A strong low pressure system dropped southeast out of the Gulf of Alaska on December 12 and intensified off the Pacific Northwest coast on December 13 pulling up some deep moisture which was pushed into central California during the afternoon.  The precipitation intensified during the evening of December 13 through the morning of December 14 as the low carved out a deep upper trough which pushed across California during the afternoon of December 14.  This system produced 2 to 4 inches of liquid precipitation over the Sierra Nevada from Sequoia National Park northward and 1 to 3 inches of liquid precipitation south of Sequoia Park.  The precipitation fell mainly in the form of snow above 5500 feet and several high elevation SNOTELs estimated 2 to 4 feet of new snowfall.  The snow level lowered to as low as 1500 feet during the evening of December 14 as the cooler airmass behind the system pushed into central California.  Much of the San Joaquin Valley picked up between 1 to 2 inches of rainfall while the Kern County Mountains picked up between 0.75 and 1.5 inches of liquid precipitation.  The Kern County Desert areas only picked up between a quarter and a half inch of rain at most locations due to rain shadowing.  The storm produced widespread minor nuisance flooding in the San Joaquin Valley and Sierra foothills with a few rock slides noticed.  Several roads were closed as a precaution and chain restrictions were implemented on some roads in the Sierra Nevada.  The storm also produced strong winds over the West Side Hills as well as in the Grapevine and Tehachapi areas in Kern County.  Several stations in these areas measured wind gusts exceeding 50 mph with a few locations near the Grapevine measuring brief gusts exceeding 70 mph. California Highway Patrol reported mud, rock and dirt covering most of North Plano St. near Lynch Dr.", "ts_dict_index": [48, 49, 50]}
+{"event_id": 931869, "event_type": "Debris Flow", "state": "ALASKA", "cz_name": "HAINES BOROUGH", "begin_date_time": "2020-12-01 22:00:00", "end_date_time": "2020-12-03 12:00:00", "narrative": "A large plume of concentrated moisture or Atmospheric River (AR) with an associated low-pressure system moved across the Pacific Ocean and transported tropical moisture from the southwest which impacted Southeast Alaska (SEAK) from December 1st through December 2nd. This event brought widespread significant, and sometimes historic record setting rainfall to locations across Southeast Alaska. There were multiple waves along the main front to produce a quasi-stationary front and allowed heavy precipitation to persist over the panhandle for a long duration. Rainfall amounts were as high as over 15 at Little Port Walter with most other locations reporting 5 to 12 over the 2 days. Juneau, Skagway and Haines airports broke their all time daily precipitation record on December 1st along with the all time 2 day total when both days are combined. Rainfall intensity recurrence intervals  ranged from a 50 to 200 year event when looking at 6,12,24,48 hour time periods. In some locations the precipitation started out as snow, minor accumulations but then changed quickly over to moderate/heavy rain. Significant snowfall did occur mainly at high elevations and along the Haines and Klondike highways before transition to rain as temperatures rose above freezing all the way up to 6000 feet with the impacting warm front. Snow accumulations were very impressive from December 1st into the 2nd with 18 at 800 feet near the Haines US customs border station and a staggering 59 at 2560 feet on Mount Ripinski above Haines. There was persistent precipitation that occured the previous weeks to keep the soils on the wet side. The heavy precipitation and warm temperatures melted snow that had already accumulated on the ground at sea level then as the snow level climbed above the mountain top this increased the amount of runoff significantly from the mountains. All the excess runoff resulted in significant and in places record flooding of roads and homes, erosion that damaged roads and infrastructure, and widespread mass wasting events such as landslides and debris flows. Most of these impacts were reported to have started in the early morning hours of December 2nd and persist into December 3rd or longer. The northern half of Southeast Alaska saw most if not all of these impacts with a few specific rivers, Salmon River in Gustavus and Jordan Creek in Juneau, seeing record river stage values. Widespread damaging debris flows impacted Juneau, Skagway and Haines that took out roads, destroyed homes and caused 2 fatalities in Haines. ��To go along with the heavy precipitation there was also very strong damaging winds as the waves moved along the front over the panhandle. These strong winds damaged power lines from falling trees.��In total there were about 7 communities (Haines, Juneau, Skagway, Gustavus, Hoonah, Tenakee Springs, and Hyder) that declared a disaster from this event. As the atmospheric river moved over the far north central inner channels of Southeast Alaska it produced significant amount of precipitation from December 1st-2nd. Heavy to moderate rainfall persisted over 48 hours with the highest amounts coming during the afternoon hours of December 1 through late morning of December 2nd. By mid morning on December 1st, near 2 of precipitation already fell. The snow levels were low at the start of the event with a few inches at sea level in Haines but as much as 12 was reported at 800 feet by the Haines40NW COOP and 20 at the 2500 foot Flower Mt SNOTEL site by the morning of December 1st. Closer to Haines, the Ripinski ridge weather station at 2560 feet reported an estimated snow accumulation of near 59 from before the warm air moved into the area. The snow level rose rapidly through the evening of December 1st to be above the mountain tops by the early morning hours of December 2nd. This warming at elevation melted the fresh snow that fell with Ripinkis Ridge losing close to 30 and Flower Mt losing near 20 by the afternoon of December 2nd. By the end of December 1st the Haines airport reported a 24 hour precipitation amount of 5.49 which was a 25 to 50 year event and broke the all time daily precipitation record from 1946. The Haines COOP reported at 7am AKST on December 2nd a 24 hour amount of 6.62 which also broke the all time daily precipitation record from 2005. Haines40NW COOP along the Haines Hwy reported at 7am AKST on December 2nd a 24 hour precipitation amount of 5.23 a new all time daily precipitation record beating out 1999 and a 25 year event. From December 1st to the 2nd precipitation amounts from the downtown Haines COOP were 8.54���,  Haines Airport 10.26��� a 200-500 year event, and the Haines40NW COOP 8.12��� a 50-100 year event, were all time 48 hours precipitation records. From December 1st to 3rd 10 to 10.50 of precipitation fell from downtown Haines to the Haines border with a 100 to 200 year event. All of this heavy rainfall and snow melt produced significant impacts in the Haines area. In the early hours of December 2 after all-time record rainfall, saturated soils, and a deep snowpack, a second impulse of heavy precipitation moved over the area, and the snow level rose above 2500ft. The rising snow level began to melt the fresh snowfall at high elevation to produce significant amount of runoff that overwhelmed drainage ditches and culverts. The intense runoff began to erode the roads at the base of Ripinski Ridge and by day break there was significant infrastructure damage to all roads near Ripinski ridge which left Piedad Rd, Cathedral View Dr, Allen Rd, Comstock Rd, 4th ave,Young Rd to name a few that were impassable as the roads were washed away from erosion. There was also significant flooding away from the steep terrain from poor drainage not keeping up with the amount of runoff. Up to 4 feet of water flooded the Haines Hitch-Up RV park along with flooding across places at the Haines airport essentially closing it down to flights.  To go along with the major road infrastructure damage there were a number significant major debris flows from the intense precipitation, super saturated soils and strong winds to help trigger the slides that blocked roads and damaged homes near steep terrain. Haines was cut off from the Canadian Border and the airport due to debris flows blocking the Haines Hwy. There were also multiple debris flows along Lutak Rd that damaged the Lutak fuel Dock, blocked the road in multiple locations and isolated residence in a subdivision at the end of the road. A few homes at the end of Lutak Rd we significantly damaged from debris flows coming down behind their homes with one getting pushed off its foundation, another with debris in the house and another with minor damage. Mud Bay Rd was blocked by a debris flow which isolated another part of town. A large avalanche came down into Chilkat Lake out the Haines Hwy that damaged a few homes. Residence in the affected areas and other locations near steep terrain were evacuated to emergency shelters throughout the morning of December 2. Heavy rain continued into the afternoon hours and around 130pm AKST a massive landslide occurred along Beach Rd that took out a 200 yard section of the road, destroyed 2 homes while causing major damage to another. One of the destroyed homes was not occupied but the other had to 2 people inside. The 2 people perished from the landslide or what the geologist are calling a geologic mass wasting event. There were about a half dozen homes on the south side of the slide that were evacuated due to the threat of another very large landside.  It continued to be very wet with freezing levels going up and down to keep increase runoff not just from the precipitation but also from snow melt for the next week with a 7 day total of 14.85 which is a near 150 year event. The continue precipitation on the super saturated soils kept the threat of more debris flows high through December 7th. There was some minor movements of a home near an old landslide from 2012 called the slump area. This was one of the most impactful flooding and debris flow event since 2005 or ever and the data backups extreme impacts. The city of Haines declared a disaster for this event from the widespread and extensive infrastructure damage, 2 homes destroyed, 7 homes with major damage, 16 homes with minor damage with another 12 home adversely affected from the area damage and the 2 deaths. The governor of Alaska also declared a disaster emergency for Southeast Alaska from the impacts of this event.", "ts_dict_index": [0, 1, 2]}
+{"event_id": 1079860, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "SAN BERNARDINO", "begin_date_time": "2023-02-24 20:30:00", "end_date_time": "2023-02-24 20:30:00", "narrative": "An intense period of heavy snow and blizzard conditions, damaging winds, low-elevation snow and widespread flooding rainfall plagued Southern California February 21-27.||Very strong, and locally damaging, winds developed in the evening on February 21 and continued through February 22, especially impacting the coast and the mountains. Numerous trees were uprooted as a result of the strong winds. Temperatures plummeted on February 22 leading to low-elevation snow and cold-core thunderstorms.||The second, and highly impactful, next wave of the storm system enveloped Southern California starting on February 23. This is the period of heaviest snowfall, and a first-ever Blizzard Warning issued by NWS San Diego was in effect for the San Bernardino County Mountains. Heavy snowfall persisted through early morning on February 26, resulting in FEET of snowfall in the mountains, with many locations in the San Bernardino County Mountains seeing over 50 of snowfall. This resulted in hard closures of many highways in the San Bernardino County Mountains and left people trapped in their homes. Snow levels once again fell on February 25, with snow levels as low as 1000-2000 feet in the Inland Empire and inland Orange County. Widespread heavy thunderstorms occurred leading to local flooding, especially across San Diego County, inland Orange County and portions of the Inland Empire, as well as produced pea size hail.||The impacts of this system, especially in San Bernardino County, would be further exacerbated by an additional significant storm system that would hit only days later, leading to additional FEET of snow. The Department of Highways reported a vehicle stuck in mud on Cleghorn Road off of SR-1138. Search and rescue in place at midnight.", "ts_dict_index": [69, 70, 71]}
+{"event_id": 798028, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-02-13 09:00:00", "end_date_time": "2019-02-13 12:00:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. The Tulare County Emergency Manager reported a mudslide at the intersection of Bear Creek Road and Balch Park Road.", "ts_dict_index": [63, 64, 65]}
+{"event_id": 1079858, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "SAN BERNARDINO", "begin_date_time": "2023-02-24 13:20:00", "end_date_time": "2023-02-24 13:20:00", "narrative": "An intense period of heavy snow and blizzard conditions, damaging winds, low-elevation snow and widespread flooding rainfall plagued Southern California February 21-27.||Very strong, and locally damaging, winds developed in the evening on February 21 and continued through February 22, especially impacting the coast and the mountains. Numerous trees were uprooted as a result of the strong winds. Temperatures plummeted on February 22 leading to low-elevation snow and cold-core thunderstorms.||The second, and highly impactful, next wave of the storm system enveloped Southern California starting on February 23. This is the period of heaviest snowfall, and a first-ever Blizzard Warning issued by NWS San Diego was in effect for the San Bernardino County Mountains. Heavy snowfall persisted through early morning on February 26, resulting in FEET of snowfall in the mountains, with many locations in the San Bernardino County Mountains seeing over 50 of snowfall. This resulted in hard closures of many highways in the San Bernardino County Mountains and left people trapped in their homes. Snow levels once again fell on February 25, with snow levels as low as 1000-2000 feet in the Inland Empire and inland Orange County. Widespread heavy thunderstorms occurred leading to local flooding, especially across San Diego County, inland Orange County and portions of the Inland Empire, as well as produced pea size hail.||The impacts of this system, especially in San Bernardino County, would be further exacerbated by an additional significant storm system that would hit only days later, leading to additional FEET of snow. The Department of Highways reported flooding and mud along the Duncan Canyon Road offramp, with two vehicles stopped and on vehicle in two feet of mud.", "ts_dict_index": [66, 67, 68]}
+{"event_id": 1064931, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 15:11:00", "end_date_time": "2023-01-09 17:11:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported boulders on I-5 south of the Lebec Rest Stop.", "ts_dict_index": [6, 7, 8]}
+{"event_id": 1005323, "event_type": "Debris Flow", "state": "KENTUCKY", "cz_name": "CLAY", "begin_date_time": "2022-01-01 11:00:00", "end_date_time": "2022-01-01 11:00:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. Clay County 911 reported a mudslide along KY-1350 about 5.5 miles up, near the community of Sexton's Creek.", "ts_dict_index": [45, 46, 47]}
+{"event_id": 801346, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 03:32:00", "end_date_time": "2019-03-07 12:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported a rock slide in the area of Burlando Rd. and Kernville Rd. in Kernville.", "ts_dict_index": [81, 82, 83]}
+{"event_id": 801344, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 02:59:00", "end_date_time": "2019-03-06 08:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported rocks in the traffic lanes if Interstate 5 at the intersection of Fort Tejon Rd. near Lebec.", "ts_dict_index": [72, 73, 74]}
+{"event_id": 938932, "event_type": "Debris Flow", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 05:30:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. A mudslide is blocking one lane on KY-1499 at mile marker 3.", "ts_dict_index": [27, 28, 29]}
+{"event_id": 938561, "event_type": "Debris Flow", "state": "KENTUCKY", "cz_name": "CLAY", "begin_date_time": "2021-02-28 22:10:00", "end_date_time": "2021-02-28 22:10:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Two mudslides near Ponders Branch Road have blocked the road, just north of the Burning Springs community.", "ts_dict_index": [18, 19, 20]}
+{"event_id": 938532, "event_type": "Debris Flow", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2021-02-27 08:50:00", "end_date_time": "2021-02-27 08:50:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. A rock and mudslide were reported near the Kimper community on KY 194.", "ts_dict_index": [15, 16, 17]}
+{"event_id": 863282, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-12-26 14:00:00", "end_date_time": "2019-12-26 16:00:00", "narrative": "A strong and very cold low pressure system dropped southward along the California coast on Christmas Day bringing some light precipitation inland into central California. The system then turned inland and moved through southern California during the evening of December 25 through the morning of December 26 bringing moderate to heavy precipitation to much of Kern County with lighter amounts further north. Between 1 and 2 inches of liquid precipitation fell across much of Kern County with the snow level between 2500 and 3000 feet. Above the snow line, 1 to 2 feet of new snowfall was reported at several stations and the heavy snowfall resulted in the closure of several highways (including Interstate 5 south of Grapevine) for an extended period of time during a period of normally heavy holiday traffic after several vehicle either slid off of the highway or spun out. One truck driver was killed after being stranded along Interstate 5 for several hours. Across the Kern County Deserts and in the San Joaquin Valley from Bakersfield southward, heavy rainfall resulted in several roads being closed for a few hours with several reports of nuisance flooding reported by the Emergency Managers office or by law enforcement. There were also several reports of strong wind gusts and some reports of minor wind damage in the Fort Tejon and Tehachapi areas. Further north precipitation amounts were significantly lower although parts of Kings County picked up between a quarter and three quarters of an inch of rainfall. The remainder of the area generally picked up a quarter of an inch or less of liquid precipitation before the system moved to the east of the area during the evening of December 26. California Highway Patrol reported 4 vehicles were stuck in a mudslide near the intersection of Holt St. and Purdy Ave. in Mojave.", "ts_dict_index": [60, 61, 62]}
+{"event_id": 938943, "event_type": "Debris Flow", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 05:30:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. All 3 lanes of US-460 are blocked at mile marker 22 due to a mudslide.", "ts_dict_index": [24, 25, 26]}
+{"event_id": 863273, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-12-26 13:26:00", "end_date_time": "2019-12-26 19:26:00", "narrative": "A strong and very cold low pressure system dropped southward along the California coast on Christmas Day bringing some light precipitation inland into central California. The system then turned inland and moved through southern California during the evening of December 25 through the morning of December 26 bringing moderate to heavy precipitation to much of Kern County with lighter amounts further north. Between 1 and 2 inches of liquid precipitation fell across much of Kern County with the snow level between 2500 and 3000 feet. Above the snow line, 1 to 2 feet of new snowfall was reported at several stations and the heavy snowfall resulted in the closure of several highways (including Interstate 5 south of Grapevine) for an extended period of time during a period of normally heavy holiday traffic after several vehicle either slid off of the highway or spun out. One truck driver was killed after being stranded along Interstate 5 for several hours. Across the Kern County Deserts and in the San Joaquin Valley from Bakersfield southward, heavy rainfall resulted in several roads being closed for a few hours with several reports of nuisance flooding reported by the Emergency Managers office or by law enforcement. There were also several reports of strong wind gusts and some reports of minor wind damage in the Fort Tejon and Tehachapi areas. Further north precipitation amounts were significantly lower although parts of Kings County picked up between a quarter and three quarters of an inch of rainfall. The remainder of the area generally picked up a quarter of an inch or less of liquid precipitation before the system moved to the east of the area during the evening of December 26. California Highway Patrol reported rocks in the roadway on southbound SR 14 near Abbott Dr.", "ts_dict_index": [57, 58, 59]}
+{"event_id": 1005379, "event_type": "Debris Flow", "state": "KENTUCKY", "cz_name": "CLAY", "begin_date_time": "2022-01-01 11:00:00", "end_date_time": "2022-01-01 11:00:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. Clay County 911 reported a mudslide onto the Hal Rogers Parkway around mile marker 11 in western Clay County.", "ts_dict_index": [42, 43, 44]}
+{"event_id": 938951, "event_type": "Debris Flow", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 05:30:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. A mudslide is blocking the road along KY-1372 at mile marker 3.", "ts_dict_index": [30, 31, 32]}
+{"event_id": 941671, "event_type": "Debris Flow", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2021-03-01 11:30:00", "end_date_time": "2021-03-01 11:30:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. An estimated 4.00 inches of rain fell in Pikeville, leading to a mudslide along Chloe Creek near the Pikeville City Elementary School.", "ts_dict_index": [21, 22, 23]}
+{"event_id": 801350, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 08:04:00", "end_date_time": "2019-03-06 11:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported Lake Isabella Blvd. completely flooded with water and mud near Elizabeth Norris Rd.", "ts_dict_index": [93, 94, 95]}
+{"event_id": 801347, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 05:46:00", "end_date_time": "2019-03-06 11:46:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported a rock slide covering the traffic lanes on State Route 178 at Walker Pass.", "ts_dict_index": [78, 79, 80]}
+{"event_id": 801345, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 03:02:00", "end_date_time": "2019-03-07 12:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported about a foot of water, mud and debris covering the roadway at the intersection of Redrock-Randsburg Rd. and Garlock Rd.", "ts_dict_index": [84, 85, 86]}
+{"event_id": 801349, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 06:54:00", "end_date_time": "2019-03-08 12:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported a rock slide on State Route 155 between Aldercreek Campground and Greenhorn Summit.", "ts_dict_index": [75, 76, 77]}
+{"event_id": 801348, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 06:11:00", "end_date_time": "2019-03-06 09:11:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported a large amount of water and mud across the roadway on Western Minerals Rd. near Hazelton.", "ts_dict_index": [87, 88, 89]}
+{"event_id": 801354, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2019-03-06 18:30:00", "end_date_time": "2019-03-06 22:30:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported State Route 41 was closed between State Route 145 and Road 200 due to a large boulder blocking the roadway.", "ts_dict_index": [102, 103, 104]}
+{"event_id": 1063338, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-05 12:00:00", "end_date_time": "2023-01-05 18:00:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Tulare County Sheriffs reported a small rock slide on Pleasant Oak Dr. near the intersection with SR 190.", "ts_dict_index": [108, 109, 110]}
+{"event_id": 801343, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-05 23:27:00", "end_date_time": "2019-03-08 12:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported a large boulders in both lanes blocking State Route 178 at Democrat Blvd.", "ts_dict_index": [90, 91, 92]}
+{"event_id": 1061849, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-27 09:00:00", "end_date_time": "2022-12-27 10:00:00", "narrative": "A strong upper low pressure system moved through California on December 27. This system had abundant moisture associated with it as it pulled up a deep fetch of moisture of tropical origin. This system brought widespread moderate to heavy precipitation to the area between the early morning until the early evening of December 27. The heavy rainfall produced a rockslide in Yosemite National Park which resulted in two fatalities. The precipitation tapered off by the early morning of December 28. Much of the higher Sierra Nevada picked up between an inch and a half and three inches of liquid precipitation with the precipitation mainly falling as snow above 7500 feet where many stations picked up between 18 and 30 inches of new snowfall. The snow level briefly lowered to around 6000 feet during the evening of December 27 and some light snowfall was observed between 6000 and 7500 feet. The Sierra foothills generally received between 1 to 2 inches of rain while 0.75 to 1.5 inches of rain fell in the San Joaquin Valley and the Tehachapi Mountains. Several reports of nuisance flooding were reported by law enforcement and on social media. Rain shadowing effects limited precipitation in the Kern County Deserts to a quarter inch or less. This system also brought some strong wind gusts to the mountains as several stations measured gusts exceeding 40 mph and a few low impact stations had brief gusts above 60 mph. Yosemite National Park employees reported two people were killed by a rockslide near the intersection of SR 140 and Big Oak Flat Road in Yosemite National Park.", "ts_dict_index": [117, 118, 119]}
+{"event_id": 793397, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-01-17 08:44:00", "end_date_time": "2019-01-17 11:44:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. California Highway Patrol reported Tulare County Fire Department response unit reported a land slide along Dry Creek Dr. and State Route 216 west of Lemon Cove.", "ts_dict_index": [123, 124, 125]}
+{"event_id": 801351, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 08:34:00", "end_date_time": "2019-03-08 12:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported a creek over flowing across Sierra Vista Dr. in Wofford Heights and a mudslide was completely covering propane tanks.", "ts_dict_index": [105, 106, 107]}
+{"event_id": 1063220, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-04 16:32:00", "end_date_time": "2023-01-04 18:32:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. California Highway Patrol reported a large boulder on the northbound lane of SR 178 near Edison.", "ts_dict_index": [111, 112, 113]}
+{"event_id": 801360, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 07:51:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooded with water, debris and trees at the intersection of Bodfish Canyon Rd. and Lake Isabella Blvd.", "ts_dict_index": [99, 100, 101]}
+{"event_id": 801362, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 08:01:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported State Route 155 and Granite Rd. in Glennville closed due to a mudslide and rock slide in the area.", "ts_dict_index": [96, 97, 98]}
+{"event_id": 805128, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "SAN BERNARDINO", "begin_date_time": "2019-01-17 10:30:00", "end_date_time": "2019-01-17 13:30:00", "narrative": "A high impact mini atmospheric river impacted Southern California January 14th and 15th which brought heavy rain and snow to the region. Seal Beach reported 2 inches of rain in 2 hours, which caused extensive flash flooding. Water was up to doorways outside of homes, and the Pacific Coast Highway was closed for over a day in Huntington Beach due to flooding. Rainfall rates remained below flash flood thresholds at the Holy and Cranston burn scars during this mini-AR event. Dense fog was reported in the Cajon Pass on the morning of January 16th, which resulted in a 19-car pileup and 35 patients with minor to moderate injuries. ||A larger atmospheric river moved into Southern California on January 17th, bringing heavy rain and snow to the region. Extensive flash flooding occurred due to the heavy rain. Swift water rescues occurred on the Santa Ana River in Riverside due to flooding. Rainfall rates exceeded flash flooding thresholds for the Holy fire burn scar on the 17th.||Overall, 6 to 12 inches of rain fell in the Santa Ana and San Bernardino County Mountains between January 14-17. Snowfall amounts in the mountains ranged from 4 to 12 inches above 6500 ft. Major surf and coastal flooding occurred during this event as well, which resulted in extensive damage of the Ocean Beach Pier in San Diego County. CalTrans reported a mud/rock slide on Highway 18 at Live Oak Drive due to heavy rain.", "ts_dict_index": [135, 136, 137]}
+{"event_id": 1061468, "event_type": "Debris Flow", "state": "ALASKA", "cz_name": "HAINES BOROUGH", "begin_date_time": "2022-10-01 00:11:00", "end_date_time": "2022-10-01 07:00:00", "narrative": "Southeast Alaska had been impacted by a number of atmospheric rivers through September to keep streamflow on small and large rivers high. Another atmospheric river lifted out of the north Pacific as the associated warm front moved over Southeast Alaska it produced heavy rain over the northern inner channels of the panhandle. The front also advected a lot of warm air with freezing levels near 10 thousand feet. The complex terrain of the region enhance the rainfall with 1.5 to 3.5 inches of rain fell over a 12 to 18 hour period. ||The heavy rain and significant ice melt from the very warm temperatures in the headwaters of the Taiya River produced a lot of overland flow. This caused moderate flooding along the Taiya River from the early morning hours to the late afternoon on October 1st. There was road closures, damage to National Park Service infrastructure along the Chilkoot trail and near the Dyea campground. This was also the 4th highest peak flood on record. There was also moderate flooding along Jordan Creek in Juneau from the early morning to the afternoon hours on October 1st. The crested was the 2nd highest peak flood on record. A large landslide along the Haines Highway around 23 mile that came down in the overnight hours of October 1st and blocked the road. The area around the landslide reported 1 to 1.5 inches of rain in 12 hours. Heavy rain was falling over the Chilkat Valley with 1 inch of rain falling in a 6 hour time frame. By Saturday morning on October 1st the Haines Police and Alaska DOT reported that a landslide came down during the overnight hours around 23 mile along the Haines Highway and blocked both lanes. It took all day for DOT to reopen the highway.", "ts_dict_index": [132, 133, 134]}
+{"event_id": 793423, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2019-01-16 20:30:00", "end_date_time": "2019-01-17 06:30:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. State Route 140 was already closed in advance as a Flash Flood Watch was issued for the Ferguson Fire burn area. Approximately 50 yards of debris had to be removed from State Route 140 west of the Yosemite Park entrance as heavy rains resulted in debris flow across the burn area.", "ts_dict_index": [120, 121, 122]}
+{"event_id": 932483, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 22:46:00", "end_date_time": "2021-01-27 23:16:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Semi was trying to make a u-turn and got stuck in mud sticking out into the road.", "ts_dict_index": [138, 139, 140]}
+{"event_id": 932441, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 15:09:00", "end_date_time": "2021-01-27 16:09:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Mudslide on River Road 1/2 mile NW of Chualar River Rd. Photos show damage to nearby homes and structures.", "ts_dict_index": [144, 145, 146]}
+{"event_id": 932440, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 14:00:00", "end_date_time": "2021-01-27 16:00:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Video shows debris flow in Anderson Canyon this afternoon, exact timing unknown but estimated between 2 and 4 pm.", "ts_dict_index": [147, 148, 149]}
+{"event_id": 932438, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 11:30:00", "end_date_time": "2021-01-27 12:30:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Mudslide on US-101 S and Camp Roberts, closure of road.", "ts_dict_index": [150, 151, 152]}
+{"event_id": 793398, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-01-17 11:50:00", "end_date_time": "2019-01-17 14:50:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. Public reports of several large rocks on the Caliente Bodfish Road and Caliente Creek Road Fork northeast of Caliente.", "ts_dict_index": [126, 127, 128]}
+{"event_id": 932437, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 10:40:00", "end_date_time": "2021-01-27 11:40:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Mudslide onto Hwy 1 at mile marker 27.", "ts_dict_index": [153, 154, 155]}
+{"event_id": 793399, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-01-17 16:10:00", "end_date_time": "2019-01-17 18:10:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. California Highway Patrol reported mud, dirt and rocks effecting Burlando Road and Kern River Dr. in Kernville.", "ts_dict_index": [129, 130, 131]}
+{"event_id": 932501, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "SANTA CRUZ", "begin_date_time": "2021-01-29 00:00:00", "end_date_time": "2021-01-29 00:30:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. A mudslide occurred in the Aptos Hills on Valencia School Rd around midnight. A 50 foot section of a rain soaked roadway gave way and a PG&E rig fell about 150 feet down the hillside https://www.ksbw.com/article/santa-cruz-utility-worker-tumbles-down-150-foot-hillside-during-landslide/35369366.", "ts_dict_index": [162, 163, 164]}
+{"event_id": 932491, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-28 10:30:00", "end_date_time": "2021-01-28 15:00:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Photo on twitter showed debris flow on Highway 1 at Rat Creek within the Dolan Burn Scar area. Over 15 inches of rain fell near the area contributing to a large section of Highway 1 collapsing into the Pacific Ocean later that day. Exact cost of repairs is unknown, the section of highway will likely remain closed for months https://www.kron4.com/news/california/when-hwy-1-collapses-by-big-sur-caltrans-engineers-face-unique-challenges/.", "ts_dict_index": [159, 160, 161]}
+{"event_id": 1116689, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 11:02:00", "end_date_time": "2023-08-20 14:02:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported a large rock on Interstate 5 south of Lebec.", "ts_dict_index": [114, 115, 116]}
+{"event_id": 932435, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 05:30:00", "end_date_time": "2021-01-27 06:30:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Mud flowing onto the road near 645 River Rd.", "ts_dict_index": [165, 166, 167]}
+{"event_id": 932489, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 00:00:00", "end_date_time": "2021-01-27 02:00:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Emergency manager sent photographs early Wednesday morning of flooding/mud flow on Pine Canyon Rd near Mesa. Exact timing of flooding/debris flow uncertain.", "ts_dict_index": [156, 157, 158]}
+{"event_id": 1062422, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2022-12-31 22:09:00", "end_date_time": "2022-12-31 23:59:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a lot of rocks and mud in the roadway on SR 216 at  Dry Creek.", "ts_dict_index": [192, 193, 194]}
+{"event_id": 1062291, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2022-12-31 14:30:00", "end_date_time": "2022-12-31 17:30:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a mudslide at the intersection of SR 41 and Hodges Hill Dr. in Oakhurst.", "ts_dict_index": [189, 190, 191]}
+{"event_id": 932442, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 15:14:00", "end_date_time": "2021-01-27 16:14:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Mudslide on River Rd and Foothill Rd, road closed.", "ts_dict_index": [177, 178, 179]}
+{"event_id": 932436, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 10:25:00", "end_date_time": "2021-01-27 11:45:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Mudslide from the River Fire burn scar. Crews worked to rescue residents and their animals (at least 50 large animals were in need of rescue). People were blocked into their homes with mild to moderate damage reported at at least 20 homes (exact amount unknown) with one homeowner injured and taken to the hospital https://www.ksbw.com/article/animals-being-rescued-people-trapped-in-their-homes-from-mudslide-near-river-fire-burn-scar/35337056 - https://abc7news.com/weather/homes-damaged-several-rescued-after-mudslide-in-monterey-co/10073282/ .", "ts_dict_index": [174, 175, 176]}
+{"event_id": 932503, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "SANTA CRUZ", "begin_date_time": "2021-01-29 04:00:00", "end_date_time": "2021-01-29 04:30:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. A mudslide occurred in the Aptos Hills Area causing damage to a home. A truck was pushed into an additional structure. Exact time and location of the slide is unknown https://www.ksbw.com/article/mother-newborn-escape-mudslide-in-aptos-hills/35369344.", "ts_dict_index": [168, 169, 170]}
+{"event_id": 932485, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "SANTA CRUZ", "begin_date_time": "2021-01-28 04:24:00", "end_date_time": "2021-01-28 04:54:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Mud/dirt/rock in 2nd between Jarvis and Sugarloaf.", "ts_dict_index": [171, 172, 173]}
+{"event_id": 1058907, "event_type": "Debris Flow", "state": "ALASKA", "cz_name": "HAINES BOROUGH", "begin_date_time": "2022-09-26 08:00:00", "end_date_time": "2022-09-26 23:00:00", "narrative": "An atmospheric river moved out of the north Pacific into the Gulf of Alaska September 25th and started to impact the northern half of the Southeast Alaska's panhandle. This event brought in very high amounts of moisture, winds and very warm temps through September 27th. These warm temps rose the freezing levels to be above 9 thousand feet to increase the amount of melt from glacier in headwaters of the Taiya River. Rain amounts from this event ranged from 3 to 5 inches in 36 hours. The heavy rain and high freezing levels produced significant amounts of runoff to cause moderate flood along the Taiya River near Skagway in Dyea and around the Jordan Creek area near Juneau from mid morning on September 26th through the morning of September 27th. ||As the front moved through the area there was a wind shift in the afternoon hours of September 26th and with the ground very wet from the heavy rain caused a tree to fall which triggered a shallow landslide in downtown Juneau to damaged 3 homes. The heavy rain also triggered a landslide near mile marker 26 along the Haines Highway Monday afternoon and 2 near mile marker 31 along Glacier Highway in Juneau one around 1700AKST and then again in the early morning of September 27th. During the early morning hours of September 26th a large landslide came down along the Haines Highway around 23 mile and blocked the highway. AKDOT was on site by day break to assess the situation and begin to clear the material. The highway was reopened by the afternoon. Six hour rainfall amounts ranged from 0.50 to as much as 1.75 at higher elevation. This is after the area had been experiencing heavy rainfall.", "ts_dict_index": [180, 181, 182]}
+{"event_id": 1062290, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2022-12-31 14:30:00", "end_date_time": "2022-12-31 17:30:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a rockslide at the intersection of SR 41 and Coyote Hollow Dr. near Coarsegold.", "ts_dict_index": [219, 220, 221]}
+{"event_id": 1062426, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 23:16:00", "end_date_time": "2022-12-31 23:59:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a large mudslide blocking the westbound lanes on SR 140 in Midpines.", "ts_dict_index": [204, 205, 206]}
+{"event_id": 1062286, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 13:41:00", "end_date_time": "2022-12-31 13:41:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported debris and water collecting on the roadway at the intersection of SR 49 and Usona Dr.", "ts_dict_index": [195, 196, 197]}
+{"event_id": 1062389, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 19:00:00", "end_date_time": "2022-12-31 22:00:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a mudslide blocking portions of Hunters Springs Rd.", "ts_dict_index": [237, 238, 239]}
+{"event_id": 1062434, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-01 00:16:00", "end_date_time": "2023-01-01 03:16:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a few feet of mud on part of SR 41 near Tenaya Lodge in Oakhurst.", "ts_dict_index": [240, 241, 242]}
+{"event_id": 909901, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-08-27 10:00:00", "end_date_time": "2020-08-27 11:15:00", "narrative": "Major Hurricane Laura tracked north northwest across the Central and Northern Gulf of Mexico from the Central Carribean Sea near Cuba, making landfall in Southwest Louisiana near Cameron around 1 am on August 27th as a strong Category 4 hurricane with maximum sustained winds near 150 mph, and a minimum central pressure of 938 mb. Laura remained a hurricane as it tracked north across Southwest and Central Louisiana and into Natchitoches Parish, before weakening to a tropical storm as it moved northeast across North-central Louisiana and South-central Arkansas. A combination of observed and estimated wind gusts ranged from 50-90+ mph, resulting in numerous to widespread downed trees and power lines over these areas throughout the morning and early afternoon, before winds weakened by mid-afternoon with the departure of Laura into Southern Arkansas. Widespread rainfall amounts of 2-6 inches was observed across North Louisiana, with higher amounts of 6-8+ inches recorded across Southern and Western DeSoto, Sabine, Natchitoches, Western Grant, Winn, Jackson, and Eastern Bienville Parishes. Flooding was mostly confined to Natchitoches and Western Caddo Parishes.||Here are the peak wind gusts at various automated stations across the affected areas of North Louisiana: ||Gum Springs RAWS (Winn Parish), 70 mph (Incomplete data due to power failure) |Natchitoches (Natchitoches Parish), 66 mph (Incomplete data due to power failure)|Shreveport Regional Airport (Caddo Parish), 66 mph |Monroe (Ouachita Parish), 62 mph (Incomplete data due to power failure)|Ouachita Christian School (Ouachita Parish), 62 mph |Benton (Bossier Parish), 61 mph|Mansfield (DeSoto Parish), 59 mph |Shreveport Downtown Airport (Caddo Parish), 58 mph|Red River Research Station (Bossier Parish), 58 mph |Catahoula RAWS (Grant Parish), 56 mph (Incomplete data due to power failure)|The University of Louisiana-Monroe, Hanna Hall (Ouachita Parish), 55 mph |Bossier City, Barksdale Air Force Base (Bossier Parish), 55 mph |South Bossier City, LSU Research Station (Bossier Parish), 48 mph|Ruston (Lincoln Parish), 44 mph (Incomplete data due to power failure) ||During the peak of the widespread power outages shortly after Laura's center of circulation exited North Louisiana during the afternoon of the 27th, 136,000 customers were without power in Western Louisiana, East Texas, and Southwest Arkansas, with nearly 108,000 Entergy customers without power across North-central and Northeast Louisiana, as well as South-central Arkansas.||Preliminary damage estimates from the LSU AgCenter indicate that Hurricane Laura caused $525.4 million in damage to Louisiana farmers, and $1.1 billion to the Louisiana timber industry, more than Hurricanes Katrina and Rita combined in 2005. Grant Parish alone was 4th in the state with the amount of timber lost, with over $111 million. Entergy reported that Hurricane Laura caused $1.7 billion to its infrastructure throughout Louisiana. ||Here are the known damage across various parishes affected in North Louisiana: ||Caddo Parish: Numerous trees and power lines down parishwide, including the city of Shreveport. Homes were sporadically damaged across the parish from fallen trees. A large tree fell on a home on Ratcliff Drive in Shreveport, causing extensive structural damage and injuring one person. Trees also fell on homes across various locations in Shreveport including West Montego Lane, Tynneside Way, Burgandy Oaks Drive, Nona Circle, and Centenary Blvd, with a large pine tree falling/crushing a truck on Midvale Drive near Ridgewood Drive. A metal building behind a large church in Meriweather Road near West 70th Street has half of its roof peeled off. The shoulder of Interstate 20 at Exit 5 in Greenwood was flooded.  ||Bossier Parish: Numerous trees and power lines down parishwide. Homes were sporadically damaged across the parish from fallen trees. ||DeSoto Parish: Numerous trees and power lines down parishwide. A metal roof was damaged on a home in Mansfield. ||Red River Parish: Numerous trees and power lines down parishwide. Power outages to nearly 100 percent of parish residents. ||Bienville Parish: Numerous trees and power lines down parishwide. Power outages to nearly 100 percent of parish residents. ||Webster Parish: Numerous trees and power lines down parishwide. Over 220 reports of incidents from trees down across the parish. The roof was partially blown off of the El Jimador restaurant in Minden.||Claiborne Parish: Numerous trees and power lines down parishwide. Power outages to nearly 100 percent of parish residents. ||Lincoln Parish: Scattered tree damage across most of the parish with more sporadic damage across the western portions of the parish. Tree damage mostly occurred from uprooted trees, with some tree trunks snapped. A tree was blown down onto a home in Ruston. The awning of an Exxon gas station was blown off along Highway 167 north of Ruston. Power outages to nearly 100 percent of parish residents. ||Union Parish: Numerous trees and power lines were down parishwide. Power outages to more than 90 percent of parish residents. ||Ouachita Parish: Numerous trees and power lines down parishwide. Power outages to nearly 80 percent of parish residents. Some trees fell on homes in West Monroe and Monroe. The awning at a Chevron gas station in West Monroe was significantly damaged. The damage and power outages led to the cancellation of classes at the University of Louisiana-Monroe for the following week. ||Jackson Parish: Numerous trees were down across the parish, particularly across the southern portion of the parish and to exposed areas along Caney Creek Reservoir in the Jimmie Davis State Park. One tree fell into a single wide mobile home and killed a 51 year old male on Ayres Loop in Jonesboro. The sustained winds bent trees and the brief stronger winds gusts helped contribute to the tree snaps in the Jimmie Davis State Park. The tree falls generally ranged from the southwest to west-southwest. Power outages to nearly 100 percent of parish residents. ||Caldwell Parish: Multiple trees and power lines down on Highway 4 West between Wiles Road and Mount Pleasant Road, as well as others areas throughout the parish. ||Winn Parish: Scattered to widespread tree damage across the parish, particularly across the central and western portions of the parish which were impacted by the eastern edge of Laura's center of circulation. The tree damage in Winnfield was significant with mostly uproots and some snaps. A few incidents of structural roof damage not caused by downed trees was observed. The tree fall ranged from the northwest to the southwest. Power outages to nearly 100 percent of parish residents. ||La Salle Parish: Scattered to numerous tree damage throughout the parish. A few incidents of structural damage not caused by downed trees were observed in Jena. The Jena High School Gymnasium lost a significant portion of its roofing material, with some damage to signs in front of the school. The awning covering a portion of the parking lot of a local Jena business was destroyed. Trees were also blown down onto homes and vehicles in Jena. The tree fall ranged from the northwest to northeast as the center of Laura's circulation passed just west of the parish. Power outages to nearly 100 percent of parish residents. ||Grant Parish: Scattered to widespread tree damage in the parish, particularly across the central and western portions of the parish which were impacted by the eastern edge of Laura's circulation. A few incidents of structural damage not caused by downed trees were observed, particularly around Dry Prong where a cluster of metal building systems lost a significant portion of roof panels. The most concentrated tree damage (and related home and electrical infrastructure damage related to tree fall) occurred between Dry Prong and the Bentley community along Rob Wallace Road. The tree fall ranged from the west through the northeast, suggesting wind damage was occurring both preceding and in wake of Laura's center of circulation. Power outages to nearly 100 percent of parish residents. ||Natchitoches Parish:Scattered to widespread tree damage in the parish, particularly across the southern and eastern portions of the parish which were impacted by the northern and eastern edge of Laura's center of circulation. The most concentrated damage observed was in Cloutierville and Natchez and locations between these communities along the Cane River. In Cloutierville, hardwood and softwood trees were snapped and uprooted around many homes. In Natchez, most trees were uprooted, while some were snapped. The roof was blown off of the Police Dept. in Robeline. Interstate 49 was closed near Highway 174 due to a fallen tree across the interstate at mile marker 154. Power outages to nearly 100 percent of parish residents. Widespread flooding was reported across much of the parish. Widespread flooding was observed across many areas of the parish. ||Sabine Parish: Scattered tree damage across most of the parish with more widespread damage across the southeastern corner of the parish and exposed areas to the open waters of Toledo Bend Reservoir in the far southwest part of the parish. Damage included snapped trees, roof damage to an apartment complex, and clusters of uprooted trees. The tree fall throughout the parish ranged from south to south-southeast. Power outages to nearly 100 percent of parish residents. I-20 at Exit 5 was covered in high water.", "ts_dict_index": [261, 262, 263]}
+{"event_id": 1000078, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "SANTA CRUZ", "begin_date_time": "2021-12-13 10:40:00", "end_date_time": "2021-12-13 11:40:00", "narrative": "A low pressure system descended from the Gulf of Alaska southward along the entire Pacific Coast and tapped into sub-tropical moisture originating from the Central Pacific to drop heavy rain throughout the state. A stalled frontal boundary over the Santa Cruz Mountains along with strong southerly winds from a coastal low-level jet, enhanced orographic rainfall over this region, leading to rainfall totals over a 2 day period (Dec 12th-13th) of up to ten inches in the coastal mountains. The stalled boundary was reinvigorated by a secondary boundary bringing in a cold unstable airmass that set off convective showers and lowered snow levels below 2000 ft. A wind advisory, later upgraded to a high wind warning was issued for the southern half of the region from the SF Peninsula down to the Big Sur Coast including the inland zones due to the coastal jet bringing sustained winds up to 40 mph with gusts up to 55 mph. A high surf advisory was issued for the entire coast due to the arrival of a strong NW swell train, along with Gale Warning throughout the coastal waters. A flash flood watch was issued for the Santa Lucia Mountains and Dolan Burn Scar area, where up to 12 inches of rain fell. Video, https://www.youtube.com/watch?v=4LFZJqrqidw, of rapid debris flow in Boulder Creek area, 200 ft from where Foreman Creek crosses under SR236. Creek runs through part of the CZU burn scar area.", "ts_dict_index": [255, 256, 257]}
+{"event_id": 1062419, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-12-31 21:29:00", "end_date_time": "2022-12-31 23:59:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a mudslide at the intersection of Lebec Rd. and Landslide Rd.", "ts_dict_index": [249, 250, 251]}
+{"event_id": 1065767, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-14 15:53:00", "end_date_time": "2023-01-14 17:53:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported the roadway washed out with several vehicles stuck on SR 33 between Brown Material Rd. and SR 46.", "ts_dict_index": [258, 259, 260]}
+{"event_id": 962305, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2021-06-06 19:00:00", "end_date_time": "2021-06-06 22:00:00", "narrative": "Hit and miss thunderstorms ramped up on the 6th. Two to more than three inches of rain was measured at Cane Creek State Park (Lincoln County), Fordyce (Dallas County), Monticello (Drew County), Nashville (Howard County), and Pine Bluff (Jefferson County). Several roads were under water between Avilla (Saline County) and Ferndale (Pulaski County), and also at Monticello (Drew County).||During the predawn hours of the 7th, thunderstorm winds downed a tree on Highway 53 just south of Gurdon (Clark County). This caused a log truck to overturn. In the afternoon, more trees were toppled in Camden and East Camden (both in Ouachita County). A chapel roof was damaged just southwest of Cummins (Lincoln County), and part of a roof was blown off close to Sorrells (Jefferson County).||At least a dozen Tornado Warnings were issued in portions of Calhoun, Clark, Cleveland, Dallas, Garland, Hot Spring, Montgomery, Ouachita, and Pike Counties. A funnel cloud was spotted by law enforcement at Gum Springs (Clark County). There was a brief tornado reported (rated EFU, where U is unknown because there was no damage to evaluate) to the west of Calion (Union County) at 426 pm CDT. The tornado apparently did little more than kick up some dust.||On the 8th, there was a life threatening deluge in southeast Arkansas. Showers and thunderstorms became widespread, and moved over the same areas for several hours.||Too much rain flooded roads at Star City and Varner (both in Lincoln County), Pine Bluff (Jefferson County), Stuttgart (Arkansas County), and also at Dumas and McGehee (both in Desha County). Water got into many homes. Crop and road damage (washouts) was reported in Bradley County. A creek was out of its banks just southeast of Timber Ridge (Pulaski County).||There was high water along Highway 114 between Calmer and Rison (both in Cleveland County), Highway 425 near Yorktown (Lincoln County), Highway 293 east of Garrett Bridge (Lincoln County), Highway 46 not far from Ebb (Grant County), Highway 276 on the south side of Stuttgart (Arkansas County), and Highway 1 at Kelso (Desha County). These highways were eventually closed temporarily.||The situation was the most serious in Desha and Drew Counties, and a Flash Flood Emergency was issued for the communities of Dumas, Pickens, Rohwer (all in Desha County), and Winchester (Drew County) at 1142 am CDT on the 8th. Radar estimated 10 to more than 15 inches of rain, and there was water everywhere. Some folks indicated (through social media) they had never witnessed flooding of this magnitude.||From an historic perspective, Rohwer (Desha County) received 9.25 inches of rain in the twenty four hour period ending at 700 am CDT on the 8th. This was the most rain in one day at the site, and the fourth largest one day total across the state in June. If that was not enough, 9.97 inches of liquid was measured the next day! Adding the numbers, the whopping 19.22 inches on the 8th/9th was the second biggest two day amount in Arkansas. It was just behind the 21.45 inches at Danville (Yell County) on December 3-4, 1982.||Relentless cloudbursts continued to start the 9th in eastern Arkansas. A rain gauge near DeValls Bluff (Prairie County) completely filled (to six inches) between 400 am and 700 am CST. Buildings were flooded and cars were stalled in Clarendon (Monroe County). It was the same story in Humnoke (Lonoke County), and sandbags were ordered to stop the water.||It was just getting worse in Stuttgart (Arkansas County), with one picture showing more water in a home than ever before (in the life of the photographer/42 years). That claim was likely true because the 7.50 inches of rain that caused the problem easily surpassed the previous one day June record of 4.07 inches on the 29th in 1939. At least fifteen homes were impacted by flooding at Altheimer (Jefferson County). Highway 302 from Highway 17 to Highway 79 was shut down in Monroe County, as was Highway 15 near Sherrill (Jefferson County), Highway 33 east of Tollville (Prairie County), and Highways 85 and 318 near Oneida (Phillips County).||As the weather calmed down in the east by the afternoon of the 9th, temperatures warmed well into the 80s to around 90 degrees across the northern and central counties. Heating and lots of humidity were enough to fuel isolated strong to severe storms toward evening.||Just after 700 pm CDT, a video showed a tornado (rated EFU) that lasted two minutes in a field near Blakemore (Lonoke County). Between 700 pm and 800 pm CDT, there was quarter size hail just east of College Station (Pulaski County). Little Rock (Pulaski County) got a quick 1.10 inches of rain. Trees were blown down at Cave City (Sharp County). At 805 pm CDT, there was a brief weak tornado (rated EF0) a few miles southeast of England (Lonoke County).||The focus shifted back to the southeast early on the 10th. You guessed it...the sky was falling again. Rain plus runoff from the soaking on the 8th/9th in northern and central Desha County inundated farms toward Halley (Desha County) in the south. At 200 pm CDT, an irrigation canal east of Pickens (Desha County) was breached, and adjacent farmland became a lake. The canal was patched by evening. At Florence (Drew County), residents were forced to use boats to get around. Water threatened structures at Dermott and Eudora (both in Chicot County), and sandbagging was in progress. It was clear that assistance was needed, and Arkansas Governor Asa Hutchinson declared a state of emergency. ||All was quiet quiet in Little Rock (Pulaski County) on the 10th, and the sun was out. For the first time in 2021, the temperature touched 90 degrees (the high was 92 degrees), and it was three weeks late (it normally happens by May 18th). Toward evening, it got loud toward Pinnacle Mountain (Pulaski County). A severe storm pumped out quarter size hail, winds strong enough to push over a few trees, and up to six inches of rain in less than two hours. The terrain accentuated the flow of water across roads and into neighborhoods. A picture on social media showed water moving across a neighborhood road in Ferndale.", "ts_dict_index": [273, 274, 275]}
+{"event_id": 1087202, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2023-03-02 21:06:00", "end_date_time": "2023-03-03 00:06:00", "narrative": "March certainly roared in like a lion across the state with back to back severe weather events on March 1st and 2nd into the 3rd. Storms on these days led to a few tornadoes as well as hail as large as 3 inches in diameter. Very heavy rainfall was noted across the area as well which led to flash flooding and widespread river flooding. One fatality occurred because of the flooding in Scott County on March 2nd. ||As the air heated up, and the atmosphere destabilized, severe thunderstorms were triggered by the front during the late afternoon and evening. The storms produced very large hail, and also caused spotty wind damage. Hail slightly larger than baseballs was reported at Woodlawn (Cleveland County), with ping pong ball size stones near Benton (Saline County) and west of Stuttgart (Arkansas County), and half dollar size hail a few miles north of Norman (Montgomery County). At Rison (Cleveland County), wind gusts up to 85 mph ripped the roof off of a church and a strip mall. Part of a brick facade was removed from latter structure. Trees were also toppled, with one tree blocking Highway 79.||The front on the 1st advanced toward the Louisiana border and stalled. The front was followed by cooler air. On the 2nd, all eyes were on a powerful storm system in the southern Rockies. In response to the approaching system, the front began lifting back to the north. By 400 pm CST, the front cleared the southern counties, and temperatures warmed into the 70s. However, readings north of Little Rock (Pulaski County) were mostly in the 50s.||As the system neared in the late afternoon, it interacted with the front and round two of thunderstorms commenced from central/northeast Texas into southeast Oklahoma. Eventually, storms congealed into a line and raced toward Arkansas. As the storms progressed into the state after dark, it was clear that severe weather (including tornadoes) was most likely south of the front (in mild air), with mainly heavy to excessive rain farther north (where cooler conditions existed).||Between 900 pm and 1000 pm CST, trees were pushed over by straight-line winds west of Y City (Scott County). About this time, rain was coming down in buckets across Scott and Yell Counties, and numerous roads were flooded/about to flood. At Boles (Scott County), there was a report of people surrounded by water and unable to leave their home.||As the night wore on, the Poteau River at Cauthron (Scott County) rose 15 feet in a hurry. The same swollen river swept a pickup truck off of Highway 80 on the east side of Waldron (Scott County). Tragically, the driver (a grandfather trying to visit his grandson) drowned. A traffic camera (provided by the Arkansas Department of Transportation) along Highway 71 south of Boles (Scott County) showed the Fourche La Fave River almost as high as the bridge over the tributary. Eventually, the pavement was inundated and became impassible. As roads turned into lakes, a vehicle stalled at Parks (Scott County), and two individuals were rescued. Similar rescues were ongoing in Yell County, and one person was transported from Corinth to a hospital in Danville (both in Yell County).||Shortly before 1100 pm CST, a tornado (rated EF2) was spawned just to the north of Kirby (Pike County). A few mobile homes were heavily damaged (resulting in three injuries). One mobile home was rolled and obliterated. Miraculously, two of the four occupants only had minor injuries. Several homes suffered roof damage, and two chicken houses were destroyed.||A couple of hours later, thunderstorm winds downed/snapped trees along Highway 229 about four miles north of Carthage (Dallas County). A few minutes before 200 am CST on the 3rd, a brief weak tornado (rated EF0) touched down in open fields east of Altheimer (Jefferson County). The tornado took out some trees along Highway 58.||Elsewhere, a weak tornado (rated EF1) was identified west of Fouke (Miller County). More trees were blown down southwest of Hope (Hempstead County) and northeast of Nashville (Howard County). Wind gusts as high as 70 to 80 mph roughed up barns, outbuildings, and signs between Damascus (Faulkner/Van Buren Counties) and Rose Bud (White County). A recreational vehicle was crushed by a fallen tree at Enola (Faulkner County).||As far as rain, there was a lot of it. Two to more than four inches of rain was common across the northern half of the state in the twenty four hour period ending at 600 am CST on the 3rd. Waldron (Scott County) had 4.90 inches of precipitation, with 4.88 inches at Blue Mountain Dam (Yell County), 4.72 inches at Danville (Yell County), 4.45 inches at Abbott (Scott County), 4.22 inches at Dardanelle (Yell County), 3.87 inches at Booneville (Logan County), 3.70 inches at Mountain View (Stone County), 3.65 inches at Gilbert (Searcy County), 3.57 inches at Calico Rock (Izard County), 3.54 inches at Mena (Polk County), 3.50 inches at Damascus (Van Buren County), 3.47 inches at Marshall (Searcy County) and Morrilton (Conway County), and 3.40 inches at Conway (Faulkner County).||Given so much rain, there was a landslide near the intersection of Highways 103 and 215 west of Oark (Johnson County). Before dawn on the 3rd, the Spring River at Hardy (Sharp County) went up six feet in two hours, was in danger of reaching a level of 14 feet (four feet above the flood stage). As a precaution, folks in homes near the river were asked to evacuate. ||The rain on the 2nd/early on the 3rd was in addition to the precipitation that fell on the 1st, especially from central into southeast Arkansas. In this part of the state, two or more inches of liquid was measured in places. This included Cane Creek State Park (Lincoln County), Keo (Lonoke County), Marianna (Lee County), Pine Bluff (Jefferson County), Sheridan (Grant County), and Stuttgart (Arkansas County).||On the 3rd, there was moderate to major flooding on the Petit Jean River, and minor to moderate flooding on the Black, Cache, Fourche La Fave, Little Red, Ouachita, Saline, Spring, and White Rivers. Concerns were growing that river levels could go even higher if a wet pattern continued into early spring. Numerous roads have been flooded throughout Scott County. However, in Boles there was a report that some people were isolated in their home due to rising flood waters. A man was found drowned the next day when flood waters began to recede, so the timing of death is uncertain. His age is unknown, but he was likely an older adult as he was described as a grandfather. He likely drove into floodwaters and got washed off the road sometime between the night of the 2nd and the morning of the 3rd.", "ts_dict_index": [264, 265, 266]}
+{"event_id": 1087267, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2023-03-02 23:40:00", "end_date_time": "2023-03-03 02:40:00", "narrative": "March certainly roared in like a lion across the state with back to back severe weather events on March 1st and 2nd into the 3rd. Storms on these days led to a few tornadoes as well as hail as large as 3 inches in diameter. Very heavy rainfall was noted across the area as well which led to flash flooding and widespread river flooding. One fatality occurred because of the flooding in Scott County on March 2nd. ||As the air heated up, and the atmosphere destabilized, severe thunderstorms were triggered by the front during the late afternoon and evening. The storms produced very large hail, and also caused spotty wind damage. Hail slightly larger than baseballs was reported at Woodlawn (Cleveland County), with ping pong ball size stones near Benton (Saline County) and west of Stuttgart (Arkansas County), and half dollar size hail a few miles north of Norman (Montgomery County). At Rison (Cleveland County), wind gusts up to 85 mph ripped the roof off of a church and a strip mall. Part of a brick facade was removed from latter structure. Trees were also toppled, with one tree blocking Highway 79.||The front on the 1st advanced toward the Louisiana border and stalled. The front was followed by cooler air. On the 2nd, all eyes were on a powerful storm system in the southern Rockies. In response to the approaching system, the front began lifting back to the north. By 400 pm CST, the front cleared the southern counties, and temperatures warmed into the 70s. However, readings north of Little Rock (Pulaski County) were mostly in the 50s.||As the system neared in the late afternoon, it interacted with the front and round two of thunderstorms commenced from central/northeast Texas into southeast Oklahoma. Eventually, storms congealed into a line and raced toward Arkansas. As the storms progressed into the state after dark, it was clear that severe weather (including tornadoes) was most likely south of the front (in mild air), with mainly heavy to excessive rain farther north (where cooler conditions existed).||Between 900 pm and 1000 pm CST, trees were pushed over by straight-line winds west of Y City (Scott County). About this time, rain was coming down in buckets across Scott and Yell Counties, and numerous roads were flooded/about to flood. At Boles (Scott County), there was a report of people surrounded by water and unable to leave their home.||As the night wore on, the Poteau River at Cauthron (Scott County) rose 15 feet in a hurry. The same swollen river swept a pickup truck off of Highway 80 on the east side of Waldron (Scott County). Tragically, the driver (a grandfather trying to visit his grandson) drowned. A traffic camera (provided by the Arkansas Department of Transportation) along Highway 71 south of Boles (Scott County) showed the Fourche La Fave River almost as high as the bridge over the tributary. Eventually, the pavement was inundated and became impassible. As roads turned into lakes, a vehicle stalled at Parks (Scott County), and two individuals were rescued. Similar rescues were ongoing in Yell County, and one person was transported from Corinth to a hospital in Danville (both in Yell County).||Shortly before 1100 pm CST, a tornado (rated EF2) was spawned just to the north of Kirby (Pike County). A few mobile homes were heavily damaged (resulting in three injuries). One mobile home was rolled and obliterated. Miraculously, two of the four occupants only had minor injuries. Several homes suffered roof damage, and two chicken houses were destroyed.||A couple of hours later, thunderstorm winds downed/snapped trees along Highway 229 about four miles north of Carthage (Dallas County). A few minutes before 200 am CST on the 3rd, a brief weak tornado (rated EF0) touched down in open fields east of Altheimer (Jefferson County). The tornado took out some trees along Highway 58.||Elsewhere, a weak tornado (rated EF1) was identified west of Fouke (Miller County). More trees were blown down southwest of Hope (Hempstead County) and northeast of Nashville (Howard County). Wind gusts as high as 70 to 80 mph roughed up barns, outbuildings, and signs between Damascus (Faulkner/Van Buren Counties) and Rose Bud (White County). A recreational vehicle was crushed by a fallen tree at Enola (Faulkner County).||As far as rain, there was a lot of it. Two to more than four inches of rain was common across the northern half of the state in the twenty four hour period ending at 600 am CST on the 3rd. Waldron (Scott County) had 4.90 inches of precipitation, with 4.88 inches at Blue Mountain Dam (Yell County), 4.72 inches at Danville (Yell County), 4.45 inches at Abbott (Scott County), 4.22 inches at Dardanelle (Yell County), 3.87 inches at Booneville (Logan County), 3.70 inches at Mountain View (Stone County), 3.65 inches at Gilbert (Searcy County), 3.57 inches at Calico Rock (Izard County), 3.54 inches at Mena (Polk County), 3.50 inches at Damascus (Van Buren County), 3.47 inches at Marshall (Searcy County) and Morrilton (Conway County), and 3.40 inches at Conway (Faulkner County).||Given so much rain, there was a landslide near the intersection of Highways 103 and 215 west of Oark (Johnson County). Before dawn on the 3rd, the Spring River at Hardy (Sharp County) went up six feet in two hours, was in danger of reaching a level of 14 feet (four feet above the flood stage). As a precaution, folks in homes near the river were asked to evacuate. ||The rain on the 2nd/early on the 3rd was in addition to the precipitation that fell on the 1st, especially from central into southeast Arkansas. In this part of the state, two or more inches of liquid was measured in places. This included Cane Creek State Park (Lincoln County), Keo (Lonoke County), Marianna (Lee County), Pine Bluff (Jefferson County), Sheridan (Grant County), and Stuttgart (Arkansas County).||On the 3rd, there was moderate to major flooding on the Petit Jean River, and minor to moderate flooding on the Black, Cache, Fourche La Fave, Little Red, Ouachita, Saline, Spring, and White Rivers. Concerns were growing that river levels could go even higher if a wet pattern continued into early spring. Two individuals were stranded and removed from a vehicle due to high water near Frost Lane.", "ts_dict_index": [267, 268, 269]}
+{"event_id": 1087239, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2023-03-02 22:23:00", "end_date_time": "2023-03-03 01:23:00", "narrative": "March certainly roared in like a lion across the state with back to back severe weather events on March 1st and 2nd into the 3rd. Storms on these days led to a few tornadoes as well as hail as large as 3 inches in diameter. Very heavy rainfall was noted across the area as well which led to flash flooding and widespread river flooding. One fatality occurred because of the flooding in Scott County on March 2nd. ||As the air heated up, and the atmosphere destabilized, severe thunderstorms were triggered by the front during the late afternoon and evening. The storms produced very large hail, and also caused spotty wind damage. Hail slightly larger than baseballs was reported at Woodlawn (Cleveland County), with ping pong ball size stones near Benton (Saline County) and west of Stuttgart (Arkansas County), and half dollar size hail a few miles north of Norman (Montgomery County). At Rison (Cleveland County), wind gusts up to 85 mph ripped the roof off of a church and a strip mall. Part of a brick facade was removed from latter structure. Trees were also toppled, with one tree blocking Highway 79.||The front on the 1st advanced toward the Louisiana border and stalled. The front was followed by cooler air. On the 2nd, all eyes were on a powerful storm system in the southern Rockies. In response to the approaching system, the front began lifting back to the north. By 400 pm CST, the front cleared the southern counties, and temperatures warmed into the 70s. However, readings north of Little Rock (Pulaski County) were mostly in the 50s.||As the system neared in the late afternoon, it interacted with the front and round two of thunderstorms commenced from central/northeast Texas into southeast Oklahoma. Eventually, storms congealed into a line and raced toward Arkansas. As the storms progressed into the state after dark, it was clear that severe weather (including tornadoes) was most likely south of the front (in mild air), with mainly heavy to excessive rain farther north (where cooler conditions existed).||Between 900 pm and 1000 pm CST, trees were pushed over by straight-line winds west of Y City (Scott County). About this time, rain was coming down in buckets across Scott and Yell Counties, and numerous roads were flooded/about to flood. At Boles (Scott County), there was a report of people surrounded by water and unable to leave their home.||As the night wore on, the Poteau River at Cauthron (Scott County) rose 15 feet in a hurry. The same swollen river swept a pickup truck off of Highway 80 on the east side of Waldron (Scott County). Tragically, the driver (a grandfather trying to visit his grandson) drowned. A traffic camera (provided by the Arkansas Department of Transportation) along Highway 71 south of Boles (Scott County) showed the Fourche La Fave River almost as high as the bridge over the tributary. Eventually, the pavement was inundated and became impassible. As roads turned into lakes, a vehicle stalled at Parks (Scott County), and two individuals were rescued. Similar rescues were ongoing in Yell County, and one person was transported from Corinth to a hospital in Danville (both in Yell County).||Shortly before 1100 pm CST, a tornado (rated EF2) was spawned just to the north of Kirby (Pike County). A few mobile homes were heavily damaged (resulting in three injuries). One mobile home was rolled and obliterated. Miraculously, two of the four occupants only had minor injuries. Several homes suffered roof damage, and two chicken houses were destroyed.||A couple of hours later, thunderstorm winds downed/snapped trees along Highway 229 about four miles north of Carthage (Dallas County). A few minutes before 200 am CST on the 3rd, a brief weak tornado (rated EF0) touched down in open fields east of Altheimer (Jefferson County). The tornado took out some trees along Highway 58.||Elsewhere, a weak tornado (rated EF1) was identified west of Fouke (Miller County). More trees were blown down southwest of Hope (Hempstead County) and northeast of Nashville (Howard County). Wind gusts as high as 70 to 80 mph roughed up barns, outbuildings, and signs between Damascus (Faulkner/Van Buren Counties) and Rose Bud (White County). A recreational vehicle was crushed by a fallen tree at Enola (Faulkner County).||As far as rain, there was a lot of it. Two to more than four inches of rain was common across the northern half of the state in the twenty four hour period ending at 600 am CST on the 3rd. Waldron (Scott County) had 4.90 inches of precipitation, with 4.88 inches at Blue Mountain Dam (Yell County), 4.72 inches at Danville (Yell County), 4.45 inches at Abbott (Scott County), 4.22 inches at Dardanelle (Yell County), 3.87 inches at Booneville (Logan County), 3.70 inches at Mountain View (Stone County), 3.65 inches at Gilbert (Searcy County), 3.57 inches at Calico Rock (Izard County), 3.54 inches at Mena (Polk County), 3.50 inches at Damascus (Van Buren County), 3.47 inches at Marshall (Searcy County) and Morrilton (Conway County), and 3.40 inches at Conway (Faulkner County).||Given so much rain, there was a landslide near the intersection of Highways 103 and 215 west of Oark (Johnson County). Before dawn on the 3rd, the Spring River at Hardy (Sharp County) went up six feet in two hours, was in danger of reaching a level of 14 feet (four feet above the flood stage). As a precaution, folks in homes near the river were asked to evacuate. ||The rain on the 2nd/early on the 3rd was in addition to the precipitation that fell on the 1st, especially from central into southeast Arkansas. In this part of the state, two or more inches of liquid was measured in places. This included Cane Creek State Park (Lincoln County), Keo (Lonoke County), Marianna (Lee County), Pine Bluff (Jefferson County), Sheridan (Grant County), and Stuttgart (Arkansas County).||On the 3rd, there was moderate to major flooding on the Petit Jean River, and minor to moderate flooding on the Black, Cache, Fourche La Fave, Little Red, Ouachita, Saline, Spring, and White Rivers. Concerns were growing that river levels could go even higher if a wet pattern continued into early spring. The emergency manager reported widespread 7 to 8 inch rainfall amounts across Scott County, the flood storage system was at full capacity, and main bridges across the county were under water.", "ts_dict_index": [270, 271, 272]}
+{"event_id": 962427, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2021-06-10 18:32:00", "end_date_time": "2021-06-10 21:32:00", "narrative": "Hit and miss thunderstorms ramped up on the 6th. Two to more than three inches of rain was measured at Cane Creek State Park (Lincoln County), Fordyce (Dallas County), Monticello (Drew County), Nashville (Howard County), and Pine Bluff (Jefferson County). Several roads were under water between Avilla (Saline County) and Ferndale (Pulaski County), and also at Monticello (Drew County).||During the predawn hours of the 7th, thunderstorm winds downed a tree on Highway 53 just south of Gurdon (Clark County). This caused a log truck to overturn. In the afternoon, more trees were toppled in Camden and East Camden (both in Ouachita County). A chapel roof was damaged just southwest of Cummins (Lincoln County), and part of a roof was blown off close to Sorrells (Jefferson County).||At least a dozen Tornado Warnings were issued in portions of Calhoun, Clark, Cleveland, Dallas, Garland, Hot Spring, Montgomery, Ouachita, and Pike Counties. A funnel cloud was spotted by law enforcement at Gum Springs (Clark County). There was a brief tornado reported (rated EFU, where U is unknown because there was no damage to evaluate) to the west of Calion (Union County) at 426 pm CDT. The tornado apparently did little more than kick up some dust.||On the 8th, there was a life threatening deluge in southeast Arkansas. Showers and thunderstorms became widespread, and moved over the same areas for several hours.||Too much rain flooded roads at Star City and Varner (both in Lincoln County), Pine Bluff (Jefferson County), Stuttgart (Arkansas County), and also at Dumas and McGehee (both in Desha County). Water got into many homes. Crop and road damage (washouts) was reported in Bradley County. A creek was out of its banks just southeast of Timber Ridge (Pulaski County).||There was high water along Highway 114 between Calmer and Rison (both in Cleveland County), Highway 425 near Yorktown (Lincoln County), Highway 293 east of Garrett Bridge (Lincoln County), Highway 46 not far from Ebb (Grant County), Highway 276 on the south side of Stuttgart (Arkansas County), and Highway 1 at Kelso (Desha County). These highways were eventually closed temporarily.||The situation was the most serious in Desha and Drew Counties, and a Flash Flood Emergency was issued for the communities of Dumas, Pickens, Rohwer (all in Desha County), and Winchester (Drew County) at 1142 am CDT on the 8th. Radar estimated 10 to more than 15 inches of rain, and there was water everywhere. Some folks indicated (through social media) they had never witnessed flooding of this magnitude.||From an historic perspective, Rohwer (Desha County) received 9.25 inches of rain in the twenty four hour period ending at 700 am CDT on the 8th. This was the most rain in one day at the site, and the fourth largest one day total across the state in June. If that was not enough, 9.97 inches of liquid was measured the next day! Adding the numbers, the whopping 19.22 inches on the 8th/9th was the second biggest two day amount in Arkansas. It was just behind the 21.45 inches at Danville (Yell County) on December 3-4, 1982.||Relentless cloudbursts continued to start the 9th in eastern Arkansas. A rain gauge near DeValls Bluff (Prairie County) completely filled (to six inches) between 400 am and 700 am CST. Buildings were flooded and cars were stalled in Clarendon (Monroe County). It was the same story in Humnoke (Lonoke County), and sandbags were ordered to stop the water.||It was just getting worse in Stuttgart (Arkansas County), with one picture showing more water in a home than ever before (in the life of the photographer/42 years). That claim was likely true because the 7.50 inches of rain that caused the problem easily surpassed the previous one day June record of 4.07 inches on the 29th in 1939. At least fifteen homes were impacted by flooding at Altheimer (Jefferson County). Highway 302 from Highway 17 to Highway 79 was shut down in Monroe County, as was Highway 15 near Sherrill (Jefferson County), Highway 33 east of Tollville (Prairie County), and Highways 85 and 318 near Oneida (Phillips County).||As the weather calmed down in the east by the afternoon of the 9th, temperatures warmed well into the 80s to around 90 degrees across the northern and central counties. Heating and lots of humidity were enough to fuel isolated strong to severe storms toward evening.||Just after 700 pm CDT, a video showed a tornado (rated EFU) that lasted two minutes in a field near Blakemore (Lonoke County). Between 700 pm and 800 pm CDT, there was quarter size hail just east of College Station (Pulaski County). Little Rock (Pulaski County) got a quick 1.10 inches of rain. Trees were blown down at Cave City (Sharp County). At 805 pm CDT, there was a brief weak tornado (rated EF0) a few miles southeast of England (Lonoke County).||The focus shifted back to the southeast early on the 10th. You guessed it...the sky was falling again. Rain plus runoff from the soaking on the 8th/9th in northern and central Desha County inundated farms toward Halley (Desha County) in the south. At 200 pm CDT, an irrigation canal east of Pickens (Desha County) was breached, and adjacent farmland became a lake. The canal was patched by evening. At Florence (Drew County), residents were forced to use boats to get around. Water threatened structures at Dermott and Eudora (both in Chicot County), and sandbagging was in progress. It was clear that assistance was needed, and Arkansas Governor Asa Hutchinson declared a state of emergency. ||All was quiet quiet in Little Rock (Pulaski County) on the 10th, and the sun was out. For the first time in 2021, the temperature touched 90 degrees (the high was 92 degrees), and it was three weeks late (it normally happens by May 18th). Toward evening, it got loud toward Pinnacle Mountain (Pulaski County). A severe storm pumped out quarter size hail, winds strong enough to push over a few trees, and up to six inches of rain in less than two hours. The terrain accentuated the flow of water across roads and into neighborhoods. Video showed flash flooding near Cantrell Rd. and Chenal Parkway.", "ts_dict_index": [276, 277, 278]}
+{"event_id": 962329, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2021-06-08 08:45:00", "end_date_time": "2021-06-08 11:45:00", "narrative": "Hit and miss thunderstorms ramped up on the 6th. Two to more than three inches of rain was measured at Cane Creek State Park (Lincoln County), Fordyce (Dallas County), Monticello (Drew County), Nashville (Howard County), and Pine Bluff (Jefferson County). Several roads were under water between Avilla (Saline County) and Ferndale (Pulaski County), and also at Monticello (Drew County).||During the predawn hours of the 7th, thunderstorm winds downed a tree on Highway 53 just south of Gurdon (Clark County). This caused a log truck to overturn. In the afternoon, more trees were toppled in Camden and East Camden (both in Ouachita County). A chapel roof was damaged just southwest of Cummins (Lincoln County), and part of a roof was blown off close to Sorrells (Jefferson County).||At least a dozen Tornado Warnings were issued in portions of Calhoun, Clark, Cleveland, Dallas, Garland, Hot Spring, Montgomery, Ouachita, and Pike Counties. A funnel cloud was spotted by law enforcement at Gum Springs (Clark County). There was a brief tornado reported (rated EFU, where U is unknown because there was no damage to evaluate) to the west of Calion (Union County) at 426 pm CDT. The tornado apparently did little more than kick up some dust.||On the 8th, there was a life threatening deluge in southeast Arkansas. Showers and thunderstorms became widespread, and moved over the same areas for several hours.||Too much rain flooded roads at Star City and Varner (both in Lincoln County), Pine Bluff (Jefferson County), Stuttgart (Arkansas County), and also at Dumas and McGehee (both in Desha County). Water got into many homes. Crop and road damage (washouts) was reported in Bradley County. A creek was out of its banks just southeast of Timber Ridge (Pulaski County).||There was high water along Highway 114 between Calmer and Rison (both in Cleveland County), Highway 425 near Yorktown (Lincoln County), Highway 293 east of Garrett Bridge (Lincoln County), Highway 46 not far from Ebb (Grant County), Highway 276 on the south side of Stuttgart (Arkansas County), and Highway 1 at Kelso (Desha County). These highways were eventually closed temporarily.||The situation was the most serious in Desha and Drew Counties, and a Flash Flood Emergency was issued for the communities of Dumas, Pickens, Rohwer (all in Desha County), and Winchester (Drew County) at 1142 am CDT on the 8th. Radar estimated 10 to more than 15 inches of rain, and there was water everywhere. Some folks indicated (through social media) they had never witnessed flooding of this magnitude.||From an historic perspective, Rohwer (Desha County) received 9.25 inches of rain in the twenty four hour period ending at 700 am CDT on the 8th. This was the most rain in one day at the site, and the fourth largest one day total across the state in June. If that was not enough, 9.97 inches of liquid was measured the next day! Adding the numbers, the whopping 19.22 inches on the 8th/9th was the second biggest two day amount in Arkansas. It was just behind the 21.45 inches at Danville (Yell County) on December 3-4, 1982.||Relentless cloudbursts continued to start the 9th in eastern Arkansas. A rain gauge near DeValls Bluff (Prairie County) completely filled (to six inches) between 400 am and 700 am CST. Buildings were flooded and cars were stalled in Clarendon (Monroe County). It was the same story in Humnoke (Lonoke County), and sandbags were ordered to stop the water.||It was just getting worse in Stuttgart (Arkansas County), with one picture showing more water in a home than ever before (in the life of the photographer/42 years). That claim was likely true because the 7.50 inches of rain that caused the problem easily surpassed the previous one day June record of 4.07 inches on the 29th in 1939. At least fifteen homes were impacted by flooding at Altheimer (Jefferson County). Highway 302 from Highway 17 to Highway 79 was shut down in Monroe County, as was Highway 15 near Sherrill (Jefferson County), Highway 33 east of Tollville (Prairie County), and Highways 85 and 318 near Oneida (Phillips County).||As the weather calmed down in the east by the afternoon of the 9th, temperatures warmed well into the 80s to around 90 degrees across the northern and central counties. Heating and lots of humidity were enough to fuel isolated strong to severe storms toward evening.||Just after 700 pm CDT, a video showed a tornado (rated EFU) that lasted two minutes in a field near Blakemore (Lonoke County). Between 700 pm and 800 pm CDT, there was quarter size hail just east of College Station (Pulaski County). Little Rock (Pulaski County) got a quick 1.10 inches of rain. Trees were blown down at Cave City (Sharp County). At 805 pm CDT, there was a brief weak tornado (rated EF0) a few miles southeast of England (Lonoke County).||The focus shifted back to the southeast early on the 10th. You guessed it...the sky was falling again. Rain plus runoff from the soaking on the 8th/9th in northern and central Desha County inundated farms toward Halley (Desha County) in the south. At 200 pm CDT, an irrigation canal east of Pickens (Desha County) was breached, and adjacent farmland became a lake. The canal was patched by evening. At Florence (Drew County), residents were forced to use boats to get around. Water threatened structures at Dermott and Eudora (both in Chicot County), and sandbagging was in progress. It was clear that assistance was needed, and Arkansas Governor Asa Hutchinson declared a state of emergency. ||All was quiet quiet in Little Rock (Pulaski County) on the 10th, and the sun was out. For the first time in 2021, the temperature touched 90 degrees (the high was 92 degrees), and it was three weeks late (it normally happens by May 18th). Toward evening, it got loud toward Pinnacle Mountain (Pulaski County). A severe storm pumped out quarter size hail, winds strong enough to push over a few trees, and up to six inches of rain in less than two hours. The terrain accentuated the flow of water across roads and into neighborhoods. A local creek flooded over its banks.", "ts_dict_index": [282, 283, 284]}
+{"event_id": 885254, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2020-05-15 15:30:00", "end_date_time": "2020-05-15 18:30:00", "narrative": "On the 15th, the focus was mainly to the west of Arkansas. Showers and thunderstorms became widespread across the southern Plains surrounding a storm system wobbling this way from the southwest. Some of the fireworks managed to work into western sections of the state during the afternoon and evening.||Rain was very heavy in places, with many streets covered by water in and around Waldron (Scott County). Strong to damaging thunderstorm winds toppled trees a few miles northwest of Murfreesboro (Pike County). There was quarter size hail at Bismarck (Hot Spring County). ||In the northwest, it rained at Harrison (Boone County). As rain departed to the southeast between 300 pm and 500 pm CST, the pressure dropped quickly. Temperatures warmed up and the air dried out. This was a sure sign that a small area of low pressure was forming in the wake of the exiting precipitation (a wake low). Winds kicked up and gusted as high as 50 mph. ||On the 16th, conditions were expected to go downhill locally. Widespread precipitation was in the forecast, especially in central and western Arkansas.||Given plenty of water to wring out of the clouds, flash flooding was a concern. Between 500 pm and 1000 pm CST, high water problems were realized as a deluge unfolded.|Water flowed across roads in Conway and Greenbrier (both in Faulkner County) and surrounding areas. Barricades had to be used in some cases. It was the same story at Shirley (Van Buren County) and south of Mount Ida (Montgomery County), and creeks were out of their banks. Five miles west and southwest of Arkadelphia (Clark County), Highways 8 and 26 were impassible due to flooding. Highway 71 at Y City (Scott County) was closed for the same reason.||There were quick rises on the Buffalo, Eleven Point, Fourche La Fave, Little Missouri, Petit Jean, Saline, and Spring Rivers, with minor flooding occurring in spots. The Ouachita River also came up fast, and this was due to the rain and releases at Remmel Dam. There was enough water to keep the Black, Cache, and lower White Rivers elevated, which was the norm for much of the year up to this point.||Storms in southeast Arkansas were very isolated, but popped up in a hurry where they managed to develop. Weak rotation in the clouds was stretched as clouds mushroomed. Rotation tightened after being extended leading to a brief landspout just north of Sherrill (Jefferson County) not long after 530 pm CST. This was unlike most springtime tornadoes that are usually associated with mesocyclones (strong persistent circulations that extend thousands of feet into the atmosphere).||The turning motion around the incoming system increased chances of isolated tornadoes southwest of Little Rock (Pulaski County). Numerous Tornado Warnings were issued in the far southwest, and there was damage in places.||Other spotty wind damage was reported. Metal roofing was removed from boat docks and at least a dozen trees were uprooted at a resort just northwest of Crystal Springs (Garland County). Trees and power lines were downed at Leola (Grant County).||The system gradually weakened once it arrived with a cold front on the 17th. Precipitation became more scattered and was not as heavy.||Three to more than five inches of rain dumped at quite a few locations in the western half of the state in the seventy two hour period ending at 600 pm CST on the 17th. This included Alexander (Pulaski/Saline Counties), Benton (Saline County), Booneville (Logan County), Conway (Faulkner County), Damascus (Van Buren County), DeGray Lake State Park (Clark/Hot Spring Counties), Delight (Pike County), Fairbanks (Van Buren County), Fordyce (Dallas County), Harrison (Boone County), Hot Springs (Garland County), Marshall (Searcy County), Mena (Polk County), Menifee (Conway County), Mountain Home (Baxter County), Mount Ida (Montgomery County), Murfreesboro (Pike County), and Waldron (Scott County).||For the month (through the 17th), there was more than the usual precipitation in central/western Arkansas, and it was drier than normal in the east. Surpluses of liquid were over an inch at Harrison (Boone County). Many roads were covered in water throughout the city and surrounding areas.", "ts_dict_index": [288, 289, 290]}
+{"event_id": 859907, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Water was flowing over the West Main Street bridge, prompting the village of Frankfort to issue a state of emergency.", "ts_dict_index": [309, 310, 311]}
+{"event_id": 859910, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 22:15:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. A bridge on Fairfield Road was severely damaged, stranding occupants of four homes.", "ts_dict_index": [306, 307, 308]}
+{"event_id": 885278, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2020-05-16 21:32:00", "end_date_time": "2020-05-16 23:50:00", "narrative": "On the 15th, the focus was mainly to the west of Arkansas. Showers and thunderstorms became widespread across the southern Plains surrounding a storm system wobbling this way from the southwest. Some of the fireworks managed to work into western sections of the state during the afternoon and evening.||Rain was very heavy in places, with many streets covered by water in and around Waldron (Scott County). Strong to damaging thunderstorm winds toppled trees a few miles northwest of Murfreesboro (Pike County). There was quarter size hail at Bismarck (Hot Spring County). ||In the northwest, it rained at Harrison (Boone County). As rain departed to the southeast between 300 pm and 500 pm CST, the pressure dropped quickly. Temperatures warmed up and the air dried out. This was a sure sign that a small area of low pressure was forming in the wake of the exiting precipitation (a wake low). Winds kicked up and gusted as high as 50 mph. ||On the 16th, conditions were expected to go downhill locally. Widespread precipitation was in the forecast, especially in central and western Arkansas.||Given plenty of water to wring out of the clouds, flash flooding was a concern. Between 500 pm and 1000 pm CST, high water problems were realized as a deluge unfolded.|Water flowed across roads in Conway and Greenbrier (both in Faulkner County) and surrounding areas. Barricades had to be used in some cases. It was the same story at Shirley (Van Buren County) and south of Mount Ida (Montgomery County), and creeks were out of their banks. Five miles west and southwest of Arkadelphia (Clark County), Highways 8 and 26 were impassible due to flooding. Highway 71 at Y City (Scott County) was closed for the same reason.||There were quick rises on the Buffalo, Eleven Point, Fourche La Fave, Little Missouri, Petit Jean, Saline, and Spring Rivers, with minor flooding occurring in spots. The Ouachita River also came up fast, and this was due to the rain and releases at Remmel Dam. There was enough water to keep the Black, Cache, and lower White Rivers elevated, which was the norm for much of the year up to this point.||Storms in southeast Arkansas were very isolated, but popped up in a hurry where they managed to develop. Weak rotation in the clouds was stretched as clouds mushroomed. Rotation tightened after being extended leading to a brief landspout just north of Sherrill (Jefferson County) not long after 530 pm CST. This was unlike most springtime tornadoes that are usually associated with mesocyclones (strong persistent circulations that extend thousands of feet into the atmosphere).||The turning motion around the incoming system increased chances of isolated tornadoes southwest of Little Rock (Pulaski County). Numerous Tornado Warnings were issued in the far southwest, and there was damage in places.||Other spotty wind damage was reported. Metal roofing was removed from boat docks and at least a dozen trees were uprooted at a resort just northwest of Crystal Springs (Garland County). Trees and power lines were downed at Leola (Grant County).||The system gradually weakened once it arrived with a cold front on the 17th. Precipitation became more scattered and was not as heavy.||Three to more than five inches of rain dumped at quite a few locations in the western half of the state in the seventy two hour period ending at 600 pm CST on the 17th. This included Alexander (Pulaski/Saline Counties), Benton (Saline County), Booneville (Logan County), Conway (Faulkner County), Damascus (Van Buren County), DeGray Lake State Park (Clark/Hot Spring Counties), Delight (Pike County), Fairbanks (Van Buren County), Fordyce (Dallas County), Harrison (Boone County), Hot Springs (Garland County), Marshall (Searcy County), Mena (Polk County), Menifee (Conway County), Mountain Home (Baxter County), Mount Ida (Montgomery County), Murfreesboro (Pike County), and Waldron (Scott County).||For the month (through the 17th), there was more than the usual precipitation in central/western Arkansas, and it was drier than normal in the east. Surpluses of liquid were over an inch at Harrison (Boone County). Highway 71 at Y City was closed due to the high water.", "ts_dict_index": [285, 286, 287]}
+{"event_id": 859101, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:12:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 28 was closed between Middleville and Poland due to flooding.", "ts_dict_index": [303, 304, 305]}
+{"event_id": 859100, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:03:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 5 was closed between Newport Road and Millers Grove Road due to flooding.", "ts_dict_index": [300, 301, 302]}
+{"event_id": 859908, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. A shed for a pump station was washed away by flood waters.", "ts_dict_index": [312, 313, 314]}
+{"event_id": 860761, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 22:15:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Water was flowing over Route 8 at Black Creek.", "ts_dict_index": [297, 298, 299]}
+{"event_id": 859102, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:56:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 5S was closed between Culver Avenue and Ilion due to a mudslide.", "ts_dict_index": [315, 316, 317]}
+{"event_id": 859118, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:30:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. The shoulder of Military Road in Norway collapsed due to flood waters. An 82-year old man's vehicle became stuck with the driver's side wheels on the pavement, and the passenger side wheels in a ravine created by the floodwaters. The man died when he exited the vehicle and was swept away by floodwaters.", "ts_dict_index": [321, 322, 323]}
+{"event_id": 859097, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 20:56:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 5 was closed due to flooding between Windfall Road and Drive-In Road.", "ts_dict_index": [318, 319, 320]}
+{"event_id": 859909, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 22:15:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. A mudslide occurred on Route 5 near Gun Club Road.", "ts_dict_index": [294, 295, 296]}
+{"event_id": 932451, "event_type": "Debris Flow", "state": "CALIFORNIA", "cz_name": "SANTA CRUZ", "begin_date_time": "2021-01-27 18:46:00", "end_date_time": "2021-01-27 19:16:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Rockslide on SR-129 and Rogge Lane.", "ts_dict_index": [141, 142, 143]}
+{"event_id": 1049202, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-07-28 02:00:00", "end_date_time": "2022-07-28 08:00:00", "narrative": "Between July 25th and July 30th, 2022, several complexes of training thunderstorms developed south of I-64 and brought heavy rain, deadly flash flooding, and devastating river flooding to eastern Kentucky and central Appalachia. These thunderstorms, at times, caused rainfall rates in excess of 4/hr across complex terrain that led to widespread devastating impacts. While it did not rain continuously during this 4-day stretch, the overwhelming amounts of rain and resultant flooding led to 39 deaths and widespread catastrophic damage. Entire homes and parts of some communities were swept away by flood waters, leading to costly damage to infrastructure in the region. Over 600 helicopter rescues and countless swift water rescues by boat were needed to evacuate people who were trapped by the quickly-rising flood waters. In total, 24 Flash Flood Warnings were issued between July 26th and July 30th. Between the evening of July 27th and the mid-morning hours on July 28th (the peak of the event), 13 warnings were issued, 3 of which were upgraded to a Flash Flood Emergency.||Radar-based rainfall estimates suggest that upwards of 14-16 of rain fell during this 5-day period in a narrow swath, with many more locations receiving 6-10 of rain. Most of this rain fell during the night of July 27th into the morning of July 28th, which is when the most devastating impacts were felt. The highest totals occurred across an axis that stretches from northern Clay and southern Owsley counties, east through southern Breathitt and northern Leslie counties, into Perry, Knott and Letcher counties. The highest rainfall total report was from southern Knott County, where 14.00 fell between July 25th and July 29th. This site, a cooperative (COOP) observer at Carr Creek Lake, reported 6.71 from 7am July 28th to 7am July 29th, following a report of 6.50 at that site on the previous day. Another COOP site in Buckhorn reported 8.00 of rain for the 24-hour period ending 7am on July 28th. The rainfall total in Buckhorn from July 25th to July 29th was 11.76. These rainfall values occurring in such a short period of time are incredibly rare: there is less than a 1 in 1000 chance for this much rainfall over five days in a given year.||The incredible rainfall also led to significant rises and flooding on many rivers in eastern Kentucky including on the main stem of the Kentucky River; North, Middle and South forks of the Kentucky River; Red River and Licking River. At Whitesburg, the North Fork of the Kentucky River swelled well above major flood stage, reaching close to 21' before gauge failure (the previous flood of record was 14.7' in 1957). The North Fork of the Kentucky River at Jackson also reached major flood, setting a new record crest of 43.47' (the previous record was 43.1' set in 1939). The river flooding caused a second round of destruction for communities in the region, and caused flooding in downstream areas that did not receive as much rainfall.||*Note* Given the widespread nature and severity of this event - any dollar amount estimated by storm data will not do the event as a whole justice. Since eastern KY was a national declaration, FEMA will be doing a full cost assessment. Will use this data once available for total monetary amounts of damage.||Visit www.weather.gov/jkl/July2022Flooding for more information on the event, as well as pictures and videos of the flooding and damage. Pike County saw multiple reports of flash flooding, mainly from the southern half of the county. Some of the reports included: ||2:00 AM EST - A submerged car in a stream and significant road damage was reported in the Long Fork area of Virgie. |3:15 AM EST - 2 feet of water was reported across Long Fork Road in Virgie.|3:30 AM EST - Elkhorn Creek was reported out of it's banks and flood waters were threatening homes along the creek. Residents in the area were evacuating multiple homes south of KY-197.", "ts_dict_index": [291, 292, 293]}
+{"event_id": 860791, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 22:15:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. There was several feet of water over Gray Road, partially submerging a car.", "ts_dict_index": [339, 340, 341]}
+{"event_id": 860787, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 22:15:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Dairy Hill Road was washed out.", "ts_dict_index": [327, 328, 329]}
+{"event_id": 860782, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 20:30:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. There was widespread flash flooding in the village of Middleville. Water entered structures with cars partially submerged. There were 27 evacuations as a result of the flooding. The West Canada Creek was nearing the road surface of the Route 28 bridge. Downstream at Kast Bridge, the creek reached moderate flood stage at 2106EST and continued to rise to major flood stage by 2124EST before cresting at a record high level of 10.92 feet at 2315EST.", "ts_dict_index": [333, 334, 335]}
+{"event_id": 860792, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 22:15:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. A bridge on Black Creek Road was washed out.", "ts_dict_index": [330, 331, 332]}
+{"event_id": 962429, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2021-06-10 19:02:00", "end_date_time": "2021-06-10 22:02:00", "narrative": "Hit and miss thunderstorms ramped up on the 6th. Two to more than three inches of rain was measured at Cane Creek State Park (Lincoln County), Fordyce (Dallas County), Monticello (Drew County), Nashville (Howard County), and Pine Bluff (Jefferson County). Several roads were under water between Avilla (Saline County) and Ferndale (Pulaski County), and also at Monticello (Drew County).||During the predawn hours of the 7th, thunderstorm winds downed a tree on Highway 53 just south of Gurdon (Clark County). This caused a log truck to overturn. In the afternoon, more trees were toppled in Camden and East Camden (both in Ouachita County). A chapel roof was damaged just southwest of Cummins (Lincoln County), and part of a roof was blown off close to Sorrells (Jefferson County).||At least a dozen Tornado Warnings were issued in portions of Calhoun, Clark, Cleveland, Dallas, Garland, Hot Spring, Montgomery, Ouachita, and Pike Counties. A funnel cloud was spotted by law enforcement at Gum Springs (Clark County). There was a brief tornado reported (rated EFU, where U is unknown because there was no damage to evaluate) to the west of Calion (Union County) at 426 pm CDT. The tornado apparently did little more than kick up some dust.||On the 8th, there was a life threatening deluge in southeast Arkansas. Showers and thunderstorms became widespread, and moved over the same areas for several hours.||Too much rain flooded roads at Star City and Varner (both in Lincoln County), Pine Bluff (Jefferson County), Stuttgart (Arkansas County), and also at Dumas and McGehee (both in Desha County). Water got into many homes. Crop and road damage (washouts) was reported in Bradley County. A creek was out of its banks just southeast of Timber Ridge (Pulaski County).||There was high water along Highway 114 between Calmer and Rison (both in Cleveland County), Highway 425 near Yorktown (Lincoln County), Highway 293 east of Garrett Bridge (Lincoln County), Highway 46 not far from Ebb (Grant County), Highway 276 on the south side of Stuttgart (Arkansas County), and Highway 1 at Kelso (Desha County). These highways were eventually closed temporarily.||The situation was the most serious in Desha and Drew Counties, and a Flash Flood Emergency was issued for the communities of Dumas, Pickens, Rohwer (all in Desha County), and Winchester (Drew County) at 1142 am CDT on the 8th. Radar estimated 10 to more than 15 inches of rain, and there was water everywhere. Some folks indicated (through social media) they had never witnessed flooding of this magnitude.||From an historic perspective, Rohwer (Desha County) received 9.25 inches of rain in the twenty four hour period ending at 700 am CDT on the 8th. This was the most rain in one day at the site, and the fourth largest one day total across the state in June. If that was not enough, 9.97 inches of liquid was measured the next day! Adding the numbers, the whopping 19.22 inches on the 8th/9th was the second biggest two day amount in Arkansas. It was just behind the 21.45 inches at Danville (Yell County) on December 3-4, 1982.||Relentless cloudbursts continued to start the 9th in eastern Arkansas. A rain gauge near DeValls Bluff (Prairie County) completely filled (to six inches) between 400 am and 700 am CST. Buildings were flooded and cars were stalled in Clarendon (Monroe County). It was the same story in Humnoke (Lonoke County), and sandbags were ordered to stop the water.||It was just getting worse in Stuttgart (Arkansas County), with one picture showing more water in a home than ever before (in the life of the photographer/42 years). That claim was likely true because the 7.50 inches of rain that caused the problem easily surpassed the previous one day June record of 4.07 inches on the 29th in 1939. At least fifteen homes were impacted by flooding at Altheimer (Jefferson County). Highway 302 from Highway 17 to Highway 79 was shut down in Monroe County, as was Highway 15 near Sherrill (Jefferson County), Highway 33 east of Tollville (Prairie County), and Highways 85 and 318 near Oneida (Phillips County).||As the weather calmed down in the east by the afternoon of the 9th, temperatures warmed well into the 80s to around 90 degrees across the northern and central counties. Heating and lots of humidity were enough to fuel isolated strong to severe storms toward evening.||Just after 700 pm CDT, a video showed a tornado (rated EFU) that lasted two minutes in a field near Blakemore (Lonoke County). Between 700 pm and 800 pm CDT, there was quarter size hail just east of College Station (Pulaski County). Little Rock (Pulaski County) got a quick 1.10 inches of rain. Trees were blown down at Cave City (Sharp County). At 805 pm CDT, there was a brief weak tornado (rated EF0) a few miles southeast of England (Lonoke County).||The focus shifted back to the southeast early on the 10th. You guessed it...the sky was falling again. Rain plus runoff from the soaking on the 8th/9th in northern and central Desha County inundated farms toward Halley (Desha County) in the south. At 200 pm CDT, an irrigation canal east of Pickens (Desha County) was breached, and adjacent farmland became a lake. The canal was patched by evening. At Florence (Drew County), residents were forced to use boats to get around. Water threatened structures at Dermott and Eudora (both in Chicot County), and sandbagging was in progress. It was clear that assistance was needed, and Arkansas Governor Asa Hutchinson declared a state of emergency. ||All was quiet quiet in Little Rock (Pulaski County) on the 10th, and the sun was out. For the first time in 2021, the temperature touched 90 degrees (the high was 92 degrees), and it was three weeks late (it normally happens by May 18th). Toward evening, it got loud toward Pinnacle Mountain (Pulaski County). A severe storm pumped out quarter size hail, winds strong enough to push over a few trees, and up to six inches of rain in less than two hours. The terrain accentuated the flow of water across roads and into neighborhoods. Several photos and video showed flash flooding in West Little Rock. Multiple roads were underwater, with water into some homes.", "ts_dict_index": [279, 280, 281]}
+{"event_id": 860783, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 22:15:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Atwood Lake Road was washed out.", "ts_dict_index": [351, 352, 353]}
+{"event_id": 860786, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 22:15:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. A bridge at White Creek Road and Newport-Gray Road was washed out.", "ts_dict_index": [345, 346, 347]}
+{"event_id": 865421, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 08:00:00", "end_date_time": "2019-11-01 13:20:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Heavy rainfall eroded the embankment along the Hilltop Bridge over Moyer Creek, resulting in the evacuation of 50-100 residents along South Litchfield Street.", "ts_dict_index": [354, 355, 356]}
+{"event_id": 807671, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-02-11 10:33:00", "end_date_time": "2019-02-11 13:33:00", "narrative": "It was a perfect setup for flooding heading into mid-February. The ground was wet (and could not hold much additional water) following six straight months of above average precipitation. Rivers were running high. The atmosphere was loaded with moisture on the 10th/11th, and a storm system in the Plains was set to wring it out of the clouds. It was a bad situation. The forecast called for several inches of rain from central into northeast Arkansas. Rain focused along and north of a front that was stalled over southeast sections of the state.||By the time the event was over, more than half a foot of liquid was measured in places. Seventy two hour precipitation totals through 600 am CST on the 12th included 6.02 inches at Newport (Jackson County), 5.18 inches at Blytheville (Mississippi County), 5.10 inches at Walnut Ridge (Lawrence County), 4.61 inches at Batesville (Independence County), 4.03 inches at North Little Rock (Pulaski County), and 4.01 inches at Russellville (Pope County).||Swollen rivers closed highways in the northeast, including Highway 37 between Cord (Independence County) and Tuckerman (Jackson County), Highway 14 between Oil Trough (Independence County) and Newport (Jackson County), Highway 37 near Grubbs (Jackson County), Highway 25 between Black Rock and Powhattan (both in Lawrence County), and Highway 166 northeast of Pocahontas (Randolph County).||There were numerous reports of flash flooding. At least two vehicles were swept off the pavement by rapidly rising creeks. The vehicles were just east of Springfield (Conway County) near Cadron Creek, and west of Hagarville (Johnson County) at the intersection of Highways 123 and 292 close to Minnow Creek. No injuries were reported in either incident. ||The rain was too much for rivers in eastern Arkansas. There was major flooding along portions of the Cache River (water threatening homes, and roads and farmland under water in Jackson and Woodruff Counties). Moderate to major flooding was noted along stretches of the Black and lower White Rivers.||At Newport (Jackson County), the White River topped out just over 30 feet on the 14th. At this level (four feet above the flood stage of 26 feet), major flooding is expected. Just south of town, an eroding levee was in danger of failing. An emergency was declared on the 12th, and people near the levee were advised to evacuate (voluntarily). As a precaution, sandbags were made available to local residents. The levee was stabilized with sandbags as well.||There was also moderate flooding along the somewhat flashy (rapid rises and falls) Little Red River at Judsonia (White County). The river crested roughly five feet above the flood stage during the morning of the 12th. Highway 161 north of highway 70 was closed due to high water.", "ts_dict_index": [357, 358, 359]}
+{"event_id": 859096, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 20:00:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Newport Road was washed out.", "ts_dict_index": [342, 343, 344]}
+{"event_id": 807675, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-02-11 11:30:00", "end_date_time": "2019-02-11 14:30:00", "narrative": "It was a perfect setup for flooding heading into mid-February. The ground was wet (and could not hold much additional water) following six straight months of above average precipitation. Rivers were running high. The atmosphere was loaded with moisture on the 10th/11th, and a storm system in the Plains was set to wring it out of the clouds. It was a bad situation. The forecast called for several inches of rain from central into northeast Arkansas. Rain focused along and north of a front that was stalled over southeast sections of the state.||By the time the event was over, more than half a foot of liquid was measured in places. Seventy two hour precipitation totals through 600 am CST on the 12th included 6.02 inches at Newport (Jackson County), 5.18 inches at Blytheville (Mississippi County), 5.10 inches at Walnut Ridge (Lawrence County), 4.61 inches at Batesville (Independence County), 4.03 inches at North Little Rock (Pulaski County), and 4.01 inches at Russellville (Pope County).||Swollen rivers closed highways in the northeast, including Highway 37 between Cord (Independence County) and Tuckerman (Jackson County), Highway 14 between Oil Trough (Independence County) and Newport (Jackson County), Highway 37 near Grubbs (Jackson County), Highway 25 between Black Rock and Powhattan (both in Lawrence County), and Highway 166 northeast of Pocahontas (Randolph County).||There were numerous reports of flash flooding. At least two vehicles were swept off the pavement by rapidly rising creeks. The vehicles were just east of Springfield (Conway County) near Cadron Creek, and west of Hagarville (Johnson County) at the intersection of Highways 123 and 292 close to Minnow Creek. No injuries were reported in either incident. ||The rain was too much for rivers in eastern Arkansas. There was major flooding along portions of the Cache River (water threatening homes, and roads and farmland under water in Jackson and Woodruff Counties). Moderate to major flooding was noted along stretches of the Black and lower White Rivers.||At Newport (Jackson County), the White River topped out just over 30 feet on the 14th. At this level (four feet above the flood stage of 26 feet), major flooding is expected. Just south of town, an eroding levee was in danger of failing. An emergency was declared on the 12th, and people near the levee were advised to evacuate (voluntarily). As a precaution, sandbags were made available to local residents. The levee was stabilized with sandbags as well.||There was also moderate flooding along the somewhat flashy (rapid rises and falls) Little Red River at Judsonia (White County). The river crested roughly five feet above the flood stage during the morning of the 12th. Roads were closed due to flash flooding with vehicles stranded.", "ts_dict_index": [360, 361, 362]}
+{"event_id": 951907, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-03-27 23:40:00", "end_date_time": "2021-03-28 00:07:00", "narrative": "An historic flash flooding event affected the central third of Middle Tennessee from the early morning hours on March 27 through the day into the early morning hours on March 28. A warm front moved northward into Middle Tennessee early on March 27 before stalling near the I-40 corridor. Between 300-400 AM CDT, numerous showers and thunderstorms developed along the warm front, many of which became severe and produced large hail up to half dollar size along with frequent lightning and heavy rainfall. Showers and storms continued off and on the rest of the day across Middle Tennessee, particularly near the stalled warm front. In fact, another round of severe thunderstorms including supercells developed during the afternoon and evening hours near and south of the warm front. These storms dropped large hail up to tennis ball size and caused a few reports of wind damage, but the main impact was additional heavy rainfall which began causing flash flooding south of Nashville. Flooding only worsened as showers and storms redeveloped over the same areas through the evening, with numerous Flash Flood Warnings issued and several reports of flooded roads and water rescues.||After midnight, even more heavy rainfall falling along the already waterlogged I-40 corridor prompted a rare Flash Flood Emergency for the southern and eastern Nashville metro area, including southeastern Davidson County, western Wilson County, and northern Williamson County. These areas received between 7 to 9 of rain, causing rapid rises on several Nashville metro creeks and streams, including Sevenmile Creek (which reached its highest level on record), Browns Creek, and Mill Creek, among others. Many of these creeks reached within their 2nd or 3rd highest water levels on record. The rapid water rises flooded hundreds of homes and businesses, with reports of some people trapped in the attics or on the roofs of their houses. Dozens of roadways were flooded and impassable, including both I-24 and I-40, with many cars submerged in the flood waters and people forced to cling onto trees to avoid getting swept away. Although the flood waters receded quickly on Sunday, March 28, many area rivers reached flood stage in the week after the event, including the Cumberland River, Harpeth River, and Duck River.||A total of 7 deaths were reported from the flooding across Middle Tennessee, with 5 in Davidson County, 1 in Cheatham County, and 1 in Maury County. Emergency management reports indicate over 500 homes and businesses were flooded, and a Presidential Disaster Proclamation was declared for many counties in May 2021. This flash flood event was the worst seen in Middle Tennessee since the May 1-2, 2010 flood. Numerous roads were flooded and closed across the county, including I-40 at mile marker 178, South Bear Creek, Hogan Road at Porter Road, Double Branch Road, and Highway 48 N at R Owen Road.", "ts_dict_index": [363, 364, 365]}
+{"event_id": 859098, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 5S was closed near Mucky Run Road due to flooding.", "ts_dict_index": [324, 325, 326]}
+{"event_id": 1131005, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. The road was washed out due to flash flooding near the intersection of Whitewater Road and Knights Road.", "ts_dict_index": [387, 388, 389]}
+{"event_id": 817684, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-04-18 07:20:00", "end_date_time": "2019-04-18 10:20:00", "narrative": "While it seemed the region was in the clear on the 13th, rain and cool air kept the pressure elevated. At the same time, a storm system strengthened in Texas, and the pressure fell to the southwest. This created a pressure gradient, and this often leads to increased wind speeds. Gusts exceeded 40 mph in the southern half of the state during the afternoon/evening, and this went on for several hours.||A 47 mph gust was measured at the airport in Hot Springs (Garland County) at 240 pm CDT. A couple of hours later, a gust reached 53 mph at Little Rock National Airport (Pulaski County). Numerous trees (200 to 300 trees) were downed on the west side of Lake Ouachita at the Little Fir and Tompkins Bend Recreation Areas (both in Montgomery County). Trees were also toppled at Hot Springs (Garland County), Houston (Perry County), Maumelle (Pulaski County), Pine Bluff (Jefferson County), and west Little Rock (Pulaski County). Some trees were on homes and blocking roads. At least 30,000 power outages were reported.||More rain was on the horizon by late on the 17th, and it was expected to be heavy. This was preceded by a few severe storms in the west. Golf ball size hail was reported at Dover (Pope County), with half dollar size hail at Atkins (Pope County), and quarter size stones at Clarksville (Johnson County) and Russellville (Pope County). Following the hail, the deluge commenced.||Three to more than five inches of rain dumped in central and western Arkansas. Forty eight hour amounts through 700 am CDT on the 19th included 6.02 inches just northeast of Bryant (Saline County), 5.44 inches at Little Rock (Pulaski County), 4.89 inches at Benton (Saline County), 4.50 inches at North Little Rock (Pulaski County), 4.50 inches at Crystal Valley (Pulaski County), 4.01 inches at Big Fork (Polk County), 3.77 inches at Conway (Faulkner County), 3.48 inches at Waldron (Scott County), 3.34 inches at Bogg Springs (Polk County), and 3.30 inches at Booneville (Logan County).|The 5.44 inches of rain at Little Rock (Pulaski County) not only shattered a daily record on the 18th, it was the 15th wettest calendar day on record locally and the 5th wettest April calendar day.||Given so much rain, there was high water along Interstate 30 near Vimy Ridge (Saline County). All lanes were closed for at least a couple of hours. In Macon (Pulaski County), flooding along Highway 107 stranded a vehicle, and people needed to be rescued. Many roads were flooded from Benton (Saline County) to the Little Rock (Pulaski County) area. Highway 11 near Hazen (Prairie County) was under water, as was Highway 31 around Woodlawn (Lonoke County). Many farm fields were converted into lakes. A water rescue was performed at Highway 107 in Macon.", "ts_dict_index": [372, 373, 374]}
+{"event_id": 834202, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2019-06-23 02:40:00", "end_date_time": "2019-06-23 02:40:00", "narrative": "On the 23rd, the focus was on a couple of big thunderstorm clusters. The first cluster hammered areas north and west of Little Rock (Pulaski County) during the early morning hours, and it had a little of everything. Two weak tornadoes were spawned to the southeast of Paris (Logan County). The tornadoes uprooted or snapped trees, with one of the trees falling through a house. A mobile home roof and porch were also damaged. At Russellville (Pope County), thunderstorm gusts reached an estimated 90 mph at Arkansas Tech. Winds this strong tore up an outfield wall and first base dugout at a baseball field.||There was a lot of rain and reports of flash flooding. Creeks and small streams were on the rise, and roads were under water. At Waldron (Scott County), Highways 28 and 71 were closed. Culverts were washed out along Highway 80 southwest of Danville (Yell County). Closer to town, there was plenty of standing water at the airport. County roads were impassible or washed out around Ozone (Johnson County) and Parthenon (Newton County).||The first round of storms was followed quickly by another round in the late morning and afternoon hours. Between 1200 pm and 300 pm CDT, trees and/or power lines were toppled at Calico Rock (Izard County), Clarkridge (Baxter County), Evening Shade (Sharp County), Harmony (Johnson County), Melbourne (Izard County), Pocahontas (Randolph County), north of Strawberry (Lawrence County), Swifton (Jackson County), and Toad Suck (Perry County). There were instances of trees on homes, on vehicles, and blocking roads. A 61 mph wind gust was measured at Walnut Ridge (Lawrence County), with a 60 mph gust estimated at Bradford (White County).||More than a month's worth of rain fell in portions of northern and western Arkansas in the forty eight hour period ending at 700 am CDT on the 24th. Nine miles west of Waldron (Scott County). One rain gauge collected 11.35 inches of precipitation! Abbott (Scott County) had 8.10 inches, with 7.50 inches at Devils Knob (Johnson County), 7.38 inches at Nunley (Polk County), and 6.20 inches at Jasper (Newton County).||As the month came to a close, a storm system aloft visited from Missouri on the 26th. Cooler air overhead associated with the system moved over much warmer conditions near the ground. This agitated the atmosphere, and hit and miss thunderstorms flared up across the north.||Storms were mostly non-severe, but there was a report of golf ball size hail just northwest of Cherokee Village (Sharp County). A low water crossing was flooded near Compton (Newton County). Numerous county roads were flooded and impassable with portions of Hwy. 28 closed as well.", "ts_dict_index": [378, 379, 380]}
+{"event_id": 817605, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-04-18 05:08:00", "end_date_time": "2019-04-18 08:08:00", "narrative": "While it seemed the region was in the clear on the 13th, rain and cool air kept the pressure elevated. At the same time, a storm system strengthened in Texas, and the pressure fell to the southwest. This created a pressure gradient, and this often leads to increased wind speeds. Gusts exceeded 40 mph in the southern half of the state during the afternoon/evening, and this went on for several hours.||A 47 mph gust was measured at the airport in Hot Springs (Garland County) at 240 pm CDT. A couple of hours later, a gust reached 53 mph at Little Rock National Airport (Pulaski County). Numerous trees (200 to 300 trees) were downed on the west side of Lake Ouachita at the Little Fir and Tompkins Bend Recreation Areas (both in Montgomery County). Trees were also toppled at Hot Springs (Garland County), Houston (Perry County), Maumelle (Pulaski County), Pine Bluff (Jefferson County), and west Little Rock (Pulaski County). Some trees were on homes and blocking roads. At least 30,000 power outages were reported.||More rain was on the horizon by late on the 17th, and it was expected to be heavy. This was preceded by a few severe storms in the west. Golf ball size hail was reported at Dover (Pope County), with half dollar size hail at Atkins (Pope County), and quarter size stones at Clarksville (Johnson County) and Russellville (Pope County). Following the hail, the deluge commenced.||Three to more than five inches of rain dumped in central and western Arkansas. Forty eight hour amounts through 700 am CDT on the 19th included 6.02 inches just northeast of Bryant (Saline County), 5.44 inches at Little Rock (Pulaski County), 4.89 inches at Benton (Saline County), 4.50 inches at North Little Rock (Pulaski County), 4.50 inches at Crystal Valley (Pulaski County), 4.01 inches at Big Fork (Polk County), 3.77 inches at Conway (Faulkner County), 3.48 inches at Waldron (Scott County), 3.34 inches at Bogg Springs (Polk County), and 3.30 inches at Booneville (Logan County).|The 5.44 inches of rain at Little Rock (Pulaski County) not only shattered a daily record on the 18th, it was the 15th wettest calendar day on record locally and the 5th wettest April calendar day.||Given so much rain, there was high water along Interstate 30 near Vimy Ridge (Saline County). All lanes were closed for at least a couple of hours. In Macon (Pulaski County), flooding along Highway 107 stranded a vehicle, and people needed to be rescued. Many roads were flooded from Benton (Saline County) to the Little Rock (Pulaski County) area. Highway 11 near Hazen (Prairie County) was under water, as was Highway 31 around Woodlawn (Lonoke County). Many farm fields were converted into lakes. Several roads in Pulaski County have been reported as flooded including Highway 365 at King Rd., Highway 161 at Trammel Rd., Wayne Rd., JF Cooley Rd., Macarthur at Cedar Rd., Marche Rd., Arch and Baseline Rd., Jim Hall Rd., Kelly/Reed Rd., Crystal Hill/Kelly Rd., Lawson/Faulkner Rd., and Pratt Rd.", "ts_dict_index": [369, 370, 371]}
+{"event_id": 834201, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2019-06-23 02:40:00", "end_date_time": "2019-06-23 05:40:00", "narrative": "On the 23rd, the focus was on a couple of big thunderstorm clusters. The first cluster hammered areas north and west of Little Rock (Pulaski County) during the early morning hours, and it had a little of everything. Two weak tornadoes were spawned to the southeast of Paris (Logan County). The tornadoes uprooted or snapped trees, with one of the trees falling through a house. A mobile home roof and porch were also damaged. At Russellville (Pope County), thunderstorm gusts reached an estimated 90 mph at Arkansas Tech. Winds this strong tore up an outfield wall and first base dugout at a baseball field.||There was a lot of rain and reports of flash flooding. Creeks and small streams were on the rise, and roads were under water. At Waldron (Scott County), Highways 28 and 71 were closed. Culverts were washed out along Highway 80 southwest of Danville (Yell County). Closer to town, there was plenty of standing water at the airport. County roads were impassible or washed out around Ozone (Johnson County) and Parthenon (Newton County).||The first round of storms was followed quickly by another round in the late morning and afternoon hours. Between 1200 pm and 300 pm CDT, trees and/or power lines were toppled at Calico Rock (Izard County), Clarkridge (Baxter County), Evening Shade (Sharp County), Harmony (Johnson County), Melbourne (Izard County), Pocahontas (Randolph County), north of Strawberry (Lawrence County), Swifton (Jackson County), and Toad Suck (Perry County). There were instances of trees on homes, on vehicles, and blocking roads. A 61 mph wind gust was measured at Walnut Ridge (Lawrence County), with a 60 mph gust estimated at Bradford (White County).||More than a month's worth of rain fell in portions of northern and western Arkansas in the forty eight hour period ending at 700 am CDT on the 24th. Nine miles west of Waldron (Scott County). One rain gauge collected 11.35 inches of precipitation! Abbott (Scott County) had 8.10 inches, with 7.50 inches at Devils Knob (Johnson County), 7.38 inches at Nunley (Polk County), and 6.20 inches at Jasper (Newton County).||As the month came to a close, a storm system aloft visited from Missouri on the 26th. Cooler air overhead associated with the system moved over much warmer conditions near the ground. This agitated the atmosphere, and hit and miss thunderstorms flared up across the north.||Storms were mostly non-severe, but there was a report of golf ball size hail just northwest of Cherokee Village (Sharp County). A low water crossing was flooded near Compton (Newton County). Numerous roadways were flooded around Waldron with state highways 71 and 28 closed in some areas.", "ts_dict_index": [375, 376, 377]}
+{"event_id": 982457, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2021-10-25 11:09:00", "end_date_time": "2021-10-25 14:09:00", "narrative": "A large upper level low pressure system in the Gulf of Alaska picked up an abundant amount of tropical moisture from the remains of Typhoon Namtheun on October 23.  This large upper low then dropped southeast to off the Pacific Northwest coast on during the morning of October 24 then underwent rapid intensification during the afternoon of October 24 resulting in a strong surge of deep tropical moisture being pushed into central California by the evening of October 24.  As the upper low tracked inland across the Pacific northwest on October 25, a cold front dropped southward through California bringing moderate to heavy precipitation to areas north of Kern County for 10-12 hours. Much of Yosemite National Park and Mariposa County picked up between 3 to 5 inches of liquid precipitation while 2 to 4 inches of liquid precipitation fell in the Sierra Nevada in Madera and Fresno Counties.  Further south, 1 to 2 inches of liquid precipitation fell in the mountains of Tulare County while the Kern County Mountains generally picked up between half and inch and an inch of rainfall.  Most of the San Joaquin Valley and West Side Hills also picked up between a half inch and an inch of rain while most of Merced County picked up between and inch to an inch and a half.  The Kern County Deserts also picked up between a quarter and a half inch of rainfall.  With most of the moisture from this system being of tropical origin, the snow level was above 9000 feet until the afternoon of October 25.  The snow level lowered to 6000 to 7000 feet before the precipitation ended during the evening of October 25.  Several SNOTEL stations measured between 9 and 15 inches of snow in 12 hours while a few stations above 9000 feet measured between 15 and 30 inches.  There were also several stations which measured peak wind gusts between 58 and 70 mph ahead of the storm during the morning of October 25 or behind the cold front during the evening of October 25.  Scattered thunderstorms developed over the San Joaquin Valley behind the cold front during the afternoon of October 25.  One supercell produced a funnel cloud over southwestern Kings County then moved southeast into Kern County bringing heavy rainfall to the Lost Hills and Wasco areas.  The precipitation tapered off by late  evening and winds diminished by the morning of October 26 as the storm moved to the east of the area. California Highway Patrol reported a rockslide covering the westbound lanes of SR 178 near mile marker 18 in Kern Canyon.", "ts_dict_index": [381, 382, 383]}
+{"event_id": 982456, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2021-10-25 10:10:00", "end_date_time": "2021-10-25 13:10:00", "narrative": "A large upper level low pressure system in the Gulf of Alaska picked up an abundant amount of tropical moisture from the remains of Typhoon Namtheun on October 23.  This large upper low then dropped southeast to off the Pacific Northwest coast on during the morning of October 24 then underwent rapid intensification during the afternoon of October 24 resulting in a strong surge of deep tropical moisture being pushed into central California by the evening of October 24.  As the upper low tracked inland across the Pacific northwest on October 25, a cold front dropped southward through California bringing moderate to heavy precipitation to areas north of Kern County for 10-12 hours. Much of Yosemite National Park and Mariposa County picked up between 3 to 5 inches of liquid precipitation while 2 to 4 inches of liquid precipitation fell in the Sierra Nevada in Madera and Fresno Counties.  Further south, 1 to 2 inches of liquid precipitation fell in the mountains of Tulare County while the Kern County Mountains generally picked up between half and inch and an inch of rainfall.  Most of the San Joaquin Valley and West Side Hills also picked up between a half inch and an inch of rain while most of Merced County picked up between and inch to an inch and a half.  The Kern County Deserts also picked up between a quarter and a half inch of rainfall.  With most of the moisture from this system being of tropical origin, the snow level was above 9000 feet until the afternoon of October 25.  The snow level lowered to 6000 to 7000 feet before the precipitation ended during the evening of October 25.  Several SNOTEL stations measured between 9 and 15 inches of snow in 12 hours while a few stations above 9000 feet measured between 15 and 30 inches.  There were also several stations which measured peak wind gusts between 58 and 70 mph ahead of the storm during the morning of October 25 or behind the cold front during the evening of October 25.  Scattered thunderstorms developed over the San Joaquin Valley behind the cold front during the afternoon of October 25.  One supercell produced a funnel cloud over southwestern Kings County then moved southeast into Kern County bringing heavy rainfall to the Lost Hills and Wasco areas.  The precipitation tapered off by late  evening and winds diminished by the morning of October 26 as the storm moved to the east of the area. California Highway Patrol reported a rockslide with large builders on the roadway near the intersection of SR 46 and SR 33 at Blackwell's Corner.", "ts_dict_index": [384, 385, 386]}
+{"event_id": 951906, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-03-27 21:13:00", "end_date_time": "2021-03-27 21:13:00", "narrative": "An historic flash flooding event affected the central third of Middle Tennessee from the early morning hours on March 27 through the day into the early morning hours on March 28. A warm front moved northward into Middle Tennessee early on March 27 before stalling near the I-40 corridor. Between 300-400 AM CDT, numerous showers and thunderstorms developed along the warm front, many of which became severe and produced large hail up to half dollar size along with frequent lightning and heavy rainfall. Showers and storms continued off and on the rest of the day across Middle Tennessee, particularly near the stalled warm front. In fact, another round of severe thunderstorms including supercells developed during the afternoon and evening hours near and south of the warm front. These storms dropped large hail up to tennis ball size and caused a few reports of wind damage, but the main impact was additional heavy rainfall which began causing flash flooding south of Nashville. Flooding only worsened as showers and storms redeveloped over the same areas through the evening, with numerous Flash Flood Warnings issued and several reports of flooded roads and water rescues.||After midnight, even more heavy rainfall falling along the already waterlogged I-40 corridor prompted a rare Flash Flood Emergency for the southern and eastern Nashville metro area, including southeastern Davidson County, western Wilson County, and northern Williamson County. These areas received between 7 to 9 of rain, causing rapid rises on several Nashville metro creeks and streams, including Sevenmile Creek (which reached its highest level on record), Browns Creek, and Mill Creek, among others. Many of these creeks reached within their 2nd or 3rd highest water levels on record. The rapid water rises flooded hundreds of homes and businesses, with reports of some people trapped in the attics or on the roofs of their houses. Dozens of roadways were flooded and impassable, including both I-24 and I-40, with many cars submerged in the flood waters and people forced to cling onto trees to avoid getting swept away. Although the flood waters receded quickly on Sunday, March 28, many area rivers reached flood stage in the week after the event, including the Cumberland River, Harpeth River, and Duck River.||A total of 7 deaths were reported from the flooding across Middle Tennessee, with 5 in Davidson County, 1 in Cheatham County, and 1 in Maury County. Emergency management reports indicate over 500 homes and businesses were flooded, and a Presidential Disaster Proclamation was declared for many counties in May 2021. This flash flood event was the worst seen in Middle Tennessee since the May 1-2, 2010 flood. Several roads were flooded across the county.", "ts_dict_index": [366, 367, 368]}
+{"event_id": 859094, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 19:30:00", "end_date_time": "2019-10-31 22:15:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. There was two to three feet of water on Graffenburg Road.", "ts_dict_index": [336, 337, 338]}
+{"event_id": 1131017, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. The road was washed out near the intersection of Good Hope Road and Hotchkiss Road.", "ts_dict_index": [390, 391, 392]}
+{"event_id": 1131016, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. A portion of the road near the intersection of Orr Road and Washington Drive was washed out due to flash flooding.", "ts_dict_index": [393, 394, 395]}
+{"event_id": 1131012, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. A portion of Gornto Road was washed out due to flash flooding.", "ts_dict_index": [405, 406, 407]}
+{"event_id": 1131014, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. A portion of Jennifer Circle was washed out due to flash flooding.", "ts_dict_index": [399, 400, 401]}
+{"event_id": 1130999, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:30:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. The road was washed out due to flash flooding near the intersection of Flatswood Lane and Cooper Road.", "ts_dict_index": [414, 415, 416]}
+{"event_id": 1131011, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. The road was washed out near the intersection of Melody Lane and W Gordon Street due to flash flooding.", "ts_dict_index": [408, 409, 410]}
+{"event_id": 1131010, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. A portion of N Barack Obama Blvd was washed out due to flash flooding.", "ts_dict_index": [411, 412, 413]}
+{"event_id": 1131009, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. The road was washed out near the intersection of Hunt Road and Inner Perimeter Road due to flash flooding.", "ts_dict_index": [420, 421, 422]}
+{"event_id": 1131013, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. A portion of Northside Dr was washed out due to flash flooding.", "ts_dict_index": [402, 403, 404]}
+{"event_id": 1131008, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. Many roads were impassible due to flash flooding in the Valdosta area.", "ts_dict_index": [423, 424, 425]}
+{"event_id": 860785, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 21:00:00", "end_date_time": "2019-10-31 22:15:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. A bridge on Gray-Wilmurt Road was washed out.", "ts_dict_index": [348, 349, 350]}
+{"event_id": 1131007, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. A portion of Exit 11 of I-75 was washed out due to flash flooding.", "ts_dict_index": [426, 427, 428]}
+{"event_id": 1131004, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. A portion of Highway 41 was washed out due to flash flooding.", "ts_dict_index": [432, 433, 434]}
+{"event_id": 875878, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-12 07:13:00", "end_date_time": "2020-04-12 10:00:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. A road was flooded and closed in Whitehouse. Vehicles were stranded. Report from mPING.", "ts_dict_index": [435, 436, 437]}
+{"event_id": 1131006, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. A portion of Scottwood Dr was washed out due to flash flooding.", "ts_dict_index": [429, 430, 431]}
+{"event_id": 833030, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2019-07-16 15:03:00", "end_date_time": "2019-07-16 17:00:00", "narrative": "The remnants of Tropical Storm Barry drifted north into Northcentral Arkansas during the early morning hours of July 16th. Meanwhile, a very moist air mass lingered south of this remnant center of circulation, as a weak shortwave trough rounded the center, enhancing large scale forcing over Eastern McCurtain County Oklahoma and the northern sections of Southwest Arkansas. Low level warm and moist air was fed into these areas on a west/southwest low level flow, and provided the additional fuel needed to trigger nearly continuous showers and embedded thunderstorms containing locally heavy rainfall, which moved repeatedly over much of Howard, Northern Hempstead, and Northern Nevada Counties. Based on available surface gauges in these areas, widespread rainfall amounts of 6-10+ inches fell through much of the morning hours of the 16th, which resulted in widespread severe flash flooding. A National Weather Service cooperative observer in Dierks (Howard County) recorded 16.17 inches, which set a maximum 24 hour rainfall record for the state of Arkansas, a maximum 24 hour rainfall record for the month of July for Arkansas, and a maximum rainfall record caused by a tropical cyclone or its remnants throughout Arkansas. The heavy rainfall finally exited the northern sections of Southwest Arkansas around midday on the 16th.||At least 13 high water rescues were performed, numerous roadways (including portions of Interstate 30 between Prescott and Gurdon) were flooded and closed, with other roadways washed out. ||Howard County sustained the most significant and widespread flooding, with at least 30-40 structures sustaining flood damage, including the Howard County Sheriff's Office and the Nashville Police Station. Numerous cars were flooded and swept away in Dierks, along with flooding to several structures, and the loss of over 200 head of cattle. ||In Northern Hempstead and Nevada Counties, structural flooding was more isolated. Numerous roads and bridges were washed out, including state and U.S. highways. In Hempstead County, 20 roads were washed out or damaged. Despite the numerous high water rescues, no injuries or fatalities were reported. Another (a second) culvert was washed out on Highway 371 east of Blevins. Highway 371 was closed between Blevins and Prescott due to flooding/portions of the road being washed out.", "ts_dict_index": [441, 442, 443]}
+{"event_id": 833029, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2019-07-16 12:06:00", "end_date_time": "2019-07-16 17:00:00", "narrative": "The remnants of Tropical Storm Barry drifted north into Northcentral Arkansas during the early morning hours of July 16th. Meanwhile, a very moist air mass lingered south of this remnant center of circulation, as a weak shortwave trough rounded the center, enhancing large scale forcing over Eastern McCurtain County Oklahoma and the northern sections of Southwest Arkansas. Low level warm and moist air was fed into these areas on a west/southwest low level flow, and provided the additional fuel needed to trigger nearly continuous showers and embedded thunderstorms containing locally heavy rainfall, which moved repeatedly over much of Howard, Northern Hempstead, and Northern Nevada Counties. Based on available surface gauges in these areas, widespread rainfall amounts of 6-10+ inches fell through much of the morning hours of the 16th, which resulted in widespread severe flash flooding. A National Weather Service cooperative observer in Dierks (Howard County) recorded 16.17 inches, which set a maximum 24 hour rainfall record for the state of Arkansas, a maximum 24 hour rainfall record for the month of July for Arkansas, and a maximum rainfall record caused by a tropical cyclone or its remnants throughout Arkansas. The heavy rainfall finally exited the northern sections of Southwest Arkansas around midday on the 16th.||At least 13 high water rescues were performed, numerous roadways (including portions of Interstate 30 between Prescott and Gurdon) were flooded and closed, with other roadways washed out. ||Howard County sustained the most significant and widespread flooding, with at least 30-40 structures sustaining flood damage, including the Howard County Sheriff's Office and the Nashville Police Station. Numerous cars were flooded and swept away in Dierks, along with flooding to several structures, and the loss of over 200 head of cattle. ||In Northern Hempstead and Nevada Counties, structural flooding was more isolated. Numerous roads and bridges were washed out, including state and U.S. highways. In Hempstead County, 20 roads were washed out or damaged. Despite the numerous high water rescues, no injuries or fatalities were reported. Highway 195 at Highway 371 was closed due to flooding.", "ts_dict_index": [444, 445, 446]}
+{"event_id": 833023, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2019-07-16 08:50:00", "end_date_time": "2019-07-16 17:00:00", "narrative": "The remnants of Tropical Storm Barry drifted north into Northcentral Arkansas during the early morning hours of July 16th. Meanwhile, a very moist air mass lingered south of this remnant center of circulation, as a weak shortwave trough rounded the center, enhancing large scale forcing over Eastern McCurtain County Oklahoma and the northern sections of Southwest Arkansas. Low level warm and moist air was fed into these areas on a west/southwest low level flow, and provided the additional fuel needed to trigger nearly continuous showers and embedded thunderstorms containing locally heavy rainfall, which moved repeatedly over much of Howard, Northern Hempstead, and Northern Nevada Counties. Based on available surface gauges in these areas, widespread rainfall amounts of 6-10+ inches fell through much of the morning hours of the 16th, which resulted in widespread severe flash flooding. A National Weather Service cooperative observer in Dierks (Howard County) recorded 16.17 inches, which set a maximum 24 hour rainfall record for the state of Arkansas, a maximum 24 hour rainfall record for the month of July for Arkansas, and a maximum rainfall record caused by a tropical cyclone or its remnants throughout Arkansas. The heavy rainfall finally exited the northern sections of Southwest Arkansas around midday on the 16th.||At least 13 high water rescues were performed, numerous roadways (including portions of Interstate 30 between Prescott and Gurdon) were flooded and closed, with other roadways washed out. ||Howard County sustained the most significant and widespread flooding, with at least 30-40 structures sustaining flood damage, including the Howard County Sheriff's Office and the Nashville Police Station. Numerous cars were flooded and swept away in Dierks, along with flooding to several structures, and the loss of over 200 head of cattle. ||In Northern Hempstead and Nevada Counties, structural flooding was more isolated. Numerous roads and bridges were washed out, including state and U.S. highways. In Hempstead County, 20 roads were washed out or damaged. Despite the numerous high water rescues, no injuries or fatalities were reported. Numerous county roads throughout Northern Hempstead County were underwater and closed.", "ts_dict_index": [438, 439, 440]}
+{"event_id": 1131015, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 12:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. The road was washed out near the intersection of Bemiss Knights Academy Road and Studstill Road.", "ts_dict_index": [396, 397, 398]}
+{"event_id": 833008, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2019-07-16 05:25:00", "end_date_time": "2019-07-16 17:00:00", "narrative": "The remnants of Tropical Storm Barry drifted north into Northcentral Arkansas during the early morning hours of July 16th. Meanwhile, a very moist air mass lingered south of this remnant center of circulation, as a weak shortwave trough rounded the center, enhancing large scale forcing over Eastern McCurtain County Oklahoma and the northern sections of Southwest Arkansas. Low level warm and moist air was fed into these areas on a west/southwest low level flow, and provided the additional fuel needed to trigger nearly continuous showers and embedded thunderstorms containing locally heavy rainfall, which moved repeatedly over much of Howard, Northern Hempstead, and Northern Nevada Counties. Based on available surface gauges in these areas, widespread rainfall amounts of 6-10+ inches fell through much of the morning hours of the 16th, which resulted in widespread severe flash flooding. A National Weather Service cooperative observer in Dierks (Howard County) recorded 16.17 inches, which set a maximum 24 hour rainfall record for the state of Arkansas, a maximum 24 hour rainfall record for the month of July for Arkansas, and a maximum rainfall record caused by a tropical cyclone or its remnants throughout Arkansas. The heavy rainfall finally exited the northern sections of Southwest Arkansas around midday on the 16th.||At least 13 high water rescues were performed, numerous roadways (including portions of Interstate 30 between Prescott and Gurdon) were flooded and closed, with other roadways washed out. ||Howard County sustained the most significant and widespread flooding, with at least 30-40 structures sustaining flood damage, including the Howard County Sheriff's Office and the Nashville Police Station. Numerous cars were flooded and swept away in Dierks, along with flooding to several structures, and the loss of over 200 head of cattle. ||In Northern Hempstead and Nevada Counties, structural flooding was more isolated. Numerous roads and bridges were washed out, including state and U.S. highways. In Hempstead County, 20 roads were washed out or damaged. Despite the numerous high water rescues, no injuries or fatalities were reported. Significant flooding was reported by the Arkansas State Police all along Highway 371 between Nashville and Prescott.", "ts_dict_index": [450, 451, 452]}
+{"event_id": 982169, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-08-21 06:00:00", "end_date_time": "2021-08-21 06:00:00", "narrative": "The deadliest flash flood to ever affect Middle Tennessee, and one of the worst natural disasters in the history of the state, struck the region on Saturday, August 21, 2021. Occurring only a few months after another deadly and disastrous flash flood impacted the Nashville metro area on March 27-28, 2021 and killed 7 people, this flash flood left catastrophic damage across several counties in western Middle Tennessee, including parts of Dickson County, Hickman County, Houston County, and especially Humphreys County. The flood waters damaged or destroyed hundreds of homes, businesses, vehicles, and schools, with many buildings washed completely off their foundations. The damage was so severe that a Presidential Disaster Declaration was declared for Humphreys County two days later on August 23, 2021. Later in the week, Dickson, Hickman, and Houston Counties also received a Presidential Disaster Declaration. Very sadly, a total of 20 people were determined to have drowned in the flood, 19 of which were in the city of Waverly, TN, and 1 in the community of Hurricane Mills.||This historic flash flood occurred as a thunderstorms repeatedly developed along a weak surface front located over western Middle Tennessee during the morning hours of August 21. With a very moisture-laden atmosphere in place characterized by precipitable water values measured at 2.37 inches on the 12Z OHX upper air balloon sounding, these thunderstorms produced extreme rainfall rates over 3 inches per hour for several hours, resulting in rainfall totals reaching over 10 to 20 inches in a narrow, roughly 25 mile wide by 50 mile long swath across Houston, Dickson, Humphreys, and Hickman Counties. A rain gauge at the McEwen Wastewater Treatment Plant measured a rainfall total of 20.73 inches from midnight to 7pm CDT, which was verified by NWS personnel and set a new Tennessee state record for 24-hour rainfall. In addition to the flash flooding, one brief tornado was determined to have touched down in rural Dickson County northwest of Charlotte. Highway 46 near College Street was closed due to flooding.", "ts_dict_index": [465, 466, 467]}
+{"event_id": 982179, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-08-21 07:03:00", "end_date_time": "2021-08-21 07:03:00", "narrative": "The deadliest flash flood to ever affect Middle Tennessee, and one of the worst natural disasters in the history of the state, struck the region on Saturday, August 21, 2021. Occurring only a few months after another deadly and disastrous flash flood impacted the Nashville metro area on March 27-28, 2021 and killed 7 people, this flash flood left catastrophic damage across several counties in western Middle Tennessee, including parts of Dickson County, Hickman County, Houston County, and especially Humphreys County. The flood waters damaged or destroyed hundreds of homes, businesses, vehicles, and schools, with many buildings washed completely off their foundations. The damage was so severe that a Presidential Disaster Declaration was declared for Humphreys County two days later on August 23, 2021. Later in the week, Dickson, Hickman, and Houston Counties also received a Presidential Disaster Declaration. Very sadly, a total of 20 people were determined to have drowned in the flood, 19 of which were in the city of Waverly, TN, and 1 in the community of Hurricane Mills.||This historic flash flood occurred as a thunderstorms repeatedly developed along a weak surface front located over western Middle Tennessee during the morning hours of August 21. With a very moisture-laden atmosphere in place characterized by precipitable water values measured at 2.37 inches on the 12Z OHX upper air balloon sounding, these thunderstorms produced extreme rainfall rates over 3 inches per hour for several hours, resulting in rainfall totals reaching over 10 to 20 inches in a narrow, roughly 25 mile wide by 50 mile long swath across Houston, Dickson, Humphreys, and Hickman Counties. A rain gauge at the McEwen Wastewater Treatment Plant measured a rainfall total of 20.73 inches from midnight to 7pm CDT, which was verified by NWS personnel and set a new Tennessee state record for 24-hour rainfall. In addition to the flash flooding, one brief tornado was determined to have touched down in rural Dickson County northwest of Charlotte. Homes were flooded around Greystone Golf Club in Dickson.", "ts_dict_index": [459, 460, 461]}
+{"event_id": 982523, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-08-21 08:06:00", "end_date_time": "2021-08-21 08:06:00", "narrative": "The deadliest flash flood to ever affect Middle Tennessee, and one of the worst natural disasters in the history of the state, struck the region on Saturday, August 21, 2021. Occurring only a few months after another deadly and disastrous flash flood impacted the Nashville metro area on March 27-28, 2021 and killed 7 people, this flash flood left catastrophic damage across several counties in western Middle Tennessee, including parts of Dickson County, Hickman County, Houston County, and especially Humphreys County. The flood waters damaged or destroyed hundreds of homes, businesses, vehicles, and schools, with many buildings washed completely off their foundations. The damage was so severe that a Presidential Disaster Declaration was declared for Humphreys County two days later on August 23, 2021. Later in the week, Dickson, Hickman, and Houston Counties also received a Presidential Disaster Declaration. Very sadly, a total of 20 people were determined to have drowned in the flood, 19 of which were in the city of Waverly, TN, and 1 in the community of Hurricane Mills.||This historic flash flood occurred as a thunderstorms repeatedly developed along a weak surface front located over western Middle Tennessee during the morning hours of August 21. With a very moisture-laden atmosphere in place characterized by precipitable water values measured at 2.37 inches on the 12Z OHX upper air balloon sounding, these thunderstorms produced extreme rainfall rates over 3 inches per hour for several hours, resulting in rainfall totals reaching over 10 to 20 inches in a narrow, roughly 25 mile wide by 50 mile long swath across Houston, Dickson, Humphreys, and Hickman Counties. A rain gauge at the McEwen Wastewater Treatment Plant measured a rainfall total of 20.73 inches from midnight to 7pm CDT, which was verified by NWS personnel and set a new Tennessee state record for 24-hour rainfall. In addition to the flash flooding, one brief tornado was determined to have touched down in rural Dickson County northwest of Charlotte. Several apartments in the Hidden Valley Apartments complex on Spring Street near Henslee Drive were flooded with water up to the roofs of cars in the parking lot.", "ts_dict_index": [453, 454, 455]}
+{"event_id": 982168, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-08-21 04:12:00", "end_date_time": "2021-08-21 04:12:00", "narrative": "The deadliest flash flood to ever affect Middle Tennessee, and one of the worst natural disasters in the history of the state, struck the region on Saturday, August 21, 2021. Occurring only a few months after another deadly and disastrous flash flood impacted the Nashville metro area on March 27-28, 2021 and killed 7 people, this flash flood left catastrophic damage across several counties in western Middle Tennessee, including parts of Dickson County, Hickman County, Houston County, and especially Humphreys County. The flood waters damaged or destroyed hundreds of homes, businesses, vehicles, and schools, with many buildings washed completely off their foundations. The damage was so severe that a Presidential Disaster Declaration was declared for Humphreys County two days later on August 23, 2021. Later in the week, Dickson, Hickman, and Houston Counties also received a Presidential Disaster Declaration. Very sadly, a total of 20 people were determined to have drowned in the flood, 19 of which were in the city of Waverly, TN, and 1 in the community of Hurricane Mills.||This historic flash flood occurred as a thunderstorms repeatedly developed along a weak surface front located over western Middle Tennessee during the morning hours of August 21. With a very moisture-laden atmosphere in place characterized by precipitable water values measured at 2.37 inches on the 12Z OHX upper air balloon sounding, these thunderstorms produced extreme rainfall rates over 3 inches per hour for several hours, resulting in rainfall totals reaching over 10 to 20 inches in a narrow, roughly 25 mile wide by 50 mile long swath across Houston, Dickson, Humphreys, and Hickman Counties. A rain gauge at the McEwen Wastewater Treatment Plant measured a rainfall total of 20.73 inches from midnight to 7pm CDT, which was verified by NWS personnel and set a new Tennessee state record for 24-hour rainfall. In addition to the flash flooding, one brief tornado was determined to have touched down in rural Dickson County northwest of Charlotte. Multiple roads were closed due to high water across Dickson and the southern part of Dickson County.", "ts_dict_index": [462, 463, 464]}
+{"event_id": 982524, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-08-21 08:09:00", "end_date_time": "2021-08-21 08:09:00", "narrative": "The deadliest flash flood to ever affect Middle Tennessee, and one of the worst natural disasters in the history of the state, struck the region on Saturday, August 21, 2021. Occurring only a few months after another deadly and disastrous flash flood impacted the Nashville metro area on March 27-28, 2021 and killed 7 people, this flash flood left catastrophic damage across several counties in western Middle Tennessee, including parts of Dickson County, Hickman County, Houston County, and especially Humphreys County. The flood waters damaged or destroyed hundreds of homes, businesses, vehicles, and schools, with many buildings washed completely off their foundations. The damage was so severe that a Presidential Disaster Declaration was declared for Humphreys County two days later on August 23, 2021. Later in the week, Dickson, Hickman, and Houston Counties also received a Presidential Disaster Declaration. Very sadly, a total of 20 people were determined to have drowned in the flood, 19 of which were in the city of Waverly, TN, and 1 in the community of Hurricane Mills.||This historic flash flood occurred as a thunderstorms repeatedly developed along a weak surface front located over western Middle Tennessee during the morning hours of August 21. With a very moisture-laden atmosphere in place characterized by precipitable water values measured at 2.37 inches on the 12Z OHX upper air balloon sounding, these thunderstorms produced extreme rainfall rates over 3 inches per hour for several hours, resulting in rainfall totals reaching over 10 to 20 inches in a narrow, roughly 25 mile wide by 50 mile long swath across Houston, Dickson, Humphreys, and Hickman Counties. A rain gauge at the McEwen Wastewater Treatment Plant measured a rainfall total of 20.73 inches from midnight to 7pm CDT, which was verified by NWS personnel and set a new Tennessee state record for 24-hour rainfall. In addition to the flash flooding, one brief tornado was determined to have touched down in rural Dickson County northwest of Charlotte. Several homes and businesses were flooded near Highway 70 South across from Tristart Horizon Hospital.", "ts_dict_index": [456, 457, 458]}
+{"event_id": 982520, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-08-21 07:11:00", "end_date_time": "2021-08-21 07:11:00", "narrative": "The deadliest flash flood to ever affect Middle Tennessee, and one of the worst natural disasters in the history of the state, struck the region on Saturday, August 21, 2021. Occurring only a few months after another deadly and disastrous flash flood impacted the Nashville metro area on March 27-28, 2021 and killed 7 people, this flash flood left catastrophic damage across several counties in western Middle Tennessee, including parts of Dickson County, Hickman County, Houston County, and especially Humphreys County. The flood waters damaged or destroyed hundreds of homes, businesses, vehicles, and schools, with many buildings washed completely off their foundations. The damage was so severe that a Presidential Disaster Declaration was declared for Humphreys County two days later on August 23, 2021. Later in the week, Dickson, Hickman, and Houston Counties also received a Presidential Disaster Declaration. Very sadly, a total of 20 people were determined to have drowned in the flood, 19 of which were in the city of Waverly, TN, and 1 in the community of Hurricane Mills.||This historic flash flood occurred as a thunderstorms repeatedly developed along a weak surface front located over western Middle Tennessee during the morning hours of August 21. With a very moisture-laden atmosphere in place characterized by precipitable water values measured at 2.37 inches on the 12Z OHX upper air balloon sounding, these thunderstorms produced extreme rainfall rates over 3 inches per hour for several hours, resulting in rainfall totals reaching over 10 to 20 inches in a narrow, roughly 25 mile wide by 50 mile long swath across Houston, Dickson, Humphreys, and Hickman Counties. A rain gauge at the McEwen Wastewater Treatment Plant measured a rainfall total of 20.73 inches from midnight to 7pm CDT, which was verified by NWS personnel and set a new Tennessee state record for 24-hour rainfall. In addition to the flash flooding, one brief tornado was determined to have touched down in rural Dickson County northwest of Charlotte. Water covered the road near 825 North Mount Sinai Road.", "ts_dict_index": [477, 478, 479]}
+{"event_id": 982170, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-08-21 06:40:00", "end_date_time": "2021-08-21 06:40:00", "narrative": "The deadliest flash flood to ever affect Middle Tennessee, and one of the worst natural disasters in the history of the state, struck the region on Saturday, August 21, 2021. Occurring only a few months after another deadly and disastrous flash flood impacted the Nashville metro area on March 27-28, 2021 and killed 7 people, this flash flood left catastrophic damage across several counties in western Middle Tennessee, including parts of Dickson County, Hickman County, Houston County, and especially Humphreys County. The flood waters damaged or destroyed hundreds of homes, businesses, vehicles, and schools, with many buildings washed completely off their foundations. The damage was so severe that a Presidential Disaster Declaration was declared for Humphreys County two days later on August 23, 2021. Later in the week, Dickson, Hickman, and Houston Counties also received a Presidential Disaster Declaration. Very sadly, a total of 20 people were determined to have drowned in the flood, 19 of which were in the city of Waverly, TN, and 1 in the community of Hurricane Mills.||This historic flash flood occurred as a thunderstorms repeatedly developed along a weak surface front located over western Middle Tennessee during the morning hours of August 21. With a very moisture-laden atmosphere in place characterized by precipitable water values measured at 2.37 inches on the 12Z OHX upper air balloon sounding, these thunderstorms produced extreme rainfall rates over 3 inches per hour for several hours, resulting in rainfall totals reaching over 10 to 20 inches in a narrow, roughly 25 mile wide by 50 mile long swath across Houston, Dickson, Humphreys, and Hickman Counties. A rain gauge at the McEwen Wastewater Treatment Plant measured a rainfall total of 20.73 inches from midnight to 7pm CDT, which was verified by NWS personnel and set a new Tennessee state record for 24-hour rainfall. In addition to the flash flooding, one brief tornado was determined to have touched down in rural Dickson County northwest of Charlotte. Water covered the roadways at Highway 48 and Brazzell Road.", "ts_dict_index": [468, 469, 470]}
+{"event_id": 982521, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-08-21 07:34:00", "end_date_time": "2021-08-21 07:34:00", "narrative": "The deadliest flash flood to ever affect Middle Tennessee, and one of the worst natural disasters in the history of the state, struck the region on Saturday, August 21, 2021. Occurring only a few months after another deadly and disastrous flash flood impacted the Nashville metro area on March 27-28, 2021 and killed 7 people, this flash flood left catastrophic damage across several counties in western Middle Tennessee, including parts of Dickson County, Hickman County, Houston County, and especially Humphreys County. The flood waters damaged or destroyed hundreds of homes, businesses, vehicles, and schools, with many buildings washed completely off their foundations. The damage was so severe that a Presidential Disaster Declaration was declared for Humphreys County two days later on August 23, 2021. Later in the week, Dickson, Hickman, and Houston Counties also received a Presidential Disaster Declaration. Very sadly, a total of 20 people were determined to have drowned in the flood, 19 of which were in the city of Waverly, TN, and 1 in the community of Hurricane Mills.||This historic flash flood occurred as a thunderstorms repeatedly developed along a weak surface front located over western Middle Tennessee during the morning hours of August 21. With a very moisture-laden atmosphere in place characterized by precipitable water values measured at 2.37 inches on the 12Z OHX upper air balloon sounding, these thunderstorms produced extreme rainfall rates over 3 inches per hour for several hours, resulting in rainfall totals reaching over 10 to 20 inches in a narrow, roughly 25 mile wide by 50 mile long swath across Houston, Dickson, Humphreys, and Hickman Counties. A rain gauge at the McEwen Wastewater Treatment Plant measured a rainfall total of 20.73 inches from midnight to 7pm CDT, which was verified by NWS personnel and set a new Tennessee state record for 24-hour rainfall. In addition to the flash flooding, one brief tornado was determined to have touched down in rural Dickson County northwest of Charlotte. A home was flooded at Highway 48 South and I-40.", "ts_dict_index": [474, 475, 476]}
+{"event_id": 982183, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-08-21 07:09:00", "end_date_time": "2021-08-21 07:09:00", "narrative": "The deadliest flash flood to ever affect Middle Tennessee, and one of the worst natural disasters in the history of the state, struck the region on Saturday, August 21, 2021. Occurring only a few months after another deadly and disastrous flash flood impacted the Nashville metro area on March 27-28, 2021 and killed 7 people, this flash flood left catastrophic damage across several counties in western Middle Tennessee, including parts of Dickson County, Hickman County, Houston County, and especially Humphreys County. The flood waters damaged or destroyed hundreds of homes, businesses, vehicles, and schools, with many buildings washed completely off their foundations. The damage was so severe that a Presidential Disaster Declaration was declared for Humphreys County two days later on August 23, 2021. Later in the week, Dickson, Hickman, and Houston Counties also received a Presidential Disaster Declaration. Very sadly, a total of 20 people were determined to have drowned in the flood, 19 of which were in the city of Waverly, TN, and 1 in the community of Hurricane Mills.||This historic flash flood occurred as a thunderstorms repeatedly developed along a weak surface front located over western Middle Tennessee during the morning hours of August 21. With a very moisture-laden atmosphere in place characterized by precipitable water values measured at 2.37 inches on the 12Z OHX upper air balloon sounding, these thunderstorms produced extreme rainfall rates over 3 inches per hour for several hours, resulting in rainfall totals reaching over 10 to 20 inches in a narrow, roughly 25 mile wide by 50 mile long swath across Houston, Dickson, Humphreys, and Hickman Counties. A rain gauge at the McEwen Wastewater Treatment Plant measured a rainfall total of 20.73 inches from midnight to 7pm CDT, which was verified by NWS personnel and set a new Tennessee state record for 24-hour rainfall. In addition to the flash flooding, one brief tornado was determined to have touched down in rural Dickson County northwest of Charlotte. Several homes were flooded on Royal Oak Drive in Dickson.", "ts_dict_index": [480, 481, 482]}
+{"event_id": 1131000, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-08-30 10:00:00", "end_date_time": "2023-08-30 11:45:00", "narrative": "Hurricane Idalia made landfall on the morning of August 30th along the coast of Taylor County Florida near Keaton Beach at approximately 745 am EDT. The hurricane made landfall with estimated sustained winds of 125 mph, making it a Category 3 hurricane on the Saffir-Simpson Hurricane Wind Scale, the first major hurricane on record to make landfall in this portion of Florida. Hurricane Idalia moved inland across the eastern Florida Big Bend and into South Central Georgia during the morning hours. Strong winds caused extensive damage to trees, buildings, and infrastructure along a broad swath stretching west to Tallahassee and east beyond the Suwannee River. Significant and devastating storm surge accompanied the hurricane into the Taylor and Dixie County coasts, where water levels rose considerably, inundating numerous structures along the coast and flooding residences and businesses many miles inland. Significant damage to property and infrastructure was associated with the storm surge that will take a considerable time to rebuild. The peak surge values observed were from Dekle Beach in Taylor County southeastward to Horseshoe Beach in Dixie County. Surge heights in this area along the immediate coast were within the range of 7 to 12 feet above normally dry ground. Lower values of up to 6 feet above normally dry ground were noted south of Horseshoe Beach near the community of Suwannee. It should also be noted the storm made landfall around the time of low tide. Had the storm made landfall 6 hours later, around the time of high tide, peak water level values could have been between 3-4 feet higher.  In the process of the high water mark surveys, interviews were conducted with several residents that lived in the area during the Storm of the Century, a non-tropical system that affected this portion of the Florida coastline on March 13, 1993. All of these residents interviewed from Keaton Beach to Horseshoe Beach indicated water levels that rivaled or exceeded those experienced in the 1993 ���Storm of the Century.��� Moreover, Dixie County Emergency Management noted that the inland extent of the storm surge from Hurricane Idalia moved much further inland from Horseshoe Beach than observed in The Storm of the Century. One direct fatality occurred in south-central Georgia as a result of the storm. A portion of Val Del Road was washed out due to flash flooding.", "ts_dict_index": [417, 418, 419]}
+{"event_id": 817179, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-05-02 01:34:00", "end_date_time": "2019-05-02 02:30:00", "narrative": "A deep southerly flow increased across much of the Ark-La-Tex during the daytime hours of April 30th through May 1st, ahead of a slow moving upper level trough that drifted east into the Southern Plains from the Four Corners Region. A complex of showers and thunderstorms that developed over Western and Central Oklahoma during the evening of April 30th ahead of a stalled surface frontal boundary sent a cold pool southeast into portions of extreme Northeast Texas and Southwest Arkansas which eventually stalled out during the early morning hours on May 1st. Weak upper level disturbances in the southwest flow aloft ahead of the approaching trough triggered additional showers and thunderstorms across Northcentral Texas, which spread east northeast across East Texas, Southwest Arkansas, and North Louisiana during the evening hours of the 1st, and continued throughout the morning hours of the 2nd. The earlier stalled boundary over Northeast Texas and Southwest Arkansas helped to enhance the showers and thunderstorms, and coupled with the instability and deep moisture in place, some of the showers and thunderstorm became severe, producing large hail, damaging winds, and locally heavy rainfall. An isolated tornado even touched down across Eastern Shelby County Texas just prior to daybreak on the 2nd. Where the storms moved repeatedly over the same areas, flash flooding was observed with several roads flooded and closed across portions of East Texas. ||While the storms diminished shortly after daybreak on the 2nd, another complex of showers and thunderstorms developed during the late afternoon through the evening hours in Central and Southeast Texas ahead of another shortwave trough, with a portion of this complex migrating into Deep East Texas by mid-evening. Given the moderate instability in place across this area due to strong daytime heating, some of these storms also became severe, with damaging winds downing trees and destroying a chicken house in Northern Nacogdoches County before weakening by late evening. Numerous roads were flooded in and near Tyler, including FM 724, FM 2868, Highway 69, and Highway 110.", "ts_dict_index": [483, 484, 485]}
+{"event_id": 817216, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-05-02 03:55:00", "end_date_time": "2019-05-02 05:30:00", "narrative": "A deep southerly flow increased across much of the Ark-La-Tex during the daytime hours of April 30th through May 1st, ahead of a slow moving upper level trough that drifted east into the Southern Plains from the Four Corners Region. A complex of showers and thunderstorms that developed over Western and Central Oklahoma during the evening of April 30th ahead of a stalled surface frontal boundary sent a cold pool southeast into portions of extreme Northeast Texas and Southwest Arkansas which eventually stalled out during the early morning hours on May 1st. Weak upper level disturbances in the southwest flow aloft ahead of the approaching trough triggered additional showers and thunderstorms across Northcentral Texas, which spread east northeast across East Texas, Southwest Arkansas, and North Louisiana during the evening hours of the 1st, and continued throughout the morning hours of the 2nd. The earlier stalled boundary over Northeast Texas and Southwest Arkansas helped to enhance the showers and thunderstorms, and coupled with the instability and deep moisture in place, some of the showers and thunderstorm became severe, producing large hail, damaging winds, and locally heavy rainfall. An isolated tornado even touched down across Eastern Shelby County Texas just prior to daybreak on the 2nd. Where the storms moved repeatedly over the same areas, flash flooding was observed with several roads flooded and closed across portions of East Texas. ||While the storms diminished shortly after daybreak on the 2nd, another complex of showers and thunderstorms developed during the late afternoon through the evening hours in Central and Southeast Texas ahead of another shortwave trough, with a portion of this complex migrating into Deep East Texas by mid-evening. Given the moderate instability in place across this area due to strong daytime heating, some of these storms also became severe, with damaging winds downing trees and destroying a chicken house in Northern Nacogdoches County before weakening by late evening. FM 2089 was flooded just southwest of Overton at the Smith/Rusk County line.", "ts_dict_index": [486, 487, 488]}
+{"event_id": 979021, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 05:50:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was reported on the 800 block of Freeport Road, which was closed.", "ts_dict_index": [495, 496, 497]}
+{"event_id": 817172, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-05-01 23:59:00", "end_date_time": "2019-05-02 02:30:00", "narrative": "A deep southerly flow increased across much of the Ark-La-Tex during the daytime hours of April 30th through May 1st, ahead of a slow moving upper level trough that drifted east into the Southern Plains from the Four Corners Region. A complex of showers and thunderstorms that developed over Western and Central Oklahoma during the evening of April 30th ahead of a stalled surface frontal boundary sent a cold pool southeast into portions of extreme Northeast Texas and Southwest Arkansas which eventually stalled out during the early morning hours on May 1st. Weak upper level disturbances in the southwest flow aloft ahead of the approaching trough triggered additional showers and thunderstorms across Northcentral Texas, which spread east northeast across East Texas, Southwest Arkansas, and North Louisiana during the evening hours of the 1st, and continued throughout the morning hours of the 2nd. The earlier stalled boundary over Northeast Texas and Southwest Arkansas helped to enhance the showers and thunderstorms, and coupled with the instability and deep moisture in place, some of the showers and thunderstorm became severe, producing large hail, damaging winds, and locally heavy rainfall. An isolated tornado even touched down across Eastern Shelby County Texas just prior to daybreak on the 2nd. Where the storms moved repeatedly over the same areas, flash flooding was observed with several roads flooded and closed across portions of East Texas. ||While the storms diminished shortly after daybreak on the 2nd, another complex of showers and thunderstorms developed during the late afternoon through the evening hours in Central and Southeast Texas ahead of another shortwave trough, with a portion of this complex migrating into Deep East Texas by mid-evening. Given the moderate instability in place across this area due to strong daytime heating, some of these storms also became severe, with damaging winds downing trees and destroying a chicken house in Northern Nacogdoches County before weakening by late evening. Spur 364 was closed due to flooding. A car was also washed off the road. Multiple reports of flooding were received throughout the city of Tyler.", "ts_dict_index": [492, 493, 494]}
+{"event_id": 817180, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-05-02 01:45:00", "end_date_time": "2019-05-02 02:30:00", "narrative": "A deep southerly flow increased across much of the Ark-La-Tex during the daytime hours of April 30th through May 1st, ahead of a slow moving upper level trough that drifted east into the Southern Plains from the Four Corners Region. A complex of showers and thunderstorms that developed over Western and Central Oklahoma during the evening of April 30th ahead of a stalled surface frontal boundary sent a cold pool southeast into portions of extreme Northeast Texas and Southwest Arkansas which eventually stalled out during the early morning hours on May 1st. Weak upper level disturbances in the southwest flow aloft ahead of the approaching trough triggered additional showers and thunderstorms across Northcentral Texas, which spread east northeast across East Texas, Southwest Arkansas, and North Louisiana during the evening hours of the 1st, and continued throughout the morning hours of the 2nd. The earlier stalled boundary over Northeast Texas and Southwest Arkansas helped to enhance the showers and thunderstorms, and coupled with the instability and deep moisture in place, some of the showers and thunderstorm became severe, producing large hail, damaging winds, and locally heavy rainfall. An isolated tornado even touched down across Eastern Shelby County Texas just prior to daybreak on the 2nd. Where the storms moved repeatedly over the same areas, flash flooding was observed with several roads flooded and closed across portions of East Texas. ||While the storms diminished shortly after daybreak on the 2nd, another complex of showers and thunderstorms developed during the late afternoon through the evening hours in Central and Southeast Texas ahead of another shortwave trough, with a portion of this complex migrating into Deep East Texas by mid-evening. Given the moderate instability in place across this area due to strong daytime heating, some of these storms also became severe, with damaging winds downing trees and destroying a chicken house in Northern Nacogdoches County before weakening by late evening. Highway 135 northwest of Troup was flooded.", "ts_dict_index": [489, 490, 491]}
+{"event_id": 984235, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 07:45:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was reported on Blythe Road, with some residents being evacuated.", "ts_dict_index": [501, 502, 503]}
+{"event_id": 984295, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 10:19:00", "end_date_time": "2021-09-01 12:24:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Route 119 was closed in both directions in the area of South Grande Boulevard due to flooding.", "ts_dict_index": [498, 499, 500]}
+{"event_id": 833014, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2019-07-16 07:31:00", "end_date_time": "2019-07-16 17:00:00", "narrative": "The remnants of Tropical Storm Barry drifted north into Northcentral Arkansas during the early morning hours of July 16th. Meanwhile, a very moist air mass lingered south of this remnant center of circulation, as a weak shortwave trough rounded the center, enhancing large scale forcing over Eastern McCurtain County Oklahoma and the northern sections of Southwest Arkansas. Low level warm and moist air was fed into these areas on a west/southwest low level flow, and provided the additional fuel needed to trigger nearly continuous showers and embedded thunderstorms containing locally heavy rainfall, which moved repeatedly over much of Howard, Northern Hempstead, and Northern Nevada Counties. Based on available surface gauges in these areas, widespread rainfall amounts of 6-10+ inches fell through much of the morning hours of the 16th, which resulted in widespread severe flash flooding. A National Weather Service cooperative observer in Dierks (Howard County) recorded 16.17 inches, which set a maximum 24 hour rainfall record for the state of Arkansas, a maximum 24 hour rainfall record for the month of July for Arkansas, and a maximum rainfall record caused by a tropical cyclone or its remnants throughout Arkansas. The heavy rainfall finally exited the northern sections of Southwest Arkansas around midday on the 16th.||At least 13 high water rescues were performed, numerous roadways (including portions of Interstate 30 between Prescott and Gurdon) were flooded and closed, with other roadways washed out. ||Howard County sustained the most significant and widespread flooding, with at least 30-40 structures sustaining flood damage, including the Howard County Sheriff's Office and the Nashville Police Station. Numerous cars were flooded and swept away in Dierks, along with flooding to several structures, and the loss of over 200 head of cattle. ||In Northern Hempstead and Nevada Counties, structural flooding was more isolated. Numerous roads and bridges were washed out, including state and U.S. highways. In Hempstead County, 20 roads were washed out or damaged. Despite the numerous high water rescues, no injuries or fatalities were reported. A culvert was washed out on Highway 371 east of Blevins. Highway 371 was closed in both directions.", "ts_dict_index": [447, 448, 449]}
+{"event_id": 984256, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 09:40:00", "end_date_time": "2021-09-01 12:24:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. On Latrobe Crabtree Road, flooding was reported.", "ts_dict_index": [537, 538, 539]}
+{"event_id": 984236, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 07:36:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooded roads occurred in Washington township, including North Washington Road, Pine Run Road, and Pine Run Church Road.", "ts_dict_index": [504, 505, 506]}
+{"event_id": 984290, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 09:53:00", "end_date_time": "2021-09-01 12:24:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. State Route 119 was flooded near Shady Lane.", "ts_dict_index": [528, 529, 530]}
+{"event_id": 984233, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 07:36:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Hulton Road was reported to be flooded.", "ts_dict_index": [525, 526, 527]}
+{"event_id": 984257, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 09:40:00", "end_date_time": "2021-09-01 12:24:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was reported on South Carbon Street.", "ts_dict_index": [534, 535, 536]}
+{"event_id": 984242, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 08:29:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Water on Goldfinch Lane is approximately waist deep.  About 12 mobile homes have water to their front porch, with four families evacuated.", "ts_dict_index": [516, 517, 518]}
+{"event_id": 984240, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 08:32:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. An underpass on North Greengate Road was flooded with four feet of water.  A vehicle was stuck in the water, with one person escaping through the vehicle window.", "ts_dict_index": [513, 514, 515]}
+{"event_id": 984293, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 10:12:00", "end_date_time": "2021-09-01 12:24:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Crabtree Creek was overflowing its banks, causing flooding on Rizzo Road.", "ts_dict_index": [522, 523, 524]}
+{"event_id": 984291, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 10:00:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was observed on Plum Street between 6th Street and Dark Hollow Road.", "ts_dict_index": [519, 520, 521]}
+{"event_id": 979034, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 06:53:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Multiple homes were flooded on Church Street.", "ts_dict_index": [531, 532, 533]}
+{"event_id": 984238, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 08:10:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was reported on Tunnelton Road.", "ts_dict_index": [507, 508, 509]}
+{"event_id": 984239, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 08:11:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. A swift water team responded to Streets Run Road for a vehicle stuck in water with one occupant.", "ts_dict_index": [510, 511, 512]}
+{"event_id": 979032, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 06:35:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. A school bus was stuck in water at the intersection of Ohio Street and Center Street.  2 adults and 7 children were trapped.  They were eventually rescued with no injuries.", "ts_dict_index": [549, 550, 551]}
+{"event_id": 979019, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 05:49:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. A video on social media showed that Piney Fork was out of its banks and flowing onto Piney Fork Road.", "ts_dict_index": [546, 547, 548]}
+{"event_id": 979033, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 06:51:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Library Road was closed between Kings School Road and Clifton Road due to flooding.  A rail line in the area was also closed.", "ts_dict_index": [543, 544, 545]}
+{"event_id": 979016, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 05:24:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Water was reported to be flowing into a residence on Salem Drive, and flooding was also occurring on Bower Hill Road.", "ts_dict_index": [561, 562, 563]}
+{"event_id": 979017, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 05:30:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was occurring on Spring Valley Road.", "ts_dict_index": [564, 565, 566]}
+{"event_id": 984243, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 08:00:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was reported throughout Oakdale Borough.  The fire and police stations were evacuated.  Approximately 18 inches of water was reported throughout the town.", "ts_dict_index": [558, 559, 560]}
+{"event_id": 984230, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 07:10:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. According to a submitted video, Girtys Run in Millvale by Frederick Street was overflowing on to roads, just shy of reaching houses.", "ts_dict_index": [555, 556, 557]}
+{"event_id": 984234, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 07:41:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. An assisted living facility was flooding and being evacuated.  Twenty-four people were in the building at the time.", "ts_dict_index": [540, 541, 542]}
+{"event_id": 982172, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2021-08-21 07:00:00", "end_date_time": "2021-08-21 07:00:00", "narrative": "The deadliest flash flood to ever affect Middle Tennessee, and one of the worst natural disasters in the history of the state, struck the region on Saturday, August 21, 2021. Occurring only a few months after another deadly and disastrous flash flood impacted the Nashville metro area on March 27-28, 2021 and killed 7 people, this flash flood left catastrophic damage across several counties in western Middle Tennessee, including parts of Dickson County, Hickman County, Houston County, and especially Humphreys County. The flood waters damaged or destroyed hundreds of homes, businesses, vehicles, and schools, with many buildings washed completely off their foundations. The damage was so severe that a Presidential Disaster Declaration was declared for Humphreys County two days later on August 23, 2021. Later in the week, Dickson, Hickman, and Houston Counties also received a Presidential Disaster Declaration. Very sadly, a total of 20 people were determined to have drowned in the flood, 19 of which were in the city of Waverly, TN, and 1 in the community of Hurricane Mills.||This historic flash flood occurred as a thunderstorms repeatedly developed along a weak surface front located over western Middle Tennessee during the morning hours of August 21. With a very moisture-laden atmosphere in place characterized by precipitable water values measured at 2.37 inches on the 12Z OHX upper air balloon sounding, these thunderstorms produced extreme rainfall rates over 3 inches per hour for several hours, resulting in rainfall totals reaching over 10 to 20 inches in a narrow, roughly 25 mile wide by 50 mile long swath across Houston, Dickson, Humphreys, and Hickman Counties. A rain gauge at the McEwen Wastewater Treatment Plant measured a rainfall total of 20.73 inches from midnight to 7pm CDT, which was verified by NWS personnel and set a new Tennessee state record for 24-hour rainfall. In addition to the flash flooding, one brief tornado was determined to have touched down in rural Dickson County northwest of Charlotte. Numerous roads were damaged and closed throughout Dickson County, with dozens of water rescues being conducted. TEMA reported damage to roads throughout the county totaled $401,606.", "ts_dict_index": [471, 472, 473]}
+{"event_id": 979026, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 06:03:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Evacuations were occurring due to flooding at the intersection of Baldwin Street and Railroad Street.", "ts_dict_index": [567, 568, 569]}
+{"event_id": 984255, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 09:27:00", "end_date_time": "2021-09-01 12:24:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was reported on Park Road.  The road was closed.", "ts_dict_index": [579, 580, 581]}
+{"event_id": 984248, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 08:50:00", "end_date_time": "2021-09-01 12:24:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. New Alexandria Road was flooded.", "ts_dict_index": [585, 586, 587]}
+{"event_id": 984253, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 09:15:00", "end_date_time": "2021-09-01 12:24:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was reported on Furnace Lane.", "ts_dict_index": [582, 583, 584]}
+{"event_id": 1101793, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 08:40:00", "end_date_time": "2023-05-01 09:40:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall between 3.5 to 4.5 inches caused a washout on Route 5 in Lovell.", "ts_dict_index": [606, 607, 608]}
+{"event_id": 1033773, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2022-05-05 11:15:00", "end_date_time": "2022-05-05 13:00:00", "narrative": "A strong storm system slowly moved from the central Rockies into the Southern and Central Plains on the 4th and 5th. The associated surface frontal boundary located over northern Texas early on the 4th moved north into central Oklahoma as a warm front by the late afternoon, and then near the Kansas border on the 5th ahead of a cold front. The first round of thunderstorms developed over eastern Oklahoma during the morning hours of the 4th. These thunderstorms were rooted above a shallow, stable layer of air near the ground, and the strongest storms produced hail up to penny size. Another round of thunderstorms developed during the early evening hours. The storms over northeastern Oklahoma were rooted above a shallow, stable layer of air near the ground, and produced large hail up to half dollar size. The thunderstorms that developed over east central Oklahoma near the warm front were rooted near the ground. These storms were able to become supercells, given the moderately strong instability that had developed during the afternoon, combined with strong deep layer wind shear. The low-level wind shear had become strong near the warm front itself, which supported the development of a few tornadoes. Thunderstorms continued to develop across the area during the overnight hours of the 4th and early morning hours of the 5th, which resulted in locally heavy rainfall and flash flooding. The final round of thunderstorms developed during the early afternoon of the 5th, with the strongest storms producing hail up to quarter size.||Widespread, heavy rainfall during this period resulted in three to eight inches of rain across much of east central and northeastern Oklahoma, with areas of up to twelve inches. In addition to the flash flooding, this widespread, heavy rainfall resulted in major flooding along portions of the Neosho River, the Illinois River, the Deep Fork River, and Baron Fork Creek, as well as moderate flooding along portions of Polecat Creek, and the Poteau River. Flooding in Bixby damaged at least 37 homes and four businesses, and flooded roads. Much of the damage was in a neighborhood south of Highway 64 and west of S Mingo Road.", "ts_dict_index": [591, 592, 593]}
+{"event_id": 979023, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 05:53:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was reported on Seavey Road.  A school bus was disabled on the road.", "ts_dict_index": [573, 574, 575]}
+{"event_id": 1101789, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 05:29:00", "end_date_time": "2023-05-01 06:30:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall between 3.5 to 4.5 inches fell over already saturated ground resulting in a 4 foot sinkhole on Smith Road.", "ts_dict_index": [603, 604, 605]}
+{"event_id": 1101804, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:08:00", "end_date_time": "2023-05-01 07:40:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall resulted in excessive runoff and a rapid rise in the Sunday River. A vehicle was stuck in flood waters and necessitated a water rescue on Sunday River Road.", "ts_dict_index": [618, 619, 620]}
+{"event_id": 1101738, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 05:51:00", "end_date_time": "2023-05-01 09:30:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall between 3 and 4 inches fell over Dixfield on the morning of May 1. The heavy rain over saturated ground caused a washout on Averill Hill Road. Severy Hill and Valley Road were closed due to flooding.  Route 164 and Coolidge Road had multiple washouts along the edge of the road. A significant washout occurred on Valley Brook Road.", "ts_dict_index": [600, 601, 602]}
+{"event_id": 1101787, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 06:31:00", "end_date_time": "2023-05-01 08:30:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall between 3.5 to 4.5 inches over already saturated ground resulted in a washout on Route 117 in Denmark.", "ts_dict_index": [627, 628, 629]}
+{"event_id": 1102059, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 08:00:00", "end_date_time": "2023-05-01 09:30:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Flooding of the Darnit Brook damaged Rosenburg and Decoster Roads in Sumner. Decoster Road sustained multiple washouts near the brook crossing and two of five culvers.", "ts_dict_index": [615, 616, 617]}
+{"event_id": 984254, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 09:13:00", "end_date_time": "2021-09-01 12:24:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was reported in a barn with livestock on Business Route 66.", "ts_dict_index": [570, 571, 572]}
+{"event_id": 1102053, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:30:00", "end_date_time": "2023-05-01 10:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Town of Hartford sustained a washout between Route 219 and 140 and damage to two bridges.", "ts_dict_index": [609, 610, 611]}
+{"event_id": 1101797, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:23:00", "end_date_time": "2023-05-01 08:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall between 3.5 to 4.5 inches caused flooding on Stow Road or Maine Route 113 resulting in a water rescue.", "ts_dict_index": [612, 613, 614]}
+{"event_id": 1101800, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:23:00", "end_date_time": "2023-05-01 08:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Flooding on North Road in Gilead resulted in a water rescue to a motorist.", "ts_dict_index": [621, 622, 623]}
+{"event_id": 984246, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-09-01 08:50:00", "end_date_time": "2021-09-01 12:24:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was reported at the intersection of Shannon Creek Road and Michigan Lane.", "ts_dict_index": [588, 589, 590]}
+{"event_id": 938851, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2021-03-01 01:51:00", "end_date_time": "2021-03-01 03:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Highway 194 is impassable due to flood waters below Meathouse Road.", "ts_dict_index": [594, 595, 596]}
+{"event_id": 938845, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2021-03-01 01:17:00", "end_date_time": "2021-03-01 03:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Water was reported flowing over Hwy 199 in the McAndrews community.", "ts_dict_index": [597, 598, 599]}
+{"event_id": 979029, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 06:20:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was occurring at the 1000 block of Evergreen Avenue.  The road was closed.", "ts_dict_index": [552, 553, 554]}
+{"event_id": 1101742, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:46:00", "end_date_time": "2023-05-01 09:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall between 3.5 and 4.5 inches on already saturated ground resulted in a washout on Maine Route 108.", "ts_dict_index": [642, 643, 644]}
+{"event_id": 1101801, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 05:08:00", "end_date_time": "2023-05-01 06:20:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rain resulted in a washout on Gibson Road in West Bethel.", "ts_dict_index": [630, 631, 632]}
+{"event_id": 1101743, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 09:14:00", "end_date_time": "2023-05-01 09:45:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall of 3.5 to 4.5 inches on the morning of May 1 resulted in a washout on South Rumford Road.", "ts_dict_index": [648, 649, 650]}
+{"event_id": 1102146, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 08:00:00", "end_date_time": "2023-05-01 10:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Runoff from Hemingway Ridge caused the Swift Cambridge River to flood and close the major access Route 26, leading to significant disruption to travel in and out of the region.", "ts_dict_index": [645, 646, 647]}
+{"event_id": 1101769, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 09:41:00", "end_date_time": "2023-05-01 10:40:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall between 3.5 to 4.5 inches fell over already saturated ground on the morning of May 1. The resultant flash flood washed out a portion of Route 160.", "ts_dict_index": [639, 640, 641]}
+{"event_id": 1102073, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:30:00", "end_date_time": "2023-05-01 09:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Flash flooding caused washouts on numerous roads in Woodstock including Redding Road, Concord Road, Pond Road, and Swinton Road.", "ts_dict_index": [633, 634, 635]}
+{"event_id": 1101744, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:00:00", "end_date_time": "2023-05-01 08:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall caused the Swift River to rapidly rise and washout on Roxbury Notch Road.", "ts_dict_index": [651, 652, 653]}
+{"event_id": 1102066, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 08:00:00", "end_date_time": "2023-05-01 09:30:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Flash flooding caused numerous shoulder washouts on roads across West Paris. The hardest hit road was along Ellingwood Road near Ryerson Hill Road where a complete washout occurred.", "ts_dict_index": [624, 625, 626]}
+{"event_id": 1102145, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 08:00:00", "end_date_time": "2023-05-01 09:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Runoff from Jim Hill in Norway flooded and resulted in the closure of Route 118.", "ts_dict_index": [666, 667, 668]}
+{"event_id": 1101763, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 04:28:00", "end_date_time": "2023-05-01 05:40:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rainfall between 3.5 to 4.5 inches fell over saturated ground on the morning of May 1. The runoff caused a washout on Waterford Road.", "ts_dict_index": [672, 673, 674]}
+{"event_id": 1101750, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 05:00:00", "end_date_time": "2023-05-01 06:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Washout occurred on Rabbit Valley Road in Otisfield after 3.5 to 4.5 inches of rain fell on saturated ground early in the morning of May 1.", "ts_dict_index": [663, 664, 665]}
+{"event_id": 1101897, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:45:00", "end_date_time": "2023-05-01 09:45:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heay rainfall resulted in numerous road closures and washouts across Brownfield including Sam Brown Hill Road, Hampshire Road, Merrill Corner Road and Dugway Road. There were numerous washouts on Old County Road.", "ts_dict_index": [654, 655, 656]}
+{"event_id": 1101745, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 06:00:00", "end_date_time": "2023-05-01 07:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Washout on Mount Micha Road after approximately 4 inches of rain fell on already saturated ground on the morning of May 1.", "ts_dict_index": [657, 658, 659]}
+{"event_id": 1101747, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 06:31:00", "end_date_time": "2023-05-01 09:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Multiple washouts between Gore Road and Hidden Lake Road on the morning of May 1 after 3.5 to 4.5 inches of rain fell over already saturated ground.", "ts_dict_index": [660, 661, 662]}
+{"event_id": 1123649, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-07-08 19:45:00", "end_date_time": "2023-07-08 20:30:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. Heavy rain on the afternoon of July 8th caused flooding on Tolman Pond and Bancroft Roads in Nelson. Some damage to the roads were reported, along with numerous private roads impacted.", "ts_dict_index": [684, 685, 686]}
+{"event_id": 1123675, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-07-09 16:00:00", "end_date_time": "2023-07-09 21:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. Severe widespread flooding in Swanzey prompted Police to issue a statement Please avoid driving in Swanzey at this time. Numerous roads across the community were flooded and damaged by floodwaters including Route 10, Holbrook Avenue, Old Homestead Highway, East Shore, and Carlton Roads, along with several others.", "ts_dict_index": [681, 682, 683]}
+{"event_id": 1101734, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 06:08:00", "end_date_time": "2023-05-01 07:15:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Flash floods caused a washout on Greenwoods Road after 3.5 to 4.5 inches of rainfall fell on the morning of May 1.", "ts_dict_index": [669, 670, 671]}
+{"event_id": 1124081, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-07-10 19:49:00", "end_date_time": "2023-07-10 21:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. Hill Road flooded from Darby Brook near Drewsville Road.", "ts_dict_index": [678, 679, 680]}
+{"event_id": 979018, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-09-01 05:36:00", "end_date_time": "2021-09-01 10:23:00", "narrative": "The remnant low pressure center of Hurricane Ida passed across West Virginia and the Central Appalachian Mountains from late August 31st through September 1st.  The abundant moisture associated with the low intersected a frontal zone which was nearly stalled in the area of the Ohio Valley.  Strong isentropic and frontogenetically-induced lift led to periods of heavy rain over much of southwestern Pennsylvania over the two-day period, both from thunderstorms ahead of the low and from a period of tropical rainfall during the morning of the 1st.  Rain tapered off by the afternoon as the remnants of Ida pulled towards the Mid-Atlantic coast.||The heaviest rainfall over the two-day period was observed in Westmoreland, Allegheny, and Washington Counties, with totals of 3 to 5 inches common. Lesser totals were noted to the north and south of this area, with areas near Interstate 80 mainly receiving a half-inch or less. The heavy rainfall resulted in widespread flooding of roads and streams, with several instances of evacuations noted.  Particularly hard hit were the municipalities of Millvale, Bridgeville, and Scott, all of which issued disaster declarations.  In Stowe Township, a school bus was trapped in flood waters, requiring the rescue of two adults and seven children.  Other rescues of trapped motorists were noted. Twenty-four residents had to be evacuated from an assisted living facility in Oakdale, where water up to 18 inches deep was observed across the town. ||Despite the heavy rain and numerous instances of flash and areal flooding, widespread river flooding was not observed after the rainfall ceased.  A dry slot near the Mason-Dixon Line on the morning of the 1st kept rainfall totals lower on the headwaters of the Monongahela River, allowing area reservoirs to mitigate the impact of the tropical rain downstream.  Thus, while short-term flooding was significant over a portion of the region, the overall event did not have the same impact as Gordon in 2018 or Frances/Ivan in 2014. Flooding was occurring on McLaughlin Run Road.  The road was being closed.", "ts_dict_index": [576, 577, 578]}
+{"event_id": 1124075, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-07-10 19:15:00", "end_date_time": "2023-07-10 21:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. Flooding caused by the significant rainfall over two days damaged property and roads in the Marlow area.  Most roads were closed due to flooding and residents were advised to stay home.  The flooding produced on the 10-11th of July occurred over areas that were already dealing with previous flooding. The North Fork of the already flooded Ashuelot River flooded portions of Marlow. Another source of flooding came when the Stoddard Lake overflowed totally surounding homes.", "ts_dict_index": [687, 688, 689]}
+{"event_id": 1123653, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-07-09 14:05:00", "end_date_time": "2023-07-09 16:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. Heavy rainfall measured around 4.5 inches caused the closure of main thruway Route 10 near Kapper Drive in Winchester on the afternoon of the 9th. An extensive washout on Route 10 required lengthy repairs to a 600 foot section of the road.", "ts_dict_index": [690, 691, 692]}
+{"event_id": 1102144, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 08:14:00", "end_date_time": "2023-05-01 09:15:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. West Branch of the Nezinscot River flooded Redding Road Bridge.", "ts_dict_index": [636, 637, 638]}
+{"event_id": 1124171, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-07-10 03:05:00", "end_date_time": "2023-07-10 04:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. Following several days of heavy rainfall caused a breach in the Forest Lake Road dam. The initial breach caused flooding on Route 10, and then flowed into the Ashuelot River where the flood wave dampened.", "ts_dict_index": [702, 703, 704]}
+{"event_id": 1124230, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-07-10 16:00:00", "end_date_time": "2023-07-10 17:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. Heavy rain caused the Partridge Brook to flood and washout a portion of Partridge Brook Road in Westmoreland.", "ts_dict_index": [696, 697, 698]}
+{"event_id": 1123652, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-07-09 14:22:00", "end_date_time": "2023-07-09 16:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. After multiple days of heavy rainfall, Swanzey Lake overflowed on July 9th. The flooding caused Swanzey Lake Road to washout and necessitated the evacuation of lakeshore residents.  Fire Department responded with the City of Keene (Cheshire County) swift water rescue team. This caused over 100 vehicles to become stranded and then required the evacuation of nearly 150 guests of the Pilgrim Pines Camp and Retreat Center.", "ts_dict_index": [699, 700, 701]}
+{"event_id": 1004606, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-01-01 09:32:00", "end_date_time": "2022-01-01 11:45:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. KY-468 was reported impassable due to high water, just north of the community of Sydney.", "ts_dict_index": [720, 721, 722]}
+{"event_id": 1005219, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-01-01 10:55:00", "end_date_time": "2022-01-01 11:45:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. A mobile home park was flooded in the community of Zebulon.", "ts_dict_index": [705, 706, 707]}
+{"event_id": 1005229, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-01-01 08:17:00", "end_date_time": "2022-01-01 11:45:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. Water is reported to be in homes in the Belfry Community. Water rescues are about to be performed.", "ts_dict_index": [711, 712, 713]}
+{"event_id": 1004610, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-01-01 10:50:00", "end_date_time": "2022-01-01 11:45:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. A report via social media showed Johns Creek Elementary surrounded by water.", "ts_dict_index": [714, 715, 716]}
+{"event_id": 1004604, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-01-01 09:17:00", "end_date_time": "2022-01-01 11:45:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. Reports of flooding in the community of Belfry. Belfry Middle School is inundated with water.", "ts_dict_index": [708, 709, 710]}
+{"event_id": 1102080, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 09:00:00", "end_date_time": "2023-05-01 09:45:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Bridge washout on Fern Road in Lovell from the Kezar River.", "ts_dict_index": [675, 676, 677]}
+{"event_id": 873205, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-01-11 00:30:00", "end_date_time": "2020-01-11 03:30:00", "narrative": "The month started off with a bang on the 10th. It felt like spring in Arkansas, with high temperatures in the 60s to lower 70s. As the day began, a powerful storm system was looming to the west in New Mexico. Moisture levels were on the rise ahead of the system. It was a perfect setup for severe weather and flash flooding.||By late afternoon and into the overnight hours/early on the 11th, a massive damaging wind episode unfolded. Wind gusts from 60 to 90 mph pounded parts of the state. Trees and/or power lines were downed at Yellville (Marion County), Henderson (Baxter County), Elizabeth (Fulton County), Melbourne (Izard County), Leslie (Searcy County), a few miles west of Arkadelphia (Clark County), Malvern (Hot Spring County), Judsonia (White County), Fordyce (Dallas County), Pine Bluff (Jefferson County), Cotton Plant (Woodruff County), Monticello (Drew County), St. Charles (Arkansas County), and Watson (Desha County). Some fallen trees landed on homes. Wind recording equipment measured a 74 mph gust at Fargo (Monroe County), and a 71 mph gust at the University of Arkansas at Monticello (Drew County).||There were also isolated tornadoes. At 740 pm CST on the 10th, a tornado (rated EF2) was spawned southwest of Midway (Logan County). The tornado cut close to a fourteen mile path before dissipating northeast of Scranton (Logan County).||Nine other mostly weak tornadoes (eight rated EF1/one rated EF2) were confirmed across the state through the wee hours of the 11th. Two of these tornadoes were in the Little Rock County Warning Area near Seaton (Lonoke County) and Jerome (Drew County). The former tornado blew in a grain bin and tossed a shed into nearby trees. The latter tornado mangled a silo. Trees were uprooted or snapped, and utility poles were taken out.||A few places reported sleet or snow on the back side of the system. Two cars were stuck in high water on LaHarpe Blvd. near the Broadway Bridge.", "ts_dict_index": [738, 739, 740]}
+{"event_id": 873213, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2020-01-10 23:00:00", "end_date_time": "2020-01-11 02:00:00", "narrative": "The month started off with a bang on the 10th. It felt like spring in Arkansas, with high temperatures in the 60s to lower 70s. As the day began, a powerful storm system was looming to the west in New Mexico. Moisture levels were on the rise ahead of the system. It was a perfect setup for severe weather and flash flooding.||By late afternoon and into the overnight hours/early on the 11th, a massive damaging wind episode unfolded. Wind gusts from 60 to 90 mph pounded parts of the state. Trees and/or power lines were downed at Yellville (Marion County), Henderson (Baxter County), Elizabeth (Fulton County), Melbourne (Izard County), Leslie (Searcy County), a few miles west of Arkadelphia (Clark County), Malvern (Hot Spring County), Judsonia (White County), Fordyce (Dallas County), Pine Bluff (Jefferson County), Cotton Plant (Woodruff County), Monticello (Drew County), St. Charles (Arkansas County), and Watson (Desha County). Some fallen trees landed on homes. Wind recording equipment measured a 74 mph gust at Fargo (Monroe County), and a 71 mph gust at the University of Arkansas at Monticello (Drew County).||There were also isolated tornadoes. At 740 pm CST on the 10th, a tornado (rated EF2) was spawned southwest of Midway (Logan County). The tornado cut close to a fourteen mile path before dissipating northeast of Scranton (Logan County).||Nine other mostly weak tornadoes (eight rated EF1/one rated EF2) were confirmed across the state through the wee hours of the 11th. Two of these tornadoes were in the Little Rock County Warning Area near Seaton (Lonoke County) and Jerome (Drew County). The former tornado blew in a grain bin and tossed a shed into nearby trees. The latter tornado mangled a silo. Trees were uprooted or snapped, and utility poles were taken out.||A few places reported sleet or snow on the back side of the system. Correction...Highway 80 between Hon and Waldron was closed due to high water flowing over the road.", "ts_dict_index": [732, 733, 734]}
+{"event_id": 1151037, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 09:30:00", "end_date_time": "2023-12-18 18:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Major flooding of the Sunday River occurred on the 18th after an estimated 7 to 9 inches of rain and snowmelt ran off into the river. The resultant flow was estimated to be over a 0.2% recurrence interval with flows between 10 and 12 kcfs. The most severe damages were in the Sunday River resort region where a landslide caused damage to a recreational building and several roads were washout out. The flooding continued downstream to Bethel where a Route 2 bridge was flooded and access in and out of the region was cut off for days. Homes were flooded on Sunday River Road including several townhomes off Cherry Lane.  Sunday River flooded a bridge and numerous other spots on Vista Road, Roderick Road, Bear River Road, and Sunday River Road, in Newry. Several roads were deemed inaccessible including Summit Road which was completely washout out with the loss of a large metal culvert. Bear River, a tributary to Sunday River also came out of its banks, washing away multiple parked vehicles, in Newry. Multiple water rescue was conducted for occupants of vehicles in flood waters on Vista Road.", "ts_dict_index": [744, 745, 746]}
+{"event_id": 873206, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-01-11 02:27:00", "end_date_time": "2020-01-11 05:27:00", "narrative": "The month started off with a bang on the 10th. It felt like spring in Arkansas, with high temperatures in the 60s to lower 70s. As the day began, a powerful storm system was looming to the west in New Mexico. Moisture levels were on the rise ahead of the system. It was a perfect setup for severe weather and flash flooding.||By late afternoon and into the overnight hours/early on the 11th, a massive damaging wind episode unfolded. Wind gusts from 60 to 90 mph pounded parts of the state. Trees and/or power lines were downed at Yellville (Marion County), Henderson (Baxter County), Elizabeth (Fulton County), Melbourne (Izard County), Leslie (Searcy County), a few miles west of Arkadelphia (Clark County), Malvern (Hot Spring County), Judsonia (White County), Fordyce (Dallas County), Pine Bluff (Jefferson County), Cotton Plant (Woodruff County), Monticello (Drew County), St. Charles (Arkansas County), and Watson (Desha County). Some fallen trees landed on homes. Wind recording equipment measured a 74 mph gust at Fargo (Monroe County), and a 71 mph gust at the University of Arkansas at Monticello (Drew County).||There were also isolated tornadoes. At 740 pm CST on the 10th, a tornado (rated EF2) was spawned southwest of Midway (Logan County). The tornado cut close to a fourteen mile path before dissipating northeast of Scranton (Logan County).||Nine other mostly weak tornadoes (eight rated EF1/one rated EF2) were confirmed across the state through the wee hours of the 11th. Two of these tornadoes were in the Little Rock County Warning Area near Seaton (Lonoke County) and Jerome (Drew County). The former tornado blew in a grain bin and tossed a shed into nearby trees. The latter tornado mangled a silo. Trees were uprooted or snapped, and utility poles were taken out.||A few places reported sleet or snow on the back side of the system. The fire department reported ongoing water rescues in the midtown area of Little Rock due to flash flooding.", "ts_dict_index": [735, 736, 737]}
+{"event_id": 1151058, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 11:00:00", "end_date_time": "2023-12-18 16:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Heavy rain and snowmelt caused the East Branch of the Swift River in Byron to flood and washed out 2 culverts on Weld Road.", "ts_dict_index": [753, 754, 755]}
+{"event_id": 1151051, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 12:49:00", "end_date_time": "2023-12-18 14:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Bridge washed away on Milton Road after the Concord River overflowed its banks following heavy rain and snowmelt.", "ts_dict_index": [741, 742, 743]}
+{"event_id": 1151036, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 09:30:00", "end_date_time": "2023-12-18 17:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Major flooding of the Bear River between Grafton Notch and Newry with an estimated rain and snowmelt combination of 8 and 9 inches. The resultant flow is estimated over a 0.2% recurrence interval with flows between 8 and 10 kcfs. Washouts occurred on Route 26 near Horseshoe Falls in the Grafton Notch Campground area and near Poplar Road, in Newry. Wheeler Road and Branch Roads in North Newry were hard hit with severe washouts running for 2 miles.  A swift water rescue was needed at the intersection of Route 2 and Route 26 caused by flooding from the Androscoggin River and the Bear River.", "ts_dict_index": [747, 748, 749]}
+{"event_id": 1151054, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 11:30:00", "end_date_time": "2023-12-18 13:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Extreme flooding across the Bethel area resulted in swift water rescues of several motorists and residents. The Bethel Fire Department performed numerous rescues starting around 11:30 am and continued through the afternoon as flood waters cut the community off. Officials estimate at least a dozen water rescues were conducted with a few dozen people being rescued. One area were numerous rescues were occurring was Mill Brook along Lovers Lane.", "ts_dict_index": [756, 757, 758]}
+{"event_id": 1151055, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 14:20:00", "end_date_time": "2023-12-18 18:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Heavy rain and snowmelt runoff caused flooding of Otter Brook onto Interval Road near the confluence with the Androscoggin River in Hanover.  Vehicles were trapped in the flood waters with occupants needing to be rescued.", "ts_dict_index": [750, 751, 752]}
+{"event_id": 1004603, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-01-01 09:16:00", "end_date_time": "2022-01-01 11:45:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. Big Creek Fire Department is inundated with water near the community of Sidney.", "ts_dict_index": [726, 727, 728]}
+{"event_id": 1004595, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-01-01 09:10:00", "end_date_time": "2022-01-01 11:45:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. Water was reported across Long Branch Road, making it impassable, near the community of Turkey Creek.", "ts_dict_index": [729, 730, 731]}
+{"event_id": 1123699, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-07-09 17:55:00", "end_date_time": "2023-07-09 19:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. Heavy rain on the afternoon of the 9th caused several washouts along Graine Lake Road in Nelson. Murdough Hill Road also closed due to a washout.", "ts_dict_index": [693, 694, 695]}
+{"event_id": 949417, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-05-19 01:00:00", "end_date_time": "2021-05-19 04:00:00", "narrative": "A closed upper low pressure system continued to spin across New Mexico during the afternoon and evening of May 18th, ejecting a shortwave trough northeast across Northeast Texas into Southeast Oklahoma. A very moist and unstable air mass had developed during the afternoon over these areas, with the trough enhancing large scale forcing for a complex of showers and thunderstorms which shifted northeast across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas. Given the extent of instability and adequate wind shear, some of these storms became severe, producing damaging winds which downed trees and power lines across portions of Western Bowie County into Southeast McCurtain County Oklahoma. These storms weakened during the early evening, before dissipating by mid-evening. ||Another shortwave trough ejecting northeast across Central and Southeast Texas ahead of the trough promoted the development of another mesoscale convective system across these areas during the evening, which shifted east northeast across Southeast Texas and portions of East Texas. While the northern extent of this system weakened over East Texas due to a more stable air mass in place from the earlier thunderstorms which moved through the area during the afternoon, locally heavy rain did fall over already saturated grounds, with rainfall amounts of two to four inches falling over Smith, Cherokee, Western and Southern Nacogdoches, and Angelina Counties, with isolated higher amounts between five and six inches falling over Southwest Smith County near Lake Palestine. This heavy rainfall resulted in rapid runoff and flash flooding across much of these areas during the late evening through the early morning hours of May 19th. The heavy rainfall and flash flooding ended by daybreak across much of East Texas. A portion of County Road 47 north of Highway 64 was washed out.", "ts_dict_index": [774, 775, 776]}
+{"event_id": 1151050, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 08:18:00", "end_date_time": "2023-12-18 12:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Flooding on Route 232 near Gore Road from the Bakers Brook in Milton.", "ts_dict_index": [759, 760, 761]}
+{"event_id": 949419, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-05-19 01:00:00", "end_date_time": "2021-05-19 04:00:00", "narrative": "A closed upper low pressure system continued to spin across New Mexico during the afternoon and evening of May 18th, ejecting a shortwave trough northeast across Northeast Texas into Southeast Oklahoma. A very moist and unstable air mass had developed during the afternoon over these areas, with the trough enhancing large scale forcing for a complex of showers and thunderstorms which shifted northeast across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas. Given the extent of instability and adequate wind shear, some of these storms became severe, producing damaging winds which downed trees and power lines across portions of Western Bowie County into Southeast McCurtain County Oklahoma. These storms weakened during the early evening, before dissipating by mid-evening. ||Another shortwave trough ejecting northeast across Central and Southeast Texas ahead of the trough promoted the development of another mesoscale convective system across these areas during the evening, which shifted east northeast across Southeast Texas and portions of East Texas. While the northern extent of this system weakened over East Texas due to a more stable air mass in place from the earlier thunderstorms which moved through the area during the afternoon, locally heavy rain did fall over already saturated grounds, with rainfall amounts of two to four inches falling over Smith, Cherokee, Western and Southern Nacogdoches, and Angelina Counties, with isolated higher amounts between five and six inches falling over Southwest Smith County near Lake Palestine. This heavy rainfall resulted in rapid runoff and flash flooding across much of these areas during the late evening through the early morning hours of May 19th. The heavy rainfall and flash flooding ended by daybreak across much of East Texas. A portion of FM 724 was closed due to flooding.", "ts_dict_index": [777, 778, 779]}
+{"event_id": 916668, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2020-08-31 07:51:00", "end_date_time": "2020-08-31 10:51:00", "narrative": "The heat/humidity energized the environment on the 29th, and this happened as a cold front slowly approached from Missouri. Ahead of the front, strong to severe thunderstorms popped up in northern Arkansas in the afternoon. There was an estimated 60 mph wind gust just northeast of Damascus (Van Buren County) and a 70 mph gust at Alicia (Lawrence County). Trees were blown down at the latter location, and also at Lynn (Lawrence County). As storms dropped to the south toward Little Rock (Pulaski County), a building on a school campus was struck by lightning in Pulaski Heights (Pulaski County). This started a fire that damaged the roof.||Later in the evening, the focus shifted to the west. A storm near Boothe (Scott County) cranked out golf ball size hail at the intersection of Highways 23 and 71. Trees were pushed onto Highway 28 just east of Hon (Scott County) and Mena (Polk County).||Two to more than four inches of rain fell in west central Arkansas. Since this part of the state had already been pounded with deluge after deluge in August, the soil was saturated and could not hold much liquid. A flash flood event unfolded in a hurry, and it was serious. Water was over Highway 23 at Elm Park (Scott County). Several roads were under water and impassible at Mena (Polk County). At the airport just southeast of town, 2.74 inches of rain fell in an hour. People on all-terrain vehicles were stranded by high water at Wolfpen Gap Campground just west of Big Fork (Polk County). Sections of Highways 270 and 27 were flooded near Mount Ida (Montgomery County).||Early on the 31st, the sky opened again in the west. Many roads were inundated with water at Waldron (Scott County). Flooding was also experienced on Highway 298 near Story (Montgomery County), and along several thoroughfares in Hot Springs (Garland County). Many roads were underwater in Waldron and in the county.", "ts_dict_index": [771, 772, 773]}
+{"event_id": 1151057, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 11:20:00", "end_date_time": "2023-12-18 15:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Heavy rain and snowmelt caused overland flooding that caused severe damage on Lohnes Farm Road including damage to a bridge and a washed out culvert.", "ts_dict_index": [762, 763, 764]}
+{"event_id": 916586, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2020-08-29 18:30:00", "end_date_time": "2020-08-29 21:30:00", "narrative": "The heat/humidity energized the environment on the 29th, and this happened as a cold front slowly approached from Missouri. Ahead of the front, strong to severe thunderstorms popped up in northern Arkansas in the afternoon. There was an estimated 60 mph wind gust just northeast of Damascus (Van Buren County) and a 70 mph gust at Alicia (Lawrence County). Trees were blown down at the latter location, and also at Lynn (Lawrence County). As storms dropped to the south toward Little Rock (Pulaski County), a building on a school campus was struck by lightning in Pulaski Heights (Pulaski County). This started a fire that damaged the roof.||Later in the evening, the focus shifted to the west. A storm near Boothe (Scott County) cranked out golf ball size hail at the intersection of Highways 23 and 71. Trees were pushed onto Highway 28 just east of Hon (Scott County) and Mena (Polk County).||Two to more than four inches of rain fell in west central Arkansas. Since this part of the state had already been pounded with deluge after deluge in August, the soil was saturated and could not hold much liquid. A flash flood event unfolded in a hurry, and it was serious. Water was over Highway 23 at Elm Park (Scott County). Several roads were under water and impassible at Mena (Polk County). At the airport just southeast of town, 2.74 inches of rain fell in an hour. People on all-terrain vehicles were stranded by high water at Wolfpen Gap Campground just west of Big Fork (Polk County). Sections of Highways 270 and 27 were flooded near Mount Ida (Montgomery County).||Early on the 31st, the sky opened again in the west. Many roads were inundated with water at Waldron (Scott County). Flooding was also experienced on Highway 298 near Story (Montgomery County), and along several thoroughfares in Hot Springs (Garland County). Scott County Sheriff office reported high water over Highway 23.", "ts_dict_index": [768, 769, 770]}
+{"event_id": 1151034, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 08:00:00", "end_date_time": "2023-12-19 00:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Major flooding occurred on the Wild River in Gilead with the USGS river gage marked the 2nd highest crest on record of 16.4 feet. The gage was established in 1960 and the only flood of higher flows was that following Irene in 2011. The streamflow was near 34 kcfs, which falls between a 0.5 and 0.2% annual chance exceedance level, otherwise referred to as a 200 to 500 year flood. The flooding was the result of 5 to 6 inches of rainfall and 3 to 4 inches of snowmelt running off within an 18-hour timeframe. The steep slopes of the Wild River combined with frozen ground resulted in a fast rise of 13 feet in 12 hours. The fast-moving water overtook Route 113 and washed out a 80-foot section. The flows from the Wild River contributed to the Androscoggin River major flooding in downstream Bethel.", "ts_dict_index": [765, 766, 767]}
+{"event_id": 1005248, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-01-01 09:00:00", "end_date_time": "2022-01-01 11:45:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. KY-319 in the community of Toler is impassable due to flood waters.", "ts_dict_index": [717, 718, 719]}
+{"event_id": 1064020, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2023-01-02 16:45:00", "end_date_time": "2023-01-03 03:00:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of Southwest Arkansas, with isolated higher totals in excess of 4-5+ inches observed especially over Southern Lafayette, much of Columbia and Union Counties. This resulted in areas of flash flooding across portions of Southern Arkansas from the afternoon through the early morning hours on the 3rd, with a brief tornado also spawning across Central Union County north of El Dorado. Highway 53 over Walker Creek was closed due to flooding.", "ts_dict_index": [786, 787, 788]}
+{"event_id": 1064214, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-01-02 22:06:00", "end_date_time": "2023-01-03 00:15:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. Four vehicles were stranded in high water at various locations throughout the city of Shreveport.", "ts_dict_index": [780, 781, 782]}
+{"event_id": 1064027, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2023-01-02 23:25:00", "end_date_time": "2023-01-03 02:30:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of Southwest Arkansas, with isolated higher totals in excess of 4-5+ inches observed especially over Southern Lafayette, much of Columbia and Union Counties. This resulted in areas of flash flooding across portions of Southern Arkansas from the afternoon through the early morning hours on the 3rd, with a brief tornado also spawning across Central Union County north of El Dorado. Water entered a home in Smackover. High water covered several roads in town as well.", "ts_dict_index": [789, 790, 791]}
+{"event_id": 1064024, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2023-01-02 21:00:00", "end_date_time": "2023-01-03 02:00:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of Southwest Arkansas, with isolated higher totals in excess of 4-5+ inches observed especially over Southern Lafayette, much of Columbia and Union Counties. This resulted in areas of flash flooding across portions of Southern Arkansas from the afternoon through the early morning hours on the 3rd, with a brief tornado also spawning across Central Union County north of El Dorado. High water covered the intersection of 19th Street and Tanglewood Drive.", "ts_dict_index": [792, 793, 794]}
+{"event_id": 1005584, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-01-01 10:55:00", "end_date_time": "2022-01-01 11:45:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. Water was reported to be up to the building of Sidney Missionary Baptist Church.", "ts_dict_index": [723, 724, 725]}
+{"event_id": 1064026, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2023-01-02 21:00:00", "end_date_time": "2023-01-03 02:00:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of Southwest Arkansas, with isolated higher totals in excess of 4-5+ inches observed especially over Southern Lafayette, much of Columbia and Union Counties. This resulted in areas of flash flooding across portions of Southern Arkansas from the afternoon through the early morning hours on the 3rd, with a brief tornado also spawning across Central Union County north of El Dorado. Several roads were flooded and closed in El Dorado.", "ts_dict_index": [795, 796, 797]}
+{"event_id": 1061209, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 19:00:00", "end_date_time": "2022-10-16 03:00:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A Maricopa County Flood Control District Streamflow Gauge along Rainbow Wash reported flow rising to above alarm stage (1.4 feet) between 17:21 and 17:25 MST, exceeding the bankfull stage (4.1 feet) between 18:17 and 18:27 MST and peaking at 4.42 feet (2368 cfs) at around 18:55 MST. Any flooding impacts from the wash included Old US-80 and Patterson Road, located about 5.6 miles downstream. The wash went below bankfull stage at around 19:31 MST, before another rise above the bankfull stage occurred at around 23:02 MST. The flow did not go below action stage until around 00:47 MST on the 16th.", "ts_dict_index": [810, 811, 812]}
+{"event_id": 1061364, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 18:46:00", "end_date_time": "2022-10-15 22:46:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. Pictures were sent in from a trained spotter of water entering the Adelante Healthcare facility and some of the downtown stores in Buckeye. Water was estimated to be 6 to 8 inches deep. No injuries were reported.", "ts_dict_index": [804, 805, 806]}
+{"event_id": 1061338, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 23:30:00", "end_date_time": "2022-10-16 15:00:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A Maricopa County Flood Control District Streamflow Gauge along Centennial Wash at the Union Pacific Railroad showed flow going above alarm stage (8.5 feet) between 21:53 and 21:56 MST and continuing to rise for several hours more to reach a peak flow of 13 feet (4315 cfs) at 02:06 MST on the 16th. Flooding along the wash likely occurred along the Old US Highway 80, located 6 miles downstream. Flow fell below alarm stage at 13:34 MST on the 16th. No damages or injuries were reported.", "ts_dict_index": [798, 799, 800]}
+{"event_id": 1061579, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2022-10-16 12:30:00", "end_date_time": "2022-10-16 15:30:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A video showed flooding occurring from Bloody Tanks. Water was reaching the bottom of a bridge as well as going around it, briefly trapping the person recording the incident. The location of the incident was in the area of Schulze Ranch Road and U.S. 60. Timing estimated from radar. No damages or injuries were reported.", "ts_dict_index": [819, 820, 821]}
+{"event_id": 1061573, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-16 02:40:00", "end_date_time": "2022-10-16 04:40:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A Maricopa County Flood Control District Streamflow Gauge along East Fork Cave Creek near 7th Avenue showed the flow going above alarm stage (2 feet) at around 2:36 MST, peaking at 3.33 feet (1239 cfs) at 3:05 MST, and dropped below alarm stage between 4:01 and 4:36 MST. Flooding likely occurred at the low water crossing along 7th Avenue. No damages or injuries were reported.", "ts_dict_index": [816, 817, 818]}
+{"event_id": 1061367, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 18:00:00", "end_date_time": "2022-10-15 22:00:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. Social media report showed slow traffic on SR-238, between mile markers 23 to 40 due to flooding on roadway. Timing estimated from radar. No damages or injuries were reported.", "ts_dict_index": [834, 835, 836]}
+{"event_id": 1061335, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 21:00:00", "end_date_time": "2022-10-16 09:00:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A Maricopa County Flood Control District Streamflow Gauge along Waterman Wash at Rainbow Valley Road showed flow going above alarm stage (3.3 feet) between 19:28 and 20:07 MST and continuing to rise for several hours more to reach a peak flow of 7.25 feet (1700 cfs) at 23:38 MST. Flooding along the wash likely occurred along Tuthill Road, located 3.2 miles downstream and Narramore Road, located 6.4 miles downstream. Flow fell below alarm stage at 07:03 MST on the 16th. A truck was swept off Narramore Road due to the strong current from the wash. There was no information received about the occupants that were inside the truck.", "ts_dict_index": [828, 829, 830]}
+{"event_id": 1061208, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 14:09:00", "end_date_time": "2022-10-15 15:09:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. Flooding reported on I-17 near Bell Road in Phoenix. No damages or injuries were reported.", "ts_dict_index": [831, 832, 833]}
+{"event_id": 1064213, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-01-02 22:00:00", "end_date_time": "2023-01-03 00:15:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. Cars were stranded in high water at the intersection of Hollywood Ave. and Kennedy Drive near the Shreveport Regional Airport.", "ts_dict_index": [783, 784, 785]}
+{"event_id": 1141477, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 14:30:00", "end_date_time": "2023-09-01 19:00:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Walters Camp Rd was closed due to flooding between Hwy-78 and the Colorado River. Sentinel2 before and after satellite imagery showed evidence of considerable flow within Milpitas Wash, which Walters Camp Rd parallels and cuts across. No damages or injuries were reported. Timing estimated from radar.", "ts_dict_index": [861, 862, 863]}
+{"event_id": 1141174, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 14:00:00", "end_date_time": "2023-09-01 18:30:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. A couple rounds of heavy rain resulted in considerable flooding and the closure of Hwy-98 between S2 and Brockman Rd. Along Hwy-98, 2 vehicles became stuck in a flooded wash, with one occupant having to climb out onto their roof. No injuries were reported and the extent of damage to the vehicles is unknown. Timing was adjusted based on radar.", "ts_dict_index": [873, 874, 875]}
+{"event_id": 1141179, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 14:20:00", "end_date_time": "2023-09-01 16:20:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Old Hwy 111 was closed due to flooding between Aten Rd and Evan Hughes Rd. No damages or injuries were reported. Timing estimated from radar.", "ts_dict_index": [855, 856, 857]}
+{"event_id": 1141046, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 14:20:00", "end_date_time": "2023-09-01 18:30:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Hwy-78 was closed between the Imperial and Riverside County line and Ogilby Rd due to many flooded washes. Many vehicles were stopped along the highway due to impassable flooded washes. Hwy-78 did not fully reopen until the morning of September 3rd due to debris cleanup. No injuries or damages were reported.", "ts_dict_index": [870, 871, 872]}
+{"event_id": 1061365, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 19:07:00", "end_date_time": "2022-10-15 23:00:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. Social media videos showed water entering homes from backyards being flooded in the area of roadway MC 85 and East Baseline Road. No injuries were reported.", "ts_dict_index": [840, 841, 842]}
+{"event_id": 1141009, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 13:38:00", "end_date_time": "2023-09-01 17:30:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. California Highway Patrol incident reports indicated there were vehicles stuck in and/or in between flooded washes on Black Mountain Rd. No injuries or damages were reported.", "ts_dict_index": [876, 877, 878]}
+{"event_id": 1141176, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 15:00:00", "end_date_time": "2023-09-01 19:00:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Westmorland Rd where it becomes Boley Rd was closed due to flooding. A bridge in the area was reportedly overtopped by water. The nearby West Main canal also experienced some washouts due to a large influx of water, per Imperial Irrigation District. No damages or injuries were reported.", "ts_dict_index": [858, 859, 860]}
+{"event_id": 1141053, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2023-09-01 16:00:00", "end_date_time": "2023-09-01 20:00:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Hwy-111 was closed between the county line and North Shore due to several instances of flooded washes along the highway. No injuries or damages were reported.", "ts_dict_index": [867, 868, 869]}
+{"event_id": 1141476, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 15:30:00", "end_date_time": "2023-09-01 19:00:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Coachella Canal Rd, a dirt road, was closed between approximately Siphon 17 and Siphon 7 of the Coachella Canal due to flooding. No damages or injuries were reported. Timing estimated from radar.", "ts_dict_index": [882, 883, 884]}
+{"event_id": 1141035, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2023-09-01 14:11:00", "end_date_time": "2023-09-01 17:30:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. A California Highway Patrol incident report said there were 5 vehicles stuck in flooded washes on Hwy-177. Some of the occupants may have had to be rescued and there was a call to close the highway. No injuries were reported and specifics on vehicle damage was not shared.", "ts_dict_index": [879, 880, 881]}
+{"event_id": 1015873, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-04-13 14:35:00", "end_date_time": "2022-04-13 17:35:00", "narrative": "A strong storm system brought multiple rounds of severe weather that led to fairly widespread rainfall and eventually river flooding. One round of severe weather occurred on Monday, April 11th. Large, individual thunderstorms known as supercells developed along the Arkansas River valley of western Arkansas. As these storms slowly drifted east, they produced four tornadoes across Sebastian, Franklin and Logan Counties and hail as large as 4.5 in diameter across Logan County. Later in the evening, storms began to develop across central Arkansas and move generally eastward. Two storms caused the most widespread severe weather across central into eastern Arkansas during the evening hours of the 11th. The main storm of interest developed across Perry and Faulkner Counties and moved east southeastward toward Lonoke County. As this storm intensified it produced a tornado as well as 3 hail near Cabot. The other main storm developed over portions of Garland County and moved east across Saline County. Before weakening, it produced a swath of hail as large as golf balls from Hot Springs Village to Bryant. ||Ahead of a cold front that moved across the state on the 13th, additional rain and thunderstorms developed and moved across the state. Fairly widespread rain, some of which was heavy and led to flash flooding, and thunderstorms shifted east across the area on the 13th. A swath of heavy rain in excess of 2-4 inches occurred from portions of southwest to east central Arkansas as well as across northwest sections of the state. Sadly, one person died after a tree fell on a mobile home in Cleveland County on April 13th. On the same day, flash flooding claimed the life of a 70 year old woman in Carroll County when she attempted to cross a flooded low water crossing. A report was received via mPING of a car stalled in water on Hwy. 70 near East Washington Rd.", "ts_dict_index": [852, 853, 854]}
+{"event_id": 1061293, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 18:45:00", "end_date_time": "2022-10-16 04:00:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A Maricopa County Flood Control District Streamflow Gauge along Winters Wash in Tonopah showed flow going above alarm stage (1.28 feet) between 18:06 and 18:08 MST, with the flow going above the bankfull stage (3.32 feet) at 18:38 MST and peaking at 4.27 feet (1400 cfs) at 19:18 MST. The flow went below bankfull at 22:49 MST and below alarm stage at 01:43 MST on the 16th. Roads intersecting the wash that were affected from the flow along Winters Wash included Indian School Road, located 1.1 miles downstream of the gauge, and along Salome Highway south of I-10 located 4.6 miles downstream of the gauge. Along Indian School Road, there were reports at around 19:37 MST from a trained spotter of many cars stranded and it is unknown whether or not any of the vehicles sustained damage. No injuries were reported.", "ts_dict_index": [846, 847, 848]}
+{"event_id": 1015876, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-04-13 14:35:00", "end_date_time": "2022-04-13 17:35:00", "narrative": "A strong storm system brought multiple rounds of severe weather that led to fairly widespread rainfall and eventually river flooding. One round of severe weather occurred on Monday, April 11th. Large, individual thunderstorms known as supercells developed along the Arkansas River valley of western Arkansas. As these storms slowly drifted east, they produced four tornadoes across Sebastian, Franklin and Logan Counties and hail as large as 4.5 in diameter across Logan County. Later in the evening, storms began to develop across central Arkansas and move generally eastward. Two storms caused the most widespread severe weather across central into eastern Arkansas during the evening hours of the 11th. The main storm of interest developed across Perry and Faulkner Counties and moved east southeastward toward Lonoke County. As this storm intensified it produced a tornado as well as 3 hail near Cabot. The other main storm developed over portions of Garland County and moved east across Saline County. Before weakening, it produced a swath of hail as large as golf balls from Hot Springs Village to Bryant. ||Ahead of a cold front that moved across the state on the 13th, additional rain and thunderstorms developed and moved across the state. Fairly widespread rain, some of which was heavy and led to flash flooding, and thunderstorms shifted east across the area on the 13th. A swath of heavy rain in excess of 2-4 inches occurred from portions of southwest to east central Arkansas as well as across northwest sections of the state. Sadly, one person died after a tree fell on a mobile home in Cleveland County on April 13th. On the same day, flash flooding claimed the life of a 70 year old woman in Carroll County when she attempted to cross a flooded low water crossing. Broadcast media tweeted a photo of deep water running over a road in Alexander.", "ts_dict_index": [849, 850, 851]}
+{"event_id": 1141178, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 13:40:00", "end_date_time": "2023-09-01 16:40:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Evan Hughes Hwy was closed due to considerable flooding between S2 and Dunaway Rd. No damages or injuries were reported. Timing estimated from radar.", "ts_dict_index": [885, 886, 887]}
+{"event_id": 1061337, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 21:10:00", "end_date_time": "2022-10-15 22:30:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A Maricopa County Flood Control District Streamflow Gauge along Cruff Wash showed flow going above alarm stage (2.5 feet) between 20:29 and 20:31 MST, reaching a peak flow of 3.25 feet (448 cfs) at 21:13 MST. Flooding along the wash likely occurred at Agua Caliente Road, located about 2 miles downstream. Flow fell below alarm stage between 21:42 and 21:48 MST. No damages or injuries were reported.", "ts_dict_index": [843, 844, 845]}
+{"event_id": 1061339, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 23:30:00", "end_date_time": "2022-10-16 06:30:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A Maricopa County Flood Control District Streamflow Gauge along Delaney Wash showed flow going above alarm stage (1.87 feet) between 22:51 and 22:53 MST, with a peak flow of 2.3 feet (255 cfs) at 23:07 MST. Flooding along the wash likely occurred along 411th Avenue, located 2.1 miles downstream and Salome Highway, located 3.7 miles downstream. Flow fell below alarm stage between 5:05 and 5:51 MST on the 16th. No damages or injuries were reported.", "ts_dict_index": [813, 814, 815]}
+{"event_id": 1140231, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 12:51:00", "end_date_time": "2023-09-01 13:30:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. An incident report from California Highway Patrol said that multiple vehicles were stopped due to flooding on Highway 78. No injuries or damages were reported.", "ts_dict_index": [888, 889, 890]}
+{"event_id": 1141050, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2023-09-01 15:33:00", "end_date_time": "2023-09-01 19:00:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Incident report from California Highway Patrol of a compromised bridge along Hwy-111 near Mecca Ave being washed out due to flooding. Also a report of a trapped party along Club View Dr. In this same area there was also a report of 2-3 vehicles being taken out by flash flooding.  Additional flooding led to Hwy-111 being closed down to the Imperial county line. No injuries or damages were reported.", "ts_dict_index": [894, 895, 896]}
+{"event_id": 1141024, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 13:57:00", "end_date_time": "2023-09-01 17:00:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. A sedan was swept off Dunaway Rd, just south of Evan Hughes Hwy, due to a flooded wash. A photo shows a man in more than waist-deep water trying to push the floating sedan. First responders had a difficult time getting to the scene due to flooding. Dunaway Rd was also closed between Evan Hughes Hwy and I-8. No injuries were reported. Damage cost based on car value.", "ts_dict_index": [891, 892, 893]}
+{"event_id": 1141005, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 13:36:00", "end_date_time": "2023-09-01 17:30:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Report for California Highway Patrol of an unknown number of vehicles stuck on Hwy-78 due to flooding. No injuries or damages reported.", "ts_dict_index": [897, 898, 899]}
+{"event_id": 1141478, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 14:05:00", "end_date_time": "2023-09-01 17:00:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Wheeler Rd was closed due to flooding between Imler Rd and Huff Rd. No damages or injuries were reported. Timing estimated from radar.", "ts_dict_index": [900, 901, 902]}
+{"event_id": 1141177, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 16:10:00", "end_date_time": "2023-09-01 19:30:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Forrester Rd, near Larsen Rd, was closed due to flooding. No damages or injuries were reported. Timing estimated from radar.", "ts_dict_index": [912, 913, 914]}
+{"event_id": 1141175, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 14:50:00", "end_date_time": "2023-09-01 19:00:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Blair Rd at Schrimpf Rd was closed due to flooding. Schrimpf Rd and Weist Rd were also closed around their intersection. No injuries or damages were reported. Time based on radar.", "ts_dict_index": [906, 907, 908]}
+{"event_id": 1131964, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-08-20 12:09:00", "end_date_time": "2023-08-20 14:09:00", "narrative": "Tropical Storm Hilary brought abundant moisture along with strong winds to southern California on the 20th. In fact, Tropical Storm Warnings were issued for the first time in history along the southern California coast. On the 19th, a trough near the southern California coast promoted deep southerly flow that allowed deeper moisture to advect into the Southwest ahead of Hilary. Combined with jet dynamics, showers and thunderstorms developed during the early morning hours on the 19th, leading to an isolated instance of flash flooding in southeast California. Going into the 20th, very anomalous moisture accompanied Hilary with PWATs across southeast California climbing upwards of 2-2.5 and IVT values in excess of 15 normalized standard deviations from average. Thus, flash flooding was the primary impact across southern California with a very rare high risk of excessive rainfall being issued by WPC for part of the area. Rainfall totals across southeast California were as high as 2-3, while most areas across Imperial County and eastern Riverside County generally measured around 1.50 or less. However, much heavier rainfall amounts were observed closer to the southern California coast. In addition to flash flooding impacts, several instances of damaging winds occurred as strong low level winds upwards of 50-60 knots at 850 mb and 925 mb mixed to the surface in some cases. Several communities around the Salton Sea were under a voluntary evacuation order as a precaution for any potential impacts stemming from flash flooding and strong winds. Multiple reports of flooding impacts and wind damage primarily across Imperial County resulted from this event. No injuries were reported. Flash flooding was reported in Salton City along Seaview Drive, which has a low water crossing through a wash. According to local media reports, a mother and her two children had to be rescued after their vehicle became stuck in a wash. No injuries were reported.", "ts_dict_index": [927, 928, 929]}
+{"event_id": 1140906, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 13:07:00", "end_date_time": "2023-09-01 18:30:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Ogilby Road, a flood-prone road, was closed between I-8 and Hwy-78 due to flooding. A later report said there were chunks of road washed out. A photo shared by Caltrans on September 2nd showed water still flowing over the road and a construction vehicle cleaning up large amounts of debris on the roadway.  No injuries or specific magnitude of damages were reported.", "ts_dict_index": [909, 910, 911]}
+{"event_id": 1141473, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-09-01 14:40:00", "end_date_time": "2023-09-01 19:40:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. Widespread 1 to 2 inches of radar estimated rain fell in Niland and areas just east into the Chocolate Mountains. A large area of considerable runoff flowed through Niland and the surrounding area, as evident in reports and before and after Sentinel2 satellite images, with upwards of 6 inches to 1 foot of flowing water in some areas, per photos and videos. Major flash flooding impacts were experienced. The East Highline Canal east of Niland, was overcome with flood waters and silt, mainly north of of Flowing Wells Rd. The overflowing canal was first reported a little after 1600PDT and only exacerbated the flooding. Several roads became impassable, unsafe, and subsequently closed due to flood water. At least a few cars became stuck in flood water leading to swift water rescues by land and air. The exact number of rescues is unknown. In Niland, several photos and videos showed flooded streets and yards, with water coming up to homes and businesses. There were a few reports of water entering homes, but it is unknown how many homes were impacted. Also impacted in the area was agriculture, as several fields had flood water moving through them. It is unknown the extent of any damages to the agricultural fields or the exact number. Sentinel2 satellite images showed evidence of all the disturbed earth, deposited mud and silt, through Niland, the agricultural fields and surrounding areas. In a statement by Imperial Irrigation District, the impacts to East Highline Canal resulted in a delay of 133 water deliveries. Also the O Lateral canal, which branches from East Highline canal, suffered structural damage. The main highway through the area, Hwy-111, was flooded in several locations, which hampered relief efforts. The small town of Slab City, to the northeast of Niland, was cut off from the rest of the Imperial Valley due to the flooded roads. As a result of the significant impacts, the County of Imperial issued an emergency proclamation for additional and better resources. Red Cross assisted in relief and a couple shelters for evacuees were established. There were no injuries reported from this event and specifics on property and crop damage is unknown and thus grossly estimated.", "ts_dict_index": [903, 904, 905]}
+{"event_id": 1132013, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-08-20 12:15:00", "end_date_time": "2023-08-20 14:15:00", "narrative": "Tropical Storm Hilary brought abundant moisture along with strong winds to southern California on the 20th. In fact, Tropical Storm Warnings were issued for the first time in history along the southern California coast. On the 19th, a trough near the southern California coast promoted deep southerly flow that allowed deeper moisture to advect into the Southwest ahead of Hilary. Combined with jet dynamics, showers and thunderstorms developed during the early morning hours on the 19th, leading to an isolated instance of flash flooding in southeast California. Going into the 20th, very anomalous moisture accompanied Hilary with PWATs across southeast California climbing upwards of 2-2.5 and IVT values in excess of 15 normalized standard deviations from average. Thus, flash flooding was the primary impact across southern California with a very rare high risk of excessive rainfall being issued by WPC for part of the area. Rainfall totals across southeast California were as high as 2-3, while most areas across Imperial County and eastern Riverside County generally measured around 1.50 or less. However, much heavier rainfall amounts were observed closer to the southern California coast. In addition to flash flooding impacts, several instances of damaging winds occurred as strong low level winds upwards of 50-60 knots at 850 mb and 925 mb mixed to the surface in some cases. Several communities around the Salton Sea were under a voluntary evacuation order as a precaution for any potential impacts stemming from flash flooding and strong winds. Multiple reports of flooding impacts and wind damage primarily across Imperial County resulted from this event. No injuries were reported. A social media video showed that a low water crossing along Marina Drive in Salton City was impassable due to flooding. No injuries were reported.", "ts_dict_index": [930, 931, 932]}
+{"event_id": 1132512, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-08-19 05:30:00", "end_date_time": "2023-08-19 07:30:00", "narrative": "Tropical Storm Hilary brought abundant moisture along with strong winds to southern California on the 20th. In fact, Tropical Storm Warnings were issued for the first time in history along the southern California coast. On the 19th, a trough near the southern California coast promoted deep southerly flow that allowed deeper moisture to advect into the Southwest ahead of Hilary. Combined with jet dynamics, showers and thunderstorms developed during the early morning hours on the 19th, leading to an isolated instance of flash flooding in southeast California. Going into the 20th, very anomalous moisture accompanied Hilary with PWATs across southeast California climbing upwards of 2-2.5 and IVT values in excess of 15 normalized standard deviations from average. Thus, flash flooding was the primary impact across southern California with a very rare high risk of excessive rainfall being issued by WPC for part of the area. Rainfall totals across southeast California were as high as 2-3, while most areas across Imperial County and eastern Riverside County generally measured around 1.50 or less. However, much heavier rainfall amounts were observed closer to the southern California coast. In addition to flash flooding impacts, several instances of damaging winds occurred as strong low level winds upwards of 50-60 knots at 850 mb and 925 mb mixed to the surface in some cases. Several communities around the Salton Sea were under a voluntary evacuation order as a precaution for any potential impacts stemming from flash flooding and strong winds. Multiple reports of flooding impacts and wind damage primarily across Imperial County resulted from this event. No injuries were reported. According to Caltrans, Highway 98 near Ocotillo was closed due to flash flooding. No injuries were reported.", "ts_dict_index": [933, 934, 935]}
+{"event_id": 920104, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2020-09-01 09:45:00", "end_date_time": "2020-09-01 12:45:00", "narrative": "On the 1st, several inches of rain dumped from Mena (Polk County) and Waldron (Scott County) to Russellville (Pope County), and Mountain View (Stone County).||The ground was already saturated in parts of the west after more than a foot of precipitation in August. Water had nowhere to go, and flooding became life threatening. At Waldron (Scott County), numerous roads were under water (including Highways 28 and 71), and this was spilling into homes and businesses. Local residents had to be rescued. Major flooding occurred along the Petit Jean River at Danville (Yell County), with a Top 10 highest crest by the 2nd.||County roads were flooded near the Petit Jean River at Booneville (Logan County). More county roads were inundated with water at Dardanelle (Yell County), and parts of Highways 27 and 28 were affected. An overflowing creek closed Highway 28 around Bluffton (Yell County). County roads were washed out near Hanover (Stone County). Highway 115 was flooded and shut down near Jessup (Lawrence County).||One storm produced three tornadoes from central into northeast sections of the state (Conway, Faulkner, and Cleburne Counties). The strongest of the tornadoes (rated EF2) cut a 5.3 mile swath through areas just south and southeast of Heber Springs (Cleburne County) between 300 pm and 330 pm CDT on the 1st. Tree damage was extensive, with numerous trees snapped four to five miles southeast of town. Some trees were on a home, and a few outbuildings were damaged.||The other two tornadoes (rated EF0/EF1) tracked just north of Plumerville and Menifee (both in Conway County), and northwest of Wooster and Greenbrier (both in Faulkner County). More trees were uprooted, and there was some minor structural damage. A water rescue was reported along Hwy. 248 West in Scott County.", "ts_dict_index": [921, 922, 923]}
+{"event_id": 920010, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2020-09-01 03:00:00", "end_date_time": "2020-09-01 06:00:00", "narrative": "On the 1st, several inches of rain dumped from Mena (Polk County) and Waldron (Scott County) to Russellville (Pope County), and Mountain View (Stone County).||The ground was already saturated in parts of the west after more than a foot of precipitation in August. Water had nowhere to go, and flooding became life threatening. At Waldron (Scott County), numerous roads were under water (including Highways 28 and 71), and this was spilling into homes and businesses. Local residents had to be rescued. Major flooding occurred along the Petit Jean River at Danville (Yell County), with a Top 10 highest crest by the 2nd.||County roads were flooded near the Petit Jean River at Booneville (Logan County). More county roads were inundated with water at Dardanelle (Yell County), and parts of Highways 27 and 28 were affected. An overflowing creek closed Highway 28 around Bluffton (Yell County). County roads were washed out near Hanover (Stone County). Highway 115 was flooded and shut down near Jessup (Lawrence County).||One storm produced three tornadoes from central into northeast sections of the state (Conway, Faulkner, and Cleburne Counties). The strongest of the tornadoes (rated EF2) cut a 5.3 mile swath through areas just south and southeast of Heber Springs (Cleburne County) between 300 pm and 330 pm CDT on the 1st. Tree damage was extensive, with numerous trees snapped four to five miles southeast of town. Some trees were on a home, and a few outbuildings were damaged.||The other two tornadoes (rated EF0/EF1) tracked just north of Plumerville and Menifee (both in Conway County), and northwest of Wooster and Greenbrier (both in Faulkner County). More trees were uprooted, and there was some minor structural damage. The Scott County sheriff's office reported several roads in Waldron were closed due to high water.", "ts_dict_index": [924, 925, 926]}
+{"event_id": 920105, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2020-09-01 11:50:00", "end_date_time": "2020-09-01 14:50:00", "narrative": "On the 1st, several inches of rain dumped from Mena (Polk County) and Waldron (Scott County) to Russellville (Pope County), and Mountain View (Stone County).||The ground was already saturated in parts of the west after more than a foot of precipitation in August. Water had nowhere to go, and flooding became life threatening. At Waldron (Scott County), numerous roads were under water (including Highways 28 and 71), and this was spilling into homes and businesses. Local residents had to be rescued. Major flooding occurred along the Petit Jean River at Danville (Yell County), with a Top 10 highest crest by the 2nd.||County roads were flooded near the Petit Jean River at Booneville (Logan County). More county roads were inundated with water at Dardanelle (Yell County), and parts of Highways 27 and 28 were affected. An overflowing creek closed Highway 28 around Bluffton (Yell County). County roads were washed out near Hanover (Stone County). Highway 115 was flooded and shut down near Jessup (Lawrence County).||One storm produced three tornadoes from central into northeast sections of the state (Conway, Faulkner, and Cleburne Counties). The strongest of the tornadoes (rated EF2) cut a 5.3 mile swath through areas just south and southeast of Heber Springs (Cleburne County) between 300 pm and 330 pm CDT on the 1st. Tree damage was extensive, with numerous trees snapped four to five miles southeast of town. Some trees were on a home, and a few outbuildings were damaged.||The other two tornadoes (rated EF0/EF1) tracked just north of Plumerville and Menifee (both in Conway County), and northwest of Wooster and Greenbrier (both in Faulkner County). More trees were uprooted, and there was some minor structural damage. Widespread flooding and multiple water rescues were reported across the county and water was getting into homes and buildings in some locations.", "ts_dict_index": [915, 916, 917]}
+{"event_id": 920038, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2020-09-01 07:30:00", "end_date_time": "2020-09-01 10:30:00", "narrative": "On the 1st, several inches of rain dumped from Mena (Polk County) and Waldron (Scott County) to Russellville (Pope County), and Mountain View (Stone County).||The ground was already saturated in parts of the west after more than a foot of precipitation in August. Water had nowhere to go, and flooding became life threatening. At Waldron (Scott County), numerous roads were under water (including Highways 28 and 71), and this was spilling into homes and businesses. Local residents had to be rescued. Major flooding occurred along the Petit Jean River at Danville (Yell County), with a Top 10 highest crest by the 2nd.||County roads were flooded near the Petit Jean River at Booneville (Logan County). More county roads were inundated with water at Dardanelle (Yell County), and parts of Highways 27 and 28 were affected. An overflowing creek closed Highway 28 around Bluffton (Yell County). County roads were washed out near Hanover (Stone County). Highway 115 was flooded and shut down near Jessup (Lawrence County).||One storm produced three tornadoes from central into northeast sections of the state (Conway, Faulkner, and Cleburne Counties). The strongest of the tornadoes (rated EF2) cut a 5.3 mile swath through areas just south and southeast of Heber Springs (Cleburne County) between 300 pm and 330 pm CDT on the 1st. Tree damage was extensive, with numerous trees snapped four to five miles southeast of town. Some trees were on a home, and a few outbuildings were damaged.||The other two tornadoes (rated EF0/EF1) tracked just north of Plumerville and Menifee (both in Conway County), and northwest of Wooster and Greenbrier (both in Faulkner County). More trees were uprooted, and there was some minor structural damage. Many bridges and roads, including Hwy. 28 and 71, across Scott County are underwater and/or washed out.", "ts_dict_index": [918, 919, 920]}
+{"event_id": 1061108, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 18:00:00", "end_date_time": "2022-10-15 19:00:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A Maricopa County Flood Control District Streamflow Gauge located along Tiger Wash reported water levels along the wash going above alarm stage (5.9 feet) at 16:48 MST, with water levels peaking at 6.06 feet (587 cfs) at 16:57 MST. Flow went below alarm stage at 17:17 MST. Flooding from the wash would have occurred 3.5 miles downstream along Eagle Eye Road 65 minutes later, at around 18:00 MST. No damages or injuries were reported.", "ts_dict_index": [837, 838, 839]}
+{"event_id": 1131747, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-08-20 12:28:00", "end_date_time": "2023-08-20 14:28:00", "narrative": "Tropical Storm Hilary brought abundant moisture along with strong winds to southern California on the 20th. In fact, Tropical Storm Warnings were issued for the first time in history along the southern California coast. On the 19th, a trough near the southern California coast promoted deep southerly flow that allowed deeper moisture to advect into the Southwest ahead of Hilary. Combined with jet dynamics, showers and thunderstorms developed during the early morning hours on the 19th, leading to an isolated instance of flash flooding in southeast California. Going into the 20th, very anomalous moisture accompanied Hilary with PWATs across southeast California climbing upwards of 2-2.5 and IVT values in excess of 15 normalized standard deviations from average. Thus, flash flooding was the primary impact across southern California with a very rare high risk of excessive rainfall being issued by WPC for part of the area. Rainfall totals across southeast California were as high as 2-3, while most areas across Imperial County and eastern Riverside County generally measured around 1.50 or less. However, much heavier rainfall amounts were observed closer to the southern California coast. In addition to flash flooding impacts, several instances of damaging winds occurred as strong low level winds upwards of 50-60 knots at 850 mb and 925 mb mixed to the surface in some cases. Several communities around the Salton Sea were under a voluntary evacuation order as a precaution for any potential impacts stemming from flash flooding and strong winds. Multiple reports of flooding impacts and wind damage primarily across Imperial County resulted from this event. No injuries were reported. Multiple unbridged areas along SR 111 between Niland and North Shore were impacted due to flash flooding. Flash flooding impacts spanned along this highway in Imperial and Riverside Counties. According to local media, there were at least 10 reports of vehicles that became stuck along the highway and needed assistance from Imperial County Fire Department. No injuries were reported.", "ts_dict_index": [939, 940, 941]}
+{"event_id": 1140907, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2023-09-01 13:20:00", "end_date_time": "2023-09-01 18:30:00", "narrative": "A deep southerly fetch of rich moisture up from the Gulf of California led to scattered to widespread heavy rainfall in Imperial and eastern Riverside counties during the afternoon of the 1st. Moisture values were well above normal for the time of year with precipitable water values analyzed around 2.0-2.2 inches. A Flash Flood Watch was issued for much of the region. Favorable dynamic and orographic forcing helped lead to strong updrafts and training of storms over certain terrain areas. Radar estimated rain rates were up to around 2-3 inches per hour with locally higher rates over shorter periods. There was a RAWS station in eastern Imperial County that measured right around 3 inches in 1 hour. These high rain rates led to areas of high rainfall accumulation, with many areas seeing at least 1 inch of rain and isolated areas up to 3.5-4.5 inches, radar estimated. This resulted in numerous reports of considerable flash flooding around the region. The hardest hit was the town of Niland and immediate surrounding area. A few inches of rain fell east of Niland leading to a canal being overcome with water and silt. This exacerbated the flooding and several inches of water flowed through the town and surrounding areas. The major impacts led to an emergency proclamation by the County of Imperial. In addition to the road closures, there were several swift water rescues across Imperial and Riverside Counties, both by land and air. One of the air rescues was completed by the San Diego US Coast Guard. On top of all the flooding, the heavy mass loading and strong updrafts resulted in strong to severe downburst winds, which caused a couple semi truck rollovers, downed many power poles, and generated dense  blowing dust. An incident report from California Highway Patrol said there was flooding along Hwy-95, prompting a call for a potential closure of the highway. No injuries or damages were reported.", "ts_dict_index": [864, 865, 866]}
+{"event_id": 913057, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-08-27 17:00:00", "end_date_time": "2020-08-27 17:00:00", "narrative": "Tropical Storm Laura moved ashore from the Gulf of Mexico near Cameron, LA, around 1200 AM CST on August 27, 2020 with 150 mph sustained winds! This part of the state had never experienced such a powerful (Category 4) hurricane. Measured gusts exceeded 130 mph in Lake Charles, LA. Not only was there widespread structural damage, a television tower was destroyed and the WSR-88D (Doppler Weather Radar) at the local National Weather Service (NWS) office was obliterated. Staff at the office was evacuated prior to the arrival of Laura, with backup provided by NWS Brownsville, TX.||Laura remained a hurricane well inland as the system ventured to the north at around 15 mph. A swath of heavy rain (two to more than five inches) spread into southern, central, and northeast Arkansas in the twenty four hour period ending at 700 am CDT on the 28th. Fordyce (Dallas County) received 5.25 inches of precipitation, with 4.48 inches at Cabot (Lonoke County), 4.39 inches at Marche (Pulaski County), 4.37 inches at North Little Rock (Pulaski County), 4.17 inches at Keo (Lonoke County), 3.85 inches at Calamine (Sharp County), 3.60 inches at Stuttgart (Arkansas County), 3.55 inches at Batesville (Independence County) and El Dorado (Union County), 3.53 inches at Sheridan (Grant County), and 3.50 inches at Alicia (Lawrence County).||The atmosphere was loaded with moisture, and this created high rainfall rates. Water came down faster than it could be carried away, and roads flooded at Benton (Saline County), North Little Rock and Sherwood (both in Pulaski County), Walnut Ridge and near Ravenden (both in Lawrence County), and a few miles east of Mena (Polk County). Several streets and intersections in North Little Rock were flooded and impassable. Several pictures and reports were acquired via social media. The time was estimated based on the time of tweet and radar data.", "ts_dict_index": [942, 943, 944]}
+{"event_id": 913051, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-08-27 16:00:00", "end_date_time": "2020-08-27 16:00:00", "narrative": "Tropical Storm Laura moved ashore from the Gulf of Mexico near Cameron, LA, around 1200 AM CST on August 27, 2020 with 150 mph sustained winds! This part of the state had never experienced such a powerful (Category 4) hurricane. Measured gusts exceeded 130 mph in Lake Charles, LA. Not only was there widespread structural damage, a television tower was destroyed and the WSR-88D (Doppler Weather Radar) at the local National Weather Service (NWS) office was obliterated. Staff at the office was evacuated prior to the arrival of Laura, with backup provided by NWS Brownsville, TX.||Laura remained a hurricane well inland as the system ventured to the north at around 15 mph. A swath of heavy rain (two to more than five inches) spread into southern, central, and northeast Arkansas in the twenty four hour period ending at 700 am CDT on the 28th. Fordyce (Dallas County) received 5.25 inches of precipitation, with 4.48 inches at Cabot (Lonoke County), 4.39 inches at Marche (Pulaski County), 4.37 inches at North Little Rock (Pulaski County), 4.17 inches at Keo (Lonoke County), 3.85 inches at Calamine (Sharp County), 3.60 inches at Stuttgart (Arkansas County), 3.55 inches at Batesville (Independence County) and El Dorado (Union County), 3.53 inches at Sheridan (Grant County), and 3.50 inches at Alicia (Lawrence County).||The atmosphere was loaded with moisture, and this created high rainfall rates. Water came down faster than it could be carried away, and roads flooded at Benton (Saline County), North Little Rock and Sherwood (both in Pulaski County), Walnut Ridge and near Ravenden (both in Lawrence County), and a few miles east of Mena (Polk County). The intersection of Brockington and Kiehl was flooded and impassable to traffic.", "ts_dict_index": [945, 946, 947]}
+{"event_id": 953792, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2021-06-07 03:00:00", "end_date_time": "2021-06-07 05:15:00", "narrative": "An upper low pressure system drifted north over Southeast Oklahoma and Western Arkansas during the early morning hours of June 7th, with an upper level disturbance beneath the attendant trough enhancing an area of showers and thunderstorms over Southwest Arkansas. A moist and unstable air mass was in place, with weak steering also present which resulted in slow-moving storms producing locally heavy rainfall. Rainfall amounts of 3-5 inches fell from Southern Howard County across Northern Hempstead and Nevada Counties, which resulted in flash flooding over Northern Hempstead County where several roads were flooded and closed. ||Another complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of another shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms, with a tornado briefly touching down just west of Calion, AR in Northeast Union County from a storm that developed ahead of the main line of storms. These storms exited Southwest Arkansas during the late afternoon hours. County Road 333 was flooded and closed due to rushing water from the Middle Fork Ozan Creek. A car attempted to cross the flooded roadway and stalled in the high water.", "ts_dict_index": [951, 952, 953]}
+{"event_id": 1080263, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "SCOTT", "begin_date_time": "2023-02-08 08:30:00", "end_date_time": "2023-02-08 11:30:00", "narrative": "Heavy to excessive rain was in the forecast on February 7th/8th, especially in northern and western Arkansas. This was ahead of a storm system in the southern Plains, and north of a nearly stationary front draped across central sections of the state. South of the front, increasing warmth/moisture set the stage for the possibility of severe thunderstorms toward evening on the 8th.||The placement of the front was obvious as of 300 pm CST on the 8th. North of the front, temperatures were only in the 40s/50s. The thermometer showed 45 degrees at Harrison (Boone County) and 49 degrees at Walnut Ridge (Lawrence County). Readings were in the 60s/70s farther south, with a springlike 78 degrees at Monticello (Drew County), and 79 degrees at Camden (Ouachita County).||Three to more than six inches of precipitation dumped at many locations in the north/west. Forty eight hour amounts through 600 am CST on the 9th included 6.60 inches at Mountain View (Stone County), 6.03 inches at Big Fork (Polk County), 5.82 inches at Mena (Polk County), 5.66 inches at Hattieville (Conway County), 5.42 inches at Witts Springs (Searcy County), 5.32 inches at Vandervoort (Polk County), 5.30 inches at Langley (Pike County), 5.24 inches at Damascus (Van Buren County), 5.19 inches at Morrilton (Conway County), 5.18 inches at Danville (Yell County), 5.12 inches at Murfreesboro (Pike County), 5.09 inches at Cushman (Independence County), 5.03 inches at Greers Ferry Dam (Cleburne County), and 5.02 inches at Mount Ida (Montgomery County). Arkansas Department of Transportation closed AR State Highway 80 between highways 28 and 71 due to highwater over the roadway at the confluence of the Poteau River and Jones Creek just northwest of Waldron.", "ts_dict_index": [978, 979, 980]}
+{"event_id": 810098, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2019-04-13 09:30:00", "end_date_time": "2019-04-13 11:00:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana to along the Arkansas border. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with reports of damaging winds received over extreme Southern Arkansas. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon. These storms continued to develop and move repeatedly over the same areas, producing flash flooding across portions of Union County Arkansas. These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Highway 275 was closed from the Highway 129 intersection south to the Louisiana border in Southern Union County. Heavy rainfall had flooded the highway at three different creek crossings.", "ts_dict_index": [966, 967, 968]}
+{"event_id": 810099, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2019-04-13 13:00:00", "end_date_time": "2019-04-13 15:45:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana to along the Arkansas border. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with reports of damaging winds received over extreme Southern Arkansas. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon. These storms continued to develop and move repeatedly over the same areas, producing flash flooding across portions of Union County Arkansas. These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Several pictures and videos of flooding across the city of El Dorado was posted to the KATV-TV Facebook page.", "ts_dict_index": [969, 970, 971]}
+{"event_id": 953791, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2021-06-07 03:00:00", "end_date_time": "2021-06-07 05:15:00", "narrative": "An upper low pressure system drifted north over Southeast Oklahoma and Western Arkansas during the early morning hours of June 7th, with an upper level disturbance beneath the attendant trough enhancing an area of showers and thunderstorms over Southwest Arkansas. A moist and unstable air mass was in place, with weak steering also present which resulted in slow-moving storms producing locally heavy rainfall. Rainfall amounts of 3-5 inches fell from Southern Howard County across Northern Hempstead and Nevada Counties, which resulted in flash flooding over Northern Hempstead County where several roads were flooded and closed. ||Another complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of another shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms, with a tornado briefly touching down just west of Calion, AR in Northeast Union County from a storm that developed ahead of the main line of storms. These storms exited Southwest Arkansas during the late afternoon hours. Hempstead Road 1315 was flooded and closed due to a washed out culvert.", "ts_dict_index": [954, 955, 956]}
+{"event_id": 801269, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 07:24:00", "end_date_time": "2019-03-06 11:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported southbound State Route 178 was completely washed out south of the Elizabeth Norris Blvd. intersection.", "ts_dict_index": [963, 964, 965]}
+{"event_id": 801268, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 07:24:00", "end_date_time": "2019-03-06 11:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported several roads were completely washed out by heavy rainfall in Havilah.", "ts_dict_index": [960, 961, 962]}
+{"event_id": 866531, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-01-10 21:40:00", "end_date_time": "2020-01-10 23:30:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across Southeast Oklahoma and East-Central Texas. Thus, an axis of showers and thunderstorms, some containing locally heavy rainfall, developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and Northeast Texas, producing widespread rainfall amounts of two to four inches, with isolated higher amounts up to five inches recorded. This heavy rainfall contributed to flash flooding across portions of McCurtain County Oklahoma, before the rains tapered off by late evening and the early morning hours of November 11th. Several roads were flooded and closed in Broken Bow.", "ts_dict_index": [981, 982, 983]}
+{"event_id": 866529, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-01-10 20:40:00", "end_date_time": "2020-01-10 23:30:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across Southeast Oklahoma and East-Central Texas. Thus, an axis of showers and thunderstorms, some containing locally heavy rainfall, developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and Northeast Texas, producing widespread rainfall amounts of two to four inches, with isolated higher amounts up to five inches recorded. This heavy rainfall contributed to flash flooding across portions of McCurtain County Oklahoma, before the rains tapered off by late evening and the early morning hours of November 11th. Highway 70 on Valliant was flooded.", "ts_dict_index": [987, 988, 989]}
+{"event_id": 953815, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-07 20:00:00", "end_date_time": "2021-06-07 21:13:00", "narrative": "A complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of a shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms across East Texas, North Louisiana, and Southwest Arkansas, before exiting the region during the late afternoon hours. This complex of storms produced a large Mesoscale Convective Vortex (MCV) as it shifted across Northeast Texas into Southwest Arkansas during the late afternoon and early evening, which focused an area of heavy rainfall across McCurtain County Oklahoma during the evening. Rainfall totals of 3-5 inches fell across this area, resulting in flash flooding with multiple roads flooded and closed and vehicles stalled in the high water. These storms finally exited the region and diminished with the passage of these upper level disturbances, before additional storms redeveloped along a remnant surface boundary over Southeast Oklahoma and the northern sections of Southwest Arkansas during the early morning hours of June 8th, resulting in additional flash flooding. Several roads were flooded and closed due to swift moving water over the roadways. Several vehicles were stalled and abandoned in the high water.", "ts_dict_index": [948, 949, 950]}
+{"event_id": 866532, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-01-10 21:40:00", "end_date_time": "2020-01-10 23:30:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across Southeast Oklahoma and East-Central Texas. Thus, an axis of showers and thunderstorms, some containing locally heavy rainfall, developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and Northeast Texas, producing widespread rainfall amounts of two to four inches, with isolated higher amounts up to five inches recorded. This heavy rainfall contributed to flash flooding across portions of McCurtain County Oklahoma, before the rains tapered off by late evening and the early morning hours of November 11th. Numerous roads were flooded and closed in and near Hochatown.", "ts_dict_index": [984, 985, 986]}
+{"event_id": 964715, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2021-07-09 07:53:00", "end_date_time": "2021-07-09 08:53:00", "narrative": "Several days of heavy to torrential rains and gusty winds were experienced across eastern Kentucky from July 9th through the 12th. A strong surface low pressure remained parked across Illinois to our WNW, with a frontal boundary expanding eastward and through Kentucky, sinking just south of the state to start the day on the 9th. During the day on the 9th and the 10th, the front began lifting northward through eastern Kentucky as a warm front, becoming the center for convective development, and also allowing for much deeper warm air and moisture advection into the region. As the front slowly continued just north of the state on the 11th and 12th, Kentucky found itself in the warm and unstable sector of the system, with showers and thunderstorms developing, peaking in coverage and intensity during the afternoon hours. ||Given the warm environment, storms were generally low centroid and moisture laden, exhibiting well above normal PWats, in the 2 to 2.5 inch range. Soundings also showed shallow inverted V signatures, indicative of steep low level lapse rates and the ability to easily mix down higher winds aloft. Pulsy scattered convection with heavy rain and high wind gusts were the main concerns. Locations where multiple storms moved over saw high water and some instances of flash flooding. Other locations experienced thunderstorm wind damage as stronger winds transferred to the surface, especially as the storms were beginning the dissipating phase. ||An 850 jet SW to NE, storms that NW to SE oriented were bowing. A video that showed that flash flooding was occurring near the Pikeville Elementary School in Pikeville was posted to one of NWS Jackson KY's social media feeds.", "ts_dict_index": [975, 976, 977]}
+{"event_id": 964716, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2021-07-09 07:55:00", "end_date_time": "2021-07-09 08:55:00", "narrative": "Several days of heavy to torrential rains and gusty winds were experienced across eastern Kentucky from July 9th through the 12th. A strong surface low pressure remained parked across Illinois to our WNW, with a frontal boundary expanding eastward and through Kentucky, sinking just south of the state to start the day on the 9th. During the day on the 9th and the 10th, the front began lifting northward through eastern Kentucky as a warm front, becoming the center for convective development, and also allowing for much deeper warm air and moisture advection into the region. As the front slowly continued just north of the state on the 11th and 12th, Kentucky found itself in the warm and unstable sector of the system, with showers and thunderstorms developing, peaking in coverage and intensity during the afternoon hours. ||Given the warm environment, storms were generally low centroid and moisture laden, exhibiting well above normal PWats, in the 2 to 2.5 inch range. Soundings also showed shallow inverted V signatures, indicative of steep low level lapse rates and the ability to easily mix down higher winds aloft. Pulsy scattered convection with heavy rain and high wind gusts were the main concerns. Locations where multiple storms moved over saw high water and some instances of flash flooding. Other locations experienced thunderstorm wind damage as stronger winds transferred to the surface, especially as the storms were beginning the dissipating phase. ||An 850 jet SW to NE, storms that NW to SE oriented were bowing. Flash flooding was reported at a few locations around downtown Pikeville.", "ts_dict_index": [972, 973, 974]}
+{"event_id": 1132067, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2023-08-20 11:53:00", "end_date_time": "2023-08-20 13:53:00", "narrative": "Tropical Storm Hilary brought abundant moisture along with strong winds to southern California on the 20th. In fact, Tropical Storm Warnings were issued for the first time in history along the southern California coast. On the 19th, a trough near the southern California coast promoted deep southerly flow that allowed deeper moisture to advect into the Southwest ahead of Hilary. Combined with jet dynamics, showers and thunderstorms developed during the early morning hours on the 19th, leading to an isolated instance of flash flooding in southeast California. Going into the 20th, very anomalous moisture accompanied Hilary with PWATs across southeast California climbing upwards of 2-2.5 and IVT values in excess of 15 normalized standard deviations from average. Thus, flash flooding was the primary impact across southern California with a very rare high risk of excessive rainfall being issued by WPC for part of the area. Rainfall totals across southeast California were as high as 2-3, while most areas across Imperial County and eastern Riverside County generally measured around 1.50 or less. However, much heavier rainfall amounts were observed closer to the southern California coast. In addition to flash flooding impacts, several instances of damaging winds occurred as strong low level winds upwards of 50-60 knots at 850 mb and 925 mb mixed to the surface in some cases. Several communities around the Salton Sea were under a voluntary evacuation order as a precaution for any potential impacts stemming from flash flooding and strong winds. Multiple reports of flooding impacts and wind damage primarily across Imperial County resulted from this event. No injuries were reported. CHP reported flash flooding near Orchard Road and Edwards Road. No injuries were reported.", "ts_dict_index": [936, 937, 938]}
+{"event_id": 1014574, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2022-04-12 23:04:00", "end_date_time": "2022-04-13 01:15:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. Pearl Street was flooded in Nacogdoches.", "ts_dict_index": [993, 994, 995]}
+{"event_id": 977072, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 11:10:00", "end_date_time": "2021-07-23 12:40:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Heavy rain fell in Fountain Hills with a few rain gages measuring a little over 1 inch in an hour. Rapid runoff led to significant flow in Ashbrook Wash. Social media videos showed at least 6-12 inches of swift moving water over Fountain Hills Boulevard near Ashbrook Drive as well as over Del Cambre Avenue near Grande Boulevard. The roads were impassable to all traffic. No damages or injuries were reported.", "ts_dict_index": [996, 997, 998]}
+{"event_id": 976652, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-22 22:21:00", "end_date_time": "2021-07-23 00:00:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Arizona Department of Transportation reported the Greenway Road underpass at Interstate-17 was flooded and the on/exit ramps were also under water. A couple vehicles became stranded in the flood water. This forced the closure of the underpass. No damages or injuries were reported.", "ts_dict_index": [1005, 1006, 1007]}
+{"event_id": 866530, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-01-10 20:45:00", "end_date_time": "2020-01-10 23:30:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across Southeast Oklahoma and East-Central Texas. Thus, an axis of showers and thunderstorms, some containing locally heavy rainfall, developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and Northeast Texas, producing widespread rainfall amounts of two to four inches, with isolated higher amounts up to five inches recorded. This heavy rainfall contributed to flash flooding across portions of McCurtain County Oklahoma, before the rains tapered off by late evening and the early morning hours of November 11th. Iron Stob Road north of Highway 37 was flooded.", "ts_dict_index": [990, 991, 992]}
+{"event_id": 976264, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-22 20:35:00", "end_date_time": "2021-07-22 20:50:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Social media video showed water flowing over Sunland Gin Road near Tonto Road. Time estimated from radar rainfall estimates. No damages or injuries reported.", "ts_dict_index": [1002, 1003, 1004]}
+{"event_id": 801363, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 16:53:00", "end_date_time": "2019-03-06 20:53:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported Tejon Highway completely washed out south of Mountain View Rd. in Lamont.", "ts_dict_index": [957, 958, 959]}
+{"event_id": 814385, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-04-24 21:15:00", "end_date_time": "2019-04-24 23:30:00", "narrative": "A strong closed upper level low pressure system advanced east across Central Texas during the evening hours of April 24th, which helped to mix a warm front north into portions of Deep East Texas and Northcentral Louisiana. As a result, warm, moist, and unstable air began to build north along and south of the front, as steepening lapse rates aloft spread east along the axis of increasing large scale forcing ahead of the low. This resulted in an increase in scattered to numerous showers and thunderstorms near and south of the warm front from the late evening hours of the 24th through the early morning hours of the 25th across East Texas and North Louisiana. Coupled with the strong wind shear present across the expanding warm sector, several supercell thunderstorms developed, with one supercell spawning six separate tornadoes from San Augustine Texas northeast to Eastern Union Parish Louisiana, directly impacting the cities of San Augustine Texas and Ruston Louisiana along its 150+ mile track across the NWS Shreveport County Warning Area. In fact, this supercell spawned another tornado across Northwest Morehouse and Southern Ashley County Arkansas, to complete its nearly 180 mile track before dissipating. Additional showers and thunderstorms developed farther north of the warm front along the I-20 corridor of East Texas, with locally heavy rainfall of 3-6+ inches resulting in areas of flash flooding across Southwest and Central Smith County. A picture was posted to social media of high water which covered many streets in Flint.", "ts_dict_index": [1053, 1054, 1055]}
+{"event_id": 814383, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-04-24 20:52:00", "end_date_time": "2019-04-24 23:30:00", "narrative": "A strong closed upper level low pressure system advanced east across Central Texas during the evening hours of April 24th, which helped to mix a warm front north into portions of Deep East Texas and Northcentral Louisiana. As a result, warm, moist, and unstable air began to build north along and south of the front, as steepening lapse rates aloft spread east along the axis of increasing large scale forcing ahead of the low. This resulted in an increase in scattered to numerous showers and thunderstorms near and south of the warm front from the late evening hours of the 24th through the early morning hours of the 25th across East Texas and North Louisiana. Coupled with the strong wind shear present across the expanding warm sector, several supercell thunderstorms developed, with one supercell spawning six separate tornadoes from San Augustine Texas northeast to Eastern Union Parish Louisiana, directly impacting the cities of San Augustine Texas and Ruston Louisiana along its 150+ mile track across the NWS Shreveport County Warning Area. In fact, this supercell spawned another tornado across Northwest Morehouse and Southern Ashley County Arkansas, to complete its nearly 180 mile track before dissipating. Additional showers and thunderstorms developed farther north of the warm front along the I-20 corridor of East Texas, with locally heavy rainfall of 3-6+ inches resulting in areas of flash flooding across Southwest and Central Smith County. Several roads were covered in high water in the Emerald Bay subdivision near Lake Palestine.", "ts_dict_index": [1056, 1057, 1058]}
+{"event_id": 977109, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 12:38:00", "end_date_time": "2021-07-23 16:31:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Two people had to be rescued from their mobile home near Central Avenue and Mingus Road after flood waters rapidly overcame the area. Water was reportedly flowing through their windows and there was concern that the home would flow away. They were rescued via helicopter because responders were unable to reach the home on the ground with multiple impassable flooded roads. Rain gages in the area measured over 1.5 inches of rain in less than an hour The two people were uninjured, but their two dogs did not survive.", "ts_dict_index": [1017, 1018, 1019]}
+{"event_id": 977020, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-23 00:15:00", "end_date_time": "2021-07-23 00:35:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Arizona Department of Transportation closed Highway-188 between mile posts 246 and 253 due to flooding with an overtopped drainage cut and debris on the road. Runoff may have been enhanced by the 2020 Bush burn scar. Timing estimated from radar. No damages or injuries were reported.", "ts_dict_index": [1032, 1033, 1034]}
+{"event_id": 977115, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 13:30:00", "end_date_time": "2021-07-23 17:30:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Video from Maricopa County Sheriff's Office showed two individuals being rescued via helicopter from the roof of a delivery truck that became stranded in a flooded wash near 7th street and Cloud Road. The two individuals were uninjured. The chopper footage also showed at least one home with roughly 1 to 2 fee of water surrounding it. No additional info provided on any impacted homes. Another video near 12th Street and Carefree Highway showed several inches of water flowing down 12th Street. An individual had to be rescued from their car after it became stranded in the flood water. The individual was uninjured, but the vehicle was lost.", "ts_dict_index": [1026, 1027, 1028]}
+{"event_id": 977434, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 14:00:00", "end_date_time": "2021-07-23 18:00:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Skunk Creek experienced a significant rise after 2 to 4 inches of rain fell over the area and upstream. At 1400MST the the streamflow gage on Skunk Creek at Carefree Highway exceeded alarm stage. The gage then exceeded bank full at 1410MST and exceeded flood stage at 1418MST. Flow crested at 6.87 feet at 1426MST and would remain above alarm stage until 1715MST. A video posted at 1307MST on social media showed significant flow and debris over Dove Valley Road between I-17 and North Valley Parkway. Maricopa County Department of Transportation reported 27th Avenue was closed between Cloud Road and Dolores Road. No damages or injuries were reported.", "ts_dict_index": [1047, 1048, 1049]}
+{"event_id": 977112, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 11:45:00", "end_date_time": "2021-07-23 14:00:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. A little over 1 inch of rain fell in roughly 1 hour east of Cave Creek between 1000MST and 1100MST. Light to moderate rain was falling beforehand and continue to fall through the early afternoon. Maricopa County Department of Transportation reported at 1335MST that Needlerock Road north of Rio Verde Drive was closed due to flooding. No injuries or damage was reported.", "ts_dict_index": [1008, 1009, 1010]}
+{"event_id": 976650, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-22 21:50:00", "end_date_time": "2021-07-23 02:40:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Very heavy rain fell in the Scottsdale area beginning around 2100MST on the 22nd. A rain gage at Indian School Road and Indian Bend Wash measured a little over 2 inches in 50 minutes. A significant amount of runoff collected in Indian Bend Wash that flooded multiple low water road crossings as well as flooded recreational parks built in the wash. Osborn Road across the wash was impassable with roughly 2 feet of moving water over the road. One vehicle became stuck trying to cross the flood waters and had to be rescued by the fire department. A flood control streamflow gage on Indian School Road, a block north, exceeded alarm stage at 2146MST on the 22nd and did not fully recede below alarm stage until 0239MST on the 23rd. Helicopter footage after sunrise on the 23rd still showed minor levels of flooding in the wash. No injuries were reported.", "ts_dict_index": [1020, 1021, 1022]}
+{"event_id": 976651, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-22 22:14:00", "end_date_time": "2021-07-23 00:00:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. The Thunderbird Road underpass at Interstate-17 became impassable with 2 to 3 feet of standing water after over 1 inch of rain fell in roughly one hour. One vehicle stalled in the flood water and had to be towed out. The road was eventually closed. No injuries reported.", "ts_dict_index": [1041, 1042, 1043]}
+{"event_id": 977447, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 13:05:00", "end_date_time": "2021-07-23 18:15:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Significant flood water moving downstream within Skunk Creek led to the closure of the low water crossing along Honda Bow Road between 7th Avenue and 9th Avenue. Time estimated from streamflow gages and radar. No damages or injuries reported.", "ts_dict_index": [1014, 1015, 1016]}
+{"event_id": 977062, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-23 02:00:00", "end_date_time": "2021-07-23 02:30:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. A local bridge along Mackey Camp Road reportedly washed out following a rapid rise in flood waters in Bloody Tanks Wash. Runoff may have been enhanced by the 2021 Telegraph burn scar. Timing based on upstream rain gage and radar. No injuries reported.", "ts_dict_index": [1035, 1036, 1037]}
+{"event_id": 977082, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 10:00:00", "end_date_time": "2021-07-23 10:20:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Hatcher Road was closed due to flooding between 11th Street and 11th Place. Nearby rain gages measured from 0.25 to 1.10 inches. Time estimated from radar and rain gages. No damages or injuries reported.", "ts_dict_index": [1011, 1012, 1013]}
+{"event_id": 977433, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 15:00:00", "end_date_time": "2021-07-23 16:30:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. U.S. Forest Service reported a 4 foot rise in Camp Creek with flow originating from the Sears burn scar. Time estimated from radar. No damages or injuries were reported.", "ts_dict_index": [1038, 1039, 1040]}
+{"event_id": 977439, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 14:10:00", "end_date_time": "2021-07-23 16:45:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. A streamflow gage on New River near Table Mesa Road exceeded alarm stage at 1404MST, bank full at 1419MST, and flood stage at 1422MST. The flood wave crested at 7.88 feet at 1426MST and remained above alarm stage until 1620MST. Three individuals were rescued by Maricopa County Sheriff's Office via helicopter after their SUV stalled in the flood waters near Table Mesa Road. A low water crossing roughly 7 miles downstream along Old Stage Road, north of New River Road, experienced significant flow and the road had to be closed. No injuries were reported.", "ts_dict_index": [1044, 1045, 1046]}
+{"event_id": 976263, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-22 20:35:00", "end_date_time": "2021-07-22 20:50:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Flash flooding reported near a truck stop at Sunland Gin Road and Interstate-10. Water was a few feet deep in spots. Timing estimated from radar rainfall estimates. No damages or injuries reported.", "ts_dict_index": [1050, 1051, 1052]}
+{"event_id": 977430, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 13:15:00", "end_date_time": "2021-07-23 18:30:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. A Flood Control District of Maricopa County streamflow gage along Skunk Creek at Desert Hills Drive exceeded alarm stage around 1315MST and bank full around 1325MST. Streamflow crested around 5.81 feet at 1329MST and was back below action stage by 1800MST. At 1805MST Maricopa County Department of Transportation reported 19th Avenue was closed between Desert Hills Drive and Irvine Road due to flooding. No damages or injuries were reported.", "ts_dict_index": [999, 1000, 1001]}
+{"event_id": 883366, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2020-03-29 02:47:00", "end_date_time": "2020-03-29 06:00:00", "narrative": "A warm front over central Ohio on the morning of Saturday March 28, 2020 was the focus for several rounds of elevated thunderstorms through the early afternoon hours. The main area for these thunderstorms were the US 30 and I-76 corridors through the morning and early afternoon hours as storms remained parallel to the warm front and moved with the 850 mb jet. These storms well utilized the steep mid-level lapse rates and hail in excess of 2 inches fell over portions of Medina, Summit, and Portage Counties. These storms began to train along this I-76 corridor and most of these areas received 1 to 2 inches of rain by the afternoon of the 28th, resulting in some minor flooding.||Convection that developed across the Mississippi Valley grew downstream and made its way east across the area between 11pm Saturday and 4am Sunday. A warm/stationary west-east oriented front stayed south of Lake Erie, which allowed additional convection to develop downstream from the line of aforementioned thunderstorms. Despite the very fast moving storms, a moist atmosphere, persistent moisture advection with a strong low level jet, and training convection with efficient rainfall allowed for a wide area of minor flooding from Hancock County to Crawford, PA County where 1-2��� of rain was observed. The hardest hit area was Cuyahoga County where Big Creek and Cuyahoga River went into major flood stage and there were numerous reports of flash flooding. Significant flooding occurred on the Mill Creek in eastern Cuyahoga County. The USGS gage 04208460 Mill Creek at Garfield Heights reported the highest flow and stage of record (2001- present day ) at 8.47 feet and a flow of 4,750cfs at 310 AM. Public safety officials reported significant flooding with flooded roads and cars stranded in Garfield Heights.", "ts_dict_index": [1083, 1084, 1085]}
+{"event_id": 883372, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2020-03-29 03:30:00", "end_date_time": "2020-03-29 06:00:00", "narrative": "A warm front over central Ohio on the morning of Saturday March 28, 2020 was the focus for several rounds of elevated thunderstorms through the early afternoon hours. The main area for these thunderstorms were the US 30 and I-76 corridors through the morning and early afternoon hours as storms remained parallel to the warm front and moved with the 850 mb jet. These storms well utilized the steep mid-level lapse rates and hail in excess of 2 inches fell over portions of Medina, Summit, and Portage Counties. These storms began to train along this I-76 corridor and most of these areas received 1 to 2 inches of rain by the afternoon of the 28th, resulting in some minor flooding.||Convection that developed across the Mississippi Valley grew downstream and made its way east across the area between 11pm Saturday and 4am Sunday. A warm/stationary west-east oriented front stayed south of Lake Erie, which allowed additional convection to develop downstream from the line of aforementioned thunderstorms. Despite the very fast moving storms, a moist atmosphere, persistent moisture advection with a strong low level jet, and training convection with efficient rainfall allowed for a wide area of minor flooding from Hancock County to Crawford, PA County where 1-2��� of rain was observed. The hardest hit area was Cuyahoga County where Big Creek and Cuyahoga River went into major flood stage and there were numerous reports of flash flooding. At the USGS Tinkers Creek gage at Bedford, Ohio (No. 04207200), on March 29th the Creek crested at 530 am with a stage of 8.44 feet and a flow of 4690 cfs as a 10-year flood, which put it just below the flood of February 28, 2011. Backwater from the Cuyahoga River exasperated flooding near the confluence near Valley View.", "ts_dict_index": [1071, 1072, 1073]}
+{"event_id": 883365, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2020-03-29 02:15:00", "end_date_time": "2020-03-29 06:00:00", "narrative": "A warm front over central Ohio on the morning of Saturday March 28, 2020 was the focus for several rounds of elevated thunderstorms through the early afternoon hours. The main area for these thunderstorms were the US 30 and I-76 corridors through the morning and early afternoon hours as storms remained parallel to the warm front and moved with the 850 mb jet. These storms well utilized the steep mid-level lapse rates and hail in excess of 2 inches fell over portions of Medina, Summit, and Portage Counties. These storms began to train along this I-76 corridor and most of these areas received 1 to 2 inches of rain by the afternoon of the 28th, resulting in some minor flooding.||Convection that developed across the Mississippi Valley grew downstream and made its way east across the area between 11pm Saturday and 4am Sunday. A warm/stationary west-east oriented front stayed south of Lake Erie, which allowed additional convection to develop downstream from the line of aforementioned thunderstorms. Despite the very fast moving storms, a moist atmosphere, persistent moisture advection with a strong low level jet, and training convection with efficient rainfall allowed for a wide area of minor flooding from Hancock County to Crawford, PA County where 1-2��� of rain was observed. The hardest hit area was Cuyahoga County where Big Creek and Cuyahoga River went into major flood stage and there were numerous reports of flash flooding. The Cuyahoga River reached the seventh-highest level in recorded history. Most of the properties impacted were businesses along the ���Flats��� portion of the Cuyahoga River in Cleveland, most of which were vacant on a Sunday morning and the result of statewide stay at home orders. Some homes were flooded in Valley View and Independence areas, mainly basement and garage flooding. The Cuyahoga Valley National Park was inundated along the canal system, railroad station, and widespread flooding of nature trails and access roads near the river.  ||The USGS 04208000 Cuyahoga River at Independence reached its 7th highest crest/flow on record since 1922. The peak occurred at 930 AM with a stage of 21.62 feet and a flow of 14,700 cfs. The estimated return period is a 10- year event. ||The USGS gage 04208504 Cuyahoga River near Newburgh Heights is downstream of the official forecast point at Independence and closer to the industrial portion of Cuyahoga County. The gage reached a stage of 74.3 feet at 6 PM on the 29th. This stage is above the rating curve so no flow data is available.", "ts_dict_index": [1086, 1087, 1088]}
+{"event_id": 883362, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2020-03-29 02:00:00", "end_date_time": "2020-03-29 06:00:00", "narrative": "A warm front over central Ohio on the morning of Saturday March 28, 2020 was the focus for several rounds of elevated thunderstorms through the early afternoon hours. The main area for these thunderstorms were the US 30 and I-76 corridors through the morning and early afternoon hours as storms remained parallel to the warm front and moved with the 850 mb jet. These storms well utilized the steep mid-level lapse rates and hail in excess of 2 inches fell over portions of Medina, Summit, and Portage Counties. These storms began to train along this I-76 corridor and most of these areas received 1 to 2 inches of rain by the afternoon of the 28th, resulting in some minor flooding.||Convection that developed across the Mississippi Valley grew downstream and made its way east across the area between 11pm Saturday and 4am Sunday. A warm/stationary west-east oriented front stayed south of Lake Erie, which allowed additional convection to develop downstream from the line of aforementioned thunderstorms. Despite the very fast moving storms, a moist atmosphere, persistent moisture advection with a strong low level jet, and training convection with efficient rainfall allowed for a wide area of minor flooding from Hancock County to Crawford, PA County where 1-2��� of rain was observed. The hardest hit area was Cuyahoga County where Big Creek and Cuyahoga River went into major flood stage and there were numerous reports of flash flooding. Significant flash flooding on the Big Creek. Roads and businesses were flooded including Tiedeman and Brookpark. ||USGS 412624081450700 East Branch Big Creek at Brooklyn reached a stage of 10.77 feet and flow of 3,120 cfs at 425 AM. ||USGS 04208502 Big Creek at Cleveland at 530 AM reached a stage of 12.03 feet with a flow of 5,240 cfs. At that stage flooding occurs in the Cleveland Zoo. This is approximately the flow of a 10 year flood.", "ts_dict_index": [1080, 1081, 1082]}
+{"event_id": 883374, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2020-03-29 01:35:00", "end_date_time": "2020-03-29 03:30:00", "narrative": "A warm front over central Ohio on the morning of Saturday March 28, 2020 was the focus for several rounds of elevated thunderstorms through the early afternoon hours. The main area for these thunderstorms were the US 30 and I-76 corridors through the morning and early afternoon hours as storms remained parallel to the warm front and moved with the 850 mb jet. These storms well utilized the steep mid-level lapse rates and hail in excess of 2 inches fell over portions of Medina, Summit, and Portage Counties. These storms began to train along this I-76 corridor and most of these areas received 1 to 2 inches of rain by the afternoon of the 28th, resulting in some minor flooding.||Convection that developed across the Mississippi Valley grew downstream and made its way east across the area between 11pm Saturday and 4am Sunday. A warm/stationary west-east oriented front stayed south of Lake Erie, which allowed additional convection to develop downstream from the line of aforementioned thunderstorms. Despite the very fast moving storms, a moist atmosphere, persistent moisture advection with a strong low level jet, and training convection with efficient rainfall allowed for a wide area of minor flooding from Hancock County to Crawford, PA County where 1-2��� of rain was observed. The hardest hit area was Cuyahoga County where Big Creek and Cuyahoga River went into major flood stage and there were numerous reports of flash flooding. West Creek runs from Parma to Brooklyn Heights. The USGS 412453081395500 West Creek at Brooklyn Heights near the confluence of the Cuyahoga River crested at 235 AM at a stage of 7.23 feet and a flow of 2,390 cfs comparable to the flood of May 12, 2014, or between a 50 and 100-year flood. Widespread street flooding along with basement flooding was reported.", "ts_dict_index": [1068, 1069, 1070]}
+{"event_id": 814380, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-04-24 19:00:00", "end_date_time": "2019-04-24 23:30:00", "narrative": "A strong closed upper level low pressure system advanced east across Central Texas during the evening hours of April 24th, which helped to mix a warm front north into portions of Deep East Texas and Northcentral Louisiana. As a result, warm, moist, and unstable air began to build north along and south of the front, as steepening lapse rates aloft spread east along the axis of increasing large scale forcing ahead of the low. This resulted in an increase in scattered to numerous showers and thunderstorms near and south of the warm front from the late evening hours of the 24th through the early morning hours of the 25th across East Texas and North Louisiana. Coupled with the strong wind shear present across the expanding warm sector, several supercell thunderstorms developed, with one supercell spawning six separate tornadoes from San Augustine Texas northeast to Eastern Union Parish Louisiana, directly impacting the cities of San Augustine Texas and Ruston Louisiana along its 150+ mile track across the NWS Shreveport County Warning Area. In fact, this supercell spawned another tornado across Northwest Morehouse and Southern Ashley County Arkansas, to complete its nearly 180 mile track before dissipating. Additional showers and thunderstorms developed farther north of the warm front along the I-20 corridor of East Texas, with locally heavy rainfall of 3-6+ inches resulting in areas of flash flooding across Southwest and Central Smith County. County Road 1139 was closed at the intersection of Maple Drive in the Indian Creek area due to flooding.", "ts_dict_index": [1062, 1063, 1064]}
+{"event_id": 814381, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-04-24 19:23:00", "end_date_time": "2019-04-24 23:30:00", "narrative": "A strong closed upper level low pressure system advanced east across Central Texas during the evening hours of April 24th, which helped to mix a warm front north into portions of Deep East Texas and Northcentral Louisiana. As a result, warm, moist, and unstable air began to build north along and south of the front, as steepening lapse rates aloft spread east along the axis of increasing large scale forcing ahead of the low. This resulted in an increase in scattered to numerous showers and thunderstorms near and south of the warm front from the late evening hours of the 24th through the early morning hours of the 25th across East Texas and North Louisiana. Coupled with the strong wind shear present across the expanding warm sector, several supercell thunderstorms developed, with one supercell spawning six separate tornadoes from San Augustine Texas northeast to Eastern Union Parish Louisiana, directly impacting the cities of San Augustine Texas and Ruston Louisiana along its 150+ mile track across the NWS Shreveport County Warning Area. In fact, this supercell spawned another tornado across Northwest Morehouse and Southern Ashley County Arkansas, to complete its nearly 180 mile track before dissipating. Additional showers and thunderstorms developed farther north of the warm front along the I-20 corridor of East Texas, with locally heavy rainfall of 3-6+ inches resulting in areas of flash flooding across Southwest and Central Smith County. Farm to Market Road 14 at Interstate 20 was closed due to flooding.", "ts_dict_index": [1059, 1060, 1061]}
+{"event_id": 883367, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2020-03-29 04:00:00", "end_date_time": "2020-03-29 05:00:00", "narrative": "A warm front over central Ohio on the morning of Saturday March 28, 2020 was the focus for several rounds of elevated thunderstorms through the early afternoon hours. The main area for these thunderstorms were the US 30 and I-76 corridors through the morning and early afternoon hours as storms remained parallel to the warm front and moved with the 850 mb jet. These storms well utilized the steep mid-level lapse rates and hail in excess of 2 inches fell over portions of Medina, Summit, and Portage Counties. These storms began to train along this I-76 corridor and most of these areas received 1 to 2 inches of rain by the afternoon of the 28th, resulting in some minor flooding.||Convection that developed across the Mississippi Valley grew downstream and made its way east across the area between 11pm Saturday and 4am Sunday. A warm/stationary west-east oriented front stayed south of Lake Erie, which allowed additional convection to develop downstream from the line of aforementioned thunderstorms. Despite the very fast moving storms, a moist atmosphere, persistent moisture advection with a strong low level jet, and training convection with efficient rainfall allowed for a wide area of minor flooding from Hancock County to Crawford, PA County where 1-2��� of rain was observed. The hardest hit area was Cuyahoga County where Big Creek and Cuyahoga River went into major flood stage and there were numerous reports of flash flooding. Chagrin Falls police department recorded fast flowing water several feet deep rushing down neighborhood streets.", "ts_dict_index": [1077, 1078, 1079]}
+{"event_id": 883373, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2020-03-29 04:00:00", "end_date_time": "2020-03-29 06:30:00", "narrative": "A warm front over central Ohio on the morning of Saturday March 28, 2020 was the focus for several rounds of elevated thunderstorms through the early afternoon hours. The main area for these thunderstorms were the US 30 and I-76 corridors through the morning and early afternoon hours as storms remained parallel to the warm front and moved with the 850 mb jet. These storms well utilized the steep mid-level lapse rates and hail in excess of 2 inches fell over portions of Medina, Summit, and Portage Counties. These storms began to train along this I-76 corridor and most of these areas received 1 to 2 inches of rain by the afternoon of the 28th, resulting in some minor flooding.||Convection that developed across the Mississippi Valley grew downstream and made its way east across the area between 11pm Saturday and 4am Sunday. A warm/stationary west-east oriented front stayed south of Lake Erie, which allowed additional convection to develop downstream from the line of aforementioned thunderstorms. Despite the very fast moving storms, a moist atmosphere, persistent moisture advection with a strong low level jet, and training convection with efficient rainfall allowed for a wide area of minor flooding from Hancock County to Crawford, PA County where 1-2��� of rain was observed. The hardest hit area was Cuyahoga County where Big Creek and Cuyahoga River went into major flood stage and there were numerous reports of flash flooding. Flash flooding occurred around University Circle on the morning of the 29th. Backwater from Doan Brook along the MLK Parkway caused flooding in University Circle, mainly from combined sewer overflows. A water rescue was needed for a resident in a basement apartment. The creek reached a 10 year flood at 9 feet and 4,690 cfs around 530 AM on the 29th.", "ts_dict_index": [1074, 1075, 1076]}
+{"event_id": 883363, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2020-03-29 02:00:00", "end_date_time": "2020-03-29 06:00:00", "narrative": "A warm front over central Ohio on the morning of Saturday March 28, 2020 was the focus for several rounds of elevated thunderstorms through the early afternoon hours. The main area for these thunderstorms were the US 30 and I-76 corridors through the morning and early afternoon hours as storms remained parallel to the warm front and moved with the 850 mb jet. These storms well utilized the steep mid-level lapse rates and hail in excess of 2 inches fell over portions of Medina, Summit, and Portage Counties. These storms began to train along this I-76 corridor and most of these areas received 1 to 2 inches of rain by the afternoon of the 28th, resulting in some minor flooding.||Convection that developed across the Mississippi Valley grew downstream and made its way east across the area between 11pm Saturday and 4am Sunday. A warm/stationary west-east oriented front stayed south of Lake Erie, which allowed additional convection to develop downstream from the line of aforementioned thunderstorms. Despite the very fast moving storms, a moist atmosphere, persistent moisture advection with a strong low level jet, and training convection with efficient rainfall allowed for a wide area of minor flooding from Hancock County to Crawford, PA County where 1-2��� of rain was observed. The hardest hit area was Cuyahoga County where Big Creek and Cuyahoga River went into major flood stage and there were numerous reports of flash flooding. Several blocks around 160th Street and Miles Ave flooded due to flash flooding.", "ts_dict_index": [1089, 1090, 1091]}
+{"event_id": 977111, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 12:50:00", "end_date_time": "2021-07-23 13:10:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. The Flood Control District of Maricopa County streamflow gage on Cline Creek near Jenny Lin Road and 12th Street exceeded alarm stage at 1250MST and bank full at 1254MST. Flow crested at 6.9 feet at 1255MST and fell back below alarm stage at 1307MST. No injuries or damages were reported.", "ts_dict_index": [1023, 1024, 1025]}
+{"event_id": 1116944, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 20:30:00", "end_date_time": "2023-08-21 02:30:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. Kern County officials reported a road closure of South Kelso Valley Rd. and Birch Springs Pass due to heavy flooding.", "ts_dict_index": [1110, 1111, 1112]}
+{"event_id": 1116692, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 11:59:00", "end_date_time": "2023-08-20 14:59:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported several large rocks as least 1 foot in diameter washed up on northbound Interstate 5 just south of Grapevine Rd..", "ts_dict_index": [1104, 1105, 1106]}
+{"event_id": 1116703, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 17:36:00", "end_date_time": "2023-08-20 23:36:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported large rocks on SR 178 southwest of Lake Isabella.", "ts_dict_index": [1116, 1117, 1118]}
+{"event_id": 1116941, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 20:20:00", "end_date_time": "2023-08-21 02:20:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. Kern County officials reported a closure of Tehachapi Blvd. east of Tehachapi Willow Springs Rd. due to heavy flooding.", "ts_dict_index": [1113, 1114, 1115]}
+{"event_id": 1116688, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 11:01:00", "end_date_time": "2023-08-20 14:01:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported a large rock on northbound Interstate 5 south south of Grapevine Rd. near the truck escape ramp.", "ts_dict_index": [1095, 1096, 1097]}
+{"event_id": 1116959, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-21 00:42:00", "end_date_time": "2023-08-21 06:42:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported several stuck vehicles on Neuralia Rd. near Cantil Rd. with a road closure in place.", "ts_dict_index": [1101, 1102, 1103]}
+{"event_id": 1116931, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 18:21:00", "end_date_time": "2023-08-21 00:21:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported the intersection of SR 43 and Panama Lane was completely flooded.", "ts_dict_index": [1092, 1093, 1094]}
+{"event_id": 1116949, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 21:00:00", "end_date_time": "2023-08-21 03:00:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported a rock slide on southbound Interstate 5 just south of Fort Tejon Rd.", "ts_dict_index": [1098, 1099, 1100]}
+{"event_id": 1116698, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 15:45:00", "end_date_time": "2023-08-21 11:00:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. The Kern County Emergency Manager reported the SR 58 was closed between Tehachapi  Willow Springs Rd. and Sand Canyon Rd. due to heavy flooding.", "ts_dict_index": [1107, 1108, 1109]}
+{"event_id": 977418, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-23 12:50:00", "end_date_time": "2021-07-23 18:00:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Very heavy rain fell in the afternoon with over 2 inches measured in the Anthem and New River area with radar estimates up to 4 inches over the New River Mesa between 1200MST and 1400MST. A social media video taken around 1400MST showed a few feet of rapid moving water running within Skunk Creek with an unoccupied SUV flowing downstream near Fig Springs Road. Timing of when flooding began estimated from radar and streamflow gages. No injuries were reported.", "ts_dict_index": [1029, 1030, 1031]}
+{"event_id": 1116686, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 10:35:00", "end_date_time": "2023-08-20 22:35:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported a large rock blocking lanes on Interstate 5 south of Wheeler Ridge Rd.", "ts_dict_index": [1128, 1129, 1130]}
+{"event_id": 1116695, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 14:36:00", "end_date_time": "2023-08-20 17:36:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported flooding causing erosion and running over the roadway at the intersection of Elm Trail and Mount Pinos Way in Frazier Park.", "ts_dict_index": [1122, 1123, 1124]}
+{"event_id": 1116673, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-19 17:29:00", "end_date_time": "2023-08-19 20:29:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. Flooding and debris on the Cameron overpass on SR 58 caused a closure in both directions as SR 58 became impassible.", "ts_dict_index": [1131, 1132, 1133]}
+{"event_id": 1116687, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 10:53:00", "end_date_time": "2023-08-20 22:53:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported large rocks in the roadway on Sand Canyon Rd. 3 miles north of Tehachapi Blvd. which required clearing with a plow.", "ts_dict_index": [1125, 1126, 1127]}
+{"event_id": 1116701, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 16:54:00", "end_date_time": "2023-08-20 22:54:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported large rocks across the roadway at the intersection of SR 58 and SR 223. near Bealville.", "ts_dict_index": [1140, 1141, 1142]}
+{"event_id": 1116685, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 07:42:00", "end_date_time": "2023-08-21 11:00:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported heavy flooding on Redrock-Randsburg Rd. between US 395 and SR 14 which required the road to be closed.", "ts_dict_index": [1134, 1135, 1136]}
+{"event_id": 883361, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2020-03-29 01:44:00", "end_date_time": "2020-03-29 06:00:00", "narrative": "A warm front over central Ohio on the morning of Saturday March 28, 2020 was the focus for several rounds of elevated thunderstorms through the early afternoon hours. The main area for these thunderstorms were the US 30 and I-76 corridors through the morning and early afternoon hours as storms remained parallel to the warm front and moved with the 850 mb jet. These storms well utilized the steep mid-level lapse rates and hail in excess of 2 inches fell over portions of Medina, Summit, and Portage Counties. These storms began to train along this I-76 corridor and most of these areas received 1 to 2 inches of rain by the afternoon of the 28th, resulting in some minor flooding.||Convection that developed across the Mississippi Valley grew downstream and made its way east across the area between 11pm Saturday and 4am Sunday. A warm/stationary west-east oriented front stayed south of Lake Erie, which allowed additional convection to develop downstream from the line of aforementioned thunderstorms. Despite the very fast moving storms, a moist atmosphere, persistent moisture advection with a strong low level jet, and training convection with efficient rainfall allowed for a wide area of minor flooding from Hancock County to Crawford, PA County where 1-2��� of rain was observed. The hardest hit area was Cuyahoga County where Big Creek and Cuyahoga River went into major flood stage and there were numerous reports of flash flooding. Multiple reports of flash flooding and water entering into basements across Parma from urban flooding and the Big Creek. The city of Parma ordered a do not travel advisory due to widespread flooding of roadways and a compromised bridge over the Big Creek. The Big Creek flooded portions of the Cleveland Zoo, which was closed at the time. Conditions noted which compound flood problems include restrictions generally by older bridges.|||USGS 412624081450700 East Branch Big Creek at Brooklyn reached a stage of 10.77 feet and flow of 3,120 cfs at 425 AM. ||USGS 04208502 Big Creek at Cleveland at 530 AM reached a stage of 12.03 feet with a flow of 5,240 cfs. At that stage flooding occurs in the Cleveland Zoo. This is approximately the flow of a 10 year flood.", "ts_dict_index": [1065, 1066, 1067]}
+{"event_id": 1116683, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 06:17:00", "end_date_time": "2023-08-21 11:00:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported Cameron Canyon Rd was closed between Tehachapi Willow Springs Rd. and SR 58 due to heavy debris covering the road.", "ts_dict_index": [1143, 1144, 1145]}
+{"event_id": 1116952, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 21:46:00", "end_date_time": "2023-08-21 03:46:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. Kern County officials reported a closure of Edison Hwy. from Bena Rd. to Towerline Rd. due to heavy flooding.", "ts_dict_index": [1152, 1153, 1154]}
+{"event_id": 1116950, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 21:11:00", "end_date_time": "2023-08-21 03:11:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported all lanes on SR 178 were blocked by heavy flooding entering the mouth of Kern Canyon.", "ts_dict_index": [1155, 1156, 1157]}
+{"event_id": 1116684, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 06:38:00", "end_date_time": "2023-08-21 11:00:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported flooding and debris in roadway completely covering the intersection of Oak Creek Rd. and CalPortland Access Rd.", "ts_dict_index": [1146, 1147, 1148]}
+{"event_id": 1116690, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 11:02:00", "end_date_time": "2023-08-20 14:02:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported several large rocks washed up on the Frazier Mountain Park onramp onto Interstate 5.", "ts_dict_index": [1149, 1150, 1151]}
+{"event_id": 1116691, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 11:56:00", "end_date_time": "2023-08-20 14:56:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported a large rock washed up on northbound Interstate 5 just south of the east escape ramp.", "ts_dict_index": [1119, 1120, 1121]}
+{"event_id": 1100858, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-07-06 19:15:00", "end_date_time": "2023-07-06 20:15:00", "narrative": "A weak upper level trough extended southwest from the Great Lakes Region southwest into Southwest Arkansas and Northeast Texas during the afternoon of July 6th, which reinforced a weak surface front south into the I-30 corridor of Northeast Texas and Southern Arkansas. Meanwhile, a strong seabreeze pushed inland across East Texas and North Louisiana during the late afternoon through the evening hours, allowing showers and thunderstorms to spread north into these areas. Strong daytime heating and large scale ascent along the slow moving front contributed to the development of scattered showers and thunderstorms along and south of the front across portions of East Texas and North Louisiana, and collided with the northward advancing storms associated with the seabreeze during the late afternoon and early evening hours, with a cluster of showers and thunderstorms redeveloping over the same areas from Harrison County Texas into Southern Caddo and Bossier Parishes in Northwest Louisiana. Given the very moist air mass in place, these slow moving storms were efficient rainfall producers, contributing to areas of flash flooding that were observed over these locations. Localized pockets of 2-5 inch rains fell over far South Shreveport and Southern Caddo Parish in a short period of time, with multiple roads flooded before the storms diminished by mid and late evening. Several cars stalled in high water in the Provenance neighborhood in extreme Southeast Shreveport. One business was also flooded in this area.", "ts_dict_index": [1170, 1171, 1172]}
+{"event_id": 824984, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-05-28 17:32:00", "end_date_time": "2019-05-28 20:30:00", "narrative": "Mid-level westerly flow of 45-70kts streamed over the Great Lakes/Upper Ohio Valley. A shortwave trough embedded within this zonal flow entered the region and moved eastward throughout the day, helping to provide forcing for ascent and strengthening of deep layer shear.  Mid-level westerly flow of 45 to 70 knots also streamed over the Great Lakes and the Upper Ohio Valley. Large hail was supported by mean layer CAPE of 1500 to 3000 J/kg and effective bulk shear of 35 to 50kts. Additionally, strong synoptic winds and steepening low-level lapse rates increased the severe wind threat.||With high precipitable water values of around 1.5 inches, training storms were also able to produce localized flooding.||The hail from this event was so severe that windows in homes broke and cars were damaged. A local car dealership said that from the time of the incident to the end of September they were booked with car repairs due to hail damage. Roughly, the damage from hail for this event cost at least 12 million dollars.||The town of Zelienople, PA was hit hard with rain, as a total of 4 to 5 inches accumulated in just a few hours. As a result, the Connoquenessing Creek rose throughout the night and crested at just over 15.3 feet on Wednesday morning, May 29th.  Based on historical crests, this was the 4th highest crest on record; records go back to the early 1920s. A 911 Call Center reported that the 1000 Block of Roupe Avenue was flooded. Rain also caused manhole covers to dislodge, as well as basement flooding.", "ts_dict_index": [1176, 1177, 1178]}
+{"event_id": 880285, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-04-22 19:21:00", "end_date_time": "2020-04-22 23:00:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well, particularly over portions of East Texas, North Louisiana, and Southeast Oklahoma. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Several roads were flooded and closed just south of Broken Bow. Report from mPING.", "ts_dict_index": [1179, 1180, 1181]}
+{"event_id": 1116932, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 18:24:00", "end_date_time": "2023-08-21 00:24:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported the roadway was completely flooded at the intersection of Piute Mountain Rd. and Kelso Valley Rd.", "ts_dict_index": [1158, 1159, 1160]}
+{"event_id": 1116947, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 20:55:00", "end_date_time": "2023-08-21 02:55:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported portions of southbound Interstate 5 from the Grapevine scales to Lebec were completely flooded.", "ts_dict_index": [1164, 1165, 1166]}
+{"event_id": 1116933, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 18:32:00", "end_date_time": "2023-08-21 00:32:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported the northbound lanes of SR 99 were completely flooded at the intersection of SR 99 and SR 166.", "ts_dict_index": [1161, 1162, 1163]}
+{"event_id": 1116700, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 16:46:00", "end_date_time": "2023-08-20 22:46:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. The Kern County Emergency Manager reported Copus Rd. was closed between Old River Rd. and Basic School Rd. due to heavy flooding.", "ts_dict_index": [1167, 1168, 1169]}
+{"event_id": 1116939, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 18:56:00", "end_date_time": "2023-08-21 06:56:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. The Ridgecrest Fire Department reported heavy flooding in a portion of Ridgecrest that resulted in an evacuation for areas bounded by West Ridgecrest Blvd, North Alvord St. West Las Flores Ave. and North China Lake Blvd. Other portions of Ridgecrest were impacted by soil erosion and instability resulting in heavy runoff.", "ts_dict_index": [1137, 1138, 1139]}
+{"event_id": 907283, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2020-08-12 10:20:00", "end_date_time": "2020-08-12 11:00:00", "narrative": "An upper level trough shifted southeast across Eastern Oklahoma and much of Arkansas during the early morning hours of August 12th, which helped to ignite scattered showers and thunderstorms over these areas. A weak inverted surface trough had developed along the Red River Valley of Southeast Oklahoma and extreme Northeast Texas, with a 25-30 kt southwesterly low level jet feeding near and atop this boundary along the base of the upper trough. As a result, a complex of showers and thunderstorms developed over Southwest Arkansas during the early morning hours, which slowly shifted south-southeast into extreme Southeast Oklahoma, Northeast Texas, and eventually into Northern Louisiana. Given the high moisture content within the atmosphere, these storms produced very heavy rainfall while moving repeatedly over the same areas, which resulted in flash flooding across portions of Southwest Arkansas where widespread rainfall amounts of 3-6+ inches fell. In fact, 7.89 inches of rain fell at an automated gauge in the Ben Lomond community in Southeast Sevier County, while 7.43 inches was recorded at the Texarkana Regional Airport in Miller County, which set a daily and August monthly rainfall record. This thunderstorm complex gradually weakened during the late morning and early afternoon hours. AR 360 north of Gin City was flooded.", "ts_dict_index": [1215, 1216, 1217]}
+{"event_id": 805127, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2019-01-17 09:30:00", "end_date_time": "2019-01-17 13:30:00", "narrative": "A high impact mini atmospheric river impacted Southern California January 14th and 15th which brought heavy rain and snow to the region. Seal Beach reported 2 inches of rain in 2 hours, which caused extensive flash flooding. Water was up to doorways outside of homes, and the Pacific Coast Highway was closed for over a day in Huntington Beach due to flooding. Rainfall rates remained below flash flood thresholds at the Holy and Cranston burn scars during this mini-AR event. Dense fog was reported in the Cajon Pass on the morning of January 16th, which resulted in a 19-car pileup and 35 patients with minor to moderate injuries. ||A larger atmospheric river moved into Southern California on January 17th, bringing heavy rain and snow to the region. Extensive flash flooding occurred due to the heavy rain. Swift water rescues occurred on the Santa Ana River in Riverside due to flooding. Rainfall rates exceeded flash flooding thresholds for the Holy fire burn scar on the 17th.||Overall, 6 to 12 inches of rain fell in the Santa Ana and San Bernardino County Mountains between January 14-17. Snowfall amounts in the mountains ranged from 4 to 12 inches above 6500 ft. Major surf and coastal flooding occurred during this event as well, which resulted in extensive damage of the Ocean Beach Pier in San Diego County. CalTrans reported Temescal Canyon Road at I-15 south closed due to flooding.", "ts_dict_index": [1206, 1207, 1208]}
+{"event_id": 805121, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2019-01-16 13:00:00", "end_date_time": "2019-01-16 15:00:00", "narrative": "A high impact mini atmospheric river impacted Southern California January 14th and 15th which brought heavy rain and snow to the region. Seal Beach reported 2 inches of rain in 2 hours, which caused extensive flash flooding. Water was up to doorways outside of homes, and the Pacific Coast Highway was closed for over a day in Huntington Beach due to flooding. Rainfall rates remained below flash flood thresholds at the Holy and Cranston burn scars during this mini-AR event. Dense fog was reported in the Cajon Pass on the morning of January 16th, which resulted in a 19-car pileup and 35 patients with minor to moderate injuries. ||A larger atmospheric river moved into Southern California on January 17th, bringing heavy rain and snow to the region. Extensive flash flooding occurred due to the heavy rain. Swift water rescues occurred on the Santa Ana River in Riverside due to flooding. Rainfall rates exceeded flash flooding thresholds for the Holy fire burn scar on the 17th.||Overall, 6 to 12 inches of rain fell in the Santa Ana and San Bernardino County Mountains between January 14-17. Snowfall amounts in the mountains ranged from 4 to 12 inches above 6500 ft. Major surf and coastal flooding occurred during this event as well, which resulted in extensive damage of the Ocean Beach Pier in San Diego County. Flash flooding from heavy rainfall over Holy fire scar in Trilogy parkway and Glen Eden with water going around homes.", "ts_dict_index": [1200, 1201, 1202]}
+{"event_id": 1113292, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-06-26 04:30:00", "end_date_time": "2023-06-26 07:30:00", "narrative": "Slow moving showers and thunderstorms associated with a broad area of low pressure moved across western Maine through the night of June 25th and into the morning of June 26th. Showers and thunderstorms repeatedly developed over the hills and mountains surrounding Andover and Byron in Oxford County, The extreme rainfall rates in hilly and mountainous terrain led to rapid run-off on multiple streams in the region. Maine. Localized heavy rain occurred in these areas with considerable flash flooding being reported. Showers and thunderstorms began in the Andover area around 2:30 am on June 26th.  The storms intensified and spread across the mountains in the surrounding towns to include Byron and Roxbury.  Rainfall rates peaked from 3:30 am to 6:00 am when the bulk of the heavy rainfall fell in the region.  The showers and thunderstorms weakened and moved off to the north with just very light rainfall through 8 am before ending.  Radar estimated rainfall amounts of 2 to 3��� in Bryon and Roxbury with even higher amounts of rain in North Andover. Radar estimated a very localized area of rainfall of up to 6��� of rainfall just north of town in mountainous terrain.   The bulk of this rainfall occurred in less than 3 hours.  The extreme rainfall rates in hilly and mountainous terrain led to rapid run-off on multiple streams in the region. Flash flooding occurred in Bryon on the morning of the 26th after 3 and 5 inches of rain fell along the south facing slopes of the Wyman Mountain. Garland Pond Road, Dingle Hill Road, #6 Road to Weld, Buckfield Hill Road, Lohnes Farm Road and Route 17 all sustained damage. Garland Pond Road, Dingle HIll Road and #6 Roads were not passable for more than 24 hours.", "ts_dict_index": [1185, 1186, 1187]}
+{"event_id": 1108946, "event_type": "Flash Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-06-26 03:10:00", "end_date_time": "2023-06-26 07:30:00", "narrative": "Slow moving showers and thunderstorms associated with a broad area of low pressure moved across western Maine through the night of June 25th and into the morning of June 26th. Showers and thunderstorms repeatedly developed over the hills and mountains surrounding Andover and Byron in Oxford County, The extreme rainfall rates in hilly and mountainous terrain led to rapid run-off on multiple streams in the region. Maine. Localized heavy rain occurred in these areas with considerable flash flooding being reported. Showers and thunderstorms began in the Andover area around 2:30 am on June 26th.  The storms intensified and spread across the mountains in the surrounding towns to include Byron and Roxbury.  Rainfall rates peaked from 3:30 am to 6:00 am when the bulk of the heavy rainfall fell in the region.  The showers and thunderstorms weakened and moved off to the north with just very light rainfall through 8 am before ending.  Radar estimated rainfall amounts of 2 to 3��� in Bryon and Roxbury with even higher amounts of rain in North Andover. Radar estimated a very localized area of rainfall of up to 6��� of rainfall just north of town in mountainous terrain.   The bulk of this rainfall occurred in less than 3 hours.  The extreme rainfall rates in hilly and mountainous terrain led to rapid run-off on multiple streams in the region. Considerable flash flooding occurred in Andover on the morning of the 26th after 3 and 6 inches of rain fell along the south facing slopes of the Wyman Mountain. Abbott Brook was redirected and severely impacted Wyman Hill Road and personal property along it. At one stretch along Wyman Hill Rd, Abbott Brook was diverted and is running directly down the middle of the road. More than a dozen residents were impacted, leaving people without road access. The main bridge at Wyman Hill Rd and Cross Rd was washed out. There was also one water rescue in Andover as a vehicle got stuck in the flood waters. The runoff caused the Ellis River to climb above flood stage cresting at 17.29 feet.||Additional roads in Andover that sustained washouts were East B Hill Road and South Arm Road. The major thruway of Route 120 was closed from Route 5 to Roxbury Pond Road due to flooding out of the Ellis River.", "ts_dict_index": [1182, 1183, 1184]}
+{"event_id": 907282, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2020-08-12 10:20:00", "end_date_time": "2020-08-12 11:00:00", "narrative": "An upper level trough shifted southeast across Eastern Oklahoma and much of Arkansas during the early morning hours of August 12th, which helped to ignite scattered showers and thunderstorms over these areas. A weak inverted surface trough had developed along the Red River Valley of Southeast Oklahoma and extreme Northeast Texas, with a 25-30 kt southwesterly low level jet feeding near and atop this boundary along the base of the upper trough. As a result, a complex of showers and thunderstorms developed over Southwest Arkansas during the early morning hours, which slowly shifted south-southeast into extreme Southeast Oklahoma, Northeast Texas, and eventually into Northern Louisiana. Given the high moisture content within the atmosphere, these storms produced very heavy rainfall while moving repeatedly over the same areas, which resulted in flash flooding across portions of Southwest Arkansas where widespread rainfall amounts of 3-6+ inches fell. In fact, 7.89 inches of rain fell at an automated gauge in the Ben Lomond community in Southeast Sevier County, while 7.43 inches was recorded at the Texarkana Regional Airport in Miller County, which set a daily and August monthly rainfall record. This thunderstorm complex gradually weakened during the late morning and early afternoon hours. Fullermill Road and Lafayette County Road 32 was flooded.", "ts_dict_index": [1218, 1219, 1220]}
+{"event_id": 907281, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2020-08-12 10:20:00", "end_date_time": "2020-08-12 11:00:00", "narrative": "An upper level trough shifted southeast across Eastern Oklahoma and much of Arkansas during the early morning hours of August 12th, which helped to ignite scattered showers and thunderstorms over these areas. A weak inverted surface trough had developed along the Red River Valley of Southeast Oklahoma and extreme Northeast Texas, with a 25-30 kt southwesterly low level jet feeding near and atop this boundary along the base of the upper trough. As a result, a complex of showers and thunderstorms developed over Southwest Arkansas during the early morning hours, which slowly shifted south-southeast into extreme Southeast Oklahoma, Northeast Texas, and eventually into Northern Louisiana. Given the high moisture content within the atmosphere, these storms produced very heavy rainfall while moving repeatedly over the same areas, which resulted in flash flooding across portions of Southwest Arkansas where widespread rainfall amounts of 3-6+ inches fell. In fact, 7.89 inches of rain fell at an automated gauge in the Ben Lomond community in Southeast Sevier County, while 7.43 inches was recorded at the Texarkana Regional Airport in Miller County, which set a daily and August monthly rainfall record. This thunderstorm complex gradually weakened during the late morning and early afternoon hours. AR 313 was flooded southeast of Lewisville.", "ts_dict_index": [1221, 1222, 1223]}
+{"event_id": 850965, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 13:30:00", "end_date_time": "2019-09-23 18:30:00", "narrative": "Copious amounts of tropical moisture spread north and into south-central Arizona during the morning hours on September 23rd, leading to widespread showers and thunderstorms. Some of the stronger storms generated intense rain with peak rain rates between 1 and 2 inches per hour. Storms and heavy persisted through the afternoon and into the evening and resulted in several episodes of flash flooding across the central deserts to the west and northwest of Phoenix. Multiple stream gauges from the Maricopa County Flood Control District indicated that washes and streams rapidly filled with water during flash flooding, easily exceeding their alarm or bankfull stages and causing the flooding of various roads and low water crossings. The reports were generally received from very open country. Additionally, at 1633MST Arizona Department of Highways reported that Eagle Eye Road 10 miles southeast of Gladden, in far northwest Maricopa County, became closed due to debris that washed over the road from the flash flooding. There were no reports of accidents or injuries due to the flash flooding. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Scattered to numerous showers and thunderstorms continued to develop across western Maricopa County during the afternoon hours on September 23rd and some of the storms produced intense rainfall with peak rain rates well in excess of 1 inch per hour. The very heavy rain led to flash flooding well to the west of Phoenix and near the La Paz County line during the late afternoon. According to the Arizona Department of Highways, at 1633MST flash flooding caused debris to flow across Eagle Eye Road and as a result the road was closed. This occurred roughly 10 miles to the southeast of Gladden and just to the east of the La Paz County line. Fortunately there were no accidents or injuries associated with the debris over the road. Although a Flash Flood Warning was in effect at the time, it was for an area to the east of where the flooding actually occurred.", "ts_dict_index": [1197, 1198, 1199]}
+{"event_id": 850964, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 19:20:00", "end_date_time": "2019-09-24 00:15:00", "narrative": "Copious amounts of tropical moisture spread north and into south-central Arizona during the morning hours on September 23rd, leading to widespread showers and thunderstorms. Some of the stronger storms generated intense rain with peak rain rates between 1 and 2 inches per hour. Storms and heavy persisted through the afternoon and into the evening and resulted in several episodes of flash flooding across the central deserts to the west and northwest of Phoenix. Multiple stream gauges from the Maricopa County Flood Control District indicated that washes and streams rapidly filled with water during flash flooding, easily exceeding their alarm or bankfull stages and causing the flooding of various roads and low water crossings. The reports were generally received from very open country. Additionally, at 1633MST Arizona Department of Highways reported that Eagle Eye Road 10 miles southeast of Gladden, in far northwest Maricopa County, became closed due to debris that washed over the road from the flash flooding. There were no reports of accidents or injuries due to the flash flooding. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Scattered to numerous showers and thunderstorms continued to develop across the central deserts to the west of Phoenix during the afternoon and early evening hours on September 23rd, and the stronger storms produced very heavy rain with peak rain rates well in excess of one inch per hour. The heavy rain led to an episode of flash flooding west of Phoenix near the town of Tonopah; at 2010MST mesonet data from a Maricopa County Flood Control District stream gauge indicated that flood waters rapidly climbed above alarm and bank full stages in the Delaney Wash. The gauge was located roughly 3 miles south of Tonopah. The flash flooding resulted in the road closures of the Salome Highway and the 411th Avenue Road crossing. A Flash Flood Warning was issued for the area prior to the report; no injuries were reported due to the flash flooding.", "ts_dict_index": [1194, 1195, 1196]}
+{"event_id": 850784, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 12:00:00", "end_date_time": "2019-09-23 16:40:00", "narrative": "Copious amounts of tropical moisture spread northward and into south-central Arizona during the morning hours on September 23rd. The moisture combined with a strong upper low west of Phoenix to generate widespread showers and thunderstorms. Many of the stronger storms produced intense rainfall with peak rain rates between one and two inches per hour. Initially the heavy rain led to episodes of flash flooding south and east of Phoenix, but by afternoon the flooding spread into areas north of Phoenix. Episodes of flash flooding occurred east of Interstate 17 and north of the Carefree Highway and impacted locations around the town of New River. At about 1300MST flash flooding caused a family in New River to be evacuated from their home. A few minutes later, flash flooding 7 miles west of Cave Creek necessitated a water rescue. Additionally, a stream gage in Skunk Creek 3 miles east of New River exceeded its alarm stage shortly after noon. Multiple Flash Flood Warnings were issued during the day and fortunately no injuries were reported due to the flooding. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Copious amounts of moisture spread north and into south-central Arizona during the morning hours on September 23rd, leading to the development of numerous showers and thunderstorms to the north of central Phoenix. Some of the stronger storms generated intense rain with peak rain rates approaching 2 inches per hour. The heavy rain led to episodes of flash flooding that occurred east of Interstate 17 and generally east of the town of New River. The flash flooding episodes took place during the early afternoon. At about 1230MST the Skunk Creek flood gauge 3 miles east of New River recorded at peak height of 5.01 feet which exceeded the alarm stage of 2.4 feet. At 1306MST, local broadcast media reported that flash flooding in New River caused a family to be evacuated from their home. Finally, at 1316MST, data from a Maricopa County Flood Control District gauge indicated that flash flooding was occurring along Cline Creek as rapidly rising water inundated various low water crossings in the area. The gauge was located roughly 4 miles southeast of New River. Multiple Flash Flood Warnings were issued for the area during the afternoon and were in effect during most of the flash flood reports. There were no reports of injuries due to flash flooding.", "ts_dict_index": [1209, 1210, 1211]}
+{"event_id": 850783, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 12:30:00", "end_date_time": "2019-09-23 16:40:00", "narrative": "Copious amounts of tropical moisture spread northward and into south-central Arizona during the morning hours on September 23rd. The moisture combined with a strong upper low west of Phoenix to generate widespread showers and thunderstorms. Many of the stronger storms produced intense rainfall with peak rain rates between one and two inches per hour. Initially the heavy rain led to episodes of flash flooding south and east of Phoenix, but by afternoon the flooding spread into areas north of Phoenix. Episodes of flash flooding occurred east of Interstate 17 and north of the Carefree Highway and impacted locations around the town of New River. At about 1300MST flash flooding caused a family in New River to be evacuated from their home. A few minutes later, flash flooding 7 miles west of Cave Creek necessitated a water rescue. Additionally, a stream gage in Skunk Creek 3 miles east of New River exceeded its alarm stage shortly after noon. Multiple Flash Flood Warnings were issued during the day and fortunately no injuries were reported due to the flooding. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Copious amounts of tropical moisture spread north and into south central Arizona during the morning hours on September 23rd, resulting in the development of numerous showers and thunderstorms. Some of the storms produced very heavy rain with peak rain rates approaching 2 inches per hour. The rain led to an episode of flash flooding to the north of Phoenix during the early afternoon. According to local broadcast media, at 1319MST flash flooding occurred near the intersection of Cloud Road and 7th street, about 7 miles west of Cave Creek and just a bit north of the Carefree Highway. The flooding necessitated a water rescue, fortunately no injuries were reported. A Flash Flood Warning was issued at 1304MST but for an area slightly north of where the water rescue was reported.", "ts_dict_index": [1212, 1213, 1214]}
+{"event_id": 850960, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 13:15:00", "end_date_time": "2019-09-23 18:30:00", "narrative": "Copious amounts of tropical moisture spread north and into south-central Arizona during the morning hours on September 23rd, leading to widespread showers and thunderstorms. Some of the stronger storms generated intense rain with peak rain rates between 1 and 2 inches per hour. Storms and heavy persisted through the afternoon and into the evening and resulted in several episodes of flash flooding across the central deserts to the west and northwest of Phoenix. Multiple stream gauges from the Maricopa County Flood Control District indicated that washes and streams rapidly filled with water during flash flooding, easily exceeding their alarm or bankfull stages and causing the flooding of various roads and low water crossings. The reports were generally received from very open country. Additionally, at 1633MST Arizona Department of Highways reported that Eagle Eye Road 10 miles southeast of Gladden, in far northwest Maricopa County, became closed due to debris that washed over the road from the flash flooding. There were no reports of accidents or injuries due to the flash flooding. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Scattered to numerous showers and thunderstorms developed across the northern and western portions of the greater Phoenix area during the late morning, and they continued into the afternoon. Some of the storms generated locally heavy rains with peak rain rates well in excess of one inch per hour. The heavy rains led to episodes of flash flooding, some of which occurred over rather open country such as the Hassayampa Plain well to the northwest of Phoenix. The flash flooding resulted in rapid rises in area washes, causing them to quickly exceed alarms stages. At 1348MST a flood control district stream gauge along Daggs Wash and West Peak View Road indicated that water quickly exceeded both alarm and bank full stages. The flash flooding resulted in quick inundation of area low water crossings. The gauge was located roughly 10 miles southwest of Circle City. A Flash Flood Warning was issued for the area at 1326MST and was in effect at the time of the flooding. No injuries were reported due to the flash flooding.", "ts_dict_index": [1191, 1192, 1193]}
+{"event_id": 850934, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 11:45:00", "end_date_time": "2019-09-23 15:40:00", "narrative": "Copious amounts of tropical moisture spread north and into south-central Arizona during the morning hours on September 23rd, leading to widespread showers and thunderstorms. Some of the stronger storms generated intense rain with peak rain rates between 1 and 2 inches per hour. Storms and heavy persisted through the afternoon and into the evening and resulted in several episodes of flash flooding across the central deserts to the west and northwest of Phoenix. Multiple stream gauges from the Maricopa County Flood Control District indicated that washes and streams rapidly filled with water during flash flooding, easily exceeding their alarm or bankfull stages and causing the flooding of various roads and low water crossings. The reports were generally received from very open country. Additionally, at 1633MST Arizona Department of Highways reported that Eagle Eye Road 10 miles southeast of Gladden, in far northwest Maricopa County, became closed due to debris that washed over the road from the flash flooding. There were no reports of accidents or injuries due to the flash flooding. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Scattered to numerous showers and thunderstorms continued to develop across the northern portions of the Phoenix area through late morning and into the afternoon hours on September 23rd, and some of the storms continued to produce very heavy rain with peak rain rates well in excess of one inch per hour. The heavy rain led to episodes of flash flooding, one of which occurred about 5 miles to the northeast of Wittmann and near Highway 74. According to data from the Picacho Wash Maricopa County Flood Control District stream gauge (ID #5678), rapidly rising waters exceeded the bank full flood levels, reaching a stage of 4.36 feet. Bank full stage was 4 feet. There were no reports of any accidents due to the flash flooding. A Flash Flood Warning was issued and was in effect at the time of the report.", "ts_dict_index": [1188, 1189, 1190]}
+{"event_id": 824981, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-05-28 18:30:00", "end_date_time": "2019-05-28 20:30:00", "narrative": "Mid-level westerly flow of 45-70kts streamed over the Great Lakes/Upper Ohio Valley. A shortwave trough embedded within this zonal flow entered the region and moved eastward throughout the day, helping to provide forcing for ascent and strengthening of deep layer shear.  Mid-level westerly flow of 45 to 70 knots also streamed over the Great Lakes and the Upper Ohio Valley. Large hail was supported by mean layer CAPE of 1500 to 3000 J/kg and effective bulk shear of 35 to 50kts. Additionally, strong synoptic winds and steepening low-level lapse rates increased the severe wind threat.||With high precipitable water values of around 1.5 inches, training storms were also able to produce localized flooding.||The hail from this event was so severe that windows in homes broke and cars were damaged. A local car dealership said that from the time of the incident to the end of September they were booked with car repairs due to hail damage. Roughly, the damage from hail for this event cost at least 12 million dollars.||The town of Zelienople, PA was hit hard with rain, as a total of 4 to 5 inches accumulated in just a few hours. As a result, the Connoquenessing Creek rose throughout the night and crested at just over 15.3 feet on Wednesday morning, May 29th.  Based on historical crests, this was the 4th highest crest on record; records go back to the early 1920s. A local 911 Call Center reported flooding at the intersection of Route 66 and Route 819 near Edgewood Washington Township.", "ts_dict_index": [1173, 1174, 1175]}
+{"event_id": 891298, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2020-06-21 22:00:00", "end_date_time": "2020-06-22 04:15:00", "narrative": "A mesoscale convective vortex (MCV) from a decayed area of showers and thunderstorms over Southeast Oklahoma drifted east into the northern sections of Southwest Arkansas during the afternoon and evening hours of June 21st, along a weak shortwave trough that drifted east across Western and Central Arkansas. A warm, moist, and unstable air mass lingered across Southwest Arkansas during the evening, with a modest southwesterly low level flow feeding additional low level moisture as large scale forcing increased ahead of the MCV. Thus, showers and thunderstorms quickly developed by mid and late evening on the 21st across the northern sections of Southwest Arkansas, and some of which became severe, producing hail and downing numerous trees and power lines across Hempstead County. As additional storms developed through the remainder of the evening into the early morning hours of the 22nd, locally heavy rainfall began to repeatedly move over the same areas of Hempstead and Nevada Counties, where widespread rainfall amounts of 3-6+ inches fell. Given the previously dry conditions over these areas during the preceding month, flash flooding was localized and confined to portions of Hempstead County, before the storms diminished and moved east into South-central Arkansas prior to daybreak. Several streets were flooded and closed in Hope.", "ts_dict_index": [1242, 1243, 1244]}
+{"event_id": 906866, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2020-08-12 05:00:00", "end_date_time": "2020-08-12 09:30:00", "narrative": "An upper level trough shifted southeast across Eastern Oklahoma and much of Arkansas during the early morning hours of August 12th, which helped to ignite scattered showers and thunderstorms over these areas. A weak inverted surface trough had developed along the Red River Valley of Southeast Oklahoma and extreme Northeast Texas, with a 25-30 kt southwesterly low level jet feeding near and atop this boundary along the base of the upper trough. As a result, a complex of showers and thunderstorms developed over Southwest Arkansas during the early morning hours, which slowly shifted south-southeast into extreme Southeast Oklahoma, Northeast Texas, and eventually into Northern Louisiana. Given the high moisture content within the atmosphere, these storms produced very heavy rainfall while moving repeatedly over the same areas, which resulted in flash flooding across portions of Southwest Arkansas where widespread rainfall amounts of 3-6+ inches fell. In fact, 7.89 inches of rain fell at an automated gauge in the Ben Lomond community in Southeast Sevier County, while 7.43 inches was recorded at the Texarkana Regional Airport in Miller County, which set a daily and August monthly rainfall record. This thunderstorm complex gradually weakened during the late morning and early afternoon hours. High water covered Highway 371 in Northwest Hempstead County near the Howard County line.", "ts_dict_index": [1224, 1225, 1226]}
+{"event_id": 809782, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2019-04-07 16:58:00", "end_date_time": "2019-04-08 00:30:00", "narrative": "A warm front mixed north across portions of Deep East Texas to near the Louisiana/Arkansas border during the early morning hours of April 7th, but steep lapse rates aloft and a shortwave trough which ejected northeast over Northeast Texas, North Louisiana, and Southern Arkansas enhanced the development of scattered elevated strong to severe thunderstorms across portions of East Texas, North Louisiana, and Southwest Arkansas near and north of the front. A report of small hail near El Dorado was received from these storms during the early morning hours prior to daybreak, with flash flooding developing across Southern Columbia and much of Union Counties as thunderstorms continued to develop and move repeatedly over these same areas for much of the day. Widespread rainfall amounts of four to nearly ten inches fell over these areas through much of the daytime and evening hours on April 7th. Additional strong thunderstorms developed later in the afternoon ahead of the primary upper level trough that lifted east out of Southwest New Mexico and across much of Central Texas and Louisiana, resulting in additional flash flooding over these same areas. These storms eventually diminished during the evening hours once the upper trough shifted east of the region into the Lower Mississippi Valley. Portions of Wesson Road and Pleasant Hill Road were covered in high water.", "ts_dict_index": [1236, 1237, 1238]}
+{"event_id": 809769, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2019-04-07 08:30:00", "end_date_time": "2019-04-07 18:30:00", "narrative": "A warm front mixed north across portions of Deep East Texas to near the Louisiana/Arkansas border during the early morning hours of April 7th, but steep lapse rates aloft and a shortwave trough which ejected northeast over Northeast Texas, North Louisiana, and Southern Arkansas enhanced the development of scattered elevated strong to severe thunderstorms across portions of East Texas, North Louisiana, and Southwest Arkansas near and north of the front. A report of small hail near El Dorado was received from these storms during the early morning hours prior to daybreak, with flash flooding developing across Southern Columbia and much of Union Counties as thunderstorms continued to develop and move repeatedly over these same areas for much of the day. Widespread rainfall amounts of four to nearly ten inches fell over these areas through much of the daytime and evening hours on April 7th. Additional strong thunderstorms developed later in the afternoon ahead of the primary upper level trough that lifted east out of Southwest New Mexico and across much of Central Texas and Louisiana, resulting in additional flash flooding over these same areas. These storms eventually diminished during the evening hours once the upper trough shifted east of the region into the Lower Mississippi Valley. A video posted to Facebook indicated that multiple roads were flooded in El Dorado.", "ts_dict_index": [1239, 1240, 1241]}
+{"event_id": 891297, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2020-06-21 22:15:00", "end_date_time": "2020-06-22 04:15:00", "narrative": "A mesoscale convective vortex (MCV) from a decayed area of showers and thunderstorms over Southeast Oklahoma drifted east into the northern sections of Southwest Arkansas during the afternoon and evening hours of June 21st, along a weak shortwave trough that drifted east across Western and Central Arkansas. A warm, moist, and unstable air mass lingered across Southwest Arkansas during the evening, with a modest southwesterly low level flow feeding additional low level moisture as large scale forcing increased ahead of the MCV. Thus, showers and thunderstorms quickly developed by mid and late evening on the 21st across the northern sections of Southwest Arkansas, and some of which became severe, producing hail and downing numerous trees and power lines across Hempstead County. As additional storms developed through the remainder of the evening into the early morning hours of the 22nd, locally heavy rainfall began to repeatedly move over the same areas of Hempstead and Nevada Counties, where widespread rainfall amounts of 3-6+ inches fell. Given the previously dry conditions over these areas during the preceding month, flash flooding was localized and confined to portions of Hempstead County, before the storms diminished and moved east into South-central Arkansas prior to daybreak. High water was reported over several roadways in and near Hope.", "ts_dict_index": [1245, 1246, 1247]}
+{"event_id": 809781, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2019-04-07 15:00:00", "end_date_time": "2019-04-08 00:30:00", "narrative": "A warm front mixed north across portions of Deep East Texas to near the Louisiana/Arkansas border during the early morning hours of April 7th, but steep lapse rates aloft and a shortwave trough which ejected northeast over Northeast Texas, North Louisiana, and Southern Arkansas enhanced the development of scattered elevated strong to severe thunderstorms across portions of East Texas, North Louisiana, and Southwest Arkansas near and north of the front. A report of small hail near El Dorado was received from these storms during the early morning hours prior to daybreak, with flash flooding developing across Southern Columbia and much of Union Counties as thunderstorms continued to develop and move repeatedly over these same areas for much of the day. Widespread rainfall amounts of four to nearly ten inches fell over these areas through much of the daytime and evening hours on April 7th. Additional strong thunderstorms developed later in the afternoon ahead of the primary upper level trough that lifted east out of Southwest New Mexico and across much of Central Texas and Louisiana, resulting in additional flash flooding over these same areas. These storms eventually diminished during the evening hours once the upper trough shifted east of the region into the Lower Mississippi Valley. Numerous streets were flooded across El Dorado. Report via social media.", "ts_dict_index": [1233, 1234, 1235]}
+{"event_id": 1140018, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-09-13 06:40:00", "end_date_time": "2023-09-13 08:40:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. The overflowing from Weekes Wash lead to several road closures in Apache Junction including: Tomahawk Rd. (4th Ave to Junction St.); 4th Ave. (Tomahawk Rd. to Cactus Rd.); Junction St. (Tomahawk Rd. to Wickiup Rd.); and Scenic St. (Vista Rd. to Wickiup Rd.). No damages nor injuries were reported.", "ts_dict_index": [1248, 1249, 1250]}
+{"event_id": 1056281, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2022-09-02 21:30:00", "end_date_time": "2022-09-02 23:30:00", "narrative": "Under a classic setup for storm motion from the Northern Arizona high terrain to Southern Arizona lower deserts, with the monsoon 500mb high positioned over Nevada and Utah, a few multicell storm clusters developed and progressed west-southwest through the lower deserts in the afternoon and evening hours of the 2nd. Increased east-northeast steering flow resulted in relatively high shear values for the monsoon (Sfc-6km shear around 25-30 kts) and very steep mid-level lapse rate (8-8.5 C/km) supported the organized multicellular storm mode with robust updrafts. Inversely, very high DCAPE values, up to 1500-1800 J/kg, supported very strong downbursts. Moisture levels were also above normal which, in combination with the strong updrafts, supported high rainfall rates (1.5-2 inches per hour average). There were a few multicell clusters that moved through Southern Arizona. One through the southeast parts of the greater Phoenix area, another that developed in Yavapai County before descending southwest along US-60 in Maricopa and La Paz Counties, and a third that developed off the Kofa Wilderness terrain south of Quartzsite before being caught by the cluster descending along US-60. Each cluster produced damaging winds, dense blowing dust, small to severe hail, and localized flash flooding. Flooding with water 3-4 feet deep was reported along US-95 about 14 miles south of Quartzsite. No damages or injuries were reported.", "ts_dict_index": [1230, 1231, 1232]}
+{"event_id": 805119, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2019-01-16 11:00:00", "end_date_time": "2019-01-16 14:00:00", "narrative": "A high impact mini atmospheric river impacted Southern California January 14th and 15th which brought heavy rain and snow to the region. Seal Beach reported 2 inches of rain in 2 hours, which caused extensive flash flooding. Water was up to doorways outside of homes, and the Pacific Coast Highway was closed for over a day in Huntington Beach due to flooding. Rainfall rates remained below flash flood thresholds at the Holy and Cranston burn scars during this mini-AR event. Dense fog was reported in the Cajon Pass on the morning of January 16th, which resulted in a 19-car pileup and 35 patients with minor to moderate injuries. ||A larger atmospheric river moved into Southern California on January 17th, bringing heavy rain and snow to the region. Extensive flash flooding occurred due to the heavy rain. Swift water rescues occurred on the Santa Ana River in Riverside due to flooding. Rainfall rates exceeded flash flooding thresholds for the Holy fire burn scar on the 17th.||Overall, 6 to 12 inches of rain fell in the Santa Ana and San Bernardino County Mountains between January 14-17. Snowfall amounts in the mountains ranged from 4 to 12 inches above 6500 ft. Major surf and coastal flooding occurred during this event as well, which resulted in extensive damage of the Ocean Beach Pier in San Diego County. Highway 60 had lane closures due to heavy rain bands of 0.50 to 0.75 per hour. Multiple swift water rescues on the Santa Ana River including helicopter extractions along Fleetwood and Via Ricardo.", "ts_dict_index": [1203, 1204, 1205]}
+{"event_id": 1046843, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 19:10:00", "end_date_time": "2022-07-30 20:10:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Photos showed flooding across Scottsdale Road near Deer Valley Road, making the road impassable. Police were on scene to prevent people from attempting to cross the flooded roadway. No damage or injuries were reported.", "ts_dict_index": [1275, 1276, 1277]}
+{"event_id": 1046878, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 20:19:00", "end_date_time": "2022-07-30 21:03:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Elevated flow in Skunk Creek led to the closure of a low water crossing along 19th Avenue between Desert Hills Drive and Irvine Road. A nearby FCDMC stream gage along Skunk Creek recorded a peak flow of 624 cfs and a peak height of 2.71 ft. No damage or injuries were reported.", "ts_dict_index": [1263, 1264, 1265]}
+{"event_id": 1140020, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2023-09-13 07:30:00", "end_date_time": "2023-09-13 10:30:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Spring Creek Wash in Roosevelt was running about 3 feet deep. No damages nor injuries were reported.", "ts_dict_index": [1254, 1255, 1256]}
+{"event_id": 1046924, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 19:20:00", "end_date_time": "2022-07-30 21:20:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. A video showed a car stalled in floodwaters over two feet deep near 7th Street and Hearn Road. No injuries were reported.", "ts_dict_index": [1260, 1261, 1262]}
+{"event_id": 1046835, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:50:00", "end_date_time": "2022-07-30 20:50:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Up to 3 ft of water and mud entered some first floor apartments at Central Avenue and Bell Road after the drainage system was overcome. Some cars in the parking lot of the apartment were also damaged. No injuries were reported.", "ts_dict_index": [1257, 1258, 1259]}
+{"event_id": 1140017, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-13 04:51:00", "end_date_time": "2023-09-13 06:51:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. State Route 88 between mileposts 229 and 242 southwest of Roosevelt Lake was closed due to flooding and rockslides, making the road impassable. No injuries were reported.", "ts_dict_index": [1251, 1252, 1253]}
+{"event_id": 1046869, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 19:50:00", "end_date_time": "2022-07-30 20:50:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Image showed stalled SUV in floodwaters at a low water crossing along Cloud Road between 7th Street and 10th Street. No injuries were reported.", "ts_dict_index": [1269, 1270, 1271]}
+{"event_id": 1047183, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:50:00", "end_date_time": "2022-07-30 19:50:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. A video showed approximately 1-2 ft of water flowing across the road near 12th Street and Hatcher Road. No damage or injuries were reported.", "ts_dict_index": [1278, 1279, 1280]}
+{"event_id": 1046907, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:47:00", "end_date_time": "2022-07-30 22:37:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. A video showed firefighters performing a swift water rescue after an SUV stalled in floodwaters when attempting to drive across a low water crossing along 7th Avenue between Greenway Parkway and Coral Gables Drive. At 1925MST, a nearby FCDMC stream gage exceeded bank full stage after recording a peak height of 8.07 ft and a peak flow of 5,080 cfs, which broke the record for this gage. No injuries were reported.", "ts_dict_index": [1272, 1273, 1274]}
+{"event_id": 1052212, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-02 19:50:00", "end_date_time": "2022-09-02 21:00:00", "narrative": "Under a classic setup for storm motion from the Northern Arizona high terrain to Southern Arizona lower deserts, with the monsoon 500mb high positioned over Nevada and Utah, a few multicell storm clusters developed and progressed west-southwest through the lower deserts in the afternoon and evening hours of the 2nd. Increased east-northeast steering flow resulted in relatively high shear values for the monsoon (Sfc-6km shear around 25-30 kts) and very steep mid-level lapse rate (8-8.5 C/km) supported the organized multicellular storm mode with robust updrafts. Inversely, very high DCAPE values, up to 1500-1800 J/kg, supported very strong downbursts. Moisture levels were also above normal which, in combination with the strong updrafts, supported high rainfall rates (1.5-2 inches per hour average). There were a few multicell clusters that moved through Southern Arizona. One through the southeast parts of the greater Phoenix area, another that developed in Yavapai County before descending southwest along US-60 in Maricopa and La Paz Counties, and a third that developed off the Kofa Wilderness terrain south of Quartzsite before being caught by the cluster descending along US-60. Each cluster produced damaging winds, dense blowing dust, small to severe hail, and localized flash flooding. Wickenburg Police Department reported Vulture Mine Road at Sols Wash was closed due to flooding. The road was reported closed at 2005MST, but flooding impacts likely began around 1950MST based on radar and an upstream streamflow gage. The streamflow gage is roughly 2 miles upstream and measured 1.69 inches in 1 hour ending at 1900MST. Streamflow exceeded alarm stage at 1930MST. The gage peaked at 4.10 feet and 4815 cfs at 2010MST. Flow fell back below alarm stage at 2100MST.  No damages or injuries were reported.", "ts_dict_index": [1227, 1228, 1229]}
+{"event_id": 880060, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-22 17:07:00", "end_date_time": "2020-04-22 19:30:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Youree Drive was flooded. Vehicles were stranded in high water. Report from mPING.", "ts_dict_index": [1308, 1309, 1310]}
+{"event_id": 1009371, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2022-03-22 03:00:00", "end_date_time": "2022-03-22 04:30:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. County Road 879 and AJ Nichols Road was impassible due to high water. County Road 979 just past County Road 486 was covered in swift moving water. Highway 204 near the power plant was partially covered in high water.", "ts_dict_index": [1323, 1324, 1325]}
+{"event_id": 823268, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-05-09 02:05:00", "end_date_time": "2019-05-09 04:00:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. Streets and parking lots were flooded in Bethany.", "ts_dict_index": [1311, 1312, 1313]}
+{"event_id": 1009372, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-03-21 23:30:00", "end_date_time": "2022-03-22 01:00:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. FM 724 west of Tyler was closed due to flooding.", "ts_dict_index": [1320, 1321, 1322]}
+{"event_id": 880247, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-22 15:00:00", "end_date_time": "2020-04-22 17:30:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. The southbound lane of Highway 259 was flooded.", "ts_dict_index": [1302, 1303, 1304]}
+{"event_id": 983653, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-16 22:30:00", "end_date_time": "2021-08-17 01:00:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Heavy rainfall over the Salt Fire burn area led to enhanced runoff that resulted in flash flooding. The Arizona Department of Transportation reported closures along SR 188 north of Globe/Claypool due to flooding. Timing was estimated using a nearby USGS stream gage along Pinal Creek at Inspiration Dam, which rose over 3 feet beginning at 2145MST and crested at 4.47 feet near midnight. No damage or injuries were reported.", "ts_dict_index": [1329, 1330, 1331]}
+{"event_id": 1046840, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 19:00:00", "end_date_time": "2022-07-30 20:00:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. A video on social media showed approximately 6-8 of water flowing south down 16th Street next to Buffalo Ridge Park. No damage or injuries were reported.", "ts_dict_index": [1281, 1282, 1283]}
+{"event_id": 983825, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:40:00", "end_date_time": "2021-08-17 03:00:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Sossaman Road and Via Del Jardin was closed at Sonoqui Wash due to flooding. A nearby Maricopa County Flood Control District stream gage near Hawes Road recorded flow in the wash climbing above alarm stage at around 2340MST. Flow in the wash continued to increase during the early morning hours on the 17th before cresting above bank full at 7.10 feet and 2237 CFS at 0010MST. Timing was estimated using the stream gage. No damage or injuries were reported.", "ts_dict_index": [1326, 1327, 1328]}
+{"event_id": 1047187, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 19:30:00", "end_date_time": "2022-07-30 21:30:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. A video showed Galloway Wash flowing over School House Road, making the road impassable. No damage or injuries were reported.", "ts_dict_index": [1293, 1294, 1295]}
+{"event_id": 1046863, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 19:34:00", "end_date_time": "2022-07-30 20:03:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. A FCDMC stream gage along Cave Creek climbed above alarm stage, peaking at 6.24 ft and 2,459 cfs at 1943MST.", "ts_dict_index": [1287, 1288, 1289]}
+{"event_id": 983867, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-17 06:30:00", "end_date_time": "2021-08-17 07:30:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Maricopa County Flood Control District stream gage ACDC at 43rd Avenue exceeded alarm stage resulting in downstream impacts at Thunderbird Paseo Park. Timing was estimated from when the gage reach alarm stage and time to travel downstream. No damage or injuries were reported.", "ts_dict_index": [1335, 1336, 1337]}
+{"event_id": 983869, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-17 08:00:00", "end_date_time": "2021-08-17 09:00:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. The City of Goodyear reported that Citrus Road was closed between I-10 and Van Buren Street as well as Yuma Road and Durango Street due to flooding. No damage or injuries were reported.", "ts_dict_index": [1332, 1333, 1334]}
+{"event_id": 1047138, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-07-30 17:42:00", "end_date_time": "2022-07-30 19:42:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. SR 238 westbound was closed at milepost 41 due to flooding. No damage or injuries were reported.", "ts_dict_index": [1296, 1297, 1298]}
+{"event_id": 1047193, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:53:00", "end_date_time": "2022-07-30 19:53:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Eagle Eye Road was closed between Salome Highway and US 60 due to flooding in multiple locations along the road. A FCDMC stream gage along Tiger Wash, which flows across an unbridged crossing along the road, briefly climbed above alarm stage after peaking at a height of 5.98 ft and a flow of 541 cfs. No damage or injuries were reported.", "ts_dict_index": [1299, 1300, 1301]}
+{"event_id": 1047134, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2022-07-30 17:30:00", "end_date_time": "2022-07-30 19:30:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Spring Creek was reported to be running approximately 8-9 ft in depth, impacting low water crossings through the creek. Over 2 of rain was reported to have fallen in the span of about an hour in this area. No damage or injuries were reported.", "ts_dict_index": [1290, 1291, 1292]}
+{"event_id": 1046838, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 19:00:00", "end_date_time": "2022-07-30 21:00:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. A video showed six cars stalled in floodwaters at the I-17 and Greenway Road underpass. No injuries were reported.", "ts_dict_index": [1284, 1285, 1286]}
+{"event_id": 809629, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2019-02-06 18:25:00", "end_date_time": "2019-02-06 18:25:00", "narrative": "Heavy rain and thunderstorms produced 2 tornadoes and widespread flash flooding across Middle Tennessee from the afternoon of February 6 through the early morning hours on February 7. A warm front that had moved northward into Kentucky early in the day on February 6 sank back southward to near the Interstate 40 corridor by the afternoon, sparking numerous showers and thunderstorms along and just north of the front. As the front effectively stalled in a west-to-east line along the Interstate 40 corridor, showers and storms continued to redevelop and move across the same areas. With rainfall rates approaching 1-2 per hour at times, this led to widespread flash flooding across Humphreys, Dickson, Cheatham, Davidson, Wilson, Smith, Jackson, Putnam, and Overton Counties. This flooding resulted in numerous closed roadways, dozens of water rescues, flooded homes and businesses, significant rises on area creeks and rivers, and unfortunately one fatality in Cheatham County. Total rainfall amounts ranged from 3 inches to nearly 7 inches across these counties. In addition to the flooding, thunderstorms produced two EF-0 tornadoes in Rutherford and Wilson Counties. Lightning also struck homes in Overton and Jackson counties, causing significant fire damage. Facebook photos showed significant flash flooding occurring on Highway 46 at Barbeque Road. Rushing water surrounded the Dickson Sportsman Store and Whitt's Barbeque, and Barbeque Road was closed due to flooding.", "ts_dict_index": [1314, 1315, 1316]}
+{"event_id": 1047136, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2022-07-30 17:30:00", "end_date_time": "2022-07-30 19:30:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Forest Service Road 396 was closed between Stagecoach Trail and the Eads Wash Day Use Site and River Access Point due to unsafe road conditions from flash flooding. No damage or injuries were reported.", "ts_dict_index": [1266, 1267, 1268]}
+{"event_id": 1145292, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-10-05 00:05:00", "end_date_time": "2023-10-05 03:15:00", "narrative": "A prolonged period of very heavy rainfall along with severe thunderstorms occurred on October 4th-5th across parts of Northeast Texas. Showers and thunderstorms with 1-3 inch per hour rainfall rates trained in the vicinity of a warm front, which was oriented across the Ark-La-Tex and in adjacent portions of Southeast Oklahoma and Northeast Louisiana. Deep convergence of moisture along the boundary resulted as the core of the low-level jet and associated moisture transport was directed due north from the Upper Texas coast. Other factors contributing to the heavy rainfall and severe storms included a sharp instability gradient with mean-layer CAPE values from 500-1500 J/kg, maximized precipitable water values from 2.0-2.2 inches and effective bulk shear of 25-30 knots. As a result, this area of Northeast Texas quickly became more favorable for increasing convective organization as multi-cell thunderstorms continued to train over the same areas from late morning throughout much of the afternoon and evening. Over time, flash flooding developed in areas impacted by 4-8 inch rainfall totals, most notably in and around the Texarkana metro area. Severe impacts from damaging wind gusts occurred farther south closer to the Interstate 20 corridor. High water reported near UT Tyler Health with several intersections flooded in the city of Tyler.", "ts_dict_index": [1347, 1348, 1349]}
+{"event_id": 878743, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2020-03-19 06:00:00", "end_date_time": "2020-03-19 06:45:00", "narrative": "Strong to severe thunderstorms developed over northwestern Texas and southwestern Oklahoma during the evening of the 18th. These storms moved northeast and affected portions of northeastern Oklahoma during the early morning hours of the 19th. Although instability had decreased ahead of these storms during the night-time hours, wind shear had strengthened significantly as these storms moved into northeast Oklahoma. As a result, one of these storms produced a tornado in Creek County. In addition, some of these thunderstorms moved repeatedly across the same areas, which resulted in locally heavy rainfall that combined with saturated soils, produced flash flooding. Another round of thunderstorms moved across northeastern Oklahoma later that morning. Another tornado developed with these thunderstorms, as well as locally damaging wind and flash flooding.||In addition to the flash flooding and severe weather, these multiple rounds of thunderstorms resulted in widespread heavy rainfall across northeastern Oklahoma. One to three inches fell across much of the area, with a heavier axis of three to six inches. This widespread heavy rainfall resulted in moderate flooding of the Caney and Neosho Rivers, and major flooding of the Illinois River. Horsepen Mobile Home Park was flooded by Horsepen Creek. Three swift water rescues were necessary.", "ts_dict_index": [1350, 1351, 1352]}
+{"event_id": 983868, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-17 07:30:00", "end_date_time": "2021-08-17 08:30:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Video on social media showed water rapidly flowing across 12th Street near the Torre Blanca community making the street impassable. No damage or injuries were reported.", "ts_dict_index": [1344, 1345, 1346]}
+{"event_id": 983866, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-17 05:15:00", "end_date_time": "2021-08-17 06:15:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Heavy rain flooded the underpass of I-17 at Greenway Road with at least one driver becoming stuck. No injuries were reported.", "ts_dict_index": [1338, 1339, 1340]}
+{"event_id": 880248, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-22 15:00:00", "end_date_time": "2020-04-22 17:30:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. North Street was flooded between Creek Bend Blvd to Pine Street.", "ts_dict_index": [1305, 1306, 1307]}
+{"event_id": 878746, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2020-03-19 06:30:00", "end_date_time": "2020-03-19 06:45:00", "narrative": "Strong to severe thunderstorms developed over northwestern Texas and southwestern Oklahoma during the evening of the 18th. These storms moved northeast and affected portions of northeastern Oklahoma during the early morning hours of the 19th. Although instability had decreased ahead of these storms during the night-time hours, wind shear had strengthened significantly as these storms moved into northeast Oklahoma. As a result, one of these storms produced a tornado in Creek County. In addition, some of these thunderstorms moved repeatedly across the same areas, which resulted in locally heavy rainfall that combined with saturated soils, produced flash flooding. Another round of thunderstorms moved across northeastern Oklahoma later that morning. Another tornado developed with these thunderstorms, as well as locally damaging wind and flash flooding.||In addition to the flash flooding and severe weather, these multiple rounds of thunderstorms resulted in widespread heavy rainfall across northeastern Oklahoma. One to three inches fell across much of the area, with a heavier axis of three to six inches. This widespread heavy rainfall resulted in moderate flooding of the Caney and Neosho Rivers, and major flooding of the Illinois River. Portions of Highway 20 were flooded between Collinsville and Skiatook.", "ts_dict_index": [1359, 1360, 1361]}
+{"event_id": 878752, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2020-03-19 09:38:00", "end_date_time": "2020-03-19 11:45:00", "narrative": "Strong to severe thunderstorms developed over northwestern Texas and southwestern Oklahoma during the evening of the 18th. These storms moved northeast and affected portions of northeastern Oklahoma during the early morning hours of the 19th. Although instability had decreased ahead of these storms during the night-time hours, wind shear had strengthened significantly as these storms moved into northeast Oklahoma. As a result, one of these storms produced a tornado in Creek County. In addition, some of these thunderstorms moved repeatedly across the same areas, which resulted in locally heavy rainfall that combined with saturated soils, produced flash flooding. Another round of thunderstorms moved across northeastern Oklahoma later that morning. Another tornado developed with these thunderstorms, as well as locally damaging wind and flash flooding.||In addition to the flash flooding and severe weather, these multiple rounds of thunderstorms resulted in widespread heavy rainfall across northeastern Oklahoma. One to three inches fell across much of the area, with a heavier axis of three to six inches. This widespread heavy rainfall resulted in moderate flooding of the Caney and Neosho Rivers, and major flooding of the Illinois River. Portions of several streets were flooded on the northwest side of Broken Arrow.", "ts_dict_index": [1356, 1357, 1358]}
+{"event_id": 1148434, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2023-08-23 19:40:00", "end_date_time": "2023-08-23 22:10:00", "narrative": "An anomalously-warm and moist air mass was in place across much of the Central Plains and Midwest, resulting in strong to perhaps extreme instability in addition to tropical-like precipitable water values exceeding 2.0 inches. The Lower Great Lakes region, specifically northern Ohio and Northwest Pennsylvania found itself on the eastern edge of this heat dome. Strong northwest flow aloft persisted along the periphery of the anomalously-warm and moist air mass, allowing for organized storms to develop across northern Ohio and Northwest Pennsylvania. A constant feed of moisture allowed these storms to maintain their intensity throughout the evening and overnight hours of Aug 23, 2023 and into the early morning hours of Aug 24, 2023 as they slowly pivoted southwest. Numerous flash flood warnings were issued with 3 considerable tags utilized throughout the course of the event. The hardest-hit areas were along the lakeshore between Toledo and Cleveland where there were several reports of 5 to 7 inches of rainfall. Elsewhere, generally 2 to 4 inches of rainfall was common, most of which fell in only a few hours. The area was on the edge of an extremely unstable airmass with sufficient deep-layer shear for organized convection. Flash flooding of area creeks/streams due to heavy rainfall. Road closures reported on Fairmount Boulevard near the Chagrin River and Bishop Road near East Branch Euclid Creek due to flooding. Radar estimated 2.25 to 3.25 inches of rainfall in a three hour period, much of which fell in 90 minutes or less.", "ts_dict_index": [1371, 1372, 1373]}
+{"event_id": 881438, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2020-03-19 10:50:00", "end_date_time": "2020-03-19 14:00:00", "narrative": "Strong to severe thunderstorms developed over northwestern Texas and southwestern Oklahoma during the evening of the 18th. These storms moved northeast and affected portions of northeastern Oklahoma during the early morning hours of the 19th. Although instability had decreased ahead of these storms during the night-time hours, wind shear had strengthened significantly as these storms moved into northeast Oklahoma. As a result, one of these storms produced a tornado in Creek County. In addition, some of these thunderstorms moved repeatedly across the same areas, which resulted in locally heavy rainfall that combined with saturated soils, produced flash flooding. Another round of thunderstorms moved across northeastern Oklahoma later that morning. Another tornado developed with these thunderstorms, as well as locally damaging wind and flash flooding.||In addition to the flash flooding and severe weather, these multiple rounds of thunderstorms resulted in widespread heavy rainfall across northeastern Oklahoma. One to three inches fell across much of the area, with a heavier axis of three to six inches. This widespread heavy rainfall resulted in moderate flooding of the Caney and Neosho Rivers, and major flooding of the Illinois River. Streets were flooded around W 81st Street S and S Elwood Avenue.", "ts_dict_index": [1353, 1354, 1355]}
+{"event_id": 1148450, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2023-08-23 20:15:00", "end_date_time": "2023-08-23 22:40:00", "narrative": "An anomalously-warm and moist air mass was in place across much of the Central Plains and Midwest, resulting in strong to perhaps extreme instability in addition to tropical-like precipitable water values exceeding 2.0 inches. The Lower Great Lakes region, specifically northern Ohio and Northwest Pennsylvania found itself on the eastern edge of this heat dome. Strong northwest flow aloft persisted along the periphery of the anomalously-warm and moist air mass, allowing for organized storms to develop across northern Ohio and Northwest Pennsylvania. A constant feed of moisture allowed these storms to maintain their intensity throughout the evening and overnight hours of Aug 23, 2023 and into the early morning hours of Aug 24, 2023 as they slowly pivoted southwest. Numerous flash flood warnings were issued with 3 considerable tags utilized throughout the course of the event. The hardest-hit areas were along the lakeshore between Toledo and Cleveland where there were several reports of 5 to 7 inches of rainfall. Elsewhere, generally 2 to 4 inches of rainfall was common, most of which fell in only a few hours. The area was on the edge of an extremely unstable airmass with sufficient deep-layer shear for organized convection. Extensive flash flooding in North Olmsted, Brooklyn, Brook Park, Parma, and Parma Heights. Widespread basement flooding and road closures. Several underpasses under I-480 inundated with flood waters. A structure collapse was reported in North Olmsted due to the weight of water on the roof. Flooded roadways include Brookpark Road, West Ridgewood Drive, Pleasant Valley Road near York Road, and Sprague Road near West 130th Street. Multiple water rescues reported in this area. Cleveland Metroparks Zoo experienced flood damage due to flooding of Big Creek. The USGS river gage near the zoo on Big Creek rose from 3.8 feet to 12.8 feet in 70 minutes before the gage was knocked out of service by a fallen tree. Radar estimated 1.5 to 2.25 inches of rainfall in less than three hours, with much of the rainfall falling in less than one hour.", "ts_dict_index": [1377, 1378, 1379]}
+{"event_id": 1148449, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2023-08-23 20:15:00", "end_date_time": "2023-08-23 22:30:00", "narrative": "An anomalously-warm and moist air mass was in place across much of the Central Plains and Midwest, resulting in strong to perhaps extreme instability in addition to tropical-like precipitable water values exceeding 2.0 inches. The Lower Great Lakes region, specifically northern Ohio and Northwest Pennsylvania found itself on the eastern edge of this heat dome. Strong northwest flow aloft persisted along the periphery of the anomalously-warm and moist air mass, allowing for organized storms to develop across northern Ohio and Northwest Pennsylvania. A constant feed of moisture allowed these storms to maintain their intensity throughout the evening and overnight hours of Aug 23, 2023 and into the early morning hours of Aug 24, 2023 as they slowly pivoted southwest. Numerous flash flood warnings were issued with 3 considerable tags utilized throughout the course of the event. The hardest-hit areas were along the lakeshore between Toledo and Cleveland where there were several reports of 5 to 7 inches of rainfall. Elsewhere, generally 2 to 4 inches of rainfall was common, most of which fell in only a few hours. The area was on the edge of an extremely unstable airmass with sufficient deep-layer shear for organized convection. Multiple road closures in and around Solon due to flash flooding. Road closures include US-422 at Brainard Road and Bainbridge Road near Harper Road. Radar estimated 1.75 to 2.25 inches of rainfall in a three hour period, with most of the rain falling in a 60 to 90 minute period.", "ts_dict_index": [1380, 1381, 1382]}
+{"event_id": 811367, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2019-02-23 20:06:00", "end_date_time": "2019-02-23 21:06:00", "narrative": "A stationary frontal boundary stalled near the Tennessee Valley for nearly a week in mid to late February 2019. Persistent southwest flow aloft brought copious amounts of Gulf of Mexico moisture northward and interacted with this boundary for many days, causing a prolonged period of heavy rain and flooding throughout Middle Tennessee from Tuesday, February 19 through early Sunday, February 24. Due to the heavy rainfall that had already fallen earlier in the month along with the already unusually wet winter season so far, widespread flash flooding and river flooding resulted, with dozens of water rescues being conducted and numerous homes and businesses flooded. This flood event was considered the worst in Middle Tennessee since the historic flood of May 2010, and damage from the flash flooding and river flooding resulted in a Presidential Disaster Declaration being declared for many Middle Tennessee counties on April 17, 2019. In addition, the heavy rainfall throughout February 2019 set new monthly rainfall records at many locations, including Nashville and Crossville, both of which saw over a foot of rain. By the end of the month, nearly the entire state of Tennessee had received between 10 and 20 of rain for February 2019. Widespread flooding continued across northern Dickson County in the Cumberland Furnace and Charlotte areas, with Highway 48N at St. Paul Road flooded and closed. Water rescues were also ongoing in the Dry Hollow area.", "ts_dict_index": [1368, 1369, 1370]}
+{"event_id": 811294, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2019-02-23 10:30:00", "end_date_time": "2019-02-23 12:30:00", "narrative": "A stationary frontal boundary stalled near the Tennessee Valley for nearly a week in mid to late February 2019. Persistent southwest flow aloft brought copious amounts of Gulf of Mexico moisture northward and interacted with this boundary for many days, causing a prolonged period of heavy rain and flooding throughout Middle Tennessee from Tuesday, February 19 through early Sunday, February 24. Due to the heavy rainfall that had already fallen earlier in the month along with the already unusually wet winter season so far, widespread flash flooding and river flooding resulted, with dozens of water rescues being conducted and numerous homes and businesses flooded. This flood event was considered the worst in Middle Tennessee since the historic flood of May 2010, and damage from the flash flooding and river flooding resulted in a Presidential Disaster Declaration being declared for many Middle Tennessee counties on April 17, 2019. In addition, the heavy rainfall throughout February 2019 set new monthly rainfall records at many locations, including Nashville and Crossville, both of which saw over a foot of rain. By the end of the month, nearly the entire state of Tennessee had received between 10 and 20 of rain for February 2019. Several secondary roads were flooded and impassable across southern Dickson County.", "ts_dict_index": [1365, 1366, 1367]}
+{"event_id": 811304, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2019-02-23 16:29:00", "end_date_time": "2019-02-23 18:29:00", "narrative": "A stationary frontal boundary stalled near the Tennessee Valley for nearly a week in mid to late February 2019. Persistent southwest flow aloft brought copious amounts of Gulf of Mexico moisture northward and interacted with this boundary for many days, causing a prolonged period of heavy rain and flooding throughout Middle Tennessee from Tuesday, February 19 through early Sunday, February 24. Due to the heavy rainfall that had already fallen earlier in the month along with the already unusually wet winter season so far, widespread flash flooding and river flooding resulted, with dozens of water rescues being conducted and numerous homes and businesses flooded. This flood event was considered the worst in Middle Tennessee since the historic flood of May 2010, and damage from the flash flooding and river flooding resulted in a Presidential Disaster Declaration being declared for many Middle Tennessee counties on April 17, 2019. In addition, the heavy rainfall throughout February 2019 set new monthly rainfall records at many locations, including Nashville and Crossville, both of which saw over a foot of rain. By the end of the month, nearly the entire state of Tennessee had received between 10 and 20 of rain for February 2019. Several main highways were flooded and closed across northern Dickson County, including Highway 49W at Bartons Creek, Highway 48 near Woods Valley, and Highway 48N at Sulphur Creek just south of Charlotte. Multiple water rescues were also conducted.", "ts_dict_index": [1362, 1363, 1364]}
+{"event_id": 810109, "event_type": "Flash Flood", "state": "TENNESSEE", "cz_name": "DICKSON", "begin_date_time": "2019-02-06 21:45:00", "end_date_time": "2019-02-07 00:00:00", "narrative": "Heavy rain and thunderstorms produced 2 tornadoes and widespread flash flooding across Middle Tennessee from the afternoon of February 6 through the early morning hours on February 7. A warm front that had moved northward into Kentucky early in the day on February 6 sank back southward to near the Interstate 40 corridor by the afternoon, sparking numerous showers and thunderstorms along and just north of the front. As the front effectively stalled in a west-to-east line along the Interstate 40 corridor, showers and storms continued to redevelop and move across the same areas. With rainfall rates approaching 1-2 per hour at times, this led to widespread flash flooding across Humphreys, Dickson, Cheatham, Davidson, Wilson, Smith, Jackson, Putnam, and Overton Counties. This flooding resulted in numerous closed roadways, dozens of water rescues, flooded homes and businesses, significant rises on area creeks and rivers, and unfortunately one fatality in Cheatham County. Total rainfall amounts ranged from 3 inches to nearly 7 inches across these counties. In addition to the flooding, thunderstorms produced two EF-0 tornadoes in Rutherford and Wilson Counties. Lightning also struck homes in Overton and Jackson counties, causing significant fire damage. Dickson County Emergency Management reported major flash flooding affected central and southern portions of Dickson County. Several roads and bridges were washed out including bridges on Coon Creek Road and on Willow Branch Road at Liberty Road near Charlotte. Numerous other roads were flooded and closed including Shady Hollow Road between College Street and Luther Road in Dickson. Vehicles were stranded in flooding in some areas with water rescues conducted, including on Eno Road and on Harris Road near Tennessee City. Total damage from the flash flooding was estimated at $1,329,000.", "ts_dict_index": [1317, 1318, 1319]}
+{"event_id": 975964, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-17 19:45:00", "end_date_time": "2021-07-17 21:00:00", "narrative": "During the evening of July 17th an area of low pressure slowly moved east along a stationary boundary that stretched from New York to Massachusetts.  The front briefly lifted northward into southern New Hampshire pulling ample moisture with precipitable water values over 2 inches, anomalously high, even for July.  Additionally, much of this region had seen 300%+ of average rainfall over the preceding few weeks. This caused soil moisture values and streamflow conditions to be well above average.  Multiple rounds of heavy rainfall produced significant flash flooding in southern New Hampshire. Reports to the weather service included totals of nearly 7 inches of rain in Jaffrey, 5 inches in Marlborough and Swanzey, and between 2 and 3 inches in Chesterfield. ||Severe flooding prompted numerous local emergency operations centers to open, and washed out road infrastructure in 14 communities in the Monadnock Region. Early estimates from state and local damages verified at over $2 million from the storm.  Cheshire County alone met the entire state indicator threshold to request a declaration of disaster for New Hampshire. Communities that sustained the most damage include Jaffrey, Keene, Richmond, and Fitzwilliam. Heavy rained washed out NH Route 124 by the town garage. Maple Lane was completely washed out and needed a temporary bridge due to approximately 25 residents being stranded. The first round of rainfall came around 8 PM EDT dropping close to 3 inches. This was followed by a second round of heavy rain shortly before midnight. The area recorded 5.5 over a 12 hour period.", "ts_dict_index": [1395, 1396, 1397]}
+{"event_id": 975657, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-17 23:32:00", "end_date_time": "2021-07-18 02:00:00", "narrative": "During the evening of July 17th an area of low pressure slowly moved east along a stationary boundary that stretched from New York to Massachusetts.  The front briefly lifted northward into southern New Hampshire pulling ample moisture with precipitable water values over 2 inches, anomalously high, even for July.  Additionally, much of this region had seen 300%+ of average rainfall over the preceding few weeks. This caused soil moisture values and streamflow conditions to be well above average.  Multiple rounds of heavy rainfall produced significant flash flooding in southern New Hampshire. Reports to the weather service included totals of nearly 7 inches of rain in Jaffrey, 5 inches in Marlborough and Swanzey, and between 2 and 3 inches in Chesterfield. ||Severe flooding prompted numerous local emergency operations centers to open, and washed out road infrastructure in 14 communities in the Monadnock Region. Early estimates from state and local damages verified at over $2 million from the storm.  Cheshire County alone met the entire state indicator threshold to request a declaration of disaster for New Hampshire. Communities that sustained the most damage include Jaffrey, Keene, Richmond, and Fitzwilliam. Multiple roads washed out. Scott Pond Road, Warren Hill Rd, Royalston Rd, Sandy Hollow Rd, Rhododendron Rd, Old Coach Road, Lower Templeton Tpke.  Nearby rain gages reported between 4 to 6 inches of rainfall, with the heaviest rain shortly after midnight.", "ts_dict_index": [1407, 1408, 1409]}
+{"event_id": 975970, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-17 19:30:00", "end_date_time": "2021-07-17 21:00:00", "narrative": "During the evening of July 17th an area of low pressure slowly moved east along a stationary boundary that stretched from New York to Massachusetts.  The front briefly lifted northward into southern New Hampshire pulling ample moisture with precipitable water values over 2 inches, anomalously high, even for July.  Additionally, much of this region had seen 300%+ of average rainfall over the preceding few weeks. This caused soil moisture values and streamflow conditions to be well above average.  Multiple rounds of heavy rainfall produced significant flash flooding in southern New Hampshire. Reports to the weather service included totals of nearly 7 inches of rain in Jaffrey, 5 inches in Marlborough and Swanzey, and between 2 and 3 inches in Chesterfield. ||Severe flooding prompted numerous local emergency operations centers to open, and washed out road infrastructure in 14 communities in the Monadnock Region. Early estimates from state and local damages verified at over $2 million from the storm.  Cheshire County alone met the entire state indicator threshold to request a declaration of disaster for New Hampshire. Communities that sustained the most damage include Jaffrey, Keene, Richmond, and Fitzwilliam. Erosion along several local roads, primarily shoulders and pavement damage. Majority of the damage occurred in the evening.", "ts_dict_index": [1386, 1387, 1388]}
+{"event_id": 975663, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-17 20:17:00", "end_date_time": "2021-07-17 21:30:00", "narrative": "During the evening of July 17th an area of low pressure slowly moved east along a stationary boundary that stretched from New York to Massachusetts.  The front briefly lifted northward into southern New Hampshire pulling ample moisture with precipitable water values over 2 inches, anomalously high, even for July.  Additionally, much of this region had seen 300%+ of average rainfall over the preceding few weeks. This caused soil moisture values and streamflow conditions to be well above average.  Multiple rounds of heavy rainfall produced significant flash flooding in southern New Hampshire. Reports to the weather service included totals of nearly 7 inches of rain in Jaffrey, 5 inches in Marlborough and Swanzey, and between 2 and 3 inches in Chesterfield. ||Severe flooding prompted numerous local emergency operations centers to open, and washed out road infrastructure in 14 communities in the Monadnock Region. Early estimates from state and local damages verified at over $2 million from the storm.  Cheshire County alone met the entire state indicator threshold to request a declaration of disaster for New Hampshire. Communities that sustained the most damage include Jaffrey, Keene, Richmond, and Fitzwilliam. Law Enforcement reported that a portion of Roxbury Street in Keene was washed out due to flash flooding.", "ts_dict_index": [1404, 1405, 1406]}
+{"event_id": 975968, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-17 21:30:00", "end_date_time": "2021-07-17 22:45:00", "narrative": "During the evening of July 17th an area of low pressure slowly moved east along a stationary boundary that stretched from New York to Massachusetts.  The front briefly lifted northward into southern New Hampshire pulling ample moisture with precipitable water values over 2 inches, anomalously high, even for July.  Additionally, much of this region had seen 300%+ of average rainfall over the preceding few weeks. This caused soil moisture values and streamflow conditions to be well above average.  Multiple rounds of heavy rainfall produced significant flash flooding in southern New Hampshire. Reports to the weather service included totals of nearly 7 inches of rain in Jaffrey, 5 inches in Marlborough and Swanzey, and between 2 and 3 inches in Chesterfield. ||Severe flooding prompted numerous local emergency operations centers to open, and washed out road infrastructure in 14 communities in the Monadnock Region. Early estimates from state and local damages verified at over $2 million from the storm.  Cheshire County alone met the entire state indicator threshold to request a declaration of disaster for New Hampshire. Communities that sustained the most damage include Jaffrey, Keene, Richmond, and Fitzwilliam. Multiple roads washed out including South Street, Quarry Rd, West Hill Rd, Prospect Rd, and Brook Rd. Perkins Pond dam was overtopping near Monadnock St and Sand Dam.", "ts_dict_index": [1383, 1384, 1385]}
+{"event_id": 975965, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-17 20:00:00", "end_date_time": "2021-07-17 21:30:00", "narrative": "During the evening of July 17th an area of low pressure slowly moved east along a stationary boundary that stretched from New York to Massachusetts.  The front briefly lifted northward into southern New Hampshire pulling ample moisture with precipitable water values over 2 inches, anomalously high, even for July.  Additionally, much of this region had seen 300%+ of average rainfall over the preceding few weeks. This caused soil moisture values and streamflow conditions to be well above average.  Multiple rounds of heavy rainfall produced significant flash flooding in southern New Hampshire. Reports to the weather service included totals of nearly 7 inches of rain in Jaffrey, 5 inches in Marlborough and Swanzey, and between 2 and 3 inches in Chesterfield. ||Severe flooding prompted numerous local emergency operations centers to open, and washed out road infrastructure in 14 communities in the Monadnock Region. Early estimates from state and local damages verified at over $2 million from the storm.  Cheshire County alone met the entire state indicator threshold to request a declaration of disaster for New Hampshire. Communities that sustained the most damage include Jaffrey, Keene, Richmond, and Fitzwilliam. Significant damage with multiple road washouts. Scott Pond Road was completely washed away where the causeway crossed over a pond.  This road damage caused 12 homes to be isolated.", "ts_dict_index": [1398, 1399, 1400]}
+{"event_id": 975655, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-18 01:00:00", "end_date_time": "2021-07-18 02:35:00", "narrative": "During the evening of July 17th an area of low pressure slowly moved east along a stationary boundary that stretched from New York to Massachusetts.  The front briefly lifted northward into southern New Hampshire pulling ample moisture with precipitable water values over 2 inches, anomalously high, even for July.  Additionally, much of this region had seen 300%+ of average rainfall over the preceding few weeks. This caused soil moisture values and streamflow conditions to be well above average.  Multiple rounds of heavy rainfall produced significant flash flooding in southern New Hampshire. Reports to the weather service included totals of nearly 7 inches of rain in Jaffrey, 5 inches in Marlborough and Swanzey, and between 2 and 3 inches in Chesterfield. ||Severe flooding prompted numerous local emergency operations centers to open, and washed out road infrastructure in 14 communities in the Monadnock Region. Early estimates from state and local damages verified at over $2 million from the storm.  Cheshire County alone met the entire state indicator threshold to request a declaration of disaster for New Hampshire. Communities that sustained the most damage include Jaffrey, Keene, Richmond, and Fitzwilliam. The town of Richmond sustained over $200,000 in verified damage. Flooding with washouts on following roads: Fish Hatchery Rd, Tully Brook Rd, Honey Hill Rd, and NH Route 32 north of four corners. No rain reports were located in Richmond, but neighboring gages reported between 4 and 6 inches of rainfall within a 12 hour period. The heaviest rain came shortly after midnight with rates over 3 inches an hour.", "ts_dict_index": [1392, 1393, 1394]}
+{"event_id": 1134209, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2023-07-20 18:40:00", "end_date_time": "2023-07-20 20:30:00", "narrative": "A surface low moved generally eastward from east-central Lower MI to the southeastern shore of Lake Huron during the evening of the 20th. Simultaneously, the low's warm front swept northeastward across southern ON and western NY toward the northern shore of Lake Ontario as the low's trailing cold front moved generally eastward across southeastern Lower MI and far-northeastern IN to central Lake Erie and northeastern OH.||Multiple lines and clusters of multicell thunderstorms persisted generally eastward and southeastward across northern OH during the early through mid-evening hours of the 20th and produced sporadic severe hail and straight-line convective wind damage as the storms encountered moderate to strong MUCAPE and effective bulk shear, respectively, within the warm sector. An embedded supercell produced large hail in Westlake, a western suburb of Cleveland. Although the thunderstorms moved progressively across the area, the thunderstorms produced torrential rainfall across Cuyahoga County, with instantaneous rainfall rates of 4 to 5 inches per hour and rainfall totals of 1.75 to 2.5 inches in a period of one hour or less. The torrential rainfall resulted in instances of flash flooding. Flash flooding across the western suburbs of Cleveland, including Bay Village, North Olmsted, Fairview Park, Rocky River and Lakewood. Notable road closures due to flooding include I-90 East near McKinley Avenue and West 117th Avenue between Berea Road and Detroit Avenue in Lakewood, West 130th Street and Bellaire Road and West 150th Street north of Brookpark Road in Cleveland. Great Northern Avenue north of Brookpark Road was flooded with several feet of standing water in North Olmsted. Extensive basement flooding reported, including between 1 to 2 dozen basements in Bay Village and 175 basements in Fairview Park.", "ts_dict_index": [1413, 1414, 1415]}
+{"event_id": 975654, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-17 23:45:00", "end_date_time": "2021-07-18 02:00:00", "narrative": "During the evening of July 17th an area of low pressure slowly moved east along a stationary boundary that stretched from New York to Massachusetts.  The front briefly lifted northward into southern New Hampshire pulling ample moisture with precipitable water values over 2 inches, anomalously high, even for July.  Additionally, much of this region had seen 300%+ of average rainfall over the preceding few weeks. This caused soil moisture values and streamflow conditions to be well above average.  Multiple rounds of heavy rainfall produced significant flash flooding in southern New Hampshire. Reports to the weather service included totals of nearly 7 inches of rain in Jaffrey, 5 inches in Marlborough and Swanzey, and between 2 and 3 inches in Chesterfield. ||Severe flooding prompted numerous local emergency operations centers to open, and washed out road infrastructure in 14 communities in the Monadnock Region. Early estimates from state and local damages verified at over $2 million from the storm.  Cheshire County alone met the entire state indicator threshold to request a declaration of disaster for New Hampshire. Communities that sustained the most damage include Jaffrey, Keene, Richmond, and Fitzwilliam. Jaffrey airport reported 6.9 in 18 hours, measuring 6 to 8 inches of rain in 24 hours. More than 15 roads were washed out, one of which lost a major culvert. Damage figures were estimated over $1 million mainly for damage to roads and bridges.  There was a voluntary evacuation for 39 homes on Letourneau Drive off Nutting Road after a bridge was flooded by a small stream.", "ts_dict_index": [1410, 1411, 1412]}
+{"event_id": 975666, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-17 23:25:00", "end_date_time": "2021-07-18 02:00:00", "narrative": "During the evening of July 17th an area of low pressure slowly moved east along a stationary boundary that stretched from New York to Massachusetts.  The front briefly lifted northward into southern New Hampshire pulling ample moisture with precipitable water values over 2 inches, anomalously high, even for July.  Additionally, much of this region had seen 300%+ of average rainfall over the preceding few weeks. This caused soil moisture values and streamflow conditions to be well above average.  Multiple rounds of heavy rainfall produced significant flash flooding in southern New Hampshire. Reports to the weather service included totals of nearly 7 inches of rain in Jaffrey, 5 inches in Marlborough and Swanzey, and between 2 and 3 inches in Chesterfield. ||Severe flooding prompted numerous local emergency operations centers to open, and washed out road infrastructure in 14 communities in the Monadnock Region. Early estimates from state and local damages verified at over $2 million from the storm.  Cheshire County alone met the entire state indicator threshold to request a declaration of disaster for New Hampshire. Communities that sustained the most damage include Jaffrey, Keene, Richmond, and Fitzwilliam. Two rounds of heavy rain impacted Keene on the evening of the 17th. The first round came around 9 PM causing some localized flash flooding. Shortly after midnight another round of heavy rainfall moved over the area resulting in another surge of floodwaters into the city. In all, over 80 residential basements flooded along with several businesses. A large sinkhole developed on Roxbury Street with severe damage. There were at least 2 evacuations, one on Wetmore Street and another at Boston Place.", "ts_dict_index": [1401, 1402, 1403]}
+{"event_id": 983865, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-17 00:11:00", "end_date_time": "2021-08-17 01:11:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. The Arizona Department of Transportation reported that SR 87 was closed due to flooding near Arizona Boulevard. No damage or injuries were reported.", "ts_dict_index": [1341, 1342, 1343]}
+{"event_id": 1009539, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-03-22 02:33:00", "end_date_time": "2022-03-22 04:15:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable air north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into North Louisiana during the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas and North Louisiana, resulting in numerous reports of damaging winds. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. Cars were flooded at the intersection of Hollywood Avenue and Kennedy Drive.", "ts_dict_index": [1425, 1426, 1427]}
+{"event_id": 1134203, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2023-07-20 18:53:00", "end_date_time": "2023-07-20 20:30:00", "narrative": "A surface low moved generally eastward from east-central Lower MI to the southeastern shore of Lake Huron during the evening of the 20th. Simultaneously, the low's warm front swept northeastward across southern ON and western NY toward the northern shore of Lake Ontario as the low's trailing cold front moved generally eastward across southeastern Lower MI and far-northeastern IN to central Lake Erie and northeastern OH.||Multiple lines and clusters of multicell thunderstorms persisted generally eastward and southeastward across northern OH during the early through mid-evening hours of the 20th and produced sporadic severe hail and straight-line convective wind damage as the storms encountered moderate to strong MUCAPE and effective bulk shear, respectively, within the warm sector. An embedded supercell produced large hail in Westlake, a western suburb of Cleveland. Although the thunderstorms moved progressively across the area, the thunderstorms produced torrential rainfall across Cuyahoga County, with instantaneous rainfall rates of 4 to 5 inches per hour and rainfall totals of 1.75 to 2.5 inches in a period of one hour or less. The torrential rainfall resulted in instances of flash flooding. Several roadways around and near downtown Cleveland flooded with cars stranded. Flooding of Doan Brook upstream of Lower Shaker Lake caused flooding of South Park Boulevard.", "ts_dict_index": [1419, 1420, 1421]}
+{"event_id": 1009565, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-03-22 03:00:00", "end_date_time": "2022-03-22 04:15:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable air north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into North Louisiana during the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas and North Louisiana, resulting in numerous reports of damaging winds. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. Flooding was reported in the Lucien Fields subdivision in South Shreveport.", "ts_dict_index": [1428, 1429, 1430]}
+{"event_id": 1134201, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2023-07-20 19:25:00", "end_date_time": "2023-07-20 21:00:00", "narrative": "A surface low moved generally eastward from east-central Lower MI to the southeastern shore of Lake Huron during the evening of the 20th. Simultaneously, the low's warm front swept northeastward across southern ON and western NY toward the northern shore of Lake Ontario as the low's trailing cold front moved generally eastward across southeastern Lower MI and far-northeastern IN to central Lake Erie and northeastern OH.||Multiple lines and clusters of multicell thunderstorms persisted generally eastward and southeastward across northern OH during the early through mid-evening hours of the 20th and produced sporadic severe hail and straight-line convective wind damage as the storms encountered moderate to strong MUCAPE and effective bulk shear, respectively, within the warm sector. An embedded supercell produced large hail in Westlake, a western suburb of Cleveland. Although the thunderstorms moved progressively across the area, the thunderstorms produced torrential rainfall across Cuyahoga County, with instantaneous rainfall rates of 4 to 5 inches per hour and rainfall totals of 1.75 to 2.5 inches in a period of one hour or less. The torrential rainfall resulted in instances of flash flooding. Flash flooding along Big Creek from just north of Brookpark Road downstream through the Cleveland Metroparks Zoo. The USGS river gage reading at Big Creek near Brooklyn (Brookpark Road) rose from 3.8 feet to a crest of 11.2 feet in 90 minutes, with the flooded creek causing flooding of a parking lot with less than 5 parked cars inundated. Downstream, the USGS river gage reading at Big Creek at Cleveland (Cleveland Metroparks Zoo) rose from 5.0 feet to a crest of 12.9 feet in 70 minutes. Flooding from the creek caused minor damage to festival displays staged in the low lying areas of the Zoo near the creek.", "ts_dict_index": [1422, 1423, 1424]}
+{"event_id": 1134185, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2023-07-20 19:25:00", "end_date_time": "2023-07-20 21:00:00", "narrative": "A surface low moved generally eastward from east-central Lower MI to the southeastern shore of Lake Huron during the evening of the 20th. Simultaneously, the low's warm front swept northeastward across southern ON and western NY toward the northern shore of Lake Ontario as the low's trailing cold front moved generally eastward across southeastern Lower MI and far-northeastern IN to central Lake Erie and northeastern OH.||Multiple lines and clusters of multicell thunderstorms persisted generally eastward and southeastward across northern OH during the early through mid-evening hours of the 20th and produced sporadic severe hail and straight-line convective wind damage as the storms encountered moderate to strong MUCAPE and effective bulk shear, respectively, within the warm sector. An embedded supercell produced large hail in Westlake, a western suburb of Cleveland. Although the thunderstorms moved progressively across the area, the thunderstorms produced torrential rainfall across Cuyahoga County, with instantaneous rainfall rates of 4 to 5 inches per hour and rainfall totals of 1.75 to 2.5 inches in a period of one hour or less. The torrential rainfall resulted in instances of flash flooding. Several flooded roadways near Cleveland Hopkins International Airport, including OH-237 South near Brookpark Road and Snow Road at OH-237. Several cars inundated by flood waters, requiring assistance from Cleveland Hopkins Airport Fire Rescue. More than one dozen flooded basements reported in Parma and North Royalton. Flooded roadways in Parma and North Royalton include Regency Drive, State Road, Thoreau Drive, Antoinette Drive, and North Akins Road near South Gateway Drive.", "ts_dict_index": [1416, 1417, 1418]}
+{"event_id": 1148437, "event_type": "Flash Flood", "state": "OHIO", "cz_name": "CUYAHOGA", "begin_date_time": "2023-08-23 19:54:00", "end_date_time": "2023-08-24 00:00:00", "narrative": "An anomalously-warm and moist air mass was in place across much of the Central Plains and Midwest, resulting in strong to perhaps extreme instability in addition to tropical-like precipitable water values exceeding 2.0 inches. The Lower Great Lakes region, specifically northern Ohio and Northwest Pennsylvania found itself on the eastern edge of this heat dome. Strong northwest flow aloft persisted along the periphery of the anomalously-warm and moist air mass, allowing for organized storms to develop across northern Ohio and Northwest Pennsylvania. A constant feed of moisture allowed these storms to maintain their intensity throughout the evening and overnight hours of Aug 23, 2023 and into the early morning hours of Aug 24, 2023 as they slowly pivoted southwest. Numerous flash flood warnings were issued with 3 considerable tags utilized throughout the course of the event. The hardest-hit areas were along the lakeshore between Toledo and Cleveland where there were several reports of 5 to 7 inches of rainfall. Elsewhere, generally 2 to 4 inches of rainfall was common, most of which fell in only a few hours. The area was on the edge of an extremely unstable airmass with sufficient deep-layer shear for organized convection. Widespread, extensive flash flooding in Cleveland, Lakewood, Rocky River, Westlake, and Bay Village. Interstate 90 flooded with several feet of water with multiple water rescues on both eastbound and westbound lanes near the McKinley Avenue exit. Lakeshore Boulevard and Martin Luther King Boulevard closed due to flooding in Cleveland, with multiple cars stranded in high water. Extensive basement flooding in Rocky River, Lakewood, and Bay Village. Radar estimated 1.5 to 2.25 inches of rainfall in less than three hours, with much of the rainfall falling in less than one hour.", "ts_dict_index": [1374, 1375, 1376]}
+{"event_id": 1009546, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-03-22 02:46:00", "end_date_time": "2022-03-22 04:15:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable air north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into North Louisiana during the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas and North Louisiana, resulting in numerous reports of damaging winds. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. Flooding was reported on I-20 East at Mile Marker 4, Roy Road at MLK Drive, Highway 173 and North Lakeshore Drive, Highway 173 and Bostwick, Waterwood Drive at West 70th Street, Starwood Lane at West Starwood in Greenwood. Three motorists were rescued from high water.", "ts_dict_index": [1437, 1438, 1439]}
+{"event_id": 974501, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2021-07-01 11:15:00", "end_date_time": "2021-07-01 12:45:00", "narrative": "A stationary front across northeastern Oklahoma and southeastern Kansas resulted in multiple rounds of thunderstorms across the region from June 26th through June 30th. Four to eight inches of rain fell across much of Ottawa County during the early morning hours of June 26th, with heavy rainfall also occurring across the Neosho River basin in eastern Kansas. Six to twelve inch rainfall amounts occurred in a 3-day period ending during the mid morning hours of June 28th. This widespread heavy rainfall resulted in moderate flooding along the Neosho River near Commerce, which continued into early July.||The frontal boundary pushed southward into northeastern Oklahoma on July 1st, with another round of thunderstorms developing during the early morning hours. This activity continued into the evening. Unusually high precipitable water in the atmosphere promoted additional heavy rainfall from these thunderstorms. Widespread two to six inch rainfall amounts occurred across northeastern Oklahoma, which resulted in flash flooding. The Deep Fork River near Beggs experienced major flooding as a result of a week's worth of rainfall totaling up to around ten inches in the basin. Portions of multiple roads were flooded and closed in Broken Arrow.", "ts_dict_index": [1455, 1456, 1457]}
+{"event_id": 1009570, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-03-22 03:00:00", "end_date_time": "2022-03-22 04:15:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable air north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into North Louisiana during the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas and North Louisiana, resulting in numerous reports of damaging winds. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. Oak Ridge Drive was flooded.", "ts_dict_index": [1440, 1441, 1442]}
+{"event_id": 1009549, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-03-22 03:32:00", "end_date_time": "2022-03-22 04:15:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable air north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into North Louisiana during the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas and North Louisiana, resulting in numerous reports of damaging winds. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. Flooding was reported at the Highway 3132 west on ramp at West 70th Street.", "ts_dict_index": [1434, 1435, 1436]}
+{"event_id": 846593, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-09-23 13:00:00", "end_date_time": "2019-09-23 17:15:00", "narrative": "A weak mid level trough extended from west to east across Southern and Southeast Oklahoma into Western and Central Arkansas during the daytime hours on September 23rd, south of a stationary front that shifted from Central Oklahoma into Northwest and Northcentral Arkansas. A very moist air mass was in place at the surface across extreme Southeast Oklahoma and Western Arkansas, as large scale forcing increased atop this mid level disturbance from mid morning through the afternoon. This resulted in the development of a cluster of showers and thunderstorms producing locally heavy rainfall, which moved over much of Southeast Oklahoma. These showers and thunderstorms continued to develop and move repeatedly over the same areas across Northern and Central McCurtain County, producing widespread rainfall amounts of 3-7+ inches. This fell atop already saturated grounds, where widespread amounts of 3-6+ inches had fallen on September 20th. This resulted in significant flash flooding across much of Northern and Central McCurtain County, with numerous roads flooded and closed, and at least two homes flooded. In all, 4 day storm total rainfall amounts of 6-10+ inches were recorded. Tebo Jones Road southwest of Broken Bow was flooded and closed.", "ts_dict_index": [1449, 1450, 1451]}
+{"event_id": 846595, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-09-23 13:00:00", "end_date_time": "2019-09-23 17:15:00", "narrative": "A weak mid level trough extended from west to east across Southern and Southeast Oklahoma into Western and Central Arkansas during the daytime hours on September 23rd, south of a stationary front that shifted from Central Oklahoma into Northwest and Northcentral Arkansas. A very moist air mass was in place at the surface across extreme Southeast Oklahoma and Western Arkansas, as large scale forcing increased atop this mid level disturbance from mid morning through the afternoon. This resulted in the development of a cluster of showers and thunderstorms producing locally heavy rainfall, which moved over much of Southeast Oklahoma. These showers and thunderstorms continued to develop and move repeatedly over the same areas across Northern and Central McCurtain County, producing widespread rainfall amounts of 3-7+ inches. This fell atop already saturated grounds, where widespread amounts of 3-6+ inches had fallen on September 20th. This resulted in significant flash flooding across much of Northern and Central McCurtain County, with numerous roads flooded and closed, and at least two homes flooded. In all, 4 day storm total rainfall amounts of 6-10+ inches were recorded. Highway 3 over the Glover River was flooded and closed. Two homes near the river were flooded. Numerous other roadways near the river were flooded and closed as well.", "ts_dict_index": [1443, 1444, 1445]}
+{"event_id": 832601, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-06-23 19:27:00", "end_date_time": "2019-06-23 22:00:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. The remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, some of which were severe given the moderate instability that had developed with afternoon heating and the deep moisture in place. Damaging winds downed several trees in and near Broken Bow, with these thunderstorms also producing very heavy rainfall which moved repeatedly over the same areas of Southern McCurtain County. This resulted in widespread flash flooding which flooded numerous roads across this area before the stronger storms gradually shifted southeast into East Texas, Southwest Arkansas, and Northern Louisiana during the late evening into the overnight/early morning hours of June 24th. Widespread flash flooding was reported across Southern McCurtain County after cumulative rainfall amounts of three to in excess of five inches fell. Numerous roads were flooded and closed.", "ts_dict_index": [1452, 1453, 1454]}
+{"event_id": 846596, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-09-23 11:15:00", "end_date_time": "2019-09-23 17:15:00", "narrative": "A weak mid level trough extended from west to east across Southern and Southeast Oklahoma into Western and Central Arkansas during the daytime hours on September 23rd, south of a stationary front that shifted from Central Oklahoma into Northwest and Northcentral Arkansas. A very moist air mass was in place at the surface across extreme Southeast Oklahoma and Western Arkansas, as large scale forcing increased atop this mid level disturbance from mid morning through the afternoon. This resulted in the development of a cluster of showers and thunderstorms producing locally heavy rainfall, which moved over much of Southeast Oklahoma. These showers and thunderstorms continued to develop and move repeatedly over the same areas across Northern and Central McCurtain County, producing widespread rainfall amounts of 3-7+ inches. This fell atop already saturated grounds, where widespread amounts of 3-6+ inches had fallen on September 20th. This resulted in significant flash flooding across much of Northern and Central McCurtain County, with numerous roads flooded and closed, and at least two homes flooded. In all, 4 day storm total rainfall amounts of 6-10+ inches were recorded. Numerous roads were flooded and closed in and west of Highway 259 in Hochatown.", "ts_dict_index": [1446, 1447, 1448]}
+{"event_id": 975664, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-17 20:00:00", "end_date_time": "2021-07-17 21:00:00", "narrative": "During the evening of July 17th an area of low pressure slowly moved east along a stationary boundary that stretched from New York to Massachusetts.  The front briefly lifted northward into southern New Hampshire pulling ample moisture with precipitable water values over 2 inches, anomalously high, even for July.  Additionally, much of this region had seen 300%+ of average rainfall over the preceding few weeks. This caused soil moisture values and streamflow conditions to be well above average.  Multiple rounds of heavy rainfall produced significant flash flooding in southern New Hampshire. Reports to the weather service included totals of nearly 7 inches of rain in Jaffrey, 5 inches in Marlborough and Swanzey, and between 2 and 3 inches in Chesterfield. ||Severe flooding prompted numerous local emergency operations centers to open, and washed out road infrastructure in 14 communities in the Monadnock Region. Early estimates from state and local damages verified at over $2 million from the storm.  Cheshire County alone met the entire state indicator threshold to request a declaration of disaster for New Hampshire. Communities that sustained the most damage include Jaffrey, Keene, Richmond, and Fitzwilliam. Law Enforcement reported that Main Street in Dublin near Dublin Pond was flooded with several feet of water and stalled out vehicles.", "ts_dict_index": [1389, 1390, 1391]}
+{"event_id": 948578, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-05-09 19:35:00", "end_date_time": "2021-05-10 04:00:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. County Road 525 near the bridge and County Road 526 were both closed due to flooding.", "ts_dict_index": [1482, 1483, 1484]}
+{"event_id": 969564, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2021-07-01 12:15:00", "end_date_time": "2021-07-01 14:15:00", "narrative": "A stationary front across northeastern Oklahoma and southeastern Kansas resulted in multiple rounds of thunderstorms across the region from June 26th through June 30th. Four to eight inches of rain fell across much of Ottawa County during the early morning hours of June 26th, with heavy rainfall also occurring across the Neosho River basin in eastern Kansas. Six to twelve inch rainfall amounts occurred in a 3-day period ending during the mid morning hours of June 28th. This widespread heavy rainfall resulted in moderate flooding along the Neosho River near Commerce, which continued into early July.||The frontal boundary pushed southward into northeastern Oklahoma on July 1st, with another round of thunderstorms developing during the early morning hours. This activity continued into the evening. Unusually high precipitable water in the atmosphere promoted additional heavy rainfall from these thunderstorms. Widespread two to six inch rainfall amounts occurred across northeastern Oklahoma, which resulted in flash flooding. The Deep Fork River near Beggs experienced major flooding as a result of a week's worth of rainfall totaling up to around ten inches in the basin. Portions of E 96th Street North were flooded near N Mingo Road.", "ts_dict_index": [1464, 1465, 1466]}
+{"event_id": 969565, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2021-07-01 11:02:00", "end_date_time": "2021-07-01 12:45:00", "narrative": "A stationary front across northeastern Oklahoma and southeastern Kansas resulted in multiple rounds of thunderstorms across the region from June 26th through June 30th. Four to eight inches of rain fell across much of Ottawa County during the early morning hours of June 26th, with heavy rainfall also occurring across the Neosho River basin in eastern Kansas. Six to twelve inch rainfall amounts occurred in a 3-day period ending during the mid morning hours of June 28th. This widespread heavy rainfall resulted in moderate flooding along the Neosho River near Commerce, which continued into early July.||The frontal boundary pushed southward into northeastern Oklahoma on July 1st, with another round of thunderstorms developing during the early morning hours. This activity continued into the evening. Unusually high precipitable water in the atmosphere promoted additional heavy rainfall from these thunderstorms. Widespread two to six inch rainfall amounts occurred across northeastern Oklahoma, which resulted in flash flooding. The Deep Fork River near Beggs experienced major flooding as a result of a week's worth of rainfall totaling up to around ten inches in the basin. Portions of E 101st Street were flooded near Cedar Ridge Country Club.", "ts_dict_index": [1461, 1462, 1463]}
+{"event_id": 948579, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-05-09 19:45:00", "end_date_time": "2021-05-10 04:00:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. County Road 555 between Woden and Etoile was closed due to flooding.", "ts_dict_index": [1494, 1495, 1496]}
+{"event_id": 948582, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-05-09 19:45:00", "end_date_time": "2021-05-10 04:00:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. County Road 411 and Farm to Market Road 226 in the Woden community were both closed due to flooding.", "ts_dict_index": [1485, 1486, 1487]}
+{"event_id": 948209, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2021-03-17 09:20:00", "end_date_time": "2021-03-17 12:20:00", "narrative": "In Arkansas, the fireworks started early (during the predawn hours) on the 17th. Isolated storms unloaded large hail, including golf ball size hail just east of Scranton (Logan County), and quarter size hail at Atkins (Pope County) and Johnsville (Bradley County). After that, it turned into a bunch of heavy rain.||Two to more than three inches of rain dumped from Newport (Jackson County) to North Little Rock (Pulaski County). Vehicles stalled in high water, and people had to be rescued. Several roads were closed. Water was also over roads in North Little Rock and Sherwood (both in Pulaski County). At the latter location, a pond near a police station overflowed, and there was water everywhere.||At Searcy (White County), lightning struck a clinic and caused damage to electronic equipment. Power was knocked out to the facility temporarily.||In southeast Arkansas, rotation ramped up in one storm, and a Tornado Warning was disseminated at 430 pm CDT for eastern Drew and southern Desha Counties. At 437 pm CDT, a brief tornado (rated EF0) was witnessed in a farm field about a mile southeast of McGehee (Desha County). It was the first tornado of 2021 in the state. Water was reported over several roadways.", "ts_dict_index": [1476, 1477, 1478]}
+{"event_id": 948583, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-05-09 19:45:00", "end_date_time": "2021-05-10 04:00:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. County Roads 228, 229, 230, and 302 were all closed due to flooding.", "ts_dict_index": [1488, 1489, 1490]}
+{"event_id": 976100, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-29 23:40:00", "end_date_time": "2021-07-30 01:00:00", "narrative": "A developing area of lower pressure crossed the state on the night of July 29th.  Abundant moisture moved into the region ahead of this area of low pressure.  Rain began by late afternoon on July 29th across the Connecticut River Valley.  Rain continued to quickly spread east through the late afternoon hours across all of Central and Southern New Hampshire.  Moderate rain was steady with embedded areas of heavy rain that allowed rainfall rates to peak at 3 to 4��� per/hour at times.  The majority of the rain fell in a 3 to 4 hour window with a general 2 to 3��� south of the White Mountains.  A concentrated band of rainfall extended from Cheshire County across the state to Southern Carroll County where most of the flood damage occurred as localized rainfall amounts approached 5���.  Another localized maximum rainfall band was located across Southern Hillsborough County as a brief but intense band traveled across this area around 10 PM EDT.  The bands of rain ended from west to east with the rain clearing the state by midnight on July 30th. The heavy rain and well above normal soil saturation led to excessive run-off even after the rain ended through the night. Flash riverine flooding occurred on the evening of the 29th in Alstead.  Flood waters upstream in Acworth along the Cold River resulted in a washout of the Route 123A road near Kelley Road.  River levels from the USGS Cold River at Alstead gage reported an all time peak flow of 11.46 feet and a flow of 10,500cfs, cresting at 11 PM on the 29th. The period of record is relatively short dating back to 2009, but significant damage occurred in the Cold River basin with an estimated 50 to 75 year flood event based on USGS data.", "ts_dict_index": [1470, 1471, 1472]}
+{"event_id": 969563, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2021-07-01 10:15:00", "end_date_time": "2021-07-01 12:15:00", "narrative": "A stationary front across northeastern Oklahoma and southeastern Kansas resulted in multiple rounds of thunderstorms across the region from June 26th through June 30th. Four to eight inches of rain fell across much of Ottawa County during the early morning hours of June 26th, with heavy rainfall also occurring across the Neosho River basin in eastern Kansas. Six to twelve inch rainfall amounts occurred in a 3-day period ending during the mid morning hours of June 28th. This widespread heavy rainfall resulted in moderate flooding along the Neosho River near Commerce, which continued into early July.||The frontal boundary pushed southward into northeastern Oklahoma on July 1st, with another round of thunderstorms developing during the early morning hours. This activity continued into the evening. Unusually high precipitable water in the atmosphere promoted additional heavy rainfall from these thunderstorms. Widespread two to six inch rainfall amounts occurred across northeastern Oklahoma, which resulted in flash flooding. The Deep Fork River near Beggs experienced major flooding as a result of a week's worth of rainfall totaling up to around ten inches in the basin. The driver of a stalled car was rescued from flood water on Woodland Drive.", "ts_dict_index": [1458, 1459, 1460]}
+{"event_id": 948212, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2021-03-17 10:30:00", "end_date_time": "2021-03-17 13:30:00", "narrative": "In Arkansas, the fireworks started early (during the predawn hours) on the 17th. Isolated storms unloaded large hail, including golf ball size hail just east of Scranton (Logan County), and quarter size hail at Atkins (Pope County) and Johnsville (Bradley County). After that, it turned into a bunch of heavy rain.||Two to more than three inches of rain dumped from Newport (Jackson County) to North Little Rock (Pulaski County). Vehicles stalled in high water, and people had to be rescued. Several roads were closed. Water was also over roads in North Little Rock and Sherwood (both in Pulaski County). At the latter location, a pond near a police station overflowed, and there was water everywhere.||At Searcy (White County), lightning struck a clinic and caused damage to electronic equipment. Power was knocked out to the facility temporarily.||In southeast Arkansas, rotation ramped up in one storm, and a Tornado Warning was disseminated at 430 pm CDT for eastern Drew and southern Desha Counties. At 437 pm CDT, a brief tornado (rated EF0) was witnessed in a farm field about a mile southeast of McGehee (Desha County). It was the first tornado of 2021 in the state. Pictures relayed, showed flash flooding of water at least one foot deep over a couple of roads in North Little Rock.", "ts_dict_index": [1473, 1474, 1475]}
+{"event_id": 948581, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-05-09 19:45:00", "end_date_time": "2021-05-10 04:00:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. County Roads 460 and 560 in the Etoile community were both closed due to flooding.", "ts_dict_index": [1479, 1480, 1481]}
+{"event_id": 976140, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2021-07-29 22:42:00", "end_date_time": "2021-07-30 00:00:00", "narrative": "A developing area of lower pressure crossed the state on the night of July 29th.  Abundant moisture moved into the region ahead of this area of low pressure.  Rain began by late afternoon on July 29th across the Connecticut River Valley.  Rain continued to quickly spread east through the late afternoon hours across all of Central and Southern New Hampshire.  Moderate rain was steady with embedded areas of heavy rain that allowed rainfall rates to peak at 3 to 4��� per/hour at times.  The majority of the rain fell in a 3 to 4 hour window with a general 2 to 3��� south of the White Mountains.  A concentrated band of rainfall extended from Cheshire County across the state to Southern Carroll County where most of the flood damage occurred as localized rainfall amounts approached 5���.  Another localized maximum rainfall band was located across Southern Hillsborough County as a brief but intense band traveled across this area around 10 PM EDT.  The bands of rain ended from west to east with the rain clearing the state by midnight on July 30th. The heavy rain and well above normal soil saturation led to excessive run-off even after the rain ended through the night. The Ashuelot River flooded Route 12A at Gilsum Road. The USGS gage at Gilsum reported a rise in stage from 3 feet to 9.5 feet between 7 PM on the 29th and 5 AM on the 30th. The streamflows rose likewise from 113 cfs to 2,280 cfs. The flows are comparable to those observed after Hurricane Irene in 2011.", "ts_dict_index": [1467, 1468, 1469]}
+{"event_id": 1009548, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-03-22 02:46:00", "end_date_time": "2022-03-22 04:15:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable air north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into North Louisiana during the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas and North Louisiana, resulting in numerous reports of damaging winds. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. Flooding was reported at Highway 171 and Old Mansfield Road.", "ts_dict_index": [1431, 1432, 1433]}
+{"event_id": 948580, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-05-09 19:45:00", "end_date_time": "2021-05-10 04:00:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. County Road 317 was closed due to flooding.", "ts_dict_index": [1497, 1498, 1499]}
+{"event_id": 948574, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-05-09 19:15:00", "end_date_time": "2021-05-10 04:00:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. County Road 789 was closed due to flooding.", "ts_dict_index": [1500, 1501, 1502]}
+{"event_id": 973789, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-04 18:20:00", "end_date_time": "2021-07-04 18:50:00", "narrative": "On the 4th, deep moisture was in place with near record level PWAT values of 1.8-2.0 inches observed by regional soundings. Instability was marginal with MLCAPE around 1000 J/kg, but it was sufficient for thunderstorms to develop across Gila county in the afternoon. With the deep moisture in place, all thunderstorms were producing very heavy rain with rain rates commonly around 1-2 inches per hour and briefly higher. Heavy rain impacted multiple burn scars across the county which are especially prone to flash flooding. Multiple flash flood warnings were issued. One storm impacted the 2021 Telegraph burn scar with 1.5-2.0 inches of rain in about 1 hour. A rain gage in Sixshooter Canyon measured 1.38 inches in 41 minutes. This led to a significant flash flood event with runoff collecting in Sixshooter Canyon and the upper portions of Pinal Creek and flowing downstream into the town of Globe. Many homes were damaged by flood waters and debris and Pinal Creek ran bankfull through much of downtown Globe with some bridges nearly overtopped. The floodwave continued several miles north of Globe with a USGS gage in Pinal Creek measuring a notable rise. Video from a trained spotter showed substantial ash-blackened flood water flowing through Pinal Creek, with flow over Beer Tree Crossing near Jess Hayes Road. No damages or injuries were reported.", "ts_dict_index": [1521, 1522, 1523]}
+{"event_id": 849961, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 08:00:00", "end_date_time": "2019-09-23 12:15:00", "narrative": "During the early morning hours on September 23rd, copious tropical moisture began to spread north and into south-central Arizona. A weather system dropping south out of Nevada began to act on the moisture, resulting in the development of numerous showers and thunderstorms. Some of the storms produced copious amounts of rain with peak rain rates in excess of 2 inches per hour. Many locations across the high terrain east of Phoenix measured more than 3 inches of rain during the morning hours. Multiple events of flash flooding occurred in locations such as Apache Junction, Tortilla Flat, Fountain Hills and terrain to the south and east of Lake Roosevelt. As an example, at 0730MST a local emergency manager reported that 7 homes were flooded in Roosevelt Estates as Campaign Creek overflowed its banks. Several Flash Flood Warnings were issued for areas to the east of Phoenix during the morning hours. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Copious amounts of tropical moisture spread north and into south-central Arizona during the morning hours on September 23rd, allowing for the development of numerous showers and thunderstorms. Locally heavy rain occurred with peak rain rates in excess of 2 inches per hour at times, and the heavy rain led to flash flooding affecting areas such as Fountain Hills. As an example of the heavy rain that fell, at 0820MST a trained spotter located about 2 miles northeast of Fountain Hills indicated that 3.5 inches of rain had fallen over the past one hour and forty minutes resulting in minor flooding. Flash flooding soon developed and at 0900MST local fire and rescue reported that Ashford Wash in Fountain Hills had exceeded its banks. Flooding occurred at the intersection of El Pueblo Boulevard and Calico Drive. A Flash Flood Warning was issued for the area at 0818MST and was in effect at the time of the flash flooding.", "ts_dict_index": [1524, 1525, 1526]}
+{"event_id": 973783, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-04 17:55:00", "end_date_time": "2021-07-04 18:30:00", "narrative": "On the 4th, deep moisture was in place with near record level PWAT values of 1.8-2.0 inches observed by regional soundings. Instability was marginal with MLCAPE around 1000 J/kg, but it was sufficient for thunderstorms to develop across Gila county in the afternoon. With the deep moisture in place, all thunderstorms were producing very heavy rain with rain rates commonly around 1-2 inches per hour and briefly higher. Heavy rain impacted multiple burn scars across the county which are especially prone to flash flooding. Multiple flash flood warnings were issued. One storm impacted the 2021 Telegraph burn scar with 1.5-2.0 inches of rain in about 1 hour. A rain gage in Sixshooter Canyon measured 1.38 inches in 41 minutes. This led to a significant flash flood event with runoff collecting in Sixshooter Canyon and the upper portions of Pinal Creek and flowing downstream into the town of Globe. Many homes were damaged by flood waters and debris and Pinal Creek ran bankfull through much of downtown Globe with some bridges nearly overtopped. The floodwave continued several miles north of Globe with a USGS gage in Pinal Creek measuring a notable rise. USGS stream gage on Pinal Creek at Inspiration Dam measured a rapid rise from 1.28 feet at 1745 MST to 5.20 feet at 1800 MST. A radar estimated 2 to 3 inches of rain fell over the area, including a portion of the 2020 Salt burn scar, between 1610 MST and 1730 MST. Additional smaller rises were measured at 2000 MST and 2330 MST that may have been related to a different flood wave that moved through the Globe area around 1800-1900 MST. No damages or injuries were reported.", "ts_dict_index": [1518, 1519, 1520]}
+{"event_id": 974404, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-04 18:55:00", "end_date_time": "2021-07-04 19:45:00", "narrative": "On the 4th, deep moisture was in place with near record level PWAT values of 1.8-2.0 inches observed by regional soundings. Instability was marginal with MLCAPE around 1000 J/kg, but it was sufficient for thunderstorms to develop across Gila county in the afternoon. With the deep moisture in place, all thunderstorms were producing very heavy rain with rain rates commonly around 1-2 inches per hour and briefly higher. Heavy rain impacted multiple burn scars across the county which are especially prone to flash flooding. Multiple flash flood warnings were issued. One storm impacted the 2021 Telegraph burn scar with 1.5-2.0 inches of rain in about 1 hour. A rain gage in Sixshooter Canyon measured 1.38 inches in 41 minutes. This led to a significant flash flood event with runoff collecting in Sixshooter Canyon and the upper portions of Pinal Creek and flowing downstream into the town of Globe. Many homes were damaged by flood waters and debris and Pinal Creek ran bankfull through much of downtown Globe with some bridges nearly overtopped. The floodwave continued several miles north of Globe with a USGS gage in Pinal Creek measuring a notable rise. Multiple social media photos and videos showed 6-8 feet of water flowing down the Pinal Creek flood retention channel in downtown Globe. Flood water nearly reached the bottom of a few of the bridges across Pinal Creek. Flood water would continue downstream in Pinal Creek for several miles north of Globe. There were no reports of damage or injuries in Downtown Globe.", "ts_dict_index": [1515, 1516, 1517]}
+{"event_id": 1060428, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-06 03:39:00", "end_date_time": "2022-10-06 05:39:00", "narrative": "A slow moving cutoff low was situated over southern Arizona, providing forced ascent. Two rounds of convection occurred, with the first round affecting portions of south-central Arizona during the very early morning hours (0000-0400MST) and the second round affecting far southwest Arizona during the early to mid afternoon hours (1300-1600MST). With the help of daytime heating boosting instability values into the moderate to high side (MLCAPE 1500-2000 J/KG), the thunderstorm activity affecting southwestern Arizona became intense with reports of hail as the cutoff low resulted in well-below normal mid-level temperatures of -13C to -14C. Moisture content was also on the high side during the two rounds of convection as the precipitable water values ranged between 1.0-1.4, which is near record values for early October. This resulted in numerous reports of flash flooding, with the first round of convection during the early morning hours generating flash flooding along State Route 238, just to the northeast of Gila Bend, and the second round of convection during the early to mid-afternoon hours generating flash flooding across State Route 95, north of Yuma. State Route 238 was closed between mile posts 7 and 24, northeast of Gila, due to flash flooding. No damages or injuries were reported.", "ts_dict_index": [1506, 1507, 1508]}
+{"event_id": 974036, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-04 17:55:00", "end_date_time": "2021-07-04 18:55:00", "narrative": "On the 4th, deep moisture was in place with near record level PWAT values of 1.8-2.0 inches observed by regional soundings. Instability was marginal with MLCAPE around 1000 J/kg, but it was sufficient for thunderstorms to develop across Gila county in the afternoon. With the deep moisture in place, all thunderstorms were producing very heavy rain with rain rates commonly around 1-2 inches per hour and briefly higher. Heavy rain impacted multiple burn scars across the county which are especially prone to flash flooding. Multiple flash flood warnings were issued. One storm impacted the 2021 Telegraph burn scar with 1.5-2.0 inches of rain in about 1 hour. A rain gage in Sixshooter Canyon measured 1.38 inches in 41 minutes. This led to a significant flash flood event with runoff collecting in Sixshooter Canyon and the upper portions of Pinal Creek and flowing downstream into the town of Globe. Many homes were damaged by flood waters and debris and Pinal Creek ran bankfull through much of downtown Globe with some bridges nearly overtopped. The floodwave continued several miles north of Globe with a USGS gage in Pinal Creek measuring a notable rise. A significant flood wave of water, ash, mud, and other debris moved downstream in Pinal Creek through Six Shooter Canyon. Flood water escaped the banks of Pinal Creek in many locations and caused varying degrees of property damage to 15 homes along Six Shooter Canyon Road with one of the homes deemed a total loss. Photos and videos of two of the impacted homes showed 1-3 feet of water and debris moving through the the yards and up against the homes with water and mud entering the homes. There were also multiple videos that showed 1-2 feet of water and debris flowing rapidly down Six Shooter Canyon Rd from Delores Lane to at least Marlin Drive. In addition to the 15 damaged homes, there was a lot of damage to fencing, roads, a few bridges, vehicles, and other infrastructure and personal property. The flood wave would continue down Pinal Creek all the way through downtown Globe. There were no reports of injuries.", "ts_dict_index": [1512, 1513, 1514]}
+{"event_id": 850042, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2019-09-23 05:30:00", "end_date_time": "2019-09-23 09:45:00", "narrative": "During the early morning hours on September 23rd, copious tropical moisture began to spread north and into south-central Arizona. A weather system dropping south out of Nevada began to act on the moisture, resulting in the development of numerous showers and thunderstorms. Some of the storms produced copious amounts of rain with peak rain rates in excess of 2 inches per hour. Many locations across the high terrain east of Phoenix measured more than 3 inches of rain during the morning hours. Multiple events of flash flooding occurred in locations such as Apache Junction, Tortilla Flat, Fountain Hills and terrain to the south and east of Lake Roosevelt. As an example, at 0730MST a local emergency manager reported that 7 homes were flooded in Roosevelt Estates as Campaign Creek overflowed its banks. Several Flash Flood Warnings were issued for areas to the east of Phoenix during the morning hours. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Copious amounts of tropical moisture spread north and into south-central Arizona during the early morning hours on September 23rd allowing for the development of numerous showers and thunderstorms. Many of the storms had heavy rain with peak rain rates in excess of 2 inches per hour. The heavy rain led to episodes of flash flooding across areas to the east and southeast of Phoenix including the communities of Apache Junction and East Mesa. According to the Arizona Department of Highways, at 0630MST flash flooding 3 miles northeast of Apache Junction resulted in State Route 88 becoming impassable at Mile Marker 199 along Weekes Wash. Flooding was also occurring along Palm Wash. In addition, at 0700MST local broadcast media reported a swift water rescue underway at the intersection of Main Drive and Mckellips Boulevard, about 3 miles northwest of Apache Junction. A Flash Flood Warning was issued for the area at 0541MST and was in effect during the flooding. No injuries were reported due to the flooding.", "ts_dict_index": [1527, 1528, 1529]}
+{"event_id": 1040740, "event_type": "Flash Flood", "state": "KENTUCKY", "cz_name": "PIKE", "begin_date_time": "2022-08-01 09:35:00", "end_date_time": "2022-08-01 11:00:00", "narrative": "A midlevel shortwave trough was situated over the Upper Midwest Sunday night (31st) into Monday morning (1st). At the surface, a strong occluded low was also present. From this low and occlusion, a warm front extended to the southeast, lifting through the Commonwealth during the same time frame. A MCS developed in the Upper Mississippi Valley and continued to push southeast towards the Commonwealth during the morning hours. This prompted SPC to put portions of northern and eastern KY in a slight risk for severe weather throughout the day. Ironically, we did not see any severe weather out of this system - however, showers that developed during the morning hours ahead of the MCS were a different story. These showers developed over the eastern portion of the state, and impacted areas that were already heavily saturated from the devastating rains that occurred the week before. More so, the convection was moving parallel to the mean flow, which meant that many of these showers continued to train over the same locations for an extended period of time. This prompted flash flood warnings, and led to impacts in Martin, Pike, Letcher, Floyd, and Knott counties. Water was reported out of the banks along Lower Dix Fork near the Canada community and getting into nearby homes.", "ts_dict_index": [1509, 1510, 1511]}
+{"event_id": 948577, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-05-09 19:30:00", "end_date_time": "2021-05-10 04:00:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. Highway 7 near Morral Bayou, County Road 620, County Road 724, and County Road 765 were all closed due to flooding.", "ts_dict_index": [1491, 1492, 1493]}
+{"event_id": 852830, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2019-09-25 15:30:00", "end_date_time": "2019-09-25 18:30:00", "narrative": "Scattered thunderstorms developed across the lower deserts of Imperial County - from the Imperial Valley eastward to the lower Colorado River valley - during the afternoon and evening hours on September 25th. Instability was elevated due to the close proximity of an upper level low pressure system and cool air aloft, and the increased instability aided the thunderstorm development. As was the case over the past couple of days, the stronger thunderstorms primarily generated very heavy rain with peak rain rates well in excess of one inch per hour. Multiple reports from the California Highway Patrol indicated that flash flooding was occurring along State Route 78, from near the Cibola National Wildlife Refuge south to near Interstate 8. Local law enforcement also reported 30 vehicles stuck due to flowing water in a wash near Ogilby Road about 10 miles northeast of Glamis. Later in the evening, around 1945PST, there was a public report of flash flooding in Brawley where water at least one foot deep was overflowing an embankment. Multiple Flash Flood Warnings were issued; fortunately there were no reports of injuries due to the flash flooding. Scattered thunderstorms developed across the eastern portion of Imperial County during the afternoon hours on September 25th. The stronger storms generated heavy rainfall with peak rain rates in excess of one inch per hour. The heavy rain resulted in some flash flooding that affected motorists on Ogilby Road to the south of State Route 78. According to the California Highway Patrol, at 1632PST flash flooding resulted in a vehicle being washed out along Ogilby Road just south of State Route 78, and about 10 miles east-northeast of the town of Glamis. The driver was not injured and was helped out of the vehicle. Additionally, 30 more vehicles were also stopped and stuck before a flowing wash in the vicinity. A Flash Flood Warning had been issued at 1436PST and was in effect at the time of the flooding.", "ts_dict_index": [1542, 1543, 1544]}
+{"event_id": 852831, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2019-09-25 19:30:00", "end_date_time": "2019-09-25 22:00:00", "narrative": "Scattered thunderstorms developed across the lower deserts of Imperial County - from the Imperial Valley eastward to the lower Colorado River valley - during the afternoon and evening hours on September 25th. Instability was elevated due to the close proximity of an upper level low pressure system and cool air aloft, and the increased instability aided the thunderstorm development. As was the case over the past couple of days, the stronger thunderstorms primarily generated very heavy rain with peak rain rates well in excess of one inch per hour. Multiple reports from the California Highway Patrol indicated that flash flooding was occurring along State Route 78, from near the Cibola National Wildlife Refuge south to near Interstate 8. Local law enforcement also reported 30 vehicles stuck due to flowing water in a wash near Ogilby Road about 10 miles northeast of Glamis. Later in the evening, around 1945PST, there was a public report of flash flooding in Brawley where water at least one foot deep was overflowing an embankment. Multiple Flash Flood Warnings were issued; fortunately there were no reports of injuries due to the flash flooding. Scattered thunderstorms continued to develop across the central portions of Imperial County during the evening hours on September 25th. Some of the stronger storms generated very heavy rain with peak rain rates in excess of one inch per hour. The heavy rain resulted in some flash flooding that impacted portions of the Imperial Valley including the town of Brawley. According to a report from the public, at 1945PST flash flooding was occurring on 1st Street in Brawley. Water at least one foot deep was observed flowing over an embankment. There were no reports of accidents or injury due to the flooding. A Flash Flood Warning was in effect at the time of the report, and was initially issued at 1804PST.", "ts_dict_index": [1539, 1540, 1541]}
+{"event_id": 852828, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2019-09-25 15:30:00", "end_date_time": "2019-09-25 18:30:00", "narrative": "Scattered thunderstorms developed across the lower deserts of Imperial County - from the Imperial Valley eastward to the lower Colorado River valley - during the afternoon and evening hours on September 25th. Instability was elevated due to the close proximity of an upper level low pressure system and cool air aloft, and the increased instability aided the thunderstorm development. As was the case over the past couple of days, the stronger thunderstorms primarily generated very heavy rain with peak rain rates well in excess of one inch per hour. Multiple reports from the California Highway Patrol indicated that flash flooding was occurring along State Route 78, from near the Cibola National Wildlife Refuge south to near Interstate 8. Local law enforcement also reported 30 vehicles stuck due to flowing water in a wash near Ogilby Road about 10 miles northeast of Glamis. Later in the evening, around 1945PST, there was a public report of flash flooding in Brawley where water at least one foot deep was overflowing an embankment. Multiple Flash Flood Warnings were issued; fortunately there were no reports of injuries due to the flash flooding. Scattered showers and thunderstorms developed across eastern portions of Imperial County during the afternoon hours on September 25th. Some of the stronger storms generated very heavy rain with peak rain rates in excess of one inch per hour. The heavy rain led to some flash flooding around the town of Glamis. According to the California Highway Patrol, at about 1544MST flash flooding forced the closure of State Route 78 at Ted Kipf Road, about one mile east of town. No accidents were reported due to the flooding. A Flash Flood Warning had been issued prior to the report of the flash flooding.", "ts_dict_index": [1551, 1552, 1553]}
+{"event_id": 852823, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2019-09-25 15:00:00", "end_date_time": "2019-09-25 19:30:00", "narrative": "Scattered thunderstorms developed across the lower deserts of Imperial County - from the Imperial Valley eastward to the lower Colorado River valley - during the afternoon and evening hours on September 25th. Instability was elevated due to the close proximity of an upper level low pressure system and cool air aloft, and the increased instability aided the thunderstorm development. As was the case over the past couple of days, the stronger thunderstorms primarily generated very heavy rain with peak rain rates well in excess of one inch per hour. Multiple reports from the California Highway Patrol indicated that flash flooding was occurring along State Route 78, from near the Cibola National Wildlife Refuge south to near Interstate 8. Local law enforcement also reported 30 vehicles stuck due to flowing water in a wash near Ogilby Road about 10 miles northeast of Glamis. Later in the evening, around 1945PST, there was a public report of flash flooding in Brawley where water at least one foot deep was overflowing an embankment. Multiple Flash Flood Warnings were issued; fortunately there were no reports of injuries due to the flash flooding. Scattered thunderstorms developed across the eastern portion of Imperial County during the afternoon hours on September 25th. Some of the stronger storms produced heavy rain, with peak rain rates in excess of one inch per hour. The heavy rain resulted in flash flooding along State Route 78 to the south-southwest of the town of Palo Verde. According to a report from the California Highway Patrol, at 1509PST flash flooding 10 miles southwest of Palo Verde forced the closure of State Route 78. The road was closed so that Caltrans would be able to clear debris off of the road. Flash flooding allowed water to rise 2.5 feet above the road at the Milpitas Wash Road.  Additionally, a bit earlier at 1427PST the California Highway Patrol indicated that State Route 78 was closed near Mile Marker 71 due to moderate flash flooding. There were no reports of accidents or injuries due to the flash flooding. A Flash Flood Warning was issued at 1500PST for areas just east of the flooding, and a second warning was put out at 1604PST that covered areas affected by the flooding.", "ts_dict_index": [1548, 1549, 1550]}
+{"event_id": 824462, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2019-05-20 22:07:00", "end_date_time": "2019-05-21 01:45:00", "narrative": "A strong upper level storm system moved into the Southern Plains from the Rockies on the 20th and 21st. The attendant warm front moved from northern Texas northward into northeastern Oklahoma during the day on the 20th, and then the cold front associated with this storm system moved through eastern Oklahoma during the late evening of the 20th and early morning hours of the 21st. Warm, moist, and very unstable air resided across eastern Oklahoma ahead of this system. This pattern resulted in multiple rounds of severe thunderstorms across eastern Oklahoma from the early afternoon of the 20th through late morning of the 21st. Very strong wind shear coexisting with the strong instability resulted in some supercell thunderstorms that produced large hail up to golfball size and multiple tornadoes on the 20th. A squall line developed along the cold front that moved into the area during the morning of the 21st, and that line of storms produced multiple tornadoes along the leading edge. Locally heavy rainfall and subsequent flash flooding occurred across northeastern Oklahoma as multiple rounds of thunderstorms affected generally the same area. Portions of E 51st Street S were flooded.", "ts_dict_index": [1557, 1558, 1559]}
+{"event_id": 824464, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2019-05-20 22:10:00", "end_date_time": "2019-05-21 01:45:00", "narrative": "A strong upper level storm system moved into the Southern Plains from the Rockies on the 20th and 21st. The attendant warm front moved from northern Texas northward into northeastern Oklahoma during the day on the 20th, and then the cold front associated with this storm system moved through eastern Oklahoma during the late evening of the 20th and early morning hours of the 21st. Warm, moist, and very unstable air resided across eastern Oklahoma ahead of this system. This pattern resulted in multiple rounds of severe thunderstorms across eastern Oklahoma from the early afternoon of the 20th through late morning of the 21st. Very strong wind shear coexisting with the strong instability resulted in some supercell thunderstorms that produced large hail up to golfball size and multiple tornadoes on the 20th. A squall line developed along the cold front that moved into the area during the morning of the 21st, and that line of storms produced multiple tornadoes along the leading edge. Locally heavy rainfall and subsequent flash flooding occurred across northeastern Oklahoma as multiple rounds of thunderstorms affected generally the same area. Numerous streets were flooded and closed across the City of Owasso.", "ts_dict_index": [1566, 1567, 1568]}
+{"event_id": 853020, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2019-09-25 14:30:00", "end_date_time": "2019-09-25 18:30:00", "narrative": "Scattered thunderstorms developed across the lower deserts of Imperial County - from the Imperial Valley eastward to the lower Colorado River valley - during the afternoon and evening hours on September 25th. Instability was elevated due to the close proximity of an upper level low pressure system and cool air aloft, and the increased instability aided the thunderstorm development. As was the case over the past couple of days, the stronger thunderstorms primarily generated very heavy rain with peak rain rates well in excess of one inch per hour. Multiple reports from the California Highway Patrol indicated that flash flooding was occurring along State Route 78, from near the Cibola National Wildlife Refuge south to near Interstate 8. Local law enforcement also reported 30 vehicles stuck due to flowing water in a wash near Ogilby Road about 10 miles northeast of Glamis. Later in the evening, around 1945PST, there was a public report of flash flooding in Brawley where water at least one foot deep was overflowing an embankment. Multiple Flash Flood Warnings were issued; fortunately there were no reports of injuries due to the flash flooding. Scattered thunderstorms developed across the eastern portion of Imperial County during the afternoon hours on September 25th. Some of the stronger storms generated heavy rain, with peak rain rates in excess of one inch per hour. The heavy rain led to some flash flooding along Ogilby Road between State Route 78 and Interstate 8. According to the California Highway Patrol, at 1449PST flash flooding along Ogilby Road resulted in the road becoming closed from Interstate 8 through State Route 78 due to a flooded wash covering the road in between those points. Due to the road closure, no vehicles were able to drive through the flooded wash and no accidents were reported. A Flash Flood Warning was issued, but for areas to the north of the flooded wash.", "ts_dict_index": [1545, 1546, 1547]}
+{"event_id": 824360, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2019-05-20 20:18:00", "end_date_time": "2019-05-21 01:45:00", "narrative": "A strong upper level storm system moved into the Southern Plains from the Rockies on the 20th and 21st. The attendant warm front moved from northern Texas northward into northeastern Oklahoma during the day on the 20th, and then the cold front associated with this storm system moved through eastern Oklahoma during the late evening of the 20th and early morning hours of the 21st. Warm, moist, and very unstable air resided across eastern Oklahoma ahead of this system. This pattern resulted in multiple rounds of severe thunderstorms across eastern Oklahoma from the early afternoon of the 20th through late morning of the 21st. Very strong wind shear coexisting with the strong instability resulted in some supercell thunderstorms that produced large hail up to golfball size and multiple tornadoes on the 20th. A squall line developed along the cold front that moved into the area during the morning of the 21st, and that line of storms produced multiple tornadoes along the leading edge. Locally heavy rainfall and subsequent flash flooding occurred across northeastern Oklahoma as multiple rounds of thunderstorms affected generally the same area. Portions of N Memorial Drive were flooded and closed.", "ts_dict_index": [1569, 1570, 1571]}
+{"event_id": 824354, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2019-05-20 19:54:00", "end_date_time": "2019-05-21 01:45:00", "narrative": "A strong upper level storm system moved into the Southern Plains from the Rockies on the 20th and 21st. The attendant warm front moved from northern Texas northward into northeastern Oklahoma during the day on the 20th, and then the cold front associated with this storm system moved through eastern Oklahoma during the late evening of the 20th and early morning hours of the 21st. Warm, moist, and very unstable air resided across eastern Oklahoma ahead of this system. This pattern resulted in multiple rounds of severe thunderstorms across eastern Oklahoma from the early afternoon of the 20th through late morning of the 21st. Very strong wind shear coexisting with the strong instability resulted in some supercell thunderstorms that produced large hail up to golfball size and multiple tornadoes on the 20th. A squall line developed along the cold front that moved into the area during the morning of the 21st, and that line of storms produced multiple tornadoes along the leading edge. Locally heavy rainfall and subsequent flash flooding occurred across northeastern Oklahoma as multiple rounds of thunderstorms affected generally the same area. E 86th Street N was flooded at N 145th E Avenue.", "ts_dict_index": [1554, 1555, 1556]}
+{"event_id": 824467, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2019-05-20 22:10:00", "end_date_time": "2019-05-21 01:45:00", "narrative": "A strong upper level storm system moved into the Southern Plains from the Rockies on the 20th and 21st. The attendant warm front moved from northern Texas northward into northeastern Oklahoma during the day on the 20th, and then the cold front associated with this storm system moved through eastern Oklahoma during the late evening of the 20th and early morning hours of the 21st. Warm, moist, and very unstable air resided across eastern Oklahoma ahead of this system. This pattern resulted in multiple rounds of severe thunderstorms across eastern Oklahoma from the early afternoon of the 20th through late morning of the 21st. Very strong wind shear coexisting with the strong instability resulted in some supercell thunderstorms that produced large hail up to golfball size and multiple tornadoes on the 20th. A squall line developed along the cold front that moved into the area during the morning of the 21st, and that line of storms produced multiple tornadoes along the leading edge. Locally heavy rainfall and subsequent flash flooding occurred across northeastern Oklahoma as multiple rounds of thunderstorms affected generally the same area. Numerous streets were flooded and closed across Collinsville.", "ts_dict_index": [1563, 1564, 1565]}
+{"event_id": 825196, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2019-05-21 03:00:00", "end_date_time": "2019-05-21 04:45:00", "narrative": "A strong upper level storm system moved into the Southern Plains from the Rockies on the 20th and 21st. The attendant warm front moved from northern Texas northward into northeastern Oklahoma during the day on the 20th, and then the cold front associated with this storm system moved through eastern Oklahoma during the late evening of the 20th and early morning hours of the 21st. Warm, moist, and very unstable air resided across eastern Oklahoma ahead of this system. This pattern resulted in multiple rounds of severe thunderstorms across eastern Oklahoma from the early afternoon of the 20th through late morning of the 21st. Very strong wind shear coexisting with the strong instability resulted in some supercell thunderstorms that produced large hail up to golfball size and multiple tornadoes on the 20th. A squall line developed along the cold front that moved into the area during the morning of the 21st, and that line of storms produced multiple tornadoes along the leading edge. Locally heavy rainfall and subsequent flash flooding occurred across northeastern Oklahoma as multiple rounds of thunderstorms affected generally the same area. A number of streets were flooded and closed across the City of Tulsa.", "ts_dict_index": [1560, 1561, 1562]}
+{"event_id": 849955, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2019-09-23 06:00:00", "end_date_time": "2019-09-23 10:45:00", "narrative": "During the early morning hours on September 23rd, copious tropical moisture began to spread north and into south-central Arizona. A weather system dropping south out of Nevada began to act on the moisture, resulting in the development of numerous showers and thunderstorms. Some of the storms produced copious amounts of rain with peak rain rates in excess of 2 inches per hour. Many locations across the high terrain east of Phoenix measured more than 3 inches of rain during the morning hours. Multiple events of flash flooding occurred in locations such as Apache Junction, Tortilla Flat, Fountain Hills and terrain to the south and east of Lake Roosevelt. As an example, at 0730MST a local emergency manager reported that 7 homes were flooded in Roosevelt Estates as Campaign Creek overflowed its banks. Several Flash Flood Warnings were issued for areas to the east of Phoenix during the morning hours. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Copious amounts of tropical moisture spread northward and into the high terrain areas east of Phoenix during the early morning hours on September 23rd and as a result, numerous showers and thunderstorms developed. Many storm produced heavy rain with peak rain rates in excess of 2 inches per hour. The heavy rain resulted in episodes of flash flooding, affecting areas to the south and east of Lake Roosevelt including Tonto National Monument. At 0700MST a federal agency reported flash flooding on the upper cliff dwelling trail about 2 miles southeast of Roosevelt. Shortly thereafter, at 0730MST, a local emergency manager located 8 miles east-southeast of Roosevelt reported that 7 homes were flooded in Roosevelt Estates as Campaign Creek overflowed its banks. As much as 18 inches of water was reported in one of the houses. Fortunately there were no reports of injuries. Two Flash Flood Warnings were issued for the area, the first was issued at 0609MST and the second at 0652MST.", "ts_dict_index": [1530, 1531, 1532]}
+{"event_id": 948586, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-05-09 20:00:00", "end_date_time": "2021-05-10 04:00:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. FM 95 was flooded just south of County Road 486.", "ts_dict_index": [1503, 1504, 1505]}
+{"event_id": 824468, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2019-05-20 22:25:00", "end_date_time": "2019-05-21 01:45:00", "narrative": "A strong upper level storm system moved into the Southern Plains from the Rockies on the 20th and 21st. The attendant warm front moved from northern Texas northward into northeastern Oklahoma during the day on the 20th, and then the cold front associated with this storm system moved through eastern Oklahoma during the late evening of the 20th and early morning hours of the 21st. Warm, moist, and very unstable air resided across eastern Oklahoma ahead of this system. This pattern resulted in multiple rounds of severe thunderstorms across eastern Oklahoma from the early afternoon of the 20th through late morning of the 21st. Very strong wind shear coexisting with the strong instability resulted in some supercell thunderstorms that produced large hail up to golfball size and multiple tornadoes on the 20th. A squall line developed along the cold front that moved into the area during the morning of the 21st, and that line of storms produced multiple tornadoes along the leading edge. Locally heavy rainfall and subsequent flash flooding occurred across northeastern Oklahoma as multiple rounds of thunderstorms affected generally the same area. N Lewis Avenue was flooded near E 41st Street N.", "ts_dict_index": [1572, 1573, 1574]}
+{"event_id": 824524, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2019-05-20 22:31:00", "end_date_time": "2019-05-21 01:45:00", "narrative": "A strong upper level storm system moved into the Southern Plains from the Rockies on the 20th and 21st. The attendant warm front moved from northern Texas northward into northeastern Oklahoma during the day on the 20th, and then the cold front associated with this storm system moved through eastern Oklahoma during the late evening of the 20th and early morning hours of the 21st. Warm, moist, and very unstable air resided across eastern Oklahoma ahead of this system. This pattern resulted in multiple rounds of severe thunderstorms across eastern Oklahoma from the early afternoon of the 20th through late morning of the 21st. Very strong wind shear coexisting with the strong instability resulted in some supercell thunderstorms that produced large hail up to golfball size and multiple tornadoes on the 20th. A squall line developed along the cold front that moved into the area during the morning of the 21st, and that line of storms produced multiple tornadoes along the leading edge. Locally heavy rainfall and subsequent flash flooding occurred across northeastern Oklahoma as multiple rounds of thunderstorms affected generally the same area. N Lewis Avenue was flooded near E 66th Street N where water rescues were conducted. Multiple other roads in and around Turley were flooded and closed.", "ts_dict_index": [1581, 1582, 1583]}
+{"event_id": 825379, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2019-05-21 06:50:00", "end_date_time": "2019-05-21 10:30:00", "narrative": "A strong upper level storm system moved into the Southern Plains from the Rockies on the 20th and 21st. The attendant warm front moved from northern Texas northward into northeastern Oklahoma during the day on the 20th, and then the cold front associated with this storm system moved through eastern Oklahoma during the late evening of the 20th and early morning hours of the 21st. Warm, moist, and very unstable air resided across eastern Oklahoma ahead of this system. This pattern resulted in multiple rounds of severe thunderstorms across eastern Oklahoma from the early afternoon of the 20th through late morning of the 21st. Very strong wind shear coexisting with the strong instability resulted in some supercell thunderstorms that produced large hail up to golfball size and multiple tornadoes on the 20th. A squall line developed along the cold front that moved into the area during the morning of the 21st, and that line of storms produced multiple tornadoes along the leading edge. Locally heavy rainfall and subsequent flash flooding occurred across northeastern Oklahoma as multiple rounds of thunderstorms affected generally the same area. A portion of E 86th Street N near Centennial Park was flooded and closed.", "ts_dict_index": [1575, 1576, 1577]}
+{"event_id": 965685, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-07-19 12:00:00", "end_date_time": "2021-07-19 15:00:00", "narrative": "A band of showers and thunderstorms developed during the early morning hours of July 19th across portions of Southeast Oklahoma and Southwest Arkansas, near a weak surface front and associated upper level trough that slowly sank south into East Texas and North Louisiana by/shortly after daybreak. Given the high moisture content available, adequate forcing aloft and available weak to moderate instability contributed to these storms becoming efficient rainfall producers, resulting in periods of heavy rain falling over portions of East Texas as additional showers and thunderstorms developed and spread southeast over the same areas of East Texas even through the early afternoon. Widespread rainfall amounts of three to six inches fell across Smith and Gregg Counties, with isolated higher amounts in excess of seven inches recorded over Northern Smith County. This resulted in flash flooding across the cities of Lindale and Longview, with high water rescues needed for stranded motorists in the flood waters. These showers and thunderstorms eventually diminished during the mid and late afternoon hours with the passage of the weak front. Flooding reported on County Roads 468 and 463 along with several other roads.", "ts_dict_index": [1590, 1591, 1592]}
+{"event_id": 965686, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-07-19 12:30:00", "end_date_time": "2021-07-19 15:00:00", "narrative": "A band of showers and thunderstorms developed during the early morning hours of July 19th across portions of Southeast Oklahoma and Southwest Arkansas, near a weak surface front and associated upper level trough that slowly sank south into East Texas and North Louisiana by/shortly after daybreak. Given the high moisture content available, adequate forcing aloft and available weak to moderate instability contributed to these storms becoming efficient rainfall producers, resulting in periods of heavy rain falling over portions of East Texas as additional showers and thunderstorms developed and spread southeast over the same areas of East Texas even through the early afternoon. Widespread rainfall amounts of three to six inches fell across Smith and Gregg Counties, with isolated higher amounts in excess of seven inches recorded over Northern Smith County. This resulted in flash flooding across the cities of Lindale and Longview, with high water rescues needed for stranded motorists in the flood waters. These showers and thunderstorms eventually diminished during the mid and late afternoon hours with the passage of the weak front. Driver pulled over on County Road 468 to avoid high water and water rose around him within minutes, trapping him inside his vehicle. Lindale Fire Department performed a high water rescue.", "ts_dict_index": [1587, 1588, 1589]}
+{"event_id": 824415, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2019-05-20 20:36:00", "end_date_time": "2019-05-21 01:45:00", "narrative": "A strong upper level storm system moved into the Southern Plains from the Rockies on the 20th and 21st. The attendant warm front moved from northern Texas northward into northeastern Oklahoma during the day on the 20th, and then the cold front associated with this storm system moved through eastern Oklahoma during the late evening of the 20th and early morning hours of the 21st. Warm, moist, and very unstable air resided across eastern Oklahoma ahead of this system. This pattern resulted in multiple rounds of severe thunderstorms across eastern Oklahoma from the early afternoon of the 20th through late morning of the 21st. Very strong wind shear coexisting with the strong instability resulted in some supercell thunderstorms that produced large hail up to golfball size and multiple tornadoes on the 20th. A squall line developed along the cold front that moved into the area during the morning of the 21st, and that line of storms produced multiple tornadoes along the leading edge. Locally heavy rainfall and subsequent flash flooding occurred across northeastern Oklahoma as multiple rounds of thunderstorms affected generally the same area. Several streets were flooded and closed from W 96th Street N to W 106th Street N in Sperry.", "ts_dict_index": [1578, 1579, 1580]}
+{"event_id": 849957, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 05:00:00", "end_date_time": "2019-09-23 10:00:00", "narrative": "During the early morning hours on September 23rd, copious tropical moisture began to spread north and into south-central Arizona. A weather system dropping south out of Nevada began to act on the moisture, resulting in the development of numerous showers and thunderstorms. Some of the storms produced copious amounts of rain with peak rain rates in excess of 2 inches per hour. Many locations across the high terrain east of Phoenix measured more than 3 inches of rain during the morning hours. Multiple events of flash flooding occurred in locations such as Apache Junction, Tortilla Flat, Fountain Hills and terrain to the south and east of Lake Roosevelt. As an example, at 0730MST a local emergency manager reported that 7 homes were flooded in Roosevelt Estates as Campaign Creek overflowed its banks. Several Flash Flood Warnings were issued for areas to the east of Phoenix during the morning hours. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Copious amounts of tropical moisture spread northward and into south-central Arizona during the early morning hours on September 23rd, leading to the development of numerous showers and thunderstorms over higher terrain areas east of Phoenix. Locally heavy rain developed, with peak rain rates in excess of 2 inches per hour. By mid morning, a number of locations had already received more than 3 inches of rain. The  heavy rain led to episodes of flash flooding from Tortilla Flat eastward. At 0605MST, the Fish Creek USGS stream gage 5 miles east of Tortilla Flat reported an increase from 5 feet to 9.5 feet. At 0615MST, Arizona Department of Highways reported that State Route 88 was closed indefinitely between Tortilla Flat and State Route 188. The closure was due to flash flooding as well as debris across the road. Additionally, at 0748MST a member of the public reported flash flooding along Lewis and Pranty Creek near State Route 88. This occurred roughly 7 miles east of Tortilla Flat and south of Apache Lake. The report also indicated that water had jumped out of the creek's banks and was inundating one of the properties in the area. Multiple Flash Flood Warnings were issued during the morning and were in effect at the time of the flooding. No injuries were reported fortunately.", "ts_dict_index": [1536, 1537, 1538]}
+{"event_id": 868962, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-02-12 08:00:00", "end_date_time": "2020-02-12 12:30:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in numerous instances of flash flooding across East and Northeast Texas, with numerous roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. Grande Blvd west of Old Grande Blvd was flooded.", "ts_dict_index": [1623, 1624, 1625]}
+{"event_id": 868981, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-02-12 08:00:00", "end_date_time": "2020-02-12 12:30:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in numerous instances of flash flooding across East and Northeast Texas, with numerous roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. Cumberland Road was closed due to flooding from Shackleford Creek.", "ts_dict_index": [1617, 1618, 1619]}
+{"event_id": 869003, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2020-02-12 09:14:00", "end_date_time": "2020-02-12 10:45:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in instances of flash flooding across portions of Southwest Arkansas, with several roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. County Road 18 was closed due to flooding.", "ts_dict_index": [1632, 1633, 1634]}
+{"event_id": 868976, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-02-12 08:00:00", "end_date_time": "2020-02-12 12:30:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in numerous instances of flash flooding across East and Northeast Texas, with numerous roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. A vehicle was submerged in high water due to flooding from Carter Creek at the intersection of Highway 271 and County Road 3110.", "ts_dict_index": [1608, 1609, 1610]}
+{"event_id": 868989, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-02-12 09:15:00", "end_date_time": "2020-02-12 12:30:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in numerous instances of flash flooding across East and Northeast Texas, with numerous roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. Both the north and south bound lanes of Highway 69 were closed due to flooding.", "ts_dict_index": [1611, 1612, 1613]}
+{"event_id": 868994, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-02-12 10:30:00", "end_date_time": "2020-02-12 12:30:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in numerous instances of flash flooding across East and Northeast Texas, with numerous roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. A high water rescue was performed on FM 346 near County Line Creek.", "ts_dict_index": [1620, 1621, 1622]}
+{"event_id": 869004, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2020-02-12 09:15:00", "end_date_time": "2020-02-12 10:45:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in instances of flash flooding across portions of Southwest Arkansas, with several roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. County Roads 5, 13, 18, and State Highway 313 were flooded.", "ts_dict_index": [1629, 1630, 1631]}
+{"event_id": 869000, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-02-12 08:00:00", "end_date_time": "2020-02-12 12:30:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in numerous instances of flash flooding across East and Northeast Texas, with numerous roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. FM 3311 north of I-20 over Wiggins Creek was washed out.", "ts_dict_index": [1596, 1597, 1598]}
+{"event_id": 868998, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-02-12 08:00:00", "end_date_time": "2020-02-12 12:30:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in numerous instances of flash flooding across East and Northeast Texas, with numerous roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. High water over FM 1252 between Highway 370 to just west of Barber Road.", "ts_dict_index": [1602, 1603, 1604]}
+{"event_id": 868974, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-02-12 08:00:00", "end_date_time": "2020-02-12 12:30:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in numerous instances of flash flooding across East and Northeast Texas, with numerous roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. Highway 271 was flooded just south of I-20.", "ts_dict_index": [1599, 1600, 1601]}
+{"event_id": 868955, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-02-12 07:30:00", "end_date_time": "2020-02-12 12:30:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in numerous instances of flash flooding across East and Northeast Texas, with numerous roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. A vehicle was submerged in high water on Greenbriar Road at Butler Creek just north of Lake Placid Road.", "ts_dict_index": [1614, 1615, 1616]}
+{"event_id": 869002, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2020-02-12 09:10:00", "end_date_time": "2020-02-12 10:45:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in instances of flash flooding across portions of Southwest Arkansas, with several roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. County Road 28 was closed due to flooding from Bodcau Creek.", "ts_dict_index": [1626, 1627, 1628]}
+{"event_id": 856900, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-11-20 06:31:00", "end_date_time": "2019-11-20 10:15:00", "narrative": "The low pressure center which approached the California coast on November 19 moved inland across southern California on November 20. This system produced widespread precipitation across the area with the most significant precipitation impacting Kern and Tulare Counties. Flooding along State Route 99 in the Wheeler Ridge and Mettler areas resulted in the highway being closed for a period of time. The Grapevine and Frazier Park areas generally picked up between half and inch and an inch of liquid precipitation while many locations in the Tehachapi and Lake Isabella areas and the Kern County Deserts as well as the southern Sierra Nevada in Tulare County picked up between a quarter inch and a half inch of precipitation. The snow level was generally around 6000 feet, but briefly lowered to 5000 feet at times in heavier showers. Most locations in the mountains in Kern and Tulare Counties above 6000 feet picked up between 6 and 9 inches of snow while there were some locally higher accumulations around Pine Mountain Club. Further north, precipitation amounts were much lower with most locations picking up less than a tenth of an inch. California Highway Patrol reported flash flooding on State Route 99 just north of the intersection with Interstate 5 near Wheeler Ridge. Mud and Debris blocked the northbound lanes and two of the southbound lanes resulting in State Route 99 being closed from the Interstate 5 intersection to Mettler until late morning.", "ts_dict_index": [1593, 1594, 1595]}
+{"event_id": 982465, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:50:00", "end_date_time": "2021-08-14 04:50:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Multiple streamflow gages along Indian Bend Wash exceeded action or alarm stage, particularly between Highway-51 and Scottsdale Road. Streamflow gages crested around 3 to 5 feet and most did not fall below action or alarm until midday on the 14th. The USGS gage at Sweetwater Avenue recorded a roughly 4 foot rise in 30 minutes and crested at 3.95 feet. Rainfall amounts between 1.5 to 2.5 inches were measured upstream just west of Highway-51. No damages or injuries were reported.", "ts_dict_index": [1650, 1651, 1652]}
+{"event_id": 982533, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:20:00", "end_date_time": "2021-08-14 00:20:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Photo on social media shows two unoccupied sedans floating in flood water near Helena Drive and 2nd Street. Flood water continued down the water channel and spilled into the apartment complex on Bell Road and Central Avenue. Broadcast media reported multiple ground floor apartments experienced flood damage with an estimated 4 feet of water moving through them. Extent of the damages and number of apartments affected was not reported. Time estimated from radar. No injuries were reported.", "ts_dict_index": [1647, 1648, 1649]}
+{"event_id": 982508, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2021-08-14 00:40:00", "end_date_time": "2021-08-14 03:40:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Highway 72 was flooded and impassable near Bouse. Timing adjusted based on radar. No damages or injuries were reported.", "ts_dict_index": [1644, 1645, 1646]}
+{"event_id": 982518, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-14 01:20:00", "end_date_time": "2021-08-14 06:20:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Maricopa County Department of Transportation reported at 0226MST that Agua Caliente Road, a dirt road, was closed between Old US 80 to Lahman Road due to flooding. Timing of impacts adjusted based on radar and location focused on area with greatest radar rainfall estimates. No damages or injuries were reported.", "ts_dict_index": [1635, 1636, 1637]}
+{"event_id": 983722, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:50:00", "end_date_time": "2021-08-14 00:50:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Arizona Department of Transportation reported State Route 88 was closed in both directions between mile posts 229 and 242 due to flooding. Timing estimated based on radar. No damages or injuries were reported.", "ts_dict_index": [1641, 1642, 1643]}
+{"event_id": 850051, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 05:00:00", "end_date_time": "2019-09-23 09:45:00", "narrative": "During the early morning hours on September 23rd, copious tropical moisture began to spread north and into south-central Arizona. A weather system dropping south out of Nevada began to act on the moisture, resulting in the development of numerous showers and thunderstorms. Some of the storms produced copious amounts of rain with peak rain rates in excess of 2 inches per hour. Many locations across the high terrain east of Phoenix measured more than 3 inches of rain during the morning hours. Multiple events of flash flooding occurred in locations such as Apache Junction, Tortilla Flat, Fountain Hills and terrain to the south and east of Lake Roosevelt. As an example, at 0730MST a local emergency manager reported that 7 homes were flooded in Roosevelt Estates as Campaign Creek overflowed its banks. Several Flash Flood Warnings were issued for areas to the east of Phoenix during the morning hours. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Copious amounts of tropical moisture spread north and into south central Arizona during the early morning hours on September 23rd, resulting in scattered to numerous showers and thunderstorms. Peak rain rates with the stronger convective cells was in excess of 2 inches per hour; the heavy rain resulted in episodes of flash flooding east of Phoenix, affecting communities such as East Mesa and Apache Junction. According to a trained spotter located about 4 miles southeast of East Mesa, at 0525MST flash flooding caused several streets to flood and an area wash was filled with several feet of water. The flooding was west of Crismon Road and between Broadway and Southern. At 0630MST, local broadcast media reported that flash flooding 1 mile southwest of Apache Junction resulted in the closure of 16th Avenue between Delaware and Ironwood Drive. The flooding occurred when a wash flowed across the road. Finally, at 0700MST local broadcast media reported an episode of flash flooding 3 miles west of Apache Junction. The flash flooding necessitated a water rescue of a stranded vehicle just north of Main Street and near Signal Butte Road. No injuries were reported for any of the flash flooding incidents. A Flash Flood Warning was issued at 0541MST and the warning covered most of the flooding incidents.", "ts_dict_index": [1533, 1534, 1535]}
+{"event_id": 982506, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-14 00:36:00", "end_date_time": "2021-08-14 01:50:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Report through mPing of impassable street flooding in the town of Maricopa. Additional details not reported.", "ts_dict_index": [1653, 1654, 1655]}
+{"event_id": 965687, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-07-19 12:35:00", "end_date_time": "2021-07-19 15:00:00", "narrative": "A band of showers and thunderstorms developed during the early morning hours of July 19th across portions of Southeast Oklahoma and Southwest Arkansas, near a weak surface front and associated upper level trough that slowly sank south into East Texas and North Louisiana by/shortly after daybreak. Given the high moisture content available, adequate forcing aloft and available weak to moderate instability contributed to these storms becoming efficient rainfall producers, resulting in periods of heavy rain falling over portions of East Texas as additional showers and thunderstorms developed and spread southeast over the same areas of East Texas even through the early afternoon. Widespread rainfall amounts of three to six inches fell across Smith and Gregg Counties, with isolated higher amounts in excess of seven inches recorded over Northern Smith County. This resulted in flash flooding across the cities of Lindale and Longview, with high water rescues needed for stranded motorists in the flood waters. These showers and thunderstorms eventually diminished during the mid and late afternoon hours with the passage of the weak front. Texas DPS reported that the Allen Branch Creek overpass at I-20 west near Lindale was eroded due to flooding, causing a large pine tree to fall on I-20 and resulting in 5 vehicles and a gooseneck trailer wrecking. Four injuries were reported, but none were life-threatening.", "ts_dict_index": [1584, 1585, 1586]}
+{"event_id": 983720, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 23:40:00", "end_date_time": "2021-08-14 01:00:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Video on social media shows at least 6 inches of swift-moving water flowing down 96th Street near Duncan Street. No damages of injuries were reported.", "ts_dict_index": [1659, 1660, 1661]}
+{"event_id": 982498, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 23:40:00", "end_date_time": "2021-08-14 01:40:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. The City of Surprise closed Jomax Road between 147th Avenue and El Granada Road due to flooding. No damages or injuries were reported. Timing based on radar.", "ts_dict_index": [1656, 1657, 1658]}
+{"event_id": 982441, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:50:00", "end_date_time": "2021-08-14 01:15:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Interstate-17 was closed in both directions due to significant standing water on the freeway near Indian School Road. Multiple cars also became stalled in the standing water. Interstate-17 was not fully reopened until approximately 0115MST on the 14th. No injuries were reported.", "ts_dict_index": [1662, 1663, 1664]}
+{"event_id": 982510, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-14 01:10:00", "end_date_time": "2021-08-14 07:10:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Arizona Department of Transportation reported via social media at 0202MST on the 14th that Highway-238 was closed in both directions between milepost 40 near Maricopa and State Route 85 near Gila Bend due to flooding. Heaviest rain, estimated around 2 to 3 inches, fell from the Maricopa mountains west toward Gila Bend. Highway-238 would remain closed through the 14th. Timing of impacts adjusted based on radar. No damages or injuries were reported.", "ts_dict_index": [1665, 1666, 1667]}
+{"event_id": 982495, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-13 23:50:00", "end_date_time": "2021-08-14 00:35:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Arizona Department of Transportation reported that US-60 was closed in both directions between Superior and Top-Of-The-World, specifically between mileposts 227 and 235, due to rocks on the roadway following heavy rainfall in the area. The highway was reopened around 0030MST on the 14th. No damages or injuries were reported.", "ts_dict_index": [1668, 1669, 1670]}
+{"event_id": 868959, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-02-12 07:30:00", "end_date_time": "2020-02-12 12:30:00", "narrative": "Areas of showers remained persistent across much of the Ark-La-Tex through much of the day on February 11th, along the subtropical jet stream that extended over much of Texas and the Lower Mississippi Valley ahead of a strong upper level low pressure system just off the Northwest Baja California coast. These rains primed the already wet soils on the 11th, before the low pressure system began to eject northeast and become absorbed into a broad upper trough as it translated east across the Southern Rockies into the Southern Plains during much of the day on the 12th. As this trough approached, an axis of moderate to locally heavy rainfall developed over Northeast Texas and Southern Arkansas, with widespread rainfall amounts of 4-6 inches, with isolated higher amounts up to 8 inches, observed. This resulted in numerous instances of flash flooding across East and Northeast Texas, with numerous roads flooded and closed, and smaller creeks, streams, and bayous spilling above its banks. The flash flooding ended by afternoon as the rains ended, but continued runoff resulted in continued flooding near and along these waterways. The northbound lane of Highway 110 was closed due to flooding from Hill Creek.", "ts_dict_index": [1605, 1606, 1607]}
+{"event_id": 982526, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-14 03:49:00", "end_date_time": "2021-08-14 06:30:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. A streamflow gage on Sauceda wash near Highway 85 exceeded alarm stage at 0349MST, with a peak flow of 1396 cfs and crest of 4.10 feet at 0509MST. The stage fell below alarm at 0552MST. With alarm stage flow, impacts to Watermelon Road just north of Interstate-8 can experience impacts, but none were reported. No damages or injuries were reported with this flow, but catastrophic impacts, including loss of life, were experienced in nearby Gila Bend from flooding of Sand Tank wash. See that event entry for details.", "ts_dict_index": [1671, 1672, 1673]}
+{"event_id": 982438, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:23:00", "end_date_time": "2021-08-14 04:23:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. The Greenway Road underpass at Interstate-17 flooded with a few feet of standing water and was closed as a result. Before being closed, a reported 5 vehicles stalled in the flood water, requiring a rescue. The underpass did not reopen until roughly noon on the 14th. No injuries were reported.", "ts_dict_index": [1680, 1681, 1682]}
+{"event_id": 982481, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 23:05:00", "end_date_time": "2021-08-14 01:00:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Interstate-17 was closed in both directions at the Durango Street curve due to standing water on the freeway, making it impassable. Interstate-17 did not fully reopen until approximately 0100MST on the 14th. No damages or injuries were reported.", "ts_dict_index": [1686, 1687, 1688]}
+{"event_id": 983721, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:23:00", "end_date_time": "2021-08-13 23:50:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Public report of flooding along 23rd Avenue between Dunlap Avenue and Northern Avenue. Video shows the intersection of 23rd Avenue and Butler Drive flooded with at least 6 inches of water. No damages or injuries were reported.", "ts_dict_index": [1689, 1690, 1691]}
+{"event_id": 983830, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-14 01:40:00", "end_date_time": "2021-08-14 10:30:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Following 2 to 4 inches of rain in 1 to 2 hours over the Sand Tank Wash watershed, catastrophic flooding occurred in the small town of Gila Bend with feet of water, mud, and debris moving through town. Storm surveys were completed by NWS Phoenix, Maricopa County Department of Emergency Management (MCDEM), American Red Cross, and Flood Control District of Maricopa County (FCDMC). FCDMC gages on Sand Tank Wash, Bender Wash, and in the Maricopa Mountains measured rainfall amounts around 3 to 4 inches in 1 to 2 hours for an annual exceedance probability of 0.1%. FCDMC found the most significant floodwaters were within Sand Tank Wash, with lesser flows in Bender and Scott Avenue Washes. The NWS Phoenix survey found evidence of out of bank flooding in Sand Tank Wash 1 to 3 miles south of Interstate-8 (I-8) with 2 to 6 feet of water and sizable debris. The streamflow gage on Sand Tank Wash at I-8 reached alarm stage at 0157MST, bank full at 0341MST, and flood stage at 0352MST. The gage crested at 7.69 feet with 5000 cfs of flow at 0408MST. The floodwaters and debris that moved through town caused flood damage to at least 140 homes and 25 businesses. Most structures impacted were between the Gila Bend Canal and Main Street and then along Pima Street. During the flooding, Maricopa County Sheriff's Office rescued at least 30 individuals from their roofs along with others pulled from stranded vehicles. Photos after the water receded showed the canal was eroded and breached where Sand Tank Wash flows over it. Photos also showed 2 to 5 foot water lines both on the outside and inside of many of the structures, piles of debris, damaged property and vehicles, and erosion. Of the homes MCDEM assessed, 21 were deemed uninhabitable after the flooding. Unfortunately there were 2 direct fatalities with this event. One made a heroic effort to save a stranded motorist before they themselves were swept away in their own vehicle. The other was swept away in one of the flooded washes. Additionally, many farm animals were killed. Besides the fatalities, no other injuries were reported. A state of emergency was declared for this event.", "ts_dict_index": [1683, 1684, 1685]}
+{"event_id": 982448, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:40:00", "end_date_time": "2021-08-14 01:30:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Video on social media showed significant flow in Ashbrook Wash over El Pueblo Boulevard just north of Grande Boulevard. In the video an uprooted mature palo verde tree was flowing across the road. The following morning it was found that a sedan had been swept off the road at some point during the night and crushed by debris, but the owner of the vehicle was able to escape. No injuries were reported.", "ts_dict_index": [1692, 1693, 1694]}
+{"event_id": 982519, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-14 02:41:00", "end_date_time": "2021-08-14 02:55:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. A streamflow gage on the Agua Fria River at Buckeye Road exceeded alarm stage at 0241MST with peak flow of 1932 cfs and a crest height of 0.79 feet. Impacts to the low water crossing at Lower Buckeye Road are common with this flow level, but no impacts were reported. No damages or injuries were reported.", "ts_dict_index": [1677, 1678, 1679]}
+{"event_id": 982494, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 23:40:00", "end_date_time": "2021-08-14 01:40:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. City of Surprise closed Cotton Lane between Peoria Avenue to Cactus Road due to flooding. No damages or injuries were reported.", "ts_dict_index": [1674, 1675, 1676]}
+{"event_id": 982493, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 23:10:00", "end_date_time": "2021-08-14 05:10:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Thunderbird Road from Interstate-17 to 35th Avenue flooded with 1 to 3 feet of standing water. At least one car became stranded in the underpass below Interstate-17. The underpass was closed for several hours. No injuries were reported.", "ts_dict_index": [1638, 1639, 1640]}
+{"event_id": 846391, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-08-10 10:41:00", "end_date_time": "2019-08-10 13:41:00", "narrative": "On the 7th, a front pushed into the region. Temperatures were in the 90s, and it was the hottest day of the year so far at some locations. At Little Rock (Pulaski County), for example, the mercury reached 99 degrees. It was also humid, and this created heat index values over 110 degrees in spots.||Relief came to parts of the state when hit and miss thunderstorms popped up in the afternoon. The storms gradually worked southward with the front, and unleashed more wind. ||A lone storm in western Arkansas cranked out 60 mph gusts about four miles northeast of Ozark (Franklin County). The same storm plowed through Paris (Logan County), and uprooted and snapped trees. There was tree debris on Highway 309.||On the 10th, precipitation setup from northwest into central Arkansas. Birdtown (Conway County) got 5.40 inches of rain, with 5.24 inches just southwest of Houston (Perry County), and 4.50 inches at Toad Suck (Perry County). ||At Little Rock (Pulaski County), 3.87 inches of liquid made it the wettest August day since 1978, and the 4th wettest calendar day in August. Records have been kept locally since 1874. Several high water rescues were performed across Little Rock due to flash flooding from heavy rainfall.", "ts_dict_index": [1701, 1702, 1703]}
+{"event_id": 987592, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:30:00", "end_date_time": "2021-09-01 22:00:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. The body of a man was found in Saxon Woods Park in White Plains after he exited his stranded car and was swept away by flood waters.", "ts_dict_index": [1713, 1714, 1715]}
+{"event_id": 987521, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:22:00", "end_date_time": "2021-09-01 22:30:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. Flood waters were up to the hoods of cars on Glen Avenue and Haseco Avenue in Port Chester.", "ts_dict_index": [1710, 1711, 1712]}
+{"event_id": 987519, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:12:00", "end_date_time": "2021-09-01 22:30:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. Several cars drove around barricades in Rye and are now stuck in flood waters.", "ts_dict_index": [1707, 1708, 1709]}
+{"event_id": 987589, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:30:00", "end_date_time": "2021-09-01 22:00:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. A 33 year old man from the Bronx died when he drove his vehicle into flood waters on South Columbus Avenue in Mount Vernon and became trapped.", "ts_dict_index": [1719, 1720, 1721]}
+{"event_id": 846390, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-08-10 09:05:00", "end_date_time": "2019-08-10 12:05:00", "narrative": "On the 7th, a front pushed into the region. Temperatures were in the 90s, and it was the hottest day of the year so far at some locations. At Little Rock (Pulaski County), for example, the mercury reached 99 degrees. It was also humid, and this created heat index values over 110 degrees in spots.||Relief came to parts of the state when hit and miss thunderstorms popped up in the afternoon. The storms gradually worked southward with the front, and unleashed more wind. ||A lone storm in western Arkansas cranked out 60 mph gusts about four miles northeast of Ozark (Franklin County). The same storm plowed through Paris (Logan County), and uprooted and snapped trees. There was tree debris on Highway 309.||On the 10th, precipitation setup from northwest into central Arkansas. Birdtown (Conway County) got 5.40 inches of rain, with 5.24 inches just southwest of Houston (Perry County), and 4.50 inches at Toad Suck (Perry County). ||At Little Rock (Pulaski County), 3.87 inches of liquid made it the wettest August day since 1978, and the 4th wettest calendar day in August. Records have been kept locally since 1874. Little Rock Fire Department reported flash flooding at a few points across Little Rock. Water rescues were performed at Hawthorne and Van Buren Streets in Little Rock. Additional reports of water rescues due to vehicles stranded in high water were coming into the fire department at the time of their report.", "ts_dict_index": [1698, 1699, 1700]}
+{"event_id": 987528, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:38:00", "end_date_time": "2021-09-01 22:30:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. The Hutchinson River Parkway was closed in both directions in Pelham due to flooding between the Cross County Parkway and I-95.", "ts_dict_index": [1716, 1717, 1718]}
+{"event_id": 984310, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-14 00:30:00", "end_date_time": "2021-08-14 03:30:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Photos on social media showed considerable tree debris washed up against a walking bridge along with washed out trails and picnic area at the Boyce Thompson Arboretum due to high flow in Queen Creek and/or Silver King Wash. As a result of the damage left behind from the flooding, the picnic area along with a couple of gardens and trails were closed. Further downstream, a USGS stream gage along Queen Creek below Whitlow Dam recorded a rapid rise near midnight going from the 13th into the 14th. Discontinuities in the data suggest that the flow in Queen Creek exceeded the gage's 6 ft maximum operating limit at around 0230MST when the gage recorded a height of 5.37 ft. Timing was estimated using the USGS gage. No injuries were reported.", "ts_dict_index": [1695, 1696, 1697]}
+{"event_id": 987428, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 18:37:00", "end_date_time": "2021-09-01 23:00:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. All lanes were closed in both directions due to flooding on US 9 in the vicinity of West Clinton Avenue in Irvington.", "ts_dict_index": [1761, 1762, 1763]}
+{"event_id": 987517, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 20:45:00", "end_date_time": "2021-09-01 22:30:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. The southbound Saw Mill River Parkway was flooded at Clarence Avenue in Hastings-on-Hudson.", "ts_dict_index": [1731, 1732, 1733]}
+{"event_id": 987581, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 22:44:00", "end_date_time": "2021-09-01 23:00:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. Route 202 was closed near Pine Grove Court in Yorktown Heights due to heavy flooding.", "ts_dict_index": [1722, 1723, 1724]}
+{"event_id": 987590, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:30:00", "end_date_time": "2021-09-01 22:00:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. The body of a 69 year old man was found near Route 119 near the Mario Cuomo Bridge in Tarrytown not far from where his car was found submerged.", "ts_dict_index": [1725, 1726, 1727]}
+{"event_id": 987573, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-02 01:42:00", "end_date_time": "2021-09-02 01:53:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. All lanes were closed due to flooding on the Saw Mill River Parkway northbound at the Ashford Avenue ramp in Ardsley.", "ts_dict_index": [1752, 1753, 1754]}
+{"event_id": 987591, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:30:00", "end_date_time": "2021-09-01 22:00:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. An elderly couple's vehicle was found pinned against a utility pole at the intersection of Lincoln Avenue and Brookside Way in Rye Brook. The couple are believed to have been swept away from their vehicle and down Blind Brook Creek and drowned.", "ts_dict_index": [1758, 1759, 1760]}
+{"event_id": 987555, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:00:00", "end_date_time": "2021-09-01 22:30:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. East Sunnyside Lane was flooded and impassable in Irvington with water more than a foot deep in spots. Widespread flooding was also occurring elsewhere in the village.", "ts_dict_index": [1737, 1738, 1739]}
+{"event_id": 987406, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 16:45:00", "end_date_time": "2021-09-01 17:15:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. All lanes were closed northbound due to flooding on the Saw Mill River Parkway between Marble Avenue (Exit 17) and Manville Road in Pleasantville.", "ts_dict_index": [1728, 1729, 1730]}
+{"event_id": 987457, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 20:30:00", "end_date_time": "2021-09-01 22:30:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. Widespread road closure along the Bronx River Parkway in Greenville due to flooding.", "ts_dict_index": [1746, 1747, 1748]}
+{"event_id": 995048, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:30:00", "end_date_time": "2021-09-01 22:00:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. Flash flooding resulted in an estimated $92.6 million in damages across Westchester County. This estimate includes $78 million in FEMA individual assistance to property owners, renters, and businesses and an additional $14.6 million in damages to Westchester County government infrastructure.", "ts_dict_index": [1734, 1735, 1736]}
+{"event_id": 987578, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:45:00", "end_date_time": "2021-09-01 22:30:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. The basement of a home on Thorne Place in Rye was flooding.", "ts_dict_index": [1764, 1765, 1766]}
+{"event_id": 987433, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 19:08:00", "end_date_time": "2021-09-01 23:00:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. The Bronx River Parkway was closed southbound in White Plains due to flooding.", "ts_dict_index": [1743, 1744, 1745]}
+{"event_id": 987426, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 18:14:00", "end_date_time": "2021-09-01 23:00:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. All lanes were closed in both directions on the Cross County Parkway in Yonkers due to flooding.", "ts_dict_index": [1749, 1750, 1751]}
+{"event_id": 987434, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 19:24:00", "end_date_time": "2021-09-01 23:00:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. Ashburton Avenue in Yonkers was closed near the Saw Mill River Parkway due to flooding.", "ts_dict_index": [1740, 1741, 1742]}
+{"event_id": 846388, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-08-10 08:50:00", "end_date_time": "2019-08-10 11:50:00", "narrative": "On the 7th, a front pushed into the region. Temperatures were in the 90s, and it was the hottest day of the year so far at some locations. At Little Rock (Pulaski County), for example, the mercury reached 99 degrees. It was also humid, and this created heat index values over 110 degrees in spots.||Relief came to parts of the state when hit and miss thunderstorms popped up in the afternoon. The storms gradually worked southward with the front, and unleashed more wind. ||A lone storm in western Arkansas cranked out 60 mph gusts about four miles northeast of Ozark (Franklin County). The same storm plowed through Paris (Logan County), and uprooted and snapped trees. There was tree debris on Highway 309.||On the 10th, precipitation setup from northwest into central Arkansas. Birdtown (Conway County) got 5.40 inches of rain, with 5.24 inches just southwest of Houston (Perry County), and 4.50 inches at Toad Suck (Perry County). ||At Little Rock (Pulaski County), 3.87 inches of liquid made it the wettest August day since 1978, and the 4th wettest calendar day in August. Records have been kept locally since 1874. Water was covering Hwy. 89.", "ts_dict_index": [1704, 1705, 1706]}
+{"event_id": 1097148, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2023-05-11 01:45:00", "end_date_time": "2023-05-11 10:45:00", "narrative": "An upper level low pressure system slowly ejected northeast across the piney woods of East Texas during the evening through the morning hours of May 10th-11th. A southerly low level jet present ahead of the low spilled copious amounts of low level moisture north into East Texas and Western Louisiana, with strong large scale forcing ahead of the low enhancing numerous shower and thunderstorm development which moved repeatedly over these areas throughout much of the overnight into the early morning hours. Widespread rainfall amounts of 3-6+ inches fell across much of Deep and extreme Eastern Texas through mid-morning on the 11th, resulting in instances of flash flooding across these areas. Catastrophic flash flooding was observed within the city of Nacogdoches, as these higher amounts fell over the city and atop the Bayou La Nana watershed, with the bayou quickly rising sharply 14.3 feet before cresting at 19.65 feet at 10 am on the 11th. This left much of Central Nacogdoches, including a portion of Stephen F. Austin State University, inundated, before the flood waters receded during the afternoon. Multiple streets were flooded and closed across the south side of Nacogdoches. Flooding of roads were widespread across Nacogdoches County.", "ts_dict_index": [1770, 1771, 1772]}
+{"event_id": 1097149, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2023-05-11 01:55:00", "end_date_time": "2023-05-11 10:45:00", "narrative": "An upper level low pressure system slowly ejected northeast across the piney woods of East Texas during the evening through the morning hours of May 10th-11th. A southerly low level jet present ahead of the low spilled copious amounts of low level moisture north into East Texas and Western Louisiana, with strong large scale forcing ahead of the low enhancing numerous shower and thunderstorm development which moved repeatedly over these areas throughout much of the overnight into the early morning hours. Widespread rainfall amounts of 3-6+ inches fell across much of Deep and extreme Eastern Texas through mid-morning on the 11th, resulting in instances of flash flooding across these areas. Catastrophic flash flooding was observed within the city of Nacogdoches, as these higher amounts fell over the city and atop the Bayou La Nana watershed, with the bayou quickly rising sharply 14.3 feet before cresting at 19.65 feet at 10 am on the 11th. This left much of Central Nacogdoches, including a portion of Stephen F. Austin State University, inundated, before the flood waters receded during the afternoon. The 3500 block of South Street in Nacogdoches was flooded and closed. A water rescue was needed for a stalled vehicle in the flood waters.", "ts_dict_index": [1773, 1774, 1775]}
+{"event_id": 1097175, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2023-05-11 09:00:00", "end_date_time": "2023-05-11 10:45:00", "narrative": "An upper level low pressure system slowly ejected northeast across the piney woods of East Texas during the evening through the morning hours of May 10th-11th. A southerly low level jet present ahead of the low spilled copious amounts of low level moisture north into East Texas and Western Louisiana, with strong large scale forcing ahead of the low enhancing numerous shower and thunderstorm development which moved repeatedly over these areas throughout much of the overnight into the early morning hours. Widespread rainfall amounts of 3-6+ inches fell across much of Deep and extreme Eastern Texas through mid-morning on the 11th, resulting in instances of flash flooding across these areas. Catastrophic flash flooding was observed within the city of Nacogdoches, as these higher amounts fell over the city and atop the Bayou La Nana watershed, with the bayou quickly rising sharply 14.3 feet before cresting at 19.65 feet at 10 am on the 11th. This left much of Central Nacogdoches, including a portion of Stephen F. Austin State University, inundated, before the flood waters receded during the afternoon. The USGS Gauge on Bayou La Nana in Nacogdoches recorded a 14.3 foot rise and crested at 19.65 feet at 10 am, May 11th. This resulted in catastrophic flooding across the city of Central and Southern Nacogdoches, including the Stephen F. Austin State University campus.", "ts_dict_index": [1776, 1777, 1778]}
+{"event_id": 977464, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-29 15:00:00", "end_date_time": "2021-07-29 17:00:00", "narrative": "A westward moving upper level trough over northern Mexico helped place much of Arizona under broad difluent flow aloft, aiding in the development of thunderstorms across the state. Scattered thunderstorms developed during the afternoon on the 29th across the high terrain of Arizona as daytime heating led to increasing upslope flow along terrain features. Abundant moisture in place allowed for thunderstorms to produce locally heavy rainfall, which led to instances of flash flooding across south-central Arizona. Thunderstorms over southern Gila County produced heavy rainfall over multiple burn scars, leading to enhanced runoff and flash flooding. The most significant impacts occurred after thunderstorms over the recent Telegraph fire burn scar produced 2-3 inches of rain, resulting in rapid rises in Bloody Tanks Wash and Russell Gulch. This resulted in catastrophic flash flooding in Miami where numerous homes, businesses, and roads were inundated with flood waters. A rare Flash Flood Emergency was issued for Miami due to the catastrophic flash flooding. No injuries were reported. At 1600MST, Arizona Department of Transportation reported Highway 188 was closed in both directions at mile post 219 due to flooding of Pinal Creek. Flood water originated from the Telegraph burn scar with flow from Bloody Tanks Wash and Russell Gulch merging into Pinal Creek. Timing of initial flood wave estimated from radar. No damages or injuries were reported.", "ts_dict_index": [1791, 1792, 1793]}
+{"event_id": 977419, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-29 18:15:00", "end_date_time": "2021-07-29 19:15:00", "narrative": "A westward moving upper level trough over northern Mexico helped place much of Arizona under broad difluent flow aloft, aiding in the development of thunderstorms across the state. Scattered thunderstorms developed during the afternoon on the 29th across the high terrain of Arizona as daytime heating led to increasing upslope flow along terrain features. Abundant moisture in place allowed for thunderstorms to produce locally heavy rainfall, which led to instances of flash flooding across south-central Arizona. Thunderstorms over southern Gila County produced heavy rainfall over multiple burn scars, leading to enhanced runoff and flash flooding. The most significant impacts occurred after thunderstorms over the recent Telegraph fire burn scar produced 2-3 inches of rain, resulting in rapid rises in Bloody Tanks Wash and Russell Gulch. This resulted in catastrophic flash flooding in Miami where numerous homes, businesses, and roads were inundated with flood waters. A rare Flash Flood Emergency was issued for Miami due to the catastrophic flash flooding. No injuries were reported. The USGS stream gage along Pinal Creek at Inspiration Dam near Globe measured an approximate rise of 4.25 feet in a 15 minute period. The gage recorded a peak of 5.73 feet at 1820MST. No damage or injuries were reported.", "ts_dict_index": [1788, 1789, 1790]}
+{"event_id": 977431, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-29 20:20:00", "end_date_time": "2021-07-29 23:45:00", "narrative": "A westward moving upper level trough over northern Mexico helped place much of Arizona under broad difluent flow aloft, aiding in the development of thunderstorms across the state. Scattered thunderstorms developed during the afternoon on the 29th across the high terrain of Arizona as daytime heating led to increasing upslope flow along terrain features. Abundant moisture in place allowed for thunderstorms to produce locally heavy rainfall, which led to instances of flash flooding across south-central Arizona. Thunderstorms over southern Gila County produced heavy rainfall over multiple burn scars, leading to enhanced runoff and flash flooding. The most significant impacts occurred after thunderstorms over the recent Telegraph fire burn scar produced 2-3 inches of rain, resulting in rapid rises in Bloody Tanks Wash and Russell Gulch. This resulted in catastrophic flash flooding in Miami where numerous homes, businesses, and roads were inundated with flood waters. A rare Flash Flood Emergency was issued for Miami due to the catastrophic flash flooding. No injuries were reported. A USGS stream gage along Tonto Creek above Gun Creek recorded a rapid rise, peaking above 6.9 feet, with high flow exceeding action stage. Flash flooding impacted unbridged crossings along Tonto Creek downstream of the gage. The public confirmed the closure of unbridged crossings due to the flooding. Timing was estimated from the gage reaching action stage. No damage or injuries were reported.", "ts_dict_index": [1785, 1786, 1787]}
+{"event_id": 976254, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-21 17:10:00", "end_date_time": "2021-07-21 17:30:00", "narrative": "With enhanced easterlies on the south end of the monsoon high and embedded weak perturbation waves rolling west across southern Arizona, scattered strong to severe thunderstorms developed in a moist unstable environment throughout the afternoon and evening on the 21st. Most storms in the afternoon developed across southwest Arizona, between Phoenix and the Colorado River, with sporadic storm motions driven by outflows and cell mergers. In the evening, new showers and thunderstorms developed and spread through south-central Arizona, including in the Phoenix metro area. With high moisture content and strong forcing, thunderstorms produced very heavy rain with rainfall rates around 1.5-2.0 inches per hour with briefly higher rates for short periods. Thunderstorms also produced damaging winds, which generated dense blowing dust in open desert areas. One storm produced a severe microburst in the small town of Tacna in Yuma county that caused significant damage. The American Red Cross Disaster Relief and Yuma County Sheriffs Office was called in to support those impacted by the storm. Hassayampa River Preserve closed several trails due to water/debris with a sudden rise in the Hassayampa River. Palm Lake in the reserve reportedly rose by 3 feet due to flood waters and video from the day after the heavy rain showed evidence of 1-3 feet of flow in the typically dry river bed. A USGS streamflow gage a few miles downstream measured a rapid 1 foot rise in 30 minutes. No damages or injuries were reported.", "ts_dict_index": [1779, 1780, 1781]}
+{"event_id": 976256, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-21 16:37:00", "end_date_time": "2021-07-21 17:00:00", "narrative": "With enhanced easterlies on the south end of the monsoon high and embedded weak perturbation waves rolling west across southern Arizona, scattered strong to severe thunderstorms developed in a moist unstable environment throughout the afternoon and evening on the 21st. Most storms in the afternoon developed across southwest Arizona, between Phoenix and the Colorado River, with sporadic storm motions driven by outflows and cell mergers. In the evening, new showers and thunderstorms developed and spread through south-central Arizona, including in the Phoenix metro area. With high moisture content and strong forcing, thunderstorms produced very heavy rain with rainfall rates around 1.5-2.0 inches per hour with briefly higher rates for short periods. Thunderstorms also produced damaging winds, which generated dense blowing dust in open desert areas. One storm produced a severe microburst in the small town of Tacna in Yuma county that caused significant damage. The American Red Cross Disaster Relief and Yuma County Sheriffs Office was called in to support those impacted by the storm. A Maricopa County Flood Control District streamflow gage on Powder House wash near Powder House Wash Road reached alarm stage and flood waters continued into and down Constellation Road and flooded the intersection with Jack Burden Road. A nearby rain gage measured 2.09 inches of rain in 56 minutes. The Public Works Department had to remove sand and debris from the road the following day. No damages or injuries were reported.", "ts_dict_index": [1782, 1783, 1784]}
+{"event_id": 977432, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-29 20:20:00", "end_date_time": "2021-07-29 21:20:00", "narrative": "A westward moving upper level trough over northern Mexico helped place much of Arizona under broad difluent flow aloft, aiding in the development of thunderstorms across the state. Scattered thunderstorms developed during the afternoon on the 29th across the high terrain of Arizona as daytime heating led to increasing upslope flow along terrain features. Abundant moisture in place allowed for thunderstorms to produce locally heavy rainfall, which led to instances of flash flooding across south-central Arizona. Thunderstorms over southern Gila County produced heavy rainfall over multiple burn scars, leading to enhanced runoff and flash flooding. The most significant impacts occurred after thunderstorms over the recent Telegraph fire burn scar produced 2-3 inches of rain, resulting in rapid rises in Bloody Tanks Wash and Russell Gulch. This resulted in catastrophic flash flooding in Miami where numerous homes, businesses, and roads were inundated with flood waters. A rare Flash Flood Emergency was issued for Miami due to the catastrophic flash flooding. No injuries were reported. A USGS gage along Cave Creek below Cottonwood Creek recorded a rapid rise and exceeded action stage. This gage measured an approximate rise of 5 feet in a 20 minute period and crested at 8.05 feet at 2030MST. No damage or injuries were reported.", "ts_dict_index": [1794, 1795, 1796]}
+{"event_id": 987585, "event_type": "Flash Flood", "state": "NEW YORK", "cz_name": "WESTCHESTER", "begin_date_time": "2021-09-01 21:48:00", "end_date_time": "2021-09-01 22:30:00", "narrative": "Extremely heavy rainfall associated with the remnants of Hurricane Ida overspread southeast New York during the evening of September 1 and continued through the early morning hours of September 2. Rainfall totals ranged from 5-8 inches across much of the region, with much of that rain falling in just a few hours. The ASOS at Central Park recorded 7.19 inches of rain, including 3.15 inches in a single hour between approximately 9:00-10:00pm. This resulted in widespread catastrophic flash flooding across New York City that resulted in extensive road and subway closures and numerous water rescues. Additional rainfall totals from around the region include 7.38 inches at a New York Mesonet station in Fordham in the Bronx, a report of 7.00 inches from a CoCoRaHS observer in Boerum Hill, Brooklyn, 6.90 inches from the ASOS at LaGuardia Airport, a spotter report of 6.18 inches in Monroe, a spotter report of 8.09 inches in Scarsdale, and a CoCoRaHS report of 6.72 inches in Locust Valley. Ultimately 17 people died as a result of the flash flooding, including 13 in New York City and 4 in the Lower Hudson Valley. Several cars were stranded in flood waters at the intersection of Bishop Avenue and Fenimore Road in Mamaroneck.", "ts_dict_index": [1755, 1756, 1757]}
+{"event_id": 983877, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2021-08-31 13:47:00", "end_date_time": "2021-08-31 18:00:00", "narrative": "A similar pattern existed on the 31st compared to the previous day with an upper level low in the eastern Pacific near the west coast of the Baja Peninsula promoting diffluent flow across southeast California. Better moisture existed on this day compared to the previous day, leading to a more enhanced flash flooding event. The most intense rainfall occurred in northeast Imperial County along SR 78, where nearly 7 inches of rain was estimated to have fallen within a 5 hour period. An unbridged crossing along SR 78 at Milpitas Wash became flooded with swiftly flowing water due to the heavy rainfall. A vehicle attempting to cross through the flooded portion of the highway was swept off the roadway before overturning in the wash. Both of the occupants perished in the flash flood. Strong to severe thunderstorms across the Imperial Valley led to damaging wind gusts that resulted in numerous downed power poles. According to the Imperial Irrigation District, extensive damage sustained to the power infrastructure on both the 30th and 31st would cost the district more than $8 million. Very heavy rainfall occurred along SR 78 in northeast Imperial County with amounts estimated to be approaching 7 inches in some places. This resulted in considerable flooding along the highway. The California Highway Patrol reported that a vehicle was swept off SR 78 at Milpitas Wash before overturning in the wash. Both occupants perished in the flash flood.", "ts_dict_index": [1800, 1801, 1802]}
+{"event_id": 983883, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2021-08-31 17:54:00", "end_date_time": "2021-08-31 18:54:00", "narrative": "A similar pattern existed on the 31st compared to the previous day with an upper level low in the eastern Pacific near the west coast of the Baja Peninsula promoting diffluent flow across southeast California. Better moisture existed on this day compared to the previous day, leading to a more enhanced flash flooding event. The most intense rainfall occurred in northeast Imperial County along SR 78, where nearly 7 inches of rain was estimated to have fallen within a 5 hour period. An unbridged crossing along SR 78 at Milpitas Wash became flooded with swiftly flowing water due to the heavy rainfall. A vehicle attempting to cross through the flooded portion of the highway was swept off the roadway before overturning in the wash. Both of the occupants perished in the flash flood. Strong to severe thunderstorms across the Imperial Valley led to damaging wind gusts that resulted in numerous downed power poles. According to the Imperial Irrigation District, extensive damage sustained to the power infrastructure on both the 30th and 31st would cost the district more than $8 million. The California Highway Patrol reported water and debris across SR 86 at Willow Wash, making the road impassable. No injuries were reported.", "ts_dict_index": [1809, 1810, 1811]}
+{"event_id": 983876, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2021-08-31 12:59:00", "end_date_time": "2021-08-31 18:00:00", "narrative": "A similar pattern existed on the 31st compared to the previous day with an upper level low in the eastern Pacific near the west coast of the Baja Peninsula promoting diffluent flow across southeast California. Better moisture existed on this day compared to the previous day, leading to a more enhanced flash flooding event. The most intense rainfall occurred in northeast Imperial County along SR 78, where nearly 7 inches of rain was estimated to have fallen within a 5 hour period. An unbridged crossing along SR 78 at Milpitas Wash became flooded with swiftly flowing water due to the heavy rainfall. A vehicle attempting to cross through the flooded portion of the highway was swept off the roadway before overturning in the wash. Both of the occupants perished in the flash flood. Strong to severe thunderstorms across the Imperial Valley led to damaging wind gusts that resulted in numerous downed power poles. According to the Imperial Irrigation District, extensive damage sustained to the power infrastructure on both the 30th and 31st would cost the district more than $8 million. Thunderstorms produced very heavy rainfall across northeast portions of Imperial County where nearly 7 inches of rain was estimated to have fallen in a 5 hour period. The Cibola RAWS site recorded 1.58 inches of rain between 1348PDT and 1548PDT. As a result, extensive flooding occurred along SR 78 from Palo Verde and areas south, damaging the road and leading to an extended closure for repairs.", "ts_dict_index": [1806, 1807, 1808]}
+{"event_id": 858096, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2019-09-02 02:00:00", "end_date_time": "2019-09-02 14:00:00", "narrative": "Upper level high pressure centered over the Four Corners ushered in moisture from the southeast into SoCal starting on Labor Day. Monsoon thunderstorms impacted the mountains and deserts September 2 through 5th. The event started with a nocturnal MCS over the Coachella Valley early in the morning on September 2nd, dumping 1-1.5 inches over a couple of hours. Even more thunderstorms formed Monday afternoon, especially in the mountains. Hail was reported on I-8 Monday afternoon. Storms continued each afternoon and evening in the mountains through September 5th. Some thunderstorms even reached the San Diego County coast on September 4th. Widespread outflow wind gusts of 30-45 mph were reported on the coast and in the valleys on September 4th.|At the end of September, 24-26, tropical moisture was wrapped into southern California from a closed upper low. This initially brought Santa Ana winds and very warm temperatures to the coast and on 25-26 brought scattered thunderstorms to the San Diego mountains. The flooding rains were confined to the Mojave Desert and Imperial Valley. North Indian Canyon Drive was closed on the morning of 9/2 due to water over the roadway. Media reports that the road was still closed monday evening.", "ts_dict_index": [1812, 1813, 1814]}
+{"event_id": 920147, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-10-28 11:43:00", "end_date_time": "2020-10-28 14:43:00", "narrative": "A big gullywasher came on the 28th as the system in the Plains neared. Rain came down in buckets over the northern half of the state, with four to more than five inch amounts at several locations. This included Des Arc (Prairie County) and Harrison (Boone County). Three to four inch totals occurred at Booneville (Logan County), Batesville (Independence County), Gilbert (Searcy County), Jonesboro (Craighead County), Lead Hill (Boone County), Marshall (Searcy County), Mena (Polk County), Mountain Home (Baxter County), Newport (Jackson County).||In and around Little Rock (Pulaski County), there was spotty flash flooding. At Sherwood (Pulaski County), an inch and a half of rain dumped in twenty minutes. The Little Rock Air Force Base (Pulaski County) got 1.66 inches in an hour.||In a four day period ending at 600 am CST on the 30th, precipitation in parts of the north and west exceeded six inches. It was a complete reversal of fortune from the dryness experienced up until the deluge. For the month, rain was just under five inches above average at Harrison (Boone County). The underpass at Pershing Boulevard and Percy Machin Drive was flooded.", "ts_dict_index": [1824, 1825, 1826]}
+{"event_id": 858095, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2019-09-02 02:00:00", "end_date_time": "2019-09-02 06:00:00", "narrative": "Upper level high pressure centered over the Four Corners ushered in moisture from the southeast into SoCal starting on Labor Day. Monsoon thunderstorms impacted the mountains and deserts September 2 through 5th. The event started with a nocturnal MCS over the Coachella Valley early in the morning on September 2nd, dumping 1-1.5 inches over a couple of hours. Even more thunderstorms formed Monday afternoon, especially in the mountains. Hail was reported on I-8 Monday afternoon. Storms continued each afternoon and evening in the mountains through September 5th. Some thunderstorms even reached the San Diego County coast on September 4th. Widespread outflow wind gusts of 30-45 mph were reported on the coast and in the valleys on September 4th.|At the end of September, 24-26, tropical moisture was wrapped into southern California from a closed upper low. This initially brought Santa Ana winds and very warm temperatures to the coast and on 25-26 brought scattered thunderstorms to the San Diego mountains. The flooding rains were confined to the Mojave Desert and Imperial Valley. Flash flooding along Date Palm Drive at Los Gatos Road from heavy rain from 0400 through mid-morning on 9/2. At one point, there was roughly 12 inches of water on the road.", "ts_dict_index": [1815, 1816, 1817]}
+{"event_id": 920146, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-10-28 11:30:00", "end_date_time": "2020-10-28 14:30:00", "narrative": "A big gullywasher came on the 28th as the system in the Plains neared. Rain came down in buckets over the northern half of the state, with four to more than five inch amounts at several locations. This included Des Arc (Prairie County) and Harrison (Boone County). Three to four inch totals occurred at Booneville (Logan County), Batesville (Independence County), Gilbert (Searcy County), Jonesboro (Craighead County), Lead Hill (Boone County), Marshall (Searcy County), Mena (Polk County), Mountain Home (Baxter County), Newport (Jackson County).||In and around Little Rock (Pulaski County), there was spotty flash flooding. At Sherwood (Pulaski County), an inch and a half of rain dumped in twenty minutes. The Little Rock Air Force Base (Pulaski County) got 1.66 inches in an hour.||In a four day period ending at 600 am CST on the 30th, precipitation in parts of the north and west exceeded six inches. It was a complete reversal of fortune from the dryness experienced up until the deluge. For the month, rain was just under five inches above average at Harrison (Boone County). Several intersections were reported to be flooded in the downtown area.", "ts_dict_index": [1827, 1828, 1829]}
+{"event_id": 1109481, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-06-26 19:50:00", "end_date_time": "2023-06-26 22:00:00", "narrative": "On the evening of June 25, moderate to heavy rain occurred with rainfall rates briefly reaching up to 4��� per hour. Numerous storms repeatedly traveled over the same area of Southern Grafton County through midnight before the rain ended shortly after. After a short break in the rain activity from midnight through the morning of June 26, showers and thunderstorms began to redevelop across southern New Hampshire by midday. Rounds of heavy showers and thunderstorms moved through Hillsborough county through the afternoon hours with one storm impacting Manchester around 3 PM where 1.5��� of rain fell in an hour. By early evening another round of heavy rain impacted the Wilton and Temple area with an additional 1 to 2��� of rain in less than an hour. This region received heavy rainfall earlier in the afternoon, with this second round bringing rainfall totals of 3 or more inches to the area. During the evening, another round of heavy rain impacted western Cheshire County from 6 pm through 10 pm. The most impactful flooding occurred in the Bristol Community in Grafton County. Heavy rain estimated between 3.5 to 5.5 inches fell between 7 and 930 pm across West Chesterfield, with rainfall rates measured over 3 inches per hour. This torrential rainfall resulted in flooding across sections of Main Street, Brook Street, Streeter Hill Road, and Gulf Road. Washouts were reported on Gulf Road.", "ts_dict_index": [1818, 1819, 1820]}
+{"event_id": 1109482, "event_type": "Flash Flood", "state": "NEW HAMPSHIRE", "cz_name": "CHESHIRE", "begin_date_time": "2023-06-26 21:00:00", "end_date_time": "2023-06-26 22:00:00", "narrative": "On the evening of June 25, moderate to heavy rain occurred with rainfall rates briefly reaching up to 4��� per hour. Numerous storms repeatedly traveled over the same area of Southern Grafton County through midnight before the rain ended shortly after. After a short break in the rain activity from midnight through the morning of June 26, showers and thunderstorms began to redevelop across southern New Hampshire by midday. Rounds of heavy showers and thunderstorms moved through Hillsborough county through the afternoon hours with one storm impacting Manchester around 3 PM where 1.5��� of rain fell in an hour. By early evening another round of heavy rain impacted the Wilton and Temple area with an additional 1 to 2��� of rain in less than an hour. This region received heavy rainfall earlier in the afternoon, with this second round bringing rainfall totals of 3 or more inches to the area. During the evening, another round of heavy rain impacted western Cheshire County from 6 pm through 10 pm. The most impactful flooding occurred in the Bristol Community in Grafton County. Pond Brook surged out of banks and onto Pond Brook Drive near Chamberlain Way.", "ts_dict_index": [1821, 1822, 1823]}
+{"event_id": 977463, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-29 14:10:00", "end_date_time": "2021-07-29 18:30:00", "narrative": "A westward moving upper level trough over northern Mexico helped place much of Arizona under broad difluent flow aloft, aiding in the development of thunderstorms across the state. Scattered thunderstorms developed during the afternoon on the 29th across the high terrain of Arizona as daytime heating led to increasing upslope flow along terrain features. Abundant moisture in place allowed for thunderstorms to produce locally heavy rainfall, which led to instances of flash flooding across south-central Arizona. Thunderstorms over southern Gila County produced heavy rainfall over multiple burn scars, leading to enhanced runoff and flash flooding. The most significant impacts occurred after thunderstorms over the recent Telegraph fire burn scar produced 2-3 inches of rain, resulting in rapid rises in Bloody Tanks Wash and Russell Gulch. This resulted in catastrophic flash flooding in Miami where numerous homes, businesses, and roads were inundated with flood waters. A rare Flash Flood Emergency was issued for Miami due to the catastrophic flash flooding. No injuries were reported. After 2.5-3.5 inches of rain fell over the northern portion of the Telegraph burn scar, runoff rapidly collected in Bloody Tanks Wash and flowed downstream through the town of Miami causing catastrophic damage. A rain gage in Russell Gulch to the south measured 2.01 inches of rain between 1316MST and 1414MST with a brief period where rain rates were as high as 8-9 inches per hour with 0.87 inches measured in 10 minutes. At 1438MST Arizona Department of Transportation (ADOT) reported US-60 was closed in both directions at mile post 243 due to water moving over the road. Between 1440MST and 1500MST, a trained spottered reported the flood water was coming out of the banks of the wash at the intersection of Canyon Avenue and US-60 and video showed 6 to 8 feet of flood water in the wash coming up to the base of multiple bridges between Sullivan Street and US-60. Water and mud spilled out of the wash near Cordova Avenue, with flow down Sullivan Street, and entered homes and businesses. ADOT ended up having US-60 closed in both directions between Miami and the town of Superior until 1920MST. According to Gila County Emergency Management and Arizona Department of Emergency and Military Affairs, approximately 600 homes and 10 businesses experienced some form of flood damage.  No injuries were reported and the full extent of damage costs are unknown.", "ts_dict_index": [1797, 1798, 1799]}
+{"event_id": 1088191, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-15 21:30:00", "end_date_time": "2023-03-15 22:30:00", "narrative": "An area of low pressure moving across the western states resulted in waves of rainfall across the region during the day on the 15th. A round of widespread light to locally moderate rainfall activity was observed during the morning hours followed by a more significant round with thunderstorms during the evening hours in association with a cold front. Moisture levels associated with this low pressure system were in the 99th percentile for mid-March, signifying that environment was favorable for heavier rainfall rates to materialize. As a result of the heavier rainfall activity observed during the evening hours, flooding was observed across the Wickenburg area in northwestern Maricopa County, where over an inch of total rainfall was observed. Flooding was also observed along the low-water crossings that intersect the Hassayampa River, which runs from north to south along the western third of Maricopa County. Strong storms were also observed during the afternoon hours across southwestern Arizona, producing isolated gusts around 60 mph in the Yuma area. Portions of Vulture Mine Rd in Wickenburg closed due to flooding. No damages or injuries were reported.", "ts_dict_index": [1851, 1852, 1853]}
+{"event_id": 872341, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2020-03-13 15:30:00", "end_date_time": "2020-03-13 18:30:00", "narrative": "A weakening but still potent upper level low pressure system continued to push east across Arizona during the day on March 13th, and the atmosphere across the central deserts was still very humid and a bit unstable. As the system moved across the greater Phoenix area, scattered afternoon thunderstorms developed over the greater Phoenix area. Some of the thunderstorms generated very heavy rains; a trained spotter near the town of Surprise measured 0.7 inches of rain within a 10 minute period. The heavy rain resulted in episodes of street flooding as well as flash flooding. At about 1700MST flash flooding on Cave Creek near 7th Avenue and Greenway Road. Water 6 inches deep was flowing across 7th Avenue as reported by the public. Heavy rain 3 miles south of Deer Valley caused flash flooding at the Interstate 17 and Greenway underpass to flood. Water 1 to 2 feet deep filled up the underpass resulting in at least one stalled car. A Flash Flood Warning was issued and in effect at the time of the underpass flooding. There were no reports of injuries due to the flooding. Afternoon thunderstorms developed across the northern portions of the greater Phoenix metropolitan area on March 13th and some of the stronger storms generated very heavy rain with peak rain rates well in excess of one inch per hour. The heavy rain led to an episode of flash flooding about 3 miles to the southeast of Deer Valley, between Bell Road and Thunderbird Road. At roughly 1650MST, the public reported flash flooding on the east fork of Cave Creek near 7th Avenue and Greenway Road. Water was seen flowing 6 inches deep across 7th Avenue. A Flash Flood Warning had been issued for the area at 1530MST. No reports of accidents or injuries were received  due to the flash flooding.", "ts_dict_index": [1839, 1840, 1841]}
+{"event_id": 870543, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2020-02-23 01:00:00", "end_date_time": "2020-02-23 05:30:00", "narrative": "Widespread rain, moderate to heavy at times, occurred on Saturday February 22nd and the excessive rain eventually led to episodes of areal flooding across higher terrain areas to the east of Phoenix. One of the more problematic areas was the Tonto Creek basin; rainfall amounts of 3 inches or more along the basin and upstream caused areal flooding to occur and forced the closure of several low water crossings. Rainfall diminished during the afternoon and evening on the 22nd allowing streamflow to level out somewhat but a new round of heavy showers occurred during late evening Saturday and into the early morning on the 23rd. The new round of moderate to heavy showers occurring on an already saturated ground led to a spike in stream flow and produced flash flooding near Punkin center shortly after midnight. According to broadcast media, at about 0140MST a motorist was rescued while trying to cross Tonto Creek at the store crossing in Punkin Center. An Areal Flood Warning remained in effect for the area at the time of the rescue. No injuries were reported, fortunately. Widespread rain across the high terrain east of Phoenix on Saturday February 22nd led to  areal flooding in the Tonto Creek basin north of Lake Roosevelt. Early in the morning on February 23rd, a fresh batch of showers and weak thunderstorms occurred which produced another period of moderate to heavy rain. The additional rain fell in a short period on already saturated ground and led to a rapid rise in the streamflow on Tonto Creek and as a result flash flooding occurred. According to local broadcast media, at 0140MST a motorist needed to be rescued while trying to cross Tonto Creek at the store crossing in Punkin center. The motorist was not injured. While a flash flood warning was not in effect at the time of the rescue, an areal flood warning remained in effect for the area; the warning was issued during the middle of the day on Saturday the 22nd.", "ts_dict_index": [1830, 1831, 1832]}
+{"event_id": 872344, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2020-03-13 15:00:00", "end_date_time": "2020-03-13 18:30:00", "narrative": "A weakening but still potent upper level low pressure system continued to push east across Arizona during the day on March 13th, and the atmosphere across the central deserts was still very humid and a bit unstable. As the system moved across the greater Phoenix area, scattered afternoon thunderstorms developed over the greater Phoenix area. Some of the thunderstorms generated very heavy rains; a trained spotter near the town of Surprise measured 0.7 inches of rain within a 10 minute period. The heavy rain resulted in episodes of street flooding as well as flash flooding. At about 1700MST flash flooding on Cave Creek near 7th Avenue and Greenway Road. Water 6 inches deep was flowing across 7th Avenue as reported by the public. Heavy rain 3 miles south of Deer Valley caused flash flooding at the Interstate 17 and Greenway underpass to flood. Water 1 to 2 feet deep filled up the underpass resulting in at least one stalled car. A Flash Flood Warning was issued and in effect at the time of the underpass flooding. There were no reports of injuries due to the flooding. An exiting but still potent upper level disturbance acted upon a still wet and unstable air mass to produce scattered afternoon thunderstorms across portions of the greater Phoenix metropolitan area on March 13th. Some of the stronger storms generated locally heavy rain with peak rain rates well in excess of one inch per hour. Portions of the heavy rain fell in the community of Buckeye resulting in an episode of flash flooding. According to a trained weather spotter located about 3 miles north of the town of Buckeye, at 1605MST flash flooding resulted in flowing water 6 inches deep covering a 20 foot wide swath across Miller Road, just south of lower Buckeye Road. Despite the quickly flowing water there were no reports of any accidents due to the flash flooding.", "ts_dict_index": [1842, 1843, 1844]}
+{"event_id": 873892, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2020-03-13 15:30:00", "end_date_time": "2020-03-13 21:00:00", "narrative": "A weakening but still potent upper level low pressure system continued to push east across Arizona during the day on March 13th, and the atmosphere across the central deserts was still very humid and a bit unstable. As the system moved across the greater Phoenix area, scattered afternoon thunderstorms developed over the greater Phoenix area. Some of the thunderstorms generated very heavy rains; a trained spotter near the town of Surprise measured 0.7 inches of rain within a 10 minute period. The heavy rain resulted in episodes of street flooding as well as flash flooding. At about 1700MST flash flooding on Cave Creek near 7th Avenue and Greenway Road. Water 6 inches deep was flowing across 7th Avenue as reported by the public. Heavy rain 3 miles south of Deer Valley caused flash flooding at the Interstate 17 and Greenway underpass to flood. Water 1 to 2 feet deep filled up the underpass resulting in at least one stalled car. A Flash Flood Warning was issued and in effect at the time of the underpass flooding. There were no reports of injuries due to the flooding. Scattered showers and thunderstorms, some with heavy rain, occurred during the afternoon hours across the deserts to the west of Phoenix on March 13th. The heavy rain caused washes, streams and rivers to flow very heavily, posing significant danger to motorists. According to local broadcast media, at 1930MST a motorist became trapped in his vehicle at Baseline Road and 319th Avenue due to the Hassayampa River flowing swiftly across the road. The Hassayampa was swollen and flowing heavily due to the earlier heavy rain in the area. About 20 minutes later, a water rescue was needed for the motorist; the rescue occurred to the west of the town of Buckeye. There were no reports of injuries to either the motorists or the rescuers. There was no flash flood warning in effect at the time of the water rescue.", "ts_dict_index": [1833, 1834, 1835]}
+{"event_id": 872342, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2020-03-13 15:30:00", "end_date_time": "2020-03-13 18:30:00", "narrative": "A weakening but still potent upper level low pressure system continued to push east across Arizona during the day on March 13th, and the atmosphere across the central deserts was still very humid and a bit unstable. As the system moved across the greater Phoenix area, scattered afternoon thunderstorms developed over the greater Phoenix area. Some of the thunderstorms generated very heavy rains; a trained spotter near the town of Surprise measured 0.7 inches of rain within a 10 minute period. The heavy rain resulted in episodes of street flooding as well as flash flooding. At about 1700MST flash flooding on Cave Creek near 7th Avenue and Greenway Road. Water 6 inches deep was flowing across 7th Avenue as reported by the public. Heavy rain 3 miles south of Deer Valley caused flash flooding at the Interstate 17 and Greenway underpass to flood. Water 1 to 2 feet deep filled up the underpass resulting in at least one stalled car. A Flash Flood Warning was issued and in effect at the time of the underpass flooding. There were no reports of injuries due to the flooding. Scattered thunderstorms developed across the northern portion of the greater Phoenix metropolitan area during the afternoon hours on March 13th. Some of the stronger storms produced intense rain with peak rain rates well in excess of one inch per hour. The heavy rain resulted in some flash flooding which affected the Interstate 17 corridor to the south of the community of Deer Valley. According to a report from local broadcast media, flash flooding along the Interstate resulted in the flooding of the Greenway Road underpass; one to two feet of water filled up the underpass leading to at least one stalled vehicle. A Flash Flood Warning was issued for the area at 1530MST and it was in effect at the time of the flooding. There were no reports of any injuries fortunately.", "ts_dict_index": [1836, 1837, 1838]}
+{"event_id": 1088187, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-15 21:30:00", "end_date_time": "2023-03-15 22:30:00", "narrative": "An area of low pressure moving across the western states resulted in waves of rainfall across the region during the day on the 15th. A round of widespread light to locally moderate rainfall activity was observed during the morning hours followed by a more significant round with thunderstorms during the evening hours in association with a cold front. Moisture levels associated with this low pressure system were in the 99th percentile for mid-March, signifying that environment was favorable for heavier rainfall rates to materialize. As a result of the heavier rainfall activity observed during the evening hours, flooding was observed across the Wickenburg area in northwestern Maricopa County, where over an inch of total rainfall was observed. Flooding was also observed along the low-water crossings that intersect the Hassayampa River, which runs from north to south along the western third of Maricopa County. Strong storms were also observed during the afternoon hours across southwestern Arizona, producing isolated gusts around 60 mph in the Yuma area. Portions of Jack Burden Rd in Wickenburg closed due to flooding. No damages or injuries were reported.", "ts_dict_index": [1854, 1855, 1856]}
+{"event_id": 1097166, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2023-05-11 05:57:00", "end_date_time": "2023-05-11 10:45:00", "narrative": "An upper level low pressure system slowly ejected northeast across the piney woods of East Texas during the evening through the morning hours of May 10th-11th. A southerly low level jet present ahead of the low spilled copious amounts of low level moisture north into East Texas and Western Louisiana, with strong large scale forcing ahead of the low enhancing numerous shower and thunderstorm development which moved repeatedly over these areas throughout much of the overnight into the early morning hours. Widespread rainfall amounts of 3-6+ inches fell across much of Deep and extreme Eastern Texas through mid-morning on the 11th, resulting in instances of flash flooding across these areas. Catastrophic flash flooding was observed within the city of Nacogdoches, as these higher amounts fell over the city and atop the Bayou La Nana watershed, with the bayou quickly rising sharply 14.3 feet before cresting at 19.65 feet at 10 am on the 11th. This left much of Central Nacogdoches, including a portion of Stephen F. Austin State University, inundated, before the flood waters receded during the afternoon. Multiple roads remain flooded and closed across the south side of Nacogdoches due to significant flooding along Bayou La Nana. Multiple other roads were also flooded and closed throughout much of Nacogdoches County.", "ts_dict_index": [1767, 1768, 1769]}
+{"event_id": 1088185, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-15 20:03:00", "end_date_time": "2023-03-15 22:03:00", "narrative": "An area of low pressure moving across the western states resulted in waves of rainfall across the region during the day on the 15th. A round of widespread light to locally moderate rainfall activity was observed during the morning hours followed by a more significant round with thunderstorms during the evening hours in association with a cold front. Moisture levels associated with this low pressure system were in the 99th percentile for mid-March, signifying that environment was favorable for heavier rainfall rates to materialize. As a result of the heavier rainfall activity observed during the evening hours, flooding was observed across the Wickenburg area in northwestern Maricopa County, where over an inch of total rainfall was observed. Flooding was also observed along the low-water crossings that intersect the Hassayampa River, which runs from north to south along the western third of Maricopa County. Strong storms were also observed during the afternoon hours across southwestern Arizona, producing isolated gusts around 60 mph in the Yuma area. A Maricopa County Flood Control District Gauge at Casandro Wash in Wickenburg registered flows going above alarm stage, which is 2.2 feet, at 20:03 MST. The flow reached a peak of 4.76 feet (343 cfs) at 20:30 MST and went below flood stage by 22:03 MST. This likely contributed to flooding along the inflow to Casandro Dam as well as small road crossings that intersect the wash. No damages or injuries were reported.", "ts_dict_index": [1857, 1858, 1859]}
+{"event_id": 883830, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-05-16 16:45:00", "end_date_time": "2020-05-16 20:15:00", "narrative": "A slow moving upper level low pressure system drifted east across Central and Eastern Texas during the daytime hours of May 16th. Meanwhile, the attendant surface low pressure system over East Central Texas drifted east into Northeast Texas during the afternoon, with a southerly low level jet allowing for a warm front to mix north into East Texas, extreme Northern Louisiana, into Southern Arkansas through the evening. Although daytime heating was limited due to extensive cloud cover and periods of showers, large scale forcing and adequate low level wind shear contributed to the development of numerous low-topped supercell showers and a few thunderstorms, several of which spawned tornadoes and wall clouds across portions of extreme Northeast Texas, Southwest Arkansas, and Southeast Oklahoma throughout the afternoon and evening. As drier air began to entrain ahead of this upper low pressure system, and the warm front had shifted north into the northern sections of Southwest Arkansas by mid-evening, the tornado threat subsided considerably. Many roads were impassable due to flooding throughout the city of Idabel.", "ts_dict_index": [1860, 1861, 1862]}
+{"event_id": 1060898, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2022-10-15 15:01:00", "end_date_time": "2022-10-15 17:01:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of southeast CA, mainly from the late morning through the late afternoon hours. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October. Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and small hail. The area of the greatest impacts occurred across the Imperial Valley, where several reports of flooding along with damaging winds and small hail were received. Water running along the eastbound lanes of I-10 resulted in closure of the highway near Ford Dry Lake Road. No damages or injuries were reported.", "ts_dict_index": [1884, 1885, 1886]}
+{"event_id": 1061006, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2022-10-15 11:49:00", "end_date_time": "2022-10-15 13:49:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of southeast CA, mainly from the late morning through the late afternoon hours. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October. Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and small hail. The area of the greatest impacts occurred across the Imperial Valley, where several reports of flooding along with damaging winds and small hail were received. Heavy flooding reported on the on and off ramp of South 4th street and I-8 in El Centro. No damages or injuries were reported.", "ts_dict_index": [1881, 1882, 1883]}
+{"event_id": 1061024, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2022-10-15 12:10:00", "end_date_time": "2022-10-15 15:10:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of southeast CA, mainly from the late morning through the late afternoon hours. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October. Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and small hail. The area of the greatest impacts occurred across the Imperial Valley, where several reports of flooding along with damaging winds and small hail were received. Significant flooding was reported in the El Centro Regional Medical Center. There was 18 inches of flowing water in the parking lot, with the water entering the facility and affecting the emergency room as well as the radiology department. No injuries were reported.", "ts_dict_index": [1890, 1891, 1892]}
+{"event_id": 1132117, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 22:30:00", "end_date_time": "2023-08-31 23:59:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Video uploaded by the Daisy Mountain Fire Department Station 142 in Anthem showed several inches of flowing water along a street within the station's jurisdiction. No damages or injuries were reported.", "ts_dict_index": [1866, 1867, 1868]}
+{"event_id": 1131811, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 22:21:00", "end_date_time": "2023-08-31 23:59:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A Maricopa County Flood Control District Gauge along Skunk Tank Wash near the intersection of Desert Hills Drive and North 7th Avenue reported flows rising to above alarm stage, which is 4.2 feet, at 22:21 MST. The flow peaked at 7.09 feet (674 cfs), which is above the flood stage of 7.00 feet, at 22:49 MST. The flow fell below alarm stage at 23:43 MST. The elevated water flow caused the closure of Desert Hills Drive between 19th and 15th Avenues due to flooding. No damages or injuries were reported.", "ts_dict_index": [1872, 1873, 1874]}
+{"event_id": 1132099, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 23:00:00", "end_date_time": "2023-08-31 23:59:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Water rescue performed on East Cloud Road just east of North 7th Street in Anthem as person was rescued from vehicle due to flooding. The vehicle, a Ford F150, was swept away by the flood waters.", "ts_dict_index": [1875, 1876, 1877]}
+{"event_id": 1132525, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 23:00:00", "end_date_time": "2023-08-31 23:59:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Water rescue reported along the intersection of North New River Road and North 67th Avenue in Anthem due to flooding. No damages or injuries were reported.", "ts_dict_index": [1863, 1864, 1865]}
+{"event_id": 1132095, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 23:00:00", "end_date_time": "2023-08-31 23:59:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A water rescue was reported in the intersection of West Joy Ranch Road and North Pioneer Road in Anthem due to flooding. No damages or injuries were reported.", "ts_dict_index": [1878, 1879, 1880]}
+{"event_id": 1132528, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-08-31 20:30:00", "end_date_time": "2023-08-31 22:30:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Barnes Road from Stanfield Road to Murphy Road closed due to Green Wash running. No damages or injuries were reported.", "ts_dict_index": [1869, 1870, 1871]}
+{"event_id": 849916, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-16 19:30:00", "end_date_time": "2019-09-16 23:30:00", "narrative": "Scattered monsoon thunderstorms developed across the central and western portions of the greater Phoenix metropolitan area during the evening hours on September 16th. Some of the stronger storms generated intense rainfall with peak rain rates well in excess of one inch per hour. The heavy rain led to episodes of flash flooding west of Phoenix, especially in areas around the town of Buckeye. A Maricopa County Flood Control District rain gage measured almost 2.5 inches of rain within 90 minutes about 4 miles north of Buckeye; the heavy rain ended around 2130MST. At 2013MST a spotter 5 miles northwest of Buckeye reported mud washed across Palo Verde Road between Interstate 10 and Southern Avenue with 8 inches or more of standing water on the road. Shortly before 2000MST the public reported flash flooding with roads closed 6 miles northwest of Buckeye; Palo Verde Road was closed just north of Interstate 10 and there were vehicles stranded. Multiple Flash Flood Warnings were issued during the course of the evening. No injuries were reported, fortunately. Scattered thunderstorms developed across the western portions of the greater Phoenix area during the evening hours on September 16th. Some of the stronger storms generated intense rainfall with peak rain rates well in excess of one inch per hour. An automated flood control gage 4 miles north of Buckeye measured 2.48 inches of rain within 90 minutes ending about 2130MST. The heavy rain led to episodes of flash flooding around the town of Buckeye. At 1955MST, the public reported flash flooding 6 miles northwest of Buckeye; flooding resulted in road closures and stranded vehicles on Palo Verde Road just north of Interstate 10. At the same time there were 2 spotter reports of flooding near the intersection of Interstate 10 and Miller Road, about 4 miles north of Buckeye. Finally, at 2013MST there were reports of mud from farm fields being washed across Palo Verde Road from Interstate 10 south to Southern Avenue. There was standing water 8 inches or more deep across the road due to the flooding. There was a Flash Flood Warning issued for the area at 2000MST. No reports of accidents or injuries were received due to the flash flooding.", "ts_dict_index": [1848, 1849, 1850]}
+{"event_id": 1107035, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 17:00:00", "end_date_time": "2023-06-03 19:30:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. High water reported at the intersection of Stoner Avenue and Centenary Boulevard in Shreveport.", "ts_dict_index": [1905, 1906, 1907]}
+{"event_id": 1060897, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2022-10-15 13:40:00", "end_date_time": "2022-10-15 15:40:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of southeast CA, mainly from the late morning through the late afternoon hours. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October. Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and small hail. The area of the greatest impacts occurred across the Imperial Valley, where several reports of flooding along with damaging winds and small hail were received. Plows from the California Highway Patrol removed flood debris from SR-111 near Milepost 65. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [1896, 1897, 1898]}
+{"event_id": 1061037, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2022-10-15 16:21:00", "end_date_time": "2022-10-15 17:21:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of southeast CA, mainly from the late morning through the late afternoon hours. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October. Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and small hail. The area of the greatest impacts occurred across the Imperial Valley, where several reports of flooding along with damaging winds and small hail were received. Car Stranded along Senator Wash Road about 5 miles south-southwest of Martinez Lake due to flooding. No injuries were reported.", "ts_dict_index": [1893, 1894, 1895]}
+{"event_id": 1107034, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 17:00:00", "end_date_time": "2023-06-03 19:30:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Kings Highway just east of Interstate 49 was flooded with cars stalled out at the intersection of Kings Highway and Barrett Street.", "ts_dict_index": [1902, 1903, 1904]}
+{"event_id": 1107040, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 17:08:00", "end_date_time": "2023-06-03 19:30:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Vehicular high water rescue on Caddo Street between McNeil Street and Louisiana Avenue in downtown Shreveport.", "ts_dict_index": [1908, 1909, 1910]}
+{"event_id": 1100157, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-05-11 07:43:00", "end_date_time": "2023-05-11 11:45:00", "narrative": "An upper level low pressure system slowly ejected northeast across the piney woods of East Texas during the evening through the morning hours of May 10th-11th. A southerly low level jet present ahead of the low spilled copious amounts of low level moisture north into East Texas and Western Louisiana, with strong large scale forcing ahead of the low enhancing numerous shower and thunderstorm development which moved repeatedly over these areas throughout much of the overnight into the early morning hours. Widespread rainfall amounts of 2-4+ inches fell across much of North Louisiana during the morning through the early afternoon hours on the 11th, resulting in instances of flash flooding across this area. Given the strong low level wind shear out ahead of the low, as well as increased instability especially with the onset of daytime heating, severe thunderstorms containing damaging winds, while also spawning a few isolated tornadoes, were observed throughout the morning as well before eventually diminishing during the afternoon. Street flooding was reported at the Kansas City Southern Railroad underpass on North Lakeshore Drive.", "ts_dict_index": [1899, 1900, 1901]}
+{"event_id": 1107031, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 16:48:00", "end_date_time": "2023-06-03 19:30:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. High water reported on several city streets and four cars submerged in downtown Shreveport.", "ts_dict_index": [1911, 1912, 1913]}
+{"event_id": 1107540, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 17:09:00", "end_date_time": "2023-06-03 19:30:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Vehicular high water rescue near Devaughn Street and Rightway Avenue at the underpass along Hearne Avenue in Shreveport. One person was rescued, but a second person was trapped in the same vehicle and drowned.", "ts_dict_index": [1917, 1918, 1919]}
+{"event_id": 1107541, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 17:10:00", "end_date_time": "2023-06-03 19:30:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Vehicular high water rescue reported near the Pines Road on-ramp to Interstate 20 westbound in Shreveport.", "ts_dict_index": [1920, 1921, 1922]}
+{"event_id": 799407, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-02-14 22:30:00", "end_date_time": "2019-02-15 01:30:00", "narrative": "Locally heavy rain occurred across portions of south-central Arizona during the afternoon and evening hours on February 14th, affecting both northern Maricopa and southern Gila Counties. The heavy rain led to episodes of flooding and flash flooding, and resulted in the issuance of various products such as Flash Flood Warnings and Areal Flood warnings. Some of the more significant flooding occurred along Tonto Creek north of Lake Roosevelt, as well as in communities such as New River and Carefree/Cave Creek. At roughly 2230MST a Flash Flood Warning was issued for areas around New River and shortly after midnight Old Stage Road at New River low water crossing became impassable and was closed by Maricopa County Department of Transportation. Flash flooding also occurred along Tonto Creek resulting in a rapid rise of water that exceeded action stage for the creek. At 2345MST several low water crossings in the Tonto Basin were closed and impassable as well. No injuries were reported due to the flooding and flash flooding. Significant amounts of rain fell across northern portions of Maricopa County, as well as over high terrain of central Arizona, during the day on February 14th and this led to many washes running very high in the areas around New River and Cave Creek. Flooding and flash flooding was observed; at 0006MST Old Stage Road was impassable at the New River low water crossing and as a result, Maricopa County Department of Transportation closed the roadway. A Flash Flood Warning had been issued earlier for the area due to the fast flow within area washes as well as the normally dry New River. The warning remained in effect through 0130MST. There were no reports of accidents or injuries due to the flash flooding.", "ts_dict_index": [1923, 1924, 1925]}
+{"event_id": 799366, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2019-02-14 21:45:00", "end_date_time": "2019-02-15 00:45:00", "narrative": "Locally heavy rain occurred across portions of south-central Arizona during the afternoon and evening hours on February 14th, affecting both northern Maricopa and southern Gila Counties. The heavy rain led to episodes of flooding and flash flooding, and resulted in the issuance of various products such as Flash Flood Warnings and Areal Flood warnings. Some of the more significant flooding occurred along Tonto Creek north of Lake Roosevelt, as well as in communities such as New River and Carefree/Cave Creek. At roughly 2230MST a Flash Flood Warning was issued for areas around New River and shortly after midnight Old Stage Road at New River low water crossing became impassable and was closed by Maricopa County Department of Transportation. Flash flooding also occurred along Tonto Creek resulting in a rapid rise of water that exceeded action stage for the creek. At 2345MST several low water crossings in the Tonto Basin were closed and impassable as well. No injuries were reported due to the flooding and flash flooding. Significant rain fell over portions of Southern Gila County and northeast Maricopa County as well as further to the north over higher terrain of central Arizona. Runoff from the heavy rain eventually drained south and into the Tonto Basin affecting Tonto Creek to the north of Lake Roosevelt. According to observations from a USGS stream gage along Tonto Creek, there was a rapid rise in water which quickly caused flow to exceed the NWS alarm stage. The heavy flow in Tonto Creek caused several low water crossings in the Tonto Basin to become closed and a Flash Flood Warning was issued due to the quickly rising water. Fortunately there were no reports of accidents or injury due to the flash flooding.", "ts_dict_index": [1926, 1927, 1928]}
+{"event_id": 983886, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2021-08-31 20:25:00", "end_date_time": "2021-08-31 21:25:00", "narrative": "A similar pattern existed on the 31st compared to the previous day with an upper level low in the eastern Pacific near the west coast of the Baja Peninsula promoting diffluent flow across southeast California. Better moisture existed on this day compared to the previous day, leading to a more enhanced flash flooding event. The most intense rainfall occurred in northeast Imperial County along SR 78, where nearly 7 inches of rain was estimated to have fallen within a 5 hour period. An unbridged crossing along SR 78 at Milpitas Wash became flooded with swiftly flowing water due to the heavy rainfall. A vehicle attempting to cross through the flooded portion of the highway was swept off the roadway before overturning in the wash. Both of the occupants perished in the flash flood. Strong to severe thunderstorms across the Imperial Valley led to damaging wind gusts that resulted in numerous downed power poles. According to the Imperial Irrigation District, extensive damage sustained to the power infrastructure on both the 30th and 31st would cost the district more than $8 million. The California Highway Patrol reported that Cole Boulevard at Dogwood Road was closed due to flooding. No injuries were reported.", "ts_dict_index": [1803, 1804, 1805]}
+{"event_id": 976259, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 11:35:00", "end_date_time": "2021-07-25 12:35:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. The Arizona Department of Transportation reported that Highway 238 was closed between MP 14 and 38, which runs through both Maricopa and Pinal Counties, due to flooding. No damage or injuries were reported.", "ts_dict_index": [1947, 1948, 1949]}
+{"event_id": 953921, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-08 06:34:00", "end_date_time": "2021-06-08 10:00:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and  Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. Numerous roads were flooded and closed near Valliant, with water rescues needed for multiple stranded vehicles. Several homes were flooded as well. Highway 70 in Valliant was flooded and closed. Several vehicles were stalled out in the high water. Numerous streets flooded in and near Valliant.", "ts_dict_index": [1935, 1936, 1937]}
+{"event_id": 977458, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 10:00:00", "end_date_time": "2021-07-25 11:00:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. Local media reported that heavy rainfall led to a home being flooded near 7th Street and Carefree Highway. Water was reported to having rose 5 feet into the home causing significant flood damage. The homeowner, who also runs a personal fitness gym at the home, reported that the gym equipment was destroyed in the flooding. The location was approximated as the exact location of the home is unknown. No injuries were reported.", "ts_dict_index": [1932, 1933, 1934]}
+{"event_id": 953923, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-08 07:07:00", "end_date_time": "2021-06-08 10:00:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and  Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. Numerous roads were flooded and closed near Valliant, with water rescues needed for multiple stranded vehicles. Several homes were flooded as well. Roads were flooded and impassable just north-northwest of Millerton, with one partially washed out.", "ts_dict_index": [1929, 1930, 1931]}
+{"event_id": 953926, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-08 08:22:00", "end_date_time": "2021-06-08 10:30:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and  Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. Numerous roads were flooded and closed near Valliant, with water rescues needed for multiple stranded vehicles. Several homes were flooded as well. Goodwater Road was flooded.", "ts_dict_index": [1938, 1939, 1940]}
+{"event_id": 976258, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-25 08:53:00", "end_date_time": "2021-07-25 09:53:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. A trained weather spotter reported multiple running washes with 6-12 inches of running water over Warren Road in multiple locations.", "ts_dict_index": [1944, 1945, 1946]}
+{"event_id": 953922, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-08 06:47:00", "end_date_time": "2021-06-08 10:00:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and  Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. Numerous roads were flooded and closed near Valliant, with water rescues needed for multiple stranded vehicles. Several homes were flooded as well. Pine Creek Road was flooded and impassable. A motorist stalled in the high water on Pine Creek Road and had to be rescued. JC Loop Road and Rufe Road were also flooded and impassable. A Valliant Police Officer stated that there was an approximately 4 inch rise in water in just 35 minutes.", "ts_dict_index": [1941, 1942, 1943]}
+{"event_id": 1060995, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2022-10-15 16:00:00", "end_date_time": "2022-10-15 19:00:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of southeast CA, mainly from the late morning through the late afternoon hours. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October. Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and small hail. The area of the greatest impacts occurred across the Imperial Valley, where several reports of flooding along with damaging winds and small hail were received. All washes along SR-177 just north of Desert Center were flooded with Big Wash estimated to have received the most rainfall. Timing estimated from radar. No damages or injuries were reported.", "ts_dict_index": [1887, 1888, 1889]}
+{"event_id": 953925, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-08 07:33:00", "end_date_time": "2021-06-08 10:00:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and  Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. Numerous roads were flooded and closed near Valliant, with water rescues needed for multiple stranded vehicles. Several homes were flooded as well. Two homes at 2nd and Norwood Streets beside the old water treatment facility in Wright City were flooded with over 3 feet of water. Another home on 9th Street was flooded. Eastside Road, Old Highway 98, and Highway 98 were flooded and closed.", "ts_dict_index": [1953, 1954, 1955]}
+{"event_id": 977457, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 11:40:00", "end_date_time": "2021-07-25 13:40:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. A video on social media showed several feet of standing water in the parking lot of an apartment, flooding numerous cars at the apartment. No injuries were reported.", "ts_dict_index": [1950, 1951, 1952]}
+{"event_id": 1107542, "event_type": "Flash Flood", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 17:10:00", "end_date_time": "2023-06-03 19:30:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Vehicular high water rescue reported at Hudson Avenue and Regent Street in Shreveport.", "ts_dict_index": [1914, 1915, 1916]}
+{"event_id": 953930, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-08 06:50:00", "end_date_time": "2021-06-08 10:00:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and  Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. Numerous roads were flooded and closed near Valliant, with water rescues needed for multiple stranded vehicles. Several homes were flooded as well. A culvert on Tidmore Road north of Valliant was washed out and the road closed.", "ts_dict_index": [1983, 1984, 1985]}
+{"event_id": 976631, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 16:30:00", "end_date_time": "2021-07-25 17:30:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. Several videos shared by broadcast media and social media showed instances of multiple vehicles getting stuck and/or swept away with multiple people having to be rescued in flash flood waters in Lower Sycamore Creek between the Verde River and Forest Service Road 403. Videos showed an SUV overturning in the creek with two men and an eight-year-old boy still inside. They were able to escape the vehicle with bystanders helping to pull them to safety on land. No injuries or fatalities were reported.", "ts_dict_index": [1962, 1963, 1964]}
+{"event_id": 976483, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 10:55:00", "end_date_time": "2021-07-25 11:55:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. Multiple water rescues were reported in Sun City, including 98th Avenue and Granada Drive as well as 99th Avenue and Burns Drive. A flood control channel along the center of 99th Avenue was also reported to be overflowing onto the street. As a result, a Maricopa County Sheriff's Office deputy stopped southbound traffic at Desert Rock Drive due to the depth of the water. No injuries were reported.", "ts_dict_index": [1986, 1987, 1988]}
+{"event_id": 953920, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-08 05:10:00", "end_date_time": "2021-06-08 10:00:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and  Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. Numerous roads were flooded and closed near Valliant, with water rescues needed for multiple stranded vehicles. Several homes were flooded as well. Widespread street flooding was observed throughout the town of Valliant.", "ts_dict_index": [1989, 1990, 1991]}
+{"event_id": 976647, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-25 12:06:00", "end_date_time": "2021-07-25 13:06:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. A trained weather spotter reported that Bloody Tanks Wash was running near bankfull and containing debris. Water levels were reported to still be on the rise. The high flow in the wash was the result of heavy rainfall over the recent Telegraph fire burn scar, leading to enhanced runoff. No damage or injuries were reported.", "ts_dict_index": [2004, 2005, 2006]}
+{"event_id": 976522, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-25 12:32:00", "end_date_time": "2021-07-25 13:32:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. Heavy rainfall over the recent Telegraph fire burn scar led to enhanced runoff into Pinal Creek. Video from a trained weather spotter showed significant flow through Pinal Creek impacting the unbridged crossing at Beer Tree Crossing and Jesse Hayes Road in Globe. No damage or injuries were reported.", "ts_dict_index": [1998, 1999, 2000]}
+{"event_id": 992752, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 10:50:00", "end_date_time": "2021-07-25 11:50:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. A photo shows a vehicle became stranded in two to three feet of water near the intersection of Dell Webb Boulevard and Bell Road. Timing estimated from radar and other nearby reports. No injuries were reported and extent of water damage to the vehicle is unknown.", "ts_dict_index": [1968, 1969, 1970]}
+{"event_id": 976514, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 11:57:00", "end_date_time": "2021-07-25 12:57:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. Social media video from local media showed three vehicles stuck in the flooded intersection at 107th Avenue and Union Hills Drive. No injuries were reported.", "ts_dict_index": [1965, 1966, 1967]}
+{"event_id": 976510, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 10:55:00", "end_date_time": "2021-07-25 11:55:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. A water rescue was reported at 107th Avenue and Mountain View Road. No injuries were reported.", "ts_dict_index": [1959, 1960, 1961]}
+{"event_id": 953924, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-08 07:17:00", "end_date_time": "2021-06-08 10:00:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and  Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. Numerous roads were flooded and closed near Valliant, with water rescues needed for multiple stranded vehicles. Several homes were flooded as well. Highway 70 from Valliant to Hugo (in Choctaw County) was closed due to high swift moving water. Multiple water rescues were needed.", "ts_dict_index": [1971, 1972, 1973]}
+{"event_id": 953927, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-08 08:00:00", "end_date_time": "2021-06-08 10:00:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and  Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. Numerous roads were flooded and closed near Valliant, with water rescues needed for multiple stranded vehicles. Several homes were flooded as well. Glory Baptist Church was covered in standing water. Chamelon Lane was closed due to flooding and a washed out culvert.", "ts_dict_index": [1980, 1981, 1982]}
+{"event_id": 976596, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 15:00:00", "end_date_time": "2021-07-25 17:00:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. The Sycamore Creek USGS gage (SYCA3) near Fort McDowell recorded a rapid rise with a 6 foot rise in 1.5 hours, cresting at 6.4 feet. This rapid rise is attributed to heavy rain that fell over the Bush fire burn scar, leading to enhanced runoff.", "ts_dict_index": [1974, 1975, 1976]}
+{"event_id": 953933, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-08 07:10:00", "end_date_time": "2021-06-08 10:00:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and  Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. Numerous roads were flooded and closed near Valliant, with water rescues needed for multiple stranded vehicles. Several homes were flooded as well. Little River Road to Golden Glover Road north of Garvin was covered in high swift moving water.  A water rescue occurred on Browning Road.", "ts_dict_index": [1977, 1978, 1979]}
+{"event_id": 976566, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 13:10:00", "end_date_time": "2021-07-25 16:00:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. A Maricopa County Flood Control District streamflow gage at Waterman Wash exceeded alarm stage, peaking at 4.66 feet and impacting downstream unbridged crossings along Tuthill Road and Narramore Road. Roads in this area along the wash were closed with social media videos showing swift moving water impacting these roads. No damage or injuries were reported.", "ts_dict_index": [1992, 1993, 1994]}
+{"event_id": 976265, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-25 12:00:00", "end_date_time": "2021-07-25 13:00:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. County Public Works reported Price Road east of SR 79 in the Florence area was closed due to flooding. No injuries were reported.", "ts_dict_index": [2001, 2002, 2003]}
+{"event_id": 976266, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-25 12:05:00", "end_date_time": "2021-07-25 13:00:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. A social media post showed knee deep water covering the road near Skyline Drive and Felix Road. No damage or injuries were reported.", "ts_dict_index": [1956, 1957, 1958]}
+{"event_id": 1060445, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2022-10-06 14:40:00", "end_date_time": "2022-10-06 16:40:00", "narrative": "A slow moving cutoff low was situated over southern Arizona, providing forced ascent. The low pressure resulted in very cold mid-level temperatures of -13C to -14C, which helped increase the instability with moderate to high levels observed (MLCAPE of 1000-2000 J/KG). High levels of moisture were also observed with PWAT ranging between 1-1.4, which is near record values for early October. The combination of all of these factors led to the development of strong to severe thunderstorms, developing initially across far southwestern Arizona during the early afternoon hours and then moving westward into Imperial County as the afternoon progressed. A well-organized outflow boundary surged well ahead of the thunderstorm complex, resulting in dense blowing dust, which traversed westward across the Imperial Valley and into the Salton Sea area. The blowing dust activity reached as far north as Joshua Tree National Park. Thunderstorms that moved into Imperial County resulted in areas of Flash Flooding along Ogilby Road. Flash flooding along Ogilby Road near Indian Pass Road resulted in mud and gravel mult spots along the road. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [2034, 2035, 2036]}
+{"event_id": 823321, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2019-05-18 20:55:00", "end_date_time": "2019-05-18 23:30:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas. An isolated tornado also touched down just southeast of Tyler with one supercell thunderstorm. These storms began to move repeatedly over the same areas during the evening, with instances of flash flooding reported as well. These storms eventually spread into portions of North Louisiana during the early morning hours of the 19th. High water covered Highway 204 just east of Cushing. The road was closed.", "ts_dict_index": [2031, 2032, 2033]}
+{"event_id": 972232, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 15:05:00", "end_date_time": "2021-07-07 15:05:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Three feet of water completely covered the road at Commercial Boulevard near Swisshelm Park.", "ts_dict_index": [2037, 2038, 2039]}
+{"event_id": 823323, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2019-05-18 21:00:00", "end_date_time": "2019-05-18 23:30:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas. An isolated tornado also touched down just southeast of Tyler with one supercell thunderstorm. These storms began to move repeatedly over the same areas during the evening, with instances of flash flooding reported as well. These storms eventually spread into portions of North Louisiana during the early morning hours of the 19th. High water covered FM 225 south of FM 343. The road was closed.", "ts_dict_index": [2025, 2026, 2027]}
+{"event_id": 823326, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2019-05-18 23:11:00", "end_date_time": "2019-05-19 02:30:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas. An isolated tornado also touched down just southeast of Tyler with one supercell thunderstorm. These storms began to move repeatedly over the same areas during the evening, with instances of flash flooding reported as well. These storms eventually spread into portions of North Louisiana during the early morning hours of the 19th. Numerous streets were flooded and vehicles were stalled out in the high water across the city of Nacogdoches.", "ts_dict_index": [2028, 2029, 2030]}
+{"event_id": 972179, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:40:00", "end_date_time": "2021-07-07 16:30:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Several vehicles were stuck in high water in the area of both Thompson Run Road and Rodi Road.", "ts_dict_index": [2040, 2041, 2042]}
+{"event_id": 976646, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2021-07-25 19:19:00", "end_date_time": "2021-07-25 20:19:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. A video on social media showed a tractor trailer attempting to cross a flooded part of Highway 95 at MP 61. As the tractor trailer drove through the flowing flood waters, it quickly tipped over onto its side. According to the Arizona Department of Transportation, Highway 95 ended up closing due to the flooding. No injuries were reported.", "ts_dict_index": [2013, 2014, 2015]}
+{"event_id": 976459, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 10:05:00", "end_date_time": "2021-07-25 12:30:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. The Maricopa County Flood Control District's Sonoran Wash streamflow gage exceeded bank full after peaking at 5.72 feet. Downstream impacts about one mile from the streamflow gage include unbridged crossings along North Valley Parkway and Dixileta Drive. No damage or injuries were reported.", "ts_dict_index": [2016, 2017, 2018]}
+{"event_id": 976642, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2021-07-25 20:00:00", "end_date_time": "2021-07-25 20:15:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. The Arizona Department of Transportation reported water, mud, rocks, and debris flowing onto Riverside Drive in Parker, impeding travel. No damage or injuries were reported.", "ts_dict_index": [2007, 2008, 2009]}
+{"event_id": 976260, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 09:00:00", "end_date_time": "2021-07-25 10:00:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. A trained weather spotter reported 4-6 inches of running water over the road near Legacy Park Boulevard and Mauna Loa Lane. No damage or injuries were reported.", "ts_dict_index": [2019, 2020, 2021]}
+{"event_id": 976590, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 16:30:00", "end_date_time": "2021-07-25 17:00:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. Tonopah-Salome Highway between 315th Avenue and 339th Avenue was closed due to flooding. This part of the highway is unbridged and crosses through the Hassayampa River. Timing estimated from a Maricopa County Flood Control District streamflow gage along the Hassayampa River. No damage or injuries were reported.", "ts_dict_index": [2010, 2011, 2012]}
+{"event_id": 976261, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 11:40:00", "end_date_time": "2021-07-25 12:40:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. Emergency management reported multiple road closures in Buckeye due to flooding. Roads that were closed after experiencing flooding include Dean Road and Broadway Road, Lower Buckeye Road between Watson Road and Rainbow Road, Verrado Way and Broadway Road, and Verrado Way and Yuma Road. No damage or injuries were reported.", "ts_dict_index": [1995, 1996, 1997]}
+{"event_id": 1045066, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2022-07-03 08:45:00", "end_date_time": "2022-07-03 14:00:00", "narrative": "A west to east oriented shear axis aloft extended along the Middle Red River Valley of North Texas into Southeast Oklahoma to along the Arkansas/Louisiana border during the morning hours of July 3rd, which enhanced large scale forcing for the development of a concentrated area of showers and thunderstorms over portions of Southern Arkansas. A very moist environment was in place across this area as well, which enhanced rain rates as these showers and thunderstorms remained nearly stationary over much of Union County Arkansas through much of the morning hours after daybreak. Widespread rainfall amounts of 3-6 inches fell across Union County, with isolated higher amounts of 7-9+ inches measured across Northern and Central portions of the county. This resulted in widespread flash flooding across much of Union County, flooding and washing away multiple roads, with high water entering multiple buildings in El Dorado. These showers and thunderstorms diminished during the afternoon hours on the 3rd. Multiple pictures were posted to social media of numerous roads that were flooded in Smackover. These pictures also revealed that water entered multiple building within the city.", "ts_dict_index": [2070, 2071, 2072]}
+{"event_id": 1045072, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2022-07-03 10:00:00", "end_date_time": "2022-07-03 14:00:00", "narrative": "A west to east oriented shear axis aloft extended along the Middle Red River Valley of North Texas into Southeast Oklahoma to along the Arkansas/Louisiana border during the morning hours of July 3rd, which enhanced large scale forcing for the development of a concentrated area of showers and thunderstorms over portions of Southern Arkansas. A very moist environment was in place across this area as well, which enhanced rain rates as these showers and thunderstorms remained nearly stationary over much of Union County Arkansas through much of the morning hours after daybreak. Widespread rainfall amounts of 3-6 inches fell across Union County, with isolated higher amounts of 7-9+ inches measured across Northern and Central portions of the county. This resulted in widespread flash flooding across much of Union County, flooding and washing away multiple roads, with high water entering multiple buildings in El Dorado. These showers and thunderstorms diminished during the afternoon hours on the 3rd. High water entered multiple buildings on West Hillsboro Street in El Dorado. Numerous roads were flooded throughout the city.", "ts_dict_index": [2058, 2059, 2060]}
+{"event_id": 972253, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 15:15:00", "end_date_time": "2021-07-07 16:30:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. McLaughlin Run came out of its banks, causing four homes to be evacuated on Baldwin Street and McLaughlin Run Road.", "ts_dict_index": [2046, 2047, 2048]}
+{"event_id": 832605, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2019-06-23 20:01:00", "end_date_time": "2019-06-23 23:15:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. The remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which downed trees across portions of Sevier, Columbia, and Hempstead Counties. They also produced very heavy rainfall which moved repeatedly over the same areas across portions of Hempstead County, which resulted in flash flooding in the city of Hope. The intersection of South Hervey Street and 3rd Street was flooded.", "ts_dict_index": [2055, 2056, 2057]}
+{"event_id": 972155, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:33:00", "end_date_time": "2021-07-07 16:30:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. A few roads were closed due to flooding in Squirrel Hill, with vehicles stranded.", "ts_dict_index": [2049, 2050, 2051]}
+{"event_id": 1045073, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2022-07-03 10:00:00", "end_date_time": "2022-07-03 14:00:00", "narrative": "A west to east oriented shear axis aloft extended along the Middle Red River Valley of North Texas into Southeast Oklahoma to along the Arkansas/Louisiana border during the morning hours of July 3rd, which enhanced large scale forcing for the development of a concentrated area of showers and thunderstorms over portions of Southern Arkansas. A very moist environment was in place across this area as well, which enhanced rain rates as these showers and thunderstorms remained nearly stationary over much of Union County Arkansas through much of the morning hours after daybreak. Widespread rainfall amounts of 3-6 inches fell across Union County, with isolated higher amounts of 7-9+ inches measured across Northern and Central portions of the county. This resulted in widespread flash flooding across much of Union County, flooding and washing away multiple roads, with high water entering multiple buildings in El Dorado. These showers and thunderstorms diminished during the afternoon hours on the 3rd. High water with depths of 3-4 feet covered West 19th Street and Tanglewood Drive in El Dorado. Multiple high water rescues were needed to rescue stranded motorists and residents from their homes.", "ts_dict_index": [2076, 2077, 2078]}
+{"event_id": 972198, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 15:00:00", "end_date_time": "2021-07-07 16:30:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Pinewood and Lakeview Drive were both closed due to flooding, with over 2 feet of running water at the intersection.", "ts_dict_index": [2052, 2053, 2054]}
+{"event_id": 1045070, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2022-07-03 09:52:00", "end_date_time": "2022-07-03 14:00:00", "narrative": "A west to east oriented shear axis aloft extended along the Middle Red River Valley of North Texas into Southeast Oklahoma to along the Arkansas/Louisiana border during the morning hours of July 3rd, which enhanced large scale forcing for the development of a concentrated area of showers and thunderstorms over portions of Southern Arkansas. A very moist environment was in place across this area as well, which enhanced rain rates as these showers and thunderstorms remained nearly stationary over much of Union County Arkansas through much of the morning hours after daybreak. Widespread rainfall amounts of 3-6 inches fell across Union County, with isolated higher amounts of 7-9+ inches measured across Northern and Central portions of the county. This resulted in widespread flash flooding across much of Union County, flooding and washing away multiple roads, with high water entering multiple buildings in El Dorado. These showers and thunderstorms diminished during the afternoon hours on the 3rd. About 3-4 feet of rushing water covered Highway 275 near Philadelphia Road. The road was closed in both directions.", "ts_dict_index": [2067, 2068, 2069]}
+{"event_id": 1045074, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2022-07-03 11:00:00", "end_date_time": "2022-07-03 14:00:00", "narrative": "A west to east oriented shear axis aloft extended along the Middle Red River Valley of North Texas into Southeast Oklahoma to along the Arkansas/Louisiana border during the morning hours of July 3rd, which enhanced large scale forcing for the development of a concentrated area of showers and thunderstorms over portions of Southern Arkansas. A very moist environment was in place across this area as well, which enhanced rain rates as these showers and thunderstorms remained nearly stationary over much of Union County Arkansas through much of the morning hours after daybreak. Widespread rainfall amounts of 3-6 inches fell across Union County, with isolated higher amounts of 7-9+ inches measured across Northern and Central portions of the county. This resulted in widespread flash flooding across much of Union County, flooding and washing away multiple roads, with high water entering multiple buildings in El Dorado. These showers and thunderstorms diminished during the afternoon hours on the 3rd. Multiple pictures were posted to social media of much of Iron Mountain Road in front of Tony's Cycle Shop was washed away.", "ts_dict_index": [2073, 2074, 2075]}
+{"event_id": 1045071, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2022-07-03 09:55:00", "end_date_time": "2022-07-03 14:00:00", "narrative": "A west to east oriented shear axis aloft extended along the Middle Red River Valley of North Texas into Southeast Oklahoma to along the Arkansas/Louisiana border during the morning hours of July 3rd, which enhanced large scale forcing for the development of a concentrated area of showers and thunderstorms over portions of Southern Arkansas. A very moist environment was in place across this area as well, which enhanced rain rates as these showers and thunderstorms remained nearly stationary over much of Union County Arkansas through much of the morning hours after daybreak. Widespread rainfall amounts of 3-6 inches fell across Union County, with isolated higher amounts of 7-9+ inches measured across Northern and Central portions of the county. This resulted in widespread flash flooding across much of Union County, flooding and washing away multiple roads, with high water entering multiple buildings in El Dorado. These showers and thunderstorms diminished during the afternoon hours on the 3rd. Manhole covers were floating away due to floodwaters throughout El Dorado. Widespread flooding was observed across much of Union County.", "ts_dict_index": [2064, 2065, 2066]}
+{"event_id": 1140616, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2023-09-02 17:00:00", "end_date_time": "2023-09-02 18:00:00", "narrative": "A deep closed low along the California coast and broad upper level ridging centered over the southern Plains promoted deep southerly flow across the Desert Southwest. This southerly flow promoted anomalous moisture advection into the area with PWATs upwards of 1.8-2 in the Lower Colorado River Valley area. Abundant moisture combined with CAPE upwards of 1,500-2,000 J/kg and a weak shortwave embedded in the flow allowed for efficient rain-producing thunderstorms to develop heading into the early afternoon hours on the 2nd. Several rain gages recorded over an inch of rainfall with these thunderstorms across southwest Arizona while radar estimates indicated locally heavier amounts in excess of 1.5 in some areas. As a result of these thunderstorms producing very heavy rainfall amounts in a short period of time, numerous instances of flash flooding occurred, particularly in the Yuma, Quartzsite, and Bouse areas. A couple of water rescues occurred, but no injuries were reported during this event. An image on social media showed elevated flow within Tyson Wash through La Paz Valley, making a low water crossing impassable. No damage or injuries were reported.", "ts_dict_index": [2079, 2080, 2081]}
+{"event_id": 972238, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 15:05:00", "end_date_time": "2021-07-07 16:30:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. A vehicle was stuck in rising water on Station Street.", "ts_dict_index": [2043, 2044, 2045]}
+{"event_id": 1101328, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2023-07-12 04:55:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. County Road 5 was flooded.", "ts_dict_index": [2112, 2113, 2114]}
+{"event_id": 1101330, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2023-07-12 05:00:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. County Road 38 was closed due to flooding.", "ts_dict_index": [2106, 2107, 2108]}
+{"event_id": 1101345, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2023-07-12 08:00:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. Significant flooding across County Road 57, with portions of the roadway and culverts washed out.", "ts_dict_index": [2109, 2110, 2111]}
+{"event_id": 1140615, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2023-09-02 14:20:00", "end_date_time": "2023-09-02 15:20:00", "narrative": "A deep closed low along the California coast and broad upper level ridging centered over the southern Plains promoted deep southerly flow across the Desert Southwest. This southerly flow promoted anomalous moisture advection into the area with PWATs upwards of 1.8-2 in the Lower Colorado River Valley area. Abundant moisture combined with CAPE upwards of 1,500-2,000 J/kg and a weak shortwave embedded in the flow allowed for efficient rain-producing thunderstorms to develop heading into the early afternoon hours on the 2nd. Several rain gages recorded over an inch of rainfall with these thunderstorms across southwest Arizona while radar estimates indicated locally heavier amounts in excess of 1.5 in some areas. As a result of these thunderstorms producing very heavy rainfall amounts in a short period of time, numerous instances of flash flooding occurred, particularly in the Yuma, Quartzsite, and Bouse areas. A couple of water rescues occurred, but no injuries were reported during this event. A video on social media showed a semi driving through a flooded low water crossing along SR 72 at Avenue 41 E with at least 6 inches of water flowing over the road. Timing was estimated from radar. No damage or injuries were reported.", "ts_dict_index": [2097, 2098, 2099]}
+{"event_id": 1140636, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2023-09-02 19:12:00", "end_date_time": "2023-09-02 20:12:00", "narrative": "A deep closed low along the California coast and broad upper level ridging centered over the southern Plains promoted deep southerly flow across the Desert Southwest. This southerly flow promoted anomalous moisture advection into the area with PWATs upwards of 1.8-2 in the Lower Colorado River Valley area. Abundant moisture combined with CAPE upwards of 1,500-2,000 J/kg and a weak shortwave embedded in the flow allowed for efficient rain-producing thunderstorms to develop heading into the early afternoon hours on the 2nd. Several rain gages recorded over an inch of rainfall with these thunderstorms across southwest Arizona while radar estimates indicated locally heavier amounts in excess of 1.5 in some areas. As a result of these thunderstorms producing very heavy rainfall amounts in a short period of time, numerous instances of flash flooding occurred, particularly in the Yuma, Quartzsite, and Bouse areas. A couple of water rescues occurred, but no injuries were reported during this event. Quartzsite Fire and Police performed a swift water rescue of two juveniles trapped on a small island in Tyson Wash. No injuries were reported.", "ts_dict_index": [2100, 2101, 2102]}
+{"event_id": 1140634, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2023-09-02 18:05:00", "end_date_time": "2023-09-02 19:05:00", "narrative": "A deep closed low along the California coast and broad upper level ridging centered over the southern Plains promoted deep southerly flow across the Desert Southwest. This southerly flow promoted anomalous moisture advection into the area with PWATs upwards of 1.8-2 in the Lower Colorado River Valley area. Abundant moisture combined with CAPE upwards of 1,500-2,000 J/kg and a weak shortwave embedded in the flow allowed for efficient rain-producing thunderstorms to develop heading into the early afternoon hours on the 2nd. Several rain gages recorded over an inch of rainfall with these thunderstorms across southwest Arizona while radar estimates indicated locally heavier amounts in excess of 1.5 in some areas. As a result of these thunderstorms producing very heavy rainfall amounts in a short period of time, numerous instances of flash flooding occurred, particularly in the Yuma, Quartzsite, and Bouse areas. A couple of water rescues occurred, but no injuries were reported during this event. A low water crossing through Tyson Wash along Kuehn Street was inundated by flash flooding, causing the road to be closed. Timing was estimated based on the stream gauge response located along Main Street. No damage or injuries were reported.", "ts_dict_index": [2082, 2083, 2084]}
+{"event_id": 1140617, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2023-09-02 14:15:00", "end_date_time": "2023-09-02 18:15:00", "narrative": "A deep closed low along the California coast and broad upper level ridging centered over the southern Plains promoted deep southerly flow across the Desert Southwest. This southerly flow promoted anomalous moisture advection into the area with PWATs upwards of 1.8-2 in the Lower Colorado River Valley area. Abundant moisture combined with CAPE upwards of 1,500-2,000 J/kg and a weak shortwave embedded in the flow allowed for efficient rain-producing thunderstorms to develop heading into the early afternoon hours on the 2nd. Several rain gages recorded over an inch of rainfall with these thunderstorms across southwest Arizona while radar estimates indicated locally heavier amounts in excess of 1.5 in some areas. As a result of these thunderstorms producing very heavy rainfall amounts in a short period of time, numerous instances of flash flooding occurred, particularly in the Yuma, Quartzsite, and Bouse areas. A couple of water rescues occurred, but no injuries were reported during this event. A stream gauge along Bouse Wash at Plomosa Road rose above Action stage around 1415MST, making low water crossings along the wash impassable. The wash remained above Action stage into the morning hours on the 3rd. No damage or injuries were reported.", "ts_dict_index": [2094, 2095, 2096]}
+{"event_id": 1140635, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2023-09-02 18:30:00", "end_date_time": "2023-09-02 19:30:00", "narrative": "A deep closed low along the California coast and broad upper level ridging centered over the southern Plains promoted deep southerly flow across the Desert Southwest. This southerly flow promoted anomalous moisture advection into the area with PWATs upwards of 1.8-2 in the Lower Colorado River Valley area. Abundant moisture combined with CAPE upwards of 1,500-2,000 J/kg and a weak shortwave embedded in the flow allowed for efficient rain-producing thunderstorms to develop heading into the early afternoon hours on the 2nd. Several rain gages recorded over an inch of rainfall with these thunderstorms across southwest Arizona while radar estimates indicated locally heavier amounts in excess of 1.5 in some areas. As a result of these thunderstorms producing very heavy rainfall amounts in a short period of time, numerous instances of flash flooding occurred, particularly in the Yuma, Quartzsite, and Bouse areas. A couple of water rescues occurred, but no injuries were reported during this event. A low water crossing through Tyson Wash along Quail Trail Street was inundated by flash flooding, causing the road to be close. Timing was estimated based on the Tyson Wash stream gauge response on Main Street. No damage or injuries were reported.", "ts_dict_index": [2085, 2086, 2087]}
+{"event_id": 1140618, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2023-09-02 15:25:00", "end_date_time": "2023-09-02 17:25:00", "narrative": "A deep closed low along the California coast and broad upper level ridging centered over the southern Plains promoted deep southerly flow across the Desert Southwest. This southerly flow promoted anomalous moisture advection into the area with PWATs upwards of 1.8-2 in the Lower Colorado River Valley area. Abundant moisture combined with CAPE upwards of 1,500-2,000 J/kg and a weak shortwave embedded in the flow allowed for efficient rain-producing thunderstorms to develop heading into the early afternoon hours on the 2nd. Several rain gages recorded over an inch of rainfall with these thunderstorms across southwest Arizona while radar estimates indicated locally heavier amounts in excess of 1.5 in some areas. As a result of these thunderstorms producing very heavy rainfall amounts in a short period of time, numerous instances of flash flooding occurred, particularly in the Yuma, Quartzsite, and Bouse areas. A couple of water rescues occurred, but no injuries were reported during this event. A swift water rescue occurred after a single occupied vehicle attempted to drive through a flooded Bouse Wash low water crossing along Rabbit Lane near Stage Coach Road. No injuries were reported.", "ts_dict_index": [2088, 2089, 2090]}
+{"event_id": 1140633, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2023-09-02 18:12:00", "end_date_time": "2023-09-02 18:42:00", "narrative": "A deep closed low along the California coast and broad upper level ridging centered over the southern Plains promoted deep southerly flow across the Desert Southwest. This southerly flow promoted anomalous moisture advection into the area with PWATs upwards of 1.8-2 in the Lower Colorado River Valley area. Abundant moisture combined with CAPE upwards of 1,500-2,000 J/kg and a weak shortwave embedded in the flow allowed for efficient rain-producing thunderstorms to develop heading into the early afternoon hours on the 2nd. Several rain gages recorded over an inch of rainfall with these thunderstorms across southwest Arizona while radar estimates indicated locally heavier amounts in excess of 1.5 in some areas. As a result of these thunderstorms producing very heavy rainfall amounts in a short period of time, numerous instances of flash flooding occurred, particularly in the Yuma, Quartzsite, and Bouse areas. A couple of water rescues occurred, but no injuries were reported during this event. A stream gauge along Tyson Wash in Quartzsite observed a rapid rise, reaching Action stage at 1812MST. As a result, low water crossings along the wash were inundated and made impassable. No damage or injuries were reported.", "ts_dict_index": [2103, 2104, 2105]}
+{"event_id": 976513, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-25 11:37:00", "end_date_time": "2021-07-25 12:37:00", "narrative": "A retrograding upper level low combined with anomalously high moisture levels led to showers and isolated thunderstorms producing heavy rainfall and numerous instances of considerable flash flooding across south-central Arizona on the 25th. The places that saw the heaviest rainfall amounts were areas that experienced heavy showers training over the same locations. Western portions of the Phoenix metro saw training showers with heavy rainfall occur, leading to widespread amounts of 1.5-2.5 with locally higher amounts of 3+. As a result, there were numerous reports of flash flooding, including multiple water rescues and numerous road closures due to flooding. Heavy rainfall also fell over multiple burn scars, leading to several instances of burn scar flash flooding. One of the burn scars that saw heavy rainfall was the Bush fire burn scar, which led to enhanced runoff and a rapid rise on Sycamore Creek. Several people were rescued after getting stuck in the increased flow in Sycamore Creek. No injuries were reported. Several lanes on I-10 near 75th Avenue and 91st Avenue were flooded and became impassable. The I-10 westbound off-ramp at 59th Avenue was closed due to flooding. No damage or injuries were reported.", "ts_dict_index": [2022, 2023, 2024]}
+{"event_id": 1101329, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2023-07-12 04:57:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. A nursing home and rehab facility in Stamps was flooded, with the residents evacuated.", "ts_dict_index": [2115, 2116, 2117]}
+{"event_id": 1101323, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2023-07-12 04:12:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. Water rescues were needed for vehicles trapped in flood waters on the south side of Hope.", "ts_dict_index": [2124, 2125, 2126]}
+{"event_id": 1101304, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2023-07-12 03:32:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. Multiple roads were flooded and impassable in Buckner.", "ts_dict_index": [2127, 2128, 2129]}
+{"event_id": 1101326, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2023-07-12 04:40:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. Highway 32 between Hope and Bodcaw was flooded.", "ts_dict_index": [2121, 2122, 2123]}
+{"event_id": 1101332, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2023-07-12 05:52:00", "end_date_time": "2023-07-12 08:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. The intersection of Lorene Street and Junction City Road was flooded in ankle deep water.", "ts_dict_index": [2118, 2119, 2120]}
+{"event_id": 1045068, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2022-07-03 09:45:00", "end_date_time": "2022-07-03 14:00:00", "narrative": "A west to east oriented shear axis aloft extended along the Middle Red River Valley of North Texas into Southeast Oklahoma to along the Arkansas/Louisiana border during the morning hours of July 3rd, which enhanced large scale forcing for the development of a concentrated area of showers and thunderstorms over portions of Southern Arkansas. A very moist environment was in place across this area as well, which enhanced rain rates as these showers and thunderstorms remained nearly stationary over much of Union County Arkansas through much of the morning hours after daybreak. Widespread rainfall amounts of 3-6 inches fell across Union County, with isolated higher amounts of 7-9+ inches measured across Northern and Central portions of the county. This resulted in widespread flash flooding across much of Union County, flooding and washing away multiple roads, with high water entering multiple buildings in El Dorado. These showers and thunderstorms diminished during the afternoon hours on the 3rd. Multiple pictures were posted to social media of portions of the 300-400 block of North Tate Street and the 500-600 block of East Padgett Street in Norphlet were washed out. A personal electronic rain gauge in Norphlet measured 9.12 inches of rain from this event.", "ts_dict_index": [2061, 2062, 2063]}
+{"event_id": 1101338, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2023-07-12 06:28:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. A water rescue was needed on Main street at Tatum Branch in Stamps, due to a vehicle that was swept off of the roadway.", "ts_dict_index": [2133, 2134, 2135]}
+{"event_id": 1101341, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2023-07-12 08:00:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. Significant flooding over County Road 8, with a portion of the roadway washed out.", "ts_dict_index": [2130, 2131, 2132]}
+{"event_id": 1101322, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2023-07-12 04:08:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. Roads were flooded along Highway 313 just south of Lewisville.", "ts_dict_index": [2145, 2146, 2147]}
+{"event_id": 1101334, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "UNION", "begin_date_time": "2023-07-12 05:54:00", "end_date_time": "2023-07-12 08:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. The eastbound lane of Strong Highway was flooded.", "ts_dict_index": [2142, 2143, 2144]}
+{"event_id": 1101321, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2023-07-12 03:45:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. Highway 82 was flooded and impassable in Stamps.", "ts_dict_index": [2139, 2140, 2141]}
+{"event_id": 1101340, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "HEMPSTEAD", "begin_date_time": "2023-07-12 06:50:00", "end_date_time": "2023-07-12 10:45:00", "narrative": "A Mesoscale Convective Vortex (MCV) that was a remnant of showers and thunderstorms over Central Oklahoma on July 11th, drifted east into Southwest Arkansas during the early morning hours of the 12th. This upper level disturbance moved over an area that was very warm, moist, and unstable, and focused a cluster of showers and thunderstorms throughout much of the morning hours before drifting east out of the region by midday. These showers and thunderstorms moved repeatedly over the same areas, and were efficient rainfall producers such that flash flooding was widespread across portions of Southwest Arkansas. Widespread rainfall amounts of 3-6 inches, with isolated higher amounts in excess of 8 inches, fell across portions of Southwest Arkansas before ending by the mid morning hours on the 12th. In addition, an isolated tornado was spawned from this cluster of thunderstorms over Eastern Lafayette County just south of Stamps before these storms shifted east of the region later that morning. A clogged storm drain resulted in repeated flooding along South Main Street at Townsend Outdoors in Hope.", "ts_dict_index": [2136, 2137, 2138]}
+{"event_id": 834612, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-06-28 19:52:00", "end_date_time": "2019-06-28 19:52:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. The broadcast media reported that water was flowing down Route 136 in town.", "ts_dict_index": [2178, 2179, 2180]}
+{"event_id": 964764, "event_type": "Flash Flood", "state": "OKLAHOMA", "cz_name": "TULSA", "begin_date_time": "2021-06-07 06:00:00", "end_date_time": "2021-06-07 07:15:00", "narrative": "A broad low pressure center in the middle and upper atmosphere moved from northern Texas to northeastern Oklahoma on the 6th and 7th. The first round of thunderstorms affected southeastern Oklahoma during the morning and afternoon hours of the 6th. Locally heavy rainfall occurred, which resulted in isolated flash flooding. ||A more pronounced and focused area of thunderstorms developed during the early morning hours of the 7th across northeastern Oklahoma. The storms were slow-moving, and very efficient rain producers due to high amounts of moisture in the air. A swath of heavy rain occurred across portions of McIntosh, Okfuskee, Okmulgee, Tulsa, and Pawnee Counties, where widespread two to eight inch amounts occurred. Personal weather stations in Okmulgee County measured over thirteen inches of rain in a several hour period, with rainfall rates as much as six and a half inches per hour. Widespread flash flooding occurred as a result of this heavy rainfall. Several roads were reported flooded, including eastbound portions of I-44 between Highway 75 and I-244.", "ts_dict_index": [2181, 2182, 2183]}
+{"event_id": 834614, "event_type": "Flash Flood", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-06-28 21:28:00", "end_date_time": "2019-06-28 22:00:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. The broadcast media reported that Market Street was flooded.", "ts_dict_index": [2175, 2176, 2177]}
+{"event_id": 1048627, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2022-07-28 12:30:00", "end_date_time": "2022-07-28 14:30:00", "narrative": "The combination of near record moisture content (PWATs 1.8-2.0 inches), moderate to strong instability (SBCAPE  2000 J/KG), very slow steering flow and an upper-level disturbance resulted in a very conducive environment for the generation of thunderstorms producing very heavy rainfall activity across portions of south-central and southwestern Arizona, resulting in flash flooding. Activity first developed across the foothills and higher terrain of Eastern Maricopa and Gila Counties during the late morning-early afternoon hours. Another area of thunderstorms developed over northwestern Arizona during the mid-late afternoon hours and move southward towards La Paz County into the evening hours. One of the areas severely hit by flash flooding was Apache Junction, AZ. Weekes Wash, which runs through the town, went of out of its banks, causing widespread flooding impacts across the city. Flooding also took place from drainage that occurred off the Goldfield and Superstitions Mountains. Social media video showed Bloody Tanks Wash in major elevated stage as it was flowing down the city of Miami. No damages or injuries were reported.", "ts_dict_index": [2163, 2164, 2165]}
+{"event_id": 1048634, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-28 12:30:00", "end_date_time": "2022-07-28 15:30:00", "narrative": "The combination of near record moisture content (PWATs 1.8-2.0 inches), moderate to strong instability (SBCAPE  2000 J/KG), very slow steering flow and an upper-level disturbance resulted in a very conducive environment for the generation of thunderstorms producing very heavy rainfall activity across portions of south-central and southwestern Arizona, resulting in flash flooding. Activity first developed across the foothills and higher terrain of Eastern Maricopa and Gila Counties during the late morning-early afternoon hours. Another area of thunderstorms developed over northwestern Arizona during the mid-late afternoon hours and move southward towards La Paz County into the evening hours. One of the areas severely hit by flash flooding was Apache Junction, AZ. Weekes Wash, which runs through the town, went of out of its banks, causing widespread flooding impacts across the city. Flooding also took place from drainage that occurred off the Goldfield and Superstitions Mountains. The Arizona Department of Transportation reported SR 88 was closed due to flooding between milepost 201 and 205. No damages or injuries were reported.", "ts_dict_index": [2166, 2167, 2168]}
+{"event_id": 1048620, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-07-28 12:00:00", "end_date_time": "2022-07-28 17:00:00", "narrative": "The combination of near record moisture content (PWATs 1.8-2.0 inches), moderate to strong instability (SBCAPE  2000 J/KG), very slow steering flow and an upper-level disturbance resulted in a very conducive environment for the generation of thunderstorms producing very heavy rainfall activity across portions of south-central and southwestern Arizona, resulting in flash flooding. Activity first developed across the foothills and higher terrain of Eastern Maricopa and Gila Counties during the late morning-early afternoon hours. Another area of thunderstorms developed over northwestern Arizona during the mid-late afternoon hours and move southward towards La Paz County into the evening hours. One of the areas severely hit by flash flooding was Apache Junction, AZ. Weekes Wash, which runs through the town, went of out of its banks, causing widespread flooding impacts across the city. Flooding also took place from drainage that occurred off the Goldfield and Superstitions Mountains. Between 1 and 3 inches of rain fell within 1-2 hours across Apache Junction and the adjacent higher terrain north and east of the city, towards the Goldfield and Superstitions mountains. Water from those mountains drained down towards the area washes, including Weekes Wash, which runs through the city. Numerous roads were flooded and damaged along with multiple water rescues taking place of residents in homes that either were surrounded with water or had water inside them. One of the more dramatic water rescues occurred when a woman had to be rescued from her vehicle that was swept away by the flood waters of Weekes Wash and traveled half a mile downstream before encountering a box culvert. No injuries or fatalities were reported.", "ts_dict_index": [2154, 2155, 2156]}
+{"event_id": 1048628, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2022-07-28 12:15:00", "end_date_time": "2022-07-28 14:15:00", "narrative": "The combination of near record moisture content (PWATs 1.8-2.0 inches), moderate to strong instability (SBCAPE  2000 J/KG), very slow steering flow and an upper-level disturbance resulted in a very conducive environment for the generation of thunderstorms producing very heavy rainfall activity across portions of south-central and southwestern Arizona, resulting in flash flooding. Activity first developed across the foothills and higher terrain of Eastern Maricopa and Gila Counties during the late morning-early afternoon hours. Another area of thunderstorms developed over northwestern Arizona during the mid-late afternoon hours and move southward towards La Paz County into the evening hours. One of the areas severely hit by flash flooding was Apache Junction, AZ. Weekes Wash, which runs through the town, went of out of its banks, causing widespread flooding impacts across the city. Flooding also took place from drainage that occurred off the Goldfield and Superstitions Mountains. A video posted on social media showed strong flow moving along the Bloody Tanks Wash, resulting a street crossing the wash near Mackey Camp to be completely impassable. No damages or injuries were reported.", "ts_dict_index": [2157, 2158, 2159]}
+{"event_id": 1048636, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2022-07-28 21:00:00", "end_date_time": "2022-07-28 23:00:00", "narrative": "The combination of near record moisture content (PWATs 1.8-2.0 inches), moderate to strong instability (SBCAPE  2000 J/KG), very slow steering flow and an upper-level disturbance resulted in a very conducive environment for the generation of thunderstorms producing very heavy rainfall activity across portions of south-central and southwestern Arizona, resulting in flash flooding. Activity first developed across the foothills and higher terrain of Eastern Maricopa and Gila Counties during the late morning-early afternoon hours. Another area of thunderstorms developed over northwestern Arizona during the mid-late afternoon hours and move southward towards La Paz County into the evening hours. One of the areas severely hit by flash flooding was Apache Junction, AZ. Weekes Wash, which runs through the town, went of out of its banks, causing widespread flooding impacts across the city. Flooding also took place from drainage that occurred off the Goldfield and Superstitions Mountains. La Paz County Dispatch reported the following roadways were closed due to flooding from water overflowing from Tyson Wash:  Tyson Street, North Washington Avenue from Quail Trail to Kenoyer Streets, and Plymouth Road. at Mockingbird St. No damages or injuries were reported.", "ts_dict_index": [2160, 2161, 2162]}
+{"event_id": 1048633, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-28 13:50:00", "end_date_time": "2022-07-28 15:50:00", "narrative": "The combination of near record moisture content (PWATs 1.8-2.0 inches), moderate to strong instability (SBCAPE  2000 J/KG), very slow steering flow and an upper-level disturbance resulted in a very conducive environment for the generation of thunderstorms producing very heavy rainfall activity across portions of south-central and southwestern Arizona, resulting in flash flooding. Activity first developed across the foothills and higher terrain of Eastern Maricopa and Gila Counties during the late morning-early afternoon hours. Another area of thunderstorms developed over northwestern Arizona during the mid-late afternoon hours and move southward towards La Paz County into the evening hours. One of the areas severely hit by flash flooding was Apache Junction, AZ. Weekes Wash, which runs through the town, went of out of its banks, causing widespread flooding impacts across the city. Flooding also took place from drainage that occurred off the Goldfield and Superstitions Mountains. North Lake Rd along Bartlett Lake was closed due to flooding and debris making the road impassable to vehicular traffic. No injuries were reported.", "ts_dict_index": [2151, 2152, 2153]}
+{"event_id": 850418, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2019-09-23 10:15:00", "end_date_time": "2019-09-23 15:15:00", "narrative": "Scattered thunderstorms developed across portions of La Paz County on September 23rd, beginning in the morning and continuing into the afternoon. Many of the storms produced intense rainfall with peak rain rates in excess of 2 inches per hour. The heavy rain resulted in episodes of late morning flash flooding across the central portion of the county and north of Interstate 10. At 1100MST local county officials reported that flash flooding forced the closure of Plomosa Road between Highways 95 and 72. Flash flooding also resulted in the closure of Highway 72 southeast of Bouse between mile markers 17 and 38. A Flash Flood Warning was issued for the area beginning at 1015MST. No accidents were reported due to the flash flooding. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Scattered to numerous showers and thunderstorms developed across portions of La Paz County during the morning hours on September 23rd, and they continued into the afternoon. The stronger storms generated intense rainfall with peak rain rates in excess of 2 inches per hour. The heavy rain led to episodes of flash flooding across central portions of the county and north of Interstate 10. According to local county officials, at 1100MST flash flooding resulted in the closure of Plomosa Road between Highways 95 and 72, roughly 6 miles to the southwest of Bouse. A Flash Flood Warning had been issued at 1015MST and was in effect at the time of the flooding. No accidents were reported.", "ts_dict_index": [2169, 2170, 2171]}
+{"event_id": 1048629, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-28 13:00:00", "end_date_time": "2022-07-28 15:00:00", "narrative": "The combination of near record moisture content (PWATs 1.8-2.0 inches), moderate to strong instability (SBCAPE  2000 J/KG), very slow steering flow and an upper-level disturbance resulted in a very conducive environment for the generation of thunderstorms producing very heavy rainfall activity across portions of south-central and southwestern Arizona, resulting in flash flooding. Activity first developed across the foothills and higher terrain of Eastern Maricopa and Gila Counties during the late morning-early afternoon hours. Another area of thunderstorms developed over northwestern Arizona during the mid-late afternoon hours and move southward towards La Paz County into the evening hours. One of the areas severely hit by flash flooding was Apache Junction, AZ. Weekes Wash, which runs through the town, went of out of its banks, causing widespread flooding impacts across the city. Flooding also took place from drainage that occurred off the Goldfield and Superstitions Mountains. Water Users Recreation Site just downstream of Saguaro Lake was closed due to flash flooding and debris deposited into the Lower Salt River, making the water unsafe for public use. No injuries were reported.", "ts_dict_index": [2148, 2149, 2150]}
+{"event_id": 1140623, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2023-09-02 15:30:00", "end_date_time": "2023-09-02 16:30:00", "narrative": "A deep closed low along the California coast and broad upper level ridging centered over the southern Plains promoted deep southerly flow across the Desert Southwest. This southerly flow promoted anomalous moisture advection into the area with PWATs upwards of 1.8-2 in the Lower Colorado River Valley area. Abundant moisture combined with CAPE upwards of 1,500-2,000 J/kg and a weak shortwave embedded in the flow allowed for efficient rain-producing thunderstorms to develop heading into the early afternoon hours on the 2nd. Several rain gages recorded over an inch of rainfall with these thunderstorms across southwest Arizona while radar estimates indicated locally heavier amounts in excess of 1.5 in some areas. As a result of these thunderstorms producing very heavy rainfall amounts in a short period of time, numerous instances of flash flooding occurred, particularly in the Yuma, Quartzsite, and Bouse areas. A couple of water rescues occurred, but no injuries were reported during this event. Numerous washes along Highway 60 between mile markers 31-50 were flooded. Timing was estimated from radar. No damage or injuries were reported.", "ts_dict_index": [2091, 2092, 2093]}
+{"event_id": 1111872, "event_type": "Flash Flood", "state": "GEORGIA", "cz_name": "LOWNDES", "begin_date_time": "2023-06-15 14:00:00", "end_date_time": "2023-06-15 15:00:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. Several roads were flooded in Lowndes county.", "ts_dict_index": [2184, 2185, 2186]}
+{"event_id": 984216, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 13:40:00", "end_date_time": "2021-08-18 18:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. A couple videos showed significant flowing water through Skunk Creek with flow over Honda Bow Road. One of the videos showed someone being rescued on the hood of a truck by a good Samaritan from their SUV that stalled in the floodwaters. Rainfall amounts over 1 inch were observed over the foothill areas upstream of this location. Timing of impacts adjusted based on radar. No injuries were reported.", "ts_dict_index": [2187, 2188, 2189]}
+{"event_id": 985133, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 15:09:00", "end_date_time": "2021-08-18 16:09:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Videos from a local TV station showed deep, swiftly moving water flowing in a wash across an unbridged crossing along 7th Avenue near Coral Gables Drive in Moon Valley. Nearby, Greenway Road was closed at I-17 due to flooding. No damage or injuries were reported.", "ts_dict_index": [2199, 2200, 2201]}
+{"event_id": 984029, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 14:35:00", "end_date_time": "2021-08-18 15:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. A Maricopa County Flood Control District stream gage along Cave Creek north of Carefree Highway exceeded bank full stage, impacting downstream low water crossings. At 1502MST, the creek crested at 7.65 feet and 5178 CFS. No damage or injuries were reported.", "ts_dict_index": [2208, 2209, 2210]}
+{"event_id": 984219, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 14:15:00", "end_date_time": "2021-08-18 17:00:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Significant flow in a typically dry wash made Carefree Highway between Tom Darlington Drive and Stagecoach Pass impassable to all traffic. There was also a photo that showed a lot of mud and gravel in one of the southbound lanes of Tom Darlington Drive near Meander Way. Both of these were reported around 1550PM. Very heavy rain began over the area and just upstream closer to 1300MST, with measured and radar estimated rainfall amounts of 2 to 4 inches in 1 hour. Timing of impacts adjusted based on radar. No damages or injuries were reported.", "ts_dict_index": [2202, 2203, 2204]}
+{"event_id": 984218, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 15:30:00", "end_date_time": "2021-08-18 20:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. After 2 to 4 inches of rain fell over the northern portions of the 2020 Bush Fire burn area, a USGS streamflow gage on Sycamore Creek (SYCA3) registered a rapid rise from 2.53 feet at 01530MST to 9.38 feet at 1545MST. Flow continued to rise and crested 11.77 feet at 1730MST, 1.73 feet below action stage. No damages or injuries were reported.", "ts_dict_index": [2214, 2215, 2216]}
+{"event_id": 983955, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 12:00:00", "end_date_time": "2021-08-18 14:00:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Arizona Department of Transportation reported State Route 188 was closed in both directions near mile post 219 due to flooding. No damages or injuries were reported.", "ts_dict_index": [2190, 2191, 2192]}
+{"event_id": 984217, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 14:30:00", "end_date_time": "2021-08-18 16:45:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Broadcast media coverage showed significant flow in East Fork Cave Creek leading to the closure of 7th Avenue near Coral Gables Street. A Flood Control District of Maricopa County streamflow gage a few hundred feet upstream from 7th Avenue exceeded alarm stage at 1422MST, crested at 3.66 feet at 1509MST, and fell back below alarm stage at 1645MST. A man tested the floodwaters with his unicycle, but wisely turned around. No damages or injuries were reported.", "ts_dict_index": [2193, 2194, 2195]}
+{"event_id": 984207, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 10:25:00", "end_date_time": "2021-08-18 12:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Photos and videos show large sections of Russell Road, in multiple spots, were eroded and washed into Russell Gulch during significant flash flooding. Some photos, after the water receded, suggest the floodwaters may have been 6 to 8 feet deep. The significant destruction of Russell Road occurred roughly 2 miles south of the catastrophic flooding that occurred in the Claypool area, between Miami and Globe. Timing based on webcam footage in the area. No injuries were reported.", "ts_dict_index": [2220, 2221, 2222]}
+{"event_id": 984194, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 15:15:00", "end_date_time": "2021-08-18 17:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Arizona Department of Transportation closed State Route 88 between mile posts 230 and 242 due to flooding. Timing of impacts based on radar. No damages or injuries were reported.", "ts_dict_index": [2217, 2218, 2219]}
+{"event_id": 984220, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 15:45:00", "end_date_time": "2021-08-18 21:45:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. The unpaved portion of State Route 88/Apache Trail was closed between NF-79 (mile post 230) and NF-51 (mile post 242) due to significant flash flooding and the road being washed out in many places. Arizona Department of Transportation reported the closure on the 19th, but the flooding impacts occurred on the 18th. According to Apache Lake Marina & Resort, some customers and employees had to be evacuated out of the area. Videos on social media show some of the road damage and washouts. The nearest rain gage at Reavis Trailhead measured 1.61 inches between 1350MST and 1550MST and radar estimates were upwards of 2 inches. Runoff on the southern end of the closure may have been enhanced by the 2019 Woodbury Fire burn area. Timing based on the rain gage and radar. No injuries were reported.", "ts_dict_index": [2223, 2224, 2225]}
+{"event_id": 985142, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 13:16:00", "end_date_time": "2021-08-18 16:16:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. A camera located along Kitty Joe Creek showed high, swiftly moving flow that was nearly topping the banks of the creek. No damage or injuries were reported.", "ts_dict_index": [2205, 2206, 2207]}
+{"event_id": 850415, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "LA PAZ", "begin_date_time": "2019-09-23 10:15:00", "end_date_time": "2019-09-23 15:15:00", "narrative": "Scattered thunderstorms developed across portions of La Paz County on September 23rd, beginning in the morning and continuing into the afternoon. Many of the storms produced intense rainfall with peak rain rates in excess of 2 inches per hour. The heavy rain resulted in episodes of late morning flash flooding across the central portion of the county and north of Interstate 10. At 1100MST local county officials reported that flash flooding forced the closure of Plomosa Road between Highways 95 and 72. Flash flooding also resulted in the closure of Highway 72 southeast of Bouse between mile markers 17 and 38. A Flash Flood Warning was issued for the area beginning at 1015MST. No accidents were reported due to the flash flooding. In 2020, the Arizona Department of Transportation was awarded $10.7 million from the Federal Highway Administration to support the repair of roads and bridges damaged due to the numerous flash flooding events that occurred across Arizona on the 23rd. Scattered to numerous showers and thunderstorms developed across portions of La Paz County during the late morning hours, and they continued into the afternoon. The stronger storms generated intense rainfall with peak rain rates in excess of 2 inches per hour. The heavy rain resulted in flash flooding which affected central portions of the county including areas around the town of Bouse. According to local county officials, at 1100MST flash flooding 9 miles southeast of Bouse forced the closure of Highway 72 between mile markers 17 and 38. A Flash Flood Warning had been issued at 1015MST and was in effect at the time of the flooding. No accidents were reported.", "ts_dict_index": [2172, 2173, 2174]}
+{"event_id": 983964, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 12:10:00", "end_date_time": "2021-08-18 18:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. A USGS streamflow gage along Pinal Creek near Inspiration Dam measured multiple a couple rapid rises between 1230MST and 1430MST with a peak stage cresting at 8 feet. The flood waves likely originated from heavy rain roughly 15 miles upstream over the 2021 Telegraph burn area southwest of Globe. There were a couple more smaller follow-on waves that were recorded as the flow was decreasing from its crest. No damages or injuries were reported.", "ts_dict_index": [2250, 2251, 2252]}
+{"event_id": 983903, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 09:10:00", "end_date_time": "2021-08-18 13:10:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Multiple photos and videos showed a few feet of rapidly flowing water within Campaign Creek, leading to the closure of Mesquite Street in Roosevelt Estates. One video even showed a 6 to 8 foot standing wave of water. Video after the water receded showed significant damage to the road. No injuries were reported.", "ts_dict_index": [2241, 2242, 2243]}
+{"event_id": 984316, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 17:00:00", "end_date_time": "2021-08-18 18:00:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Roads into Bartlett Lake were reported to be flooded and impassable in multiple locations, with some people having to be rescued out of the lake area.", "ts_dict_index": [2226, 2227, 2228]}
+{"event_id": 984027, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 13:34:00", "end_date_time": "2021-08-18 20:15:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. FCDMC STREAM GAUGE||A Maricopa County Flood Control District stream gage located along Indian Bend Wash at Shea Boulevard exceeded alarm stage, resulting in impacts to downstream low water crossings as well as to the Indian Bend Wash greenbelt. At 1501MST, flow in Indian Bend Wash crested at 3.02 feet and 2031 CFS. According to a nearby mPING report close to Paradise Valley Mall, a flooded street led to a vehicle becoming stranded. No injuries were reported.", "ts_dict_index": [2229, 2230, 2231]}
+{"event_id": 983962, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 11:00:00", "end_date_time": "2021-08-18 14:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Multiple photos and videos show significant flow in Pinto and Spring (tributary to Pinto) along State Route 188 near mile post 234. One photo showed a storage structure (possibly abandoned) in Spring Creek with roughly 8 feet of water flowing through it. It is unknown if the structure had any damage. Many of the photos and videos were posted in the early afternoon, but flood impacts likely began in the morning after 2 to 4 inches of rain fell over the 2019 Woodbury burn area. No injuries were reported.", "ts_dict_index": [2235, 2236, 2237]}
+{"event_id": 983904, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 08:10:00", "end_date_time": "2021-08-18 12:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Dirt road up to Reevis Mountain School, which cuts through Campaign Creek, was washed out by significant flash flooding. A couple yurpees on the property of the school were damaged or destroyed. Their fire circle and labyrinth were also washed away. The school and road are inside the 2019 Woodbury burn area. Rainfall of 4.5 inches was measured in 3 to 4 hours. Timing based on radar. No injuries were reported.", "ts_dict_index": [2238, 2239, 2240]}
+{"event_id": 983968, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 16:30:00", "end_date_time": "2021-08-18 19:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Gila County Emergency Manager reported Russell Gulch experienced flash flooding, in the Claypool area between Miami and Globe, after heavy rain fell over the Pinal Mountains within the 2021 Telegraph Fire burn area. Measured and radar estimated rainfall amounts were around 1 to 2 inches over the area and upstream, bringing the day's total to around 2.5 to 4.5 inches over the burn scar. Flash flooding impacted the same areas as the catastrophic flooding earlier in the morning, but was less intense according to the emergency manager. Still the bridge to the hospital near Hospital Road and Russell Road was impassable and nearby homes likely experienced impacts again. No injuries were reported and there were no reports of new damage costs.", "ts_dict_index": [2253, 2254, 2255]}
+{"event_id": 983967, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 15:25:00", "end_date_time": "2021-08-18 17:00:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Arizona Department of Transportation closed State Route 188 in both directions due to a mudslide across the highway. Initially the closure was between mile posts 246 and 255, but was updated to between 252 and 255. The mudslide was around mile post 253 and was the same location as a debris flow in July 2020. Runoff may have been enhanced by the 2020 Bush Fire burn area. Photos of the mud slide show roughly 1 to 3 feet of sediment, with burnt tree branches and twigs, across the highway and the guardrail in the southbound lane was destroyed. No injuries or additional damages were reported.", "ts_dict_index": [2259, 2260, 2261]}
+{"event_id": 984315, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 16:05:00", "end_date_time": "2021-08-18 19:42:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. A Maricopa County Flood Control District stream gage along Cave Creek at Cactus Road recorded flow climbing above alarm stage, impacting nearby low-lying areas. At 1632MST, the gage crested at 11.14 feet and 1,567 CFS. No damage or injuries were reported.", "ts_dict_index": [2247, 2248, 2249]}
+{"event_id": 983969, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-18 18:10:00", "end_date_time": "2021-08-18 21:10:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Arizona Department of Transportation reported State Route 238 was closed for several hours between mile posts 35 and 40 due to flooding. Timing of impacts based on radar. No damages or injuries were reported.", "ts_dict_index": [2256, 2257, 2258]}
+{"event_id": 984002, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 12:47:00", "end_date_time": "2021-08-18 13:10:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Heavy rainfall led to a rapid increase in flow in Sycamore Creek. A Maricopa County Flood Control District stream gage along Sycamore Creek near NF-201 and Beeline Highway recorded the creek climbing above alarm stage, cresting at 4.54 feet at 1247MST. Downstream impacts included old SR 87 and low-lying homes. No damage or injuries were reported.", "ts_dict_index": [2244, 2245, 2246]}
+{"event_id": 984028, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 13:40:00", "end_date_time": "2021-08-18 15:45:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. The Cave Creek Ashdale Maricopa County Flood Control District stream gage recorded flow exceeding alarm stage, impacting low water crossings along with properties in the area. At 1513MST, the creek crested at 6.7 feet and 2027 CFS. No damage or injuries were reported.", "ts_dict_index": [2196, 2197, 2198]}
+{"event_id": 947004, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-30 03:30:00", "end_date_time": "2021-04-30 06:15:00", "narrative": "A cluster of showers and thunderstorms developed during the late evening hours of April 29th over Deep East Texas, near and just south of a weak cold front that drifted south across East Texas and North-Central Louisiana. These storms developed in a very moist air mass, near an inverted low level trough that extended from Deep East Texas into West-Central Louisiana. Additional forcing aloft was provided by increasing large scale forcing ahead of a closed upper low over Northern Mexico, which resulted in additional redevelopment of these storms containing heavy rainfall, moving repeatedly over the same areas through much of the early morning hours on the 30th. Widespread rainfall amounts of 3-6+ inches fell across Southern Cherokee, Nacogdoches, Angelina, and San Augustine Counties, which resulted in widespread flash flooding across the areas, with numerous roads closed. These storms diminished by the mid and late morning hours on the 30th. Water covered Highway 21 at County Road 508.", "ts_dict_index": [2292, 2293, 2294]}
+{"event_id": 819095, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "LAFAYETTE", "begin_date_time": "2019-05-08 14:55:00", "end_date_time": "2019-05-08 17:45:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Locally heavy rainfall from the stronger storms within a short period of time also resulted in localized flash flooding across portions of Southwest Arkansas. Numerous roads in and near Lewisville were flooded. Several school buses were forced to turn around away from these flooded roads.", "ts_dict_index": [2289, 2290, 2291]}
+{"event_id": 983942, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 16:20:00", "end_date_time": "2021-08-18 18:00:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Video shows significant flow in Six Shooter Canyon with floodwaters overtopping a small bridge at Six Shooter Canyon Road and Delores Lane. Homes may have been impacted with this flow level, considering a previous event, but there were no reports of damages and no reports of injuries either. It is uncertain if this event occurred in the morning or afternoon, but a downstream gage at Beer Tree Crossing registered a greater rise in the afternoon versus the morning. The gage crested at 3.91 feet at 1659MST. Although not reported, Beer Tree Crossing was likely impassable.", "ts_dict_index": [2268, 2269, 2270]}
+{"event_id": 983850, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 08:20:00", "end_date_time": "2021-08-18 10:20:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Multiple photos and videos show significant flow within the typically dry Reno Creek with flow over Old Highway 188, leading to its closure. Runoff may have been enhanced by the 2020 Bush Fire burn area. Reno Creek would experience another flash flood again in the early afternoon following another round of heavy rain upstream. This kept 188 closed for an extended period. No damages or injuries were reported.", "ts_dict_index": [2274, 2275, 2276]}
+{"event_id": 984209, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 16:00:00", "end_date_time": "2021-08-18 17:50:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. A photo showed an outhouse public bathroom at the Eads Wash River Access Point Recreation site had the ground beneath it eroded away due to flash flooding. Floodwaters appeared to be traveling within Poison Spring Wash toward the Salt River. Tonto National Forest posted a couple days later that access to the Eads Wash rec site was closed due to erosion damage and unsafe conditions in the area as a result of the flash flooding. Exact timing of when impacts occurred is unknown, so based the timing off of radar. No injuries were reported.", "ts_dict_index": [2280, 2281, 2282]}
+{"event_id": 984004, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 14:00:00", "end_date_time": "2021-08-18 15:00:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Old Stage Road and parts of New River Road were closed due to flooding associated with increased flow in New River. A Maricopa County Flood Control District upstream from the impacts climbed above alarm stage, cresting at 2.93 feet and 2801 CFS at 1442MST. No damage or injuries were reported.", "ts_dict_index": [2262, 2263, 2264]}
+{"event_id": 984215, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 14:10:00", "end_date_time": "2021-08-18 17:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Videos show significant floodwaters in Galloway Wash with flow across Spur Cross Road, making the road impassable to all traffic. Measured and radar estimated rainfall amounts were around 2 to 4 inches in 2 to 3 hours over areas upstream of this location. Timing adjusted based on radar. No damages or injuries were reported.", "ts_dict_index": [2283, 2284, 2285]}
+{"event_id": 983905, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 09:40:00", "end_date_time": "2021-08-18 12:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Video shows considerable flow through Pinal Creek with at least 6 inches of swift-moving water over Beer Tree Crossing near Jess Hayes Road. Rainfall of 1.5 to 2 inches was measured in the area and upstream. Runoff may have been enhanced by the 2021 Telegraph burn area. No damages or injuries were reported.", "ts_dict_index": [2286, 2287, 2288]}
+{"event_id": 983944, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 11:05:00", "end_date_time": "2021-08-18 12:35:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Arizona Department of Transportation reported State Route 77 was overtopped by floodwaters at mile post 163.2. Timing based on report time and radar. No damages or injuries were reported.", "ts_dict_index": [2271, 2272, 2273]}
+{"event_id": 983936, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 13:45:00", "end_date_time": "2021-08-18 15:45:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. According to local media reports, the Maricopa County Sheriff's Office found two people had perished inside an ATV that was buried in mud and debris downstream in Camp Creek. MCSO was notified and began searching for the missing people around 1600MST on the 18th but did not recover the ATV until 0800MST on the 19th. Media reported that other recreationists were successfully rescued from the area, including a father and daughter who were trapped near Needle Rock Recreation Site and had to be rescued by helicopter. A Camp Creek rain gauge recorded 3.54 inches of rain between 1300MST and 1420MST. The Rackensack Canyon rain gauge measured 3.83 inches of rain between 1250MST and 1430MST. The Maricopa County Flood Control District also reported that Bartlett Dam Road was closed due to swiftly flowing water over the roadway from Camp Creek.", "ts_dict_index": [2277, 2278, 2279]}
+{"event_id": 984030, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 14:18:00", "end_date_time": "2021-08-18 15:30:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. A Maricopa County Flood Control District stream gage along Seven Springs Wash exceeded alarm stage, impacting the unbridged Seven Springs Road downstream. At 1418MST, the flow crested at 5.06 feet and 1574 CFS.", "ts_dict_index": [2211, 2212, 2213]}
+{"event_id": 947002, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-30 03:30:00", "end_date_time": "2021-04-30 06:15:00", "narrative": "A cluster of showers and thunderstorms developed during the late evening hours of April 29th over Deep East Texas, near and just south of a weak cold front that drifted south across East Texas and North-Central Louisiana. These storms developed in a very moist air mass, near an inverted low level trough that extended from Deep East Texas into West-Central Louisiana. Additional forcing aloft was provided by increasing large scale forcing ahead of a closed upper low over Northern Mexico, which resulted in additional redevelopment of these storms containing heavy rainfall, moving repeatedly over the same areas through much of the early morning hours on the 30th. Widespread rainfall amounts of 3-6+ inches fell across Southern Cherokee, Nacogdoches, Angelina, and San Augustine Counties, which resulted in widespread flash flooding across the areas, with numerous roads closed. These storms diminished by the mid and late morning hours on the 30th. Water covered the road along County Road 715 at FM 225.", "ts_dict_index": [2298, 2299, 2300]}
+{"event_id": 974535, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-07-09 21:50:00", "end_date_time": "2021-07-09 22:50:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. Heavy rainfall combined with enhanced runoff from the recent Telegraph burn scar led to flooding across Ice House Canyon road in Ice House Canyon. Images from Forest Service officials showed a considerable amount of debris on the banks of the wash with some debris covering the surface of the road. No injuries or damage were reported.", "ts_dict_index": [2295, 2296, 2297]}
+{"event_id": 983931, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 10:45:00", "end_date_time": "2021-08-18 13:00:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. After 2 to 4 inches of rain fell, beginning around 0830MST, over the 2021 Telegraph burn area, catastrophic flooding occurred in Claypool area between Miami and Globe. Runoff mostly collected in Russell Gulch and a few feet of floodwaters moved downhill through the Claypool community. Security cam footage from a pizza shop showed floodwaters reached US-60 near mile post 247 around 1056MST. US-60 became impassible a couple minutes later and was closed in both directions for a couple hours before being reopened around 1240MST. The same areas were impacted again in the mid-afternoon after another wave of flash flooding move through the area. The Gila County Emergency Manager estimated over 50 homes and structures were damaged by flooding. Included in the damage was the pizza shop with the security footage, which was fully surrounded by flooding. A hotel next to the pizza shop had all of its ground level rooms flooded, including a wall that collapsed due to the force of the water. Roads to the nearby hospital were cutoff by floodwaters. The hardest hit area was Little Acres Mobile Home Park, 1 mile south of US-60. Most if not all of the mobile homes had flood damage as an estimated 4 feet of water and mud moved through the park. Security footage shows one home was even swept from one side of the park to the other and was destroyed. Many of the owners were displaced from their homes for several days while the park was cleaned. A power substation next to the park also experienced significant flooding. Fortunately there were no injuries or fatalities reported from this event.", "ts_dict_index": [2232, 2233, 2234]}
+{"event_id": 866214, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2019-11-28 10:00:00", "end_date_time": "2019-11-28 16:00:00", "narrative": "A cold unstable upper level low pressure system from the northwest brought widespread heavy rain, thunderstorms and mountain snow to southern California over the Thanksgiving holiday. One to three feet of snow fell above 5,500 feet in the mountains, impacting highways and passes. Big Bear and Mountain High reported 30 to 48 inches total. Highway 18 was closed through December 1st. Over 40 vehicles were stuck on Highway 74 and 371, while 20 vehicles were abandoned on Highway 38. There were 10 car accidents involving snow plows. Heavy rainfall of 1 to 3 inches fell at the coast and in the valleys. San Diego River reached 9.5 feet with flooding. Numerous roadways were flooded out, especially on November 28th when the heaviest rain fell. An RV park in La Mesa flooded out due to flash flooding. The San Diego River at Fashion Valley reached 9.5 feet. 2 separate episodes of severe thunderstorms occurred in San Diego County on Thanksgiving Day. A sinkhole opened up on the shoulder of I-10 in Redlands due to heavy rain. Total cost to repair the large sinkhole was $760,000.", "ts_dict_index": [2313, 2314, 2315]}
+{"event_id": 947003, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-30 03:30:00", "end_date_time": "2021-04-30 06:15:00", "narrative": "A cluster of showers and thunderstorms developed during the late evening hours of April 29th over Deep East Texas, near and just south of a weak cold front that drifted south across East Texas and North-Central Louisiana. These storms developed in a very moist air mass, near an inverted low level trough that extended from Deep East Texas into West-Central Louisiana. Additional forcing aloft was provided by increasing large scale forcing ahead of a closed upper low over Northern Mexico, which resulted in additional redevelopment of these storms containing heavy rainfall, moving repeatedly over the same areas through much of the early morning hours on the 30th. Widespread rainfall amounts of 3-6+ inches fell across Southern Cherokee, Nacogdoches, Angelina, and San Augustine Counties, which resulted in widespread flash flooding across the areas, with numerous roads closed. These storms diminished by the mid and late morning hours on the 30th. Water covered both lanes of Highway 7 at the intersection of FM 2782.", "ts_dict_index": [2307, 2308, 2309]}
+{"event_id": 947006, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-30 03:45:00", "end_date_time": "2021-04-30 06:15:00", "narrative": "A cluster of showers and thunderstorms developed during the late evening hours of April 29th over Deep East Texas, near and just south of a weak cold front that drifted south across East Texas and North-Central Louisiana. These storms developed in a very moist air mass, near an inverted low level trough that extended from Deep East Texas into West-Central Louisiana. Additional forcing aloft was provided by increasing large scale forcing ahead of a closed upper low over Northern Mexico, which resulted in additional redevelopment of these storms containing heavy rainfall, moving repeatedly over the same areas through much of the early morning hours on the 30th. Widespread rainfall amounts of 3-6+ inches fell across Southern Cherokee, Nacogdoches, Angelina, and San Augustine Counties, which resulted in widespread flash flooding across the areas, with numerous roads closed. These storms diminished by the mid and late morning hours on the 30th. FM 95 was flooded in the Polly Branch community.", "ts_dict_index": [2310, 2311, 2312]}
+{"event_id": 974902, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 02:30:00", "end_date_time": "2021-07-10 03:30:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. Thunderstorms produced locally heavy rainfall late in the evening on the 9th near midnight across southern portions of Maricopa County and western portions of Pinal County. According to the Arizona Department of Transportation, the flood prone Highway 238 was closed due to flooding. No injuries or damage was reported as a result of the flooding.", "ts_dict_index": [2304, 2305, 2306]}
+{"event_id": 983970, "event_type": "Flash Flood", "state": "ARIZONA", "cz_name": "GILA", "begin_date_time": "2021-08-18 13:00:00", "end_date_time": "2021-08-18 19:00:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Photos and videos show considerable floodwaters, roughly a few feet deep, rapidly moving down Reno Creek and flowing across Old Highway 188, making it impassable. Runoff may have been enhanced by the 2020 Bush Fire burn area. Reno Creek flooded earlier in the morning as well. No damages or injuries were reported.", "ts_dict_index": [2265, 2266, 2267]}
+{"event_id": 1057987, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2022-08-24 16:20:00", "end_date_time": "2022-08-24 20:30:00", "narrative": "A very moist (PWATs 2.0+ inches) and unstable (MLCAPE 2000-3000 J/KG) air mass led to a very conducive environment for vigorous thunderstorm activity across portions of southeast California. Thunderstorms first developed across the higher terrain near Joshua Tree National Park as well as across the mountains of Northern Baja California. With the upper-level flow from the west, these thunderstorms moved eastward into Imperial and Riverside counties, moving into the very moist and unstable air mass. Radar estimated rainfall amounts were upwards of 2-3 inches in some areas, with most of the rain falling in less than 2 hours. There were several incidences of flash flooding and wind impacts around the region. The biggest impact of the day was a washout of a section of eastbound lanes along Interstate-10, which is a major throughway for ground traffic between Phoenix, AZ and Los Angeles, CA. This caused major traffic delays and detours. Caltrans closed SR-177 in both directions between I-10 and SR-62 due to flooding in multiple locations. Power lines were also down along SR-177. SR-177 was reopened around 0800PST, August 25th. Timing of flooding impacts based on radar. No injuries were reported.", "ts_dict_index": [2325, 2326, 2327]}
+{"event_id": 1054030, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2022-08-24 18:55:00", "end_date_time": "2022-08-24 19:55:00", "narrative": "A very moist (PWATs 2.0+ inches) and unstable (MLCAPE 2000-3000 J/KG) air mass led to a very conducive environment for vigorous thunderstorm activity across portions of southeast California. Thunderstorms first developed across the higher terrain near Joshua Tree National Park as well as across the mountains of Northern Baja California. With the upper-level flow from the west, these thunderstorms moved eastward into Imperial and Riverside counties, moving into the very moist and unstable air mass. Radar estimated rainfall amounts were upwards of 2-3 inches in some areas, with most of the rain falling in less than 2 hours. There were several incidences of flash flooding and wind impacts around the region. The biggest impact of the day was a washout of a section of eastbound lanes along Interstate-10, which is a major throughway for ground traffic between Phoenix, AZ and Los Angeles, CA. This caused major traffic delays and detours. Clatrans closed SR-78 in both directions near the I-10 interchange due to flooding. SR-78 was reopened around 0800PST, August 25th. Timing of flooding impacts estimated from radar. No damages or injuries were reported.", "ts_dict_index": [2322, 2323, 2324]}
+{"event_id": 865923, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-11-01 14:05:00", "end_date_time": "2019-11-02 16:17:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. The Hudson River at Fort Edward rose above moderate flood stage at 1405EST 1 November, crested at 27.96 feet at 2215EST 1 November, and fell below moderate flood stage by 1617EST 2 November. Water was over the road at Rogers Island Drive and surrounded a private club on the southern tip of the island.", "ts_dict_index": [2358, 2359, 2360]}
+{"event_id": 1054033, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "IMPERIAL", "begin_date_time": "2022-08-24 15:30:00", "end_date_time": "2022-08-24 17:30:00", "narrative": "A very moist (PWATs 2.0+ inches) and unstable (MLCAPE 2000-3000 J/KG) air mass led to a very conducive environment for vigorous thunderstorm activity across portions of southeast California. Thunderstorms first developed across the higher terrain near Joshua Tree National Park as well as across the mountains of Northern Baja California. With the upper-level flow from the west, these thunderstorms moved eastward into Imperial and Riverside counties, moving into the very moist and unstable air mass. Radar estimated rainfall amounts were upwards of 2-3 inches in some areas, with most of the rain falling in less than 2 hours. There were several incidences of flash flooding and wind impacts around the region. The biggest impact of the day was a washout of a section of eastbound lanes along Interstate-10, which is a major throughway for ground traffic between Phoenix, AZ and Los Angeles, CA. This caused major traffic delays and detours. S22(Borrego-Salton roadway) was closed due to flooding. Timing estimated from radar. No damages or injuries were reported.", "ts_dict_index": [2328, 2329, 2330]}
+{"event_id": 1054023, "event_type": "Flash Flood", "state": "CALIFORNIA", "cz_name": "RIVERSIDE", "begin_date_time": "2022-08-24 17:35:00", "end_date_time": "2022-08-24 20:30:00", "narrative": "A very moist (PWATs 2.0+ inches) and unstable (MLCAPE 2000-3000 J/KG) air mass led to a very conducive environment for vigorous thunderstorm activity across portions of southeast California. Thunderstorms first developed across the higher terrain near Joshua Tree National Park as well as across the mountains of Northern Baja California. With the upper-level flow from the west, these thunderstorms moved eastward into Imperial and Riverside counties, moving into the very moist and unstable air mass. Radar estimated rainfall amounts were upwards of 2-3 inches in some areas, with most of the rain falling in less than 2 hours. There were several incidences of flash flooding and wind impacts around the region. The biggest impact of the day was a washout of a section of eastbound lanes along Interstate-10, which is a major throughway for ground traffic between Phoenix, AZ and Los Angeles, CA. This caused major traffic delays and detours. Interstate-10, a major throughway between Phoenix, AZ and Southern California, had a section of the two eastbound (EB) lanes fully washed out due to flash flooding. Video during the washout appear to show the drainage pipes under the road were overcome and compromised by the magnitude of floodwaters. Radar rainfall estimates in this area were around 2-3 inches, with much of the rain falling in less than 2 hours. The washout occurred a few miles east of State Route 177/Desert Center. Caltrans closed I-10 EB due to the washout. I-10 westbound (WB) was also closed briefly due to an overturned semi-truck and SR-177 had already been closed, due to its own separate flooding impacts and downed power lines, by the time of the I-10 washout. This caused major traffic delays and detours through Eastern Riverside County. One EB detour lane was opened around 0700PST on August 25th after emergency construction and the second EB detour lane was not opened until 2300PST August 27th. Timing of flooding impacts based on radar. No injuries were reported from this event.", "ts_dict_index": [2316, 2317, 2318]}
+{"event_id": 1049442, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2022-07-28 05:00:00", "end_date_time": "2022-07-30 12:00:00", "narrative": "Between July 25th and July 30th, 2022, several complexes of training thunderstorms developed south of I-64 and brought heavy rain, deadly flash flooding, and devastating river flooding to eastern Kentucky and central Appalachia. These thunderstorms, at times, caused rainfall rates in excess of 4/hr across complex terrain that led to widespread devastating impacts. While it did not rain continuously during this 4-day stretch, the overwhelming amounts of rain and resultant flooding led to 39 deaths and widespread catastrophic damage. Entire homes and parts of some communities were swept away by flood waters, leading to costly damage to infrastructure in the region. Over 600 helicopter rescues and countless swift water rescues by boat were needed to evacuate people who were trapped by the quickly-rising flood waters. In total, 24 Flash Flood Warnings were issued between July 26th and July 30th. Between the evening of July 27th and the mid-morning hours on July 28th (the peak of the event), 13 warnings were issued, 3 of which were upgraded to a Flash Flood Emergency.||Radar-based rainfall estimates suggest that upwards of 14-16 of rain fell during this 5-day period in a narrow swath, with many more locations receiving 6-10 of rain. Most of this rain fell during the night of July 27th into the morning of July 28th, which is when the most devastating impacts were felt. The highest totals occurred across an axis that stretches from northern Clay and southern Owsley counties, east through southern Breathitt and northern Leslie counties, into Perry, Knott and Letcher counties. The highest rainfall total report was from southern Knott County, where 14.00 fell between July 25th and July 29th. This site, a cooperative (COOP) observer at Carr Creek Lake, reported 6.71 from 7am July 28th to 7am July 29th, following a report of 6.50 at that site on the previous day. Another COOP site in Buckhorn reported 8.00 of rain for the 24-hour period ending 7am on July 28th. The rainfall total in Buckhorn from July 25th to July 29th was 11.76. These rainfall values occurring in such a short period of time are incredibly rare: there is less than a 1 in 1000 chance for this much rainfall over five days in a given year.||The incredible rainfall also led to significant rises and flooding on many rivers in eastern Kentucky including on the main stem of the Kentucky River; North, Middle and South forks of the Kentucky River; Red River and Licking River. At Whitesburg, the North Fork of the Kentucky River swelled well above major flood stage, reaching close to 21' before gauge failure (the previous flood of record was 14.7' in 1957). The North Fork of the Kentucky River at Jackson also reached major flood, setting a new record crest of 43.47' (the previous record was 43.1' set in 1939). The river flooding caused a second round of destruction for communities in the region, and caused flooding in downstream areas that did not receive as much rainfall.||*Note* Given the widespread nature and severity of this event - any dollar amount estimated by storm data will not do the event as a whole justice. Since eastern KY was a national declaration, FEMA will be doing a full cost assessment. Will use this data once available for total monetary amounts of damage.||Visit www.weather.gov/jkl/July2022Flooding for more information on the event, as well as pictures and videos of the flooding and damage. Flash flooding across Breathitt County then led to areal flooding, and record flooding of the North Fork Kentucky River at Jackson. Before the flooding, the North Fork was about 10 feet. Within a few hours, at 5 AM EST on July 28, it reached minor flood stage of 29 feet. It then went on to crest at a record 43.47 feet at 1:30 AM EST July 29th. It fell below flood stage later that day around noon EST. ||Some other flood reports that were received across the county during this time include: ||08:53 AM EST - Kiwanis Park in Jackson was inundated by the North Fork Kentucky River.|09:16 AM EST - A church and a home at the intersection of Joe Little Fork and KY-3237 in Canoe was inundated by flood waters from Joe Little and Canoe Creeks. |10:00 AM EST - A picture shows Old Caney School surrounded by Troublesome Creek flood waters up to the second story near the community of Hardshell.|10:19 AM EST - Douthitt Park ball field is inundated with several feet of water from the North Fork Kentucky River. |10:26 AM EST - Lost Creek Evangelical Free Church along KY-476 is inundated by Troublesome Creek to within a couple feet of the roof. |11:21 AM EST - The intersection of KY-397 and KY-1110 is inundated by the North Fork Kentucky River near the Howard Creek community. |11:40 AM EST - Homes along KY-476 near the intersection with KY-15 are inundated half way up the first story by Troublesome Creek. |12:26 PM EST - Homes in the Lost Creek Community, as well as the Riverside School campus, are inundated by flood waters from Troublesome and Lost Creeks. |1:00 PM EST - A picture shows Canoe Road inundated by the Middle Fork of the Kentucky River in the Canoe community. |2:00 PM EST - Pictures show the electric substation at the intersection of KY-397 and KY-1110 inundated by the North Fork Kentucky River. |2:26 PM EST - KY-1098 in Quicksand is submerged at the intersection of KY-15 from Quicksand Creek flood waters.|2:28 PM EST - Video footage shows South Jackson inundated by the North Fork Kentucky River.|4:00 PM EST - The North Fork KEntucky River began to inundate Slones Trailer Park in Jackson. |4:11 PM EST - A horse barn is submerged to it's roof at Wolverine by the North Fork Kentucky River. |7:10 AM EST (7/29) - Pictures show widespread inundation in downtown Jackson at the intersection of Broadway and Hawk Street.|8:11 AM EST - Pictures on social media show flood waters surrounding the Elkatawa Free Methodist Church. KY-52 is also inundated.  |9:25 AM EST - Jackson Save-A-Lot and Tractor Supply Co. were inundated by the North Fork Kentucky River. |9:47 AM EST - Pictures show the North Fork Kentucky River inundating Slones Trailer Park up to the windows of a car. ||Multiple other creeks and streams that fed into the North Fork Kentucky River also experienced extensive flooding.", "ts_dict_index": [2334, 2335, 2336]}
+{"event_id": 800214, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2019-02-23 23:45:00", "end_date_time": "2019-02-24 11:30:00", "narrative": "Periods of rain worked back into eastern Kentucky early on February 20 as a warm frontal boundary lifted north across the Commonwealth. A cold front brought additional rainfall through the afternoon and evening, before drier conditions worked into eastern Kentucky during the morning of February 21. ||Rain quickly spread back north that evening into the 22nd with southeastern Kentucky continuing to see prolonged light rain into the afternoon of the 23rd. A cold front brought additional rain to much of eastern Kentucky late on the 23rd. ||A spike in moisture ahead of this front resulted in additional moderate to heavy rain and high rainfall rates across portions of eastern Kentucky late on the 23rd. The convection ahead of the cold front that evening resulted in the majority of the flooding and flash flooding issues across eastern Kentucky. Showers and thunderstorms capable of heavy rainfall trained over parts of Wayne, Pulaski, Rockcastle, and other counties along the I-75 corridor, resulting in deadly flash flooding and river flooding along the Cumberland River. Later in the evening, the bulk of the rainfall shifted north to counties along the Mountain Parkway. Flash flooding and river flooding occurred in Powell, Wolfe, Breathitt, Magoffin, and Johnson Counties. Lighter rainfall continued into the night as flooding issues remained widespread into the 24th.||Rainfall amounts from this event ranged from near 2 inches in portions of the Bluegrass region and northeast Kentucky, to greater than 4 inches across locations in southern and southeast Kentucky. ||This additional water on top of saturated ground continued to promote mud and rock slides across eastern Kentucky, complete with power outages from fallen debris and trees. Pikeville experienced a massive rockslide early on February 22, resulting in several cars and a building being damaged. Other impacts included countless roads being inundated with standing water, pavement and water pipes breaking, water threatening homes, roads and bridges being washed away, and rising lake levels.||Of the 33 counties across eastern Kentucky, at least 27 were forced to declare State of Emergencies due to rainfall during and before this event. This included Knott County due to over $150,000 in county road damages. Beattyville, Clay City, Harlan, Hazard, Jenkins, Monticello, Paintsville, Pikeville, Salyersville, Stanton, West Liberty, and Whitesburg also declared State of Emergencies. Additionally, the Kentucky Governor declared a State of Emergency across the entire Commonwealth.||The persistent rainfall of the winter season and the amount of rainfall from this event led to Lake Cumberland reporting their highest lake level of 756.52 feet on February 26th, breaking the old record of 751.69 feet dating back to May 1984. As a result, Wolf Creek Dam had to release at a record discharge level of 59,880 cubic feet per second. Cave Run Lake also rose to within 6 feet of their record pool elevation. Buckhorn Lake came within 10 feet of their all-time record, partially resulting in Kentucky Highway 257 near Confluence having flood waters cover the highway isolating 40 to 50 families for three weeks following the end of the flooding rains. A National Weather Service employee reported Kentucky Highway 541 at Kentucky Mountain Bible College being inundated by water from the North Fork of the Kentucky River. Portions of Kentucky Highway 205 also remained flooded overnight.", "ts_dict_index": [2340, 2341, 2342]}
+{"event_id": 839214, "event_type": "Flash Flood", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-07-10 17:34:00", "end_date_time": "2019-07-10 20:34:00", "narrative": "On the 8th, a deluge in Pine Bluff (Jefferson County) resulted in three to five inches of precipitation in parts of the city (with two inches of this in about 30 minutes). Many roads flooded, and so did a municipal building. This affected local police and fire departments.||It stayed hot during this time frame, with Heat Advisories posted by the National Weather Service. On the 9th, for example, heat indices approached 110 degrees in parts of the south/east.||It stayed hot during this time frame, with Heat Advisories posted by the National Weather Service. On the 9th, for example, heat indices approached 110 degrees in parts of the south/east.||As the tropical system formed, thunderstorms came to life ahead of the aforementioned cold front. The storms made the most impact in western Arkansas, with wind damage in several places. Trees were toppled at Waldron (Scott County), Mount Ida (Montgomery County), and Big Fork (Polk County). Water was reported on Cherry Hill Drive and Cypress Street. Debris was floating down the road.", "ts_dict_index": [2319, 2320, 2321]}
+{"event_id": 859159, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-10-31 23:36:00", "end_date_time": "2019-10-31 23:59:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. Showers across the southern Adirondacks and Mohawk Valley became steadier and heavier during the evening ahead of a strong cold front as the low continued to strengthen. Strong winds aloft mixed down to the surface as an intense line of showers developed along the front, resulting in sporadic wind damage and scattered power outages over eastern New York.||A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope.  Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam.  Although river rises and some impacts occurred prior to midnight, the crests occurred on 1 November, and impacts persisted into the first week of November in some areas (see also November StormData). The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed. There was one fatality as a result of the flooding as a man was swept away by flood waters when he exited his vehicle. ||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage. ||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 5S was closed due to flooding at Sandy Lane.", "ts_dict_index": [2355, 2356, 2357]}
+{"event_id": 797970, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2019-02-20 12:10:00", "end_date_time": "2019-02-20 15:50:00", "narrative": "Periods of rain worked back into eastern Kentucky early on February 20 as a warm frontal boundary lifted north across the Commonwealth. A cold front brought additional rainfall through the afternoon and evening, before drier conditions worked into eastern Kentucky during the morning of February 21. ||Rain quickly spread back north that evening into the 22nd with southeastern Kentucky continuing to see prolonged light rain into the afternoon of the 23rd. A cold front brought additional rain to much of eastern Kentucky late on the 23rd. ||A spike in moisture ahead of this front resulted in additional moderate to heavy rain and high rainfall rates across portions of eastern Kentucky late on the 23rd. The convection ahead of the cold front that evening resulted in the majority of the flooding and flash flooding issues across eastern Kentucky. Showers and thunderstorms capable of heavy rainfall trained over parts of Wayne, Pulaski, Rockcastle, and other counties along the I-75 corridor, resulting in deadly flash flooding and river flooding along the Cumberland River. Later in the evening, the bulk of the rainfall shifted north to counties along the Mountain Parkway. Flash flooding and river flooding occurred in Powell, Wolfe, Breathitt, Magoffin, and Johnson Counties. Lighter rainfall continued into the night as flooding issues remained widespread into the 24th.||Rainfall amounts from this event ranged from near 2 inches in portions of the Bluegrass region and northeast Kentucky, to greater than 4 inches across locations in southern and southeast Kentucky. ||This additional water on top of saturated ground continued to promote mud and rock slides across eastern Kentucky, complete with power outages from fallen debris and trees. Pikeville experienced a massive rockslide early on February 22, resulting in several cars and a building being damaged. Other impacts included countless roads being inundated with standing water, pavement and water pipes breaking, water threatening homes, roads and bridges being washed away, and rising lake levels.||Of the 33 counties across eastern Kentucky, at least 27 were forced to declare State of Emergencies due to rainfall during and before this event. This included Knott County due to over $150,000 in county road damages. Beattyville, Clay City, Harlan, Hazard, Jenkins, Monticello, Paintsville, Pikeville, Salyersville, Stanton, West Liberty, and Whitesburg also declared State of Emergencies. Additionally, the Kentucky Governor declared a State of Emergency across the entire Commonwealth.||The persistent rainfall of the winter season and the amount of rainfall from this event led to Lake Cumberland reporting their highest lake level of 756.52 feet on February 26th, breaking the old record of 751.69 feet dating back to May 1984. As a result, Wolf Creek Dam had to release at a record discharge level of 59,880 cubic feet per second. Cave Run Lake also rose to within 6 feet of their record pool elevation. Buckhorn Lake came within 10 feet of their all-time record, partially resulting in Kentucky Highway 257 near Confluence having flood waters cover the highway isolating 40 to 50 families for three weeks following the end of the flooding rains. A citizen relayed a report of water over Smith Branch Road southeast of Jackson.", "ts_dict_index": [2343, 2344, 2345]}
+{"event_id": 864314, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 00:00:00", "end_date_time": "2019-11-01 07:56:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 5 was closed due to flooding between Windfall Road and Drive-In Road.", "ts_dict_index": [2361, 2362, 2363]}
+{"event_id": 797884, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2019-02-20 17:25:00", "end_date_time": "2019-02-20 18:55:00", "narrative": "Periods of rain worked back into eastern Kentucky early on February 20 as a warm frontal boundary lifted north across the Commonwealth. A cold front brought additional rainfall through the afternoon and evening, before drier conditions worked into eastern Kentucky during the morning of February 21. ||Rain quickly spread back north that evening into the 22nd with southeastern Kentucky continuing to see prolonged light rain into the afternoon of the 23rd. A cold front brought additional rain to much of eastern Kentucky late on the 23rd. ||A spike in moisture ahead of this front resulted in additional moderate to heavy rain and high rainfall rates across portions of eastern Kentucky late on the 23rd. The convection ahead of the cold front that evening resulted in the majority of the flooding and flash flooding issues across eastern Kentucky. Showers and thunderstorms capable of heavy rainfall trained over parts of Wayne, Pulaski, Rockcastle, and other counties along the I-75 corridor, resulting in deadly flash flooding and river flooding along the Cumberland River. Later in the evening, the bulk of the rainfall shifted north to counties along the Mountain Parkway. Flash flooding and river flooding occurred in Powell, Wolfe, Breathitt, Magoffin, and Johnson Counties. Lighter rainfall continued into the night as flooding issues remained widespread into the 24th.||Rainfall amounts from this event ranged from near 2 inches in portions of the Bluegrass region and northeast Kentucky, to greater than 4 inches across locations in southern and southeast Kentucky. ||This additional water on top of saturated ground continued to promote mud and rock slides across eastern Kentucky, complete with power outages from fallen debris and trees. Pikeville experienced a massive rockslide early on February 22, resulting in several cars and a building being damaged. Other impacts included countless roads being inundated with standing water, pavement and water pipes breaking, water threatening homes, roads and bridges being washed away, and rising lake levels.||Of the 33 counties across eastern Kentucky, at least 27 were forced to declare State of Emergencies due to rainfall during and before this event. This included Knott County due to over $150,000 in county road damages. Beattyville, Clay City, Harlan, Hazard, Jenkins, Monticello, Paintsville, Pikeville, Salyersville, Stanton, West Liberty, and Whitesburg also declared State of Emergencies. Additionally, the Kentucky Governor declared a State of Emergency across the entire Commonwealth.||The persistent rainfall of the winter season and the amount of rainfall from this event led to Lake Cumberland reporting their highest lake level of 756.52 feet on February 26th, breaking the old record of 751.69 feet dating back to May 1984. As a result, Wolf Creek Dam had to release at a record discharge level of 59,880 cubic feet per second. Cave Run Lake also rose to within 6 feet of their record pool elevation. Buckhorn Lake came within 10 feet of their all-time record, partially resulting in Kentucky Highway 257 near Confluence having flood waters cover the highway isolating 40 to 50 families for three weeks following the end of the flooding rains. A trained spotter observed water covering Kentucky Highway 1427 east of Bonanza.", "ts_dict_index": [2346, 2347, 2348]}
+{"event_id": 797885, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2019-02-20 15:20:00", "end_date_time": "2019-02-20 17:20:00", "narrative": "Periods of rain worked back into eastern Kentucky early on February 20 as a warm frontal boundary lifted north across the Commonwealth. A cold front brought additional rainfall through the afternoon and evening, before drier conditions worked into eastern Kentucky during the morning of February 21. ||Rain quickly spread back north that evening into the 22nd with southeastern Kentucky continuing to see prolonged light rain into the afternoon of the 23rd. A cold front brought additional rain to much of eastern Kentucky late on the 23rd. ||A spike in moisture ahead of this front resulted in additional moderate to heavy rain and high rainfall rates across portions of eastern Kentucky late on the 23rd. The convection ahead of the cold front that evening resulted in the majority of the flooding and flash flooding issues across eastern Kentucky. Showers and thunderstorms capable of heavy rainfall trained over parts of Wayne, Pulaski, Rockcastle, and other counties along the I-75 corridor, resulting in deadly flash flooding and river flooding along the Cumberland River. Later in the evening, the bulk of the rainfall shifted north to counties along the Mountain Parkway. Flash flooding and river flooding occurred in Powell, Wolfe, Breathitt, Magoffin, and Johnson Counties. Lighter rainfall continued into the night as flooding issues remained widespread into the 24th.||Rainfall amounts from this event ranged from near 2 inches in portions of the Bluegrass region and northeast Kentucky, to greater than 4 inches across locations in southern and southeast Kentucky. ||This additional water on top of saturated ground continued to promote mud and rock slides across eastern Kentucky, complete with power outages from fallen debris and trees. Pikeville experienced a massive rockslide early on February 22, resulting in several cars and a building being damaged. Other impacts included countless roads being inundated with standing water, pavement and water pipes breaking, water threatening homes, roads and bridges being washed away, and rising lake levels.||Of the 33 counties across eastern Kentucky, at least 27 were forced to declare State of Emergencies due to rainfall during and before this event. This included Knott County due to over $150,000 in county road damages. Beattyville, Clay City, Harlan, Hazard, Jenkins, Monticello, Paintsville, Pikeville, Salyersville, Stanton, West Liberty, and Whitesburg also declared State of Emergencies. Additionally, the Kentucky Governor declared a State of Emergency across the entire Commonwealth.||The persistent rainfall of the winter season and the amount of rainfall from this event led to Lake Cumberland reporting their highest lake level of 756.52 feet on February 26th, breaking the old record of 751.69 feet dating back to May 1984. As a result, Wolf Creek Dam had to release at a record discharge level of 59,880 cubic feet per second. Cave Run Lake also rose to within 6 feet of their record pool elevation. Buckhorn Lake came within 10 feet of their all-time record, partially resulting in Kentucky Highway 257 near Confluence having flood waters cover the highway isolating 40 to 50 families for three weeks following the end of the flooding rains. Local Emergency Management reported that Bucks Branch Road was impassable due to high water west of Martin.", "ts_dict_index": [2349, 2350, 2351]}
+{"event_id": 1049468, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2022-07-28 08:30:00", "end_date_time": "2022-07-29 03:30:00", "narrative": "Between July 25th and July 30th, 2022, several complexes of training thunderstorms developed south of I-64 and brought heavy rain, deadly flash flooding, and devastating river flooding to eastern Kentucky and central Appalachia. These thunderstorms, at times, caused rainfall rates in excess of 4/hr across complex terrain that led to widespread devastating impacts. While it did not rain continuously during this 4-day stretch, the overwhelming amounts of rain and resultant flooding led to 39 deaths and widespread catastrophic damage. Entire homes and parts of some communities were swept away by flood waters, leading to costly damage to infrastructure in the region. Over 600 helicopter rescues and countless swift water rescues by boat were needed to evacuate people who were trapped by the quickly-rising flood waters. In total, 24 Flash Flood Warnings were issued between July 26th and July 30th. Between the evening of July 27th and the mid-morning hours on July 28th (the peak of the event), 13 warnings were issued, 3 of which were upgraded to a Flash Flood Emergency.||Radar-based rainfall estimates suggest that upwards of 14-16 of rain fell during this 5-day period in a narrow swath, with many more locations receiving 6-10 of rain. Most of this rain fell during the night of July 27th into the morning of July 28th, which is when the most devastating impacts were felt. The highest totals occurred across an axis that stretches from northern Clay and southern Owsley counties, east through southern Breathitt and northern Leslie counties, into Perry, Knott and Letcher counties. The highest rainfall total report was from southern Knott County, where 14.00 fell between July 25th and July 29th. This site, a cooperative (COOP) observer at Carr Creek Lake, reported 6.71 from 7am July 28th to 7am July 29th, following a report of 6.50 at that site on the previous day. Another COOP site in Buckhorn reported 8.00 of rain for the 24-hour period ending 7am on July 28th. The rainfall total in Buckhorn from July 25th to July 29th was 11.76. These rainfall values occurring in such a short period of time are incredibly rare: there is less than a 1 in 1000 chance for this much rainfall over five days in a given year.||The incredible rainfall also led to significant rises and flooding on many rivers in eastern Kentucky including on the main stem of the Kentucky River; North, Middle and South forks of the Kentucky River; Red River and Licking River. At Whitesburg, the North Fork of the Kentucky River swelled well above major flood stage, reaching close to 21' before gauge failure (the previous flood of record was 14.7' in 1957). The North Fork of the Kentucky River at Jackson also reached major flood, setting a new record crest of 43.47' (the previous record was 43.1' set in 1939). The river flooding caused a second round of destruction for communities in the region, and caused flooding in downstream areas that did not receive as much rainfall.||*Note* Given the widespread nature and severity of this event - any dollar amount estimated by storm data will not do the event as a whole justice. Since eastern KY was a national declaration, FEMA will be doing a full cost assessment. Will use this data once available for total monetary amounts of damage.||Visit www.weather.gov/jkl/July2022Flooding for more information on the event, as well as pictures and videos of the flooding and damage. Runoff from heavy rains eventually found their way to to the Right Fork of Beaver Creek in southwest Floyd County, and Beaver Creek near Martin, leading to multiple reports of flooding in communities near the water. Some reports included:||At 8:30 AM EST - Pictures show the Marathon Gas Station along KY-7 (Main Street) in Wayland inundated by flood waters. Fuel pumps were completely submerged. |At 3:14 PM EST - Video footage showed a water rescue by the bridge on KY-7 near Maddy's Pizza in Hueysville.|At 4:00 PM EST - A picture on social media showed water up to the windows on trailer homes in Hueysville.|At 4:19 PM EST - The Garret community was reported to be inundated by several feet of flood waters from the Right Fork Beaver Creek.|At 6:28 PM EST - The Martin Fire Department reported flood waters over Brawley Street in Martin.", "ts_dict_index": [2337, 2338, 2339]}
+{"event_id": 797974, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2019-02-21 11:00:00", "end_date_time": "2019-02-21 18:00:00", "narrative": "Periods of rain worked back into eastern Kentucky early on February 20 as a warm frontal boundary lifted north across the Commonwealth. A cold front brought additional rainfall through the afternoon and evening, before drier conditions worked into eastern Kentucky during the morning of February 21. ||Rain quickly spread back north that evening into the 22nd with southeastern Kentucky continuing to see prolonged light rain into the afternoon of the 23rd. A cold front brought additional rain to much of eastern Kentucky late on the 23rd. ||A spike in moisture ahead of this front resulted in additional moderate to heavy rain and high rainfall rates across portions of eastern Kentucky late on the 23rd. The convection ahead of the cold front that evening resulted in the majority of the flooding and flash flooding issues across eastern Kentucky. Showers and thunderstorms capable of heavy rainfall trained over parts of Wayne, Pulaski, Rockcastle, and other counties along the I-75 corridor, resulting in deadly flash flooding and river flooding along the Cumberland River. Later in the evening, the bulk of the rainfall shifted north to counties along the Mountain Parkway. Flash flooding and river flooding occurred in Powell, Wolfe, Breathitt, Magoffin, and Johnson Counties. Lighter rainfall continued into the night as flooding issues remained widespread into the 24th.||Rainfall amounts from this event ranged from near 2 inches in portions of the Bluegrass region and northeast Kentucky, to greater than 4 inches across locations in southern and southeast Kentucky. ||This additional water on top of saturated ground continued to promote mud and rock slides across eastern Kentucky, complete with power outages from fallen debris and trees. Pikeville experienced a massive rockslide early on February 22, resulting in several cars and a building being damaged. Other impacts included countless roads being inundated with standing water, pavement and water pipes breaking, water threatening homes, roads and bridges being washed away, and rising lake levels.||Of the 33 counties across eastern Kentucky, at least 27 were forced to declare State of Emergencies due to rainfall during and before this event. This included Knott County due to over $150,000 in county road damages. Beattyville, Clay City, Harlan, Hazard, Jenkins, Monticello, Paintsville, Pikeville, Salyersville, Stanton, West Liberty, and Whitesburg also declared State of Emergencies. Additionally, the Kentucky Governor declared a State of Emergency across the entire Commonwealth.||The persistent rainfall of the winter season and the amount of rainfall from this event led to Lake Cumberland reporting their highest lake level of 756.52 feet on February 26th, breaking the old record of 751.69 feet dating back to May 1984. As a result, Wolf Creek Dam had to release at a record discharge level of 59,880 cubic feet per second. Cave Run Lake also rose to within 6 feet of their record pool elevation. Buckhorn Lake came within 10 feet of their all-time record, partially resulting in Kentucky Highway 257 near Confluence having flood waters cover the highway isolating 40 to 50 families for three weeks following the end of the flooding rains. Local media reported flooding in Archer Park in Prestonsburg, due in part to the rising of the Levisa Fork of the Big Sandy River. A few small mudslides were also noted in vicinity of the area.", "ts_dict_index": [2352, 2353, 2354]}
+{"event_id": 947001, "event_type": "Flash Flood", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-30 03:30:00", "end_date_time": "2021-04-30 06:15:00", "narrative": "A cluster of showers and thunderstorms developed during the late evening hours of April 29th over Deep East Texas, near and just south of a weak cold front that drifted south across East Texas and North-Central Louisiana. These storms developed in a very moist air mass, near an inverted low level trough that extended from Deep East Texas into West-Central Louisiana. Additional forcing aloft was provided by increasing large scale forcing ahead of a closed upper low over Northern Mexico, which resulted in additional redevelopment of these storms containing heavy rainfall, moving repeatedly over the same areas through much of the early morning hours on the 30th. Widespread rainfall amounts of 3-6+ inches fell across Southern Cherokee, Nacogdoches, Angelina, and San Augustine Counties, which resulted in widespread flash flooding across the areas, with numerous roads closed. These storms diminished by the mid and late morning hours on the 30th. Highway 59 South was flooded at the intersection of County Road 522.", "ts_dict_index": [2301, 2302, 2303]}
+{"event_id": 865407, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 10:52:00", "end_date_time": "2019-11-02 17:25:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 8 was closed between Poland and Five Acres Road due to flooding.", "ts_dict_index": [2367, 2368, 2369]}
+{"event_id": 864421, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 00:00:00", "end_date_time": "2019-11-01 12:36:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 5S was closed due to flooding at Sandy Lane.", "ts_dict_index": [2397, 2398, 2399]}
+{"event_id": 865411, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 03:00:00", "end_date_time": "2019-11-01 16:29:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. The Route 29A bridge over the East Canada Creek was closed due to flooding.", "ts_dict_index": [2364, 2365, 2366]}
+{"event_id": 864417, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 00:00:00", "end_date_time": "2019-11-01 07:57:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 5 was closed between Newport Road and Millers Grove Road due to flooding.", "ts_dict_index": [2388, 2389, 2390]}
+{"event_id": 865405, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 00:20:00", "end_date_time": "2019-11-05 08:24:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 8 was closed between Five Acres Lane and Gray-Wilmurt Road due to flooding.", "ts_dict_index": [2382, 2383, 2384]}
+{"event_id": 864419, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 00:00:00", "end_date_time": "2019-11-02 14:27:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 28 was closed between Middleville and Poland due to flooding.", "ts_dict_index": [2394, 2395, 2396]}
+{"event_id": 865404, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 03:52:00", "end_date_time": "2019-11-03 00:45:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. The West Canada Creek reached a record high level of 1231.49 feet at 1430EST 1 November at Hinckley Dam. It was at moderate flood stage 0352EST 1 November through 0045EST 3 November. It was at major flood stage between 0745EST 1 November through 0429EST 2 November. Extensive flooding occurred downstream with Route 28 closed in several spots between Barneveld and Herkimer. Water was several feet high at Creekview Automotive in Poland, and flooded the nearby gas station near the pumps. Residents of the West Canada Creek Village mobile home park had to be evacuated due to high water entering the park.", "ts_dict_index": [2385, 2386, 2387]}
+{"event_id": 864418, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 00:00:00", "end_date_time": "2019-11-03 14:25:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Water was flowing over Route 8 at Black Creek.", "ts_dict_index": [2391, 2392, 2393]}
+{"event_id": 865420, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 00:00:00", "end_date_time": "2019-11-03 01:55:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. The West Canada Creek reached a record high stage of 10.92 feet at Kast Bridge at 2315EST 31 October. It fell below major flood stage at 0400EST 1 November, then had a secondary crest, rising above major flood stage again at 1231EST 1 November. It remained above major flood stage until 1615EST 2 November, and fell below moderate flood stage by 0155EST 3 November. There was widespread flooding along the West Canada Creek between Middleville and Herkimer, resulting in the closure of Route 28. There was widespread flooding in the village of Middleville. Water entered structures with cars partially submerged. There were 27 evacuations as a result of the flooding. The West Canada Creek was nearing the road surface of the Route 28 bridge.", "ts_dict_index": [2376, 2377, 2378]}
+{"event_id": 865916, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 00:55:00", "end_date_time": "2019-11-03 00:22:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Heavy rainfall resulted in a record high flood stage on the Mohawk River at Little Falls. The river reached moderate flood stage by 0055EST 1 November, and exceeded major flood stage shortly thereafter by 0150EST. The first crest occurred at 0516EST 1 November at 19.73 feet before it receded slightly, but a second, higher crest of 19.86 feet occurred at 0345EST 2 November. The river fell below major flood stage by 1915EST 2 November, and below moderate flood stage by 0022EST 3 November. The high water impacted nearby rail tracks such that Amtrak service was suspended on some routes between Albany and Syracuse, and some inbound passengers were transferred to buses.", "ts_dict_index": [2379, 2380, 2381]}
+{"event_id": 865412, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 00:00:00", "end_date_time": "2019-11-01 23:24:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Route 5S was closed between Culver Avenue and Ilion due to a mudslide.", "ts_dict_index": [2370, 2371, 2372]}
+{"event_id": 1124138, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2023-07-16 02:00:00", "end_date_time": "2023-07-17 19:00:00", "narrative": "On the evening of July 15th isolated thunderstorms developed across southern New Hampshire.  Storm movement mitigated flash flooding across the state, except for the city of Manchester where multiple storms traveled directly over the city on the evening of July 15th.  Up to 2��� fell in an hour over the urban city area.  The intense rainfall rates lead to rapid run-off and caused localized urban street flooding with water due to run-off entering some building structures.  Lighter showers passed across the area later in the evening before rain ended.||On July 16th a more widespread area of rain impacted most of the state.  Rain showers began to develop around daybreak on July 16th and quickly became more widespread during the morning hours.  Light to moderate rainfall became widespread across the state with embedded bands of heavy rain.  Locally heavy rainfall continued straight through the morning hours into early afternoon on the 16th before rainfall intensity and coverage began to decrease.  Central and Southern New Hampshire received the heaviest rainfall through the day, with less rainfall across the Connecticut River Valley and the Seacoast.  Rainfall amounts of 2+��� were widespread across Central New Hampshire with two corridors of locally heavier rain in this area.  One corridor of heavy rain was from eastern Cheshire County through northwest Hillsborough County and into Central Merrimack County.  Observed reports of 3+��� of rain occurred in this region with one localized report of 4+���.  The heavy rain caused isolated areas of flooded roads along with wash-outs in Antrim where a localized area of heavy rain occurred.  The second corridor of heavy rain across the state was the most significant for the event.  This corridor of rain ran from the Massachusetts border around Nashua all the way to the Maine border in southern Carroll County.  There were numerous reports of 3+��� of rain with localized areas receiving over 4��� of rainfall by early afternoon.  The majority of this rainfall fell in a 3 to 4 hour window in the late morning hours.  The heavy rainfall rates and saturated grounds led to rapid run-off of small streams and creeks which led to flash flooding.  Flash flooding was considerable in the Barnstead, Alton and Wolfeboro region where numerous roads were closed due to severe flooding and wash-outs.  Additional urban flash flooding also occurred in the Manchester area due to flooded roads.  Minor property flooding was also reported on numerous lakefronts across the region due to very high lake levels after this rain event.   ||Localized river flooding also occurred in response to the July 15-16th rainfall with river flooding beginning on July 16th and lasting through the 18th, with river crests occurring on July 17th.  The Warner River touched minor flood stage with no significant impacts.  The Suncook River crested at 3.53ft above flood stage on July 17th.  This led to flooding of campgrounds along the river that caused the evacuation of at least one located in the floodplain. All rivers dropped below flood stage on July 18th.||In addition to the flooding, the environment supported a conditional threat for severe weather as the abundant low level moisture and strong low level jet caused significant low level shear.  This caused for numerous storms to have rotation with them that triggered tornado warnings but no tornadoes were confirmed.  There was however some localized tree damage with the associated thunderstorms across Southern New Hampshire. The Saco River came out of banks on July 16th following heavy rain showers. The USGS river gage at Conway exceeded the flood stage of 9 feet, cresting at 8.3 feet on the 16th. The impacts were mainly focused at low lying campgrounds and flooding at Transvale Road.", "ts_dict_index": [2331, 2332, 2333]}
+{"event_id": 933178, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2020-12-25 01:00:00", "end_date_time": "2020-12-26 01:00:00", "narrative": "An area of low pressure tracking from the Great Lakes to Hudson Bay advected in an unseasonably warm air mass into the region from Thursday, December 24 to Friday, December 25, 2020. Rain gradually overspread the region from west to east during the day on December 24 with the steadiest, heaviest rainfall during the overnight hours and early morning hours of December 25. Rain showers continued through the day on December 25 and changed to snow showers during the evening and overnight hours of December 25-26 as colder air returned.||The region still dealt with nearly the entire snowpack from the blockbuster winter storm from December 16-17. While the snow compacted over time, very little water was lost from the snow. Observations concluded that between 1.50 to 3.00 inches of water was in the snowpack prior to this event and most if not all of this snow melted.||Rainfall totals across eastern New York were generally between 1 to 3 inches; however, the eastern Catskills received 4 to 6 inches of rain. These amounts do not include the additional 1.50 to 3.00 inches of water that melted from the snowpack. The combination of warm air, rainfall, and melting snowpack led to areal and river flooding across the region. There were numerous reports of roads being closed due to the flooding. Local emergency managers had to evacuate a few communities due to the rising waters. Some roads across Greene and Ulster counties were washed out and had to be rebuilt. Two area rivers reached or exceeded moderate flood stage, Esopus Creek and Schoharie Creek. The Esopus briefly reached major flood stage at Mount Tremper between 0345EST and 0435EST. The Schoharie reached moderate flood stage at Breakabeen and Burtonsville, and major flood stage at Prattsville (0338EST to 0742EST) and Gilboa Bridge (0450EST to 1034EST). The Schoharie County Department of Public Works and town highway departments identified $332,000 in damage, mostly to roads. Damage estimates were $30,000 in Conesville and $50,000 in Blenheim. A mass of supersaturated snow due to heavy rain slid down a slope at the Belleayre Ski Center and crashed into the lodge, breaking doors and windows and causing water damage inside.||In addition to the rainfall, gusty winds accompanied the event with wind gusts reaching 40 to 60 mph, especially across the mid-Hudson Valley and Taconics. A 68 mph wind gust was recorded at Bannerman Island. Scattered trees were downed as a result of the wind and softened soils due to the warm air and recent rainfall. ||Key Impacts: road closures, tree damage, damage to structures, evacuations. One lane of Route 214 was washed out near the Greene/Ulster County line, resulting in a road closure. A complete rebuild of the roadway was required. One lane of alternating traffic was opened on the 26th between Moggre Road in Ulster County and Saw Mill Road in Greene County.", "ts_dict_index": [2415, 2416, 2417]}
+{"event_id": 932715, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2020-12-25 10:00:00", "end_date_time": "2020-12-25 16:00:00", "narrative": "An area of low pressure tracking from the Great Lakes to Hudson Bay advected in an unseasonably warm air mass into the region from Thursday, December 24 to Friday, December 25, 2020. Rain gradually overspread the region from west to east during the day on December 24 with the steadiest, heaviest rainfall during the overnight hours and early morning hours of December 25. Rain showers continued through the day on December 25 and changed to snow showers during the evening and overnight hours of December 25-26 as colder air returned.||The region still dealt with nearly the entire snowpack from the blockbuster winter storm from December 16-17. While the snow compacted over time, very little water was lost from the snow. Observations concluded that between 1.50 to 3.00 inches of water was in the snowpack prior to this event and most if not all of this snow melted.||Rainfall totals across eastern New York were generally between 1 to 3 inches; however, the eastern Catskills received 4 to 6 inches of rain. These amounts do not include the additional 1.50 to 3.00 inches of water that melted from the snowpack. The combination of warm air, rainfall, and melting snowpack led to areal and river flooding across the region. There were numerous reports of roads being closed due to the flooding. Local emergency managers had to evacuate a few communities due to the rising waters. Some roads across Greene and Ulster counties were washed out and had to be rebuilt. Two area rivers reached or exceeded moderate flood stage, Esopus Creek and Schoharie Creek. The Esopus briefly reached major flood stage at Mount Tremper between 0345EST and 0435EST. The Schoharie reached moderate flood stage at Breakabeen and Burtonsville, and major flood stage at Prattsville (0338EST to 0742EST) and Gilboa Bridge (0450EST to 1034EST). The Schoharie County Department of Public Works and town highway departments identified $332,000 in damage, mostly to roads. Damage estimates were $30,000 in Conesville and $50,000 in Blenheim. A mass of supersaturated snow due to heavy rain slid down a slope at the Belleayre Ski Center and crashed into the lodge, breaking doors and windows and causing water damage inside.||In addition to the rainfall, gusty winds accompanied the event with wind gusts reaching 40 to 60 mph, especially across the mid-Hudson Valley and Taconics. A 68 mph wind gust was recorded at Bannerman Island. Scattered trees were downed as a result of the wind and softened soils due to the warm air and recent rainfall. ||Key Impacts: road closures, tree damage, damage to structures, evacuations. Route 42 Northbound and Southbound lanes were closed due to flooding between County Route 6 and Howard Road in the Hamlet of West Kill.", "ts_dict_index": [2409, 2410, 2411]}
+{"event_id": 932737, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2020-12-25 02:00:00", "end_date_time": "2020-12-25 05:30:00", "narrative": "An area of low pressure tracking from the Great Lakes to Hudson Bay advected in an unseasonably warm air mass into the region from Thursday, December 24 to Friday, December 25, 2020. Rain gradually overspread the region from west to east during the day on December 24 with the steadiest, heaviest rainfall during the overnight hours and early morning hours of December 25. Rain showers continued through the day on December 25 and changed to snow showers during the evening and overnight hours of December 25-26 as colder air returned.||The region still dealt with nearly the entire snowpack from the blockbuster winter storm from December 16-17. While the snow compacted over time, very little water was lost from the snow. Observations concluded that between 1.50 to 3.00 inches of water was in the snowpack prior to this event and most if not all of this snow melted.||Rainfall totals across eastern New York were generally between 1 to 3 inches; however, the eastern Catskills received 4 to 6 inches of rain. These amounts do not include the additional 1.50 to 3.00 inches of water that melted from the snowpack. The combination of warm air, rainfall, and melting snowpack led to areal and river flooding across the region. There were numerous reports of roads being closed due to the flooding. Local emergency managers had to evacuate a few communities due to the rising waters. Some roads across Greene and Ulster counties were washed out and had to be rebuilt. Two area rivers reached or exceeded moderate flood stage, Esopus Creek and Schoharie Creek. The Esopus briefly reached major flood stage at Mount Tremper between 0345EST and 0435EST. The Schoharie reached moderate flood stage at Breakabeen and Burtonsville, and major flood stage at Prattsville (0338EST to 0742EST) and Gilboa Bridge (0450EST to 1034EST). The Schoharie County Department of Public Works and town highway departments identified $332,000 in damage, mostly to roads. Damage estimates were $30,000 in Conesville and $50,000 in Blenheim. A mass of supersaturated snow due to heavy rain slid down a slope at the Belleayre Ski Center and crashed into the lodge, breaking doors and windows and causing water damage inside.||In addition to the rainfall, gusty winds accompanied the event with wind gusts reaching 40 to 60 mph, especially across the mid-Hudson Valley and Taconics. A 68 mph wind gust was recorded at Bannerman Island. Scattered trees were downed as a result of the wind and softened soils due to the warm air and recent rainfall. ||Key Impacts: road closures, tree damage, damage to structures, evacuations. Flooding occurred in Downtown Phoenicia between 2:00 am and 5:30 am. Water was flowing down Main Street from the Esopus Creek. Eleven people were evacuated.", "ts_dict_index": [2406, 2407, 2408]}
+{"event_id": 933180, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2020-12-25 00:00:00", "end_date_time": "2020-12-26 00:00:00", "narrative": "An area of low pressure tracking from the Great Lakes to Hudson Bay advected in an unseasonably warm air mass into the region from Thursday, December 24 to Friday, December 25, 2020. Rain gradually overspread the region from west to east during the day on December 24 with the steadiest, heaviest rainfall during the overnight hours and early morning hours of December 25. Rain showers continued through the day on December 25 and changed to snow showers during the evening and overnight hours of December 25-26 as colder air returned.||The region still dealt with nearly the entire snowpack from the blockbuster winter storm from December 16-17. While the snow compacted over time, very little water was lost from the snow. Observations concluded that between 1.50 to 3.00 inches of water was in the snowpack prior to this event and most if not all of this snow melted.||Rainfall totals across eastern New York were generally between 1 to 3 inches; however, the eastern Catskills received 4 to 6 inches of rain. These amounts do not include the additional 1.50 to 3.00 inches of water that melted from the snowpack. The combination of warm air, rainfall, and melting snowpack led to areal and river flooding across the region. There were numerous reports of roads being closed due to the flooding. Local emergency managers had to evacuate a few communities due to the rising waters. Some roads across Greene and Ulster counties were washed out and had to be rebuilt. Two area rivers reached or exceeded moderate flood stage, Esopus Creek and Schoharie Creek. The Esopus briefly reached major flood stage at Mount Tremper between 0345EST and 0435EST. The Schoharie reached moderate flood stage at Breakabeen and Burtonsville, and major flood stage at Prattsville (0338EST to 0742EST) and Gilboa Bridge (0450EST to 1034EST). The Schoharie County Department of Public Works and town highway departments identified $332,000 in damage, mostly to roads. Damage estimates were $30,000 in Conesville and $50,000 in Blenheim. A mass of supersaturated snow due to heavy rain slid down a slope at the Belleayre Ski Center and crashed into the lodge, breaking doors and windows and causing water damage inside.||In addition to the rainfall, gusty winds accompanied the event with wind gusts reaching 40 to 60 mph, especially across the mid-Hudson Valley and Taconics. A 68 mph wind gust was recorded at Bannerman Island. Scattered trees were downed as a result of the wind and softened soils due to the warm air and recent rainfall. ||Key Impacts: road closures, tree damage, damage to structures, evacuations. County Route 17 in Jewett was closed between Route 23A and Mill Hollow Road due to a washout. A power pole on the side of the road was also washed out. A complete rebuild of the road was required, and the road remained closed as of mid-February 2021.", "ts_dict_index": [2418, 2419, 2420]}
+{"event_id": 932735, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2020-12-25 01:22:00", "end_date_time": "2020-12-25 10:07:00", "narrative": "An area of low pressure tracking from the Great Lakes to Hudson Bay advected in an unseasonably warm air mass into the region from Thursday, December 24 to Friday, December 25, 2020. Rain gradually overspread the region from west to east during the day on December 24 with the steadiest, heaviest rainfall during the overnight hours and early morning hours of December 25. Rain showers continued through the day on December 25 and changed to snow showers during the evening and overnight hours of December 25-26 as colder air returned.||The region still dealt with nearly the entire snowpack from the blockbuster winter storm from December 16-17. While the snow compacted over time, very little water was lost from the snow. Observations concluded that between 1.50 to 3.00 inches of water was in the snowpack prior to this event and most if not all of this snow melted.||Rainfall totals across eastern New York were generally between 1 to 3 inches; however, the eastern Catskills received 4 to 6 inches of rain. These amounts do not include the additional 1.50 to 3.00 inches of water that melted from the snowpack. The combination of warm air, rainfall, and melting snowpack led to areal and river flooding across the region. There were numerous reports of roads being closed due to the flooding. Local emergency managers had to evacuate a few communities due to the rising waters. Some roads across Greene and Ulster counties were washed out and had to be rebuilt. Two area rivers reached or exceeded moderate flood stage, Esopus Creek and Schoharie Creek. The Esopus briefly reached major flood stage at Mount Tremper between 0345EST and 0435EST. The Schoharie reached moderate flood stage at Breakabeen and Burtonsville, and major flood stage at Prattsville (0338EST to 0742EST) and Gilboa Bridge (0450EST to 1034EST). The Schoharie County Department of Public Works and town highway departments identified $332,000 in damage, mostly to roads. Damage estimates were $30,000 in Conesville and $50,000 in Blenheim. A mass of supersaturated snow due to heavy rain slid down a slope at the Belleayre Ski Center and crashed into the lodge, breaking doors and windows and causing water damage inside.||In addition to the rainfall, gusty winds accompanied the event with wind gusts reaching 40 to 60 mph, especially across the mid-Hudson Valley and Taconics. A 68 mph wind gust was recorded at Bannerman Island. Scattered trees were downed as a result of the wind and softened soils due to the warm air and recent rainfall. ||Key Impacts: road closures, tree damage, damage to structures, evacuations. Fire Department crews evacuated 20 to 25 residents along County Route 7 in Prattsville due to rising waters on the Schoharie Creek.", "ts_dict_index": [2424, 2425, 2426]}
+{"event_id": 865402, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 03:00:00", "end_date_time": "2019-11-02 09:54:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. The East Canada Creek flowed out of its banks in the Village of Dolgeville, leading to extensive severe flooding. Swiftwater rescues occurred due to the rapidly rising waters, with around 75 people evacuated from homes due to the flooding. Several homes were severely damaged or destroyed with walls ripped from their foundations. The damage was heaviest along North Main Street where several feet of water was coursing down the street and into residences. The Route 29 bridge over the East Canada Creek was closed due to high water as well.", "ts_dict_index": [2403, 2404, 2405]}
+{"event_id": 933182, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2020-12-25 01:22:00", "end_date_time": "2020-12-25 10:07:00", "narrative": "An area of low pressure tracking from the Great Lakes to Hudson Bay advected in an unseasonably warm air mass into the region from Thursday, December 24 to Friday, December 25, 2020. Rain gradually overspread the region from west to east during the day on December 24 with the steadiest, heaviest rainfall during the overnight hours and early morning hours of December 25. Rain showers continued through the day on December 25 and changed to snow showers during the evening and overnight hours of December 25-26 as colder air returned.||The region still dealt with nearly the entire snowpack from the blockbuster winter storm from December 16-17. While the snow compacted over time, very little water was lost from the snow. Observations concluded that between 1.50 to 3.00 inches of water was in the snowpack prior to this event and most if not all of this snow melted.||Rainfall totals across eastern New York were generally between 1 to 3 inches; however, the eastern Catskills received 4 to 6 inches of rain. These amounts do not include the additional 1.50 to 3.00 inches of water that melted from the snowpack. The combination of warm air, rainfall, and melting snowpack led to areal and river flooding across the region. There were numerous reports of roads being closed due to the flooding. Local emergency managers had to evacuate a few communities due to the rising waters. Some roads across Greene and Ulster counties were washed out and had to be rebuilt. Two area rivers reached or exceeded moderate flood stage, Esopus Creek and Schoharie Creek. The Esopus briefly reached major flood stage at Mount Tremper between 0345EST and 0435EST. The Schoharie reached moderate flood stage at Breakabeen and Burtonsville, and major flood stage at Prattsville (0338EST to 0742EST) and Gilboa Bridge (0450EST to 1034EST). The Schoharie County Department of Public Works and town highway departments identified $332,000 in damage, mostly to roads. Damage estimates were $30,000 in Conesville and $50,000 in Blenheim. A mass of supersaturated snow due to heavy rain slid down a slope at the Belleayre Ski Center and crashed into the lodge, breaking doors and windows and causing water damage inside.||In addition to the rainfall, gusty winds accompanied the event with wind gusts reaching 40 to 60 mph, especially across the mid-Hudson Valley and Taconics. A 68 mph wind gust was recorded at Bannerman Island. Scattered trees were downed as a result of the wind and softened soils due to the warm air and recent rainfall. ||Key Impacts: road closures, tree damage, damage to structures, evacuations. Route 23 had both lanes closed due to high water from the Delaware County line to County Route 2 in Prattsville.", "ts_dict_index": [2412, 2413, 2414]}
+{"event_id": 865401, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 06:42:00", "end_date_time": "2019-11-02 10:40:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. The Route 29 bridge over Spruce Creek was closed due to flooding.", "ts_dict_index": [2400, 2401, 2402]}
+{"event_id": 865403, "event_type": "Flood", "state": "NEW YORK", "cz_name": "HERKIMER", "begin_date_time": "2019-11-01 06:00:00", "end_date_time": "2019-11-02 06:00:00", "narrative": "A strengthening low pressure system moving from Ohio to Lake Ontario drew anomalous warmth and moisture northward on Halloween, with temperatures surging into the 60s and 70s over eastern New York and western New England. A large swath of rainfall totaling 2-5 inches, with isolated areas as high as 7 inches, occurred over the Mohawk Valley and southern Adirondacks, resulting in reports of flash flooding. The runoff caused rapid rises on area creeks and streams, with river gauges reaching record levels along the Mohawk River at Little Falls, the West Canada Creek at Hinckley and Kast Bridge, and the Sacandaga River at Hope. Moderate flooding also occurred on the Hudson River at Fort Edward, Hadley, and North Creek; the Schroon River at Riverbank; and the Mohawk River at Delta Dam. Although river rises and some impacts occurred prior to midnight (see also October 2019 StormData), the crests occurred on 1 November, and impacts persisted into the first week of November in some areas. The flooding was extensive over portions of the area, damaging and destroying numerous roads and structures and resulting in water rescues. Between 150 and 200 people were evacuated in Herkimer County. The number of dwellings damaged by the flooding was 344, of which 135 sustained major damage, and 18 were destroyed.||As a result of the flooding, a major disaster for the state of New York was requested by Governor Cuomo and approved by the President. The monetary damages for public infrastructure requested for the Mohawk Valley and southern Adirondacks totaled around $17 million ($1.2 million for Fulton County, $3.0 million for Hamilton County, $8.8 million for Herkimer County, $0.5 million for Montgomery, $1.6 million for Saratoga, and $1.9 million for Warren). Actual damage amounts were estimated to be even higher by county emergency managers. A state of emergency was declared for Dutchess, Herkimer, Hamilton, Saratoga, and Warren Counties, and boil water notices were issued in Herkimer, Hamilton, and Warren Counties due to floodwater inundation of private and public water systems. The American Red Cross opened shelters to house those displaced by flood damage.||Behind the system, westerly winds became very strong with gusts recorded as high as 63 miles per hour. The winds brought down numerous trees and resulted in widespread power outages over portions of eastern New York. Over 92,000 customers lost power, including around 26,000 in Saratoga County, 15,000 in Ulster County, and 14,000 in Dutchess County.||Other impacts from the flooding and high winds included the cancellation of Amtrak service between Syracuse and Albany due to high water encroaching on train tracks, and portions of the Adirondack Park backcountry becoming impassable due to bridge washouts, high water at stream crossings, and downed trees and debris on trails and at trailheads. Roads and a bridge were washed out in the Town of Fairfield, prompting swiftwater rescues. The bridge on Farrington Road was washed out, stranding the residents of four homes.", "ts_dict_index": [2373, 2374, 2375]}
+{"event_id": 933183, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2020-12-25 01:00:00", "end_date_time": "2020-12-26 01:00:00", "narrative": "An area of low pressure tracking from the Great Lakes to Hudson Bay advected in an unseasonably warm air mass into the region from Thursday, December 24 to Friday, December 25, 2020. Rain gradually overspread the region from west to east during the day on December 24 with the steadiest, heaviest rainfall during the overnight hours and early morning hours of December 25. Rain showers continued through the day on December 25 and changed to snow showers during the evening and overnight hours of December 25-26 as colder air returned.||The region still dealt with nearly the entire snowpack from the blockbuster winter storm from December 16-17. While the snow compacted over time, very little water was lost from the snow. Observations concluded that between 1.50 to 3.00 inches of water was in the snowpack prior to this event and most if not all of this snow melted.||Rainfall totals across eastern New York were generally between 1 to 3 inches; however, the eastern Catskills received 4 to 6 inches of rain. These amounts do not include the additional 1.50 to 3.00 inches of water that melted from the snowpack. The combination of warm air, rainfall, and melting snowpack led to areal and river flooding across the region. There were numerous reports of roads being closed due to the flooding. Local emergency managers had to evacuate a few communities due to the rising waters. Some roads across Greene and Ulster counties were washed out and had to be rebuilt. Two area rivers reached or exceeded moderate flood stage, Esopus Creek and Schoharie Creek. The Esopus briefly reached major flood stage at Mount Tremper between 0345EST and 0435EST. The Schoharie reached moderate flood stage at Breakabeen and Burtonsville, and major flood stage at Prattsville (0338EST to 0742EST) and Gilboa Bridge (0450EST to 1034EST). The Schoharie County Department of Public Works and town highway departments identified $332,000 in damage, mostly to roads. Damage estimates were $30,000 in Conesville and $50,000 in Blenheim. A mass of supersaturated snow due to heavy rain slid down a slope at the Belleayre Ski Center and crashed into the lodge, breaking doors and windows and causing water damage inside.||In addition to the rainfall, gusty winds accompanied the event with wind gusts reaching 40 to 60 mph, especially across the mid-Hudson Valley and Taconics. A 68 mph wind gust was recorded at Bannerman Island. Scattered trees were downed as a result of the wind and softened soils due to the warm air and recent rainfall. ||Key Impacts: road closures, tree damage, damage to structures, evacuations. A creek washed over a bridge on Pennsylvania Avenue in Catskill, depositing debris and damaging the roadway.", "ts_dict_index": [2430, 2431, 2432]}
+{"event_id": 916799, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2020-07-26 16:00:00", "end_date_time": "2020-07-31 23:59:00", "narrative": "Hurricane Hanna, the 2020 Atlantic season's first Hurricane, made landfall along the unpopulated Padre Island National Seashore on the mid-Kenedy County coastline as a Category 1 storm at around 5 PM Central Time Saturday, July 25th, carrying sustained 90 mph winds with gusts over 100 mph in a small portion of the inner eye wall. The hurricane spun slowly but steadily into southern Kenedy and northern Hidalgo County through just after midnight on the 26th, then through Starr County as a Tropical Storm before moving into Tamaulipas before daybreak and eventually near Monterrey, Nuevo Leon, by noon before dissipating during the evening of the 26th. Following the passage of the inner eye wall, broad feeder bands of torrential rains and gusty tropical storm force winds continued through the mid to late morning hours of July 26th, slowly migrating from east to west across the populated Rio Grande Valley. ||Other than storm surge flooding, which peaked just north of Baffin Bay on the Kleberg and Nueces County coast near Corpus Christi, Hanna's memory for the Rio Grande Valley will be flooding rainfall, power outages, and an array of damage to poorly constructed buildings, from minor roof damage to complete demolition.  Between 8 and 15 inches of rain fell from Port Mansfield to Harlingen, and along Interstate Highway 2 out through Mission and Sullivan City. The combination of high rainfall, locally high rainfall rates, and poor drainage left between 18 inches and four feet of water depth in many areas, most commonly from western Cameron through southeastern Hidalgo County, as well as a separate pocket in the Mission/La Joya/Sullivan City area. The rainfall wiped out 95% of the region's cotton crop; the combination of crop loss and production loss was more than one third of a billion dollars alone ($366 million)...most of which was in the Rio Grande Valley region.  ||At the peak of the storm, 250 thousand electric customers were without power, including all of Willacy County. Though storm surge was cut short by strong westerly flow across Cameron County, radiating swells did produce a notable surge of 3 feet or greater (estimated) from near Port Mansfield through Kenedy County. When the damage and economic loss is counted to infrastructure and agriculture combined, it is likely that Hanna cost at least one billion dollars across the Rio Grande Valley and the Deep S. Texas ranch country. High standing water due to a total of 7 to 12 inches of rainfall that fell directly from Hurricane/Tropical Storm Hanna from late on July 25th through early afternoon on July 26th continued to close roads and stand in neighborhoods, fields, and ditches through the end of July in western Cameron County, from the Cameron/Hidalgo and Cameron/Willacy County lines through the west side of Harlingen. An additional 2 to 5 inches fell during the late afternoon and early evening of July 27th from an unrelated tropical rain band, leaving total rainfall of 10 to 15 inches in the area.  ||A combination of the heavy rain with known drainage capacity issues in the form of pumps, pipes, and retention kept water levels ranging from 18 inches to four feet deep on at least a dozen roads, including portions of SR 107 around Santa Rosa as well as along Farm-to-Market Road 506  between La Feria and Santa Rosa, continuing north to near the Willacy County line and east to near Primera and Palm Valley.  Fields saw similar water levels, and low lying neighborhoods had high water near homes, with spot-built farm homes seeing some water inside.  Santa Rosa to La Feria had similar high water for a third straight summer. | |Another round of heavy rainfall of 1 to 4 inches arrived during the evening of August 1st, prolonging the high water for a few more days into the following month, before dry weather arrived and allowed all water to recede. ||Note:  Public Assistance (which includes damage to roads and bridges) and Crop damage is listed on the Flash Flood event in western Cameron County for brevity. Individual assistance and insured damage estimated from the National Flood Insurance Program of FEMA, which was estimated at nearly $10 million, was added to the flash flood entry for Cameron County for brevity, as mentioned above.", "ts_dict_index": [2484, 2485, 2486]}
+{"event_id": 933197, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2020-12-25 02:00:00", "end_date_time": "2020-12-26 02:00:00", "narrative": "An area of low pressure tracking from the Great Lakes to Hudson Bay advected in an unseasonably warm air mass into the region from Thursday, December 24 to Friday, December 25, 2020. Rain gradually overspread the region from west to east during the day on December 24 with the steadiest, heaviest rainfall during the overnight hours and early morning hours of December 25. Rain showers continued through the day on December 25 and changed to snow showers during the evening and overnight hours of December 25-26 as colder air returned.||The region still dealt with nearly the entire snowpack from the blockbuster winter storm from December 16-17. While the snow compacted over time, very little water was lost from the snow. Observations concluded that between 1.50 to 3.00 inches of water was in the snowpack prior to this event and most if not all of this snow melted.||Rainfall totals across eastern New York were generally between 1 to 3 inches; however, the eastern Catskills received 4 to 6 inches of rain. These amounts do not include the additional 1.50 to 3.00 inches of water that melted from the snowpack. The combination of warm air, rainfall, and melting snowpack led to areal and river flooding across the region. There were numerous reports of roads being closed due to the flooding. Local emergency managers had to evacuate a few communities due to the rising waters. Some roads across Greene and Ulster counties were washed out and had to be rebuilt. Two area rivers reached or exceeded moderate flood stage, Esopus Creek and Schoharie Creek. The Esopus briefly reached major flood stage at Mount Tremper between 0345EST and 0435EST. The Schoharie reached moderate flood stage at Breakabeen and Burtonsville, and major flood stage at Prattsville (0338EST to 0742EST) and Gilboa Bridge (0450EST to 1034EST). The Schoharie County Department of Public Works and town highway departments identified $332,000 in damage, mostly to roads. Damage estimates were $30,000 in Conesville and $50,000 in Blenheim. A mass of supersaturated snow due to heavy rain slid down a slope at the Belleayre Ski Center and crashed into the lodge, breaking doors and windows and causing water damage inside.||In addition to the rainfall, gusty winds accompanied the event with wind gusts reaching 40 to 60 mph, especially across the mid-Hudson Valley and Taconics. A 68 mph wind gust was recorded at Bannerman Island. Scattered trees were downed as a result of the wind and softened soils due to the warm air and recent rainfall. ||Key Impacts: road closures, tree damage, damage to structures, evacuations. Cauterskill Road and County Route 23B in Leeds were closed due to water over the road.", "ts_dict_index": [2433, 2434, 2435]}
+{"event_id": 914459, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2020-07-26 04:00:00", "end_date_time": "2020-07-26 08:00:00", "narrative": "Hurricane Hanna, the 2020 Atlantic season's first Hurricane, made landfall along the unpopulated Padre Island National Seashore on the mid-Kenedy County coastline as a Category 1 storm at around 5 PM Central Time Saturday, July 25th, carrying sustained 90 mph winds with gusts over 100 mph in a small portion of the inner eye wall. The hurricane spun slowly but steadily into southern Kenedy and northern Hidalgo County through just after midnight on the 26th, then through Starr County as a Tropical Storm before moving into Tamaulipas before daybreak and eventually near Monterrey, Nuevo Leon, by noon before dissipating during the evening of the 26th. Following the passage of the inner eye wall, broad feeder bands of torrential rains and gusty tropical storm force winds continued through the mid to late morning hours of July 26th, slowly migrating from east to west across the populated Rio Grande Valley. ||Other than storm surge flooding, which peaked just north of Baffin Bay on the Kleberg and Nueces County coast near Corpus Christi, Hanna's memory for the Rio Grande Valley will be flooding rainfall, power outages, and an array of damage to poorly constructed buildings, from minor roof damage to complete demolition.  Between 8 and 15 inches of rain fell from Port Mansfield to Harlingen, and along Interstate Highway 2 out through Mission and Sullivan City. The combination of high rainfall, locally high rainfall rates, and poor drainage left between 18 inches and four feet of water depth in many areas, most commonly from western Cameron through southeastern Hidalgo County, as well as a separate pocket in the Mission/La Joya/Sullivan City area. The rainfall wiped out 95% of the region's cotton crop; the combination of crop loss and production loss was more than one third of a billion dollars alone ($366 million)...most of which was in the Rio Grande Valley region.  ||At the peak of the storm, 250 thousand electric customers were without power, including all of Willacy County. Though storm surge was cut short by strong westerly flow across Cameron County, radiating swells did produce a notable surge of 3 feet or greater (estimated) from near Port Mansfield through Kenedy County. When the damage and economic loss is counted to infrastructure and agriculture combined, it is likely that Hanna cost at least one billion dollars across the Rio Grande Valley and the Deep S. Texas ranch country. Trusted reports from Facebook indicated 1 to 2 feet of standing water in some neighborhood streets in Los Fresnos during a period of outer south to north moving feeder bands well east of the center of Tropical Storm Hanna which was moving into northern Mexico south of Starr County at around the same time.  An estimated 3 to 5 inches additional rainfall fell during this period, with measured and estimated storm totals of 6 to 9 inches in southeastern Cameron County.  No significant flooding was reported, and any property damage was unknown. ||Some of the cotton crop (lint, or bolls) and perhaps other crop was flattened by the torrential rains in fields between San Benito and Bayview.  Exact dollar damage estimates for these fields was unknown; an estimated total is provided in the Flash Flood Entry for this episode in Cameron County.", "ts_dict_index": [2481, 2482, 2483]}
+{"event_id": 814116, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 07:49:00", "end_date_time": "2019-03-13 08:49:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. Water was on the road on Highway 30 west of North Bend.", "ts_dict_index": [2460, 2461, 2462]}
+{"event_id": 813960, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 09:00:00", "end_date_time": "2019-03-14 07:00:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. This is for flooding along the Pebble Creek. The river gage at Scribner, operated by the Nebraska DNR, peaked at 24.09 feet at 9 pm on March 13th. Minor flood stage is 18 feet, moderate flood stage is 21 feet while major flood stage is 23 feet. Preliminarily this peak is the 3rd highest on record. Flood gates placed on Highway 275 kept water out of Scribner likely saving it from major flooding.", "ts_dict_index": [2445, 2446, 2447]}
+{"event_id": 815781, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 23:26:00", "end_date_time": "2019-03-14 00:26:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. Residents south of Inglewood are being evacuated.", "ts_dict_index": [2436, 2437, 2438]}
+{"event_id": 815774, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 15:15:00", "end_date_time": "2019-03-13 16:15:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. Parts of Nickerson are under water due to overflow from Maple Creek.", "ts_dict_index": [2439, 2440, 2441]}
+{"event_id": 814115, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 07:47:00", "end_date_time": "2019-03-13 08:47:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. Water was covering the intersection of Highway 275 and Highway 91.", "ts_dict_index": [2457, 2458, 2459]}
+{"event_id": 813983, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 07:00:00", "end_date_time": "2019-03-16 21:00:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. This is for flooding along the Logan Creek. The river gage at Uehling, operated by the USGS, peaked at 21.16 feet at 4 pm on March 15th. Minor flood stage is 18 feet, moderate flood stage is 19 feet while major flood stage is 21 feet. Preliminarily this peak is the highest on record. The only known damages were to county roads along the Logan Creek. Other flooded areas were low-lying areas of Oakland which included their city park.", "ts_dict_index": [2448, 2449, 2450]}
+{"event_id": 813958, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 08:00:00", "end_date_time": "2019-03-15 04:30:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. This is for flooding along the Maple Creek. The river gage near Nickerson, operated by the USGS, peaked at 17.78 feet at 8 am on March 14th. Minor flood stage is 11.5 feet, moderate flood stage is 13 feet while major flood stage is 17 feet. Preliminarily this peak is the highest on record. The town of Nickerson experienced major flooding with many homes impacted.", "ts_dict_index": [2475, 2476, 2477]}
+{"event_id": 815776, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 20:00:00", "end_date_time": "2019-03-13 21:00:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. The housing that holds the gauge equipment was knocked over by flowing ice. Data measurement on the Platte River at this location unavailable until further notice.", "ts_dict_index": [2442, 2443, 2444]}
+{"event_id": 814342, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 10:30:00", "end_date_time": "2019-03-17 07:15:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. This is for flooding along the Platte River. The river gage at North Bend, operated by the USGS, peaked at 11.91 feet at 8 am on March 17th. Minor flood stage is 8 feet, moderate flood stage is 12 feet while major flood stage is 15 feet. Preliminary this peak is the 3rd highest on record. Ice jamming also played a role in the flooding at this location. The net effect of this flooding was overwhelmed by the high water that immediately proceeded any river ice movement. Areas that were severely impacted include: North Bend, Inglewood, south Fremont, Big Island area and Fremont Lake State Recreation areas. Many highways and gravels roads were flooded.", "ts_dict_index": [2451, 2452, 2453]}
+{"event_id": 813933, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 11:00:00", "end_date_time": "2019-03-18 23:00:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. This is for flooding along the Elkhorn River. The river gage at Winslow, operated by the Nebraska DNR, peaked at 24.14 feet at 1 am on March 14th. Minor flood stage is 17 feet. Major flood stage is 24 feet. Preliminary this is a record crest.  The town of Winslow received extensive damage as their levee was easily overtopped. This river gage stopped reporting around 6 am on March 14th. This was likely due to river ice damaging the gage sensor.", "ts_dict_index": [2463, 2464, 2465]}
+{"event_id": 815806, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-15 13:17:00", "end_date_time": "2019-03-15 14:17:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. Water in Fremont is up to the tracks in the south part of town.", "ts_dict_index": [2478, 2479, 2480]}
+{"event_id": 814129, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 09:45:00", "end_date_time": "2019-03-13 10:45:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. Water is encroaching the bridge guards along Maple Creek.", "ts_dict_index": [2469, 2470, 2471]}
+{"event_id": 814309, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 11:47:00", "end_date_time": "2019-03-13 12:47:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. The Platte River has begun to ruse out of its banks at Highway 77.", "ts_dict_index": [2466, 2467, 2468]}
+{"event_id": 814128, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 09:42:00", "end_date_time": "2019-03-13 10:42:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. Water from Maple Creek is beginning to cross the bridge at Nickerson Road.", "ts_dict_index": [2472, 2473, 2474]}
+{"event_id": 933181, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2020-12-25 00:00:00", "end_date_time": "2020-12-26 00:00:00", "narrative": "An area of low pressure tracking from the Great Lakes to Hudson Bay advected in an unseasonably warm air mass into the region from Thursday, December 24 to Friday, December 25, 2020. Rain gradually overspread the region from west to east during the day on December 24 with the steadiest, heaviest rainfall during the overnight hours and early morning hours of December 25. Rain showers continued through the day on December 25 and changed to snow showers during the evening and overnight hours of December 25-26 as colder air returned.||The region still dealt with nearly the entire snowpack from the blockbuster winter storm from December 16-17. While the snow compacted over time, very little water was lost from the snow. Observations concluded that between 1.50 to 3.00 inches of water was in the snowpack prior to this event and most if not all of this snow melted.||Rainfall totals across eastern New York were generally between 1 to 3 inches; however, the eastern Catskills received 4 to 6 inches of rain. These amounts do not include the additional 1.50 to 3.00 inches of water that melted from the snowpack. The combination of warm air, rainfall, and melting snowpack led to areal and river flooding across the region. There were numerous reports of roads being closed due to the flooding. Local emergency managers had to evacuate a few communities due to the rising waters. Some roads across Greene and Ulster counties were washed out and had to be rebuilt. Two area rivers reached or exceeded moderate flood stage, Esopus Creek and Schoharie Creek. The Esopus briefly reached major flood stage at Mount Tremper between 0345EST and 0435EST. The Schoharie reached moderate flood stage at Breakabeen and Burtonsville, and major flood stage at Prattsville (0338EST to 0742EST) and Gilboa Bridge (0450EST to 1034EST). The Schoharie County Department of Public Works and town highway departments identified $332,000 in damage, mostly to roads. Damage estimates were $30,000 in Conesville and $50,000 in Blenheim. A mass of supersaturated snow due to heavy rain slid down a slope at the Belleayre Ski Center and crashed into the lodge, breaking doors and windows and causing water damage inside.||In addition to the rainfall, gusty winds accompanied the event with wind gusts reaching 40 to 60 mph, especially across the mid-Hudson Valley and Taconics. A 68 mph wind gust was recorded at Bannerman Island. Scattered trees were downed as a result of the wind and softened soils due to the warm air and recent rainfall. ||Key Impacts: road closures, tree damage, damage to structures, evacuations. Hunter Brook washed mud, rock, and debris onto the end of Spruceton Road, blocking access to a popular hiking trailhead.", "ts_dict_index": [2421, 2422, 2423]}
+{"event_id": 1064899, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 17:47:00", "end_date_time": "2023-01-09 19:47:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a vehicle stuck in a mudslide at the end of Lopes Ave. in Merced.", "ts_dict_index": [2511, 2512, 2513]}
+{"event_id": 982451, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2021-10-25 09:33:00", "end_date_time": "2021-10-25 11:33:00", "narrative": "A large upper level low pressure system in the Gulf of Alaska picked up an abundant amount of tropical moisture from the remains of Typhoon Namtheun on October 23.  This large upper low then dropped southeast to off the Pacific Northwest coast on during the morning of October 24 then underwent rapid intensification during the afternoon of October 24 resulting in a strong surge of deep tropical moisture being pushed into central California by the evening of October 24.  As the upper low tracked inland across the Pacific northwest on October 25, a cold front dropped southward through California bringing moderate to heavy precipitation to areas north of Kern County for 10-12 hours. Much of Yosemite National Park and Mariposa County picked up between 3 to 5 inches of liquid precipitation while 2 to 4 inches of liquid precipitation fell in the Sierra Nevada in Madera and Fresno Counties.  Further south, 1 to 2 inches of liquid precipitation fell in the mountains of Tulare County while the Kern County Mountains generally picked up between half and inch and an inch of rainfall.  Most of the San Joaquin Valley and West Side Hills also picked up between a half inch and an inch of rain while most of Merced County picked up between and inch to an inch and a half.  The Kern County Deserts also picked up between a quarter and a half inch of rainfall.  With most of the moisture from this system being of tropical origin, the snow level was above 9000 feet until the afternoon of October 25.  The snow level lowered to 6000 to 7000 feet before the precipitation ended during the evening of October 25.  Several SNOTEL stations measured between 9 and 15 inches of snow in 12 hours while a few stations above 9000 feet measured between 15 and 30 inches.  There were also several stations which measured peak wind gusts between 58 and 70 mph ahead of the storm during the morning of October 25 or behind the cold front during the evening of October 25.  Scattered thunderstorms developed over the San Joaquin Valley behind the cold front during the afternoon of October 25.  One supercell produced a funnel cloud over southwestern Kings County then moved southeast into Kern County bringing heavy rainfall to the Lost Hills and Wasco areas.  The precipitation tapered off by late  evening and winds diminished by the morning of October 26 as the storm moved to the east of the area. California Highway Patrol reported roadway flooding near the intersection of Rd. 48 and Ave. 408 west of Dinuba.", "ts_dict_index": [2502, 2503, 2504]}
+{"event_id": 982458, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2021-10-25 12:12:00", "end_date_time": "2021-10-25 14:12:00", "narrative": "A large upper level low pressure system in the Gulf of Alaska picked up an abundant amount of tropical moisture from the remains of Typhoon Namtheun on October 23.  This large upper low then dropped southeast to off the Pacific Northwest coast on during the morning of October 24 then underwent rapid intensification during the afternoon of October 24 resulting in a strong surge of deep tropical moisture being pushed into central California by the evening of October 24.  As the upper low tracked inland across the Pacific northwest on October 25, a cold front dropped southward through California bringing moderate to heavy precipitation to areas north of Kern County for 10-12 hours. Much of Yosemite National Park and Mariposa County picked up between 3 to 5 inches of liquid precipitation while 2 to 4 inches of liquid precipitation fell in the Sierra Nevada in Madera and Fresno Counties.  Further south, 1 to 2 inches of liquid precipitation fell in the mountains of Tulare County while the Kern County Mountains generally picked up between half and inch and an inch of rainfall.  Most of the San Joaquin Valley and West Side Hills also picked up between a half inch and an inch of rain while most of Merced County picked up between and inch to an inch and a half.  The Kern County Deserts also picked up between a quarter and a half inch of rainfall.  With most of the moisture from this system being of tropical origin, the snow level was above 9000 feet until the afternoon of October 25.  The snow level lowered to 6000 to 7000 feet before the precipitation ended during the evening of October 25.  Several SNOTEL stations measured between 9 and 15 inches of snow in 12 hours while a few stations above 9000 feet measured between 15 and 30 inches.  There were also several stations which measured peak wind gusts between 58 and 70 mph ahead of the storm during the morning of October 25 or behind the cold front during the evening of October 25.  Scattered thunderstorms developed over the San Joaquin Valley behind the cold front during the afternoon of October 25.  One supercell produced a funnel cloud over southwestern Kings County then moved southeast into Kern County bringing heavy rainfall to the Lost Hills and Wasco areas.  The precipitation tapered off by late  evening and winds diminished by the morning of October 26 as the storm moved to the east of the area. California Highway Patrol reported roadway flooding on Panama Lane 5 miles east of the SR 43 intersection.", "ts_dict_index": [2496, 2497, 2498]}
+{"event_id": 982454, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2021-10-25 09:50:00", "end_date_time": "2021-10-25 11:50:00", "narrative": "A large upper level low pressure system in the Gulf of Alaska picked up an abundant amount of tropical moisture from the remains of Typhoon Namtheun on October 23.  This large upper low then dropped southeast to off the Pacific Northwest coast on during the morning of October 24 then underwent rapid intensification during the afternoon of October 24 resulting in a strong surge of deep tropical moisture being pushed into central California by the evening of October 24.  As the upper low tracked inland across the Pacific northwest on October 25, a cold front dropped southward through California bringing moderate to heavy precipitation to areas north of Kern County for 10-12 hours. Much of Yosemite National Park and Mariposa County picked up between 3 to 5 inches of liquid precipitation while 2 to 4 inches of liquid precipitation fell in the Sierra Nevada in Madera and Fresno Counties.  Further south, 1 to 2 inches of liquid precipitation fell in the mountains of Tulare County while the Kern County Mountains generally picked up between half and inch and an inch of rainfall.  Most of the San Joaquin Valley and West Side Hills also picked up between a half inch and an inch of rain while most of Merced County picked up between and inch to an inch and a half.  The Kern County Deserts also picked up between a quarter and a half inch of rainfall.  With most of the moisture from this system being of tropical origin, the snow level was above 9000 feet until the afternoon of October 25.  The snow level lowered to 6000 to 7000 feet before the precipitation ended during the evening of October 25.  Several SNOTEL stations measured between 9 and 15 inches of snow in 12 hours while a few stations above 9000 feet measured between 15 and 30 inches.  There were also several stations which measured peak wind gusts between 58 and 70 mph ahead of the storm during the morning of October 25 or behind the cold front during the evening of October 25.  Scattered thunderstorms developed over the San Joaquin Valley behind the cold front during the afternoon of October 25.  One supercell produced a funnel cloud over southwestern Kings County then moved southeast into Kern County bringing heavy rainfall to the Lost Hills and Wasco areas.  The precipitation tapered off by late  evening and winds diminished by the morning of October 26 as the storm moved to the east of the area. California Highway Patrol reported roadway flooding near the intersection of Baldwin Rd. and La France Dr. in Bakersfield. Vehicles were not able to drive through the intersection.", "ts_dict_index": [2499, 2500, 2501]}
+{"event_id": 982453, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2021-10-25 09:47:00", "end_date_time": "2021-10-25 11:47:00", "narrative": "A large upper level low pressure system in the Gulf of Alaska picked up an abundant amount of tropical moisture from the remains of Typhoon Namtheun on October 23.  This large upper low then dropped southeast to off the Pacific Northwest coast on during the morning of October 24 then underwent rapid intensification during the afternoon of October 24 resulting in a strong surge of deep tropical moisture being pushed into central California by the evening of October 24.  As the upper low tracked inland across the Pacific northwest on October 25, a cold front dropped southward through California bringing moderate to heavy precipitation to areas north of Kern County for 10-12 hours. Much of Yosemite National Park and Mariposa County picked up between 3 to 5 inches of liquid precipitation while 2 to 4 inches of liquid precipitation fell in the Sierra Nevada in Madera and Fresno Counties.  Further south, 1 to 2 inches of liquid precipitation fell in the mountains of Tulare County while the Kern County Mountains generally picked up between half and inch and an inch of rainfall.  Most of the San Joaquin Valley and West Side Hills also picked up between a half inch and an inch of rain while most of Merced County picked up between and inch to an inch and a half.  The Kern County Deserts also picked up between a quarter and a half inch of rainfall.  With most of the moisture from this system being of tropical origin, the snow level was above 9000 feet until the afternoon of October 25.  The snow level lowered to 6000 to 7000 feet before the precipitation ended during the evening of October 25.  Several SNOTEL stations measured between 9 and 15 inches of snow in 12 hours while a few stations above 9000 feet measured between 15 and 30 inches.  There were also several stations which measured peak wind gusts between 58 and 70 mph ahead of the storm during the morning of October 25 or behind the cold front during the evening of October 25.  Scattered thunderstorms developed over the San Joaquin Valley behind the cold front during the afternoon of October 25.  One supercell produced a funnel cloud over southwestern Kings County then moved southeast into Kern County bringing heavy rainfall to the Lost Hills and Wasco areas.  The precipitation tapered off by late  evening and winds diminished by the morning of October 26 as the storm moved to the east of the area. California Highway Patrol reported roadway flooding on SR 99 just northwest of Bakersfield.", "ts_dict_index": [2508, 2509, 2510]}
+{"event_id": 1064898, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 16:54:00", "end_date_time": "2023-01-09 18:54:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding at the intersection of Cottonwood Rd. and Whitworth Rd.", "ts_dict_index": [2514, 2515, 2516]}
+{"event_id": 1064903, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 18:03:00", "end_date_time": "2023-01-09 20:03:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of flooding on southbound I-5 just south of Taglio Road concealing potholes on the roadway.", "ts_dict_index": [2520, 2521, 2522]}
+{"event_id": 1064900, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 17:55:00", "end_date_time": "2023-01-09 19:55:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of flooding from heavy rainfall on southbound SR 99 near the Martin Luther King exchange in Merced.", "ts_dict_index": [2517, 2518, 2519]}
+{"event_id": 933859, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2020-12-25 09:00:00", "end_date_time": "2020-12-25 14:30:00", "narrative": "An area of low pressure tracking from the Great Lakes to Hudson Bay advected in an unseasonably warm air mass into the region from Thursday, December 24 to Friday, December 25, 2020. Rain gradually overspread the region from west to east during the day on December 24 with the steadiest, heaviest rainfall during the overnight hours and early morning hours of December 25. Rain showers continued through the day on December 25 and changed to snow showers during the evening and overnight hours of December 25-26 as colder air returned.||The region still dealt with nearly the entire snowpack from the blockbuster winter storm from December 16-17. While the snow compacted over time, very little water was lost from the snow. Observations concluded that between 1.50 to 3.00 inches of water was in the snowpack prior to this event and most if not all of this snow melted.||Rainfall totals across eastern New York were generally between 1 to 3 inches; however, the eastern Catskills received 4 to 6 inches of rain. These amounts do not include the additional 1.50 to 3.00 inches of water that melted from the snowpack. The combination of warm air, rainfall, and melting snowpack led to areal and river flooding across the region. There were numerous reports of roads being closed due to the flooding. Local emergency managers had to evacuate a few communities due to the rising waters. Some roads across Greene and Ulster counties were washed out and had to be rebuilt. Two area rivers reached or exceeded moderate flood stage, Esopus Creek and Schoharie Creek. The Esopus briefly reached major flood stage at Mount Tremper between 0345EST and 0435EST. The Schoharie reached moderate flood stage at Breakabeen and Burtonsville, and major flood stage at Prattsville (0338EST to 0742EST) and Gilboa Bridge (0450EST to 1034EST). The Schoharie County Department of Public Works and town highway departments identified $332,000 in damage, mostly to roads. Damage estimates were $30,000 in Conesville and $50,000 in Blenheim. A mass of supersaturated snow due to heavy rain slid down a slope at the Belleayre Ski Center and crashed into the lodge, breaking doors and windows and causing water damage inside.||In addition to the rainfall, gusty winds accompanied the event with wind gusts reaching 40 to 60 mph, especially across the mid-Hudson Valley and Taconics. A 68 mph wind gust was recorded at Bannerman Island. Scattered trees were downed as a result of the wind and softened soils due to the warm air and recent rainfall. ||Key Impacts: road closures, tree damage, damage to structures, evacuations. Water was over a roadway at Dutchmen's Landing.", "ts_dict_index": [2427, 2428, 2429]}
+{"event_id": 1064541, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 19:40:00", "end_date_time": "2023-01-09 23:40:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a telephone pole leaning over the roadway on SR 137 east of Farmersville Blvd.", "ts_dict_index": [2526, 2527, 2528]}
+{"event_id": 1064906, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 18:58:00", "end_date_time": "2023-01-09 20:58:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of flooding on SR 99 north of the E. Childs Ave. exchange.", "ts_dict_index": [2529, 2530, 2531]}
+{"event_id": 814114, "event_type": "Flood", "state": "NEBRASKA", "cz_name": "DODGE", "begin_date_time": "2019-03-13 07:42:00", "end_date_time": "2019-03-13 08:42:00", "narrative": "A 971mb bomb cyclone moved out of the central Rockies on Wednesday, March 13, 2019 and helped to create widespread, moderate to major, and in many cases historic, flooding across eastern Nebraska and western Iowa. From 4 to 15 inches of snow cover remained across the mid Missouri River valley, and the ground was frozen with existing frost depths of 15 to 23 inches. Warm temperatures allowed all of the snow to rapidly melt and record moisture allowed 1 to 2.5 inches of rain to fall over a 48 hour period.  Due to the frozen ground, and that 1 to 2 feet of thick ice remained in area rivers, widespread, and in many cases, catastrophic flooding developed. Due to expansive levee breaches on many rivers and streams, the flood damage was particularly devastating to many communities. Four individuals lost their lives due to the extreme conditions, and several hundred people required rescue via air or boat. Tens of thousands of people were evacuated from their homes or businesses. Nearly 50 levees were breached on the Platte, Elkhorn and Missouri Rivers due to the large volume of water. One such levee breach along the Platte River near Leshara, Nebraska forced the evacuation of National Weather Service Omaha, located in Valley, Nebraska for 8 days. Nebraska Governor Pete Ricketts presented US$1.3 billion preliminary damage estimates for the entire state, including specific sector losses of: $439 million infrastructure (including roads and bridges), $85 million private homes and businesses, $400 million livestock and $440 million crop. About 2,000 miles of state roads including 15 Nebraska state highway bridges and numerous local bridges, roughly 20 percent of the entire state road system were impacted. Iowa Governor Kim Reynolds provided a $1.6 billion preliminary damage estimate due to flooding across the state. U.S. Interstate 29, extending north-south along the Missouri River, was inundated and partially destroyed, as was the Interstate 680 bypass around Council Bluffs-Omaha metropolitan area. Also noteworthy was damage to Offutt Air Force Base located near Bellevue, Nebraska. One-third of the base���s main runway was inundated, along with one-third of Offutt���s buildings, with several hundred employees, and several families displaced. Preliminary damage estimates released by the Department of Defense are on the order of $450 million. Nebraska and Iowa severe flooding impacts culminated in Federal Disaster Declaration 4420. Water was reported on roadways at County Road G and County Road 18 near Hooper.", "ts_dict_index": [2454, 2455, 2456]}
+{"event_id": 1064543, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 21:15:00", "end_date_time": "2023-01-09 23:15:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public reports of a traffic collision with a solo vehicle in knee high water on Rd. 124 near the intersection of Ave. 120.", "ts_dict_index": [2538, 2539, 2540]}
+{"event_id": 1064904, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 18:39:00", "end_date_time": "2023-01-09 20:39:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of flooding concealing a large pothole on SR 99 just north of the Franklin Rd. exchange.", "ts_dict_index": [2541, 2542, 2543]}
+{"event_id": 1064907, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 18:59:00", "end_date_time": "2023-01-09 20:59:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding at the intersection of Westside Blvd. and Weir Ave.", "ts_dict_index": [2532, 2533, 2534]}
+{"event_id": 1064908, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 19:00:00", "end_date_time": "2023-01-09 21:00:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding at the intersection of Sutter St. and Santa Fe Ave. in Planada with vehicles stuck in the middle lane.", "ts_dict_index": [2535, 2536, 2537]}
+{"event_id": 1064905, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 18:44:00", "end_date_time": "2023-01-09 20:44:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding in the eastbound lanes of SR 140 near Franklin Rd.", "ts_dict_index": [2523, 2524, 2525]}
+{"event_id": 1064919, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 20:09:00", "end_date_time": "2023-01-09 22:09:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of mud, dirt and rocks on SR 140 just west of Old Rd.", "ts_dict_index": [2571, 2572, 2573]}
+{"event_id": 1064916, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 18:48:00", "end_date_time": "2023-01-10 00:48:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Multiple road slides with heavy rain along Bear Valley Rd. resulted in the road being closed for flooding.", "ts_dict_index": [2580, 2581, 2582]}
+{"event_id": 1064920, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 20:14:00", "end_date_time": "2023-01-09 22:14:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of mud, dirt and rock on the eastbound lane of SR 140 northeast of  Briceburg.", "ts_dict_index": [2547, 2548, 2549]}
+{"event_id": 1064924, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 21:21:00", "end_date_time": "2023-01-09 23:21:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a barn roof washed up onto Hornitos Rd. at High St.", "ts_dict_index": [2559, 2560, 2561]}
+{"event_id": 1064923, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 21:15:00", "end_date_time": "2023-01-09 23:15:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding in the left lane of SR 49 at Smith Rd. in Mariposa.", "ts_dict_index": [2556, 2557, 2558]}
+{"event_id": 1064910, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 19:47:00", "end_date_time": "2023-01-09 21:47:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of an SUV stuck in water with the roadway flooded at the intersection of Childs Ave. and Pico St. in Planada.", "ts_dict_index": [2595, 2596, 2597]}
+{"event_id": 1064915, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 18:25:00", "end_date_time": "2023-01-09 20:25:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a driver stuck in flood waters on the westbound lane of Hornitos Rd. near La Paloma Rd. just west of the Merced River.", "ts_dict_index": [2583, 2584, 2585]}
+{"event_id": 1064540, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 19:35:00", "end_date_time": "2023-01-09 21:35:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of flooding at the intersection of Ave. 80 and Rd. 134.", "ts_dict_index": [2604, 2605, 2606]}
+{"event_id": 1064921, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 20:48:00", "end_date_time": "2023-01-09 22:48:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of flooding with debris at Springhill Grade at SR 49 and Drury Ln.", "ts_dict_index": [2544, 2545, 2546]}
+{"event_id": 1064917, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 19:59:00", "end_date_time": "2023-01-10 01:59:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported Miles Creek was flooding the roadway and SR 140 was closed to the east of the Merced/Mariposa County line.", "ts_dict_index": [2577, 2578, 2579]}
+{"event_id": 1064542, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 19:53:00", "end_date_time": "2023-01-09 21:53:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of flooding at the intersection of Rd. 152 and Ave 120.", "ts_dict_index": [2598, 2599, 2600]}
+{"event_id": 1064913, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 20:48:00", "end_date_time": "2023-01-09 22:48:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. CDF reported that some barns were washed out into the roadway on Merced Falls Rd. in Merced Falls.", "ts_dict_index": [2586, 2587, 2588]}
+{"event_id": 1064909, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 19:18:00", "end_date_time": "2023-01-09 21:18:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public reports of vehicles stuck in water at the intersection of Sutter St. and Stanford Ave. in Planada.", "ts_dict_index": [2550, 2551, 2552]}
+{"event_id": 1064927, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-09 18:41:00", "end_date_time": "2023-01-09 20:41:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding on Rd. 36 just south of Ave. 15 in Madera Ranchos.", "ts_dict_index": [2568, 2569, 2570]}
+{"event_id": 1064925, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 21:34:00", "end_date_time": "2023-01-09 23:34:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding near the auto camp on SR 140 and Colorado Rd.", "ts_dict_index": [2562, 2563, 2564]}
+{"event_id": 1064926, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-09 16:47:00", "end_date_time": "2023-01-09 18:47:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a large concealed pothole on southbound SR 99 just north of Ave. 24 1/2 in Chowchilla.", "ts_dict_index": [2565, 2566, 2567]}
+{"event_id": 1064912, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 20:22:00", "end_date_time": "2023-01-09 22:22:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding under Baker Dr. at SR 140 in Merced.", "ts_dict_index": [2589, 2590, 2591]}
+{"event_id": 1064918, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 20:04:00", "end_date_time": "2023-01-09 22:04:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of mud, dirt and rocks on SR 140 at Trower Rd.", "ts_dict_index": [2574, 2575, 2576]}
+{"event_id": 1064539, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 19:23:00", "end_date_time": "2023-01-09 21:23:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of the roadway flooded and rock and mudslides on eastbound SR 198 near Dinely Rd. and Craig Branch Rd.", "ts_dict_index": [2607, 2608, 2609]}
+{"event_id": 1064911, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 20:06:00", "end_date_time": "2023-01-09 22:06:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of multiple vehicles hitting a concealed pothole just north of the Yosemite Parkway exit on southbound SR 99.", "ts_dict_index": [2592, 2593, 2594]}
+{"event_id": 1068107, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 05:30:00", "end_date_time": "2023-01-10 09:00:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Television station report of several buildings, tractors and other goods were totally destroyed by about 6 feet of floodwater in Strathmore.", "ts_dict_index": [2622, 2623, 2624]}
+{"event_id": 1064498, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-09 15:54:00", "end_date_time": "2023-01-09 17:54:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a traffic collision on Ave. 7 between Rd. 30 and Rd. 31.5. The roadway was flooded and 2 vehicles spun out off the roadway into the field.", "ts_dict_index": [2640, 2641, 2642]}
+{"event_id": 1065326, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 18:08:00", "end_date_time": "2023-01-10 20:08:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding at Athlone Rd. and Doppler Rd.", "ts_dict_index": [2655, 2656, 2657]}
+{"event_id": 1064494, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-09 15:31:00", "end_date_time": "2023-01-09 17:31:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of flooding on the roadway and a vehicle stuck in water on Rd. 22 south of the intersection with Santa Fe Dr. near Sharon.", "ts_dict_index": [2649, 2650, 2651]}
+{"event_id": 1064929, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2023-01-09 17:56:00", "end_date_time": "2023-01-09 19:56:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a washed up tree covering half of Lacey Blvd just west of 8th Ave.", "ts_dict_index": [2658, 2659, 2660]}
+{"event_id": 1064538, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 19:14:00", "end_date_time": "2023-01-09 21:14:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a washed up tree in the roadway with a large branch blocking the eastbound lanes of SR 198 just west of Mehrten Dr.", "ts_dict_index": [2673, 2674, 2675]}
+{"event_id": 1064495, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 15:34:00", "end_date_time": "2023-01-09 17:34:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of multiple rocks in the roadway at the intersection of Kern River Dr. and Burlando Rd. in Kernville.", "ts_dict_index": [2646, 2647, 2648]}
+{"event_id": 1064537, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 19:05:00", "end_date_time": "2023-01-09 21:05:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of large rocks in the roadway on Boyd Dr. east of Orosi.", "ts_dict_index": [2676, 2677, 2678]}
+{"event_id": 1064534, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 16:44:00", "end_date_time": "2023-01-09 18:44:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of flooding on Rd. 38 just south of Ave. 50 in Alpaugh.", "ts_dict_index": [2685, 2686, 2687]}
+{"event_id": 1064536, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 18:31:00", "end_date_time": "2023-01-09 20:31:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report that the road is flooded on the northbound lane on SR 99 just south of the Court St. offramp in Pixley.", "ts_dict_index": [2679, 2680, 2681]}
+{"event_id": 1064535, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 18:11:00", "end_date_time": "2023-01-09 20:11:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a large standing pool of water all the way into the northbound lanes of SR. 99 at the Ave. 152 offramp in Tipton.", "ts_dict_index": [2682, 2683, 2684]}
+{"event_id": 1064922, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 20:48:00", "end_date_time": "2023-01-09 22:48:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding at the at Jones Creek near the intersection of Triangle Rd. and Carter Rd.", "ts_dict_index": [2553, 2554, 2555]}
+{"event_id": 1064928, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2023-01-09 16:27:00", "end_date_time": "2023-01-09 18:27:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report that 12th Ave. is flooded between Kent Ave. and Houston Ave.", "ts_dict_index": [2721, 2722, 2723]}
+{"event_id": 1065176, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-10 08:49:00", "end_date_time": "2023-01-10 10:49:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of mud, dirt and rock washed up at the intersection of Whitlock Rd. and Mosher Rd.", "ts_dict_index": [2730, 2731, 2732]}
+{"event_id": 1063596, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 08:51:00", "end_date_time": "2023-01-09 10:51:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported rocks falling onto SR 140 at Ferguson Slide.", "ts_dict_index": [2751, 2752, 2753]}
+{"event_id": 1065172, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-10 08:22:00", "end_date_time": "2023-01-10 10:22:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of trees blocking 19000 Caliente Creek Rd. just west of Darkside Canyon Rd.", "ts_dict_index": [2733, 2734, 2735]}
+{"event_id": 1065173, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-10 08:23:00", "end_date_time": "2023-01-10 10:23:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding at the intersection of northbound SR 99 and the SR 119 offramp causing vehicles to swerve.", "ts_dict_index": [2736, 2737, 2738]}
+{"event_id": 1063600, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 10:22:00", "end_date_time": "2023-01-09 12:22:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported water has risen over the bridge and is covering the roadway on SR 140 at Yosemite Oaks Dr.", "ts_dict_index": [2763, 2764, 2765]}
+{"event_id": 1064940, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 19:14:00", "end_date_time": "2023-01-09 21:14:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding a the intersection of Taft Hwy. and Panama Rd in Bakersfield.", "ts_dict_index": [2754, 2755, 2756]}
+{"event_id": 1065177, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 09:28:00", "end_date_time": "2023-01-10 11:28:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of Ave. 336 flooded between Rd. 132 and Rd. 140.", "ts_dict_index": [2775, 2776, 2777]}
+{"event_id": 1065170, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 07:51:00", "end_date_time": "2023-01-10 09:51:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding at the intersection of Rd. 212 and Ave. 256.", "ts_dict_index": [2778, 2779, 2780]}
+{"event_id": 1065178, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 09:30:00", "end_date_time": "2023-01-10 11:30:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding on the onramp of southbound SR 99 and W. 16th St. in Merced.", "ts_dict_index": [2781, 2782, 2783]}
+{"event_id": 1064492, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 15:18:00", "end_date_time": "2023-01-09 17:18:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a washed up tree blocking the roadway on Ave. 381 just east of Rd. 154 in Seville.", "ts_dict_index": [2652, 2653, 2654]}
+{"event_id": 1065180, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 09:44:00", "end_date_time": "2023-01-10 11:44:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a tree down on eastbound SR 65 at Spruce Ave.", "ts_dict_index": [2787, 2788, 2789]}
+{"event_id": 1065227, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 10:38:00", "end_date_time": "2023-01-10 12:38:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a downed power pole into a saturated ground near the intersection of Ave. 432 and Rd. 140.", "ts_dict_index": [2802, 2803, 2804]}
+{"event_id": 1065239, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 10:45:00", "end_date_time": "2023-01-10 12:45:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of two vehicles stuck in water at the intersection of Minturn rd. and Buchanan Hollow Rd.", "ts_dict_index": [2805, 2806, 2807]}
+{"event_id": 1065181, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 09:52:00", "end_date_time": "2023-01-10 11:52:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a telephone pole leaning towards the roadway east of the railroad tracks at the intersection of  Ave 424 and Rd. 72.", "ts_dict_index": [2790, 2791, 2792]}
+{"event_id": 1065225, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 10:04:00", "end_date_time": "2023-01-10 12:04:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding near the intersection of Sunny Acres Ave. and Newport Ave.", "ts_dict_index": [2793, 2794, 2795]}
+{"event_id": 1065226, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 10:13:00", "end_date_time": "2023-01-10 12:13:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report roadway flooding at the intersection of Applegate Rd. and Bailey Rd.", "ts_dict_index": [2796, 2797, 2798]}
+{"event_id": 1065447, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 15:00:00", "end_date_time": "2023-01-11 12:00:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Mariposa County Emergency Manager reported debris flow flooding captured in a gabion about 750 feet above El Portal at the west end of Yosemite National Park which threatened nearly all of the residences and buildings in El Portal and prompted the issuance of an evacuation advisory for the area. A Flood Watch had been in effect and  several Flood Advisories had been issued for the Sierra Nevada during the day and evening on January 9.", "ts_dict_index": [2799, 2800, 2801]}
+{"event_id": 1065431, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 12:00:00", "end_date_time": "2023-01-11 12:00:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. The Merced County Emergency Manager reported that several mandatory evacuations took place in Merced County as a result of flooding, The impacted areas included Planada which was completely evacuated as well as portions of Merced. Rainfall amounts in the Merced area were between 2 and 3 inches between noon on January 9 and the early morning of January 10 resulting in several cars being stranded and abandoned in flood waters as SR 99 through Merced and 16th St. in Merced were inundated with flood waters. A Flood Warning was already in place for Bear Creek since January 8 and continued through January 11. Bear Creek overflowed and peaked at a new record crest of 26.2 feet during the morning of January 10. Due to the anticipated severity of this event, resources were deployed to the Merced County EOC during the event with frequent live briefings taking place. In addition the the evacuations the took place in and around Merced, Amtrak cancelled several trains and buses through and into Merced  due to the train station being flooded.", "ts_dict_index": [2811, 2812, 2813]}
+{"event_id": 1063593, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 05:42:00", "end_date_time": "2023-01-09 07:42:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding along SR 99 near Shanks Rd. in Delhi.", "ts_dict_index": [2745, 2746, 2747]}
+{"event_id": 1064954, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 03:09:00", "end_date_time": "2023-01-10 05:09:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding along SR 137 near Rd. 168.", "ts_dict_index": [2838, 2839, 2840]}
+{"event_id": 1064491, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 15:12:00", "end_date_time": "2023-01-09 17:12:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported flooding on N. Fork Dr. near Three Rivers.", "ts_dict_index": [2814, 2815, 2816]}
+{"event_id": 1064952, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 02:13:00", "end_date_time": "2023-01-10 04:13:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding along Rd. 108 at Ave. 368.", "ts_dict_index": [2841, 2842, 2843]}
+{"event_id": 1065169, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-10 07:40:00", "end_date_time": "2023-01-10 09:40:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding on Ave 18 1/2 with vehicles being swept into an orchard.", "ts_dict_index": [2826, 2827, 2828]}
+{"event_id": 1063659, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 14:49:00", "end_date_time": "2023-01-09 16:49:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding on Wade Ave. in Le Grand.", "ts_dict_index": [2820, 2821, 2822]}
+{"event_id": 1064948, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2023-01-10 00:46:00", "end_date_time": "2023-01-10 02:46:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding along SR 43 near Kent Ave.", "ts_dict_index": [2847, 2848, 2849]}
+{"event_id": 1064953, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 03:01:00", "end_date_time": "2023-01-10 05:01:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding along SR 140 near Thornton Rd. in Merced.", "ts_dict_index": [2835, 2836, 2837]}
+{"event_id": 1064950, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 01:06:00", "end_date_time": "2023-01-10 03:06:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding along SR 140 near Plainsburg Rd. in Planada.", "ts_dict_index": [2844, 2845, 2846]}
+{"event_id": 1064934, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 17:40:00", "end_date_time": "2023-01-09 19:40:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of stalled vehicles and 2 feet of standing water with 3 vehicles stuck on Northbound Airport Dr. just south of the Roberts Ln. intersection.", "ts_dict_index": [2829, 2830, 2831]}
+{"event_id": 1064955, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 03:18:00", "end_date_time": "2023-01-10 05:18:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding near the intersection of Ave. 168 and Rd. 166 in Woodville.", "ts_dict_index": [2853, 2854, 2855]}
+{"event_id": 1064938, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 19:00:00", "end_date_time": "2023-01-09 21:00:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of flooding on Southgate Dr. north of Ming Ave.", "ts_dict_index": [2850, 2851, 2852]}
+{"event_id": 1065154, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 07:08:00", "end_date_time": "2023-01-10 09:08:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a car stuck in flood waters just west of the intersection of Ashby Rd. and Miles Ct. in Merced.", "ts_dict_index": [2865, 2866, 2867]}
+{"event_id": 1064947, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 00:28:00", "end_date_time": "2023-01-10 02:28:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding along Sandy Mush Rd. near Gurr Rd.", "ts_dict_index": [2868, 2869, 2870]}
+{"event_id": 1065153, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 07:02:00", "end_date_time": "2023-01-10 09:02:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of tree and branch debris washed up on the offramp to Sierra Ave. off of northbound SR 99 in Earlimart.", "ts_dict_index": [2862, 2863, 2864]}
+{"event_id": 1065152, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-10 07:01:00", "end_date_time": "2023-01-10 09:01:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of mud, dirt and rock washed up at the intersection of SR 140 and Old Highway Rd. in Cathey's Valley.", "ts_dict_index": [2859, 2860, 2861]}
+{"event_id": 1065155, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-10 07:10:00", "end_date_time": "2023-01-10 09:10:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a fallen oak tree on the roadway near the intersection of Ben Hur Rd. and Silver Bar Rd.", "ts_dict_index": [2874, 2875, 2876]}
+{"event_id": 1064936, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 18:41:00", "end_date_time": "2023-01-09 20:41:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding just north of S. Edison Rd and E. Panama Ln.", "ts_dict_index": [2883, 2884, 2885]}
+{"event_id": 1064937, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 18:52:00", "end_date_time": "2023-01-09 20:52:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report that the fast lane is flooded on northbound SR 99 just south of Rosedale Hwy.", "ts_dict_index": [2871, 2872, 2873]}
+{"event_id": 1064935, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 18:22:00", "end_date_time": "2023-01-09 20:22:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of  large amount of rocks on the roadway at the intersection of Burlando Rd. and Kern River Dr.", "ts_dict_index": [2886, 2887, 2888]}
+{"event_id": 1064945, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 22:11:00", "end_date_time": "2023-01-10 00:11:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding along SR 46 near Brown Material Rd.", "ts_dict_index": [2889, 2890, 2891]}
+{"event_id": 1064946, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 22:21:00", "end_date_time": "2023-01-10 00:21:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding along SR 46 near Lost Hills Rd.", "ts_dict_index": [2877, 2878, 2879]}
+{"event_id": 1064943, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 22:16:00", "end_date_time": "2023-01-10 00:16:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report that flooding in the area caused logs to block SR 178. at Elizabeth Norris Rd. near Lake Isabella.", "ts_dict_index": [2898, 2899, 2900]}
+{"event_id": 1064944, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 22:03:00", "end_date_time": "2023-01-10 04:03:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported SR 33 was closed from SR 46 to Lokern Rd. due to flooding.", "ts_dict_index": [2895, 2896, 2897]}
+{"event_id": 1064942, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 20:30:00", "end_date_time": "2023-01-09 22:30:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding at SR 43 and Wasco Ave.", "ts_dict_index": [2901, 2902, 2903]}
+{"event_id": 1063660, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 14:55:00", "end_date_time": "2023-01-09 16:55:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported both lanes of Southern Pacific Ave. at N. Buhach Rd. in Atwater were flooded.", "ts_dict_index": [2817, 2818, 2819]}
+{"event_id": 1063391, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 01:32:00", "end_date_time": "2023-01-09 03:32:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. The California Department of Transportation reported SR 59 was closed from Dickenson Rd. to Sandy Mush Rd. due to flooding.", "ts_dict_index": [2907, 2908, 2909]}
+{"event_id": 1065162, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2023-01-10 07:18:00", "end_date_time": "2023-01-10 09:18:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of power liens down on 14th Ave between Kent Ave. and Jersey Ave.", "ts_dict_index": [2913, 2914, 2915]}
+{"event_id": 1063658, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-09 14:41:00", "end_date_time": "2023-01-09 16:41:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported on SR 99 north of Ave. 17 in Madera.", "ts_dict_index": [2925, 2926, 2927]}
+{"event_id": 1065158, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2023-01-10 07:15:00", "end_date_time": "2023-01-10 09:15:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of downed power lines across the roadway on Grangeville Blvd. near 8 1/2 Ave. in Hanford.", "ts_dict_index": [2910, 2911, 2912]}
+{"event_id": 1064939, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 19:02:00", "end_date_time": "2023-01-09 21:02:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Pubic report of extreme flooding on northbound SR 99 just north of Olive Dr. in Bakersfield.", "ts_dict_index": [2928, 2929, 2930]}
+{"event_id": 1065167, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-10 07:36:00", "end_date_time": "2023-01-10 09:36:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of mud, dirt and rock washed up onto the intersection of E. Evans Rd. and Pinewood Dr. near Lake Isabella.", "ts_dict_index": [2922, 2923, 2924]}
+{"event_id": 1065240, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 11:07:00", "end_date_time": "2023-01-10 13:07:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a road closure of Ave 368 due to flooding at the intersection at Rd. 108.", "ts_dict_index": [2937, 2938, 2939]}
+{"event_id": 1063613, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-09 12:37:00", "end_date_time": "2023-01-09 14:37:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported flooding at the intersection of SR 41 and SR 145.", "ts_dict_index": [2934, 2935, 2936]}
+{"event_id": 1063615, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-09 12:44:00", "end_date_time": "2023-01-09 14:44:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported flooding on Rd. 274 at Beasore Rd. near the Pine Resort at Bass Lake.", "ts_dict_index": [2943, 2944, 2945]}
+{"event_id": 1065179, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 09:43:00", "end_date_time": "2023-01-10 11:43:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding at the intersection of Plainsburg Rd. and Buchannan Hollow Rd. with vehicles sliding across the road.", "ts_dict_index": [2784, 2785, 2786]}
+{"event_id": 1065266, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 15:15:00", "end_date_time": "2023-01-10 17:15:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported flooding in the roadway at the intersection of Ave 250 and Rd. 216 due to debris blocking Culvert.", "ts_dict_index": [2946, 2947, 2948]}
+{"event_id": 1065265, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 15:14:00", "end_date_time": "2023-01-10 17:14:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a lot of debris backing up and covering the roadway at the intersection of SR 63 and Ave. 412 in Orosi.", "ts_dict_index": [2949, 2950, 2951]}
+{"event_id": 1065264, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 14:44:00", "end_date_time": "2023-01-10 16:44:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported one lane flooded on Indian Reservation Rd.", "ts_dict_index": [2958, 2959, 2960]}
+{"event_id": 1063620, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 13:05:00", "end_date_time": "2023-01-09 17:05:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported Snelling Rd. was closed between Franklin and Fox due to flooding.", "ts_dict_index": [2952, 2953, 2954]}
+{"event_id": 1065261, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-10 14:41:00", "end_date_time": "2023-01-10 20:41:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of large boulders blocking traffic and covering both lanes on SR 178.", "ts_dict_index": [2961, 2962, 2963]}
+{"event_id": 1065328, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 19:10:00", "end_date_time": "2023-01-10 21:10:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding at the intersection of Hatch Rd. and E. Yosemite Ave.", "ts_dict_index": [2964, 2965, 2966]}
+{"event_id": 1064941, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 19:18:00", "end_date_time": "2023-01-09 21:18:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of a rockslide blocking half of the eastbound lane near MM 33 and a large boulder at MM 25 on SR 178.", "ts_dict_index": [2904, 2905, 2906]}
+{"event_id": 1065338, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 19:22:00", "end_date_time": "2023-01-10 21:22:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding on SR 198 at the intersection of Ave. 330. in Lemoncove.", "ts_dict_index": [2967, 2968, 2969]}
+{"event_id": 1065346, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-11 10:58:00", "end_date_time": "2023-01-11 12:58:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of Washington Rd. washed out between Short Ave. and Johnson Ave.", "ts_dict_index": [3000, 3001, 3002]}
+{"event_id": 1063617, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 12:58:00", "end_date_time": "2023-01-09 16:58:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported a road closure of SR 190 in Camp Nelson at Tule River Bridge due to flooding.", "ts_dict_index": [2973, 2974, 2975]}
+{"event_id": 1065307, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-10 17:18:00", "end_date_time": "2023-01-10 23:18:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported the intersection of Ave. 17 1/2 and Rd. 18 completely washed out.", "ts_dict_index": [3018, 3019, 3020]}
+{"event_id": 1063624, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-09 13:28:00", "end_date_time": "2023-01-09 15:28:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported flooding on the railroad tracks and the roadway of Santa Fe Ave. in Le Grand.", "ts_dict_index": [3006, 3007, 3008]}
+{"event_id": 1065341, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 22:28:00", "end_date_time": "2023-01-11 00:28:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding on Doppler Rd. at Athlone Rd.", "ts_dict_index": [2985, 2986, 2987]}
+{"event_id": 1064930, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2023-01-09 17:31:00", "end_date_time": "2023-01-09 19:31:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding at the intersection of Excelsior Ave. and Ave. 22.", "ts_dict_index": [2997, 2998, 2999]}
+{"event_id": 1065430, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 05:00:00", "end_date_time": "2023-01-10 09:00:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. The Tulare County Emergency Manager reported that the eastern portion of town of Strathmore was inundated by rapidly rising flood waters with over 40 homes impacted with water ranging from several inches to several feet deep.", "ts_dict_index": [3012, 3013, 3014]}
+{"event_id": 1063623, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 13:16:00", "end_date_time": "2023-01-09 15:16:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported the bridge flooded on N. Fork Dr. near SR 198.", "ts_dict_index": [3003, 3004, 3005]}
+{"event_id": 1065309, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 17:35:00", "end_date_time": "2023-01-10 19:35:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding on Ferguson Dr. at Flynn Dr. in Camp Nelson.", "ts_dict_index": [3015, 3016, 3017]}
+{"event_id": 1065244, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 14:15:00", "end_date_time": "2023-01-10 16:15:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported a large sinkhole on southbound I-5 just  north of the  scales near Santa Nella.", "ts_dict_index": [2979, 2980, 2981]}
+{"event_id": 1064933, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 17:28:00", "end_date_time": "2023-01-09 19:28:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of roadway flooding at the intersection of Rosedale Hwy. and Calloway Dr. in Bakersfield.", "ts_dict_index": [3009, 3010, 3011]}
+{"event_id": 1065241, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-10 11:15:00", "end_date_time": "2023-01-10 13:15:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report of mud, dirt and rocks flowing onto the intersection of SR 178 and Democrat Rd.", "ts_dict_index": [2994, 2995, 2996]}
+{"event_id": 1064932, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-09 16:54:00", "end_date_time": "2023-01-09 18:54:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public report that Airport Rd was flooded at the intersection of Roberts Ln.", "ts_dict_index": [2991, 2992, 2993]}
+{"event_id": 1065429, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 05:00:00", "end_date_time": "2023-01-10 09:00:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. The Tulare County Emergency Manager reported that the town of Three Rivers was trapped behind flood waters moving over the egress route. This resulted in several emergency response personnel being trapped behind the flood waters who were in place to limit flood waters impact on structures.", "ts_dict_index": [3021, 3022, 3023]}
+{"event_id": 1065428, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 05:30:00", "end_date_time": "2023-01-10 09:00:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. The Tulare County Emergency Manager reported that flooding from heavy rainfall resulted in a large eucalyptus tree falling on northbound SR 99 causing a multi-car chain reaction crash at the intersection of SR 99 and Betty Dr. in Goshen which caused one fatality. The fallen tree also killed an individual who was riding a motorcycle and hit the tree.", "ts_dict_index": [3024, 3025, 3026]}
+{"event_id": 1065351, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-11 14:11:00", "end_date_time": "2023-01-11 16:11:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding at the intersection of Plainsburg Rd. and Buchanan Hollow Rd.", "ts_dict_index": [3030, 3031, 3032]}
+{"event_id": 1063656, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 14:23:00", "end_date_time": "2023-01-09 16:23:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding on Rd. 142 near Orosi.", "ts_dict_index": [3042, 3043, 3044]}
+{"event_id": 1063627, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-09 13:51:00", "end_date_time": "2023-01-09 15:51:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported flooding on S. Fork Dr.  at Heidi Dr. in Three Rivers.", "ts_dict_index": [3039, 3040, 3041]}
+{"event_id": 1063606, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 11:04:00", "end_date_time": "2023-01-09 13:04:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding on SR 140 near Chase Ranch.", "ts_dict_index": [3054, 3055, 3056]}
+{"event_id": 1063608, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-09 11:36:00", "end_date_time": "2023-01-09 13:36:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported a flood caused a closure of Ave. 13 between Rd. 29 and Rd. 30 in Madera. A nearby creek overflowed and took out a portion of the roadway of Ave. 13.", "ts_dict_index": [3060, 3061, 3062]}
+{"event_id": 1063605, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-09 10:55:00", "end_date_time": "2023-01-09 12:55:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported water running down an embankment onto the roadway of SR 41 near Yosemite Lakes.", "ts_dict_index": [3051, 3052, 3053]}
+{"event_id": 854914, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2019-06-25 04:00:00", "end_date_time": "2019-06-29 11:00:00", "narrative": "Just 367 days after the last of the Great June Flood of 2018 had left its memorable mark on nearly all of the populated Rio Grande Valley, a confluence of atmospheric events came together during the late afternoon and evening of June 24th, 2019, to produce another memorable - and unfortunate - situation for parts of the Rio Grande Valley. This time, the impacted area was smaller and less populated but the results the same. For most of Willacy County's population, the western third of Cameron, and a corner of eastern Hidalgo, significant impacts were noted.  These included:||Over a foot of rain fell in about six hours, including a peak total of more than 15 inches near Santa Rosa (Cameron/Hidalgo line); hundreds of streets flooded, including 30 Texas-managed highways; 1,188 homes were considered destroyed or incurring major damage requiring significant repairs, with an additional 182 homes sustaining minor damage or mildly affected (as of July 10).  Individual Assistance (IA) costs were estimated at $27.6 million. Public Assistance (PA) costs were likely over $5 million, but totals were not available as of this writing. Total damage was likely to range from $50 to $100 million or more when all estimates have been received, and final estimated may not be known until late 2019.||More than 100 persons were evacuated to safe high ground from dozens of homes threatened by 2 or more feet of water in several locations in each county.  At least 45,000 private and public utility power customers were without power at the peak of the storm, and estimated 65 to 75 mph winds caused at least five poorly built mobile homes to be rolled or demolished in eastern Hidalgo County.  Lightning struck a wind turbine and set it ablaze in Willacy County, costing an estimated $5 million in damage.|New daily rainfall records were set at most available Rio Grande Valley climate recording locations. These totals ranged from 2.06 inches in Brownsville to 15.20 inches in Santa Rosa. Slow drainage of torrential rains of 6 to 15 inches in just six hours during the evening of June 24th through just after midnight on June 25th maintained widespread flooding of 1 to as much as 3 feet of water depth across many neighborhoods and roads in the eastern portion of the Rio Grande Valley. Hundreds of roads remained closed or impassible, and hundreds to more than a thousand homes continued to have some water in them for several (mainly fair weather days) following the causative event. Water did not recede completely in some neighborhoods until up to 2 weeks following the rains, much due to the interconnected drainage system which was unable to handle the rainfall rate, which was a 1 in 500 probability event occurring in locations only built to sustain 1 in 5 or 1 in 10 probability events. ||Please note: Damage listed here is shown as *zero*. Estimated total damage for this event is listed in the flash flood entries for these locations.", "ts_dict_index": [3072, 3073, 3074]}
+{"event_id": 1063602, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-09 10:39:00", "end_date_time": "2023-01-09 12:39:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported rockslides onto SR 140 at Triangle Rd.", "ts_dict_index": [3048, 3049, 3050]}
+{"event_id": 938491, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2021-02-28 21:50:00", "end_date_time": "2021-02-28 23:59:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Highway 1812 closed in the Vancleve community due to high water.", "ts_dict_index": [3075, 3076, 3077]}
+{"event_id": 938493, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2021-02-28 21:54:00", "end_date_time": "2021-02-28 23:59:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Water is covering the road at mile marker 1 on Hwy 315 east of Morris Fork.", "ts_dict_index": [3084, 3085, 3086]}
+{"event_id": 938218, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2021-02-28 17:00:00", "end_date_time": "2021-02-28 23:59:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Flooding of roads and low lying areas was reported in the Clover Bottom area. No specifics were given.", "ts_dict_index": [3078, 3079, 3080]}
+{"event_id": 938533, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-02-27 09:48:00", "end_date_time": "2021-02-27 17:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Flood waters were reported to be over KY-1085 in the community of Wayland.", "ts_dict_index": [3081, 3082, 3083]}
+{"event_id": 938539, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-02-27 11:51:00", "end_date_time": "2021-02-27 17:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Broadcast media had a picture shared on social media from the public, showing flooding across a road in the community of Estill and up to the edge of a home. The exact road is unknown.", "ts_dict_index": [3087, 3088, 3089]}
+{"event_id": 938247, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-02-28 19:46:00", "end_date_time": "2021-02-28 23:59:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Middle Creek is flooded and continuing to rise in the Dotson community, encompassing yards and low lying areas along the creek.", "ts_dict_index": [3090, 3091, 3092]}
+{"event_id": 1065340, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-10 22:21:00", "end_date_time": "2023-01-11 00:21:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported roadway flooding on S. Arboleda Dr. at E. Mission Ave.", "ts_dict_index": [2988, 2989, 2990]}
+{"event_id": 938520, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2021-02-27 08:35:00", "end_date_time": "2021-02-27 17:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. At mile marker 2 on Hwy 1098, water is across one lane. Also about 2.5 miles on Hwy 1098, both lanes are impassable.", "ts_dict_index": [3102, 3103, 3104]}
+{"event_id": 941676, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2021-03-01 12:35:00", "end_date_time": "2021-03-02 07:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Water is over several portions of Quicksand Road in Jackson. Numerous homes and property are surrounded by or inundated with water, on both sides of the Kentucky River.", "ts_dict_index": [3111, 3112, 3113]}
+{"event_id": 938909, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Pictures on social media show Riverside Christian School flooded. Water rescues had to take place for residents.", "ts_dict_index": [3129, 3130, 3131]}
+{"event_id": 941664, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2021-03-01 11:00:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Several homes were reported having been flooded along the Kentucky River on KY-541 near the community of Lawson.", "ts_dict_index": [3108, 3109, 3110]}
+{"event_id": 941677, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2021-03-01 12:40:00", "end_date_time": "2021-03-02 07:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Park Road, including Kiwanis and Douthitt Parks in Jackson, is inundated with water from the Kentucky River.", "ts_dict_index": [3135, 3136, 3137]}
+{"event_id": 938492, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Hwy 1812 is closed on the Vancleve community due to high water.", "ts_dict_index": [3132, 3133, 3134]}
+{"event_id": 938933, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Route 194 is blocked due to high water across the road near German Bridge Campground.", "ts_dict_index": [3114, 3115, 3116]}
+{"event_id": 938931, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. KY-7 is blocked in several spots near the Lackey and Wayland communities due to high water over the road.", "ts_dict_index": [3138, 3139, 3140]}
+{"event_id": 938223, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2021-02-28 17:20:00", "end_date_time": "2021-02-28 23:59:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Moderate flooding was reported in the low lying areas along Horse Lick Creek.", "ts_dict_index": [3105, 3106, 3107]}
+{"event_id": 938228, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-02-28 17:40:00", "end_date_time": "2021-02-28 19:45:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. KY 1427 (Abbott Creek Rd) about 3 miles west of U.S. 23 was impassable with 2.5 to 3 feet of water estimated to be flowing over it. A vehicle was stranded in the flood waters in this location. This is a very flood prone area.", "ts_dict_index": [3099, 3100, 3101]}
+{"event_id": 938958, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. KY-979 is blocked due to high water across the road near the Mud Creek Clinic just south of Grethel.", "ts_dict_index": [3126, 3127, 3128]}
+{"event_id": 938961, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. KY-1210 is blocked due to high water across the road near Stephen's Branch.", "ts_dict_index": [3117, 3118, 3119]}
+{"event_id": 938925, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Route 122 is blocked due to high water across the road near Hall Funeral Home.", "ts_dict_index": [3123, 3124, 3125]}
+{"event_id": 941675, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2021-03-01 12:33:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. The intersection of KY Highways 577 and 3630 are covered by high water.", "ts_dict_index": [3120, 3121, 3122]}
+{"event_id": 1065347, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-11 14:04:00", "end_date_time": "2023-01-11 16:04:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. California Highway Patrol reported reported roadway flooding on Turner Island Rd. at Henry Miller Ave.", "ts_dict_index": [3045, 3046, 3047]}
+{"event_id": 938930, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. KY-404 is blocked due to high water across the road near the community of David.", "ts_dict_index": [3141, 3142, 3143]}
+{"event_id": 938956, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. KY-777 is blocked due to high water across the road along Turkey Creek.", "ts_dict_index": [3150, 3151, 3152]}
+{"event_id": 941674, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 11:55:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Evacuations and high-water rescues are ongoing in the community of Garrett.", "ts_dict_index": [3147, 3148, 3149]}
+{"event_id": 938289, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-02-28 20:22:00", "end_date_time": "2021-02-28 23:59:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Spotter reported 5 feet of water now over KY 1427 (Abbott Creek Rd) just west of Prestonsburg. Water was also continuing to rise.", "ts_dict_index": [3093, 3094, 3095]}
+{"event_id": 938494, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "BREATHITT", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Water is covering the road at mile marker 1 on Hwy 315 east of Morris Fork.", "ts_dict_index": [3165, 3166, 3167]}
+{"event_id": 938921, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Route 1427 is blocked at several spots due to high water across the road near Abbott Creek.", "ts_dict_index": [3153, 3154, 3155]}
+{"event_id": 938922, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Ky-1426 is blocked due to high water across the road near Tanyard Hollow (Branch) and Little Mud Creek.", "ts_dict_index": [3159, 3160, 3161]}
+{"event_id": 938551, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. The flooding of low lying areas continues in the community of Clover Bottom. Water is rising, having gone up a few feet in the last 2 hours. There is now at least 1 to 2 feet over a roadway in the community (roadway unspecified).", "ts_dict_index": [3162, 3163, 3164]}
+{"event_id": 938929, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 05:30:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Route 122 is blocked near the Dollar General store due to high water over the road between Hi Hat and Wheelright Junction.", "ts_dict_index": [3156, 3157, 3158]}
+{"event_id": 938552, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Middle Creek is flooded and continuing to rise in the Dotson community, encompassing yards and low lying areas along the creek.", "ts_dict_index": [3171, 3172, 3173]}
+{"event_id": 938549, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. KY 1427 (Abbott Creek Rd) about 3 miles west of U.S. 23 was impassable with 2.5 to 3 feet of water estimated to be flowing over it. A vehicle was stranded in the flood waters in this location. This is a very flood prone area.", "ts_dict_index": [3174, 3175, 3176]}
+{"event_id": 938547, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Flooding of roads and low lying areas was reported in the Clover Bottom area. No specifics were given.", "ts_dict_index": [3168, 3169, 3170]}
+{"event_id": 938548, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Moderate flooding was reported in the low lying areas along Horse Lick Creek.", "ts_dict_index": [3177, 3178, 3179]}
+{"event_id": 938550, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2021-02-28 19:00:00", "end_date_time": "2021-02-28 23:59:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date. ||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. The flooding of low lying areas continues in the community of Clover Bottom. Water is rising, having gone up a few feet in the last 2 hours. There is now at least 1 to 2 feet over a roadway in the community (roadway unspecified).", "ts_dict_index": [3096, 3097, 3098]}
+{"event_id": 930587, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2021-01-28 17:36:00", "end_date_time": "2021-01-28 19:36:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. California Highway Patrol reported roadway flooding due to heavy rain near the intersection of Ave. 228 and Rd. 130 east of Tulare.", "ts_dict_index": [3183, 3184, 3185]}
+{"event_id": 930787, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2021-01-29 05:23:00", "end_date_time": "2021-01-29 09:23:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. California Highway Patrol reported a portion of Road 204 near Woodlake compeltely flooded.", "ts_dict_index": [3222, 3223, 3224]}
+{"event_id": 930580, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2021-01-28 16:04:00", "end_date_time": "2021-01-28 18:04:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. California Highway Patrol reported roadway flooding due to heavy rain on Vinewood Ave. in Livingston.", "ts_dict_index": [3216, 3217, 3218]}
+{"event_id": 930576, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2021-01-28 08:30:00", "end_date_time": "2021-01-28 09:30:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. California Highway Patrol reported lane #1 on SR 99 in Madera was closed to pump out ponding water.", "ts_dict_index": [3219, 3220, 3221]}
+{"event_id": 930582, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2021-01-28 16:06:00", "end_date_time": "2021-01-28 18:06:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. The Madera County Sheriffs Office reported roadway flooding due to heavy rain on Daley Rd. in Madera.", "ts_dict_index": [3207, 3208, 3209]}
+{"event_id": 930572, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2021-01-27 08:55:00", "end_date_time": "2021-01-27 12:55:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. California Highway Patrol reported roadway flooding due to heavy rain at the intersection of SR 41 and SR 33 near Kettleman City.", "ts_dict_index": [3201, 3202, 3203]}
+{"event_id": 930590, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2021-01-28 18:42:00", "end_date_time": "2021-01-28 20:42:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. California Highway Patrol reported roadway flooding due to heavy rain at the intersection of E. Nebraska Ave. and Rd. 100 near Sultana.", "ts_dict_index": [3243, 3244, 3245]}
+{"event_id": 930573, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2021-01-27 16:45:00", "end_date_time": "2021-01-27 18:45:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. California Highway Patrol reported roadway flooding due to heavy rain at the intersection of SR 165 and Mervel Ave. near Los Banos which caused several vehicles to hydroplane.", "ts_dict_index": [3237, 3238, 3239]}
+{"event_id": 930575, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2021-01-28 02:57:00", "end_date_time": "2021-01-28 04:57:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. California Highway Patrol reported roadway flooding due to heavy rain at the intersection of SR 33 and SR 140 in Gustine.", "ts_dict_index": [3228, 3229, 3230]}
+{"event_id": 930574, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2021-01-27 21:18:00", "end_date_time": "2021-01-27 23:18:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. California Highway Patrol reported roadway flooding due to heavy rain at the intersection of Shaffer Rd. and Eucalyptus Ave. near Atwater.", "ts_dict_index": [3234, 3235, 3236]}
+{"event_id": 1101949, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 07:00:00", "end_date_time": "2023-05-01 12:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Flooding along the Sandy River between Phillips and Strong caused numerous road closures including parts of Route 4 and River Road. Hardest hit was in Avon where backwater along a brook paralleling the Avon Valley Road flooded a home.", "ts_dict_index": [3246, 3247, 3248]}
+{"event_id": 1102143, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:00:00", "end_date_time": "2023-05-01 11:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Hardscrabble Road closed due to flooding.", "ts_dict_index": [3249, 3250, 3251]}
+{"event_id": 930591, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2021-01-28 19:20:00", "end_date_time": "2021-01-28 21:20:00", "narrative": "A very potent storm system brought heavy precipitation, areas of flooding and damaging winds to the area as it moved through central California between the early morning of January 27 and the morning of January 29. As the storm approached the northern California coast on January 27, strong southeast winds picked up in the Fort Tejon area in the Tehachapi Mountains and along the West Side Hills. For much of the day on the 27th winds were gusting above 45 mph with several stations reporting peak gusts exceeding 60 mph. The winds caused several local power outages. There were also several winds gusts between 45 and 60 mph in the Sierra Nevada which had been impacted just 8 days before by a very strong offshore wind event. This resulted in even more trees being blown down. As the large upper low approached central California, it pulled up a surge of deep moisture which provided for a period of heavy precipitation across much of the area between the evening of January 27 and the morning of January 29. Several stations in the Sierra foothills picked up between 4 and 7 inches of rain while several stations in the San Joaquin Valley from Fresno County northward picked up between 2.5 and 4 inches of rainfall with this system. Further south in the valley several stations in Kings and Tulare Counties picked up between 1 and 2.5 inches of rain while much of the valley portion of Kern County picked up between a half inch and an inch of rain. There were several reports of roadway flooding in the San Joaquin Valley and mudslides and debris flows were reported in the West Side Hills near the Mineral Fire burn area. The storm also brought heavy snowfall to the Sierra Nevada where several stations above 7000 feet picked up between 4 and 6 feet of new snowfall. The snow also restricted travel across the Sierra Nevada and closed several roads. The storm moved through central California on January 28 and 29 and moved out of the area by the afternoon of January 29. California Highway Patrol reported roadway flooding due to heavy rain on southbound SR 99 just north of the Houghton Rd. junction south of Bakersfield.", "ts_dict_index": [3240, 3241, 3242]}
+{"event_id": 1102142, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:00:00", "end_date_time": "2023-05-01 10:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Greenwood Road impassable due to flooding.", "ts_dict_index": [3252, 3253, 3254]}
+{"event_id": 938553, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 16:00:00", "narrative": "Several rounds of heavy rain moved across eastern Kentucky from late Friday, February 26th through early Monday, March 1st.  The combination of all the heavy rainfall led to significant flooding across a good portion of central and east Kentucky.  For some areas, this was the most significant flooding in the last 50 to 60 years, or more. FEMA estimates that this event cost $350-400 million dollars in damages, including both individual and public infrastructure. This is now the costliest event in Kentucky to date.||The first round of heavy rain came through on the morning of Saturday, February 27th.  This early rainfall targeted areas along the Hal Rogers Parkway, including Laurel, Clay, Perry, and Knott counties. Flash flooding let to some closed roads for a short time in these areas.  ||The second round of rainfall occurred late Saturday night as a warm front lifted northward across east Kentucky. The heavy rain stalled out over portions of Powell and Menifee Counties, leading to flash flooding into the early morning hours of Sunday.||Finally, the third round of heavy rain started late Sunday afternoon and continued through Sunday night. Given that much of the area had already received significant amounts of rain from the past two events, the ground was very saturated, and this last round caused widespread flash flooding across much of east Kentucky. As water made it's way to the larger creeks and rivers, these began to flood as well. River levels on the Kentucky river were some of the highest readings ever recorded, namely at Booneville and Ravenna. Clay City, Heidelberg, Jackson, Paintsville, and Salyersville also saw significant river flooding of which hadn't been seen in 40 to 50 years.  ||The periods of heavy rain and flooding led to numerous water rescues and mud/rock slides.  Many areas were cut off or blocked due to the flooding.  Power outages were also noted and reached as high as 12,000 during the peak of the flash flooding Sunday night. Spotter reported 5 feet of water now over KY 1427 (Abbott Creek Rd) just west of Prestonsburg. Water was also continuing to rise.", "ts_dict_index": [3144, 3145, 3146]}
+{"event_id": 1101909, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 01:00:00", "end_date_time": "2023-05-01 18:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Heavy rain caused the Swift River to come out of banks and flood portions of Byron and Roxbury. The river came out of banks during the early morning hours which caused the closure of Maine Route 17, that resulted in significant disruption to travel in and out of the area. The river crested at 10.8 feet by early afternoon, which is 3.8 feet above flood stage.", "ts_dict_index": [3261, 3262, 3263]}
+{"event_id": 1102121, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 07:13:00", "end_date_time": "2023-05-01 10:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Interval Road flooded in Temple.", "ts_dict_index": [3264, 3265, 3266]}
+{"event_id": 1102150, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-05-01 07:00:00", "end_date_time": "2023-05-02 02:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. The Androscoggin River reached flood stage during the morning of May 1. Flood waters out of Gorham flooded areas from Gilead, to extensive flooding in Bethel and Rumford. Flooding started at North Road in Gilead, followed by Route 26 in Bethel between Cross Street and Intervale Road. In Rumford, South Rumford Road flooded.  Low spots flood along the Swift and Androscoggin Rivers in Mexico and Rumford flooded including parks and boat launches. The USGS river gage in Rumford crested at 15.76 feet, less than a foot above flood stage.", "ts_dict_index": [3258, 3259, 3260]}
+{"event_id": 1102120, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 06:18:00", "end_date_time": "2023-05-01 10:18:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Route 41 flooded in Farmington.", "ts_dict_index": [3255, 3256, 3257]}
+{"event_id": 1102119, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 07:13:00", "end_date_time": "2023-05-01 11:13:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. A portion of Main Street flooded.", "ts_dict_index": [3282, 3283, 3284]}
+{"event_id": 1102134, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 07:15:00", "end_date_time": "2023-05-01 11:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Flooding on Route 27 and 234 in New Vineyard.", "ts_dict_index": [3276, 3277, 3278]}
+{"event_id": 1124131, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2023-07-11 00:00:00", "end_date_time": "2023-07-12 00:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. The Saco River came out of banks on July 11th following heavy rain showers. The USGS river gage at Conway exceeded the flood stage of 9 feet, cresting at 9.4 feet on the 11th. The impacts were mainly focused at low lying campgrounds and flooding at Transvale Road.", "ts_dict_index": [3300, 3301, 3302]}
+{"event_id": 1102138, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 09:10:00", "end_date_time": "2023-05-01 14:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. West Kingfield Road closed after the West Branch of the Carrabasset River flooded.", "ts_dict_index": [3288, 3289, 3290]}
+{"event_id": 1101919, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 06:00:00", "end_date_time": "2023-05-01 12:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. The headwaters of the Sandy River came out of banks and flooded the basements and garages of homes in Phillips and closed Route 142 and 149. Additional roads that flooded were Bray Hill Road, East Madrid Road, Weld Road, Bridge Street, Salem Road near Auger Drive, #6 road. The USGS river gage at Madrid indicated the river crested at 10.64 feet, which was just below the highest peak on record for this short period of record gauge. In Madrid Township River Road flooded.", "ts_dict_index": [3270, 3271, 3272]}
+{"event_id": 1102137, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 08:44:00", "end_date_time": "2023-05-01 11:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Norton Hill Road flooded and closed.", "ts_dict_index": [3285, 3286, 3287]}
+{"event_id": 1102043, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 08:00:00", "end_date_time": "2023-05-01 12:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. The Carrabassett River rose 7 feet above flood stage on May 1 after 3 to 4 inches of rain fell over the watershed. The river crested at 22.08 feet in the early afternoon, reaching the 2nd highest flow since the flood of April 1987. Floodwaters washout Island Road cutting off residential properties.", "ts_dict_index": [3291, 3292, 3293]}
+{"event_id": 1151063, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-12-18 12:00:00", "end_date_time": "2023-12-19 00:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. After heavy rain and snowmelt, the main thruway to Rangeley, ME Route 17 north of Height of Land was flooded in numerous locations.", "ts_dict_index": [3333, 3334, 3335]}
+{"event_id": 1151033, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-12-18 12:00:00", "end_date_time": "2023-12-19 00:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Record flooding was reached on Spencer Stream near Grand Falls, Maine. The river crested at 11.4 feet during the early morning of December 19th. The information is based on the USGS river gage that was installed in 2000.  The streamflows were measured over 12,000 cfs comparable to a 0.2% annual chance exceedance event, otherwise referred to as a 500 year flood. The flooding was the result of approximately 5 inches of rainfall and another 1 to 2 inches of snowmelt runoff, all of which occurred within 18 hours.", "ts_dict_index": [3339, 3340, 3341]}
+{"event_id": 1151022, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-12-18 09:00:00", "end_date_time": "2023-12-19 06:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Near record flooding occurred on the Sandy River following a heavy rain and snowmelt event on the 18th. The rainfall across the headwaters of the Sandy was estimated between 5 and 6 inches, but it was the combination of this and an additional 3 inches of snowmelt runoff that caused the catastrophic flooding. The USGS river gage reached a stage of 12.79 feet on the late afternoon of the 18th, with a measured streamflow over 10 kcfs. The streamflows measured surpassed a 0.2% annual chance exceedance flood, otherwise referred to as a 500-year flood. The river rise went from 5 feet at midnight to over 12 feet by the early afternoon, breaking the previous record set after the remnants of Irene in 2011. The most significant impacts occurred in Farmington where several homes and businesses were flooded. Of particular severity were businesses along Front Street and Main Street where the water depth was chest deep. The confluence of the Temple Stream and Sandy River resulted in additional business and residential flooding necessitating evacuations and some destruction of property with flood waters up to 4 feet deep.  Further downriver, into Farmington Falls, several homes were damaged and a new bridge construction was overtopped and damaged.  Routes 2 and 41 were flooded and closed.  The river washed out the Route 145 bridge in Strong.  Route 4 was flooded in several locations between Sandy River Plantation and Farmington, cutting off the major thruway in the region.  Numerous roads in Phillips were flooded or blocked off to include Ross Ave, Smiths East Madrid Road and the Number Six Road.  Emergency officials declared Farmington 'essentially completely flooded' with all roads closed and issued a do not travel advisory for the region.", "ts_dict_index": [3303, 3304, 3305]}
+{"event_id": 1102124, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 07:15:00", "end_date_time": "2023-05-01 09:50:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Manor Road flooded in Rangeley.", "ts_dict_index": [3267, 3268, 3269]}
+{"event_id": 1102132, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 07:00:00", "end_date_time": "2023-05-01 10:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Bray Bill Road flooded in Wilton/Salem.", "ts_dict_index": [3273, 3274, 3275]}
+{"event_id": 1152139, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-12-18 15:00:00", "end_date_time": "2023-12-19 02:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. The Sandy River reached major flood level on the afternoon of December 18th. The river crested at a stage of 17.35 feet which was the 3rd highest crest ever recorded. The flooding was most severe in the headwaters between Sandy River Plantation and Farmington where bridges were washed out and homes were inundated. Between Farmington Falls and Madison the flooding was widespread. Several homes in New Sharon were flooded along Route 134. Main thruways in the area were cut off including Route 2 which flooded in multiple locations including the New Sharon bridge. Route 134 north of the river flooded into Beans Corner Road and Glenn Harris Roads. On the south side of the river, several local roads flooded including Flagg Road, Starks Road, and West Dandy River Road. Multiple homes were surrounded with basement and minor first floor flooding, particularly in Farmington Falls.  Further downstream in Norridgewock, the Sandy River Road flooded.", "ts_dict_index": [3309, 3310, 3311]}
+{"event_id": 1101931, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-05-01 07:00:00", "end_date_time": "2023-05-01 14:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday, April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday, April 30th through Monday, May 1st. Widespread heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and vegetation still being dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd.  Public infrastructure impacts were widespread for the event with over $4.2 million in damage.  Oxford and Androscoggin Counties reported the most monetary damage to roads for the event.  ||Another aspect of the system was a period of strong gusty winds Sunday night that started along the coastline and extended inland causing localized power outages and tree damage. Wind gusts of 50 mph were recorded at the Portland Jetport, and gusts to near 50 mph were also recorded inland.  Strongest wind gusts up to 65 mph were reported across the Mid-coast region.  Power outages were reported due to a few downed trees and numerous snapped tree limbs. Floodwaters from the Sandy River combined with local runoff from the Beaver Brook in Farmington to cause significant flooding along Main Street by the Hippach Field as well as Front Street. Floodwaters inundated Abbott Park with water several feet deep. Businesses on Main Street had floodwaters of a few inches deep within their first floors. The USGS river gage in Madrid crested at a stage of 10.6 feet and the Mercer gage crested at 14.62 feet, both 2 to 4 feet above flood stage. The high flows on the Sandy River resulted in backwater along the Temple Stream which flooded a business off Route 2 & 4 in Farmington.", "ts_dict_index": [3279, 3280, 3281]}
+{"event_id": 1151025, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 14:00:00", "end_date_time": "2023-12-20 14:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Catastrophic flooding on the Androscoggin River resulting from 5 to 6 inches of rainfall and 2 to 3 inches of snowmelt. The river rose 17��� in roughly 12 hours, cresting at 22.1 feet.  The record is 24��� set in 1936. Access in and out of the region was cut off for days, including both Route 2 and 108 running on either side of the river. The Flooding started upstream in Gorham, reaching major severity in Bethel and continuing through Rumford and downstream through Mexico, Canton, Peru, Dixfield, Jay, and Livermore Falls. The flood severity was impacted by record flooding from the Ellis and Swift River tributaries from the north. Numerous swift water rescues were needed to move trapped residents and motorists to safety.  On the evening of the 18th a vehicle was swept up by the Swift River off of Main Street and deposited into the Androscoggin River. Water rescues saved two of the passengers, but the driver and another passenger perished and were recovered a few days later. Floodwaters moved a house off its foundation on Prospect Avenue in Rumford. Water was up to street signs along Route 140 from Dixfield, Canton, to Jay. In Mexico numerous buildings flooded along Main Street, and properties off Canton Point Road in Peru. In Canton the flood waters entered buildings along Pleasant Street. The cost of the damage to roads and infrastructure was estimated at $2 million. There was at least home was destroyed and another 20-30 damaged by flood water with a total cost estimated around $2 million. About 2 dozen businesses between Rumford and Livermore sustained major flood damage.", "ts_dict_index": [3324, 3325, 3326]}
+{"event_id": 1151059, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 10:00:00", "end_date_time": "2023-12-18 16:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Heavy rain over frozen ground caused widespread flooding and road closures in Buckfield. The following roads were listed as needing repairs. Turner Street, Faunce Road, Paris Hill Road, E. Buckfield Road, Darnit Road, and N. Hill Road, cumulatively needing 20 loads of gravel to repair.", "ts_dict_index": [3336, 3337, 3338]}
+{"event_id": 1151052, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 09:05:00", "end_date_time": "2023-12-18 14:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Chushman Road flooded with water running off the hillsides, road closed.", "ts_dict_index": [3306, 3307, 3308]}
+{"event_id": 1151053, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 11:44:00", "end_date_time": "2023-12-18 14:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Heavy rain and snowmelt caused Willow Brook to leave its banks near and wash out portions of East Oxford Road near Cross Road, with a vehicle in the flood waters.", "ts_dict_index": [3330, 3331, 3332]}
+{"event_id": 1151020, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 08:30:00", "end_date_time": "2023-12-19 04:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Record flooding occurred along the Swift River in Roxbury with a river crest at 14.2 feet, breaking the record of 12.87 feet set in October of 1959. The flooding was caused after 6 inches of rain and an estimated 2 inches of snowmelt caused the river to rise 12 feet in 16 hours. The streamflows measured over 21 kcfs had a 0.5 to 0.2% annual chance exceedance, otherwise referred to as a 200 or 500 year flood recurrence interval.  The most significant damage occurred near the confluence of the Swift River and the Androscoggin River in Mexico and Rumford. Major flooding on the Androscoggin coincided with the timing of the peak flood wave on the Swift River. This resulted is destructive flooding between Carlton Avenue to Riverside Avenue including Route 2 in Mexico, and Rumford Avenue up to the Hosmer Field complex. A few dozen homes and businesses observed floodwaters several feet deep, with some properties condemned.  Additional significant damage occurred in downtown Roxbury where the river came out of banks over Frye Crossover Road bridge, flooding all the way to Route 17 and up to the base of the Post Office and at flooding at least 4 separate residences. Route 17, a main thruway in the region was severely damaged in dozens of locations in the Byron and Roxbury area.   The bridge over Coos Canyon was compromised on both the east and west sides. A home was flooded on Weld Road in Byron. A well-constructed snowmobile bridge was washed out in Byron.", "ts_dict_index": [3312, 3313, 3314]}
+{"event_id": 1151024, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 10:00:00", "end_date_time": "2023-12-20 00:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Catastrophic flooding occurred in and around Bethel after a storm brought 7 to 10 inches of combined rain and snowmelt to the region. The Androscoggin River only reached minor flood stage at the upstream river gage in Gorham, yet the contribution of flows from the mountains in between the two towns were sufficient to cause the river to reach major flood levels. Estimates put the Androscoggin River flows somewhere between the 0.5 to 0.2% annual chance exceedance levels, otherwise referred to as the 200 to 500 year floods. The tributaries out of the mountains are estimated to have exceeded 500 year flood levels including the Moose Brook, Moose River, Peabody River, Wild River, and Sunday Rivers. The Mill Brook ran high and contributed to the flooding in Bethel, but was not the significant contributor when compared to the other sources. The combined flows caused severe damage to properties and roads in the community, isolating the area for days.  The flooding was recorded as the 3rd highest in downstream Rumford, and estimated to be the 4th highest in Bethel since 1860. The floodwaters reached levels near, above, and just below high-water marks from the flood of 1987, though that flood had un-natural responses due to complications from river ice.  Though streamflows were likely less than that of 1987, the reported damage was worse.  The hardest hit part of the community was in town near the Kowloon Village and Bethel Wastewater Treatment facility, and north of the river along Interval Road and Route 2 & 5. Further downstream in Hanover, flooding was extensive including inundation at the town office off Route 2.  About 7 businesses in Bethel sustained major flood damage.  The cost of the damage to roads and infrastructure was estimated at $1 million. There were over a dozen homes damaged by flood water with a total cost estimated around $750,000.", "ts_dict_index": [3318, 3319, 3320]}
+{"event_id": 1124124, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2023-07-10 15:00:00", "end_date_time": "2023-07-11 22:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. The Connecticut River at West Lebanon flooded between July 10-11. The USGS river gage at West Lebanon has a flood stage of 22 feet and crested at 22.9 feet on the 11th.  The river was out of banks and caused minor inundation of a showing plaza parking lot and property adjacent to the publics water department in Lebanon.", "ts_dict_index": [3294, 3295, 3296]}
+{"event_id": 1124237, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2023-07-10 20:55:00", "end_date_time": "2023-07-10 22:00:00", "narrative": "Saturday, July 8th through Monday, July 10th was an active weather period with numerous rounds of heavy rainfall moving across the state.  Thunderstorms developed during the afternoon of Saturday, July 8th with scattered thunderstorms from the White Mountains down through the Monadnocks.  Storms came to an end during the evening hours. Localized 3-hr rainfall totals ranged from 1 to 3���, but no flooding was reported.  ||There was a short break in rainfall activity the night of July 8th through noon on July 9th, before a cluster of showers and thunderstorms developed around noon on Sunday across Cheshire County.  The storms continued to train over the same region with storms repeatedly hitting the same areas in Cheshire County.  Thunderstorms and showers expanded in aerial coverage across western New Hampshire through the late evening.  The rain ended in the hardest hit areas of Cheshire County by 9 PM on July 9th.  ||After a brief lull in the rainfall activity around midnight, rainfall activity began to increase once again during the early morning hours of July 10th.  A large area of rainfall pushed into Western New Hampshire as an area of low pressure moved into Northern New England.  Rainfall was light with areas of moderate rainfall rates through the morning hours of July 10th. Overall rainfall rates were not as heavy as previous days but the rain was more widespread and constant across the Connecticut River Valley region of New Hampshire.  There was a short lull in rainfall across Southwest New Hampshire during the afternoon hours, before a heavy band of heavy rain showers with intense rainfall rates pushed through the region during the evening of July 10th.  Rainfall rates up 1 to 1.25��� per/hour were reported with this band.  Additional flooding was reported as saturated soils led to rapid run-off, especially in Sullivan and Northern Cheshire County. Heavy rain over saturated ground led to flooding on Pinneo Hill Road near Lyme Road in Hanover.", "ts_dict_index": [3297, 3298, 3299]}
+{"event_id": 1152096, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-12-18 14:00:00", "end_date_time": "2023-12-19 03:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Heavy rain and snowmelt runoff caused already swollen lakes to overflow their banks. In New Sharon, Crowell Pond flooded Route 41with water up to 2 feet for numerous days.", "ts_dict_index": [3327, 3328, 3329]}
+{"event_id": 988982, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2021-12-14 10:59:00", "end_date_time": "2021-12-14 11:59:00", "narrative": "A strong low pressure system dropped southeast out of the Gulf of Alaska on December 12 and intensified off the Pacific Northwest coast on December 13 pulling up some deep moisture which was pushed into central California during the afternoon.  The precipitation intensified during the evening of December 13 through the morning of December 14 as the low carved out a deep upper trough which pushed across California during the afternoon of December 14.  This system produced 2 to 4 inches of liquid precipitation over the Sierra Nevada from Sequoia National Park northward and 1 to 3 inches of liquid precipitation south of Sequoia Park.  The precipitation fell mainly in the form of snow above 5500 feet and several high elevation SNOTELs estimated 2 to 4 feet of new snowfall.  The snow level lowered to as low as 1500 feet during the evening of December 14 as the cooler airmass behind the system pushed into central California.  Much of the San Joaquin Valley picked up between 1 to 2 inches of rainfall while the Kern County Mountains picked up between 0.75 and 1.5 inches of liquid precipitation.  The Kern County Desert areas only picked up between a quarter and a half inch of rain at most locations due to rain shadowing.  The storm produced widespread minor nuisance flooding in the San Joaquin Valley and Sierra foothills with a few rock slides noticed.  Several roads were closed as a precaution and chain restrictions were implemented on some roads in the Sierra Nevada.  The storm also produced strong winds over the West Side Hills as well as in the Grapevine and Tehachapi areas in Kern County.  Several stations in these areas measured wind gusts exceeding 50 mph with a few locations near the Grapevine measuring brief gusts exceeding 70 mph. California Highway Patrol reported roadway flooding near the intersection of north Valencia Blvd. and West Cajon Ave. in Woodlake.", "ts_dict_index": [3354, 3355, 3356]}
+{"event_id": 1069776, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2022-12-23 13:30:00", "end_date_time": "2022-12-23 15:30:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages to the region with upwards to 240,000 customers without power. ||Precipitation moved into southern Maine during the late evening hours of December 22, and moved across the remainder of the state into the early morning of December 23. Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd.  The precipitation continued through the evening hours of December 23, then gradually ended from south to north early morning, December 24. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the beaches and Mid-Coast of Maine. Cobb Road washout between Ashton Road and Country Club Road.", "ts_dict_index": [3363, 3364, 3365]}
+{"event_id": 1151064, "event_type": "Flood", "state": "MAINE", "cz_name": "FRANKLIN", "begin_date_time": "2023-12-18 11:30:00", "end_date_time": "2023-12-18 20:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. After heavy rain and snowmelt, several roads around Rangeley flooded including Bald Mountain Road and South Shore Road which were impassable due to flooding.", "ts_dict_index": [3342, 3343, 3344]}
+{"event_id": 1069795, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2022-12-24 02:00:00", "end_date_time": "2022-12-24 12:00:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages to the region with upwards to 240,000 customers without power. ||Precipitation moved into southern Maine during the late evening hours of December 22, and moved across the remainder of the state into the early morning of December 23. Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd.  The precipitation continued through the evening hours of December 23, then gradually ended from south to north early morning, December 24. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the beaches and Mid-Coast of Maine. Ice flows from Gorham were transported downstream to Rumford on December 23rd when rain and snowmelt raised river levels. The ice jammed at the Rumford dam, causing fast rising water during the early morning hours of December 24. All three roads into Rumford from the west were flooded. Route 232 and Route 2 were severely flooded with water 1 to 5 feet deep. Flood waters entered around a dozen properties, including the first floor of at least 5 structures. Multiple cold water rescues were conducted for motorists surprised by the flooded roads at night. No fatalities or injuries were reported.", "ts_dict_index": [3366, 3367, 3368]}
+{"event_id": 1151060, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 09:45:00", "end_date_time": "2023-12-18 18:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Heavy rain over frozen ground caused widespread flooding and road closures in Paris including Brown Way, Christian Ridge Road, Old Route 26, and Stock Farm Road.", "ts_dict_index": [3345, 3346, 3347]}
+{"event_id": 988983, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2021-12-14 12:29:00", "end_date_time": "2021-12-14 13:29:00", "narrative": "A strong low pressure system dropped southeast out of the Gulf of Alaska on December 12 and intensified off the Pacific Northwest coast on December 13 pulling up some deep moisture which was pushed into central California during the afternoon.  The precipitation intensified during the evening of December 13 through the morning of December 14 as the low carved out a deep upper trough which pushed across California during the afternoon of December 14.  This system produced 2 to 4 inches of liquid precipitation over the Sierra Nevada from Sequoia National Park northward and 1 to 3 inches of liquid precipitation south of Sequoia Park.  The precipitation fell mainly in the form of snow above 5500 feet and several high elevation SNOTELs estimated 2 to 4 feet of new snowfall.  The snow level lowered to as low as 1500 feet during the evening of December 14 as the cooler airmass behind the system pushed into central California.  Much of the San Joaquin Valley picked up between 1 to 2 inches of rainfall while the Kern County Mountains picked up between 0.75 and 1.5 inches of liquid precipitation.  The Kern County Desert areas only picked up between a quarter and a half inch of rain at most locations due to rain shadowing.  The storm produced widespread minor nuisance flooding in the San Joaquin Valley and Sierra foothills with a few rock slides noticed.  Several roads were closed as a precaution and chain restrictions were implemented on some roads in the Sierra Nevada.  The storm also produced strong winds over the West Side Hills as well as in the Grapevine and Tehachapi areas in Kern County.  Several stations in these areas measured wind gusts exceeding 50 mph with a few locations near the Grapevine measuring brief gusts exceeding 70 mph. California Highway Patrol reported roadway flooding near the intersection Taft Highway and Buena Vista Rd. west of Bakersfield.", "ts_dict_index": [3360, 3361, 3362]}
+{"event_id": 988984, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2021-12-14 12:33:00", "end_date_time": "2021-12-14 13:33:00", "narrative": "A strong low pressure system dropped southeast out of the Gulf of Alaska on December 12 and intensified off the Pacific Northwest coast on December 13 pulling up some deep moisture which was pushed into central California during the afternoon.  The precipitation intensified during the evening of December 13 through the morning of December 14 as the low carved out a deep upper trough which pushed across California during the afternoon of December 14.  This system produced 2 to 4 inches of liquid precipitation over the Sierra Nevada from Sequoia National Park northward and 1 to 3 inches of liquid precipitation south of Sequoia Park.  The precipitation fell mainly in the form of snow above 5500 feet and several high elevation SNOTELs estimated 2 to 4 feet of new snowfall.  The snow level lowered to as low as 1500 feet during the evening of December 14 as the cooler airmass behind the system pushed into central California.  Much of the San Joaquin Valley picked up between 1 to 2 inches of rainfall while the Kern County Mountains picked up between 0.75 and 1.5 inches of liquid precipitation.  The Kern County Desert areas only picked up between a quarter and a half inch of rain at most locations due to rain shadowing.  The storm produced widespread minor nuisance flooding in the San Joaquin Valley and Sierra foothills with a few rock slides noticed.  Several roads were closed as a precaution and chain restrictions were implemented on some roads in the Sierra Nevada.  The storm also produced strong winds over the West Side Hills as well as in the Grapevine and Tehachapi areas in Kern County.  Several stations in these areas measured wind gusts exceeding 50 mph with a few locations near the Grapevine measuring brief gusts exceeding 70 mph. California Highway Patrol reported roadway flooding along SR 58 7WNW of Keene.", "ts_dict_index": [3348, 3349, 3350]}
+{"event_id": 1069777, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2022-12-23 14:00:00", "end_date_time": "2022-12-23 15:30:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages to the region with upwards to 240,000 customers without power. ||Precipitation moved into southern Maine during the late evening hours of December 22, and moved across the remainder of the state into the early morning of December 23. Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd.  The precipitation continued through the evening hours of December 23, then gradually ended from south to north early morning, December 24. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the beaches and Mid-Coast of Maine. Bullring Road flooding from Dragon Meadow Brook.", "ts_dict_index": [3369, 3370, 3371]}
+{"event_id": 1151023, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-19 00:00:00", "end_date_time": "2023-12-20 00:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. The combined runoff from rain and snowmelt averaged 7 to 10 inches in the higher terrain, and 4 to 6 inches in the Saco River Valley Basin. The steep terrain and frozen ground supported rapid runoff which caused flash flooding along all streams and brooks in the region. The Swift River, a western tributary to the Saco River in Conway, was estimated to have had flows around 12-16 kcfs. The flows in the Saco River in Bartlett reached 24 kcfs. The annual chance occurrence of these flows are estimated around 1% to 0.2%, otherwise referred to as a 100 or 500 year flood. The combined flows in Conway resulted in flows over 60 kcfs as measured by the USGS gage. The stream height reached 17.72 on the evening of the 18th, exceeding the record held by Irene in 2011 which crested at 17.23 feet with a flow of 58.2 kcfs.  The river climbed from 4 feet on the 17th to 17 feet in under 24 hours due to the rapid nature of the runoff.  The flood wave moved down the Saco River into the Fryeburg area, flooding along Route 113 River Street from Conway to Fryeburg.  River street was flooded and closed for a period of time.  The flood wave reached the marshy areas with limited impacts further downriver from Fryeburg.", "ts_dict_index": [3321, 3322, 3323]}
+{"event_id": 1068875, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2022-12-23 12:15:00", "end_date_time": "2022-12-23 17:00:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages to the region with upwards to 240,000 customers without power. ||Precipitation moved into southern Maine during the late evening hours of December 22, and moved across the remainder of the state into the early morning of December 23. Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd.  The precipitation continued through the evening hours of December 23, then gradually ended from south to north early morning, December 24. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the beaches and Mid-Coast of Maine. Road flooding at Robinson Hill Rd at Jam Hill Road in Oxford.", "ts_dict_index": [3372, 3373, 3374]}
+{"event_id": 1068873, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2022-12-23 22:30:00", "end_date_time": "2022-12-24 02:00:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages to the region with upwards to 240,000 customers without power. ||Precipitation moved into southern Maine during the late evening hours of December 22, and moved across the remainder of the state into the early morning of December 23. Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd.  The precipitation continued through the evening hours of December 23, then gradually ended from south to north early morning, December 24. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the beaches and Mid-Coast of Maine. The Swift River came out of banks reaching 8.2 feet on the evening of the 23rd, climbing 1.2 feet above flood stage set at the USGS gage in Roxbury. Flood waters inundated Route 17 in Byron near the intersection of Byron Village Road at 9 feet.", "ts_dict_index": [3375, 3376, 3377]}
+{"event_id": 1151035, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-12-18 11:00:00", "end_date_time": "2023-12-19 05:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Hundreds of thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Widespread moderate to major flooding occurred along mainstem rivers.  The storm destroyed 13 homes, caused major damage to 106 others, with an additional 65 homes receiving minor flood damage.  Private damage was in the millions with public infrastructure damage of 20+ million being reported by FEMA. Record flooding occurred on December 18th after a storm brought heavy rain and rapid snowmelt to the Ellis River. The river reached major flood stage cresting at 21.5 feet with a flow of 15,800 cfs, surpassing the previous flood of record of 19.26 feet set in December of 2003. The storm was estimated as a 0.2% annual chance exceedance flood, otherwise referred to as a 500-year event. Flooding cut off the town of Andover with closures of Maine Route 120, Roxbury Pond Road, Route 5, and Upton Road.  Water cut-off a historic covered bridge, compromising the structure.  Route 5 was closed for several weeks due to severe damage to the road.  Meadow Brook, a tributary to the Ellis, caused a washout on Roxbury Notch Road.  Infrastructure loss from roads and bridges across the area is about $100,000.", "ts_dict_index": [3315, 3316, 3317]}
+{"event_id": 1068884, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2022-12-24 00:00:00", "end_date_time": "2022-12-24 06:00:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. The Saco River climbed 1.5 feet above flood stage, cresting at 10.5 feet at the USGS gage. Minor flooding occurred as floodwaters surrounded properties across Transvale Acres in Conway. Flood waters 1 to 2 feet deep in sections of east bank camping areas.", "ts_dict_index": [3411, 3412, 3413]}
+{"event_id": 1069784, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2022-12-23 16:45:00", "end_date_time": "2022-12-23 18:30:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. Flooding at RT-153 at Madison and Freedom Town Line.", "ts_dict_index": [3402, 3403, 3404]}
+{"event_id": 1069739, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2022-12-23 10:00:00", "end_date_time": "2022-12-23 11:30:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. Road flooding on NH 109 Between Governors Road and Brice Drive.", "ts_dict_index": [3396, 3397, 3398]}
+{"event_id": 1069781, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2022-12-23 16:30:00", "end_date_time": "2022-12-23 17:30:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. Flooding reported on NH RT-153 between Brownfield Road and Potter Road.", "ts_dict_index": [3384, 3385, 3386]}
+{"event_id": 1068890, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2022-12-23 21:30:00", "end_date_time": "2022-12-24 00:00:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. The Pemigewasset River climbed a foot above flood stage at the USGS river gage in Woodstock. Route 175 flooded at Cox Farm Road in Woodstock. Campgrounds along the river also flooded, but were not damaged due to it being the off-season.", "ts_dict_index": [3381, 3382, 3383]}
+{"event_id": 1068888, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2022-12-23 21:00:00", "end_date_time": "2022-12-24 02:00:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. Excessive rainfall and snowmelt caused the Ammonoosuc River to back up water on the Black Brook on the evening of December 23. The flood waters inundated River Road. The USGS gage at Bethlehem exceeded flood stage by a little more than a foot.", "ts_dict_index": [3390, 3391, 3392]}
+{"event_id": 1069769, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2022-12-23 14:45:00", "end_date_time": "2022-12-23 15:30:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. Water over the road at 37 Braley Road. The road is dead end with a number of houses cut off from emergency access.", "ts_dict_index": [3378, 3379, 3380]}
+{"event_id": 1069767, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2022-12-23 16:10:00", "end_date_time": "2022-12-23 17:30:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. Flooding at Fairgrounds Road at mile marker 400.", "ts_dict_index": [3399, 3400, 3401]}
+{"event_id": 1069430, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2022-12-24 03:15:00", "end_date_time": "2022-12-24 08:00:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. The Pemigewasset River at Plymouth came out of banks exceeding the 13 ft flood stage set at the USGS river gage. The river cresting at 15.2 feet during the early morning hours of the 24th. Flood waters reached the road at the Irving station on route 175A in Holderness and flooded the recreational fields and parking lot by PSU.", "ts_dict_index": [3408, 3409, 3410]}
+{"event_id": 1069770, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2022-12-23 17:45:00", "end_date_time": "2022-12-23 19:00:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. Nichols Hill Road Roads closed due to flooding and multiple washouts. North Dorchester Road Road closed due to flooding, water 2-3 feet over the road.", "ts_dict_index": [3405, 3406, 3407]}
+{"event_id": 1069763, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2022-12-23 16:10:00", "end_date_time": "2022-12-23 17:30:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. Road flooding on Landaff Titus Road and Landaff Mill Brook Road.", "ts_dict_index": [3387, 3388, 3389]}
+{"event_id": 863266, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-12-26 05:00:00", "end_date_time": "2019-12-26 07:00:00", "narrative": "A strong and very cold low pressure system dropped southward along the California coast on Christmas Day bringing some light precipitation inland into central California. The system then turned inland and moved through southern California during the evening of December 25 through the morning of December 26 bringing moderate to heavy precipitation to much of Kern County with lighter amounts further north. Between 1 and 2 inches of liquid precipitation fell across much of Kern County with the snow level between 2500 and 3000 feet. Above the snow line, 1 to 2 feet of new snowfall was reported at several stations and the heavy snowfall resulted in the closure of several highways (including Interstate 5 south of Grapevine) for an extended period of time during a period of normally heavy holiday traffic after several vehicle either slid off of the highway or spun out. One truck driver was killed after being stranded along Interstate 5 for several hours. Across the Kern County Deserts and in the San Joaquin Valley from Bakersfield southward, heavy rainfall resulted in several roads being closed for a few hours with several reports of nuisance flooding reported by the Emergency Managers office or by law enforcement. There were also several reports of strong wind gusts and some reports of minor wind damage in the Fort Tejon and Tehachapi areas. Further north precipitation amounts were significantly lower although parts of Kings County picked up between a quarter and three quarters of an inch of rainfall. The remainder of the area generally picked up a quarter of an inch or less of liquid precipitation before the system moved to the east of the area during the evening of December 26. Kern County Emergency Manager reported roadway flooding on Laval Rd. from Rancho Rd. to Wheeler Ridge Rd.", "ts_dict_index": [3414, 3415, 3416]}
+{"event_id": 988981, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2021-12-14 10:46:00", "end_date_time": "2021-12-14 11:46:00", "narrative": "A strong low pressure system dropped southeast out of the Gulf of Alaska on December 12 and intensified off the Pacific Northwest coast on December 13 pulling up some deep moisture which was pushed into central California during the afternoon.  The precipitation intensified during the evening of December 13 through the morning of December 14 as the low carved out a deep upper trough which pushed across California during the afternoon of December 14.  This system produced 2 to 4 inches of liquid precipitation over the Sierra Nevada from Sequoia National Park northward and 1 to 3 inches of liquid precipitation south of Sequoia Park.  The precipitation fell mainly in the form of snow above 5500 feet and several high elevation SNOTELs estimated 2 to 4 feet of new snowfall.  The snow level lowered to as low as 1500 feet during the evening of December 14 as the cooler airmass behind the system pushed into central California.  Much of the San Joaquin Valley picked up between 1 to 2 inches of rainfall while the Kern County Mountains picked up between 0.75 and 1.5 inches of liquid precipitation.  The Kern County Desert areas only picked up between a quarter and a half inch of rain at most locations due to rain shadowing.  The storm produced widespread minor nuisance flooding in the San Joaquin Valley and Sierra foothills with a few rock slides noticed.  Several roads were closed as a precaution and chain restrictions were implemented on some roads in the Sierra Nevada.  The storm also produced strong winds over the West Side Hills as well as in the Grapevine and Tehachapi areas in Kern County.  Several stations in these areas measured wind gusts exceeding 50 mph with a few locations near the Grapevine measuring brief gusts exceeding 70 mph. California Highway Patrol reported roadway flooding on the southbound lanes of SR 99 near the SR 58 intersection.", "ts_dict_index": [3357, 3358, 3359]}
+{"event_id": 798016, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2019-02-13 12:01:00", "end_date_time": "2019-02-13 15:01:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. California Highway Patrol reported the westbound lanes on State Route 140 near Bull Creek near Briceburg were completely covered with debris due to heavy rain.", "ts_dict_index": [3438, 3439, 3440]}
+{"event_id": 798023, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-02-15 16:19:00", "end_date_time": "2019-02-15 19:19:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. California Highway Patrol reported one foot of water covering the left lane of eastbound State Route 198 just west of Exeter Blvd.", "ts_dict_index": [3441, 3442, 3443]}
+{"event_id": 798021, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-02-15 14:03:00", "end_date_time": "2019-02-15 16:03:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. Video obtained through social media indicated flooding at the intersection of Peach Ave. and Olive Ave. in Fresno.", "ts_dict_index": [3447, 3448, 3449]}
+{"event_id": 798022, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-02-15 14:49:00", "end_date_time": "2019-02-15 17:49:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. California Highway Patrol reported 6 to 8 inches of water rushing over the roadway on State Route 180 near Cove Ave.", "ts_dict_index": [3435, 3436, 3437]}
+{"event_id": 863268, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-12-26 14:00:00", "end_date_time": "2019-12-26 18:00:00", "narrative": "A strong and very cold low pressure system dropped southward along the California coast on Christmas Day bringing some light precipitation inland into central California. The system then turned inland and moved through southern California during the evening of December 25 through the morning of December 26 bringing moderate to heavy precipitation to much of Kern County with lighter amounts further north. Between 1 and 2 inches of liquid precipitation fell across much of Kern County with the snow level between 2500 and 3000 feet. Above the snow line, 1 to 2 feet of new snowfall was reported at several stations and the heavy snowfall resulted in the closure of several highways (including Interstate 5 south of Grapevine) for an extended period of time during a period of normally heavy holiday traffic after several vehicle either slid off of the highway or spun out. One truck driver was killed after being stranded along Interstate 5 for several hours. Across the Kern County Deserts and in the San Joaquin Valley from Bakersfield southward, heavy rainfall resulted in several roads being closed for a few hours with several reports of nuisance flooding reported by the Emergency Managers office or by law enforcement. There were also several reports of strong wind gusts and some reports of minor wind damage in the Fort Tejon and Tehachapi areas. Further north precipitation amounts were significantly lower although parts of Kings County picked up between a quarter and three quarters of an inch of rainfall. The remainder of the area generally picked up a quarter of an inch or less of liquid precipitation before the system moved to the east of the area during the evening of December 26. Kern County Emergency Manager reported Redrock-Randsburg Rd. was closed between SR 14 and US 395 due to flooding.", "ts_dict_index": [3429, 3430, 3431]}
+{"event_id": 863269, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-12-26 15:00:00", "end_date_time": "2019-12-26 17:00:00", "narrative": "A strong and very cold low pressure system dropped southward along the California coast on Christmas Day bringing some light precipitation inland into central California. The system then turned inland and moved through southern California during the evening of December 25 through the morning of December 26 bringing moderate to heavy precipitation to much of Kern County with lighter amounts further north. Between 1 and 2 inches of liquid precipitation fell across much of Kern County with the snow level between 2500 and 3000 feet. Above the snow line, 1 to 2 feet of new snowfall was reported at several stations and the heavy snowfall resulted in the closure of several highways (including Interstate 5 south of Grapevine) for an extended period of time during a period of normally heavy holiday traffic after several vehicle either slid off of the highway or spun out. One truck driver was killed after being stranded along Interstate 5 for several hours. Across the Kern County Deserts and in the San Joaquin Valley from Bakersfield southward, heavy rainfall resulted in several roads being closed for a few hours with several reports of nuisance flooding reported by the Emergency Managers office or by law enforcement. There were also several reports of strong wind gusts and some reports of minor wind damage in the Fort Tejon and Tehachapi areas. Further north precipitation amounts were significantly lower although parts of Kings County picked up between a quarter and three quarters of an inch of rainfall. The remainder of the area generally picked up a quarter of an inch or less of liquid precipitation before the system moved to the east of the area during the evening of December 26. Kern County Emergency Manager reported Shallock Rd. was closed between Copus Rd. and Valpredo Ave. due to flooding.", "ts_dict_index": [3432, 3433, 3434]}
+{"event_id": 863270, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-12-26 15:00:00", "end_date_time": "2019-12-26 17:00:00", "narrative": "A strong and very cold low pressure system dropped southward along the California coast on Christmas Day bringing some light precipitation inland into central California. The system then turned inland and moved through southern California during the evening of December 25 through the morning of December 26 bringing moderate to heavy precipitation to much of Kern County with lighter amounts further north. Between 1 and 2 inches of liquid precipitation fell across much of Kern County with the snow level between 2500 and 3000 feet. Above the snow line, 1 to 2 feet of new snowfall was reported at several stations and the heavy snowfall resulted in the closure of several highways (including Interstate 5 south of Grapevine) for an extended period of time during a period of normally heavy holiday traffic after several vehicle either slid off of the highway or spun out. One truck driver was killed after being stranded along Interstate 5 for several hours. Across the Kern County Deserts and in the San Joaquin Valley from Bakersfield southward, heavy rainfall resulted in several roads being closed for a few hours with several reports of nuisance flooding reported by the Emergency Managers office or by law enforcement. There were also several reports of strong wind gusts and some reports of minor wind damage in the Fort Tejon and Tehachapi areas. Further north precipitation amounts were significantly lower although parts of Kings County picked up between a quarter and three quarters of an inch of rainfall. The remainder of the area generally picked up a quarter of an inch or less of liquid precipitation before the system moved to the east of the area during the evening of December 26. Kern County Emergency Manager reported Panama Ln. was closed between Weedpatch Hwy. and Edison Rd. due to flooding.", "ts_dict_index": [3423, 3424, 3425]}
+{"event_id": 798017, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-02-14 10:37:00", "end_date_time": "2019-02-14 13:37:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. California Highway Patrol reported 4 feet of roadway on Caliente-Bodfish Road were washed away.", "ts_dict_index": [3444, 3445, 3446]}
+{"event_id": 863267, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-12-26 09:30:00", "end_date_time": "2019-12-26 12:30:00", "narrative": "A strong and very cold low pressure system dropped southward along the California coast on Christmas Day bringing some light precipitation inland into central California. The system then turned inland and moved through southern California during the evening of December 25 through the morning of December 26 bringing moderate to heavy precipitation to much of Kern County with lighter amounts further north. Between 1 and 2 inches of liquid precipitation fell across much of Kern County with the snow level between 2500 and 3000 feet. Above the snow line, 1 to 2 feet of new snowfall was reported at several stations and the heavy snowfall resulted in the closure of several highways (including Interstate 5 south of Grapevine) for an extended period of time during a period of normally heavy holiday traffic after several vehicle either slid off of the highway or spun out. One truck driver was killed after being stranded along Interstate 5 for several hours. Across the Kern County Deserts and in the San Joaquin Valley from Bakersfield southward, heavy rainfall resulted in several roads being closed for a few hours with several reports of nuisance flooding reported by the Emergency Managers office or by law enforcement. There were also several reports of strong wind gusts and some reports of minor wind damage in the Fort Tejon and Tehachapi areas. Further north precipitation amounts were significantly lower although parts of Kings County picked up between a quarter and three quarters of an inch of rainfall. The remainder of the area generally picked up a quarter of an inch or less of liquid precipitation before the system moved to the east of the area during the evening of December 26. Kern County Emergency Manager reported Airport Dr. was closed from Roberts Ln. to State Rd. due to flooding.", "ts_dict_index": [3426, 3427, 3428]}
+{"event_id": 863271, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-12-26 15:00:00", "end_date_time": "2019-12-26 17:00:00", "narrative": "A strong and very cold low pressure system dropped southward along the California coast on Christmas Day bringing some light precipitation inland into central California. The system then turned inland and moved through southern California during the evening of December 25 through the morning of December 26 bringing moderate to heavy precipitation to much of Kern County with lighter amounts further north. Between 1 and 2 inches of liquid precipitation fell across much of Kern County with the snow level between 2500 and 3000 feet. Above the snow line, 1 to 2 feet of new snowfall was reported at several stations and the heavy snowfall resulted in the closure of several highways (including Interstate 5 south of Grapevine) for an extended period of time during a period of normally heavy holiday traffic after several vehicle either slid off of the highway or spun out. One truck driver was killed after being stranded along Interstate 5 for several hours. Across the Kern County Deserts and in the San Joaquin Valley from Bakersfield southward, heavy rainfall resulted in several roads being closed for a few hours with several reports of nuisance flooding reported by the Emergency Managers office or by law enforcement. There were also several reports of strong wind gusts and some reports of minor wind damage in the Fort Tejon and Tehachapi areas. Further north precipitation amounts were significantly lower although parts of Kings County picked up between a quarter and three quarters of an inch of rainfall. The remainder of the area generally picked up a quarter of an inch or less of liquid precipitation before the system moved to the east of the area during the evening of December 26. Kern County Emergency Manager reported South Vineland Rd. was closed between Mountain View Rd. and Hermosa Rd. due to flooding.", "ts_dict_index": [3420, 3421, 3422]}
+{"event_id": 1069437, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2022-12-23 23:20:00", "end_date_time": "2022-12-24 03:00:00", "narrative": "Beginning on December 22nd a powerful storm was developing over the Ohio River Valley. On December 23rd the center of the storm was deepening rapidly (974mb) as it lifted through the eastern Great Lakes. While the center tracked into southern Ontario, high pressure retreated into the Canadian Maritimes creating a strong pressure gradient across the region. Strong southerly winds developed as a result, with speeds in excess of 80 knots at around 2,000 feet. Several rounds of strong to damaging wind gusts occurred, which brought widespread power outages with over 120,000 customers without power.||Precipitation moved into western New Hampshire during the late evening hours of December 22, and moved across the remainder of the state by the early morning of December 23.  Snow quickly changed over to rain on the night of December 22nd, with a changeover later in the mountains towards daybreak on December 23rd. The precipitation continued through the evening hours of December 23, then gradually ended from south to north that night. Overland flooding was prevalent for areas where rainfall exceeded 2 inches. The impacts varied from standing water in fields to complete road washouts. The runoff exceeded capacity for most feeder creeks and rivers.||The rapidly deepening area of low pressure over the Great Lakes region combined with very high astronomical tides to produce the fourth highest storm tide ever in Portland. In addition, storm to hurricane force east to southeasterly winds occurred along the coast with nearshore waves of 15 to 20 feet coinciding during peak storm surge.  Significant to major coastal damage occurred during the morning high tide cycle across the Seacoast of New Hampshire. According to the USGS River Gage on the Baker River at Rumney, the river exceeded the 10 ft flood stage on the evening of the 23rd and crested at 10.6 feet. The resulting flooding impacted area campgrounds.", "ts_dict_index": [3393, 3394, 3395]}
+{"event_id": 798018, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2019-02-14 12:24:00", "end_date_time": "2019-02-14 15:24:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. California Highway Patrol reported roadway flooding on State Route 140 near Hornitos Road on both lanes.", "ts_dict_index": [3453, 3454, 3455]}
+{"event_id": 1151014, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2023-12-18 09:10:00", "end_date_time": "2023-12-18 14:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the White Mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Localized moderate to major flooding occurred along mainstem rivers with the majority of New Hampshire Rivers outside of the mountains only reaching minor flood stage. Heavy rain and snowmelt caused rapid runoff and flooding from the Cold River.  River overflowed the Stone House Road bridge in Chatham along the Maine and New Hampshire stateline.", "ts_dict_index": [3480, 3481, 3482]}
+{"event_id": 798020, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-02-14 20:55:00", "end_date_time": "2019-02-14 23:55:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. California Highway Patrol reported State Route 269 was closed north of State Route 198 due to heavy rainfall which flooded the road.", "ts_dict_index": [3450, 3451, 3452]}
+{"event_id": 1150890, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2023-12-18 10:00:00", "end_date_time": "2023-12-19 14:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the White Mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Localized moderate to major flooding occurred along mainstem rivers with the majority of New Hampshire Rivers outside of the mountains only reaching minor flood stage. Catastrophic flooding occurred across the Conway area on December 18th following heavy rain and snowmelt. The storm featured strong southeast winds measured between 30 to 55 mph in the region, which supported orographically enhanced rainfall and supported rapid snowmelt. The combined runoff from rain and snowmelt averaged 7 to 10 inches in the higher terrain, and 4 to 6 inches in the valley. The steep terrain and frozen ground supported rapid runoff which caused flash flooding along all streams and brooks in the region. The Swift River, a western tributary to the Saco River in Conway, was estimated to have had flows around 12-16 kcfs. The flows in the Saco River in Bartlett reached 24 kcfs. The annual chance occrrence of these flows are estimated around 1% to 0.2%, otherwise referred to as a 100 or 500 year flood. The combined flows in Conway resulted in flows over 60 kcfs as measured by the USGS gage. The stream height reached 17.72 on the evening of the 18th, exceeding the record held by Irene in 2011 which crested at 17.23 feet with a flow of 58.2 kcfs.  The river climbed from 4 feet on the 17th to 17 feet in under 24 hours due to the rapid nature of the runoff. ||Flooding and Damage was extensive with hundreds of residents impacted. The confluence of the Swift and Saco Rivers in North Conway drowned Washington St and shutting down both ends of West Side Road and preventing most traffic from getting in or out of the region. Over a dozen residents of Transvale Acres had to be rescued with 5 airlifted by helecopter from the National Guard. Homes in this community sustained severe damages with water several feet deep. Properties off Route 302 in Center Conway including Kenwood Circle, Robinwood Road, Burbank Road flooded with water several feet deep.  Numerous campgrounds and recreational facilities including a golf course were completely inundated with water chest deep. The flooding continued along Route 113 River Street from Conway to Fryeburg.", "ts_dict_index": [3468, 3469, 3470]}
+{"event_id": 1151013, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2023-12-18 09:10:00", "end_date_time": "2023-12-18 14:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the White Mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Localized moderate to major flooding occurred along mainstem rivers with the majority of New Hampshire Rivers outside of the mountains only reaching minor flood stage. Heavy rain and snowmelt caused rapid runoff and flooding of the Ossipee River in Effingham causing NH 153 or Province Lake Road to be closed.", "ts_dict_index": [3471, 3472, 3473]}
+{"event_id": 1078261, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-17 06:00:00", "end_date_time": "2023-02-17 16:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. A National Weather Service employee reported signs that Anthony Creek, as well as multiple tributaries of the creek were out of their banks and covering Highway 92 near the community of Neola, WV during the 17th.  No damage was reported, though removal of debris was likely necessary.", "ts_dict_index": [3483, 3484, 3485]}
+{"event_id": 1150881, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2023-12-18 09:00:00", "end_date_time": "2023-12-19 01:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the White Mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Localized moderate to major flooding occurred along mainstem rivers with the majority of New Hampshire Rivers outside of the mountains only reaching minor flood stage. The Ammonoosuc River reached moderate flood stage on December 18th. The USGS river gage in Bethlehem reported a stage of 12.15 feet, the second highest crest on record since the site was established in 1940. The flooding was the result of heavy rainfall combined with snowmelt in the mountains. The combined runoff was estimated between 6 and 7 inches which moved rapidly down steep terrain over frozen ground. The river rose from 2 feet to over 12 feet within 15 hours, cresting in the early afternoon of the 18th. Hardest hit areas were in Littleton off of Meadow Street where numerous businesses were impacted south of the Route 93 exit. Flooding was also reported along Union and Cottage Street at Lane House, and Littleton Water and Light.  Community fields in Lisbon under several feet of water.", "ts_dict_index": [3465, 3466, 3467]}
+{"event_id": 1150879, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2023-12-18 13:00:00", "end_date_time": "2023-12-19 15:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the White Mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Localized moderate to major flooding occurred along mainstem rivers with the majority of New Hampshire Rivers outside of the mountains only reaching minor flood stage. Significant flooding occurred from Woodstock to Plymouth after a storm brought 3 to 6 inches of combined rain and snow melt to the region.  The heaviest rainfall and most significant snowmelt water contribution occurred across the higher terrain of the watershed, where up to 10 inches of combined rainfall and snowmelt was released into the Pemigewasset basin.  This caused the river to rise to its third highest crest at Woodstock, and 10th highest on record at Plymouth. This was also the highest crest on the Pemigewasset since Tropical Storm Irene in 2011. Estimates near the start of the watershed put the flow in the 1.0 to 0.5% chance of exceedance levels, also referred to as a 100-200 year flood event. It was less significant downstream however, with estimated flows at Woodstock being more consistent with a 25-50 year, and flows at Plymouth being more consistent with a 25 year event. The decreasing recurrence interval timeframe with downstream progress on the river highlights the significant role the higher rainfall amounts and snowmelt factored in near the top of the watershed, while relatively less input with decreasing elevation resulted in a tapering in the relative significance of the event. Damage was widespread along the Pemigewasset between Woodstock to Ashland.  In the town of Holderness, up to two feet of water entered homes and local businesses on Avery Street, South River St, and North River St.  Individuals that declined to evacuate were stuck in their homes as floodwaters entered during the early morning hours on the 19th.  Water levels rose to the edge of the Plymouth State University Ice Arena doors.  Numerous road closures were reported along Route 3, with up to five feet of water covering the roadways in Plymouth and Campton.  Water up to two feet deep covered Route 3 in Thornton, and flooded numerous trailers and campers at local riverside campgrounds.  Anecdotally, locals reported that the water levels in Thornton were higher than they were during Irene.", "ts_dict_index": [3462, 3463, 3464]}
+{"event_id": 1150880, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "GRAFTON", "begin_date_time": "2023-12-18 09:00:00", "end_date_time": "2023-12-19 01:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the White Mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Localized moderate to major flooding occurred along mainstem rivers with the majority of New Hampshire Rivers outside of the mountains only reaching minor flood stage. The Ammonoosuc River reached moderate flood stage on December 18th. The USGS river gage in Bethlehem reported a stage of 12.15 feet, the second highest crest on record since the site was established in 1940. The flooding was the result of heavy rainfall combined with snowmelt in the mountains. The combined runoff was estimated between 6 and 7 inches which moved rapidly down steep terrain over frozen ground. The river rose from 2 feet to over 12 feet within 15 hours, cresting in the early afternoon of the 18th. In upstream Bethlehem, there was flooding along several small streams and brooks.  Access was cut off on River Road with flooding in multiple locations.  Significant flooding occurred upstream at Twin Mountain and Zealand Campgrounds. Flooding occurred at the Stark Village Inn with basement inundation and water up to the bottom of the covered bridge in Stark.", "ts_dict_index": [3474, 3475, 3476]}
+{"event_id": 798019, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-02-14 15:06:00", "end_date_time": "2019-02-14 21:06:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. California Highway Patrol reported blocked culverts and roadway completely flooded on Lake Isabella Blvd. at Elizabeth Morris Road.", "ts_dict_index": [3456, 3457, 3458]}
+{"event_id": 863272, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-12-26 15:00:00", "end_date_time": "2019-12-26 17:00:00", "narrative": "A strong and very cold low pressure system dropped southward along the California coast on Christmas Day bringing some light precipitation inland into central California. The system then turned inland and moved through southern California during the evening of December 25 through the morning of December 26 bringing moderate to heavy precipitation to much of Kern County with lighter amounts further north. Between 1 and 2 inches of liquid precipitation fell across much of Kern County with the snow level between 2500 and 3000 feet. Above the snow line, 1 to 2 feet of new snowfall was reported at several stations and the heavy snowfall resulted in the closure of several highways (including Interstate 5 south of Grapevine) for an extended period of time during a period of normally heavy holiday traffic after several vehicle either slid off of the highway or spun out. One truck driver was killed after being stranded along Interstate 5 for several hours. Across the Kern County Deserts and in the San Joaquin Valley from Bakersfield southward, heavy rainfall resulted in several roads being closed for a few hours with several reports of nuisance flooding reported by the Emergency Managers office or by law enforcement. There were also several reports of strong wind gusts and some reports of minor wind damage in the Fort Tejon and Tehachapi areas. Further north precipitation amounts were significantly lower although parts of Kings County picked up between a quarter and three quarters of an inch of rainfall. The remainder of the area generally picked up a quarter of an inch or less of liquid precipitation before the system moved to the east of the area during the evening of December 26. Kern County Emergency Manager reported Southgate Dr. was closed between Chester Ave. and P St. due to flooding.", "ts_dict_index": [3417, 3418, 3419]}
+{"event_id": 801328, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2019-03-06 14:22:00", "end_date_time": "2019-03-06 16:22:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding at the intersection of Canal Dr. and South Ave. in Delhi.", "ts_dict_index": [3513, 3514, 3515]}
+{"event_id": 1079840, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-02-23 07:43:00", "end_date_time": "2023-02-23 07:43:00", "narrative": "An intense period of heavy snow and blizzard conditions, damaging winds, low-elevation snow and widespread flooding rainfall plagued Southern California February 21-27.||Very strong, and locally damaging, winds developed in the evening on February 21 and continued through February 22, especially impacting the coast and the mountains. Numerous trees were uprooted as a result of the strong winds. Temperatures plummeted on February 22 leading to low-elevation snow and cold-core thunderstorms.||The second, and highly impactful, next wave of the storm system enveloped Southern California starting on February 23. This is the period of heaviest snowfall, and a first-ever Blizzard Warning issued by NWS San Diego was in effect for the San Bernardino County Mountains. Heavy snowfall persisted through early morning on February 26, resulting in FEET of snowfall in the mountains, with many locations in the San Bernardino County Mountains seeing over 50 of snowfall. This resulted in hard closures of many highways in the San Bernardino County Mountains and left people trapped in their homes. Snow levels once again fell on February 25, with snow levels as low as 1000-2000 feet in the Inland Empire and inland Orange County. Widespread heavy thunderstorms occurred leading to local flooding, especially across San Diego County, inland Orange County and portions of the Inland Empire, as well as produced pea size hail.||The impacts of this system, especially in San Bernardino County, would be further exacerbated by an additional significant storm system that would hit only days later, leading to additional FEET of snow. Public report of flooding at Country Club Dip south of Harmony Grove Road, resulting in its closure.", "ts_dict_index": [3504, 3505, 3506]}
+{"event_id": 801324, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-03-06 08:26:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding on East Putnam Ave. in Porterville.", "ts_dict_index": [3519, 3520, 3521]}
+{"event_id": 1079839, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-02-25 07:06:00", "end_date_time": "2023-02-25 07:06:00", "narrative": "An intense period of heavy snow and blizzard conditions, damaging winds, low-elevation snow and widespread flooding rainfall plagued Southern California February 21-27.||Very strong, and locally damaging, winds developed in the evening on February 21 and continued through February 22, especially impacting the coast and the mountains. Numerous trees were uprooted as a result of the strong winds. Temperatures plummeted on February 22 leading to low-elevation snow and cold-core thunderstorms.||The second, and highly impactful, next wave of the storm system enveloped Southern California starting on February 23. This is the period of heaviest snowfall, and a first-ever Blizzard Warning issued by NWS San Diego was in effect for the San Bernardino County Mountains. Heavy snowfall persisted through early morning on February 26, resulting in FEET of snowfall in the mountains, with many locations in the San Bernardino County Mountains seeing over 50 of snowfall. This resulted in hard closures of many highways in the San Bernardino County Mountains and left people trapped in their homes. Snow levels once again fell on February 25, with snow levels as low as 1000-2000 feet in the Inland Empire and inland Orange County. Widespread heavy thunderstorms occurred leading to local flooding, especially across San Diego County, inland Orange County and portions of the Inland Empire, as well as produced pea size hail.||The impacts of this system, especially in San Bernardino County, would be further exacerbated by an additional significant storm system that would hit only days later, leading to additional FEET of snow. CalTrans report of flooding across both lanes of Foothill Drive due to heavy rain.", "ts_dict_index": [3507, 3508, 3509]}
+{"event_id": 1078264, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-17 05:00:00", "end_date_time": "2023-02-17 11:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. Portions of Germany Road were closed due to heavy runoff from prolonged rainfall.  No damage to the road was reported.", "ts_dict_index": [3486, 3487, 3488]}
+{"event_id": 1077837, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-17 07:50:00", "end_date_time": "2023-02-17 18:50:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. The stream gage at Anthony Creek near Anthony (ANYW2) crested at 15.87 feet (7,865 cfs) at 1:20 pm EST on 2/17/23.  This is roughly a 2-year event (50% AEP) per USGS Streamstats for this location and the highest crest on record since 2014.  The Anthony Creek basin received between 1.75 and 2.5 inches of rainfall in about a 24-hour period ending 8:00 AM EST on 2/17/23, falling over ground that was moistened by widespread rainfall on the 12th and 13th a few days prior.  There was no snow cover prior to this event.", "ts_dict_index": [3498, 3499, 3500]}
+{"event_id": 1078259, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-17 06:30:00", "end_date_time": "2023-02-17 10:30:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. The James River and Kanawha Turnpike was closed due to flooding of small creeks between the communities of Rainelle and Meadow Bluff.  The road was reopened after flooding receded, with no damage reported.", "ts_dict_index": [3501, 3502, 3503]}
+{"event_id": 1078257, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-17 07:30:00", "end_date_time": "2023-02-17 10:30:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. Brad Paisley community park was flooded up to the foundation of a pavilion there from water rising out of Wades Creek.  The park is located at the confluence of Wades Creek and Howard Creek.  No damage to the park was reported.", "ts_dict_index": [3489, 3490, 3491]}
+{"event_id": 1077865, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-17 21:00:00", "end_date_time": "2023-02-18 04:35:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. The Meadow River at Hines, WV crested at 14.15 feet (Flood stage is 14 feet).  This was caused by between 2.5 and 3.5 inches of rain over a 24-25 hour period. No snow melt or frozen ground was involved, but the ground was moist from widespread rainfall on the 12th and 13th a few days prior.  Water was observed creeping up to Highway 60 in the Hines and McRoss areas, but it is unknown if the highway was actually closed.", "ts_dict_index": [3492, 3493, 3494]}
+{"event_id": 1078270, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-17 10:00:00", "end_date_time": "2023-02-17 16:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. Portions of Highway 43 were reported to have standing water on them up to a foot deep.  The road was closed briefly to allow the water to run off.  No damage was reported.", "ts_dict_index": [3495, 3496, 3497]}
+{"event_id": 801337, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 15:00:00", "end_date_time": "2019-03-06 18:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. Kern County officials closed Panama Rd. between Malaga Rd. and Habecker Rd. in Lamont due to flooding.", "ts_dict_index": [3522, 3523, 3524]}
+{"event_id": 801270, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-05 21:10:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported flooding on one lane of northbound State Route 99 at Wilson Rd. in Bakersfield.", "ts_dict_index": [3525, 3526, 3527]}
+{"event_id": 801271, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 00:50:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding on San Emideo St. in Lamont.", "ts_dict_index": [3516, 3517, 3518]}
+{"event_id": 801329, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 14:30:00", "end_date_time": "2019-03-06 18:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. Kern County Emergency Manager reported Sierra Way was closed between State Route 178 and Hanning Flat due to flooding.", "ts_dict_index": [3528, 3529, 3530]}
+{"event_id": 801322, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 08:07:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. The Kern County superintendent of schools reported roadway flooding on Walker Basin Rd. and Caliente Creek Rd.", "ts_dict_index": [3534, 3535, 3536]}
+{"event_id": 801327, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 13:00:00", "end_date_time": "2019-03-06 18:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. Kern County Officials reported Tejon Highway closed between Panama Rd. and Mountain View Rd. 5N Arvin.", "ts_dict_index": [3510, 3511, 3512]}
+{"event_id": 1151012, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2023-12-18 09:55:00", "end_date_time": "2023-12-18 15:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the White Mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Localized moderate to major flooding occurred along mainstem rivers with the majority of New Hampshire Rivers outside of the mountains only reaching minor flood stage. Heavy rain and snowmelt caused rapid runoff that flooded a section of NH 109 just west of Wakefield.", "ts_dict_index": [3459, 3460, 3461]}
+{"event_id": 801319, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 07:09:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding at the intersection of Kelso Creek Rd. and Kelso Valley Rd. south of Weldon.", "ts_dict_index": [3543, 3544, 3545]}
+{"event_id": 801359, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 07:48:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported State Route 166 was closed from Basic School Rd. to State Route 33 in Maricopa due to flooding.", "ts_dict_index": [3537, 3538, 3539]}
+{"event_id": 801326, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 11:02:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding at the intersection of West China Grade Loop and Airport Dr.", "ts_dict_index": [3540, 3541, 3542]}
+{"event_id": 801279, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 06:28:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding at the intersection of 7th Standard Rd. and State Route 43 in Shafter.", "ts_dict_index": [3546, 3547, 3548]}
+{"event_id": 801325, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 08:53:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported the intersection of 7th Standard Rd. and Creek Rd. was completely flooded.", "ts_dict_index": [3531, 3532, 3533]}
+{"event_id": 801330, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2019-03-06 14:48:00", "end_date_time": "2019-03-06 16:48:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding at the intersection of Looney Rd. and East Ave.", "ts_dict_index": [3555, 3556, 3557]}
+{"event_id": 801340, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-03-06 15:57:00", "end_date_time": "2019-03-06 17:57:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported Outside Creek was overflowing onto State Route 137 between Tulare and Lindsay.", "ts_dict_index": [3549, 3550, 3551]}
+{"event_id": 1076259, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 07:51:00", "end_date_time": "2023-03-10 10:51:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on SR 201 at Rd. 156.", "ts_dict_index": [3594, 3595, 3596]}
+{"event_id": 1076258, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 07:48:00", "end_date_time": "2023-03-10 10:48:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on SR 198 west of Pierce Dr.", "ts_dict_index": [3600, 3601, 3602]}
+{"event_id": 1076292, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 11:13:00", "end_date_time": "2023-03-10 14:13:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a tree on SR 198 near Yokohl Dr.", "ts_dict_index": [3615, 3616, 3617]}
+{"event_id": 1076239, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 06:05:00", "end_date_time": "2023-03-10 09:05:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported Summit Dr. flooded near SR 198.", "ts_dict_index": [3603, 3604, 3605]}
+{"event_id": 1076315, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-03-10 13:10:00", "end_date_time": "2023-03-10 16:10:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a large boulder partially blocking the southbound lane of SR 41 south of Deadwood.", "ts_dict_index": [3609, 3610, 3611]}
+{"event_id": 1076275, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 08:50:00", "end_date_time": "2023-03-10 11:50:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a vehicle hydroplaned in high water on northbound SR 99 between Traver and Kingsburg.", "ts_dict_index": [3612, 3613, 3614]}
+{"event_id": 801338, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2019-03-06 15:11:00", "end_date_time": "2019-03-06 17:11:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding at the intersection of Westside Blvd. and Washington Blvd.", "ts_dict_index": [3561, 3562, 3563]}
+{"event_id": 1076330, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 15:59:00", "end_date_time": "2023-03-10 18:59:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. Image shown on Twitter showing the River Island Country Club in Springville flooded.", "ts_dict_index": [3591, 3592, 3593]}
+{"event_id": 1069121, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-02-05 02:00:00", "end_date_time": "2023-02-05 04:00:00", "narrative": "A fairly strong upper low pressure system moved eastward across northern California on February 5 with precipitation from this system extending southward into central California between the evening of February 4 and the evening of February 5. This system brought 0.75 to 1.5 inches of liquid precipitation to the Sierra Nevada with the snow level running around 6500 feet during the evening of February 4 lowering to around 4000 feet by time the precipitation tapered off during the evening of February 5. SNOTEL estimates indicated between 9 and 15 inches of new snow fell above 6500 feet from Fresno County northward. Between 0.25 to 0.75 inches of rain fell in the Sierra foothills and 0.10 to 0.25 inches of rain fell in the San Joaquin Valley. Precipitation in the Tehachapi Mountains varied due to the showery nature of the precipitation by the time it arrived in Kern County, but many stations picked up between 1 and 3 tenths of an inch of liquid precipitation. Traffic was paced along Interstate 5 by the evening a February 5 as light snow began to accumulate along the Tejon Pass. This system also brought some strong wind gusts to the Mohave Desert slopes with several stations reporting gusts exceeding 45 mph and a few low impact indicator sites briefly measuring gusts above 60 mph. As the colder post-frontal airmass pushed into the area during the afternoon of February 5, scattered thunderstorms broke out over the San Joaquin Valley with a few reports of trees being knocked down by strong thunderstorm wind gusts and pea sized hail being reported. California Highway Patrol reported a tree and large rocks washed up in the roadway on SR 140 and the Ferguson Slide Bridge.", "ts_dict_index": [3579, 3580, 3581]}
+{"event_id": 1076277, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 09:27:00", "end_date_time": "2023-03-10 12:27:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on Pine Flat Rd. at Deer Creek Mill Rd.", "ts_dict_index": [3597, 3598, 3599]}
+{"event_id": 801273, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 03:53:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding on Lake Isabella Blvd. northeast of Erskine Creek Rd.", "ts_dict_index": [3576, 3577, 3578]}
+{"event_id": 801274, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 04:35:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported approximately four inches of water across Highline Rd. between Turf St. and South Dennison Rd. in Tehachapi.", "ts_dict_index": [3570, 3571, 3572]}
+{"event_id": 801339, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 15:30:00", "end_date_time": "2019-03-06 18:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. Kern County officials closed South Edison Rd. from Digirogio Rd. to Mountain View Rd. in Lamont due to flooding.", "ts_dict_index": [3567, 3568, 3569]}
+{"event_id": 801272, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 02:29:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding at the intersection of Roberts Ln. and Hart St. in Bakersfield.", "ts_dict_index": [3558, 3559, 3560]}
+{"event_id": 801320, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 07:12:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported the westbound lane of State Route 119 flooded for two miles west of the intersection of Buena Vista Rd.", "ts_dict_index": [3573, 3574, 3575]}
+{"event_id": 872117, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2020-03-13 04:26:00", "end_date_time": "2020-03-13 06:56:00", "narrative": "Severe thunderstorms downed trees and powerlines, while also causing damage to some buildings and homes across McCreary County during the late evening hours of March 12th.||One of these storms produced an EF-1 tornado just north of downtown Whitley City. A supercell thunderstorm tracked across McCreary County during the late evening hours of March 12th. A National Weather Service Jackson survey team found intermittent damage along the entire path. There were three distinct areas of damage where the tornado touched down. On Chitwood Ridge Rd, several hardwood trees were snapped off. There was also a house that sustained some roof damage. The next area of tornado damage was on the northern side of Whitley City along north Highway 1651, where more hardwood trees were snapped off along with some damage to a few two-story buildings. Finally, the third area of tornado damage was northeast of Whitley City on Stephens Farm Rd. A tree landed on a house, leading to major damage. There were also several more houses with roof damage and additional trees snapped off.||Large hail was also reported in McCreary and Wayne Counties as these strong to severe thunderstorms moved through. Additionally, periodic heavy and training rainfall led to flooding in portions of Floyd and Pike Counties as localized amounts of 2-3 inches fell early on March 13th. Floyd County was forced to declare a State of Emergency as low-lying portions of Abbott Creek along Kentucky Highway 1427 and Middle Creek Levisa Fork along Kentucky Highway 114 were hit hard. Emergency Management reported water from Abbott Creek was approaching the foundation of several low lying homes along Kentucky Highway 1427 east of Bonanza. Over one foot of water made it into a few homes, causing major damage.", "ts_dict_index": [3582, 3583, 3584]}
+{"event_id": 801275, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 05:27:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported three vehicles stuck in water and unable to move near the intersection of State Route 33 and State Route 46.", "ts_dict_index": [3564, 3565, 3566]}
+{"event_id": 1076314, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 13:08:00", "end_date_time": "2023-03-10 16:08:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a boulder on the roadway on eastbound SR 178 3 to 4 miles west of Democrat Rd.", "ts_dict_index": [3618, 3619, 3620]}
+{"event_id": 872116, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2020-03-13 03:30:00", "end_date_time": "2020-03-13 05:45:00", "narrative": "Severe thunderstorms downed trees and powerlines, while also causing damage to some buildings and homes across McCreary County during the late evening hours of March 12th.||One of these storms produced an EF-1 tornado just north of downtown Whitley City. A supercell thunderstorm tracked across McCreary County during the late evening hours of March 12th. A National Weather Service Jackson survey team found intermittent damage along the entire path. There were three distinct areas of damage where the tornado touched down. On Chitwood Ridge Rd, several hardwood trees were snapped off. There was also a house that sustained some roof damage. The next area of tornado damage was on the northern side of Whitley City along north Highway 1651, where more hardwood trees were snapped off along with some damage to a few two-story buildings. Finally, the third area of tornado damage was northeast of Whitley City on Stephens Farm Rd. A tree landed on a house, leading to major damage. There were also several more houses with roof damage and additional trees snapped off.||Large hail was also reported in McCreary and Wayne Counties as these strong to severe thunderstorms moved through. Additionally, periodic heavy and training rainfall led to flooding in portions of Floyd and Pike Counties as localized amounts of 2-3 inches fell early on March 13th. Floyd County was forced to declare a State of Emergency as low-lying portions of Abbott Creek along Kentucky Highway 1427 and Middle Creek Levisa Fork along Kentucky Highway 114 were hit hard. A trained spotter observed water from Middle Creek Levisa Fork threatening low lying homes along Kentucky Highway 114 near Dotson.", "ts_dict_index": [3585, 3586, 3587]}
+{"event_id": 1076240, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 06:11:00", "end_date_time": "2023-03-10 09:11:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported SR 198 flooded in Three Rivers.", "ts_dict_index": [3624, 3625, 3626]}
+{"event_id": 1150889, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2023-12-18 09:00:00", "end_date_time": "2023-12-18 09:00:00", "narrative": "Low pressure began organizing in the Gulf of Mexico on the 16th, setting record low sea level pressures as it traversed the Southeast through the 17th. Strong high pressure over the North Atlantic created a deep southeasterly flow that drew warm air into New England ahead of the approaching storm. By the time precipitation arrived on the evening of the 17th, temperatures were warm enough for rain everywhere except the highest peaks. Early on the 18th a shortwave trough was approaching from the Great Lakes and led to rapid deepening of the low pressure as it paralleled the Eastern Seaboard. Even as the center of the storm remained near Chesapeake Bay on the morning of the 18th, a strong low level jet had developed and winds began to gust in excess of 50 mph well inland from the coast. Damaging wind gusts continued into the afternoon. Thousands of customers lost power due to falling limbs and downed wires. The anomalously warm air mass also led to intense rainfall rates beginning on the evening of the 17th, which continued into the 18th. Upsloping winds also enhanced precipitation along the southeast facing slopes of the White Mountains. Widespread 3 to 4 inches of rain fell, with isolated pockets of 6 to 8 inches. This fell on top of snow that was ripe from previous rainfall about a week earlier. An additional 2 to 3 inches of snow water equivalent was likely added to rainfall runoff. Numerous road washouts and road closures occurred due to flash flooding and fast responding small stream and tributaries. Localized moderate to major flooding occurred along mainstem rivers with the majority of New Hampshire Rivers outside of the mountains only reaching minor flood stage. Severe flooding occurred in Bartlett and upstream in Hart's Location, New Hampshire on December 18th. The flooding was the result of heavy rain and rapid snowmelt along the steep slopes of the south facing mountains around Bartlett. The combined runoff from rainfall and snowmelt is estimated to be around 10 inches. The steep terrain and frozen ground resulted in very rapid runoff with flash flooding occurring along every small stream and brook in the region.  The USGS river gage at Bartlett went from 3 feet at 9 PM on the 17th, to 13.8 feet by noon on the 18th. The discharge was measured over 25 kcfs, which has an annual chance exceedance of 1% to 0.2%, otherwise referred to as a 100 to 500 year flood. The river stage reached was the 3rd highest on record, and a foot below that reached during Irene in 2011.   The hardest hit areas were the confluence of the Saco River, the Rocky Branch and at the confluence of the Ellis River. Route 302, a main thruway to the region closed from Glen to Jericho due to severe flooding. West Side Road was flooded along with numerous homes and camps. In Bartlett, the flood waters flooding River Street up to Route 302. Additionally, several local road closures and washouts were reported along the Saco and other small streams and brooks.  There was significant damage to a campground in Bartlett and another in Glen Ellis.", "ts_dict_index": [3477, 3478, 3479]}
+{"event_id": 1076001, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 05:49:00", "end_date_time": "2023-03-10 08:49:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding, rocks and debris on SR 198 east of Encina Ave. in Three Rivers.", "ts_dict_index": [3636, 3637, 3638]}
+{"event_id": 1076316, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 13:14:00", "end_date_time": "2023-03-10 16:14:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a tree on the roadway on SR 65 at the Olive Ave. offramp.", "ts_dict_index": [3627, 3628, 3629]}
+{"event_id": 1076260, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 07:53:00", "end_date_time": "2023-03-10 10:53:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported mud, dirt and rocks on Dry Creek Dr. at SR 216.", "ts_dict_index": [3630, 3631, 3632]}
+{"event_id": 1076256, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 07:38:00", "end_date_time": "2023-03-10 10:38:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a spinout in high water on northbound SR 99 where a car crashed into the center divide.", "ts_dict_index": [3588, 3589, 3590]}
+{"event_id": 1076274, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-03-10 08:44:00", "end_date_time": "2023-03-10 11:44:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported 40 feet of mud on Road 200.", "ts_dict_index": [3657, 3658, 3659]}
+{"event_id": 1076278, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 09:34:00", "end_date_time": "2023-03-10 12:34:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on Rd. 172 north of Ave. 352.", "ts_dict_index": [3648, 3649, 3650]}
+{"event_id": 1076317, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 13:23:00", "end_date_time": "2023-03-10 16:23:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on Rd. 60 north of Ave. 328.", "ts_dict_index": [3654, 3655, 3656]}
+{"event_id": 1076329, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 15:45:00", "end_date_time": "2023-03-10 18:45:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. Video posted on Twitter showing flooding in Exeter.", "ts_dict_index": [3660, 3661, 3662]}
+{"event_id": 1076264, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 08:00:00", "end_date_time": "2023-03-10 11:00:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a landslide blocking the eastbound lanes of SR 190 at Pleasant Oak Dr.", "ts_dict_index": [3669, 3670, 3671]}
+{"event_id": 801277, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-03-06 05:37:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. California Highway Patrol reported roadway flooding on Norris Rd. near the intersection of Knudsen Dr.", "ts_dict_index": [3552, 3553, 3554]}
+{"event_id": 1076324, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 14:21:00", "end_date_time": "2023-03-10 17:21:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported roadway flooding and debris in the creek on Rd. 192 and Ave. 96.", "ts_dict_index": [3687, 3688, 3689]}
+{"event_id": 1076312, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 12:58:00", "end_date_time": "2023-03-10 15:58:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding and a possible road washed out near Rd. 264 and Ave. 116.", "ts_dict_index": [3684, 3685, 3686]}
+{"event_id": 1075993, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 05:03:00", "end_date_time": "2023-03-10 08:03:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on westbound SR 198 at the Linwood Ave. overcrossing.", "ts_dict_index": [3690, 3691, 3692]}
+{"event_id": 1076290, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 10:44:00", "end_date_time": "2023-03-10 13:44:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. Video posted on Facebook showing Globe Dr. flooded by the Tule River in Springville.", "ts_dict_index": [3675, 3676, 3677]}
+{"event_id": 1075991, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 05:00:00", "end_date_time": "2023-03-10 08:00:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding across all four lanes on Ave 196 at Rd. 230.", "ts_dict_index": [3681, 3682, 3683]}
+{"event_id": 1076248, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-03-10 07:00:00", "end_date_time": "2023-03-10 10:00:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported boulders on Rd. 600 1 miles south of SR 49.", "ts_dict_index": [3678, 3679, 3680]}
+{"event_id": 1076304, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-03-10 12:27:00", "end_date_time": "2023-03-10 15:27:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a foot deep puddle on eastbound SR 152 near the Romero Visitor Center.", "ts_dict_index": [3693, 3694, 3695]}
+{"event_id": 1075990, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 04:45:00", "end_date_time": "2023-03-10 07:45:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on Rd. 180 between N Anderson Rd. and Ave 288.", "ts_dict_index": [3705, 3706, 3707]}
+{"event_id": 1076328, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-03-10 14:57:00", "end_date_time": "2023-03-10 17:57:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported rocks, mud and dirt blocking a lane of Jerseydale Rd. and Triangle Rd. This area was affected by the Oak Fire.", "ts_dict_index": [3708, 3709, 3710]}
+{"event_id": 1076257, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 07:47:00", "end_date_time": "2023-03-10 10:47:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported softball sized rocks washed up on the roadway on eastbound SR 178 at Walker Pass.", "ts_dict_index": [3639, 3640, 3641]}
+{"event_id": 1076326, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 14:32:00", "end_date_time": "2023-03-10 17:32:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported that Balch Park Rd. near Yokohl Valley Dr. was about to give out.", "ts_dict_index": [3723, 3724, 3725]}
+{"event_id": 1076287, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-03-10 10:25:00", "end_date_time": "2023-03-10 13:25:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a mudslide on SR 41 near Victoria Ln.", "ts_dict_index": [3717, 3718, 3719]}
+{"event_id": 1076282, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 09:57:00", "end_date_time": "2023-03-10 12:57:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on Rd. 172 at Ave. 352.", "ts_dict_index": [3711, 3712, 3713]}
+{"event_id": 1076253, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 07:25:00", "end_date_time": "2023-03-10 10:25:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported SR 190 flooded at Coffee Camp.", "ts_dict_index": [3735, 3736, 3737]}
+{"event_id": 1075992, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 05:00:00", "end_date_time": "2023-03-10 08:00:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a spinout in high water on SR 198 east of Lovers Lane.", "ts_dict_index": [3744, 3745, 3746]}
+{"event_id": 1076252, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-03-10 07:20:00", "end_date_time": "2023-03-10 10:20:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported mud, dirt and rocks on SR 140 at Briceburg.", "ts_dict_index": [3738, 3739, 3740]}
+{"event_id": 1076263, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 08:00:00", "end_date_time": "2023-03-10 11:00:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported SR 155 closed due to flooding between Woody and Glennville.", "ts_dict_index": [3732, 3733, 3734]}
+{"event_id": 1076325, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 14:30:00", "end_date_time": "2023-03-10 17:30:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported SR 155 was closed due to flooding between Shady Oak Ln. and Marina Dr.", "ts_dict_index": [3756, 3757, 3758]}
+{"event_id": 1076307, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 12:32:00", "end_date_time": "2023-03-10 15:32:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on Ave 280 near N. Anderson Rd.", "ts_dict_index": [3765, 3766, 3767]}
+{"event_id": 1076310, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 12:39:00", "end_date_time": "2023-03-10 15:39:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. Video posted on Twitter showing flooding in Springville.", "ts_dict_index": [3768, 3769, 3770]}
+{"event_id": 1076319, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 13:27:00", "end_date_time": "2023-03-10 16:27:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported Caliente Bodfish Rd. collapsed near Clear Creek Rd.", "ts_dict_index": [3771, 3772, 3773]}
+{"event_id": 1076323, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 14:21:00", "end_date_time": "2023-03-10 17:21:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on Ave. 192 near Rd. 196.", "ts_dict_index": [3774, 3775, 3776]}
+{"event_id": 1076281, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 09:47:00", "end_date_time": "2023-03-10 12:47:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on SR 155 near Old State Rd.", "ts_dict_index": [3663, 3664, 3665]}
+{"event_id": 1076303, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 12:22:00", "end_date_time": "2023-03-10 15:22:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on S. Thompson Rd. near E. Klindera Ave. in Tipton.", "ts_dict_index": [3777, 3778, 3779]}
+{"event_id": 1075988, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-03-10 04:36:00", "end_date_time": "2023-03-10 07:36:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported dirt, rocks and mud on SR 41 near Old Corral Rd.", "ts_dict_index": [3789, 3790, 3791]}
+{"event_id": 1076266, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-03-10 08:10:00", "end_date_time": "2023-03-10 11:10:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported rocks, mud and dirt blocking SR 41 north of Cedar Valley Dr.", "ts_dict_index": [3783, 3784, 3785]}
+{"event_id": 1076321, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 13:40:00", "end_date_time": "2023-03-10 16:40:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported the number 1 lane on southbound SR 99 south of Rosedale highway was flooded.", "ts_dict_index": [3792, 3793, 3794]}
+{"event_id": 1076300, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 12:16:00", "end_date_time": "2023-03-10 15:16:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. Social media report of flooding of the Kern River in Kernville.", "ts_dict_index": [3798, 3799, 3800]}
+{"event_id": 1076268, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 08:21:00", "end_date_time": "2023-03-10 11:21:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on W. Addle Ave. at S. Pratt St.", "ts_dict_index": [3699, 3700, 3701]}
+{"event_id": 1076283, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 09:58:00", "end_date_time": "2023-03-10 12:58:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported a road closure due to flooding on SR 201 between Rd. Rd. 156 and Rd. 164.", "ts_dict_index": [3804, 3805, 3806]}
+{"event_id": 1076265, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 08:01:00", "end_date_time": "2023-03-10 11:01:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported on SR 201 west of SR 245.", "ts_dict_index": [3807, 3808, 3809]}
+{"event_id": 1076299, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2023-03-10 12:08:00", "end_date_time": "2023-03-10 15:08:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on eastbound SR 198 east of 18th Ave.", "ts_dict_index": [3801, 3802, 3803]}
+{"event_id": 1076244, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 06:46:00", "end_date_time": "2023-03-10 09:46:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported Mil Portero Highway was closed at Cuddy Valley Rd. due to flooding.", "ts_dict_index": [3813, 3814, 3815]}
+{"event_id": 1076279, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-03-10 09:45:00", "end_date_time": "2023-03-10 12:45:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding, snow and debris on Oak Rd. neat Yosemite Oaks Dr.", "ts_dict_index": [3819, 3820, 3821]}
+{"event_id": 1076255, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 07:34:00", "end_date_time": "2023-03-10 10:34:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported on SR 198 at Sierra Dr.", "ts_dict_index": [3837, 3838, 3839]}
+{"event_id": 1076291, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 11:06:00", "end_date_time": "2023-03-10 14:06:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on E. Fir St. between Foothill Ave. and Hillcrest Ave.", "ts_dict_index": [3831, 3832, 3833]}
+{"event_id": 1076246, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 06:59:00", "end_date_time": "2023-03-10 09:59:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported eastbound SR 190 flooded west of Pleasant Oak Dr.", "ts_dict_index": [3861, 3862, 3863]}
+{"event_id": 1075995, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 05:14:00", "end_date_time": "2023-03-10 08:14:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol and the Tulare County Fire Department reported rocks in the roadway on Lemon Rd. near SR 198.", "ts_dict_index": [3840, 3841, 3842]}
+{"event_id": 1076271, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 08:35:00", "end_date_time": "2023-03-10 11:35:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported water a foot deep on Rd. 144 at Ave. 142.", "ts_dict_index": [3852, 3853, 3854]}
+{"event_id": 1076251, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 07:19:00", "end_date_time": "2023-03-10 10:19:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported mud/dirt and rocks on Hot Springs Rd.", "ts_dict_index": [3846, 3847, 3848]}
+{"event_id": 1076302, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 12:20:00", "end_date_time": "2023-03-10 15:20:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on SR 137 east of Rd. 152.", "ts_dict_index": [3876, 3877, 3878]}
+{"event_id": 1076272, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 08:38:00", "end_date_time": "2023-03-10 11:38:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on SR 137 at Road 152.", "ts_dict_index": [3858, 3859, 3860]}
+{"event_id": 1076320, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 13:28:00", "end_date_time": "2023-03-10 16:28:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported SR 65 flooded near E. List Ave.", "ts_dict_index": [3864, 3865, 3866]}
+{"event_id": 885466, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2020-05-18 17:00:00", "end_date_time": "2020-05-18 18:00:00", "narrative": "A low pressure system dropped southward off the northern California coast on May 17 than moved inland across central California on May 18. As a result, precipitation spread southward across the area north of Fresno County during the evening of May 17 and became widespread across our area on May 18. Several stations in the Sierra Nevada picked up between an inch and 2.50 inches of liquid precipitation while a few stations from Madera County northward picked up between 2.50 and 3.25 inches of liquid precipitation. Snow levels were between 8000 to 9000 feet early on, but lowered to around 6000 feet by the afternoon of May 18. Several higher elevation SNOTEL stations picked up between 2 and 6 inches of new snowfall while a few stations picked up 7 inches or more. As a cooler airmass pushed into the area during the afternoon of May 18, thunderstorms developed during the afternoon. One thunderstorm produced nuisance roadway flooding near Riverdale while another produced nuisance roadway flooding near Parlier. A third thunderstorm produced a funnel cloud near North Fork. Finally, This system produced a period of strong winds over the Kern County Deserts as well as over the Lake Isabella and Tehachapi areas between the evening of May 18 and the morning of May 19.  Several stations in these areas reported wind gusts between 45 and 60 mph. A few low impact indicator sites reported gusts between 60 and 70 mph. The winds diminished by late morning on May 19 as the storm moved out of the area. Public report of roadway flooding and half inch hail in Parlier.", "ts_dict_index": [3891, 3892, 3893]}
+{"event_id": 1076297, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 11:56:00", "end_date_time": "2023-03-10 14:56:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. A social media video was posted of a water rescue on the Tule River in Springville.", "ts_dict_index": [3867, 3868, 3869]}
+{"event_id": 1075989, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-03-10 04:40:00", "end_date_time": "2023-03-10 07:40:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported water and debris flooding SR 41 in the southern part of Oakhurst.", "ts_dict_index": [3870, 3871, 3872]}
+{"event_id": 1076254, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-03-10 07:30:00", "end_date_time": "2023-03-10 10:30:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on Hot Springs Rd. east of Old Stage Rd.", "ts_dict_index": [3843, 3844, 3845]}
+{"event_id": 1063315, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-05 16:24:00", "end_date_time": "2023-01-05 18:24:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Public report of flooding at the intersection of Ave. 416 and Rd. 127 in Orosi.", "ts_dict_index": [3906, 3907, 3908]}
+{"event_id": 881935, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2020-05-18 16:14:00", "end_date_time": "2020-05-18 18:00:00", "narrative": "A low pressure system dropped southward off the northern California coast on May 17 than moved inland across central California on May 18. As a result, precipitation spread southward across the area north of Fresno County during the evening of May 17 and became widespread across our area on May 18. Several stations in the Sierra Nevada picked up between an inch and 2.50 inches of liquid precipitation while a few stations from Madera County northward picked up between 2.50 and 3.25 inches of liquid precipitation. Snow levels were between 8000 to 9000 feet early on, but lowered to around 6000 feet by the afternoon of May 18. Several higher elevation SNOTEL stations picked up between 2 and 6 inches of new snowfall while a few stations picked up 7 inches or more. As a cooler airmass pushed into the area during the afternoon of May 18, thunderstorms developed during the afternoon. One thunderstorm produced nuisance roadway flooding near Riverdale while another produced nuisance roadway flooding near Parlier. A third thunderstorm produced a funnel cloud near North Fork. Finally, This system produced a period of strong winds over the Kern County Deserts as well as over the Lake Isabella and Tehachapi areas between the evening of May 18 and the morning of May 19.  Several stations in these areas reported wind gusts between 45 and 60 mph. A few low impact indicator sites reported gusts between 60 and 70 mph. The winds diminished by late morning on May 19 as the storm moved out of the area. An NWS Employee observed roadway flooding just west of Riverdale at the intersection of |W. Mount Whitney Ave and S. Brawley Ave.", "ts_dict_index": [3894, 3895, 3896]}
+{"event_id": 1076327, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 14:33:00", "end_date_time": "2023-03-10 17:33:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding on northbound SR 99 south of Wilson Rd. in Bakersfield.", "ts_dict_index": [3825, 3826, 3827]}
+{"event_id": 964717, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2021-07-09 07:37:00", "end_date_time": "2021-07-09 08:37:00", "narrative": "Several days of heavy to torrential rains and gusty winds were experienced across eastern Kentucky from July 9th through the 12th. A strong surface low pressure remained parked across Illinois to our WNW, with a frontal boundary expanding eastward and through Kentucky, sinking just south of the state to start the day on the 9th. During the day on the 9th and the 10th, the front began lifting northward through eastern Kentucky as a warm front, becoming the center for convective development, and also allowing for much deeper warm air and moisture advection into the region. As the front slowly continued just north of the state on the 11th and 12th, Kentucky found itself in the warm and unstable sector of the system, with showers and thunderstorms developing, peaking in coverage and intensity during the afternoon hours. ||Given the warm environment, storms were generally low centroid and moisture laden, exhibiting well above normal PWats, in the 2 to 2.5 inch range. Soundings also showed shallow inverted V signatures, indicative of steep low level lapse rates and the ability to easily mix down higher winds aloft. Pulsy scattered convection with heavy rain and high wind gusts were the main concerns. Locations where multiple storms moved over saw high water and some instances of flash flooding. Other locations experienced thunderstorm wind damage as stronger winds transferred to the surface, especially as the storms were beginning the dissipating phase. ||An 850 jet SW to NE, storms that NW to SE oriented were bowing. Minor flooding of a structure occurred in Grethel.", "ts_dict_index": [3888, 3889, 3890]}
+{"event_id": 1063314, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-05 16:13:00", "end_date_time": "2023-01-05 18:13:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Public report of a downed tree washed up on SR 178 near where the road splits into four lanes.", "ts_dict_index": [3909, 3910, 3911]}
+{"event_id": 1076301, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-03-10 12:16:00", "end_date_time": "2023-03-10 15:16:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. Social media report showing Riverside Park in Kernville flooded.", "ts_dict_index": [3879, 3880, 3881]}
+{"event_id": 1063323, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-05 19:54:00", "end_date_time": "2023-01-05 21:54:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Public report of mud, dirt and rocks on the eastbound lanes of SR 198 near the Mineral King Rd. exchange.", "ts_dict_index": [3921, 3922, 3923]}
+{"event_id": 1063324, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-05 20:14:00", "end_date_time": "2023-01-05 22:14:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Public report of a rockslide blocking northbound lanes of SR 49 a quarter mile south of Bagby.", "ts_dict_index": [3942, 3943, 3944]}
+{"event_id": 1063309, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-05 15:01:00", "end_date_time": "2023-01-05 17:01:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Public report of flooding on the eastbound SR 198 offramp onto Mooney Blvd. in Visalia.", "ts_dict_index": [3924, 3925, 3926]}
+{"event_id": 1063300, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-05 06:25:00", "end_date_time": "2023-01-05 08:25:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. California Highway Patrol reported debris blocking both lanes on SR 41 at Miami Motorcycle Trail.", "ts_dict_index": [3933, 3934, 3935]}
+{"event_id": 1063294, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-05 04:52:00", "end_date_time": "2023-01-05 06:52:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. California Highway Patrol reported roadway flooding on SR 59 near the Merced County Regional Waste Landfill.", "ts_dict_index": [3945, 3946, 3947]}
+{"event_id": 1063227, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-04 22:20:00", "end_date_time": "2023-01-05 00:20:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. California Highway Patrol reported a traffic collision near the intersection of Libson Rd. and S. Bert Crane Rd. in Merced County. The response found the roadway to be completely flooded.", "ts_dict_index": [3930, 3931, 3932]}
+{"event_id": 1063303, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-05 07:35:00", "end_date_time": "2023-01-05 09:35:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. California Highway Patrol reported water two feet into the roadway in the northbound lane on G St. near Snelling Rd.", "ts_dict_index": [3954, 3955, 3956]}
+{"event_id": 1063305, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-05 13:33:00", "end_date_time": "2023-01-05 15:33:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Public report that the right lane of eastbound SR 198 at the SR 99 exchange is completely flooded with 8 feet of water into the lane.", "ts_dict_index": [3966, 3967, 3968]}
+{"event_id": 1063318, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-05 16:44:00", "end_date_time": "2023-01-05 18:44:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Public report of Rd. 132 just south of Ave. 384 flooded for two miles.", "ts_dict_index": [3969, 3970, 3971]}
+{"event_id": 1063235, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2023-01-05 00:50:00", "end_date_time": "2023-01-05 02:50:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. California Highway Patrol reported a large rockslide blocking the roadway on SR 41 southwest of the intersection with SR 33.", "ts_dict_index": [3978, 3979, 3980]}
+{"event_id": 1063317, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-05 16:43:00", "end_date_time": "2023-01-05 18:43:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Public report of flooding east of the intersection of August Ave. and SR 165 in Hilmar with the roadway torn up.", "ts_dict_index": [3972, 3973, 3974]}
+{"event_id": 1063304, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-05 11:07:00", "end_date_time": "2023-01-05 19:07:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. California Highway Patrol reported that Redrock-Randsburg Rd. was closed between SR 14 and Garlock due to flooding.", "ts_dict_index": [3963, 3964, 3965]}
+{"event_id": 1063319, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-05 16:58:00", "end_date_time": "2023-01-05 18:58:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Public report of a boulder in the roadway on Poso Flat Rd. east of the exchange with Granite Rd.", "ts_dict_index": [3975, 3976, 3977]}
+{"event_id": 1048480, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2022-07-27 08:50:00", "end_date_time": "2022-07-27 09:00:00", "narrative": "A stationary front was observed situated south of the Ohio River across northern Kentucky and West Virginia during July 26th when an upper level disturbance approached the state from the west late that evening. A 30 to 35 mph nocturnal low level jet developed just south of the boundary, tapping deep moisture in place across central Kentucky, carrying it northeast toward Greenbrier County, resulting in deep moisture convergence across the area. Precipitable water values were estimated to have risen from around 1.7 inches around 10 pm on the 26th to nearly 2 inches by around 6 am on the 27th, or two standard deviations above normal for late July. Given the latent heat of the tropical air being carried toward southeast West Virginia, most-unstable layer CAPE values were estimated to be between 500 and 1,000 J/Kg just after midnight on the 27th. Soils were already moistened from 0.5 to locally 1.5 inches of rain that fell during early afternoon on the 26th when another round of storms developed across the western part of the county beginning around 10 pm. Perhaps enhanced by upsloping as the storms entered the higher terrain across the western half of the county, the low-topped convection proved to be efficient, producing prolonged 1 to 2 inch per hour rainfall rates in multiple waves. The heaviest rainfall began to diminish by 5 am on the 27th, leaving only residual shower activity after dropping a large swath of 2 to over 4 inches within the 7 hour period. Sewell Creek above Little Sewell Creek at Rainelle (RANW2) crested right at flood stage of 14.00 feet at 9:50 am to 10:00 am EDT on the 27th.", "ts_dict_index": [3984, 3985, 3986]}
+{"event_id": 1076284, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-03-10 09:59:00", "end_date_time": "2023-03-10 12:59:00", "narrative": "A large upper trough off the Pacific Northwest coast pulled up a deep moisture fetch from the Pacific Ocean which spread inland into central California on March 9 and 10. This atmospheric river event produced 4 to 8 inches of liquid precipitation across much of the Sierra Nevada. With this moisture being of tropical origin, snow levels were high and were above 9500 feet for much of this event. The rain falling on top of a large snowpack over the Sierra Nevada produced a large amount of runoff resulting in widespread catastrophic flooding over the San Joaquin Valley, the valley facing slopes as well as across the Sierra foothills with over 100 reports of flooding being reported to WFO Hanford. The conditions were made worse by the fact that soils already very saturated over the lower elevations from previous storms. In addition, the Sierra foothills generally picked up between 2 and 5 inches of rainfall while the San Joaquin Valley had between 0.75 to 1.5 inches of rainfall. Flash Flood Emergencies were issued for the Springville area in Tulare County and for the Kernville and Wofford Heights area in Kern County near Lake Isabella for life threatening flooding caused by heavy rainfall on top of snowmelt runoff from higher elevations. By the time the deep moisture fetch moved out of the area during the evening of March 10, several communities were evacuated due to the widespread flooding and numerous roads were closed for several days either because of flooding or because repairs were required to make the roads usable. California Highway Patrol reported flooding a quarter mile from SR 41 on Serpa Canyon Rd.", "ts_dict_index": [3882, 3883, 3884]}
+{"event_id": 1121920, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2023-07-09 13:18:00", "end_date_time": "2023-07-09 18:15:00", "narrative": "A strong upper-level system brought widespread rounds of showers and thunderstorms to eastern New York on July 9-11, 2023. The steadiest and heaviest rainfall occurred during the afternoon hours on July 9, the early morning hours on July 10 and during the evening hours on July 10 into the overnight hours on July 11. Rainfall totals varied greatly from region to region but the hardest hit areas (Hudson Valley and into northeastern Hamilton County) received 3 to 6 inches of rainfall.||Areal and flash flooding was primarily focused across areas along the Hudson River on July 9-10. Damage consisted of closed and washed out roads. A section of Metro-North's railroad tracks were washed out due to flood waters from Poughkeepsie southward.||The combination of heavy rain and beaver dam failures resulted in destruction of roads, bridges and sidewalks across northeastern Hamilton County during the early morning hours on July 11 focused on the areas of Long Lake and Blue Mountain Lake. A State of Emergency was declared for the towns of Long Lake and Indian Lake. New York Governor Kathy Hochul declared a State of Emergency for Hamilton County. Hamilton County Emergency Manager estimated damage to be in the millions of dollars.||In addition to the heavy rainfall, a few severe thunderstorms also developed across portions of the Hudson Valley leading to downed trees and wires. A lightning strike caused an auto body shop to catch fire. Creek Road was flooded near Accord in the Town of Rochester.", "ts_dict_index": [4008, 4009, 4010]}
+{"event_id": 1043035, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2022-07-27 15:20:00", "end_date_time": "2022-07-28 08:45:00", "narrative": "A stationary front was observed situated south of the Ohio River across northern Kentucky and West Virginia during July 26th when an upper level disturbance approached the state from the west late that evening. A 30 to 35 mph nocturnal low level jet developed just south of the boundary, tapping deep moisture in place across central Kentucky, carrying it northeast toward Greenbrier County, resulting in deep moisture convergence across the area. Precipitable water values were estimated to have risen from around 1.7 inches around 10 pm on the 26th to nearly 2 inches by around 6 am on the 27th, or two standard deviations above normal for late July. Given the latent heat of the tropical air being carried toward southeast West Virginia, most-unstable layer CAPE values were estimated to be between 500 and 1,000 J/Kg just after midnight on the 27th. Soils were already moistened from 0.5 to locally 1.5 inches of rain that fell during early afternoon on the 26th when another round of storms developed across the western part of the county beginning around 10 pm. Perhaps enhanced by upsloping as the storms entered the higher terrain across the western half of the county, the low-topped convection proved to be efficient, producing prolonged 1 to 2 inch per hour rainfall rates in multiple waves. The heaviest rainfall began to diminish by 5 am on the 27th, leaving only residual shower activity after dropping a large swath of 2 to over 4 inches within the 7 hour period. The Meadow River crested at a stage of 13.96 feet at 11:30 pm EDT on the 27th, and remained above 13 feet from 4:20 pm EDT on the 27th to 9:45 am EDT on the 28th.  The river appeared out of its banks at multiple locations along Highway 60 between the communities of Rupert and Rainelle, causing the highway to be closed until flood waters receded.", "ts_dict_index": [3987, 3988, 3989]}
+{"event_id": 912739, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2020-09-13 11:00:00", "end_date_time": "2020-09-13 15:00:00", "narrative": "Deep moisture anchored across east Kentucky, combined with a stalled frontal boundary, then a cold front, led to several rounds of heavy rain from the evening of September 12th through the early afternoon hours on September 13th. This rain led to many reports of flooding and flash flooding, with several water rescues occurring during the late evening hours of September 12th. Rainfall amounts ranged from 2 to 5.5 inches in the area where the heaviest rains fell.||In Powell county, at the Middlefork Campground, a truck was caught up in flood waters, but all passengers were able to get to safety. Powell County search and rescue were also involved in getting people to safety in the Indian Creek area of the Red River Gorge.||In Menifee county, 30 to 40 campers had to seek higher ground as the Red River Adventure Campground saw extensive flooding.  Two other campers had to be rescued who were camping near Brushy Creek in the northern part of the county.||In Morgan county, the cow branch community saw extensive flooding, along with significant flooding in and around West Liberty.  Several roads sustained damage in West Liberty.  There was also extensive flooding along Spaws Creek. Bethany Enterprise Baptist Church along war creek also saw some damage to their property.||Finally, in Jackson county, there were several instances of roads being shut down due to flash flooding, especially late Sunday morning into Sunday afternoon with a second surge in rainfall. Water was reported over KY-421 near Egypt Penecostal Church.", "ts_dict_index": [3996, 3997, 3998]}
+{"event_id": 912746, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2020-09-13 11:00:00", "end_date_time": "2020-09-13 15:00:00", "narrative": "Deep moisture anchored across east Kentucky, combined with a stalled frontal boundary, then a cold front, led to several rounds of heavy rain from the evening of September 12th through the early afternoon hours on September 13th. This rain led to many reports of flooding and flash flooding, with several water rescues occurring during the late evening hours of September 12th. Rainfall amounts ranged from 2 to 5.5 inches in the area where the heaviest rains fell.||In Powell county, at the Middlefork Campground, a truck was caught up in flood waters, but all passengers were able to get to safety. Powell County search and rescue were also involved in getting people to safety in the Indian Creek area of the Red River Gorge.||In Menifee county, 30 to 40 campers had to seek higher ground as the Red River Adventure Campground saw extensive flooding.  Two other campers had to be rescued who were camping near Brushy Creek in the northern part of the county.||In Morgan county, the cow branch community saw extensive flooding, along with significant flooding in and around West Liberty.  Several roads sustained damage in West Liberty.  There was also extensive flooding along Spaws Creek. Bethany Enterprise Baptist Church along war creek also saw some damage to their property.||Finally, in Jackson county, there were several instances of roads being shut down due to flash flooding, especially late Sunday morning into Sunday afternoon with a second surge in rainfall. Water was reported over Dunigam Road near the community of Tyner as water from an adjacent creek overflowed its banks.", "ts_dict_index": [4002, 4003, 4004]}
+{"event_id": 912734, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2020-09-13 11:00:00", "end_date_time": "2020-09-13 15:00:00", "narrative": "Deep moisture anchored across east Kentucky, combined with a stalled frontal boundary, then a cold front, led to several rounds of heavy rain from the evening of September 12th through the early afternoon hours on September 13th. This rain led to many reports of flooding and flash flooding, with several water rescues occurring during the late evening hours of September 12th. Rainfall amounts ranged from 2 to 5.5 inches in the area where the heaviest rains fell.||In Powell county, at the Middlefork Campground, a truck was caught up in flood waters, but all passengers were able to get to safety. Powell County search and rescue were also involved in getting people to safety in the Indian Creek area of the Red River Gorge.||In Menifee county, 30 to 40 campers had to seek higher ground as the Red River Adventure Campground saw extensive flooding.  Two other campers had to be rescued who were camping near Brushy Creek in the northern part of the county.||In Morgan county, the cow branch community saw extensive flooding, along with significant flooding in and around West Liberty.  Several roads sustained damage in West Liberty.  There was also extensive flooding along Spaws Creek. Bethany Enterprise Baptist Church along war creek also saw some damage to their property.||Finally, in Jackson county, there were several instances of roads being shut down due to flash flooding, especially late Sunday morning into Sunday afternoon with a second surge in rainfall. Water was reported over Roark Road near the community of Annville.", "ts_dict_index": [3993, 3994, 3995]}
+{"event_id": 916410, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2020-09-13 11:00:00", "end_date_time": "2020-09-13 15:00:00", "narrative": "Deep moisture anchored across east Kentucky, combined with a stalled frontal boundary, then a cold front, led to several rounds of heavy rain from the evening of September 12th through the early afternoon hours on September 13th. This rain led to many reports of flooding and flash flooding, with several water rescues occurring during the late evening hours of September 12th. Rainfall amounts ranged from 2 to 5.5 inches in the area where the heaviest rains fell.||In Powell county, at the Middlefork Campground, a truck was caught up in flood waters, but all passengers were able to get to safety. Powell County search and rescue were also involved in getting people to safety in the Indian Creek area of the Red River Gorge.||In Menifee county, 30 to 40 campers had to seek higher ground as the Red River Adventure Campground saw extensive flooding.  Two other campers had to be rescued who were camping near Brushy Creek in the northern part of the county.||In Morgan county, the cow branch community saw extensive flooding, along with significant flooding in and around West Liberty.  Several roads sustained damage in West Liberty.  There was also extensive flooding along Spaws Creek. Bethany Enterprise Baptist Church along war creek also saw some damage to their property.||Finally, in Jackson county, there were several instances of roads being shut down due to flash flooding, especially late Sunday morning into Sunday afternoon with a second surge in rainfall. Water was reported over Mac Stevens Road making it impassable. After the water resided,  a section of the asphalt had been washed away on the road.", "ts_dict_index": [3990, 3991, 3992]}
+{"event_id": 912742, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2020-09-13 11:00:00", "end_date_time": "2020-09-13 15:00:00", "narrative": "Deep moisture anchored across east Kentucky, combined with a stalled frontal boundary, then a cold front, led to several rounds of heavy rain from the evening of September 12th through the early afternoon hours on September 13th. This rain led to many reports of flooding and flash flooding, with several water rescues occurring during the late evening hours of September 12th. Rainfall amounts ranged from 2 to 5.5 inches in the area where the heaviest rains fell.||In Powell county, at the Middlefork Campground, a truck was caught up in flood waters, but all passengers were able to get to safety. Powell County search and rescue were also involved in getting people to safety in the Indian Creek area of the Red River Gorge.||In Menifee county, 30 to 40 campers had to seek higher ground as the Red River Adventure Campground saw extensive flooding.  Two other campers had to be rescued who were camping near Brushy Creek in the northern part of the county.||In Morgan county, the cow branch community saw extensive flooding, along with significant flooding in and around West Liberty.  Several roads sustained damage in West Liberty.  There was also extensive flooding along Spaws Creek. Bethany Enterprise Baptist Church along war creek also saw some damage to their property.||Finally, in Jackson county, there were several instances of roads being shut down due to flash flooding, especially late Sunday morning into Sunday afternoon with a second surge in rainfall. The junction of KY-421 and KY-3630 was closed due to high water in the town of Tyner. Local dispatch also reported that traffic was backed up for a quarter of a mile because of the closure.", "ts_dict_index": [4005, 4006, 4007]}
+{"event_id": 1063311, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-05 15:25:00", "end_date_time": "2023-01-05 17:25:00", "narrative": "A large low pressure system brought moderate to heavy precipitation, widespread flooding and strong winds to the area on January 4 and 5. This system had an atmospheric river associated with it which contained a deep fetch of moisture of tropical origin resulting in widespread moderate to heavy precipitation across the area with the snow level ranging between 7000 and 8000 feet for much of the event. Several stations above 8000 feet picked up 18 to 30 inches of new snowfall from this storm. Many stations in the Sierra Nevada picked up an inch and a half to three inches of liquid precipitation while the adjacent foothills picked up 1 to 2 inches of rain and the San Joaquin Valley received around a half inch to an inch from Fresno County northward and a quarter to a half inch further southward. This rainfall came on top of already saturated soils from the late December storms resulting in widespread nuisance flooding across the area. The Tehachapi Mountains generally picked up between a quarter to a half inch of rainfall while rain shadowing effect limited rainfall in the Kern County Deserts to a tenth of an inch or less at most stations. This system also produced very strong winds across much of the area with several stations in the Kern County Mountains and West Side hills measuring gusts in excess of 60 mph with several ridge top stations in Kern County reporting peak gusts in excess of 75 mph. Several reports of wind damage were received by WFO Hanford during this event. Public report of southbound SR 99 center divider being flooded and spilling into the roadway between the Caldwell Ave. and the Ave. 260 exchanges.", "ts_dict_index": [3951, 3952, 3953]}
+{"event_id": 1121947, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2023-07-09 13:52:00", "end_date_time": "2023-07-09 18:15:00", "narrative": "A strong upper-level system brought widespread rounds of showers and thunderstorms to eastern New York on July 9-11, 2023. The steadiest and heaviest rainfall occurred during the afternoon hours on July 9, the early morning hours on July 10 and during the evening hours on July 10 into the overnight hours on July 11. Rainfall totals varied greatly from region to region but the hardest hit areas (Hudson Valley and into northeastern Hamilton County) received 3 to 6 inches of rainfall.||Areal and flash flooding was primarily focused across areas along the Hudson River on July 9-10. Damage consisted of closed and washed out roads. A section of Metro-North's railroad tracks were washed out due to flood waters from Poughkeepsie southward.||The combination of heavy rain and beaver dam failures resulted in destruction of roads, bridges and sidewalks across northeastern Hamilton County during the early morning hours on July 11 focused on the areas of Long Lake and Blue Mountain Lake. A State of Emergency was declared for the towns of Long Lake and Indian Lake. New York Governor Kathy Hochul declared a State of Emergency for Hamilton County. Hamilton County Emergency Manager estimated damage to be in the millions of dollars.||In addition to the heavy rainfall, a few severe thunderstorms also developed across portions of the Hudson Valley leading to downed trees and wires. A lightning strike caused an auto body shop to catch fire. Portions of Quaker Street near Plattekill were flooded.", "ts_dict_index": [4011, 4012, 4013]}
+{"event_id": 1061530, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2022-12-27 09:33:00", "end_date_time": "2022-12-27 11:33:00", "narrative": "A strong upper low pressure system moved through California on December 27. This system had abundant moisture associated with it as it pulled up a deep fetch of moisture of tropical origin. This system brought widespread moderate to heavy precipitation to the area between the early morning until the early evening of December 27. The heavy rainfall produced a rockslide in Yosemite National Park which resulted in two fatalities. The precipitation tapered off by the early morning of December 28. Much of the higher Sierra Nevada picked up between an inch and a half and three inches of liquid precipitation with the precipitation mainly falling as snow above 7500 feet where many stations picked up between 18 and 30 inches of new snowfall. The snow level briefly lowered to around 6000 feet during the evening of December 27 and some light snowfall was observed between 6000 and 7500 feet. The Sierra foothills generally received between 1 to 2 inches of rain while 0.75 to 1.5 inches of rain fell in the San Joaquin Valley and the Tehachapi Mountains. Several reports of nuisance flooding were reported by law enforcement and on social media. Rain shadowing effects limited precipitation in the Kern County Deserts to a quarter inch or less. This system also brought some strong wind gusts to the mountains as several stations measured gusts exceeding 40 mph and a few low impact stations had brief gusts above 60 mph. California Highway Patrol reported roadway flooding at SR 152 and the Romero Visitor Center.", "ts_dict_index": [4047, 4048, 4049]}
+{"event_id": 1116682, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-08-21 12:41:00", "end_date_time": "2023-08-21 15:41:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported roadway flooding on Interstate 5 9S Los Banos north of the SR 165 exchange.", "ts_dict_index": [4038, 4039, 4040]}
+{"event_id": 1062371, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-12-27 18:13:00", "end_date_time": "2022-12-27 20:13:00", "narrative": "A strong upper low pressure system moved through California on December 27. This system had abundant moisture associated with it as it pulled up a deep fetch of moisture of tropical origin. This system brought widespread moderate to heavy precipitation to the area between the early morning until the early evening of December 27. The heavy rainfall produced a rockslide in Yosemite National Park which resulted in two fatalities. The precipitation tapered off by the early morning of December 28. Much of the higher Sierra Nevada picked up between an inch and a half and three inches of liquid precipitation with the precipitation mainly falling as snow above 7500 feet where many stations picked up between 18 and 30 inches of new snowfall. The snow level briefly lowered to around 6000 feet during the evening of December 27 and some light snowfall was observed between 6000 and 7500 feet. The Sierra foothills generally received between 1 to 2 inches of rain while 0.75 to 1.5 inches of rain fell in the San Joaquin Valley and the Tehachapi Mountains. Several reports of nuisance flooding were reported by law enforcement and on social media. Rain shadowing effects limited precipitation in the Kern County Deserts to a quarter inch or less. This system also brought some strong wind gusts to the mountains as several stations measured gusts exceeding 40 mph and a few low impact stations had brief gusts above 60 mph. California Highway Patrol reported flooding on Calloway Dr. underneath the railroad bridge north of Slinker Dr.", "ts_dict_index": [4044, 4045, 4046]}
+{"event_id": 1116702, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 17:23:00", "end_date_time": "2023-08-20 20:23:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported roadway flooding on Garlock Rd. near SR 395.", "ts_dict_index": [4014, 4015, 4016]}
+{"event_id": 1116666, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-19 17:01:00", "end_date_time": "2023-08-19 17:01:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported standing water on SR 99 under the overpasses of Cecil Ave. and Garces Hwy. in Delano.", "ts_dict_index": [4035, 4036, 4037]}
+{"event_id": 1116696, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 14:45:00", "end_date_time": "2023-08-21 02:45:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. The Kern County Emergency Manager reported Oak Creek Blvd. was closed between Tehachapi Willow Springs Rd. and Koch St. due to flooding.", "ts_dict_index": [4029, 4030, 4031]}
+{"event_id": 1116694, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 13:47:00", "end_date_time": "2023-08-20 16:47:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported roadway flooding on Sand Canyon Rd. north of SR 58.", "ts_dict_index": [4020, 4021, 4022]}
+{"event_id": 1116693, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 13:32:00", "end_date_time": "2023-08-20 16:32:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. Public report of roadway flooding at the intersection of Kratzmeyer Rd. and Nord Ave.", "ts_dict_index": [4017, 4018, 4019]}
+{"event_id": 1116699, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 14:13:00", "end_date_time": "2023-08-20 17:13:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported roadway flooding at northbound SR 99 and SR 166 just south of Mettler.", "ts_dict_index": [4041, 4042, 4043]}
+{"event_id": 1116954, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 23:20:00", "end_date_time": "2023-08-21 03:20:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported roadway flooding on Lebec Rd. from Frazier Mountain Park Rd. to Landfill Rd.", "ts_dict_index": [4026, 4027, 4028]}
+{"event_id": 1116953, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 22:14:00", "end_date_time": "2023-08-21 02:14:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. Caltrans reported a road closure of SR 14 between SR 58 and SR 178 due to flooding.", "ts_dict_index": [4023, 4024, 4025]}
+{"event_id": 912737, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2020-09-13 11:00:00", "end_date_time": "2020-09-13 15:00:00", "narrative": "Deep moisture anchored across east Kentucky, combined with a stalled frontal boundary, then a cold front, led to several rounds of heavy rain from the evening of September 12th through the early afternoon hours on September 13th. This rain led to many reports of flooding and flash flooding, with several water rescues occurring during the late evening hours of September 12th. Rainfall amounts ranged from 2 to 5.5 inches in the area where the heaviest rains fell.||In Powell county, at the Middlefork Campground, a truck was caught up in flood waters, but all passengers were able to get to safety. Powell County search and rescue were also involved in getting people to safety in the Indian Creek area of the Red River Gorge.||In Menifee county, 30 to 40 campers had to seek higher ground as the Red River Adventure Campground saw extensive flooding.  Two other campers had to be rescued who were camping near Brushy Creek in the northern part of the county.||In Morgan county, the cow branch community saw extensive flooding, along with significant flooding in and around West Liberty.  Several roads sustained damage in West Liberty.  There was also extensive flooding along Spaws Creek. Bethany Enterprise Baptist Church along war creek also saw some damage to their property.||Finally, in Jackson county, there were several instances of roads being shut down due to flash flooding, especially late Sunday morning into Sunday afternoon with a second surge in rainfall. Water was reported over KY-30 near Hicks Branch Road.", "ts_dict_index": [3999, 4000, 4001]}
+{"event_id": 1061534, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-27 11:26:00", "end_date_time": "2022-12-27 13:26:00", "narrative": "A strong upper low pressure system moved through California on December 27. This system had abundant moisture associated with it as it pulled up a deep fetch of moisture of tropical origin. This system brought widespread moderate to heavy precipitation to the area between the early morning until the early evening of December 27. The heavy rainfall produced a rockslide in Yosemite National Park which resulted in two fatalities. The precipitation tapered off by the early morning of December 28. Much of the higher Sierra Nevada picked up between an inch and a half and three inches of liquid precipitation with the precipitation mainly falling as snow above 7500 feet where many stations picked up between 18 and 30 inches of new snowfall. The snow level briefly lowered to around 6000 feet during the evening of December 27 and some light snowfall was observed between 6000 and 7500 feet. The Sierra foothills generally received between 1 to 2 inches of rain while 0.75 to 1.5 inches of rain fell in the San Joaquin Valley and the Tehachapi Mountains. Several reports of nuisance flooding were reported by law enforcement and on social media. Rain shadowing effects limited precipitation in the Kern County Deserts to a quarter inch or less. This system also brought some strong wind gusts to the mountains as several stations measured gusts exceeding 40 mph and a few low impact stations had brief gusts above 60 mph. California Highway Patrol reported SR 140 entrance to Yosemite closed due to a rockfall 3 miles east of the tollbooths.", "ts_dict_index": [4068, 4069, 4070]}
+{"event_id": 1062349, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2022-12-27 14:17:00", "end_date_time": "2022-12-27 16:17:00", "narrative": "A strong upper low pressure system moved through California on December 27. This system had abundant moisture associated with it as it pulled up a deep fetch of moisture of tropical origin. This system brought widespread moderate to heavy precipitation to the area between the early morning until the early evening of December 27. The heavy rainfall produced a rockslide in Yosemite National Park which resulted in two fatalities. The precipitation tapered off by the early morning of December 28. Much of the higher Sierra Nevada picked up between an inch and a half and three inches of liquid precipitation with the precipitation mainly falling as snow above 7500 feet where many stations picked up between 18 and 30 inches of new snowfall. The snow level briefly lowered to around 6000 feet during the evening of December 27 and some light snowfall was observed between 6000 and 7500 feet. The Sierra foothills generally received between 1 to 2 inches of rain while 0.75 to 1.5 inches of rain fell in the San Joaquin Valley and the Tehachapi Mountains. Several reports of nuisance flooding were reported by law enforcement and on social media. Rain shadowing effects limited precipitation in the Kern County Deserts to a quarter inch or less. This system also brought some strong wind gusts to the mountains as several stations measured gusts exceeding 40 mph and a few low impact stations had brief gusts above 60 mph. California Highway Patrol reported roadway flooding at Ave 224 and Ave 216 south of SR 137 west of Tulare.", "ts_dict_index": [4050, 4051, 4052]}
+{"event_id": 1069210, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-14 18:17:00", "end_date_time": "2023-01-14 18:17:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. Department of Highways reported two to three lanes of southbound I-5 bypass at Highway 56 was flooded. Vehicles were unable to drive in the slow lane.", "ts_dict_index": [4086, 4087, 4088]}
+{"event_id": 1069369, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-16 14:00:00", "end_date_time": "2023-01-16 14:00:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. Escondido Creek overflowed, and flooded fields and parking areas alongside the river and Rancho Santa Fe Road.", "ts_dict_index": [4077, 4078, 4079]}
+{"event_id": 1069373, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-16 05:30:00", "end_date_time": "2023-01-16 05:30:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. San Diego County official reported flooding at on Pine Creek Crossing, resulting in the closure of the road.", "ts_dict_index": [4089, 4090, 4091]}
+{"event_id": 1069374, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-16 05:38:00", "end_date_time": "2023-01-16 07:09:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. Flooding was reported early in the morning on January 16 due to heavy rain, with the area having received 1.5 to 2 inches in the prior 12 hours, and 2.5 to 4 inches in the preceding 24 hours. Alpine Blvd was closed due to flooding, with flooding also reported south of Alpine due to the local creek.", "ts_dict_index": [4092, 4093, 4094]}
+{"event_id": 1069215, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-14 17:00:00", "end_date_time": "2023-01-14 20:00:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. Moderate to heavy rain occurred across the San Diego County metro area from 5-7 pm, resulting in flooding of major freeways. Highway 94 at Euclid Ave was flooded in Lanes 3 and 4; I-5 at Mile of Cars north was flooded, with a large amount of water in all lanes making it difficult for vehicles to drive; I-805 Bonita Rd offramp was flooded.", "ts_dict_index": [4083, 4084, 4085]}
+{"event_id": 1062372, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-12-27 18:26:00", "end_date_time": "2022-12-27 20:26:00", "narrative": "A strong upper low pressure system moved through California on December 27. This system had abundant moisture associated with it as it pulled up a deep fetch of moisture of tropical origin. This system brought widespread moderate to heavy precipitation to the area between the early morning until the early evening of December 27. The heavy rainfall produced a rockslide in Yosemite National Park which resulted in two fatalities. The precipitation tapered off by the early morning of December 28. Much of the higher Sierra Nevada picked up between an inch and a half and three inches of liquid precipitation with the precipitation mainly falling as snow above 7500 feet where many stations picked up between 18 and 30 inches of new snowfall. The snow level briefly lowered to around 6000 feet during the evening of December 27 and some light snowfall was observed between 6000 and 7500 feet. The Sierra foothills generally received between 1 to 2 inches of rain while 0.75 to 1.5 inches of rain fell in the San Joaquin Valley and the Tehachapi Mountains. Several reports of nuisance flooding were reported by law enforcement and on social media. Rain shadowing effects limited precipitation in the Kern County Deserts to a quarter inch or less. This system also brought some strong wind gusts to the mountains as several stations measured gusts exceeding 40 mph and a few low impact stations had brief gusts above 60 mph. California Highway Patrol reported flooding on westbound SR 58 at the intersection of Cottonwood Rd.", "ts_dict_index": [4053, 4054, 4055]}
+{"event_id": 1062370, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-12-27 17:18:00", "end_date_time": "2022-12-27 19:18:00", "narrative": "A strong upper low pressure system moved through California on December 27. This system had abundant moisture associated with it as it pulled up a deep fetch of moisture of tropical origin. This system brought widespread moderate to heavy precipitation to the area between the early morning until the early evening of December 27. The heavy rainfall produced a rockslide in Yosemite National Park which resulted in two fatalities. The precipitation tapered off by the early morning of December 28. Much of the higher Sierra Nevada picked up between an inch and a half and three inches of liquid precipitation with the precipitation mainly falling as snow above 7500 feet where many stations picked up between 18 and 30 inches of new snowfall. The snow level briefly lowered to around 6000 feet during the evening of December 27 and some light snowfall was observed between 6000 and 7500 feet. The Sierra foothills generally received between 1 to 2 inches of rain while 0.75 to 1.5 inches of rain fell in the San Joaquin Valley and the Tehachapi Mountains. Several reports of nuisance flooding were reported by law enforcement and on social media. Rain shadowing effects limited precipitation in the Kern County Deserts to a quarter inch or less. This system also brought some strong wind gusts to the mountains as several stations measured gusts exceeding 40 mph and a few low impact stations had brief gusts above 60 mph. California Highway Patrol reported a small mudslide blocking the southbound lane of Tupman Road north of SR 119.", "ts_dict_index": [4074, 4075, 4076]}
+{"event_id": 1062367, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-12-27 16:43:00", "end_date_time": "2022-12-27 18:43:00", "narrative": "A strong upper low pressure system moved through California on December 27. This system had abundant moisture associated with it as it pulled up a deep fetch of moisture of tropical origin. This system brought widespread moderate to heavy precipitation to the area between the early morning until the early evening of December 27. The heavy rainfall produced a rockslide in Yosemite National Park which resulted in two fatalities. The precipitation tapered off by the early morning of December 28. Much of the higher Sierra Nevada picked up between an inch and a half and three inches of liquid precipitation with the precipitation mainly falling as snow above 7500 feet where many stations picked up between 18 and 30 inches of new snowfall. The snow level briefly lowered to around 6000 feet during the evening of December 27 and some light snowfall was observed between 6000 and 7500 feet. The Sierra foothills generally received between 1 to 2 inches of rain while 0.75 to 1.5 inches of rain fell in the San Joaquin Valley and the Tehachapi Mountains. Several reports of nuisance flooding were reported by law enforcement and on social media. Rain shadowing effects limited precipitation in the Kern County Deserts to a quarter inch or less. This system also brought some strong wind gusts to the mountains as several stations measured gusts exceeding 40 mph and a few low impact stations had brief gusts above 60 mph. California Highway Patrol reported flooding on southbound SR 99 as well as on the off ramp of southbound SR 99 to SR 119.", "ts_dict_index": [4062, 4063, 4064]}
+{"event_id": 1062373, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-12-27 18:56:00", "end_date_time": "2022-12-27 20:56:00", "narrative": "A strong upper low pressure system moved through California on December 27. This system had abundant moisture associated with it as it pulled up a deep fetch of moisture of tropical origin. This system brought widespread moderate to heavy precipitation to the area between the early morning until the early evening of December 27. The heavy rainfall produced a rockslide in Yosemite National Park which resulted in two fatalities. The precipitation tapered off by the early morning of December 28. Much of the higher Sierra Nevada picked up between an inch and a half and three inches of liquid precipitation with the precipitation mainly falling as snow above 7500 feet where many stations picked up between 18 and 30 inches of new snowfall. The snow level briefly lowered to around 6000 feet during the evening of December 27 and some light snowfall was observed between 6000 and 7500 feet. The Sierra foothills generally received between 1 to 2 inches of rain while 0.75 to 1.5 inches of rain fell in the San Joaquin Valley and the Tehachapi Mountains. Several reports of nuisance flooding were reported by law enforcement and on social media. Rain shadowing effects limited precipitation in the Kern County Deserts to a quarter inch or less. This system also brought some strong wind gusts to the mountains as several stations measured gusts exceeding 40 mph and a few low impact stations had brief gusts above 60 mph. California Highway Patrol reported flooding near the intersection of SR 43 and Merced Ave. near Shafter.", "ts_dict_index": [4056, 4057, 4058]}
+{"event_id": 1069363, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-16 06:48:00", "end_date_time": "2023-01-16 06:48:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. Heavy rain occurred across northern San Diego County on January 15-16, resulting in flooding near Rainbow. County officials announced the closure of Pala Mission Road near Highway 76, and Pala Temecula Road. Rainfall of 1 to 1.5 inch had been reported leading up to the flooding.", "ts_dict_index": [4095, 4096, 4097]}
+{"event_id": 1069377, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-16 14:06:00", "end_date_time": "2023-01-16 14:06:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. Flooding was reported at Honey Springs Road and Mother Grundy truck trail, with two feet of water over the road. Three inches of rainfall was reported in the 24 hours preceding the flooding.", "ts_dict_index": [4098, 4099, 4100]}
+{"event_id": 1069218, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-15 16:00:00", "end_date_time": "2023-01-15 16:00:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. Four feet of flowing water was reported on Saturn Blvd from the Tijuana River. A stolen SUV was found in the water, though no one was seen near the vehicle; speculated that the vehicle had been stolen.", "ts_dict_index": [4101, 4102, 4103]}
+{"event_id": 1116958, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-08-20 23:21:00", "end_date_time": "2023-08-21 03:21:00", "narrative": "A strong surge of moisture associated with Hurricane Hillary pushed northward into central California on August 19. This moisture surge resulted in the development of showers and thunderstorms mainly the San Joaquin Valley during the afternoon and evening hours with the most noticeable impact being outflow wind gusts. Hillary weakened into a Tropical Storm and moved into southern California on August 20 resulting in moderate to heavy rainfall across the mountains and deserts of Kern County with several stations picking up between 3 and 5 inches of rainfall with a few stations receiving more than 5.5 inches of rainfall. Much of the Sierra Nevada south of Kings Canyon picked up between 1 and 3 inches of rainfall while the south San Joaquin Valley measured between a half inch and an inch. Further north, rainfall amounts were lower, but many new daily rainfall records were set for August 20. Numerous reports of flash flooding and road closures were observed in Kern County during the afternoon of August 20 through the early morning of August 21. The rains dissipated during the morning of August 21, but an offshore trough provided for enough instability for thunderstorms to break out over the area during the afternoon of August 21 which produced locally heavy rainfall. The trough lifted northeast on August 22 resulting in the moisture being pushed out of our area and drier conditions prevailed for the remainder of the week. California Highway Patrol reported roadway flooding on southbound Interstate 5 between the scales and Grapevine Rd.", "ts_dict_index": [4032, 4033, 4034]}
+{"event_id": 1088761, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2023-03-24 07:45:00", "end_date_time": "2023-03-24 15:00:00", "narrative": "The most impactful storm system to affect the region during the month of March began during the late afternoon and early evening of the 23rd as strong to severe thunderstorms trained along and north of a front that had stalled over northwest Arkansas and south central Missouri. While the storms produced sporadic wind damage and hail, rainfall accumulations exceeded three inches within a 6-hour period during the evening of the 23rd. This led to numerous flooded low water crossings, evacuations at Roaring River State Park, and swift water rescues from McDonald County to Dent County. Unfortunately, there were three flash flood related fatalities that occurred - two fatalities occurred along Parks Creek to the southwest of Grovespring in Wright County, and one fatality occurred in southern Webster County along Finley Creek. In both instances, people drove across flooded low water crossings and were swept off the road. Minor to moderate river flooding occurred along many of the larger creeks and rivers including the James, Jacks Fork, Elk, Spring, Current, Big Piney, Roubidoux and Gasconade Rivers and Shoal Creek. Rainfall accumulations averaging around two inches for the 24-hour period ending at 6 PM on the 24th occurred along and east of a line from Neosho to Osage Beach. Within this area, there was a swath of over five inches of rain from Billings to Cabool. Highway H between Noel and Pineville along the Elk River was flooded and impassable.", "ts_dict_index": [4119, 4120, 4121]}
+{"event_id": 1069207, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-14 14:00:00", "end_date_time": "2023-01-14 20:00:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. Heavy rain resulted in the flooding of Huffstatler Creek flowing over Huffstatler Road at 2nd St and 5th St; roads were closed due to flooding.", "ts_dict_index": [4107, 4108, 4109]}
+{"event_id": 801384, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2019-01-24 16:36:00", "end_date_time": "2019-01-24 20:00:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. Route 213 was closed between Creek Locks Road and Mountain Road due to flooding.", "ts_dict_index": [4128, 4129, 4130]}
+{"event_id": 1088801, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2023-03-24 07:11:00", "end_date_time": "2023-03-24 16:00:00", "narrative": "The most impactful storm system to affect the region during the month of March began during the late afternoon and early evening of the 23rd as strong to severe thunderstorms trained along and north of a front that had stalled over northwest Arkansas and south central Missouri. While the storms produced sporadic wind damage and hail, rainfall accumulations exceeded three inches within a 6-hour period during the evening of the 23rd. This led to numerous flooded low water crossings, evacuations at Roaring River State Park, and swift water rescues from McDonald County to Dent County. Unfortunately, there were three flash flood related fatalities that occurred - two fatalities occurred along Parks Creek to the southwest of Grovespring in Wright County, and one fatality occurred in southern Webster County along Finley Creek. In both instances, people drove across flooded low water crossings and were swept off the road. Minor to moderate river flooding occurred along many of the larger creeks and rivers including the James, Jacks Fork, Elk, Spring, Current, Big Piney, Roubidoux and Gasconade Rivers and Shoal Creek. Rainfall accumulations averaging around two inches for the 24-hour period ending at 6 PM on the 24th occurred along and east of a line from Neosho to Osage Beach. Within this area, there was a swath of over five inches of rain from Billings to Cabool. Highway 76 at Indian Creek in Anderson was flooded and closed.", "ts_dict_index": [4116, 4117, 4118]}
+{"event_id": 1088803, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2023-03-24 06:44:00", "end_date_time": "2023-03-24 16:00:00", "narrative": "The most impactful storm system to affect the region during the month of March began during the late afternoon and early evening of the 23rd as strong to severe thunderstorms trained along and north of a front that had stalled over northwest Arkansas and south central Missouri. While the storms produced sporadic wind damage and hail, rainfall accumulations exceeded three inches within a 6-hour period during the evening of the 23rd. This led to numerous flooded low water crossings, evacuations at Roaring River State Park, and swift water rescues from McDonald County to Dent County. Unfortunately, there were three flash flood related fatalities that occurred - two fatalities occurred along Parks Creek to the southwest of Grovespring in Wright County, and one fatality occurred in southern Webster County along Finley Creek. In both instances, people drove across flooded low water crossings and were swept off the road. Minor to moderate river flooding occurred along many of the larger creeks and rivers including the James, Jacks Fork, Elk, Spring, Current, Big Piney, Roubidoux and Gasconade Rivers and Shoal Creek. Rainfall accumulations averaging around two inches for the 24-hour period ending at 6 PM on the 24th occurred along and east of a line from Neosho to Osage Beach. Within this area, there was a swath of over five inches of rain from Billings to Cabool. Route CC at Flat Creek was flooded and impassable.", "ts_dict_index": [4122, 4123, 4124]}
+{"event_id": 801395, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-01-24 16:09:00", "end_date_time": "2019-01-24 20:47:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. County Route 61 was closed between Route 22 and Ackley Road due to flooding.", "ts_dict_index": [4131, 4132, 4133]}
+{"event_id": 801392, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-01-24 14:30:00", "end_date_time": "2019-01-25 12:45:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. Burch Hollow Road was closed between Burton Road and Easton Station Road due to flooding.", "ts_dict_index": [4125, 4126, 4127]}
+{"event_id": 1069378, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-16 06:47:00", "end_date_time": "2023-01-16 06:47:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. Swift water rescue on Otay Lakes Road and milepost 8. Victim was rescued on top of the vehicle.", "ts_dict_index": [4104, 4105, 4106]}
+{"event_id": 1069211, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-14 15:00:00", "end_date_time": "2023-01-14 20:00:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. Heavy rain of 0.50 to 1.00 inch was reported on the afternoon and evening of January 14. The right lane of southbound I-805 north of Clairemont Mesa Blvd was flooded, and at Murray Ridge Road was flooded. All lanes except the HOV were flooded and vehicles were unable to pass. 10 inches of water were reported in lanes 1 and 2.", "ts_dict_index": [4110, 4111, 4112]}
+{"event_id": 1069381, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2023-01-16 11:00:00", "end_date_time": "2023-01-16 11:00:00", "narrative": "The last in a series of atmospheric rivers impact Southern California January 14-16. Widespread heavy rainfall occurred in back-to-back two waves, with the first occurring the afternoon of January 14 into the early morning hours on January 15, and the second occurring the night of January 15 through January 16.||The first storm system resulted in numerous reports of flooding in San Diego County, Orange County and Riverside County and high-elevation snow in the mountains of San Bernardino and Riverside Counties. Rainfall amounts generally ranged from 1 to 2 inches for the coast, 1 to 2.5 inches in the valleys, 2 to 5 inches in the mountains and up to one-half of an inch in the deserts.||The second, colder system again produced widespread moderate to heavy rainfall, with the heaviest rain focusing on San Diego County. Many reports of flooding were received in San Diego County, with numerous swiftwater rescues performed, with 19 alone by San Diego City. The San Diego River overflowed, with the highest impacts reported in Fashion Valley on January 16, with a dozen swiftwater rescues performed before dawn. Nearby areas in Hotel Circle were evacuated due to the threat of flooding.||Impressive precipitation amounts were reported from the two back-to-back system, with 2 to 4 inches of rain received at the coast, 2 to 5 inches for the inland valley and 3 to 8+ inches for the mountains. A woman was rescued by San Diego lifeguard after being stranded in her vehicle in four feet of water near the Tijuana River. 7 inches of rain had been reported at Otay Mountain in the preceding 3 days, with 4.2 inches of rain in Bonita.", "ts_dict_index": [4080, 4081, 4082]}
+{"event_id": 802961, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-01-24 19:52:00", "end_date_time": "2019-01-25 12:59:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. Gray Lane at Upper Turnpike Road was closed due to flooding along the Mettawee River.", "ts_dict_index": [4152, 4153, 4154]}
+{"event_id": 801383, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-01-24 13:01:00", "end_date_time": "2019-01-24 17:41:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. A residence on Ashgrove Road was evacuated due to flooding from an ice jam on White Creek.", "ts_dict_index": [4146, 4147, 4148]}
+{"event_id": 801393, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-01-24 10:17:00", "end_date_time": "2019-01-25 00:00:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. East Street was closed between Rogers Street and Baldwin Avenue due to flooding.", "ts_dict_index": [4155, 4156, 4157]}
+{"event_id": 801396, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-01-24 18:06:00", "end_date_time": "2019-01-25 12:45:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. Hickory Hill Road was closed between State Route 313 and Perry Hill Road due to flooding.", "ts_dict_index": [4137, 4138, 4139]}
+{"event_id": 802963, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-01-24 17:07:00", "end_date_time": "2019-01-25 15:00:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. River Road was closed at the Buskirk Covered Bridge due to an ice jam on the Hoosic River.", "ts_dict_index": [4143, 4144, 4145]}
+{"event_id": 801391, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-01-24 17:57:00", "end_date_time": "2019-01-25 15:20:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. King Road was closed at County Road 59 due to flooding.", "ts_dict_index": [4149, 4150, 4151]}
+{"event_id": 801394, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-01-24 16:08:00", "end_date_time": "2019-01-25 15:15:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. Cross Road was closed between Routes 30 and 31 due to flooding.", "ts_dict_index": [4134, 4135, 4136]}
+{"event_id": 815480, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2019-05-26 15:41:00", "end_date_time": "2019-05-26 17:41:00", "narrative": "A strong upper low pressure system pushed southward through the Pacific Northwest on May 25. Warm air advection ahead of this system produced instability over the San Joaquin Valley during the afternoon and evening of May 25 which resulted in the development of scattered thunderstorms. One thunderstorm produced nickel sized hail between Mettler and Maricopa along State Route 166 and also produced roadway flooding in the area. The low moved southward through California on May 26 bringing increased clouds, significant rainfall and mountain snowfall, locally strong winds as well as thunderstorms with heavy rain. Much of the area received between a quarter and three quarters of an inch of liquid precipitation while several stations in the Sierra Nevada picked up between 2 to 5 inches of new snowfall with a few stations picking up 6 to 7 inches. Thunderstorms developed during the afternoon of May 26 across the San Joaquin Valley producing heavy rainfall, roadway flooding and a few funnel clouds. In addition, gusty winds prevailed for much of the day in the Tehachapi and Lake Isabella areas where there were several reports of wind gusts exceeding 35 mph while a few low impact indicator sites measured gusts above 55 mph. Several all time daily record precipitation records were shattered on May 26. Posts on Twitter indicated flooding in a neighborhood in southwest Hanford.", "ts_dict_index": [4191, 4192, 4193]}
+{"event_id": 805349, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2019-03-27 16:05:00", "end_date_time": "2019-03-27 17:25:00", "narrative": "A low pressure system moved into Northern California during the morning of March 27 then dropped southeast during the afternoon resulting in increasing precipitation coverage across the area. The precipitation was most significant in Merced and Mariposa Counties which were impacted by the deeper moisture associated with this system as well as the unstable airmass behind the cold front which moved over central California during the day. Afternoon showers and thunderstorms increased in coverage during the late afternoon producing locally heavy rainfall as well as pea sized hail and a few funnel clouds. Much of the Southern Sierra Nevada north of Kings Canyon picked up between a half inch and an inch of liquid precipitation while while areas near Yosemite National Park picked up between one and two inches. Between a tenth and a quarter inch of rain fell across much of the central San Joaquin Valley with locally heavier amounts in areas impacted by thunderstorms. The precipitation fell as snow above 7500 feet and a few locations in Yosemite Park picked up around a foot of fresh snowfall above 8000 feet. Areas south of Fresno County generally did not receive much precipitation. The precipitation tapered off during the evening of March 27 and ended by late morning on March 28 as the storm moved east of the area. California Highway Patrol reported flooding at the intersection of Fields Road and La Grange Road.", "ts_dict_index": [4188, 4189, 4190]}
+{"event_id": 978530, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2021-10-01 15:45:00", "end_date_time": "2021-10-01 18:45:00", "narrative": "The combination of an upper level disturbance crossing the southern Great Plains, upper level wind and a low level low pressure system moving east from Nuevo Leon, Mexico, and prior boundaries from earlier thunderstorms north of the Rio Grande Valley and from morning thunderstorms along the coast combined with deep atmospheric tropical moisture to create a thunderstorm system, including a heavy-precipitation supercell event. Measured and estimated rainfall of 4 to 8 inches in just two hours or so was too much for many drainage systems to handle, and significant flash flooding occurred during the peak of the October 1st (Friday afternoon) late afternoon and evening commute.  The peak of the heavy rainfall occurred between 330 and 7 PM, with some locations in east and northeast Brownsville receiving 7 to 8 inches in two hours or so within that window. Multiple records for daily rainfall were shattered, specifically in the Harlingen and Brownsville areas. Other reports of relatively minor flooding were received from neighboring Willacy and Hidalgo Counties. In addition to widespread flooding, some minor wind damage occurred along with a reported funnel cloud near Harlingen.||Total rainfall in east Brownsville for the date (October 1) ranged from 8 to nearly 11 inches. Picture received from public of Madison Ave in Harlingen under several inches of water. Exact depth unknown at this time.", "ts_dict_index": [4218, 4219, 4220]}
+{"event_id": 802320, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-03-08 05:47:00", "end_date_time": "2019-03-08 09:47:00", "narrative": "Following the departure of the warm and very moist system which brought heavy rain to portions of the area on March 6, a cold upper trough approached the area on March 7 and moved through the region during the morning of March 8. This system provided additional liquid precipitation totals of half an inch to an inch over much of the southern Sierra Nevada with the snow level lowering from 5000 feet during the evening of March 7 to 3500 feet by the afternoon of March 8. While precipitation amounts were generally lower in the San Joaquin Valley and the Kern County Mountains, a few locations impacted by heavier showers or thunderstorms on March 8 received over half an inch. Several locations in the higher elevations of the southern Sierra Nevada (above 7000 feet) picked up between 6 an 12 inches of new snow between the evening of March 7 and the afternoon of March 8. There were some reports of funnel clouds in the San Joaquin Valley although there were no confirmed reports of tornadoes from this system. There were several reports of wind gusts exceeding 45 mph in the Kern County Mountains and Deserts and a few low impact indicator sites measured gusts exceeding 70 mph. This cold system moved out of the area during the evening of March 8 with a drier airmass moving into the area behind it. California Highway Patrol reported flooding at the intersection of State Route 190 and Pleasant Oaks Dr. 4SW Springville.", "ts_dict_index": [4209, 4210, 4211]}
+{"event_id": 815477, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2019-05-26 13:30:00", "end_date_time": "2019-05-26 16:30:00", "narrative": "A strong upper low pressure system pushed southward through the Pacific Northwest on May 25. Warm air advection ahead of this system produced instability over the San Joaquin Valley during the afternoon and evening of May 25 which resulted in the development of scattered thunderstorms. One thunderstorm produced nickel sized hail between Mettler and Maricopa along State Route 166 and also produced roadway flooding in the area. The low moved southward through California on May 26 bringing increased clouds, significant rainfall and mountain snowfall, locally strong winds as well as thunderstorms with heavy rain. Much of the area received between a quarter and three quarters of an inch of liquid precipitation while several stations in the Sierra Nevada picked up between 2 to 5 inches of new snowfall with a few stations picking up 6 to 7 inches. Thunderstorms developed during the afternoon of May 26 across the San Joaquin Valley producing heavy rainfall, roadway flooding and a few funnel clouds. In addition, gusty winds prevailed for much of the day in the Tehachapi and Lake Isabella areas where there were several reports of wind gusts exceeding 35 mph while a few low impact indicator sites measured gusts above 55 mph. Several all time daily record precipitation records were shattered on May 26. Several public reports and social media posts of flooding in downtown Hanford.", "ts_dict_index": [4194, 4195, 4196]}
+{"event_id": 990206, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2021-10-01 21:30:00", "end_date_time": "2021-10-02 18:00:00", "narrative": "The combination of an upper level disturbance crossing the southern Great Plains, upper level wind and a low level low pressure system moving east from Nuevo Leon, Mexico, and prior boundaries from earlier thunderstorms north of the Rio Grande Valley and from morning thunderstorms along the coast combined with deep atmospheric tropical moisture to create a thunderstorm system, including a heavy-precipitation supercell event. Measured and estimated rainfall of 4 to 8 inches in just two hours or so was too much for many drainage systems to handle, and significant flash flooding occurred during the peak of the October 1st (Friday afternoon) late afternoon and evening commute.  The peak of the heavy rainfall occurred between 330 and 7 PM, with some locations in east and northeast Brownsville receiving 7 to 8 inches in two hours or so within that window. Multiple records for daily rainfall were shattered, specifically in the Harlingen and Brownsville areas. Other reports of relatively minor flooding were received from neighboring Willacy and Hidalgo Counties. In addition to widespread flooding, some minor wind damage occurred along with a reported funnel cloud near Harlingen.||Total rainfall in east Brownsville for the date (October 1) ranged from 8 to nearly 11 inches. A resaca continued to overflow its banks along Vermillion Avenue, from 1 to 1.5 miles north of the intersection with Boca Chica Blvd. (State Road 4), well into October 2nd with the road remaining closed. At 18 inches to two feet of water covered the center of the road, with up to four feet on the normal road edges. A CoCoRaHS observer along Vermillion Avenue reported more than 10 inches on the 1st, with most falling during this period; the two-day total was 13.53 inches. End time of the significant flooding is estimated.", "ts_dict_index": [4215, 4216, 4217]}
+{"event_id": 978539, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2021-10-01 16:00:00", "end_date_time": "2021-10-01 19:00:00", "narrative": "The combination of an upper level disturbance crossing the southern Great Plains, upper level wind and a low level low pressure system moving east from Nuevo Leon, Mexico, and prior boundaries from earlier thunderstorms north of the Rio Grande Valley and from morning thunderstorms along the coast combined with deep atmospheric tropical moisture to create a thunderstorm system, including a heavy-precipitation supercell event. Measured and estimated rainfall of 4 to 8 inches in just two hours or so was too much for many drainage systems to handle, and significant flash flooding occurred during the peak of the October 1st (Friday afternoon) late afternoon and evening commute.  The peak of the heavy rainfall occurred between 330 and 7 PM, with some locations in east and northeast Brownsville receiving 7 to 8 inches in two hours or so within that window. Multiple records for daily rainfall were shattered, specifically in the Harlingen and Brownsville areas. Other reports of relatively minor flooding were received from neighboring Willacy and Hidalgo Counties. In addition to widespread flooding, some minor wind damage occurred along with a reported funnel cloud near Harlingen.||Total rainfall in east Brownsville for the date (October 1) ranged from 8 to nearly 11 inches. Video received from public of water reaching up to car bumpers along Washington Ave between Commerce and 1st Streets in Harlingen.", "ts_dict_index": [4212, 4213, 4214]}
+{"event_id": 815479, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-05-26 14:48:00", "end_date_time": "2019-05-26 17:48:00", "narrative": "A strong upper low pressure system pushed southward through the Pacific Northwest on May 25. Warm air advection ahead of this system produced instability over the San Joaquin Valley during the afternoon and evening of May 25 which resulted in the development of scattered thunderstorms. One thunderstorm produced nickel sized hail between Mettler and Maricopa along State Route 166 and also produced roadway flooding in the area. The low moved southward through California on May 26 bringing increased clouds, significant rainfall and mountain snowfall, locally strong winds as well as thunderstorms with heavy rain. Much of the area received between a quarter and three quarters of an inch of liquid precipitation while several stations in the Sierra Nevada picked up between 2 to 5 inches of new snowfall with a few stations picking up 6 to 7 inches. Thunderstorms developed during the afternoon of May 26 across the San Joaquin Valley producing heavy rainfall, roadway flooding and a few funnel clouds. In addition, gusty winds prevailed for much of the day in the Tehachapi and Lake Isabella areas where there were several reports of wind gusts exceeding 35 mph while a few low impact indicator sites measured gusts above 55 mph. Several all time daily record precipitation records were shattered on May 26. California Highway Patrol reported water 2 feet deep between Kingsburg and Selma.", "ts_dict_index": [4200, 4201, 4202]}
+{"event_id": 978541, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2021-10-01 16:30:00", "end_date_time": "2021-10-01 19:30:00", "narrative": "The combination of an upper level disturbance crossing the southern Great Plains, upper level wind and a low level low pressure system moving east from Nuevo Leon, Mexico, and prior boundaries from earlier thunderstorms north of the Rio Grande Valley and from morning thunderstorms along the coast combined with deep atmospheric tropical moisture to create a thunderstorm system, including a heavy-precipitation supercell event. Measured and estimated rainfall of 4 to 8 inches in just two hours or so was too much for many drainage systems to handle, and significant flash flooding occurred during the peak of the October 1st (Friday afternoon) late afternoon and evening commute.  The peak of the heavy rainfall occurred between 330 and 7 PM, with some locations in east and northeast Brownsville receiving 7 to 8 inches in two hours or so within that window. Multiple records for daily rainfall were shattered, specifically in the Harlingen and Brownsville areas. Other reports of relatively minor flooding were received from neighboring Willacy and Hidalgo Counties. In addition to widespread flooding, some minor wind damage occurred along with a reported funnel cloud near Harlingen.||Total rainfall in east Brownsville for the date (October 1) ranged from 8 to nearly 11 inches. Picture received from the public of water halfway up the wheel wells of several cars in Los Fresnos near the library.", "ts_dict_index": [4221, 4222, 4223]}
+{"event_id": 1108949, "event_type": "Flood", "state": "MAINE", "cz_name": "OXFORD", "begin_date_time": "2023-06-26 06:00:00", "end_date_time": "2023-06-26 10:00:00", "narrative": "Slow moving showers and thunderstorms associated with a broad area of low pressure moved across western Maine through the night of June 25th and into the morning of June 26th. Showers and thunderstorms repeatedly developed over the hills and mountains surrounding Andover and Byron in Oxford County, The extreme rainfall rates in hilly and mountainous terrain led to rapid run-off on multiple streams in the region. Maine. Localized heavy rain occurred in these areas with considerable flash flooding being reported. Showers and thunderstorms began in the Andover area around 2:30 am on June 26th.  The storms intensified and spread across the mountains in the surrounding towns to include Byron and Roxbury.  Rainfall rates peaked from 3:30 am to 6:00 am when the bulk of the heavy rainfall fell in the region.  The showers and thunderstorms weakened and moved off to the north with just very light rainfall through 8 am before ending.  Radar estimated rainfall amounts of 2 to 3��� in Bryon and Roxbury with even higher amounts of rain in North Andover. Radar estimated a very localized area of rainfall of up to 6��� of rainfall just north of town in mountainous terrain.   The bulk of this rainfall occurred in less than 3 hours.  The extreme rainfall rates in hilly and mountainous terrain led to rapid run-off on multiple streams in the region. Heavy rainfall between 3 and 4 inches fell across the headwaters of the Swift River during the early morning hours of the 26th. The resultant runoff caused the river to rise above flood stage (7Ft) and crest at 8.32 feet around 945 AM based on data from the USGS river gage in Roxbury. State Route 17 is closed in Roxbury due to flooding from Frye Crossover Road to Black Ridge Road.", "ts_dict_index": [4182, 4183, 4184]}
+{"event_id": 793383, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-01-17 05:10:00", "end_date_time": "2019-01-17 07:10:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. California Highway Patrol reported roadway flooding affecting the westbound lanes of State Route 58 east of Cottonwood Road in Bakersfield.", "ts_dict_index": [4179, 4180, 4181]}
+{"event_id": 793390, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-01-17 09:06:00", "end_date_time": "2019-01-17 11:06:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. California Highway Patrol reported roadway flooding on Joshua St. in South Lake.", "ts_dict_index": [4170, 4171, 4172]}
+{"event_id": 793389, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-01-17 08:33:00", "end_date_time": "2019-01-17 10:33:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. Public report of roadway flooding on F St. in Bakersfield.", "ts_dict_index": [4158, 4159, 4160]}
+{"event_id": 815476, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-05-25 16:27:00", "end_date_time": "2019-05-25 18:27:00", "narrative": "A strong upper low pressure system pushed southward through the Pacific Northwest on May 25. Warm air advection ahead of this system produced instability over the San Joaquin Valley during the afternoon and evening of May 25 which resulted in the development of scattered thunderstorms. One thunderstorm produced nickel sized hail between Mettler and Maricopa along State Route 166 and also produced roadway flooding in the area. The low moved southward through California on May 26 bringing increased clouds, significant rainfall and mountain snowfall, locally strong winds as well as thunderstorms with heavy rain. Much of the area received between a quarter and three quarters of an inch of liquid precipitation while several stations in the Sierra Nevada picked up between 2 to 5 inches of new snowfall with a few stations picking up 6 to 7 inches. Thunderstorms developed during the afternoon of May 26 across the San Joaquin Valley producing heavy rainfall, roadway flooding and a few funnel clouds. In addition, gusty winds prevailed for much of the day in the Tehachapi and Lake Isabella areas where there were several reports of wind gusts exceeding 35 mph while a few low impact indicator sites measured gusts above 55 mph. Several all time daily record precipitation records were shattered on May 26. California Highway report reported roadway flooding on Wheeler Ridge Rd. east of Mettler.", "ts_dict_index": [4206, 4207, 4208]}
+{"event_id": 793386, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-01-17 06:33:00", "end_date_time": "2019-01-17 08:33:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. California Highway Patrol reported roadway flooding at the intersection of Pellisier Road and Banducci Road near Stallion Springs.", "ts_dict_index": [4164, 4165, 4166]}
+{"event_id": 793384, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-01-17 05:44:00", "end_date_time": "2019-01-17 09:44:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. California Highway Patrol reported the northbound lanes of Lake Isabella Blvd. completely flooded at the Chain Ave. intersection in Bodfish.", "ts_dict_index": [4167, 4168, 4169]}
+{"event_id": 793385, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-01-17 06:19:00", "end_date_time": "2019-01-17 10:19:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. California Highway Patrol reported Redrock-Randsburg Road flooded at the intersection of Garlock Road near Randsburg.", "ts_dict_index": [4176, 4177, 4178]}
+{"event_id": 815474, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-05-25 15:46:00", "end_date_time": "2019-05-25 17:46:00", "narrative": "A strong upper low pressure system pushed southward through the Pacific Northwest on May 25. Warm air advection ahead of this system produced instability over the San Joaquin Valley during the afternoon and evening of May 25 which resulted in the development of scattered thunderstorms. One thunderstorm produced nickel sized hail between Mettler and Maricopa along State Route 166 and also produced roadway flooding in the area. The low moved southward through California on May 26 bringing increased clouds, significant rainfall and mountain snowfall, locally strong winds as well as thunderstorms with heavy rain. Much of the area received between a quarter and three quarters of an inch of liquid precipitation while several stations in the Sierra Nevada picked up between 2 to 5 inches of new snowfall with a few stations picking up 6 to 7 inches. Thunderstorms developed during the afternoon of May 26 across the San Joaquin Valley producing heavy rainfall, roadway flooding and a few funnel clouds. In addition, gusty winds prevailed for much of the day in the Tehachapi and Lake Isabella areas where there were several reports of wind gusts exceeding 35 mph while a few low impact indicator sites measured gusts above 55 mph. Several all time daily record precipitation records were shattered on May 26. California Highway Patrol reported roadway flooding on State Route 166 west of the Old River Rd. intersection.", "ts_dict_index": [4203, 4204, 4205]}
+{"event_id": 793388, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-01-17 08:24:00", "end_date_time": "2019-01-17 10:24:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. California Highway Patrol reported roadway flooding on Rosamond Blvd. in Rosamond.", "ts_dict_index": [4173, 4174, 4175]}
+{"event_id": 817485, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "FLOYD", "begin_date_time": "2019-06-06 17:25:00", "end_date_time": "2019-06-06 18:55:00", "narrative": "Slow moving storms developed during the late afternoon and early��evening of June 6th. The slow movement produced locally heavy rainfall which produced some flash flooding in a few communities of eastern Kentucky, including Rockcastle and Powell Counties.||In Rockcastle County, at least 6 businesses, a church, and city hall were inundated with water in Brodhead. Several local, county, and state highways were closed during the peak of the flooding. Two storage buildings were washed off of their foundations, while about 10 mobile homes were damaged as nearly 4 inches of rain fell in a 2 1/2 hour window during the late afternoon into the early evening of the 6th.||In Powell County, flash flooding occurred in and around the Natural Bridge State Park area, northward to the Slade exit off the Mountain Parkway. Multiple water rescues were performed as many homes became surrounded by water. A water rescue took place at the 5900 block of High Rock Road, where 2 people were trapped in their car surrounded by flood waters. Multiple locations along Highway 11 had flowing water across the road. Several cars were at least partially submerged. Little Abner's Motel near the park��was also flooded out.||Light to moderate rain continued through June 7, producing additional minor issues. These included mudslides and road closures. Emergency Management reported water causing travel issues near Hite.", "ts_dict_index": [4185, 4186, 4187]}
+{"event_id": 802962, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2019-01-24 18:21:00", "end_date_time": "2019-01-25 05:42:00", "narrative": "Following a heavy snowfall event on January 19-20 over much of eastern New York, a strong low pressure system tracking through southern Canada ushered in an unseasonably warm and moist airmass on January 24th. Temperatures surged into the 40s to mid-50s. Steady rainfall occurred during much of the 24th as a secondary low pressure system developed over the Mid-Atlantic and tracked into southern New England. One to two inches of rainfall occurred over much of the region, although a few reports of three to four inches were recorded over portions of the southern Adirondacks and the eastern Catskills. New daily rainfall records were set at Albany, Glens Falls, and Poughkeepsie.||The combination of the rainfall along with the mild temperatures melting some of the snow resulted in urban and poor drainage flooding over portions of the region along with minor to moderate river flooding in the Hoosic basin. Some ice jam flooding also occurred. Numerous road closures also occurred due to flooding in Washington County, NY. In addition, seven vessels along the Hudson River near Troy were ripped from their moorings during the early morning of the 25th, likely by a surge of water and ice from upstream. Some of these vessels struck bridges, resulting in bridge closures during the morning rush hour, including the Patroon Island Bridge which carries I-90 over the Hudson. Rathbun Avenue was closed due to flooding along the Mettawee River.", "ts_dict_index": [4140, 4141, 4142]}
+{"event_id": 815478, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-05-26 13:37:00", "end_date_time": "2019-05-26 15:37:00", "narrative": "A strong upper low pressure system pushed southward through the Pacific Northwest on May 25. Warm air advection ahead of this system produced instability over the San Joaquin Valley during the afternoon and evening of May 25 which resulted in the development of scattered thunderstorms. One thunderstorm produced nickel sized hail between Mettler and Maricopa along State Route 166 and also produced roadway flooding in the area. The low moved southward through California on May 26 bringing increased clouds, significant rainfall and mountain snowfall, locally strong winds as well as thunderstorms with heavy rain. Much of the area received between a quarter and three quarters of an inch of liquid precipitation while several stations in the Sierra Nevada picked up between 2 to 5 inches of new snowfall with a few stations picking up 6 to 7 inches. Thunderstorms developed during the afternoon of May 26 across the San Joaquin Valley producing heavy rainfall, roadway flooding and a few funnel clouds. In addition, gusty winds prevailed for much of the day in the Tehachapi and Lake Isabella areas where there were several reports of wind gusts exceeding 35 mph while a few low impact indicator sites measured gusts above 55 mph. Several all time daily record precipitation records were shattered on May 26. A trained spotter reported minor street flooding south of Selma.", "ts_dict_index": [4197, 4198, 4199]}
+{"event_id": 978540, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2021-10-01 16:15:00", "end_date_time": "2021-10-01 20:15:00", "narrative": "The combination of an upper level disturbance crossing the southern Great Plains, upper level wind and a low level low pressure system moving east from Nuevo Leon, Mexico, and prior boundaries from earlier thunderstorms north of the Rio Grande Valley and from morning thunderstorms along the coast combined with deep atmospheric tropical moisture to create a thunderstorm system, including a heavy-precipitation supercell event. Measured and estimated rainfall of 4 to 8 inches in just two hours or so was too much for many drainage systems to handle, and significant flash flooding occurred during the peak of the October 1st (Friday afternoon) late afternoon and evening commute.  The peak of the heavy rainfall occurred between 330 and 7 PM, with some locations in east and northeast Brownsville receiving 7 to 8 inches in two hours or so within that window. Multiple records for daily rainfall were shattered, specifically in the Harlingen and Brownsville areas. Other reports of relatively minor flooding were received from neighboring Willacy and Hidalgo Counties. In addition to widespread flooding, some minor wind damage occurred along with a reported funnel cloud near Harlingen.||Total rainfall in east Brownsville for the date (October 1) ranged from 8 to nearly 11 inches. Video received from the public of water covering US-77/Sunshine Strip near the VA Health Center in Harlingen. Water was reaching up to the bumpers of some sedans.", "ts_dict_index": [4230, 4231, 4232]}
+{"event_id": 932347, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 17:12:00", "end_date_time": "2021-01-27 17:42:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Roadway flooding at US-101 N and Esperanza Rd.", "ts_dict_index": [4263, 4264, 4265]}
+{"event_id": 932371, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-28 20:58:00", "end_date_time": "2021-01-28 21:28:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Flooding on River Rd at Fairview Rd.", "ts_dict_index": [4242, 4243, 4244]}
+{"event_id": 932349, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 18:47:00", "end_date_time": "2021-01-27 19:17:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Roadway flooding at US-101 N and Hudson Rd.", "ts_dict_index": [4254, 4255, 4256]}
+{"event_id": 932367, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-28 19:32:00", "end_date_time": "2021-01-28 20:02:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Flooding at US-101 N and Sanborn.", "ts_dict_index": [4248, 4249, 4250]}
+{"event_id": 932346, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 16:25:00", "end_date_time": "2021-01-27 16:55:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Roadway flooding at US-101 N and Main St. Flooding is causing vehicles to hydroplane.", "ts_dict_index": [4260, 4261, 4262]}
+{"event_id": 978542, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2021-10-01 16:30:00", "end_date_time": "2021-10-01 20:30:00", "narrative": "The combination of an upper level disturbance crossing the southern Great Plains, upper level wind and a low level low pressure system moving east from Nuevo Leon, Mexico, and prior boundaries from earlier thunderstorms north of the Rio Grande Valley and from morning thunderstorms along the coast combined with deep atmospheric tropical moisture to create a thunderstorm system, including a heavy-precipitation supercell event. Measured and estimated rainfall of 4 to 8 inches in just two hours or so was too much for many drainage systems to handle, and significant flash flooding occurred during the peak of the October 1st (Friday afternoon) late afternoon and evening commute.  The peak of the heavy rainfall occurred between 330 and 7 PM, with some locations in east and northeast Brownsville receiving 7 to 8 inches in two hours or so within that window. Multiple records for daily rainfall were shattered, specifically in the Harlingen and Brownsville areas. Other reports of relatively minor flooding were received from neighboring Willacy and Hidalgo Counties. In addition to widespread flooding, some minor wind damage occurred along with a reported funnel cloud near Harlingen.||Total rainfall in east Brownsville for the date (October 1) ranged from 8 to nearly 11 inches. Public report of several inches of water flooding the intersection of Boca Chica Blvd and Central Ave.", "ts_dict_index": [4233, 4234, 4235]}
+{"event_id": 978525, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2021-10-01 15:00:00", "end_date_time": "2021-10-01 18:00:00", "narrative": "The combination of an upper level disturbance crossing the southern Great Plains, upper level wind and a low level low pressure system moving east from Nuevo Leon, Mexico, and prior boundaries from earlier thunderstorms north of the Rio Grande Valley and from morning thunderstorms along the coast combined with deep atmospheric tropical moisture to create a thunderstorm system, including a heavy-precipitation supercell event. Measured and estimated rainfall of 4 to 8 inches in just two hours or so was too much for many drainage systems to handle, and significant flash flooding occurred during the peak of the October 1st (Friday afternoon) late afternoon and evening commute.  The peak of the heavy rainfall occurred between 330 and 7 PM, with some locations in east and northeast Brownsville receiving 7 to 8 inches in two hours or so within that window. Multiple records for daily rainfall were shattered, specifically in the Harlingen and Brownsville areas. Other reports of relatively minor flooding were received from neighboring Willacy and Hidalgo Counties. In addition to widespread flooding, some minor wind damage occurred along with a reported funnel cloud near Harlingen.||Total rainfall in east Brownsville for the date (October 1) ranged from 8 to nearly 11 inches. Report received from public of several inches of water topping the curbs at the intersection of Business 77 and Harrison Road in Harlingen.", "ts_dict_index": [4227, 4228, 4229]}
+{"event_id": 932351, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 20:55:00", "end_date_time": "2021-01-27 21:25:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. US-101 N closed at Airport Rd due to flooding.", "ts_dict_index": [4266, 4267, 4268]}
+{"event_id": 932350, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 20:37:00", "end_date_time": "2021-01-27 21:07:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Roadway flooding at US-101 N and Gloria Rd.", "ts_dict_index": [4251, 4252, 4253]}
+{"event_id": 932353, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 22:09:00", "end_date_time": "2021-01-27 22:39:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Roadway flooding on US-101 S and Jolon Rd.", "ts_dict_index": [4269, 4270, 4271]}
+{"event_id": 932450, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 18:45:00", "end_date_time": "2021-01-27 19:15:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Roadway flooding at Old Stage Rd and Esperanza Rd.", "ts_dict_index": [4239, 4240, 4241]}
+{"event_id": 1001672, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-03-04 06:44:00", "end_date_time": "2022-03-04 09:44:00", "narrative": "A low pressure system dropped southward off the California coast on March 3 then turned inland and moved across southern California during the morning of March 4 spreading moderate to locally heavy precipitation into the south San Joaquin Valley with localized street flooding being observed in the Bakersfield area. Light precipitation impacted the Tehachapi Mountains with the snow level lowering from 5000 feet at the onset of the precipitation to 4000 feet by the evening of March 4.  A colder system then dropped southward along the California Nevada border on March 5 which pushed a cold front southward through the area bringing mainly light precipitation to much of our area and lowering the snow level to around 2000 feet.  Snowfall was generally 3 to 6 inches of above 5000 feet and 1 to 3 inches between 2500 feet and 5000 feet.  The snow did result in traffic being paced along Interstate 5 over the Tejon Pass for a few hours on March 5 and briefly closed a few roads in the Kern County Mountains as some precautionary measures were taken.  Parts of the south San Joaquin Valley picked up between 0.75 inches and 1.5 inches of rainfall, but further north the the central valley most locations picked up between a quarter and a half inch of rainfall. California Highway Patrol reported that the intersection of SR 184 and Redbank Rd. in Bakersfield was completely flooded.", "ts_dict_index": [4236, 4237, 4238]}
+{"event_id": 793387, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-01-17 07:03:00", "end_date_time": "2019-01-17 09:03:00", "narrative": "A strong low pressure system with a deep moisture fetch pushed into central California during the afternoon of January 16 and brought moderate to heavy precipitation along with strong winds to much of the area through the afternoon of January 17. Several reports of roadway flooding were received during the morning of January 17 when the heaviest precipitation occurred. Flash flooding and debris flows were reported in the Ferguson Fire burn area in Mariposa County and State Route 140 was closed for over 11 hours. The precipitation turned to showers and isolated thunderstorms during the afternoon of January 17. One thunderstorm produced a tornado east of Clovis which was rated as EF-1 following a storm survey of the damage it produced. Most of the San Joaquin Valley and Kern County Deserts picked up between half an inch to an inch of rain while the Southern Sierra Nevada had 2 to 4 inches of liquid precipitation and the Kern County Mountains had 1.5 to 3 inches of liquid precipitation. The precipitation mainly fell as snow above 7000 feet where several locations in the higher elevations of the Southern Sierra Nevada above 7000 feet picked up 10 to 20 inches of new snowfall. There were also several reports of post-frontal wind gusts exceeding 50 mph in the Kern County Mountains and Deserts while a few low impact indicator sites had gusts exceeding 65 mph. California Highway Patrol reported roadway flooding at the intersection of Niles St. and Mount Vernon Ave in Bakersfield.", "ts_dict_index": [4161, 4162, 4163]}
+{"event_id": 932340, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 14:43:00", "end_date_time": "2021-01-27 15:13:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Road flooded at US-101 N and Chualar, lane closed.", "ts_dict_index": [4278, 4279, 4280]}
+{"event_id": 932341, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 14:55:00", "end_date_time": "2021-01-27 15:25:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Roadway flooding at US-101 south near King City.", "ts_dict_index": [4275, 4276, 4277]}
+{"event_id": 932354, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 22:30:00", "end_date_time": "2021-01-27 23:00:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. US-101 N closed from Front St to Front St SB off ramp due to flooding.", "ts_dict_index": [4281, 4282, 4283]}
+{"event_id": 932345, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 16:18:00", "end_date_time": "2021-01-27 16:48:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Roadway flooding at Elm and Metz near Greenfield.", "ts_dict_index": [4272, 4273, 4274]}
+{"event_id": 978507, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2021-10-01 20:30:00", "end_date_time": "2021-10-02 08:30:00", "narrative": "The combination of an upper level disturbance crossing the southern Great Plains, upper level wind and a low level low pressure system moving east from Nuevo Leon, Mexico, and prior boundaries from earlier thunderstorms north of the Rio Grande Valley and from morning thunderstorms along the coast combined with deep atmospheric tropical moisture to create a thunderstorm system, including a heavy-precipitation supercell event. Measured and estimated rainfall of 4 to 8 inches in just two hours or so was too much for many drainage systems to handle, and significant flash flooding occurred during the peak of the October 1st (Friday afternoon) late afternoon and evening commute.  The peak of the heavy rainfall occurred between 330 and 7 PM, with some locations in east and northeast Brownsville receiving 7 to 8 inches in two hours or so within that window. Multiple records for daily rainfall were shattered, specifically in the Harlingen and Brownsville areas. Other reports of relatively minor flooding were received from neighboring Willacy and Hidalgo Counties. In addition to widespread flooding, some minor wind damage occurred along with a reported funnel cloud near Harlingen.||Total rainfall in east Brownsville for the date (October 1) ranged from 8 to nearly 11 inches. Many portions of FM 802/Ruben Torres Blvd in Brownsville remained under several feet of water through the morning hours on the 2nd due to overwhelmed drainage systems in the area. It was not until around 9:00-9:30 AM local time on October 2nd that flood waters finally began to recede to the point of roads being traversable by mid-size cars.  Other high water of 2 to 3 feet along the sides of roads in a subdivision along Dana Avenue north of Ruben Torres Blvd. continued through the afternoon of October 2nd.  Damage to vehicles and property was not known as of this writing.", "ts_dict_index": [4224, 4225, 4226]}
+{"event_id": 1065824, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-16 10:37:00", "end_date_time": "2023-01-16 12:37:00", "narrative": "The strong storm that brought widespread precipitation and additional flooding to the area on January 14 was followed by another storm which moved through the area between the afternoon of January 15 and the afternoon of January 16. While precipitation amounts from this storm were significantly less across most of the area than with the previous two storms which impacted the area over the previous week, this system produced a period of damaging wind gusts in the San Joaquin Valley during the morning of January 16 as the cold front from this system pushed through the area. There were several reports of wind gusts exceeding 40 mph in the San Joaquin Valley and Sierra foothills and wind gusts exceeding 60 mph in the Tehachapi Mountains and the West Side Hills. The strong winds resulted in numerous power outages as power poles and power lines were toppled as well as road closures as the winds brought trees down across roads. Some more flooding occurred in the area as a result of additional rainfall on soil which had been heavily saturated by previous recent storms. The winds did taper off by the afternoon of January 16, but the precipitation was very slow to taper off as the storm didn't completely move out of the area until January 17. California Highway Patrol reported flooding on SR 33 just north of Sullivan Rd. in Gustine.", "ts_dict_index": [4296, 4297, 4298]}
+{"event_id": 1065830, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-16 16:14:00", "end_date_time": "2023-01-16 18:14:00", "narrative": "The strong storm that brought widespread precipitation and additional flooding to the area on January 14 was followed by another storm which moved through the area between the afternoon of January 15 and the afternoon of January 16. While precipitation amounts from this storm were significantly less across most of the area than with the previous two storms which impacted the area over the previous week, this system produced a period of damaging wind gusts in the San Joaquin Valley during the morning of January 16 as the cold front from this system pushed through the area. There were several reports of wind gusts exceeding 40 mph in the San Joaquin Valley and Sierra foothills and wind gusts exceeding 60 mph in the Tehachapi Mountains and the West Side Hills. The strong winds resulted in numerous power outages as power poles and power lines were toppled as well as road closures as the winds brought trees down across roads. Some more flooding occurred in the area as a result of additional rainfall on soil which had been heavily saturated by previous recent storms. The winds did taper off by the afternoon of January 16, but the precipitation was very slow to taper off as the storm didn't completely move out of the area until January 17. California Highway Patrol reported roadway flooding along W. Sandy Mush Rd. near S. Gurr Rd.", "ts_dict_index": [4287, 4288, 4289]}
+{"event_id": 1065833, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-17 08:47:00", "end_date_time": "2023-01-17 14:47:00", "narrative": "The strong storm that brought widespread precipitation and additional flooding to the area on January 14 was followed by another storm which moved through the area between the afternoon of January 15 and the afternoon of January 16. While precipitation amounts from this storm were significantly less across most of the area than with the previous two storms which impacted the area over the previous week, this system produced a period of damaging wind gusts in the San Joaquin Valley during the morning of January 16 as the cold front from this system pushed through the area. There were several reports of wind gusts exceeding 40 mph in the San Joaquin Valley and Sierra foothills and wind gusts exceeding 60 mph in the Tehachapi Mountains and the West Side Hills. The strong winds resulted in numerous power outages as power poles and power lines were toppled as well as road closures as the winds brought trees down across roads. Some more flooding occurred in the area as a result of additional rainfall on soil which had been heavily saturated by previous recent storms. The winds did taper off by the afternoon of January 16, but the precipitation was very slow to taper off as the storm didn't completely move out of the area until January 17. California Highway Patrol reported road 108 was closed between Ave. 368 and Ave. 384 due to flooding.", "ts_dict_index": [4290, 4291, 4292]}
+{"event_id": 1065829, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-16 14:43:00", "end_date_time": "2023-01-16 16:43:00", "narrative": "The strong storm that brought widespread precipitation and additional flooding to the area on January 14 was followed by another storm which moved through the area between the afternoon of January 15 and the afternoon of January 16. While precipitation amounts from this storm were significantly less across most of the area than with the previous two storms which impacted the area over the previous week, this system produced a period of damaging wind gusts in the San Joaquin Valley during the morning of January 16 as the cold front from this system pushed through the area. There were several reports of wind gusts exceeding 40 mph in the San Joaquin Valley and Sierra foothills and wind gusts exceeding 60 mph in the Tehachapi Mountains and the West Side Hills. The strong winds resulted in numerous power outages as power poles and power lines were toppled as well as road closures as the winds brought trees down across roads. Some more flooding occurred in the area as a result of additional rainfall on soil which had been heavily saturated by previous recent storms. The winds did taper off by the afternoon of January 16, but the precipitation was very slow to taper off as the storm didn't completely move out of the area until January 17. California Highway Patrol reported a tree washed up on the roadway on eastbound SR 140 east of Hummingbird Ln.", "ts_dict_index": [4299, 4300, 4301]}
+{"event_id": 932352, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-27 22:02:00", "end_date_time": "2021-01-27 22:32:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Roadway flooding on US-101 S and Central.", "ts_dict_index": [4284, 4285, 4286]}
+{"event_id": 1065823, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-16 09:58:00", "end_date_time": "2023-01-16 11:58:00", "narrative": "The strong storm that brought widespread precipitation and additional flooding to the area on January 14 was followed by another storm which moved through the area between the afternoon of January 15 and the afternoon of January 16. While precipitation amounts from this storm were significantly less across most of the area than with the previous two storms which impacted the area over the previous week, this system produced a period of damaging wind gusts in the San Joaquin Valley during the morning of January 16 as the cold front from this system pushed through the area. There were several reports of wind gusts exceeding 40 mph in the San Joaquin Valley and Sierra foothills and wind gusts exceeding 60 mph in the Tehachapi Mountains and the West Side Hills. The strong winds resulted in numerous power outages as power poles and power lines were toppled as well as road closures as the winds brought trees down across roads. Some more flooding occurred in the area as a result of additional rainfall on soil which had been heavily saturated by previous recent storms. The winds did taper off by the afternoon of January 16, but the precipitation was very slow to taper off as the storm didn't completely move out of the area until January 17. California Highway Patrol reported rock, dirt and mud in the roadway on SR 140 near Guadalupe Fire Rd.", "ts_dict_index": [4308, 4309, 4310]}
+{"event_id": 1065825, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-16 10:56:00", "end_date_time": "2023-01-16 12:56:00", "narrative": "The strong storm that brought widespread precipitation and additional flooding to the area on January 14 was followed by another storm which moved through the area between the afternoon of January 15 and the afternoon of January 16. While precipitation amounts from this storm were significantly less across most of the area than with the previous two storms which impacted the area over the previous week, this system produced a period of damaging wind gusts in the San Joaquin Valley during the morning of January 16 as the cold front from this system pushed through the area. There were several reports of wind gusts exceeding 40 mph in the San Joaquin Valley and Sierra foothills and wind gusts exceeding 60 mph in the Tehachapi Mountains and the West Side Hills. The strong winds resulted in numerous power outages as power poles and power lines were toppled as well as road closures as the winds brought trees down across roads. Some more flooding occurred in the area as a result of additional rainfall on soil which had been heavily saturated by previous recent storms. The winds did taper off by the afternoon of January 16, but the precipitation was very slow to taper off as the storm didn't completely move out of the area until January 17. Kern County officials reported Lytle Ave was closed between Cecil Ave. and Dirt Rd. due to flooding.", "ts_dict_index": [4302, 4303, 4304]}
+{"event_id": 1065832, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-16 18:54:00", "end_date_time": "2023-01-16 20:54:00", "narrative": "The strong storm that brought widespread precipitation and additional flooding to the area on January 14 was followed by another storm which moved through the area between the afternoon of January 15 and the afternoon of January 16. While precipitation amounts from this storm were significantly less across most of the area than with the previous two storms which impacted the area over the previous week, this system produced a period of damaging wind gusts in the San Joaquin Valley during the morning of January 16 as the cold front from this system pushed through the area. There were several reports of wind gusts exceeding 40 mph in the San Joaquin Valley and Sierra foothills and wind gusts exceeding 60 mph in the Tehachapi Mountains and the West Side Hills. The strong winds resulted in numerous power outages as power poles and power lines were toppled as well as road closures as the winds brought trees down across roads. Some more flooding occurred in the area as a result of additional rainfall on soil which had been heavily saturated by previous recent storms. The winds did taper off by the afternoon of January 16, but the precipitation was very slow to taper off as the storm didn't completely move out of the area until January 17. California Highway Patrol reported standing water on SR 99 near Cecil Ave.", "ts_dict_index": [4305, 4306, 4307]}
+{"event_id": 932363, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-28 15:00:00", "end_date_time": "2021-01-28 16:00:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. Flooding, mud, rocks, and other debris shown in photograph on Nacimiento-Fergusson Rd and Del Venturi.", "ts_dict_index": [4245, 4246, 4247]}
+{"event_id": 1065831, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-16 16:15:00", "end_date_time": "2023-01-16 18:15:00", "narrative": "The strong storm that brought widespread precipitation and additional flooding to the area on January 14 was followed by another storm which moved through the area between the afternoon of January 15 and the afternoon of January 16. While precipitation amounts from this storm were significantly less across most of the area than with the previous two storms which impacted the area over the previous week, this system produced a period of damaging wind gusts in the San Joaquin Valley during the morning of January 16 as the cold front from this system pushed through the area. There were several reports of wind gusts exceeding 40 mph in the San Joaquin Valley and Sierra foothills and wind gusts exceeding 60 mph in the Tehachapi Mountains and the West Side Hills. The strong winds resulted in numerous power outages as power poles and power lines were toppled as well as road closures as the winds brought trees down across roads. Some more flooding occurred in the area as a result of additional rainfall on soil which had been heavily saturated by previous recent storms. The winds did taper off by the afternoon of January 16, but the precipitation was very slow to taper off as the storm didn't completely move out of the area until January 17. California Highway Patrol reported roadway flooding along Westside Blvd. near Weir Ave.", "ts_dict_index": [4314, 4315, 4316]}
+{"event_id": 1071061, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2022-12-23 14:00:00", "end_date_time": "2022-12-23 18:00:00", "narrative": "Two separate frontal systems merged to form a powerful winter storm over the Great Lakes from December 22 to December 24 bringing multiple hazards to the region including heavy rain, snow, strong winds and a very cold air mass in its wake.||Widespread rainfall amounts of 1 to 3 inches were observed with some localized amounts of 4 inches. The combination of the rain and snowmelt in some places resulted in some flooding and some creeks to overflow their banks.||Strong pre-frontal and post-frontal winds occurred with this event with widespread wind gusts of 40 to 55 mph. Such winds resulted in some downed trees and power lines as well as minor damage to some structures. A few power outages occurred as a result.||Snow showers in the wake of the cold front brought mainly light accumulations. However, a pocket of more moderate snow occurred across the northern and central Taconics with snowfall amounts in the 4 to 8 inch range.||Much colder air built into the region in the wake of the front which, combined with the strong winds, led to wind chill values as low as 15 to 25 degrees below zero in some areas. A few warming centers opened up across the region as a result of the cold.||Key impacts: minor flooding, tree damage, power outages. Broadcast Media reported water over Lighthouse Drive and Ferry Street in Saugerties.", "ts_dict_index": [4317, 4318, 4319]}
+{"event_id": 932492, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-01-28 04:30:00", "end_date_time": "2021-01-28 11:00:00", "narrative": "A plume of moisture from the tropical Pacific brought an Atmospheric River to the Bay Area January 26th-29th. This system generated heavy rain rates causing flooding and debris flows over area burn scars as well as 15 to 20 inches of rain in the Santa Lucia Mountains. Mudflows near the River Fire burn scar in Monterey County caused damage to homes, covered roadways, and trapped animals at local ranches. Debris flows near the Dolan Fire burn scar caused an entire section of Highway 1 near Rat Creek to collapse into the Pacific Ocean. This was an unusually cold system for an Atmospheric River resulting in lower snow levels and allowing for accumulating snow as low as 1300 feet in elevation. Additionally, strong south to southeast winds gusted to 60-70 mph across area peaks with Mt Diablo reaching 80 mph. Valley locations were gusting up to 40 mph. Numerous trees fell across the region including into homes and onto cars. Multiple power outages were also reported. It is estimated that the storm caused millions of dollars in damage across Santa Cruz County https://www.ksbw.com/article/emergency-declaration-made-in-santa-cruz-county-for-millions-in-damages/35400060.  Full storm summary https://www.weather.gov/mtr/AtmosphericRiver_1_26-29_2021. At the mouth of the Carmel River a sandbar blocked off the Carmel River Lagoon. Persistent heavy rain sent water into low-lying areas just north of the lagoon with flooding reported at homes on 16th street. The lagoon breached the sandbar by 11 am https://www.ksbw.com/article/californias-covid-19-death-toll-edges-past-new-york/35481836.", "ts_dict_index": [4257, 4258, 4259]}
+{"event_id": 1102186, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2023-05-01 09:19:00", "end_date_time": "2023-05-01 13:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday April 30th through Monday May 1st. Heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and the vegetation still dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd. Locally heavy rain caused Route 16B flooding at the intersection of Route 16 in Center Ossipee.", "ts_dict_index": [4323, 4324, 4325]}
+{"event_id": 1102196, "event_type": "Flood", "state": "NEW HAMPSHIRE", "cz_name": "CARROLL", "begin_date_time": "2023-05-01 06:00:00", "end_date_time": "2023-05-02 01:00:00", "narrative": "A broad area of low pressure across the Great Lakes region stalled out well to the west of the region early on Sunday April 30th.  A secondary area of low pressure developed and moved up the Eastern Seaboard and tracked across interior New England from Sunday April 30th through Monday May 1st. Heavy rainfall occurred, and flooding was enhanced for this weather event due to the seasonal timing of the rains with spring soils being high in moisture and the vegetation still dormant.  These two factors lead to increased run-off. Rain started across southern and coastal areas early on Sunday April 30th, with the heaviest rainfall Sunday night into early Monday morning. The rainfall on Sunday produced limited flooding, but set the stage for what was to come by swelling rivers and filling ditches ahead of the heavier rain. Heavy rain started around 3 AM and continued through 10 AM Monday with rainfall rates between 1 to 1.5 inches an hour. This caused flooding to rapidly develop, resulting in widespread flash flooding. The rainfall ended by midday on Monday May 1st. Runoff spilled into tributary rivers and major rivers that led to ongoing flooding for the next several days with most rivers cresting late on Monday May 1st or on May 2nd. The Saco River came out of banks on May 1st that caused significant flooding to several camps and campgrounds between Conway and Bartlett.  The flooding significantly impacted travel in and out of the area due to closed roads. Flooding started on the upper portion of the West Side Road with minor property inundation. The floodwater moved downstream causing significant damage to area campgrounds in North Conway and backwater on the Ellis River.  In North Conway a section of West Side Road flooded, cutting off access to several homes. River Road flooded on the west bank of the Saco River flooding agricultural lands.  Floodwaters inundated first floors of properties in Transvale Acres.  Moat Brook Road flooded cutting off seasonal camps. Widespread agricultural flooding occurred between Conway and Fryberg.  The river levels were at the bridge deck of the Saco River Covered Bridge in Conway.  The USGS river gage in Conway crested at a 13.6 feet, exceeding the 9 foot flood stage by 4.6 feet.", "ts_dict_index": [4320, 4321, 4322]}
+{"event_id": 1090025, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. Buckeye Fire Department performed a water rescue at the unbridged Gila River crossing along El Mirage Road between Southern Avenue and Indian Springs Road on the 18th. The exact details surrounding the water rescue are unknown. The road had been closed since the 14th due to the elevated flow in the river. Event timing is based on releases from Granite Reef Dam.", "ts_dict_index": [4329, 4330, 4331]}
+{"event_id": 1090100, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. Two people kayaking on the Salt River approaching the Phon D Sutton Recreation Area became separated before one of them capsized on the 19th. The capsized kayaker was able to hold onto trees while the Maricopa County Sheriff's Office worked to rescue him via helicopter. The man was safely rescued with no injuries reported. Ongoing dam releases were resulting in strong currents in the river at the time. Event timing is based on downstream Granite Reef Dam releases.", "ts_dict_index": [4332, 4333, 4334]}
+{"event_id": 1065827, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-16 14:30:00", "end_date_time": "2023-01-16 16:30:00", "narrative": "The strong storm that brought widespread precipitation and additional flooding to the area on January 14 was followed by another storm which moved through the area between the afternoon of January 15 and the afternoon of January 16. While precipitation amounts from this storm were significantly less across most of the area than with the previous two storms which impacted the area over the previous week, this system produced a period of damaging wind gusts in the San Joaquin Valley during the morning of January 16 as the cold front from this system pushed through the area. There were several reports of wind gusts exceeding 40 mph in the San Joaquin Valley and Sierra foothills and wind gusts exceeding 60 mph in the Tehachapi Mountains and the West Side Hills. The strong winds resulted in numerous power outages as power poles and power lines were toppled as well as road closures as the winds brought trees down across roads. Some more flooding occurred in the area as a result of additional rainfall on soil which had been heavily saturated by previous recent storms. The winds did taper off by the afternoon of January 16, but the precipitation was very slow to taper off as the storm didn't completely move out of the area until January 17. California Highway Patrol reported  a tree washed up on the roadway on eastbound SR 140 east of Guadalupe Fire Rd.", "ts_dict_index": [4293, 4294, 4295]}
+{"event_id": 1088544, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. According to MCDOT, the unbridged Gila River crossing along El Mirage Road between Southern Avenue and Indian Springs Road was closed due to flooding beginning on the 14th and continued into April. Timing based on water releases from Granite Reef Dam.", "ts_dict_index": [4350, 4351, 4352]}
+{"event_id": 1090095, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. A man was swept away after attempting to walk through the flooded unbridged El Mirage Road crossing that goes through the normally dry Gila River between Southern Avenue and Indian Springs Road. The man was walking through the water while carrying his bicycle when he was swept away on the 17th. The man was successfully rescued with no injuries reported. Event timing is based on Granite Reef Dam releases.", "ts_dict_index": [4347, 4348, 4349]}
+{"event_id": 812242, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-05-10 09:28:00", "end_date_time": "2019-05-10 19:30:00", "narrative": "A cold low pressure system dropped southwestward from the northern Rocky Mountain region through the Great Basin on May 9 and into central California by the morning of May 10 which destabilized the airmass over the area and produced showers and thunderstorms across the area. This low then slowly moved southward through central California during the morning of May 10 which resulted in locally heavy rainfall over Tulare and Kern Counties. Precipitation amounts varied due to the convective nature of the precipitation. A few locations over the higher elevations in Tulare and Kern County picked up over an inch of rainfall. Most locations in the San Joaquin Valley picked up less than a quarter inch of rainfall although several stations in the Bakersfield area picked up between a quarter inch and a half inch of rain. The most noticeable impacts from the thunderstorms were several reports of roadway flooding in the Bakersfield area which led to some brief road closures, and some reports of nuisance flooding and small hail in the mountains and Kern County Deserts. Some light snow fell over the higher elevations of the Southern Sierra Nevada with several stations above 8000 feet picking up between 3 and 6 inches. California Highway Patrol reported Kimberlina Rd. was impassible between Scofield Ave. and Jumper Ave. due to flooding.", "ts_dict_index": [4368, 4369, 4370]}
+{"event_id": 1090054, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. Maricopa County Sheriff's deputies received a call around 1145 MST on the 18th of a reported drowning after an 81-year-old man fell out of his kayak and didn't resurface. The incident occurred near the Pebble Beach area along the Salt River. Other kayakers on the river pulled the man out and administered first aid but were not successful. The man was pronounced dead at the scene. Approximately 20 minutes later, a family kayaking downstream on the Salt River near the Phon D Sutton Recreation Area had to be rescued after their kayak capsized. The family managed to stay afloat by holding onto some bushes and trees. All of the family members were safely rescued via helicopter by the Maricopa County Sheriff's Office. Ongoing dam releases were resulting in strong currents in the river at the time of these incidents. Event timing is based on downstream Granite Reef Dam releases.", "ts_dict_index": [4356, 4357, 4358]}
+{"event_id": 812241, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-05-10 07:30:00", "end_date_time": "2019-05-10 10:30:00", "narrative": "A cold low pressure system dropped southwestward from the northern Rocky Mountain region through the Great Basin on May 9 and into central California by the morning of May 10 which destabilized the airmass over the area and produced showers and thunderstorms across the area. This low then slowly moved southward through central California during the morning of May 10 which resulted in locally heavy rainfall over Tulare and Kern Counties. Precipitation amounts varied due to the convective nature of the precipitation. A few locations over the higher elevations in Tulare and Kern County picked up over an inch of rainfall. Most locations in the San Joaquin Valley picked up less than a quarter inch of rainfall although several stations in the Bakersfield area picked up between a quarter inch and a half inch of rain. The most noticeable impacts from the thunderstorms were several reports of roadway flooding in the Bakersfield area which led to some brief road closures, and some reports of nuisance flooding and small hail in the mountains and Kern County Deserts. Some light snow fell over the higher elevations of the Southern Sierra Nevada with several stations above 8000 feet picking up between 3 and 6 inches. Kern County Emergency Manager reported Edison Rd. closed between Di Giorgio Rd. and Mountain View Rd. were closed due to flooding.", "ts_dict_index": [4362, 4363, 4364]}
+{"event_id": 1090023, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. Two people became stranded on top of their vehicle in the Salt River along 91st Avenue near Baseline Road after attempting to cross through the flooded roadway. The initial call for help occurred on the 17th around 1845 MST. They were safely rescued by the fire department via helicopter. No injuries were reported. Event timing is based on releases from Granite Reef Dam.", "ts_dict_index": [4335, 4336, 4337]}
+{"event_id": 1088517, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. According to the Maricopa County DOT, McKellips Road between Alma School Road and SR 202 was closed due to flooding from the Salt River beginning on the 7th and continued into April. Timing based on water releases from Granite Reef Dam.", "ts_dict_index": [4338, 4339, 4340]}
+{"event_id": 947327, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 09:00:00", "narrative": "Multiple waves of low pressure passing along a cold front approaching from near the Ohio River resulted in several rounds of prolonged and, at times, heavy rain across northern and western portions of Greenbrier County.  In the 72-hour period ending 7 am on March 1st, the northwestern half of the county had received between 2.5 to locally 4 inches of rainfall from shower and thunderstorm activity. Snow pack prior to the arrival of the rainfall was confined to the highest elevations of the western half of the county, where 2 to locally 4 inches was on the ground.  Portions of Pocahontas County to the north, where the upstream reaches of the Greenbrier River are located, had up to 9 inches of snow pack.  Nearly all remaining snow in both counties melted with this rainfall, contributing to the runoff entering the local rivers by the morning of the 1st, when widespread minor to moderate river flooding occurred.  On March 3rd, Gov. Jim Justice included Greenbrier County among eighteen total West Virginia counties in a declared State of Emergency due of the flood damage.  Heavy rain moved south during the early hours of the 1st, impacting Mercer County with more localized flooding that caused a road closure. Runoff from heavy rainfall caused Lick Hollow Creek to rise out of its banks and flood across Slab Camp Road. Portions of the road were damaged by the flooding and required repairs.", "ts_dict_index": [4380, 4381, 4382]}
+{"event_id": 812243, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-05-10 15:12:00", "end_date_time": "2019-05-10 21:30:00", "narrative": "A cold low pressure system dropped southwestward from the northern Rocky Mountain region through the Great Basin on May 9 and into central California by the morning of May 10 which destabilized the airmass over the area and produced showers and thunderstorms across the area. This low then slowly moved southward through central California during the morning of May 10 which resulted in locally heavy rainfall over Tulare and Kern Counties. Precipitation amounts varied due to the convective nature of the precipitation. A few locations over the higher elevations in Tulare and Kern County picked up over an inch of rainfall. Most locations in the San Joaquin Valley picked up less than a quarter inch of rainfall although several stations in the Bakersfield area picked up between a quarter inch and a half inch of rain. The most noticeable impacts from the thunderstorms were several reports of roadway flooding in the Bakersfield area which led to some brief road closures, and some reports of nuisance flooding and small hail in the mountains and Kern County Deserts. Some light snow fell over the higher elevations of the Southern Sierra Nevada with several stations above 8000 feet picking up between 3 and 6 inches. California Highway Patrol reported flooding due to heavy rain along Red Rock-Randsburg Rd. between State Route 14 and US 395. The road was closed due to flooding.", "ts_dict_index": [4371, 4372, 4373]}
+{"event_id": 812240, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-05-10 07:30:00", "end_date_time": "2019-05-10 10:30:00", "narrative": "A cold low pressure system dropped southwestward from the northern Rocky Mountain region through the Great Basin on May 9 and into central California by the morning of May 10 which destabilized the airmass over the area and produced showers and thunderstorms across the area. This low then slowly moved southward through central California during the morning of May 10 which resulted in locally heavy rainfall over Tulare and Kern Counties. Precipitation amounts varied due to the convective nature of the precipitation. A few locations over the higher elevations in Tulare and Kern County picked up over an inch of rainfall. Most locations in the San Joaquin Valley picked up less than a quarter inch of rainfall although several stations in the Bakersfield area picked up between a quarter inch and a half inch of rain. The most noticeable impacts from the thunderstorms were several reports of roadway flooding in the Bakersfield area which led to some brief road closures, and some reports of nuisance flooding and small hail in the mountains and Kern County Deserts. Some light snow fell over the higher elevations of the Southern Sierra Nevada with several stations above 8000 feet picking up between 3 and 6 inches. Kern County Emergency Manager reported Copus Rd. between Old River Rd. and Interstate 5 were closed due to flooding.", "ts_dict_index": [4377, 4378, 4379]}
+{"event_id": 1088530, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. According to MCDOT, the unbridged Salt River crossing along 67th Avenue between Broadway Road and Southern Avenue was closed due to flooding beginning on the 12th and continued into April. Timing based on water releases from Granite Reef Dam.", "ts_dict_index": [4344, 4345, 4346]}
+{"event_id": 812239, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-05-10 07:14:00", "end_date_time": "2019-05-10 10:14:00", "narrative": "A cold low pressure system dropped southwestward from the northern Rocky Mountain region through the Great Basin on May 9 and into central California by the morning of May 10 which destabilized the airmass over the area and produced showers and thunderstorms across the area. This low then slowly moved southward through central California during the morning of May 10 which resulted in locally heavy rainfall over Tulare and Kern Counties. Precipitation amounts varied due to the convective nature of the precipitation. A few locations over the higher elevations in Tulare and Kern County picked up over an inch of rainfall. Most locations in the San Joaquin Valley picked up less than a quarter inch of rainfall although several stations in the Bakersfield area picked up between a quarter inch and a half inch of rain. The most noticeable impacts from the thunderstorms were several reports of roadway flooding in the Bakersfield area which led to some brief road closures, and some reports of nuisance flooding and small hail in the mountains and Kern County Deserts. Some light snow fell over the higher elevations of the Southern Sierra Nevada with several stations above 8000 feet picking up between 3 and 6 inches. California Highway Patrol reported  traffic was not able to get through the intersection of Southgate Dr. and South Chester Ave. in Bakersfield due to roadway flooding.", "ts_dict_index": [4365, 4366, 4367]}
+{"event_id": 812237, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-05-09 22:25:00", "end_date_time": "2019-05-10 00:30:00", "narrative": "A cold low pressure system dropped southwestward from the northern Rocky Mountain region through the Great Basin on May 9 and into central California by the morning of May 10 which destabilized the airmass over the area and produced showers and thunderstorms across the area. This low then slowly moved southward through central California during the morning of May 10 which resulted in locally heavy rainfall over Tulare and Kern Counties. Precipitation amounts varied due to the convective nature of the precipitation. A few locations over the higher elevations in Tulare and Kern County picked up over an inch of rainfall. Most locations in the San Joaquin Valley picked up less than a quarter inch of rainfall although several stations in the Bakersfield area picked up between a quarter inch and a half inch of rain. The most noticeable impacts from the thunderstorms were several reports of roadway flooding in the Bakersfield area which led to some brief road closures, and some reports of nuisance flooding and small hail in the mountains and Kern County Deserts. Some light snow fell over the higher elevations of the Southern Sierra Nevada with several stations above 8000 feet picking up between 3 and 6 inches. California Highway Patrol reported roadway flooding along State Route 58 at Edison Rd.", "ts_dict_index": [4359, 4360, 4361]}
+{"event_id": 812238, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-05-10 03:30:00", "end_date_time": "2019-05-10 10:30:00", "narrative": "A cold low pressure system dropped southwestward from the northern Rocky Mountain region through the Great Basin on May 9 and into central California by the morning of May 10 which destabilized the airmass over the area and produced showers and thunderstorms across the area. This low then slowly moved southward through central California during the morning of May 10 which resulted in locally heavy rainfall over Tulare and Kern Counties. Precipitation amounts varied due to the convective nature of the precipitation. A few locations over the higher elevations in Tulare and Kern County picked up over an inch of rainfall. Most locations in the San Joaquin Valley picked up less than a quarter inch of rainfall although several stations in the Bakersfield area picked up between a quarter inch and a half inch of rain. The most noticeable impacts from the thunderstorms were several reports of roadway flooding in the Bakersfield area which led to some brief road closures, and some reports of nuisance flooding and small hail in the mountains and Kern County Deserts. Some light snow fell over the higher elevations of the Southern Sierra Nevada with several stations above 8000 feet picking up between 3 and 6 inches. Kern County Emergency Manager reported Malaga Rd. closed between Di Giorgio Rd. and Mountain View Rd. were closed due to flooding.", "ts_dict_index": [4374, 4375, 4376]}
+{"event_id": 1090522, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. Two people were rescued after driving around road closure barricades and attempting to drive through a flooded roadway with a recreational vehicle. While attempting to cross the flooded roadway, the recreational vehicle was swept off the road. The incident occurred around 2100 MST on the 30th at the unbridged El Mirage Road crossing that goes through the normally dry Gila River between Southern Avenue and Indian Springs Road. The two people were safely rescued by the fire department via helicopter. No injuries were reported. Event timing is based on Granite Reef Dam releases.", "ts_dict_index": [4326, 4327, 4328]}
+{"event_id": 1062280, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 12:23:00", "end_date_time": "2022-12-31 15:23:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported roadway flooding at the intersection of Triangle Rd. and Carter Rd.", "ts_dict_index": [4404, 4405, 4406]}
+{"event_id": 1062459, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-01 10:16:00", "end_date_time": "2023-01-01 13:16:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported roadway flooding on Buchanan Hallow Rd. south of LeGrand.", "ts_dict_index": [4401, 4402, 4403]}
+{"event_id": 1062379, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2022-12-31 19:50:00", "end_date_time": "2022-12-31 22:50:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a 5 foot boulder on SR 152 east of Pacheco Pass.", "ts_dict_index": [4413, 4414, 4415]}
+{"event_id": 947322, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2021-03-01 09:15:00", "end_date_time": "2021-03-02 05:05:00", "narrative": "Multiple waves of low pressure passing along a cold front approaching from near the Ohio River resulted in several rounds of prolonged and, at times, heavy rain across northern and western portions of Greenbrier County.  In the 72-hour period ending 7 am on March 1st, the northwestern half of the county had received between 2.5 to locally 4 inches of rainfall from shower and thunderstorm activity. Snow pack prior to the arrival of the rainfall was confined to the highest elevations of the western half of the county, where 2 to locally 4 inches was on the ground.  Portions of Pocahontas County to the north, where the upstream reaches of the Greenbrier River are located, had up to 9 inches of snow pack.  Nearly all remaining snow in both counties melted with this rainfall, contributing to the runoff entering the local rivers by the morning of the 1st, when widespread minor to moderate river flooding occurred.  On March 3rd, Gov. Jim Justice included Greenbrier County among eighteen total West Virginia counties in a declared State of Emergency due of the flood damage.  Heavy rain moved south during the early hours of the 1st, impacting Mercer County with more localized flooding that caused a road closure. The Greenbrier River at Alderson (ALDV2) crested at the moderate flood stage of 17.53 feet (52,600 cfs) at 8:15 pm EST on March 1st.  This crest ranked between a 5- and 10-year average return interval per USGS StreamStats, and is the 11th highest crest for this gauge since 1960. Flooding within this stretch of the Greenbrier River caused Highway 3/12 to be covered by several feet of water and impassible at multiple locations downstream from the gauge between Alderson and Talcott.  It did not appear much flooding occurred within the town of Alderson itself and no buildings were reported to be impacted.  All damage was confined to the professional removal of fallen trees blocking stream channels within the area and other related repairs.", "ts_dict_index": [4386, 4387, 4388]}
+{"event_id": 947326, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 07:00:00", "narrative": "Multiple waves of low pressure passing along a cold front approaching from near the Ohio River resulted in several rounds of prolonged and, at times, heavy rain across northern and western portions of Greenbrier County.  In the 72-hour period ending 7 am on March 1st, the northwestern half of the county had received between 2.5 to locally 4 inches of rainfall from shower and thunderstorm activity. Snow pack prior to the arrival of the rainfall was confined to the highest elevations of the western half of the county, where 2 to locally 4 inches was on the ground.  Portions of Pocahontas County to the north, where the upstream reaches of the Greenbrier River are located, had up to 9 inches of snow pack.  Nearly all remaining snow in both counties melted with this rainfall, contributing to the runoff entering the local rivers by the morning of the 1st, when widespread minor to moderate river flooding occurred.  On March 3rd, Gov. Jim Justice included Greenbrier County among eighteen total West Virginia counties in a declared State of Emergency due of the flood damage.  Heavy rain moved south during the early hours of the 1st, impacting Mercer County with more localized flooding that caused a road closure. Otter Creek was observed rising out of its banks after several hours of prolonged rainfall, resulting in flooding across Miller Road.  The road reopened once the flood waters receded, with no reports of damage.", "ts_dict_index": [4389, 4390, 4391]}
+{"event_id": 947321, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2021-03-01 07:23:00", "end_date_time": "2021-03-02 01:40:00", "narrative": "Multiple waves of low pressure passing along a cold front approaching from near the Ohio River resulted in several rounds of prolonged and, at times, heavy rain across northern and western portions of Greenbrier County.  In the 72-hour period ending 7 am on March 1st, the northwestern half of the county had received between 2.5 to locally 4 inches of rainfall from shower and thunderstorm activity. Snow pack prior to the arrival of the rainfall was confined to the highest elevations of the western half of the county, where 2 to locally 4 inches was on the ground.  Portions of Pocahontas County to the north, where the upstream reaches of the Greenbrier River are located, had up to 9 inches of snow pack.  Nearly all remaining snow in both counties melted with this rainfall, contributing to the runoff entering the local rivers by the morning of the 1st, when widespread minor to moderate river flooding occurred.  On March 3rd, Gov. Jim Justice included Greenbrier County among eighteen total West Virginia counties in a declared State of Emergency due of the flood damage.  Heavy rain moved south during the early hours of the 1st, impacting Mercer County with more localized flooding that caused a road closure. The Greenbrier River at Ronceverte (RONW2) crested at a stage of 18.43 feet at 5:05 pm EST, resulting in extensive flooding of Island Park in the community of Ronceverte.  The floor of the concession stand at the park was destroyed. Repairs were also necessary to a railing at the community amphitheater, and several loads of gravel and dirt were needed to fill a hole next to the amphitheater formed by the flooding.  Flood waters over the park rose to within inches of entering the lowest level of homes along Monroe Avenue upstream of the gauge (would be around 19.0 ft), though there were no reports of water entering any homes.  Water covered the roads and entered the yards of homes downstream of the park on both Monroe Avenue (right bank) and River Road (left bank), but no damage was reported in these locations either.  There is no defined level for moderate flood stage at this gauge, so somewhere between 19.0 feet and 21.0 would seem appropriate.  There is no rating curve developed for this gauge at this time, and no defined ARI for flooding of this magnitude.", "ts_dict_index": [4395, 4396, 4397]}
+{"event_id": 947325, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2021-03-01 08:40:00", "end_date_time": "2021-03-01 18:35:00", "narrative": "Multiple waves of low pressure passing along a cold front approaching from near the Ohio River resulted in several rounds of prolonged and, at times, heavy rain across northern and western portions of Greenbrier County.  In the 72-hour period ending 7 am on March 1st, the northwestern half of the county had received between 2.5 to locally 4 inches of rainfall from shower and thunderstorm activity. Snow pack prior to the arrival of the rainfall was confined to the highest elevations of the western half of the county, where 2 to locally 4 inches was on the ground.  Portions of Pocahontas County to the north, where the upstream reaches of the Greenbrier River are located, had up to 9 inches of snow pack.  Nearly all remaining snow in both counties melted with this rainfall, contributing to the runoff entering the local rivers by the morning of the 1st, when widespread minor to moderate river flooding occurred.  On March 3rd, Gov. Jim Justice included Greenbrier County among eighteen total West Virginia counties in a declared State of Emergency due of the flood damage.  Heavy rain moved south during the early hours of the 1st, impacting Mercer County with more localized flooding that caused a road closure. Sewell Creek above Little Sewell Creek at Rainelle (RANW2) crested at the moderate flood stage of 14.58 feet at 12:15 pm EST on March 1st. The mayor of Rainelle reported that there was little damage caused by the flooding, with some side streets off of Horton Avenue and adjacent properties covered with water.  Kanawha Avenue was also closed due to flooding for a short time.  The Rainelle City Park was covered with several inches of water from Sewell Creek.  The mayor reported that there was little damage and that any city expenses would be related to cleanup of debris.  No evacuations were necessary.  The gauge was installed during September 2019, so has a short operational history.", "ts_dict_index": [4383, 4384, 4385]}
+{"event_id": 947324, "event_type": "Flood", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2021-03-01 03:55:00", "end_date_time": "2021-03-02 15:00:00", "narrative": "Multiple waves of low pressure passing along a cold front approaching from near the Ohio River resulted in several rounds of prolonged and, at times, heavy rain across northern and western portions of Greenbrier County.  In the 72-hour period ending 7 am on March 1st, the northwestern half of the county had received between 2.5 to locally 4 inches of rainfall from shower and thunderstorm activity. Snow pack prior to the arrival of the rainfall was confined to the highest elevations of the western half of the county, where 2 to locally 4 inches was on the ground.  Portions of Pocahontas County to the north, where the upstream reaches of the Greenbrier River are located, had up to 9 inches of snow pack.  Nearly all remaining snow in both counties melted with this rainfall, contributing to the runoff entering the local rivers by the morning of the 1st, when widespread minor to moderate river flooding occurred.  On March 3rd, Gov. Jim Justice included Greenbrier County among eighteen total West Virginia counties in a declared State of Emergency due of the flood damage.  Heavy rain moved south during the early hours of the 1st, impacting Mercer County with more localized flooding that caused a road closure. The Meadow River near Hines (HNEW2) crested at the moderate flood stage of 16.69 feet (52,600 cfs) at 3:25 pm EST on March 1st.  Highway 60 was flooded by multiple feet of water and impassible in several spots between the communities of Rupert and Rainelle, leaving mud and debris which required cleaning reopen the road.  Multiple homes along the river between these points were observed surrounded by flood waters, but it is unknown to what degree, if any, that water entered the homes.  This gauge does not currently have a rating curve.", "ts_dict_index": [4392, 4393, 4394]}
+{"event_id": 1062321, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-12-31 18:32:00", "end_date_time": "2022-12-31 21:32:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported roadway flooding on northbound SR 99 at the SR 119 exchange.", "ts_dict_index": [4407, 4408, 4409]}
+{"event_id": 1062395, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 21:11:00", "end_date_time": "2022-12-31 23:59:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a boulder on the westbound lane of SR 140 west of the intersection of Old Hwy.", "ts_dict_index": [4416, 4417, 4418]}
+{"event_id": 1062433, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-01 00:09:00", "end_date_time": "2023-01-01 03:09:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported closing the mouth of Kern Canyon with two sections of large boulders blocking the eastbound lanes of SR 178 near NM 17 and NM 21.", "ts_dict_index": [4419, 4420, 4421]}
+{"event_id": 1090021, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. According to MCDOT, the unbridged Salt River crossing along Gilbert Road between Thomas Road and SR 87 was closed due to flooding beginning on the 14th and continued into April. Timing based on water releases from Granite Reef Dam.", "ts_dict_index": [4341, 4342, 4343]}
+{"event_id": 1062282, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 12:33:00", "end_date_time": "2022-12-31 15:33:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a large tree stump washed onto SR 41 north of Fish Camp.", "ts_dict_index": [4425, 4426, 4427]}
+{"event_id": 1062448, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-01 03:17:00", "end_date_time": "2023-01-01 06:17:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported rocks washed up on the road at the intersection of SR 198 and SR 216 in Lemoncove.", "ts_dict_index": [4422, 4423, 4424]}
+{"event_id": 1062457, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-01 05:12:00", "end_date_time": "2023-01-01 08:12:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a tree blocking the roadway on Rd. 426 near Rd. 222. at Bass Lake.", "ts_dict_index": [4434, 4435, 4436]}
+{"event_id": 1062414, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 22:24:00", "end_date_time": "2022-12-31 23:59:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported trees blocking both lanes of SR 49 near the intersection with Harris Rd.", "ts_dict_index": [4437, 4438, 4439]}
+{"event_id": 1090574, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-04 04:00:00", "end_date_time": "2023-03-31 23:59:00", "narrative": "Anomalous snowfall across the high terrain of Arizona as well as lower elevation rainfall led to greater than normal runoff into the Salt and Verde watersheds. As a result of this, dam releases were conducted at multiple locations in these watersheds, leading to heightened flows in these rivers. Upstream releases led to additional releases from Granite Reef Dam, which initially began to cause impacts on the 4th when releases from the dam increased above 1,000 cfs. Granite Reef Dam releases continued to increase going through the month of March and at one point during the month was releasing nearly 40,000 cfs. Releases from this dam led to downstream flow in the normally dry Salt River, which runs through the Phoenix metro. The anomalous runoff into the Salt and Verde watersheds and the resultant dam releases led to numerous impacts along the Salt, Verde, and Gila Rivers, including multiple unbridged river crossings being flooded, multiple water rescues, and one recreational fatality. Flow in the Salt River continued downstream into the Gila River, causing more impacts along the way down to Painted Rock Dam. Releases continued through the remainder of the month and into April, resulting in prolonged impacts. Lake levels at Bartlett Lake quickly rose during the overnight hours Thursday night into Friday morning on the 16th-17th. Levels reportedly rose 10 feet during the overnight hours, leaving at least two camp trailers submerged in several feet of water. No injuries were reported.", "ts_dict_index": [4353, 4354, 4355]}
+{"event_id": 1062375, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2022-12-31 19:13:00", "end_date_time": "2022-12-31 22:13:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported roadway flooding  at the intersection of SR 165 and Mervel Ave.", "ts_dict_index": [4440, 4441, 4442]}
+{"event_id": 1062281, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2022-12-31 12:25:00", "end_date_time": "2022-12-31 15:25:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported flooding on SR 152 at the Merced College entrance west of Los Banos.", "ts_dict_index": [4455, 4456, 4457]}
+{"event_id": 1062460, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-01 10:40:00", "end_date_time": "2023-01-01 13:40:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported water from a canal flooding onto the roadway south of Merced.", "ts_dict_index": [4446, 4447, 4448]}
+{"event_id": 1062279, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 06:41:00", "end_date_time": "2022-12-31 09:41:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a boulder in the road on the westbound lane of Old Toll Rd. near Corbett Creek.", "ts_dict_index": [4458, 4459, 4460]}
+{"event_id": 1062413, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2022-12-31 22:18:00", "end_date_time": "2022-12-31 23:59:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a large rock washed up on the roadway just west of the intersection of SR 190 and Rd. 320.", "ts_dict_index": [4461, 4462, 4463]}
+{"event_id": 1062412, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-12-31 22:00:00", "end_date_time": "2022-12-31 23:59:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a rockslide at  the intersection of SR 178 and Democrat Rd.", "ts_dict_index": [4467, 4468, 4469]}
+{"event_id": 1062411, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2022-12-31 21:54:00", "end_date_time": "2022-12-31 23:59:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported the roadway washed out at the intersection of SR 41 and Ave. 15. east of Madera Ranchos.", "ts_dict_index": [4449, 4450, 4451]}
+{"event_id": 1062296, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2022-12-31 15:28:00", "end_date_time": "2022-12-31 18:28:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported the southbound lane of North Fork Rd. flooded at Fine Gold Creek.", "ts_dict_index": [4473, 4474, 4475]}
+{"event_id": 1062377, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 19:41:00", "end_date_time": "2022-12-31 22:41:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported mud, dirty and rocks on the roadway on SR 140 at Briceburg.", "ts_dict_index": [4485, 4486, 4487]}
+{"event_id": 1062278, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 04:30:00", "end_date_time": "2022-12-31 07:30:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported mud, dirt and rock on the roadway on SR 140 at Briceburg at the Octagon.", "ts_dict_index": [4470, 4471, 4472]}
+{"event_id": 1062288, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 13:55:00", "end_date_time": "2022-12-31 16:55:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported a tree that was washed away landed on the bridge neat the intersection of SR 140 and Oak Rd. blocking all lanes.", "ts_dict_index": [4494, 4495, 4496]}
+{"event_id": 1062277, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2022-12-31 01:12:00", "end_date_time": "2022-12-31 04:12:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported rocks blocking the road at road 274 near Marina View Dr.", "ts_dict_index": [4479, 4480, 4481]}
+{"event_id": 1062458, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-01 05:12:00", "end_date_time": "2023-01-01 08:12:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported roadway flooding at the intersection of SR 59 and McNamara Rd.", "ts_dict_index": [4497, 4498, 4499]}
+{"event_id": 1065750, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-14 10:42:00", "end_date_time": "2023-01-14 12:42:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported on Ave. 396 near the intersection with Rd 16. in Kingsburg.", "ts_dict_index": [4530, 4531, 4532]}
+{"event_id": 1062293, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2022-12-31 14:42:00", "end_date_time": "2022-12-31 17:42:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported roadway flooding at the intersection of Triangle Rd. and Meadow Ln.", "ts_dict_index": [4488, 4489, 4490]}
+{"event_id": 1065753, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-14 12:38:00", "end_date_time": "2023-01-14 14:38:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported roadway flooding on Healy Rd. at McMaster Rd.", "ts_dict_index": [4524, 4525, 4526]}
+{"event_id": 1065761, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-01-14 20:21:00", "end_date_time": "2023-01-14 22:21:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported the closure of Snelling Rd. north of La Paloma Rd. due to flooding.", "ts_dict_index": [4515, 4516, 4517]}
+{"event_id": 1065752, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-14 10:43:00", "end_date_time": "2023-01-14 12:43:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported Globe Dr. over the Tulare River Bridge in Springville was closed due to flooding.", "ts_dict_index": [4539, 4540, 4541]}
+{"event_id": 861994, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-12-22 18:00:00", "end_date_time": "2019-12-22 20:00:00", "narrative": "A frontal system slowly moved east across central California on December 22 and 23. Strong winds ahead of the system impacted the Fort Tejon area as well as the west side hills of the San Joaquin Valley and the Bakersfield area where there were a few reports of minor wind damage. Widespread gusts of 50 mph or higher were reported in the foothill and mountain areas with a couple of stations near Lebec reporting gusts exceeding 75 mph. After the winds diminished during the afternoon of December 22, widespread precipitation spread across the area with several reports of 1 to 1.5 inches of liquid precipitation in the Sierra Nevada and adjacent foothills. Rain shadowing generally kept precipitation totals down in the San Joaquin Valley where most locations picked up between a quarter and half and inch of rainfall. A swath of moderate to locally heavy rainfall was observed in central Tulare County during the evening of December 22 as the main low pressure center tracked north through the area and impacted Porterville, Lindsay and Exeter. The precipitation mainly fell as snow above 5000 feet and several stations in the higher Sierra picked up between 10 and 15 inches of new snowfall. Fresno Police reported roadway flooding at the intersection of Jansen Ave. and Willow Ave. in Fresno.", "ts_dict_index": [4506, 4507, 4508]}
+{"event_id": 1000119, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-12-13 13:07:00", "end_date_time": "2021-12-13 14:07:00", "narrative": "A low pressure system descended from the Gulf of Alaska southward along the entire Pacific Coast and tapped into sub-tropical moisture originating from the Central Pacific to drop heavy rain throughout the state. A stalled frontal boundary over the Santa Cruz Mountains along with strong southerly winds from a coastal low-level jet, enhanced orographic rainfall over this region, leading to rainfall totals over a 2 day period (Dec 12th-13th) of up to ten inches in the coastal mountains. The stalled boundary was reinvigorated by a secondary boundary bringing in a cold unstable airmass that set off convective showers and lowered snow levels below 2000 ft. A wind advisory, later upgraded to a high wind warning was issued for the southern half of the region from the SF Peninsula down to the Big Sur Coast including the inland zones due to the coastal jet bringing sustained winds up to 40 mph with gusts up to 55 mph. A high surf advisory was issued for the entire coast due to the arrival of a strong NW swell train, along with Gale Warning throughout the coastal waters. A flash flood watch was issued for the Santa Lucia Mountains and Dolan Burn Scar area, where up to 12 inches of rain fell. Rocks slid onto SR1 and blocked the northbound lane near Bixby Bridge. https://kion546.com/news/2021/12/14/a-look-at-the-damage-from-the-rain-storm/.", "ts_dict_index": [4503, 4504, 4505]}
+{"event_id": 1065763, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-15 02:28:00", "end_date_time": "2023-01-15 04:28:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported roadway flooding along SR 14 near Redrock-Randsburg Rd.", "ts_dict_index": [4533, 4534, 4535]}
+{"event_id": 1062374, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-12-31 19:09:00", "end_date_time": "2022-12-31 22:09:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported flooding in all lanes of SR 99 at the intersection of White Ln.", "ts_dict_index": [4482, 4483, 4484]}
+{"event_id": 861995, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-12-23 11:30:00", "end_date_time": "2019-12-23 13:00:00", "narrative": "A frontal system slowly moved east across central California on December 22 and 23. Strong winds ahead of the system impacted the Fort Tejon area as well as the west side hills of the San Joaquin Valley and the Bakersfield area where there were a few reports of minor wind damage. Widespread gusts of 50 mph or higher were reported in the foothill and mountain areas with a couple of stations near Lebec reporting gusts exceeding 75 mph. After the winds diminished during the afternoon of December 22, widespread precipitation spread across the area with several reports of 1 to 1.5 inches of liquid precipitation in the Sierra Nevada and adjacent foothills. Rain shadowing generally kept precipitation totals down in the San Joaquin Valley where most locations picked up between a quarter and half and inch of rainfall. A swath of moderate to locally heavy rainfall was observed in central Tulare County during the evening of December 22 as the main low pressure center tracked north through the area and impacted Porterville, Lindsay and Exeter. The precipitation mainly fell as snow above 5000 feet and several stations in the higher Sierra picked up between 10 and 15 inches of new snowfall. Kern County Emergency Manager reported Redrock-Randsburg Road was closed due to flooding.", "ts_dict_index": [4509, 4510, 4511]}
+{"event_id": 1062326, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2022-12-31 18:35:00", "end_date_time": "2022-12-31 21:35:00", "narrative": "A large upper trough moved slowly through California on December 30 and 31. This system had a deep fetch of tropical moisture associated with it which resulted in a period of moderate to heavy precipitation along with widespread flooding across much of the area on December 31. Numerous reports of flooding and debris flows were reported by law enforcement with several roads being briefly closed as a result of flooding. The system also produced strong wind gusts across the area between the afternoon of December 30 and the morning of January 1 with several stations in the West Side Hills and Tehachapi Mountains reporting gusts exceeding 60 mph. Several stations in the Sierra Nevada below 7500 feet picked up between 4 and 7 inches of rainfall while the adjacent foothills picked up 2 to 4 inches of rainfall. Rain shadowing effects limited precipitation in the San Joaquin Valley to between half an inch and an inch of rain at most locations while many stations in the Tehachapi Mountains also picked up between half an inch and an inch of rain. Several higher elevations SNOTEL stations picked up 18 to 30 inches of new snowfall adding to the heavy snowpack which had already accumulated earlier in December. California Highway Patrol reported roadway flooding on northbound SR 99 at the White Ln. exchange.", "ts_dict_index": [4476, 4477, 4478]}
+{"event_id": 1065754, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-14 12:54:00", "end_date_time": "2023-01-14 14:54:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported a rockslide with golfball to football sized boulders near Kernville Rd. and Kern River Dr.", "ts_dict_index": [4527, 4528, 4529]}
+{"event_id": 1065751, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-14 10:43:00", "end_date_time": "2023-01-14 12:43:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported Rd. 184 was closed between Ave. 24 to Ave. 32 due to flooding.", "ts_dict_index": [4545, 4546, 4547]}
+{"event_id": 1065756, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-14 13:07:00", "end_date_time": "2023-01-14 15:07:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported flooding on Rd. 25 near Ave. 18 in Madera.", "ts_dict_index": [4551, 4552, 4553]}
+{"event_id": 1065760, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-14 15:11:00", "end_date_time": "2023-01-14 17:11:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported flooding on Seminole Ave. near Delaware Rd. caused the roadway to collapse.", "ts_dict_index": [4557, 4558, 4559]}
+{"event_id": 1065759, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-14 14:33:00", "end_date_time": "2023-01-14 16:33:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported a tree on the roadway on Rd. 200 west of Mountain View Peak Rd.", "ts_dict_index": [4554, 4555, 4556]}
+{"event_id": 1065764, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-01-15 10:43:00", "end_date_time": "2023-01-15 12:43:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported a large boulder washed up onto the roadway on SR 140 in Briceburg.", "ts_dict_index": [4560, 4561, 4562]}
+{"event_id": 1065749, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-14 10:35:00", "end_date_time": "2023-01-14 12:35:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported Rd. 236 was closed between Ave. 196 and Ave. 200 in Strathmore due to flooding.", "ts_dict_index": [4566, 4567, 4568]}
+{"event_id": 795400, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-02-02 12:43:00", "end_date_time": "2019-02-02 15:43:00", "narrative": "A strong upper low pressure system approached the central California coast during the morning of February 2. Ahead of the low, strong southerly winds impacted the Grapevine area along Interstate 5 for much of the morning. By late morning the strong winds spread northward into the Bakersfield area where there were numerous reports of downed trees and wind damage. As the main low moved inland during the day, moderate to heavy precipitation spread into area and produced several instances of roadway and nuisance flooding. Scattered thunderstorms brought additional rainfall and small hail to the San Joaquin Valley and southern Sierra foothills during the late afternoon. One thunderstorm produced a brief small tornado south of Mariposa. Several stations in the San Joaquin Valley picked up over an inch of rain while several stations in the mountains measured  between 2 and 5 inches of liquid precipitation. The precipitation fell mainly as snow above 5000 feet where heavy snowfall was reported at several stations and several feet of new snowfall was estimated at several SNOTELS from this storm and the following storm which moved through the area on February 4 and 5. California Highway Patrol reported Hogback Dr. near Sierra Glen washed out due to runoff from heavy rainfall.", "ts_dict_index": [4581, 4582, 4583]}
+{"event_id": 989095, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2021-10-26 09:30:00", "end_date_time": "2021-10-26 11:30:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Minor flooding was reported around the Town of Shandaken.", "ts_dict_index": [4584, 4585, 4586]}
+{"event_id": 795404, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-02-02 15:32:00", "end_date_time": "2019-02-02 17:32:00", "narrative": "A strong upper low pressure system approached the central California coast during the morning of February 2. Ahead of the low, strong southerly winds impacted the Grapevine area along Interstate 5 for much of the morning. By late morning the strong winds spread northward into the Bakersfield area where there were numerous reports of downed trees and wind damage. As the main low moved inland during the day, moderate to heavy precipitation spread into area and produced several instances of roadway and nuisance flooding. Scattered thunderstorms brought additional rainfall and small hail to the San Joaquin Valley and southern Sierra foothills during the late afternoon. One thunderstorm produced a brief small tornado south of Mariposa. Several stations in the San Joaquin Valley picked up over an inch of rain while several stations in the mountains measured  between 2 and 5 inches of liquid precipitation. The precipitation fell mainly as snow above 5000 feet where heavy snowfall was reported at several stations and several feet of new snowfall was estimated at several SNOTELS from this storm and the following storm which moved through the area on February 4 and 5. California Highway Patrol reported roadway flooding on the southbound lane of State Route 33 east of Coalinga.", "ts_dict_index": [4572, 4573, 4574]}
+{"event_id": 795405, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-02-02 19:17:00", "end_date_time": "2019-02-02 21:17:00", "narrative": "A strong upper low pressure system approached the central California coast during the morning of February 2. Ahead of the low, strong southerly winds impacted the Grapevine area along Interstate 5 for much of the morning. By late morning the strong winds spread northward into the Bakersfield area where there were numerous reports of downed trees and wind damage. As the main low moved inland during the day, moderate to heavy precipitation spread into area and produced several instances of roadway and nuisance flooding. Scattered thunderstorms brought additional rainfall and small hail to the San Joaquin Valley and southern Sierra foothills during the late afternoon. One thunderstorm produced a brief small tornado south of Mariposa. Several stations in the San Joaquin Valley picked up over an inch of rain while several stations in the mountains measured  between 2 and 5 inches of liquid precipitation. The precipitation fell mainly as snow above 5000 feet where heavy snowfall was reported at several stations and several feet of new snowfall was estimated at several SNOTELS from this storm and the following storm which moved through the area on February 4 and 5. California Highway Patrol reported roadway flooding on State Route 269 which resulted in the road being closed north of State Route 198 near Huron.", "ts_dict_index": [4578, 4579, 4580]}
+{"event_id": 1093106, "event_type": "Flood", "state": "TEXAS", "cz_name": "CAMERON", "begin_date_time": "2023-06-05 15:00:00", "end_date_time": "2023-06-05 16:00:00", "narrative": "A shortwave that turned into a baggy trough over eastern Texas provided Deep South Texas and the Rio Grande Valley with several rounds of showers and storms June 3rd through June 5th. Large hail fell in a storm just northwest of Rio Grande City on June 3rd before turning into a sub-severe line of showers and storms across the populated Rio Grande Valley. ||Northwesterly flow aloft on the southwestern side of the trough led to several more showers and storms across the eastern half of Deep South Texas and the Rio Grande Valley on June 4th. The storms headed south from Corpus Christi's area and moved along the coast of Kenedy and Willacy Counties before moving southwestward into Cameron County where it produced very large hail, up to 2.5 in diameter, and 80 mph wind gusts at Valley International Airport in Harlingen. Additional storms flared up in Hidalgo County and produced 1 hail. ||The storms on June 5th followed a similar script to June 4th with storms along the coast of Kenedy and Willacy Counties before developing inland. While the storms weren't as strong, they still produced large hail in northern Cameron County and 50 to 60 mph wind gusts near Brownsville. Members of the public shared videos of Mexico Blvd, just north of the intersection with Sam Perl Blvd, under the railroad tracks with an estimated 2 feet of water. One car was stranded and flooded in the video. The car and flooding was still there an hour later showing the car still stranded.", "ts_dict_index": [4569, 4570, 4571]}
+{"event_id": 795399, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-02-02 12:27:00", "end_date_time": "2019-02-02 14:27:00", "narrative": "A strong upper low pressure system approached the central California coast during the morning of February 2. Ahead of the low, strong southerly winds impacted the Grapevine area along Interstate 5 for much of the morning. By late morning the strong winds spread northward into the Bakersfield area where there were numerous reports of downed trees and wind damage. As the main low moved inland during the day, moderate to heavy precipitation spread into area and produced several instances of roadway and nuisance flooding. Scattered thunderstorms brought additional rainfall and small hail to the San Joaquin Valley and southern Sierra foothills during the late afternoon. One thunderstorm produced a brief small tornado south of Mariposa. Several stations in the San Joaquin Valley picked up over an inch of rain while several stations in the mountains measured  between 2 and 5 inches of liquid precipitation. The precipitation fell mainly as snow above 5000 feet where heavy snowfall was reported at several stations and several feet of new snowfall was estimated at several SNOTELS from this storm and the following storm which moved through the area on February 4 and 5. California Highway Patrol reported roadway flooding on Manning Ave. between the bridge and Zediker Ave. in Parlier.", "ts_dict_index": [4575, 4576, 4577]}
+{"event_id": 989096, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2021-10-26 09:30:00", "end_date_time": "2021-10-26 12:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Minor flooding was reported along Route 296 in the Town of Jewett.", "ts_dict_index": [4587, 4588, 4589]}
+{"event_id": 1065758, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-01-14 14:21:00", "end_date_time": "2023-01-14 16:21:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported standing water on westbound SR 58 near Oswell St.", "ts_dict_index": [4563, 4564, 4565]}
+{"event_id": 1065747, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2023-01-14 10:21:00", "end_date_time": "2023-01-14 12:21:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported roadway flooding on northbound SR 99 and the W. Cleveland Ave. offramp.", "ts_dict_index": [4512, 4513, 4514]}
+{"event_id": 989102, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2021-10-26 12:30:00", "end_date_time": "2021-10-27 03:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Water covered portions of Route 47 near McKenley Hollow Road near Oliverea. Later in the afternoon, the Esopus Creek was out of its banks and sent water down Route 47, surrounding a home near Brown Road. A portion of County Route 47 remained closed into the morning hours of October 27.", "ts_dict_index": [4599, 4600, 4601]}
+{"event_id": 989123, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2021-10-26 13:00:00", "end_date_time": "2021-10-27 03:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Route 213 in Rosendale was closed between Mountain Road and Creek Locks Road due to flooding.", "ts_dict_index": [4590, 4591, 4592]}
+{"event_id": 989115, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2021-10-26 15:00:00", "end_date_time": "2021-10-27 03:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Hervey Street Road was closed between Stone Bridge Road and Golden Hill Road near Cornwallville due to flooding.", "ts_dict_index": [4593, 4594, 4595]}
+{"event_id": 1065757, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-14 13:38:00", "end_date_time": "2023-01-14 15:38:00", "narrative": "Another strong low pressure system impacted central California as it moved eastward across northern California on January 14. The deeper moisture associated with this system arrived during the evening on January 13 and the precipitation continued across the area until the evening of January 14 when it finally tapered off. Strong upper jet dynamics associated with this system produced a period of widespread heavy precipitation across the area during the afternoon of January 14. Between 2 and 4 inches of liquid precipitation fell over the Sierra Nevada while 1.5 to 3 inches of rain fell over the adjacent foothills. Most of the San Joaquin Valley only picked up between a quarter of an inch and three quarters of an inch of rain due to rain shadowing effects. Several higher elevation SNOTEL stations picked up between 1.5 and 3 feet of new snowfall above 6000 feet with a few inches of snow falling as low as 4500 feet in the Sierra Nevada as cooler air pushed into the area during the evening of January 14. The main impacts from this system came from flooding which was a result of significant rainfall taking place over already saturated soil and continued runoff from previous storms. California Highway Patrol reported a tree washed up on the roadway at Rd. 140 near Ave. 192.", "ts_dict_index": [4542, 4543, 4544]}
+{"event_id": 1028555, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2022-05-05 14:43:00", "end_date_time": "2022-05-05 18:00:00", "narrative": "A stalled front from the storm a system on May 2-3 moved northward back into the Ozarks as a warm front as a strong upper level low over southern Colorado moved eastward into the southern Plains. This led to another several rounds of widespread heavy rainfall that occurred from the late morning of the 4th to the early morning of the 6th, when the surface low exited the area. Widespread accumulations of two to five inches occurred, with isolated accumulations over six inches over parts of Jasper and Dade Counties. Numerous reports of flash flooding indicated that not only were low water crossings flooding, but major highways as well. Evacuations were conducted at both Roaring River State Park in Barry County and at Bennett Spring State Park on the Dallas/Laclede County Border. Several people were stranded in cabins and RVs at Bennett Spring during the peak of the flood. There were 11 swift water rescues reported in southwest Missouri. Unfortunately, there was one fatality in Dade County when a 65-year old male drove into a flooded low water crossing and was swept downstream after exiting his vehicle and attempting to swim to shore. State Highway 59 was flooded along Elk Creek.", "ts_dict_index": [4638, 4639, 4640]}
+{"event_id": 989125, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2021-10-26 13:00:00", "end_date_time": "2021-10-27 03:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Springtown Road in New Paltz was closed from Route 299 to areas North of Dug Road for flooding in the area.", "ts_dict_index": [4602, 4603, 4604]}
+{"event_id": 989124, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2021-10-26 13:00:00", "end_date_time": "2021-10-27 03:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Samsonville Road was closed between Queens Highway and Sundown Road for a flooded roadway.", "ts_dict_index": [4605, 4606, 4607]}
+{"event_id": 1028552, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2022-05-05 10:37:00", "end_date_time": "2022-05-05 18:00:00", "narrative": "A stalled front from the storm a system on May 2-3 moved northward back into the Ozarks as a warm front as a strong upper level low over southern Colorado moved eastward into the southern Plains. This led to another several rounds of widespread heavy rainfall that occurred from the late morning of the 4th to the early morning of the 6th, when the surface low exited the area. Widespread accumulations of two to five inches occurred, with isolated accumulations over six inches over parts of Jasper and Dade Counties. Numerous reports of flash flooding indicated that not only were low water crossings flooding, but major highways as well. Evacuations were conducted at both Roaring River State Park in Barry County and at Bennett Spring State Park on the Dallas/Laclede County Border. Several people were stranded in cabins and RVs at Bennett Spring during the peak of the flood. There were 11 swift water rescues reported in southwest Missouri. Unfortunately, there was one fatality in Dade County when a 65-year old male drove into a flooded low water crossing and was swept downstream after exiting his vehicle and attempting to swim to shore. State Highway U at the Mikes Creek low water crossing was closed due to flooding.", "ts_dict_index": [4647, 4648, 4649]}
+{"event_id": 989121, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2021-10-26 13:00:00", "end_date_time": "2021-10-27 03:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Hang Glider Road was closed at the bridge due to flooding.", "ts_dict_index": [4611, 4612, 4613]}
+{"event_id": 1028554, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2022-05-05 11:38:00", "end_date_time": "2022-05-05 18:00:00", "narrative": "A stalled front from the storm a system on May 2-3 moved northward back into the Ozarks as a warm front as a strong upper level low over southern Colorado moved eastward into the southern Plains. This led to another several rounds of widespread heavy rainfall that occurred from the late morning of the 4th to the early morning of the 6th, when the surface low exited the area. Widespread accumulations of two to five inches occurred, with isolated accumulations over six inches over parts of Jasper and Dade Counties. Numerous reports of flash flooding indicated that not only were low water crossings flooding, but major highways as well. Evacuations were conducted at both Roaring River State Park in Barry County and at Bennett Spring State Park on the Dallas/Laclede County Border. Several people were stranded in cabins and RVs at Bennett Spring during the peak of the flood. There were 11 swift water rescues reported in southwest Missouri. Unfortunately, there was one fatality in Dade County when a 65-year old male drove into a flooded low water crossing and was swept downstream after exiting his vehicle and attempting to swim to shore. Highway H at the low water crossing on Elk Creek was closed due to flooding.", "ts_dict_index": [4635, 4636, 4637]}
+{"event_id": 1028558, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2022-05-05 14:44:00", "end_date_time": "2022-05-05 18:00:00", "narrative": "A stalled front from the storm a system on May 2-3 moved northward back into the Ozarks as a warm front as a strong upper level low over southern Colorado moved eastward into the southern Plains. This led to another several rounds of widespread heavy rainfall that occurred from the late morning of the 4th to the early morning of the 6th, when the surface low exited the area. Widespread accumulations of two to five inches occurred, with isolated accumulations over six inches over parts of Jasper and Dade Counties. Numerous reports of flash flooding indicated that not only were low water crossings flooding, but major highways as well. Evacuations were conducted at both Roaring River State Park in Barry County and at Bennett Spring State Park on the Dallas/Laclede County Border. Several people were stranded in cabins and RVs at Bennett Spring during the peak of the flood. There were 11 swift water rescues reported in southwest Missouri. Unfortunately, there was one fatality in Dade County when a 65-year old male drove into a flooded low water crossing and was swept downstream after exiting his vehicle and attempting to swim to shore. State Highway TT was closed due to flooding at the Elk Creek.", "ts_dict_index": [4629, 4630, 4631]}
+{"event_id": 989120, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2021-10-26 13:00:00", "end_date_time": "2021-10-27 03:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Flooding was observed along residential homes near the Hamlet of Pine Hill.", "ts_dict_index": [4614, 4615, 4616]}
+{"event_id": 989119, "event_type": "Flood", "state": "NEW YORK", "cz_name": "ULSTER", "begin_date_time": "2021-10-26 18:00:00", "end_date_time": "2021-10-27 03:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Water overflowing the Esopus Creek flooded portions of Plank Road near Mount Tremper, across from Emerson Resort and Spa.", "ts_dict_index": [4617, 4618, 4619]}
+{"event_id": 1028550, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2022-05-05 10:37:00", "end_date_time": "2022-05-05 18:00:00", "narrative": "A stalled front from the storm a system on May 2-3 moved northward back into the Ozarks as a warm front as a strong upper level low over southern Colorado moved eastward into the southern Plains. This led to another several rounds of widespread heavy rainfall that occurred from the late morning of the 4th to the early morning of the 6th, when the surface low exited the area. Widespread accumulations of two to five inches occurred, with isolated accumulations over six inches over parts of Jasper and Dade Counties. Numerous reports of flash flooding indicated that not only were low water crossings flooding, but major highways as well. Evacuations were conducted at both Roaring River State Park in Barry County and at Bennett Spring State Park on the Dallas/Laclede County Border. Several people were stranded in cabins and RVs at Bennett Spring during the peak of the flood. There were 11 swift water rescues reported in southwest Missouri. Unfortunately, there was one fatality in Dade County when a 65-year old male drove into a flooded low water crossing and was swept downstream after exiting his vehicle and attempting to swim to shore. State Highway KK at the Big Sugar Creek low water crossing was closed due to flooding.", "ts_dict_index": [4623, 4624, 4625]}
+{"event_id": 989117, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2021-10-26 20:00:00", "end_date_time": "2021-10-27 03:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Catskill Creek went over its banks causing minor flooding along West Main Street in the Village of Catskill.", "ts_dict_index": [4620, 4621, 4622]}
+{"event_id": 1028556, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2022-05-05 12:22:00", "end_date_time": "2022-05-05 18:00:00", "narrative": "A stalled front from the storm a system on May 2-3 moved northward back into the Ozarks as a warm front as a strong upper level low over southern Colorado moved eastward into the southern Plains. This led to another several rounds of widespread heavy rainfall that occurred from the late morning of the 4th to the early morning of the 6th, when the surface low exited the area. Widespread accumulations of two to five inches occurred, with isolated accumulations over six inches over parts of Jasper and Dade Counties. Numerous reports of flash flooding indicated that not only were low water crossings flooding, but major highways as well. Evacuations were conducted at both Roaring River State Park in Barry County and at Bennett Spring State Park on the Dallas/Laclede County Border. Several people were stranded in cabins and RVs at Bennett Spring during the peak of the flood. There were 11 swift water rescues reported in southwest Missouri. Unfortunately, there was one fatality in Dade County when a 65-year old male drove into a flooded low water crossing and was swept downstream after exiting his vehicle and attempting to swim to shore. State Highway DD was closed due to flooding at Elk Creek.", "ts_dict_index": [4641, 4642, 4643]}
+{"event_id": 1028553, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2022-05-05 10:37:00", "end_date_time": "2022-05-05 18:00:00", "narrative": "A stalled front from the storm a system on May 2-3 moved northward back into the Ozarks as a warm front as a strong upper level low over southern Colorado moved eastward into the southern Plains. This led to another several rounds of widespread heavy rainfall that occurred from the late morning of the 4th to the early morning of the 6th, when the surface low exited the area. Widespread accumulations of two to five inches occurred, with isolated accumulations over six inches over parts of Jasper and Dade Counties. Numerous reports of flash flooding indicated that not only were low water crossings flooding, but major highways as well. Evacuations were conducted at both Roaring River State Park in Barry County and at Bennett Spring State Park on the Dallas/Laclede County Border. Several people were stranded in cabins and RVs at Bennett Spring during the peak of the flood. There were 11 swift water rescues reported in southwest Missouri. Unfortunately, there was one fatality in Dade County when a 65-year old male drove into a flooded low water crossing and was swept downstream after exiting his vehicle and attempting to swim to shore. State Highway CC at the low water crossing on Indian Creek was closed due to flooding.", "ts_dict_index": [4632, 4633, 4634]}
+{"event_id": 989113, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2021-10-26 15:00:00", "end_date_time": "2021-10-27 03:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Stone Bridge Road was closed between Brown Road and Shady Glen Road near East Durham due to flooding.", "ts_dict_index": [4608, 4609, 4610]}
+{"event_id": 1028551, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2022-05-05 10:37:00", "end_date_time": "2022-05-05 18:00:00", "narrative": "A stalled front from the storm a system on May 2-3 moved northward back into the Ozarks as a warm front as a strong upper level low over southern Colorado moved eastward into the southern Plains. This led to another several rounds of widespread heavy rainfall that occurred from the late morning of the 4th to the early morning of the 6th, when the surface low exited the area. Widespread accumulations of two to five inches occurred, with isolated accumulations over six inches over parts of Jasper and Dade Counties. Numerous reports of flash flooding indicated that not only were low water crossings flooding, but major highways as well. Evacuations were conducted at both Roaring River State Park in Barry County and at Bennett Spring State Park on the Dallas/Laclede County Border. Several people were stranded in cabins and RVs at Bennett Spring during the peak of the flood. There were 11 swift water rescues reported in southwest Missouri. Unfortunately, there was one fatality in Dade County when a 65-year old male drove into a flooded low water crossing and was swept downstream after exiting his vehicle and attempting to swim to shore. State Highway E was closed due to flooding at Big Sugar Creek and Mikes Creek.", "ts_dict_index": [4644, 4645, 4646]}
+{"event_id": 989097, "event_type": "Flood", "state": "NEW YORK", "cz_name": "GREENE", "begin_date_time": "2021-10-26 09:30:00", "end_date_time": "2021-10-26 12:00:00", "narrative": "A coastal storm brought a prolonged period of moderate rainfall across portions of eastern New York, mainly on Tuesday, October 26, 2021. While the rain was not falling particularly heavily, persistent rainfall rates of 0.25 to 0.50 of an inch an hour occurred for several hours across portions of Ulster, Greene, Schoharie and Schenectady counties. This resulted in rainfall amounts of 2 to 5 inches across the region. Minor flooding began as early as the late morning hours on October 26, but the greatest coverage of flooding occurred during the afternoon and evening hours as roads began to close. Rivers, creeks and streams also began overflowing their banks leading to additional flooding. Rain ended during the overnight hours, slowly allowing waters to recede. However, roads damaged by the flooding remained closed into the daytime hours of October 27.||Gusty winds between 30 and 40 mph also accompanied the storm which resulted in a few downed trees and some power outages.||New York Governor Kathy Hochul declared a State of Emergency for selected counties across New York State including Greene, Montgomery, Schenectady, Schoharie and Ulster. Minor flooding was reported along Route 145 in the Town of Durham.", "ts_dict_index": [4596, 4597, 4598]}
+{"event_id": 1060467, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2022-12-10 20:21:00", "end_date_time": "2022-12-10 22:21:00", "narrative": "A strong low pressure system slowly moved across central California on December 10 and 11 providing the area with moderate to heavy precipitation. The precipitation fell as snow above 5000 feet with several SNOTEL stations picking up between 18 and 30 inches of estimated new snowfall. The snow level lowered to near 3000 feet by the afternoon of December 11 with some stations in the Sierra Nevada and higher foothills picking up between 3 and 6 inches of new snowfall. Many stations in the Sierra Nevada received between 3 and 5 inches of liquid precipitation while the adjacent foothills picked up between 1.5 and 3 inches of rainfall and much of the San Joaquin Valley and Tehachapi Mountains received between half an inch and an inch of rainfall. The precipitation did change over the snow in the Tehachapi Mountains above 4000 feet, but snowfall amounts were generally light. Rain shadowing effects limited precipitation across the Kern County Deserts with most stations receiving between a tenth of an inch and a quarter inch of rainfall. The precipitation tapered off during the evening of December 11 and ended by midday on December 12. California Highway Patrol reported roadway flooding at the intersection of N. Fox and W. Cardella in Atwater.", "ts_dict_index": [4671, 4672, 4673]}
+{"event_id": 1060471, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2022-12-10 21:24:00", "end_date_time": "2022-12-10 23:24:00", "narrative": "A strong low pressure system slowly moved across central California on December 10 and 11 providing the area with moderate to heavy precipitation. The precipitation fell as snow above 5000 feet with several SNOTEL stations picking up between 18 and 30 inches of estimated new snowfall. The snow level lowered to near 3000 feet by the afternoon of December 11 with some stations in the Sierra Nevada and higher foothills picking up between 3 and 6 inches of new snowfall. Many stations in the Sierra Nevada received between 3 and 5 inches of liquid precipitation while the adjacent foothills picked up between 1.5 and 3 inches of rainfall and much of the San Joaquin Valley and Tehachapi Mountains received between half an inch and an inch of rainfall. The precipitation did change over the snow in the Tehachapi Mountains above 4000 feet, but snowfall amounts were generally light. Rain shadowing effects limited precipitation across the Kern County Deserts with most stations receiving between a tenth of an inch and a quarter inch of rainfall. The precipitation tapered off during the evening of December 11 and ended by midday on December 12. California Highway Patrol reported roadway flooding near the intersection of Lee and Bradbury Roads.", "ts_dict_index": [4659, 4660, 4661]}
+{"event_id": 1060464, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2022-12-10 19:19:00", "end_date_time": "2022-12-10 21:19:00", "narrative": "A strong low pressure system slowly moved across central California on December 10 and 11 providing the area with moderate to heavy precipitation. The precipitation fell as snow above 5000 feet with several SNOTEL stations picking up between 18 and 30 inches of estimated new snowfall. The snow level lowered to near 3000 feet by the afternoon of December 11 with some stations in the Sierra Nevada and higher foothills picking up between 3 and 6 inches of new snowfall. Many stations in the Sierra Nevada received between 3 and 5 inches of liquid precipitation while the adjacent foothills picked up between 1.5 and 3 inches of rainfall and much of the San Joaquin Valley and Tehachapi Mountains received between half an inch and an inch of rainfall. The precipitation did change over the snow in the Tehachapi Mountains above 4000 feet, but snowfall amounts were generally light. Rain shadowing effects limited precipitation across the Kern County Deserts with most stations receiving between a tenth of an inch and a quarter inch of rainfall. The precipitation tapered off during the evening of December 11 and ended by midday on December 12. California Highway Patrol reported roadway flooding on SR J59 in Snelling.", "ts_dict_index": [4656, 4657, 4658]}
+{"event_id": 1060466, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2022-12-10 20:07:00", "end_date_time": "2022-12-10 22:07:00", "narrative": "A strong low pressure system slowly moved across central California on December 10 and 11 providing the area with moderate to heavy precipitation. The precipitation fell as snow above 5000 feet with several SNOTEL stations picking up between 18 and 30 inches of estimated new snowfall. The snow level lowered to near 3000 feet by the afternoon of December 11 with some stations in the Sierra Nevada and higher foothills picking up between 3 and 6 inches of new snowfall. Many stations in the Sierra Nevada received between 3 and 5 inches of liquid precipitation while the adjacent foothills picked up between 1.5 and 3 inches of rainfall and much of the San Joaquin Valley and Tehachapi Mountains received between half an inch and an inch of rainfall. The precipitation did change over the snow in the Tehachapi Mountains above 4000 feet, but snowfall amounts were generally light. Rain shadowing effects limited precipitation across the Kern County Deserts with most stations receiving between a tenth of an inch and a quarter inch of rainfall. The precipitation tapered off during the evening of December 11 and ended by midday on December 12. California Highway Patrol reported roadway flooding on northbound SR 99 in Atwater.", "ts_dict_index": [4650, 4651, 4652]}
+{"event_id": 1095867, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-04-01 00:00:00", "end_date_time": "2023-04-10 12:00:00", "narrative": "Snowmelt runoff from the anomalous amounts of snow over the Arizona high terrain led to continued elevated flows in the Salt and Verde River watersheds. Dam releases being conducted in these watersheds to deal with the abnormal runoff led to continued downstream impacts along the Salt and Gila Rivers, which initially began in March. Continued releases from Granite Reef Dam allowed for elevated flows to persist in the normally dry Salt River with multiple unbridged river crossings remaining closed due to flooding. The heightened flows in the Salt River led to the fatalities of two men who were caught in an undercurrent while paddle boarding down the river. Releases from Granite Reef Dam were significantly reduced by the end of April as runoff into the watersheds decreased. Flow in the Salt and Gila Rivers continued to travel downstream to Painted Rock Dam. Releases from this dam led to elevated flows traveling down the Gila River into Yuma County, leading to numerous additional closures of unbridged river crossings. Elevated flows in the Salt and Gila Rivers allowed for impacts to persist into the month of May. According to MCDOT, the unbridged Salt River crossing along Gilbert Road between Thomas Road and SR 87 was closed due to flooding beginning on March 14th and continuing into April. The unbridged Gilbert Road crossing sustained heavy damage due to the high flows in the river, keeping the road closed after waters had receded. End timing based on water releases from Granite Reef Dam.", "ts_dict_index": [4674, 4675, 4676]}
+{"event_id": 1095873, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-04-01 00:00:00", "end_date_time": "2023-04-09 10:15:00", "narrative": "Snowmelt runoff from the anomalous amounts of snow over the Arizona high terrain led to continued elevated flows in the Salt and Verde River watersheds. Dam releases being conducted in these watersheds to deal with the abnormal runoff led to continued downstream impacts along the Salt and Gila Rivers, which initially began in March. Continued releases from Granite Reef Dam allowed for elevated flows to persist in the normally dry Salt River with multiple unbridged river crossings remaining closed due to flooding. The heightened flows in the Salt River led to the fatalities of two men who were caught in an undercurrent while paddle boarding down the river. Releases from Granite Reef Dam were significantly reduced by the end of April as runoff into the watersheds decreased. Flow in the Salt and Gila Rivers continued to travel downstream to Painted Rock Dam. Releases from this dam led to elevated flows traveling down the Gila River into Yuma County, leading to numerous additional closures of unbridged river crossings. Elevated flows in the Salt and Gila Rivers allowed for impacts to persist into the month of May. Two men paddle boarding down the Salt River were caught in an undercurrent near 19th Avenue and Broadway on the 9th. They became stuck in the undercurrent around 1000MST and began yelling for help before disappearing under the water. The bodies of the two men were recovered about a week later on the 15th and 16th. Flow in the Salt River was unusually high at the time due to continued upstream releases from Granite Reef Dam. Start time based on continued releases from Granite Reef Dam.", "ts_dict_index": [4677, 4678, 4679]}
+{"event_id": 1095876, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-04-01 00:00:00", "end_date_time": "2023-04-30 23:59:00", "narrative": "Snowmelt runoff from the anomalous amounts of snow over the Arizona high terrain led to continued elevated flows in the Salt and Verde River watersheds. Dam releases being conducted in these watersheds to deal with the abnormal runoff led to continued downstream impacts along the Salt and Gila Rivers, which initially began in March. Continued releases from Granite Reef Dam allowed for elevated flows to persist in the normally dry Salt River with multiple unbridged river crossings remaining closed due to flooding. The heightened flows in the Salt River led to the fatalities of two men who were caught in an undercurrent while paddle boarding down the river. Releases from Granite Reef Dam were significantly reduced by the end of April as runoff into the watersheds decreased. Flow in the Salt and Gila Rivers continued to travel downstream to Painted Rock Dam. Releases from this dam led to elevated flows traveling down the Gila River into Yuma County, leading to numerous additional closures of unbridged river crossings. Elevated flows in the Salt and Gila Rivers allowed for impacts to persist into the month of May. Water being released from Painted Rock Dam traveled down the Gila River, flooding several low water crossings between the dam and the Yuma County line. This led to the closures of Poco Dinero Road between Painted Rock Dam Road and Saddle Road as well as Rocky Point Road between Hyder Road and Painted Rock Dam Road.", "ts_dict_index": [4680, 4681, 4682]}
+{"event_id": 1059221, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2022-09-18 09:30:00", "end_date_time": "2022-09-19 01:30:00", "narrative": "An upper level jet diving down the coast of California, combined with plentiful lower level moisture advected from the Pacific set the stage for an early season rain storm and strong winds around much of the Bay Area and Central Coast. The highest winds occurred along the coast, where various sites reported gusts between 35 and 50 mph. A wind advisory was in effect from early Sunday morning through Sunday evening for the immediate coast and coastal hills. Highest rainfall totals were recorded in the coastal mountains from Sonoma County southward through Big Sur, resulting in localized flooding, downed trees/powerlines and debris/rocks sliding onto Highway 1 in Big Sur. A flood advisory was issued for a large portion of the Monterey Bay coastal zone and Big Sur coast from late night on the 18th through early morning on the 19th. Storm Total Rainfall measured 2 to 3.5 inches in North Bay Coastal Mountains, 1.5 to 2.2 inches in the Santa Cruz Mountains and 2 to 4.7 inches in the Santa Lucia's. Lower totals closer to an inch or less were recorded around the SF Bay Shoreline and coastal Monterey Bay. Highway 1 closed between Point Lobos and Ragged Point due to highway flooding and weather conditions.", "ts_dict_index": [4692, 4693, 4694]}
+{"event_id": 1095860, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-04-01 00:00:00", "end_date_time": "2023-04-10 12:00:00", "narrative": "Snowmelt runoff from the anomalous amounts of snow over the Arizona high terrain led to continued elevated flows in the Salt and Verde River watersheds. Dam releases being conducted in these watersheds to deal with the abnormal runoff led to continued downstream impacts along the Salt and Gila Rivers, which initially began in March. Continued releases from Granite Reef Dam allowed for elevated flows to persist in the normally dry Salt River with multiple unbridged river crossings remaining closed due to flooding. The heightened flows in the Salt River led to the fatalities of two men who were caught in an undercurrent while paddle boarding down the river. Releases from Granite Reef Dam were significantly reduced by the end of April as runoff into the watersheds decreased. Flow in the Salt and Gila Rivers continued to travel downstream to Painted Rock Dam. Releases from this dam led to elevated flows traveling down the Gila River into Yuma County, leading to numerous additional closures of unbridged river crossings. Elevated flows in the Salt and Gila Rivers allowed for impacts to persist into the month of May. According to MCDOT, the unbridged Gila River crossing along El Mirage Road between Southern Avenue and Indian Springs Road was closed due to flooding beginning on March 14th and continuing into April. End timing based on upstream FCDMC stream gauge along the Gila River at 116th Avenue.", "ts_dict_index": [4689, 4690, 4691]}
+{"event_id": 1095858, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-04-01 00:00:00", "end_date_time": "2023-04-15 13:30:00", "narrative": "Snowmelt runoff from the anomalous amounts of snow over the Arizona high terrain led to continued elevated flows in the Salt and Verde River watersheds. Dam releases being conducted in these watersheds to deal with the abnormal runoff led to continued downstream impacts along the Salt and Gila Rivers, which initially began in March. Continued releases from Granite Reef Dam allowed for elevated flows to persist in the normally dry Salt River with multiple unbridged river crossings remaining closed due to flooding. The heightened flows in the Salt River led to the fatalities of two men who were caught in an undercurrent while paddle boarding down the river. Releases from Granite Reef Dam were significantly reduced by the end of April as runoff into the watersheds decreased. Flow in the Salt and Gila Rivers continued to travel downstream to Painted Rock Dam. Releases from this dam led to elevated flows traveling down the Gila River into Yuma County, leading to numerous additional closures of unbridged river crossings. Elevated flows in the Salt and Gila Rivers allowed for impacts to persist into the month of May. According to MCDOT, the unbridged Salt River crossing along 67th Avenue between Broadway Road and Southern Avenue was closed due to flooding beginning on March 12th and continuing into April. End timing estimated based on upstream FCDMC stream gauge at 51st Avenue.", "ts_dict_index": [4686, 4687, 4688]}
+{"event_id": 1027932, "event_type": "Flood", "state": "MISSOURI", "cz_name": "MCDONALD", "begin_date_time": "2022-05-04 16:19:00", "end_date_time": "2022-05-05 02:00:00", "narrative": "A stalled front from the storm a system on May 2-3 moved northward back into the Ozarks as a warm front as a strong upper level low over southern Colorado moved eastward into the southern Plains. This led to another several rounds of widespread heavy rainfall that occurred from the late morning of the 4th to the early morning of the 6th, when the surface low exited the area. Widespread accumulations of two to five inches occurred, with isolated accumulations over six inches over parts of Jasper and Dade Counties. Numerous reports of flash flooding indicated that not only were low water crossings flooding, but major highways as well. Evacuations were conducted at both Roaring River State Park in Barry County and at Bennett Spring State Park on the Dallas/Laclede County Border. Several people were stranded in cabins and RVs at Bennett Spring during the peak of the flood. There were 11 swift water rescues reported in southwest Missouri. Unfortunately, there was one fatality in Dade County when a 65-year old male drove into a flooded low water crossing and was swept downstream after exiting his vehicle and attempting to swim to shore. Highway CC at Indian Creek was flooded and impassable.", "ts_dict_index": [4626, 4627, 4628]}
+{"event_id": 917763, "event_type": "Flood", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-08-24 21:15:00", "end_date_time": "2020-08-25 08:36:00", "narrative": "A hot and humid airmass was in place, providing enough energy for scattered thunderstorms to develop across the region. The hardest hit area was in the town of Whitehall, New York which saw repeated rounds of heavy rain and thunderstorms during the afternoon and early evening hours of August 24th. An impressive 4 to 6 inches of rain fell across the far northeast portions of Washington County, resulting in 8 flooded roadways, 21 flooded structures, 1 water rescue, several cars partially submerged and the Whitehall Junior-Senior High School being significantly damaged by the flood waters. The school superintendent estimated that it would cost 16 million dollars to repair the damages from the flood waters. Overall, 40 homes and 13 businesses or non-profit organizations sustained damage totaling 1.5 million dollars. There was also about 1,200 power outages as a result of the storms in Washington County. A Physical Disaster Declaration was declared for Washington County as a result of the storms. There was also one isolated report of trees down in Albany county from a separate storm. ", "ts_dict_index": [4725, 4726, 4727]}
+{"event_id": 876220, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2020-04-05 14:06:00", "end_date_time": "2020-04-05 16:06:00", "narrative": "A very cold and moist low pressure system dropped south out of the Gulf of Alaska on April 4 and moved slowly southward off the California coast on April 5 and 6. This system brought moderate to heavy precipitation to the area between the afternoon of April 5 to the afternoon of April 6. Several stations in the Sierra Nevada and adjacent foothills picked up between 1.5 and 3 inches of liquid precipitation while much of the eastern San Joaquin Valley picked up between 0.75 and 1.5 inches of rainfall. The west side of the San Joaquin Valley along with the Kern County Mountains and Deserts generally picked up between half and inch and an inch of rain. Several STOTEL stations in the Sierra Nevada above 5500 feet picked up an estimated 18 to 36 of new snowfall with a few stations above 8000 feet picking up higher amounts. There were reports of localized nuisance flooding, as a few thunderstorms popped up during the afternoon of April 6. One of the thunderstorms produced a funnel cloud near Laton which was observed by several spotters and reported by several media outlets. California Highway Patrol reported roadway flooding at the intersection of SR 165 and August Ave. in Hilmar.", "ts_dict_index": [4728, 4729, 4730]}
+{"event_id": 1059206, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2022-09-18 22:00:00", "end_date_time": "2022-09-19 02:00:00", "narrative": "An upper level jet diving down the coast of California, combined with plentiful lower level moisture advected from the Pacific set the stage for an early season rain storm and strong winds around much of the Bay Area and Central Coast. The highest winds occurred along the coast, where various sites reported gusts between 35 and 50 mph. A wind advisory was in effect from early Sunday morning through Sunday evening for the immediate coast and coastal hills. Highest rainfall totals were recorded in the coastal mountains from Sonoma County southward through Big Sur, resulting in localized flooding, downed trees/powerlines and debris/rocks sliding onto Highway 1 in Big Sur. A flood advisory was issued for a large portion of the Monterey Bay coastal zone and Big Sur coast from late night on the 18th through early morning on the 19th. Storm Total Rainfall measured 2 to 3.5 inches in North Bay Coastal Mountains, 1.5 to 2.2 inches in the Santa Cruz Mountains and 2 to 4.7 inches in the Santa Lucia's. Lower totals closer to an inch or less were recorded around the SF Bay Shoreline and coastal Monterey Bay. Social media report of flooding in roadways in pacific grove after 45 minutes of heavy rainfall.", "ts_dict_index": [4695, 4696, 4697]}
+{"event_id": 990429, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2021-12-23 16:35:00", "end_date_time": "2021-12-23 17:35:00", "narrative": "A deep upper trough with a warm subtropical moisture fetch in front of it pushed into central California during the evening of December 22 and brought a period of rain and higher elevation snow to the area which continued through the evening of December 23. Several stations in the Sierra Nevada measured between 1 and 3 inches of liquid precipitation with the snow level between 8000 and 9000 feet.  Rain shadowing kept precipitation amounts in the San Joaquin Valley lower with a half inch to an inch of rain on the east side and a quarter to half inch of the west side.  Some localized nuisance flooding was reported during the afternoon of December 23.  Cooler air pushed into the area during the evening of December 23 resulting in showery precipitation which continued through the early morning of December 24.  A few higher elevation SNOTELs picked up an estimated 18 to 24 inches of new snowfall.  Some ice pellet showers and a few thunderstorms were observed in the Sierra foothills and the snow level in the Sierra Nevada lowered to around 5500 feet before the precipitation tapered off. California Highway Patrol reported roadway flooding at the intersection of SR 65 and Harvard Ave.", "ts_dict_index": [4713, 4714, 4715]}
+{"event_id": 876231, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2020-04-08 12:15:00", "end_date_time": "2020-04-09 08:00:00", "narrative": "The cold upper low pressure system that brought moderate to heavy precipitation across much of the area on April 5 and 6 was situated off the southern California coast on April 7 then tracked slowly northeast toward central California on April 8 and across the area on April 9. As a result, additional precipitation spread into Kern County during the evening of April 7 and spread northward across the area on April 8. This system produced periods of heavy rainfall across Kern County on April 8 where there were widespread reports of a half inch to an inch of rainfall which resulted in several instances of debris flows and nuisance roadway flooding. Further north, much of Fresno, Kings and Tulare Counties measured between a quarter and a half inch of liquid precipitation while areas north of Fresno County generally picked up between a tenth of an inch to a quarter inch of liquid precipitation. Several stations above 5500 feet in Kern and Tulare Counties picked up between 3 and 6 inches of new snowfall. The precipitation finally ended by the evening of April 9 as the low moved out of our area. California Highway Patrol reported roadway flooding at the intersection of Hart St. and East McCord Ave. in Oildale.", "ts_dict_index": [4698, 4699, 4700]}
+{"event_id": 876227, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2020-04-07 23:06:00", "end_date_time": "2020-04-09 08:00:00", "narrative": "The cold upper low pressure system that brought moderate to heavy precipitation across much of the area on April 5 and 6 was situated off the southern California coast on April 7 then tracked slowly northeast toward central California on April 8 and across the area on April 9. As a result, additional precipitation spread into Kern County during the evening of April 7 and spread northward across the area on April 8. This system produced periods of heavy rainfall across Kern County on April 8 where there were widespread reports of a half inch to an inch of rainfall which resulted in several instances of debris flows and nuisance roadway flooding. Further north, much of Fresno, Kings and Tulare Counties measured between a quarter and a half inch of liquid precipitation while areas north of Fresno County generally picked up between a tenth of an inch to a quarter inch of liquid precipitation. Several stations above 5500 feet in Kern and Tulare Counties picked up between 3 and 6 inches of new snowfall. The precipitation finally ended by the evening of April 9 as the low moved out of our area. California Highway Patrol reported roadway flooding on SR 166 between Maricopa and Mettler due to earlier heavy rain.", "ts_dict_index": [4704, 4705, 4706]}
+{"event_id": 876226, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2020-04-07 21:45:00", "end_date_time": "2020-04-10 08:00:00", "narrative": "The cold upper low pressure system that brought moderate to heavy precipitation across much of the area on April 5 and 6 was situated off the southern California coast on April 7 then tracked slowly northeast toward central California on April 8 and across the area on April 9. As a result, additional precipitation spread into Kern County during the evening of April 7 and spread northward across the area on April 8. This system produced periods of heavy rainfall across Kern County on April 8 where there were widespread reports of a half inch to an inch of rainfall which resulted in several instances of debris flows and nuisance roadway flooding. Further north, much of Fresno, Kings and Tulare Counties measured between a quarter and a half inch of liquid precipitation while areas north of Fresno County generally picked up between a tenth of an inch to a quarter inch of liquid precipitation. Several stations above 5500 feet in Kern and Tulare Counties picked up between 3 and 6 inches of new snowfall. The precipitation finally ended by the evening of April 9 as the low moved out of our area. California Highway Patrol reported roadway flooding on Red Rock-Randsburg Road which resulted in the road being closed for over 2 days.", "ts_dict_index": [4710, 4711, 4712]}
+{"event_id": 870340, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2020-02-22 15:45:00", "end_date_time": "2020-02-22 23:00:00", "narrative": "A strong, wet Pacific upper level low pressure system spread copious amounts of moisture into south central Arizona on Saturday February 22nd; as a result widespread rain developed early in the morning and the moderate to heavy rain persisted for much of the day. The heaviest rainfall amounts occurred over higher terrain areas to the east of Phoenix; most of the rain gages in the area measured between 1.25 and 3 inches with the most significant rain occurring during the morning hours. The excessive rain resulted in a few episodes of areal flooding which included the Sycamore Creek and Tonto Creek basins. During the afternoon hours, local law enforcement reported multiple roads closed due to flooding in the Tonto Creek basin; the closures occurred to the northwest of Lake Roosevelt. An areal flood warning was issued for the basin due to elevated flow in the creek and the warning persisted for several days. In addition, during the evening hours a family of 5 drove into Sycamore Creek, which was flowing heavily, and became stranded necessitating a water rescue. A strong Pacific upper low spread copious amounts of moisture into south-central Arizona on Saturday February 22nd; this led to widespread moderate to heavy rain across higher terrain areas to the northeast of Phoenix. The excessive rain resulted in some areal flooding during the afternoon and evening hours, affecting the Sycamore Creek basin. According to local broadcast media, at roughly 2115MST a family of 5 drove their vehicle into Sycamore Creek, about 7 miles to the north-northwest of Saguaro Lake. Due to flowing water in the creek, their vehicle became stuck and necessitated a water rescue. There were several other vehicles trapped on river banks   awaiting the waters to recede so that they could proceed. There were no reports of accidents, injuries or fatalities. At the time there were no flood warnings in effect for the area as heavy rain had ended a long time ago.", "ts_dict_index": [4731, 4732, 4733]}
+{"event_id": 876228, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2020-04-08 09:54:00", "end_date_time": "2020-04-09 08:00:00", "narrative": "The cold upper low pressure system that brought moderate to heavy precipitation across much of the area on April 5 and 6 was situated off the southern California coast on April 7 then tracked slowly northeast toward central California on April 8 and across the area on April 9. As a result, additional precipitation spread into Kern County during the evening of April 7 and spread northward across the area on April 8. This system produced periods of heavy rainfall across Kern County on April 8 where there were widespread reports of a half inch to an inch of rainfall which resulted in several instances of debris flows and nuisance roadway flooding. Further north, much of Fresno, Kings and Tulare Counties measured between a quarter and a half inch of liquid precipitation while areas north of Fresno County generally picked up between a tenth of an inch to a quarter inch of liquid precipitation. Several stations above 5500 feet in Kern and Tulare Counties picked up between 3 and 6 inches of new snowfall. The precipitation finally ended by the evening of April 9 as the low moved out of our area. California Highway Patrol reported roadway flooding at the intersection of SR 223 and Adobe Road 5SW Lamont.", "ts_dict_index": [4707, 4708, 4709]}
+{"event_id": 1088383, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-16 07:00:00", "end_date_time": "2023-03-16 20:00:00", "narrative": "An area of low pressure moving across the western states resulted in waves of rainfall across the region during the day on the 15th. A round of widespread light to locally moderate rainfall activity was observed during the morning hours followed by a more significant round with thunderstorms during the evening hours in association with a cold front. Moisture levels associated with this low pressure system were in the 99th percentile for mid-March, signifying that environment was favorable for heavier rainfall rates to materialize. As a result of the heavier rainfall activity observed during the evening hours, flooding was observed across the Wickenburg area in northwestern Maricopa County, where over an inch of total rainfall was observed. Flooding was also observed along the low-water crossings that intersect the Hassayampa River, which runs from north to south along the western third of Maricopa County. Strong storms were also observed during the afternoon hours across southwestern Arizona, producing isolated gusts around 60 mph in the Yuma area. Tonopah Salome Highway between 327th Drive and 315th Avenue was closed due to overflow from the Hassayampa River. No damages or injuries were reported.", "ts_dict_index": [4734, 4735, 4736]}
+{"event_id": 1088385, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-16 00:00:00", "end_date_time": "2023-03-16 13:00:00", "narrative": "An area of low pressure moving across the western states resulted in waves of rainfall across the region during the day on the 15th. A round of widespread light to locally moderate rainfall activity was observed during the morning hours followed by a more significant round with thunderstorms during the evening hours in association with a cold front. Moisture levels associated with this low pressure system were in the 99th percentile for mid-March, signifying that environment was favorable for heavier rainfall rates to materialize. As a result of the heavier rainfall activity observed during the evening hours, flooding was observed across the Wickenburg area in northwestern Maricopa County, where over an inch of total rainfall was observed. Flooding was also observed along the low-water crossings that intersect the Hassayampa River, which runs from north to south along the western third of Maricopa County. Strong storms were also observed during the afternoon hours across southwestern Arizona, producing isolated gusts around 60 mph in the Yuma area. Patton Road between 293rd Ave and Douglas Ranch Rd was closed due to flooding from the overflow of the Hassayampa River. A Maricopa County Flood Control District Gauge located 11 miles upstream registered flows going above alarm stage, which is 9.0 feet, at 21:50 MST on 3/15, peaking at 9.81 feet (2011 cfs) at 23:30 MST. The flow went below alarm stage at 10:58 MST on 3/16. No damages or injuries were reported.", "ts_dict_index": [4737, 4738, 4739]}
+{"event_id": 1088384, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-16 07:00:00", "end_date_time": "2023-03-16 20:00:00", "narrative": "An area of low pressure moving across the western states resulted in waves of rainfall across the region during the day on the 15th. A round of widespread light to locally moderate rainfall activity was observed during the morning hours followed by a more significant round with thunderstorms during the evening hours in association with a cold front. Moisture levels associated with this low pressure system were in the 99th percentile for mid-March, signifying that environment was favorable for heavier rainfall rates to materialize. As a result of the heavier rainfall activity observed during the evening hours, flooding was observed across the Wickenburg area in northwestern Maricopa County, where over an inch of total rainfall was observed. Flooding was also observed along the low-water crossings that intersect the Hassayampa River, which runs from north to south along the western third of Maricopa County. Strong storms were also observed during the afternoon hours across southwestern Arizona, producing isolated gusts around 60 mph in the Yuma area. Baseline Rd between Johnson Rd and 331st Ave was closed due to flooding from the overflow of the Hassayampa River. No damages or injuries were reported.", "ts_dict_index": [4740, 4741, 4742]}
+{"event_id": 1072364, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-02-24 17:05:00", "end_date_time": "2023-02-24 19:05:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported near Lake Success on Success Valley Dr.", "ts_dict_index": [4767, 4768, 4769]}
+{"event_id": 1072356, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2023-02-24 12:57:00", "end_date_time": "2023-02-24 14:57:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported roadway flooding in the southbound lanes of SR 99 just north of Westside Blvd. in Atwater.", "ts_dict_index": [4761, 4762, 4763]}
+{"event_id": 859402, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-12-08 14:27:00", "end_date_time": "2019-12-08 14:57:00", "narrative": "An upper trough slowly moved across California during the weekend of December 7 and 8 producing widespread precipitation across the area. The heaviest precipitation occurred from Fresno County northward where several stations in the Sierra measured between 1 and 2 inches of liquid precipitation while several stations in the valley measured between a half inch and an inch of rainfall. Further south, much of Kings and Tulare Counties picked up between a quarter inch and a half inch of precipitation and most stations in Kern County picking up less than a quarter inch of rainfall. The snow level ranged between 7000 and 8000 feet for most of this event with several locations in the higher Sierra picking up between 8 ans 12 inches of new snowfall over the weekend. In addition the rain and mountain snowfall, scattered thunderstorms produced some areas of locally heavy rainfall, roadway flooding and small hail from the late morning the early evening of December 8. The precipitation ended by late evening as the trough moved to the east of the area. A trained spotted reported minor road flooding from heavy rain in Clovis along Shaw Ave.", "ts_dict_index": [4758, 4759, 4760]}
+{"event_id": 882100, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2020-05-19 09:05:00", "end_date_time": "2020-05-19 20:35:00", "narrative": "A slow moving low pressure system drifted across the Ohio Valley on May 18 and 19, bringing several rounds of heavy rain to the eastern reaches of the Commonwealth. The hardest hit areas spanned from the Cumberland Valley to the Bluegrass region where widespread rainfall amounts of 3-6 inches fell over the two day period. This caused several road closures and flooding of low lying areas as points on the Red, Kentucky, and Cumberland Rivers reached minor to moderate flood stage. In Jackson County, a couple of water rescues had to be performed as motorists became trapped.||Flash flooding was confined to the afternoon and evening hours of May 18th across portions of Pulaski and Fleming Counties, while isolated severe thunderstorm winds occurred in Laurel and Jackson Counties. Additionally, a home near Somerset was hit by lightning while mudslides occurred near Bledsoe in Harlan County on U.S. Highway 421, on Kentucky Highway 1110 south of Jackson in Breathitt County, and on Proctor Road near Beattyville in Lee County due to the abundant rainfall. A citizen observed low lying flooding near Gray Hawk.", "ts_dict_index": [4746, 4747, 4748]}
+{"event_id": 882300, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2020-05-19 09:10:00", "end_date_time": "2020-05-19 20:40:00", "narrative": "A slow moving low pressure system drifted across the Ohio Valley on May 18 and 19, bringing several rounds of heavy rain to the eastern reaches of the Commonwealth. The hardest hit areas spanned from the Cumberland Valley to the Bluegrass region where widespread rainfall amounts of 3-6 inches fell over the two day period. This caused several road closures and flooding of low lying areas as points on the Red, Kentucky, and Cumberland Rivers reached minor to moderate flood stage. In Jackson County, a couple of water rescues had to be performed as motorists became trapped.||Flash flooding was confined to the afternoon and evening hours of May 18th across portions of Pulaski and Fleming Counties, while isolated severe thunderstorm winds occurred in Laurel and Jackson Counties. Additionally, a home near Somerset was hit by lightning while mudslides occurred near Bledsoe in Harlan County on U.S. Highway 421, on Kentucky Highway 1110 south of Jackson in Breathitt County, and on Proctor Road near Beattyville in Lee County due to the abundant rainfall. Low lying flooding occurred south and west of McKee, resulting in two water rescues as motorists became stranded in flood waters on and just off of Kentucky Highway 89.", "ts_dict_index": [4755, 4756, 4757]}
+{"event_id": 1072419, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-02-25 19:27:00", "end_date_time": "2023-02-25 21:27:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported a car crashed on northbound SR 99 just south of the California Ave. exchange after it hit standing water.", "ts_dict_index": [4764, 4765, 4766]}
+{"event_id": 882111, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2020-05-19 09:05:00", "end_date_time": "2020-05-19 20:35:00", "narrative": "A slow moving low pressure system drifted across the Ohio Valley on May 18 and 19, bringing several rounds of heavy rain to the eastern reaches of the Commonwealth. The hardest hit areas spanned from the Cumberland Valley to the Bluegrass region where widespread rainfall amounts of 3-6 inches fell over the two day period. This caused several road closures and flooding of low lying areas as points on the Red, Kentucky, and Cumberland Rivers reached minor to moderate flood stage. In Jackson County, a couple of water rescues had to be performed as motorists became trapped.||Flash flooding was confined to the afternoon and evening hours of May 18th across portions of Pulaski and Fleming Counties, while isolated severe thunderstorm winds occurred in Laurel and Jackson Counties. Additionally, a home near Somerset was hit by lightning while mudslides occurred near Bledsoe in Harlan County on U.S. Highway 421, on Kentucky Highway 1110 south of Jackson in Breathitt County, and on Proctor Road near Beattyville in Lee County due to the abundant rainfall. Local media reported flooding of low lying and poor drainage areas near Tyner.", "ts_dict_index": [4752, 4753, 4754]}
+{"event_id": 882101, "event_type": "Flood", "state": "KENTUCKY", "cz_name": "JACKSON", "begin_date_time": "2020-05-19 09:10:00", "end_date_time": "2020-05-19 20:40:00", "narrative": "A slow moving low pressure system drifted across the Ohio Valley on May 18 and 19, bringing several rounds of heavy rain to the eastern reaches of the Commonwealth. The hardest hit areas spanned from the Cumberland Valley to the Bluegrass region where widespread rainfall amounts of 3-6 inches fell over the two day period. This caused several road closures and flooding of low lying areas as points on the Red, Kentucky, and Cumberland Rivers reached minor to moderate flood stage. In Jackson County, a couple of water rescues had to be performed as motorists became trapped.||Flash flooding was confined to the afternoon and evening hours of May 18th across portions of Pulaski and Fleming Counties, while isolated severe thunderstorm winds occurred in Laurel and Jackson Counties. Additionally, a home near Somerset was hit by lightning while mudslides occurred near Bledsoe in Harlan County on U.S. Highway 421, on Kentucky Highway 1110 south of Jackson in Breathitt County, and on Proctor Road near Beattyville in Lee County due to the abundant rainfall. A citizen observed flooding of low lying areas near McKee.", "ts_dict_index": [4749, 4750, 4751]}
+{"event_id": 1088387, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-03-16 07:00:00", "end_date_time": "2023-03-16 11:00:00", "narrative": "An area of low pressure moving across the western states resulted in waves of rainfall across the region during the day on the 15th. A round of widespread light to locally moderate rainfall activity was observed during the morning hours followed by a more significant round with thunderstorms during the evening hours in association with a cold front. Moisture levels associated with this low pressure system were in the 99th percentile for mid-March, signifying that environment was favorable for heavier rainfall rates to materialize. As a result of the heavier rainfall activity observed during the evening hours, flooding was observed across the Wickenburg area in northwestern Maricopa County, where over an inch of total rainfall was observed. Flooding was also observed along the low-water crossings that intersect the Hassayampa River, which runs from north to south along the western third of Maricopa County. Strong storms were also observed during the afternoon hours across southwestern Arizona, producing isolated gusts around 60 mph in the Yuma area. Old Stage Rd Northbound at New River Rd was closed due to flooding. No damages or injuries were reported.", "ts_dict_index": [4743, 4744, 4745]}
+{"event_id": 1095857, "event_type": "Flood", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-04-01 00:00:00", "end_date_time": "2023-04-30 23:59:00", "narrative": "Snowmelt runoff from the anomalous amounts of snow over the Arizona high terrain led to continued elevated flows in the Salt and Verde River watersheds. Dam releases being conducted in these watersheds to deal with the abnormal runoff led to continued downstream impacts along the Salt and Gila Rivers, which initially began in March. Continued releases from Granite Reef Dam allowed for elevated flows to persist in the normally dry Salt River with multiple unbridged river crossings remaining closed due to flooding. The heightened flows in the Salt River led to the fatalities of two men who were caught in an undercurrent while paddle boarding down the river. Releases from Granite Reef Dam were significantly reduced by the end of April as runoff into the watersheds decreased. Flow in the Salt and Gila Rivers continued to travel downstream to Painted Rock Dam. Releases from this dam led to elevated flows traveling down the Gila River into Yuma County, leading to numerous additional closures of unbridged river crossings. Elevated flows in the Salt and Gila Rivers allowed for impacts to persist into the month of May. According to the Maricopa County DOT, McKellips Road between Alma School Road and SR 202 remained closed due to flooding from the Salt River beginning on March 7th and continuing through April. Timing based on water releases from Granite Reef Dam.", "ts_dict_index": [4683, 4684, 4685]}
+{"event_id": 1072365, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2023-02-24 17:30:00", "end_date_time": "2023-02-24 19:30:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported roadway flooding on northbound SR 99 south of the SR 41 exchange.", "ts_dict_index": [4776, 4777, 4778]}
+{"event_id": 1072418, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-02-25 14:57:00", "end_date_time": "2023-02-25 16:57:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported the entire roadway on Ave. 32 and Richgrove Dr. were flooded.", "ts_dict_index": [4773, 4774, 4775]}
+{"event_id": 1072423, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-02-25 22:06:00", "end_date_time": "2023-02-26 00:06:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported all lanes of eastbound SR 178 at Union Ave in Bakersfield were flooded. Several vehicles hydroplaned.", "ts_dict_index": [4770, 4771, 4772]}
+{"event_id": 1072358, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2023-02-24 13:18:00", "end_date_time": "2023-02-24 15:18:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported a downed tree blocking the northbound lane of Del North Ave. just north of Whitesbridge Ave. in Kerman.", "ts_dict_index": [4788, 4789, 4790]}
+{"event_id": 1072378, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2023-02-24 20:50:00", "end_date_time": "2023-02-24 22:50:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported a vehicle hit a flooded area on northbound SR 99 south of the North Ave. exchange and spun out.", "ts_dict_index": [4800, 4801, 4802]}
+{"event_id": 1072359, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-02-24 14:26:00", "end_date_time": "2023-02-24 16:26:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported a tree down blocking the entire roadway at the intersection of Ashworth Rd. and Old Oak Ln.", "ts_dict_index": [4782, 4783, 4784]}
+{"event_id": 1072351, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2023-02-24 08:03:00", "end_date_time": "2023-02-24 10:03:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported roadway flooding just east of the SR 198/18th Ave onramp and flooding on eastbound SR 198 under the 17th Ave and Houston Ave exchange.", "ts_dict_index": [4806, 4807, 4808]}
+{"event_id": 1072415, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-02-25 09:30:00", "end_date_time": "2023-02-25 11:30:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported Rd. 236 was closed due to flooding between Ave. 80 and Ave. 60 north of Ducor.", "ts_dict_index": [4785, 4786, 4787]}
+{"event_id": 1072355, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-02-24 12:56:00", "end_date_time": "2023-02-24 14:56:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported a car slid down the embankment in the westbound lane of SR 41 just east of the county line. Heavy rain was occurring in the area at the time.", "ts_dict_index": [4779, 4780, 4781]}
+{"event_id": 1072422, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-02-25 20:23:00", "end_date_time": "2023-02-25 22:23:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported flooding on southbound SR 99 south of Wilson Rd.", "ts_dict_index": [4794, 4795, 4796]}
+{"event_id": 1072407, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-02-25 08:20:00", "end_date_time": "2023-02-25 10:20:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported flooding on Sandrini Rd. between Adobe Rd. and Wheeler Ridge Rd.", "ts_dict_index": [4809, 4810, 4811]}
+{"event_id": 1072352, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-02-24 11:10:00", "end_date_time": "2023-02-24 14:10:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported flooding at the intersection of Kelso Valley Rd. and Kelso Creek Rd. resulting in the closures of both roads.", "ts_dict_index": [4791, 4792, 4793]}
+{"event_id": 1072376, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-02-24 20:27:00", "end_date_time": "2023-02-24 22:27:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported rocks up to 3 feet in diameter washed up on Interstate 5 north of Lebec.", "ts_dict_index": [4803, 4804, 4805]}
+{"event_id": 1060468, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2022-12-10 20:51:00", "end_date_time": "2022-12-10 22:51:00", "narrative": "A strong low pressure system slowly moved across central California on December 10 and 11 providing the area with moderate to heavy precipitation. The precipitation fell as snow above 5000 feet with several SNOTEL stations picking up between 18 and 30 inches of estimated new snowfall. The snow level lowered to near 3000 feet by the afternoon of December 11 with some stations in the Sierra Nevada and higher foothills picking up between 3 and 6 inches of new snowfall. Many stations in the Sierra Nevada received between 3 and 5 inches of liquid precipitation while the adjacent foothills picked up between 1.5 and 3 inches of rainfall and much of the San Joaquin Valley and Tehachapi Mountains received between half an inch and an inch of rainfall. The precipitation did change over the snow in the Tehachapi Mountains above 4000 feet, but snowfall amounts were generally light. Rain shadowing effects limited precipitation across the Kern County Deserts with most stations receiving between a tenth of an inch and a quarter inch of rainfall. The precipitation tapered off during the evening of December 11 and ended by midday on December 12. California Highway Patrol reported roadway flooding at the intersection of Westside and Lincoln Boulevards in Livingston.", "ts_dict_index": [4665, 4666, 4667]}
+{"event_id": 1072362, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2023-02-24 17:00:00", "end_date_time": "2023-02-24 19:00:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. Video broadcast on a Fresno TV station showed flooding at the intersection of Shields Ave. and Sunnyside Ave.", "ts_dict_index": [4824, 4825, 4826]}
+{"event_id": 1072368, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2023-02-24 18:49:00", "end_date_time": "2023-02-24 20:49:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported roadway flooding on east SR 180 at S. Reed Rd.", "ts_dict_index": [4818, 4819, 4820]}
+{"event_id": 1072354, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "MARIPOSA", "begin_date_time": "2023-02-24 12:50:00", "end_date_time": "2023-02-24 14:50:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported mud, dirt and rocks blocking the eastbound lane of SR 140 near the intersection of Hites Mine Rd.", "ts_dict_index": [4815, 4816, 4817]}
+{"event_id": 1072411, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-02-25 08:46:00", "end_date_time": "2023-02-25 10:46:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported roadway flooding at the intersection of Ave 400 and Rd. 140.", "ts_dict_index": [4821, 4822, 4823]}
+{"event_id": 1072406, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-02-25 08:18:00", "end_date_time": "2023-02-25 10:18:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported flooding on David Rd. between Wheeler Ridge Rd. and  Rancho Dr.", "ts_dict_index": [4812, 4813, 4814]}
+{"event_id": 876229, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2020-04-08 10:50:00", "end_date_time": "2020-04-09 08:00:00", "narrative": "The cold upper low pressure system that brought moderate to heavy precipitation across much of the area on April 5 and 6 was situated off the southern California coast on April 7 then tracked slowly northeast toward central California on April 8 and across the area on April 9. As a result, additional precipitation spread into Kern County during the evening of April 7 and spread northward across the area on April 8. This system produced periods of heavy rainfall across Kern County on April 8 where there were widespread reports of a half inch to an inch of rainfall which resulted in several instances of debris flows and nuisance roadway flooding. Further north, much of Fresno, Kings and Tulare Counties measured between a quarter and a half inch of liquid precipitation while areas north of Fresno County generally picked up between a tenth of an inch to a quarter inch of liquid precipitation. Several stations above 5500 feet in Kern and Tulare Counties picked up between 3 and 6 inches of new snowfall. The precipitation finally ended by the evening of April 9 as the low moved out of our area. California Highway Patrol reported roadway flooding along with rock and mud debris in Hart Park.", "ts_dict_index": [4701, 4702, 4703]}
+{"event_id": 1072353, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2023-02-24 12:26:00", "end_date_time": "2023-02-24 14:26:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported several sections of roadway flooded near the SR 33 and W. Elkhorn Ave. exchange.", "ts_dict_index": [4827, 4828, 4829]}
+{"event_id": 1065283, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 16:50:00", "end_date_time": "2023-01-10 17:00:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. Public reports posted on social media showing a funnel cloud south of Woodlake.", "ts_dict_index": [4845, 4846, 4847]}
+{"event_id": 798024, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-02-15 13:40:00", "end_date_time": "2019-02-15 13:40:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. Social media posts of a funnel cloud in Sanger at 1340 PST.", "ts_dict_index": [4860, 4861, 4862]}
+{"event_id": 826001, "event_type": "Funnel Cloud", "state": "TEXAS", "cz_name": "LIPSCOMB", "begin_date_time": "2019-05-07 17:56:00", "end_date_time": "2019-05-07 17:56:00", "narrative": "May 7th, 2019 was a very active day for significant severe weather which lasted from early morning into the evening.  A combination of an approaching strong upper level storm system that moved across Arizona into New Mexico, moderate to high levels of wind shear and moderate to high levels of instability led to the severe thunderstorm and tornadic events.  Thunderstorms that started in the late morning hours for the northwestern Texas/Oklahoma produced hail that was generally below 1 inch.  This activity drifted into the north central Texas and Oklahoma Panhandles by early afternoon.  ||Wind shear and large scale lift increased as an upper level disturbance continued to move east crossing Arizona into New Mexico in the the afternoon and evening hours.  As a result, supercell development increased as did storm intensity.  Maximum hail size increased from less than one inch to golf ball and eventually baseball size with the strongest storms.  Cooling produced by morning and early afternoon activity enhanced an existing weak surface boundary that extended across the south central Texas Panhandle northeastward into the eastern Oklahoma Panhandles.  Supercell thunderstorms that developed along and near this boundary began generating tornadoes due to the additional wind shear it produced.  In all, eight tornadoes formed across portions of the central and eastern Texas Panhandle into the early evening hours.  The storms eventually congealed into a line of thunderstorms across the far eastern Panhandles before moving east out the region during the late evening of the 7th.  In addition to the very large hail and tornadoes, severe wind gusts and localized flash flooding were all reported during this event across the Texas and Oklahoma Panhandles. Funnel cloud northwest of location and halfway down.", "ts_dict_index": [4848, 4849, 4850]}
+{"event_id": 798025, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-02-15 13:45:00", "end_date_time": "2019-02-15 13:45:00", "narrative": "A deep moisture plume moved through central California on February 13 and 14 as a strong low pressure system approached the area. Heavy rainfall and strong southerly winds impacted the area as this moisture moved through the area. Several reports of winds gusts exceeding 60 mph were reported and snow levels rose to near 9000 feet which resulted in widespread flooding in the area and several road closures from flooding and debris flows were reported. A strong cold front pushed through the area during the morning of February 15 which resulted in snow levels plummeting to around 5000 feet. Thunderstorms broke out in the colder and unstable post-frontal airmass and several reports of small hail were observed in the San Joaquin Valley. In addition, a small EF 0 tornado briefly touched down n ear Yosemite Lakes and funnel clouds were observed in the San Joaquin Valley. A colder system moved into the area on February 16 and snow levels lowered further down to 1500 feet. Low elevation snowfall on February 16 and 17 resulted in numerous road closures and travel delays and there were several reports of 10 to 20 inches of new snowfall reported in the Southern Sierra Nevada between the evening of February 15 and the evening of February 17. Rainfall totals between February 13 and February 17 were generally between 3 and 7 inches of liquid precipitation in the higher elevations of the Southern Sierra Nevada with 2 to 5 inches in the adjacent foothills. Much of the San Joaquin Valley picked up between a half inch and an inch and a half of rainfall during this period while the Tehachapi Mountains generally picked up between 1 to 2 inches of liquid precipitation during the 5 day period. An off duty NWS employee reported a funnel cloud on State Highway 43 between Hanford and Selma.", "ts_dict_index": [4857, 4858, 4859]}
+{"event_id": 982460, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2021-10-25 15:36:00", "end_date_time": "2021-10-25 15:46:00", "narrative": "A large upper level low pressure system in the Gulf of Alaska picked up an abundant amount of tropical moisture from the remains of Typhoon Namtheun on October 23.  This large upper low then dropped southeast to off the Pacific Northwest coast on during the morning of October 24 then underwent rapid intensification during the afternoon of October 24 resulting in a strong surge of deep tropical moisture being pushed into central California by the evening of October 24.  As the upper low tracked inland across the Pacific northwest on October 25, a cold front dropped southward through California bringing moderate to heavy precipitation to areas north of Kern County for 10-12 hours. Much of Yosemite National Park and Mariposa County picked up between 3 to 5 inches of liquid precipitation while 2 to 4 inches of liquid precipitation fell in the Sierra Nevada in Madera and Fresno Counties.  Further south, 1 to 2 inches of liquid precipitation fell in the mountains of Tulare County while the Kern County Mountains generally picked up between half and inch and an inch of rainfall.  Most of the San Joaquin Valley and West Side Hills also picked up between a half inch and an inch of rain while most of Merced County picked up between and inch to an inch and a half.  The Kern County Deserts also picked up between a quarter and a half inch of rainfall.  With most of the moisture from this system being of tropical origin, the snow level was above 9000 feet until the afternoon of October 25.  The snow level lowered to 6000 to 7000 feet before the precipitation ended during the evening of October 25.  Several SNOTEL stations measured between 9 and 15 inches of snow in 12 hours while a few stations above 9000 feet measured between 15 and 30 inches.  There were also several stations which measured peak wind gusts between 58 and 70 mph ahead of the storm during the morning of October 25 or behind the cold front during the evening of October 25.  Scattered thunderstorms developed over the San Joaquin Valley behind the cold front during the afternoon of October 25.  One supercell produced a funnel cloud over southwestern Kings County then moved southeast into Kern County bringing heavy rainfall to the Lost Hills and Wasco areas.  The precipitation tapered off by late  evening and winds diminished by the morning of October 26 as the storm moved to the east of the area. A TV station filmed a funnel cloud southwest of Lemoore.", "ts_dict_index": [4839, 4840, 4841]}
+{"event_id": 826003, "event_type": "Funnel Cloud", "state": "TEXAS", "cz_name": "LIPSCOMB", "begin_date_time": "2019-05-07 18:18:00", "end_date_time": "2019-05-07 18:18:00", "narrative": "May 7th, 2019 was a very active day for significant severe weather which lasted from early morning into the evening.  A combination of an approaching strong upper level storm system that moved across Arizona into New Mexico, moderate to high levels of wind shear and moderate to high levels of instability led to the severe thunderstorm and tornadic events.  Thunderstorms that started in the late morning hours for the northwestern Texas/Oklahoma produced hail that was generally below 1 inch.  This activity drifted into the north central Texas and Oklahoma Panhandles by early afternoon.  ||Wind shear and large scale lift increased as an upper level disturbance continued to move east crossing Arizona into New Mexico in the the afternoon and evening hours.  As a result, supercell development increased as did storm intensity.  Maximum hail size increased from less than one inch to golf ball and eventually baseball size with the strongest storms.  Cooling produced by morning and early afternoon activity enhanced an existing weak surface boundary that extended across the south central Texas Panhandle northeastward into the eastern Oklahoma Panhandles.  Supercell thunderstorms that developed along and near this boundary began generating tornadoes due to the additional wind shear it produced.  In all, eight tornadoes formed across portions of the central and eastern Texas Panhandle into the early evening hours.  The storms eventually congealed into a line of thunderstorms across the far eastern Panhandles before moving east out the region during the late evening of the 7th.  In addition to the very large hail and tornadoes, severe wind gusts and localized flash flooding were all reported during this event across the Texas and Oklahoma Panhandles. Late report of a funnel cloud southeast of Follett. Came down about half way to the ground and then lifted.  Only lasted a few minutes.", "ts_dict_index": [4851, 4852, 4853]}
+{"event_id": 962310, "event_type": "Funnel Cloud", "state": "ARKANSAS", "cz_name": "CLARK", "begin_date_time": "2021-06-07 13:35:00", "end_date_time": "2021-06-07 13:35:00", "narrative": "Hit and miss thunderstorms ramped up on the 6th. Two to more than three inches of rain was measured at Cane Creek State Park (Lincoln County), Fordyce (Dallas County), Monticello (Drew County), Nashville (Howard County), and Pine Bluff (Jefferson County). Several roads were under water between Avilla (Saline County) and Ferndale (Pulaski County), and also at Monticello (Drew County).||During the predawn hours of the 7th, thunderstorm winds downed a tree on Highway 53 just south of Gurdon (Clark County). This caused a log truck to overturn. In the afternoon, more trees were toppled in Camden and East Camden (both in Ouachita County). A chapel roof was damaged just southwest of Cummins (Lincoln County), and part of a roof was blown off close to Sorrells (Jefferson County).||At least a dozen Tornado Warnings were issued in portions of Calhoun, Clark, Cleveland, Dallas, Garland, Hot Spring, Montgomery, Ouachita, and Pike Counties. A funnel cloud was spotted by law enforcement at Gum Springs (Clark County). There was a brief tornado reported (rated EFU, where U is unknown because there was no damage to evaluate) to the west of Calion (Union County) at 426 pm CDT. The tornado apparently did little more than kick up some dust.||On the 8th, there was a life threatening deluge in southeast Arkansas. Showers and thunderstorms became widespread, and moved over the same areas for several hours.||Too much rain flooded roads at Star City and Varner (both in Lincoln County), Pine Bluff (Jefferson County), Stuttgart (Arkansas County), and also at Dumas and McGehee (both in Desha County). Water got into many homes. Crop and road damage (washouts) was reported in Bradley County. A creek was out of its banks just southeast of Timber Ridge (Pulaski County).||There was high water along Highway 114 between Calmer and Rison (both in Cleveland County), Highway 425 near Yorktown (Lincoln County), Highway 293 east of Garrett Bridge (Lincoln County), Highway 46 not far from Ebb (Grant County), Highway 276 on the south side of Stuttgart (Arkansas County), and Highway 1 at Kelso (Desha County). These highways were eventually closed temporarily.||The situation was the most serious in Desha and Drew Counties, and a Flash Flood Emergency was issued for the communities of Dumas, Pickens, Rohwer (all in Desha County), and Winchester (Drew County) at 1142 am CDT on the 8th. Radar estimated 10 to more than 15 inches of rain, and there was water everywhere. Some folks indicated (through social media) they had never witnessed flooding of this magnitude.||From an historic perspective, Rohwer (Desha County) received 9.25 inches of rain in the twenty four hour period ending at 700 am CDT on the 8th. This was the most rain in one day at the site, and the fourth largest one day total across the state in June. If that was not enough, 9.97 inches of liquid was measured the next day! Adding the numbers, the whopping 19.22 inches on the 8th/9th was the second biggest two day amount in Arkansas. It was just behind the 21.45 inches at Danville (Yell County) on December 3-4, 1982.||Relentless cloudbursts continued to start the 9th in eastern Arkansas. A rain gauge near DeValls Bluff (Prairie County) completely filled (to six inches) between 400 am and 700 am CST. Buildings were flooded and cars were stalled in Clarendon (Monroe County). It was the same story in Humnoke (Lonoke County), and sandbags were ordered to stop the water.||It was just getting worse in Stuttgart (Arkansas County), with one picture showing more water in a home than ever before (in the life of the photographer/42 years). That claim was likely true because the 7.50 inches of rain that caused the problem easily surpassed the previous one day June record of 4.07 inches on the 29th in 1939. At least fifteen homes were impacted by flooding at Altheimer (Jefferson County). Highway 302 from Highway 17 to Highway 79 was shut down in Monroe County, as was Highway 15 near Sherrill (Jefferson County), Highway 33 east of Tollville (Prairie County), and Highways 85 and 318 near Oneida (Phillips County).||As the weather calmed down in the east by the afternoon of the 9th, temperatures warmed well into the 80s to around 90 degrees across the northern and central counties. Heating and lots of humidity were enough to fuel isolated strong to severe storms toward evening.||Just after 700 pm CDT, a video showed a tornado (rated EFU) that lasted two minutes in a field near Blakemore (Lonoke County). Between 700 pm and 800 pm CDT, there was quarter size hail just east of College Station (Pulaski County). Little Rock (Pulaski County) got a quick 1.10 inches of rain. Trees were blown down at Cave City (Sharp County). At 805 pm CDT, there was a brief weak tornado (rated EF0) a few miles southeast of England (Lonoke County).||The focus shifted back to the southeast early on the 10th. You guessed it...the sky was falling again. Rain plus runoff from the soaking on the 8th/9th in northern and central Desha County inundated farms toward Halley (Desha County) in the south. At 200 pm CDT, an irrigation canal east of Pickens (Desha County) was breached, and adjacent farmland became a lake. The canal was patched by evening. At Florence (Drew County), residents were forced to use boats to get around. Water threatened structures at Dermott and Eudora (both in Chicot County), and sandbagging was in progress. It was clear that assistance was needed, and Arkansas Governor Asa Hutchinson declared a state of emergency. ||All was quiet quiet in Little Rock (Pulaski County) on the 10th, and the sun was out. For the first time in 2021, the temperature touched 90 degrees (the high was 92 degrees), and it was three weeks late (it normally happens by May 18th). Toward evening, it got loud toward Pinnacle Mountain (Pulaski County). A severe storm pumped out quarter size hail, winds strong enough to push over a few trees, and up to six inches of rain in less than two hours. The terrain accentuated the flow of water across roads and into neighborhoods. An Arkansas State Trooper reported a funnel cloud at Gum Springs south of Highway 26.", "ts_dict_index": [4836, 4837, 4838]}
+{"event_id": 1072421, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-02-25 19:51:00", "end_date_time": "2023-02-25 21:51:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported Mount Vernon Ave at Niles St. in Bakersfield were flooded.", "ts_dict_index": [4833, 4834, 4835]}
+{"event_id": 1072405, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2023-02-25 08:17:00", "end_date_time": "2023-02-25 10:17:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. PG&E reported a fallen telephone pole on Edison Rd. between Sandrini Rd. and David Rd.", "ts_dict_index": [4830, 4831, 4832]}
+{"event_id": 880424, "event_type": "Funnel Cloud", "state": "TEXAS", "cz_name": "TITUS", "begin_date_time": "2020-04-24 19:00:00", "end_date_time": "2020-04-24 19:00:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Numerous reports of large hail were reported from these storms, with some isolated instances of damaging winds and funnel clouds across portions of Northeast Texas. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening, thus ending the severe threat for Northeast Texas with the cold frontal passage. A rapidly rotating funnel cloud was observed near Talco.", "ts_dict_index": [4863, 4864, 4865]}
+{"event_id": 1072357, "event_type": "Flood", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-02-24 13:11:00", "end_date_time": "2023-02-24 15:11:00", "narrative": "A large cold upper low pressure system dropped slowly southward off the California coast on February 24 and 25. This system brought 1.5 to 3 inches of liquid precipitation between the early morning of February 24 and the late morning of February 25 to the Sierra Nevada and adjacent foothills as well as to the Tehachapi Mountains and the San Joaquin Valley. This was a cold storm with snow levels lowering from around 3000 feet during the morning of February 24 lowering to 1500 to 2000 feet during the morning of February 25 with some locations near 1000 feet picking up some light snowfall while higher elevations generally picked up between 2 and 4 feet of new snowfall. The snowfall resulted in several mountain roads being closed for extended periods of time. In addition several reports of flooding were observed in the San Joaquin Valley and the lower Sierra foothills resulting in additional road closures. The low moved across southern California during the evening of February 25 and east of the area during the morning of February 26. California Highway Patrol reported a vehicle spun out on SR 198 and became stuck in mud at the SR 198 and Plaza Dr. offramp.", "ts_dict_index": [4797, 4798, 4799]}
+{"event_id": 880426, "event_type": "Funnel Cloud", "state": "TEXAS", "cz_name": "TITUS", "begin_date_time": "2020-04-24 19:05:00", "end_date_time": "2020-04-24 19:05:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Numerous reports of large hail were reported from these storms, with some isolated instances of damaging winds and funnel clouds across portions of Northeast Texas. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening, thus ending the severe threat for Northeast Texas with the cold frontal passage. A rotating wall cloud was observed about 4 miles north of Mount Pleasant.", "ts_dict_index": [4866, 4867, 4868]}
+{"event_id": 880420, "event_type": "Funnel Cloud", "state": "TEXAS", "cz_name": "TITUS", "begin_date_time": "2020-04-24 19:05:00", "end_date_time": "2020-04-24 19:05:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Numerous reports of large hail were reported from these storms, with some isolated instances of damaging winds and funnel clouds across portions of Northeast Texas. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening, thus ending the severe threat for Northeast Texas with the cold frontal passage. A visual report of a rotating wall cloud was received west of Mount Pleasant High School.", "ts_dict_index": [4869, 4870, 4871]}
+{"event_id": 1065282, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2023-01-10 16:36:00", "end_date_time": "2023-01-10 16:46:00", "narrative": "A strong low pressure system moved through central California on January 9 and 10. This system picked up a deep moisture fetch of tropical origin while tracking rapidly eastward across the Pacific and produced widespread heavy precipitation across the area between the morning of January 9 and the evening of January 10 while the deep surge of moisture moved inland across central California. This storm produced widespread liquid precipitation totals of 3 to 6 inches in the Sierra Nevada. For much of this event, the snow level was around 7500 feet which resulted in heavy runoff of snow accumulations from recent colder storms. This runoff combined with rainfall of 2 to 4 inches in the Sierra foothills and 1 to 2.5 inches in the San Joaquin Valley to produce widespread flooding across the area with at least 150 separate incidents of flooding being reported to the Hanford NWS office. The flooding resulted in numerous roads being closed and several evacuations took place including the entire town of Planada in Merced County which was inundated with flood waters. In addition, Bear Creek overflowed it's banks and reached a new record peak flood of 26.2 feet at McKee Bridge east of Merced on January 10. Above the snow line, there were several reports of 2 to 4 feet of new snowfall above 7500 feet in the Sierra Nevada. This system also produced strong downslope winds on January 9 with several stations in the Tehachapi Mountains, West Side Hills and Sierra foothills measuring gusts exceeding 60 mph and resulting in several power outages across the area as power lines were blown down by the strong winds. Thunderstorms broke out across the much of the area on January 10 as colder air aloft moved over the area resulting in numerous issuances of Significant Weather Advisories along with a few warnings. The storm moved to the east of the area on January 11 with precipitation ending and winds diminishing. However, flooding continued across much of the area due to residual runoff from the heavy precipitation that fell over the previous two days. Several county Emergency Operations Centers were staffed by NWS personnel during this event do to the unusual severity with this storm as numerous warnings were issued for flooding, strong winds and heavy mountain snowfall. A trained spotter sent a video of rotating clouds in Woodlake which was confirmed by rotation indicated by radar.", "ts_dict_index": [4842, 4843, 4844]}
+{"event_id": 858710, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2019-11-28 13:35:00", "end_date_time": "2019-11-28 13:40:00", "narrative": "A cold low pressure system dropped southeast out of the Gulf of Alaska on during the morning of November 26 and dropped southward to the Pacific Northwest coast by the afternoon of the 26th. The low continued to drop southward off the California coast during the morning of November 27 spreading widespread precipitation into central California which continued through the late morning of November 28 which being Thanksgiving Day the storm adversely impacted holiday travel as several major roads were impacted. As this system was a cold storm, snow levels were between 2000 and 2500 feet with widespread accumulating snow taking place across the southern Sierra foothills where many locations above 2500 feet picked up between 5 and 10 inches of snow and the Kern County Deserts where several which picked up between 3 and 8 inches at most locations. Much of the higher Sierra above 7000 feet picked up between 18 and 36 inches of new snow. Most of the San Joaquin Valley picked up between a quarter and half an inch of rain while a few locations which were impacted by thunderstorms picked up close to an inch of rainfall. The most noticeable impacts from this storm were closures of Interstate 5 between Grapevine and Tajon Pass and State Route 58 in the Tehachapi area due to heavy snowfall and several accidents. In addition to the widespread precipitation and low elevation snowfall, thunderstorms produced locally heavier rainfall and small hail across the San Joaquin Valley during the afternoon and early evenings of both days. Video posted on twitter showed a funnel cloud over El Nido.", "ts_dict_index": [4878, 4879, 4880]}
+{"event_id": 858709, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-11-27 15:53:00", "end_date_time": "2019-11-27 15:58:00", "narrative": "A cold low pressure system dropped southeast out of the Gulf of Alaska on during the morning of November 26 and dropped southward to the Pacific Northwest coast by the afternoon of the 26th. The low continued to drop southward off the California coast during the morning of November 27 spreading widespread precipitation into central California which continued through the late morning of November 28 which being Thanksgiving Day the storm adversely impacted holiday travel as several major roads were impacted. As this system was a cold storm, snow levels were between 2000 and 2500 feet with widespread accumulating snow taking place across the southern Sierra foothills where many locations above 2500 feet picked up between 5 and 10 inches of snow and the Kern County Deserts where several which picked up between 3 and 8 inches at most locations. Much of the higher Sierra above 7000 feet picked up between 18 and 36 inches of new snow. Most of the San Joaquin Valley picked up between a quarter and half an inch of rain while a few locations which were impacted by thunderstorms picked up close to an inch of rainfall. The most noticeable impacts from this storm were closures of Interstate 5 between Grapevine and Tajon Pass and State Route 58 in the Tehachapi area due to heavy snowfall and several accidents. In addition to the widespread precipitation and low elevation snowfall, thunderstorms produced locally heavier rainfall and small hail across the San Joaquin Valley during the afternoon and early evenings of both days. Fresno Television Station reported a funnel cloud over Dinuba.", "ts_dict_index": [4881, 4882, 4883]}
+{"event_id": 937252, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2021-03-10 15:30:00", "end_date_time": "2021-03-10 15:45:00", "narrative": "A slow moving cold upper low pressure system which had originated in the Gulf of Alaska that was off the Pacific Northwest coast during the morning of March 9 dropped southeast into northwest California on March 10 and dropped further southeast into central California on March 11. This system did produce a period of moderate to locally heavy snowfall between the evening of March 9 and the early morning of March 11 over the Sierra Nevada as well as the adjacent foothills where snow levels lowered to near 2500 feet. Much of the mountains and foothills received a half inch to an inch of liquid precipitation from this system. Most stations above 7000 feet picked up between 12 to 18 inches of new snowfall while 5 to 10 inches of snow fell at many locations in between 3000 and 7000 feet. Only a few inches of snow fell in the Tehachapi Mountains, but travel was briefly impacted on Interstate 5 over the Tejon Pass and State Route 58 in thye Tehachapi area due to black ice during the morning of March 11. Much of the San Joaquin Valley picked up between a quarter inch and a half inch of rainfall while rain shadowing limited much of the Kern County Deserts to a tenth of an inch or less. Several strong thunderstorms developed in the San Joaquin Valley during the afternoon of March 10 producing heavy rainfall and pea sized hail. A funnel cloud was briefly observed near Hanford with one of the strong thunderstorms. The low finally moved east of the area on March 12 leaving a cool airmass over the area as it moved out. A Fresno television station observed a funnel cloud south of Hanford while a thunderstorm was in progress.", "ts_dict_index": [4884, 4885, 4886]}
+{"event_id": 858540, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-11-27 11:19:00", "end_date_time": "2019-11-27 11:24:00", "narrative": "A cold low pressure system dropped southeast out of the Gulf of Alaska on during the morning of November 26 and dropped southward to the Pacific Northwest coast by the afternoon of the 26th. The low continued to drop southward off the California coast during the morning of November 27 spreading widespread precipitation into central California which continued through the late morning of November 28 which being Thanksgiving Day the storm adversely impacted holiday travel as several major roads were impacted. As this system was a cold storm, snow levels were between 2000 and 2500 feet with widespread accumulating snow taking place across the southern Sierra foothills where many locations above 2500 feet picked up between 5 and 10 inches of snow and the Kern County Deserts where several which picked up between 3 and 8 inches at most locations. Much of the higher Sierra above 7000 feet picked up between 18 and 36 inches of new snow. Most of the San Joaquin Valley picked up between a quarter and half an inch of rain while a few locations which were impacted by thunderstorms picked up close to an inch of rainfall. The most noticeable impacts from this storm were closures of Interstate 5 between Grapevine and Tajon Pass and State Route 58 in the Tehachapi area due to heavy snowfall and several accidents. In addition to the widespread precipitation and low elevation snowfall, thunderstorms produced locally heavier rainfall and small hail across the San Joaquin Valley during the afternoon and early evenings of both days. Several photos and a video were posted of a cold air funnel cloud northeast of Goshen.", "ts_dict_index": [4875, 4876, 4877]}
+{"event_id": 802322, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-03-08 10:25:00", "end_date_time": "2019-03-08 10:35:00", "narrative": "Following the departure of the warm and very moist system which brought heavy rain to portions of the area on March 6, a cold upper trough approached the area on March 7 and moved through the region during the morning of March 8. This system provided additional liquid precipitation totals of half an inch to an inch over much of the southern Sierra Nevada with the snow level lowering from 5000 feet during the evening of March 7 to 3500 feet by the afternoon of March 8. While precipitation amounts were generally lower in the San Joaquin Valley and the Kern County Mountains, a few locations impacted by heavier showers or thunderstorms on March 8 received over half an inch. Several locations in the higher elevations of the southern Sierra Nevada (above 7000 feet) picked up between 6 an 12 inches of new snow between the evening of March 7 and the afternoon of March 8. There were some reports of funnel clouds in the San Joaquin Valley although there were no confirmed reports of tornadoes from this system. There were several reports of wind gusts exceeding 45 mph in the Kern County Mountains and Deserts and a few low impact indicator sites measured gusts exceeding 70 mph. This cold system moved out of the area during the evening of March 8 with a drier airmass moving into the area behind it. Several media reports of a cold air funnel northwest of Porterville.", "ts_dict_index": [4911, 4912, 4913]}
+{"event_id": 813467, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2019-05-16 10:34:00", "end_date_time": "2019-05-16 10:39:00", "narrative": "A cold upper low pressure center dropped southeast out of the Gulf of Alaska on May 15 and moved into northern California on May 16. A strong cold front associated with this system crossed central California during the afternoon and evening of May 16 which produced significant precipitation across the area. Several stations in the Sierra Nevada range above 6000 feet from Yosemite Park southward picked up between 6 and 12 inches of new snow. Below 6000 feet, much of the central Sierra and adjacent foothills picked up between 1 and 2 inches of rainfall while Sequoia Park area generally picked up between 0.75 and 1.5 inches of rain. Between a half inch and an inch of rain fell in the Merced and Fresno areas while several other stations in the San Joaquin Valley picked up between a quarter and a half inch of rain. In addition to the precipitation, strong winds impacted the Kern County Mountains near Tehachapi and Lake Isabella between the afternoon of May 16 and the morning of May 17. Several stations measured gusts above 45 mph and a few low impact indicator sites reported gusts above 60 mph. Reports on social media from a storm chaser with pictures of a funnel cloud near Kettlemen City.", "ts_dict_index": [4920, 4921, 4922]}
+{"event_id": 805350, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2019-03-27 13:35:00", "end_date_time": "2019-03-27 13:40:00", "narrative": "A low pressure system moved into Northern California during the morning of March 27 then dropped southeast during the afternoon resulting in increasing precipitation coverage across the area. The precipitation was most significant in Merced and Mariposa Counties which were impacted by the deeper moisture associated with this system as well as the unstable airmass behind the cold front which moved over central California during the day. Afternoon showers and thunderstorms increased in coverage during the late afternoon producing locally heavy rainfall as well as pea sized hail and a few funnel clouds. Much of the Southern Sierra Nevada north of Kings Canyon picked up between a half inch and an inch of liquid precipitation while while areas near Yosemite National Park picked up between one and two inches. Between a tenth and a quarter inch of rain fell across much of the central San Joaquin Valley with locally heavier amounts in areas impacted by thunderstorms. The precipitation fell as snow above 7500 feet and a few locations in Yosemite Park picked up around a foot of fresh snowfall above 8000 feet. Areas south of Fresno County generally did not receive much precipitation. The precipitation tapered off during the evening of March 27 and ended by late morning on March 28 as the storm moved east of the area. KFSN TV-30 called in with a report of a funnel cloud west of Merced on State Route 140 at 1435 PDT. NWS received clear photo evidence of a funnel cloud. Location was estimated by radar.", "ts_dict_index": [4899, 4900, 4901]}
+{"event_id": 881936, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2020-05-18 16:43:00", "end_date_time": "2020-05-18 16:45:00", "narrative": "A low pressure system dropped southward off the northern California coast on May 17 than moved inland across central California on May 18. As a result, precipitation spread southward across the area north of Fresno County during the evening of May 17 and became widespread across our area on May 18. Several stations in the Sierra Nevada picked up between an inch and 2.50 inches of liquid precipitation while a few stations from Madera County northward picked up between 2.50 and 3.25 inches of liquid precipitation. Snow levels were between 8000 to 9000 feet early on, but lowered to around 6000 feet by the afternoon of May 18. Several higher elevation SNOTEL stations picked up between 2 and 6 inches of new snowfall while a few stations picked up 7 inches or more. As a cooler airmass pushed into the area during the afternoon of May 18, thunderstorms developed during the afternoon. One thunderstorm produced nuisance roadway flooding near Riverdale while another produced nuisance roadway flooding near Parlier. A third thunderstorm produced a funnel cloud near North Fork. Finally, This system produced a period of strong winds over the Kern County Deserts as well as over the Lake Isabella and Tehachapi areas between the evening of May 18 and the morning of May 19.  Several stations in these areas reported wind gusts between 45 and 60 mph. A few low impact indicator sites reported gusts between 60 and 70 mph. The winds diminished by late morning on May 19 as the storm moved out of the area. Public observation of a funnel cloud near North Fork.", "ts_dict_index": [4887, 4888, 4889]}
+{"event_id": 815482, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-05-26 13:20:00", "end_date_time": "2019-05-26 13:20:00", "narrative": "A strong upper low pressure system pushed southward through the Pacific Northwest on May 25. Warm air advection ahead of this system produced instability over the San Joaquin Valley during the afternoon and evening of May 25 which resulted in the development of scattered thunderstorms. One thunderstorm produced nickel sized hail between Mettler and Maricopa along State Route 166 and also produced roadway flooding in the area. The low moved southward through California on May 26 bringing increased clouds, significant rainfall and mountain snowfall, locally strong winds as well as thunderstorms with heavy rain. Much of the area received between a quarter and three quarters of an inch of liquid precipitation while several stations in the Sierra Nevada picked up between 2 to 5 inches of new snowfall with a few stations picking up 6 to 7 inches. Thunderstorms developed during the afternoon of May 26 across the San Joaquin Valley producing heavy rainfall, roadway flooding and a few funnel clouds. In addition, gusty winds prevailed for much of the day in the Tehachapi and Lake Isabella areas where there were several reports of wind gusts exceeding 35 mph while a few low impact indicator sites measured gusts above 55 mph. Several all time daily record precipitation records were shattered on May 26. Posts on Facebook and Twitter of a funnel cloud near Tipton.", "ts_dict_index": [4902, 4903, 4904]}
+{"event_id": 801342, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2019-03-06 13:50:00", "end_date_time": "2019-03-06 14:00:00", "narrative": "A strong and very moist upper low pressure system approached the central California coast on March 5. This system pulled up a deep fetch of moisture of sub-tropical origin which pushed into the area during the evening of March 5 then stalled over the southern portion of central California during the morning of March 6 as a strong southwest upper jet was overhead. This resulted in widespread heavy precipitation over Kern County with moderate to locally heavy precipitation further north over an already saturated ground producing widespread flooding, debris flows, rock slides and mud slides across the area. Several roads were closed as a result of the flooding. Thunderstorms broke out during the afternoon producing additional moderate to locally heavy rainfall. Much of the Southern Sierra Nevada picked up between 2 and 4 inches of liquid precipitation with the snow level running between 8000 and 8500 feet for much of the event. Between 1 to 3 inches of rain fell in the adjacent foothills and across the Kern County Mountains. Kelso Creek to the southeast of Lake Isabella filled up that a potential levee breach led to an evacuation of the communities of Weldon Valley Ranchos, Valley Estates and Power Tracts within the town of Kelso Creek. State Route 178 was closed in Kern Canyon for two days due to a rock slide. Much of the San Joaquin Valley and Kern County Deserts picked up between a half inch and an inch of rain while locally heavier amounts fell in the south end of the San Joaquin Valley and across the Indian Wells Valley, and as a result road flooding was widespread in Kern County. A storm chaser filmed a funnel cloud 9 miles northeast of Madera and shared with broadcast media and NWS.", "ts_dict_index": [4872, 4873, 4874]}
+{"event_id": 860402, "event_type": "Funnel Cloud", "state": "FLORIDA", "cz_name": "ST. JOHNS", "begin_date_time": "2019-12-14 05:20:00", "end_date_time": "2019-12-14 05:20:00", "narrative": "On Friday, 13 December 2019, a warm front lifted and lingered across northeast Florida with surface dew points rising into the mid to upper 60s generally along and south of a line from St. Augustine to Gainesville. A strong upper level trough deepened across the central Gulf Coast region with a resultant surface low positioned over the northeast Gulf of Mexico coast just south of Panama City that evening around 10 pm EST. As the upper level trough axis started to lift and becoming positively tilted overnight into 14 December, the surface low edge farther east northeast and tracked over southeast Georgia then offshore of the local Atlantic coast through 4 am EST. The corridor of unstable low-level air remained across our southern Florida zones with surface-based CAPE values rising into the 1000-1300 J/kg range per LAPS analysis while aloft strong directional (0-6 km) bulk shear near the mid/upper level trough axis increased to 50-70 kts. The phased low-level instability, plentiful deep layer moisture and strong dynamical lift under the upper low and just south of the surface low spawned a couple of persistent supercells with long-lived mesocyclones. A funnel cloud was reported over 762 Gilda Drive.", "ts_dict_index": [4917, 4918, 4919]}
+{"event_id": 802321, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "KINGS", "begin_date_time": "2019-03-07 17:10:00", "end_date_time": "2019-03-07 17:20:00", "narrative": "Following the departure of the warm and very moist system which brought heavy rain to portions of the area on March 6, a cold upper trough approached the area on March 7 and moved through the region during the morning of March 8. This system provided additional liquid precipitation totals of half an inch to an inch over much of the southern Sierra Nevada with the snow level lowering from 5000 feet during the evening of March 7 to 3500 feet by the afternoon of March 8. While precipitation amounts were generally lower in the San Joaquin Valley and the Kern County Mountains, a few locations impacted by heavier showers or thunderstorms on March 8 received over half an inch. Several locations in the higher elevations of the southern Sierra Nevada (above 7000 feet) picked up between 6 an 12 inches of new snow between the evening of March 7 and the afternoon of March 8. There were some reports of funnel clouds in the San Joaquin Valley although there were no confirmed reports of tornadoes from this system. There were several reports of wind gusts exceeding 45 mph in the Kern County Mountains and Deserts and a few low impact indicator sites measured gusts exceeding 70 mph. This cold system moved out of the area during the evening of March 8 with a drier airmass moving into the area behind it. An NWS employee spotted a funnel cloud 4N Hanford which remained well above the ground.", "ts_dict_index": [4908, 4909, 4910]}
+{"event_id": 816142, "event_type": "Funnel Cloud", "state": "NEW MEXICO", "cz_name": "UNION", "begin_date_time": "2019-05-26 15:50:00", "end_date_time": "2019-05-26 15:55:00", "narrative": "A potent upper level storm system approaching New Mexico from the west interacted with deep moisture and very unstable conditions along a sharp dryline over eastern New Mexico on May 26, 2019. Dry showers and thunderstorms with strong downburst winds first developed along the Continental Divide by late morning before marching east into the Rio Grande Valley through the afternoon. Several locations within the Rio Grande Valley reported wind gusts in excess of 60 mph, including Los Lunas, Albuquerque, Santa Fe, and Taos. Wind damage was also reported as this activity moved across the central mountain chain into the Estancia Valley. Meanwhile, showers and thunderstorms fired up along the dryline in eastern New Mexico then quickly became severe with large hail, high winds, and several tornados. A violent supercell thunderstorm that moved through Union County during the late afternoon produced at least two tornadoes and three inch hail. Severe thunderstorms then evolved into a quasi-linear convective system over the Caprock region and resulted in a large area of high winds and large hail. Several more tornadoes developed along the southern edge of this line, including a spectacular wedge tornado near Dora. In addition to all the severe thunderstorms that impacted the region, many areas outside of thunderstorm activity in central and western New Mexico also reported strong southwest winds with gusts of 50 to 60 mph. A funnel cloud was spotted along U.S. 56 south of Mount Dora.", "ts_dict_index": [4893, 4894, 4895]}
+{"event_id": 815481, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-05-26 12:25:00", "end_date_time": "2019-05-26 12:25:00", "narrative": "A strong upper low pressure system pushed southward through the Pacific Northwest on May 25. Warm air advection ahead of this system produced instability over the San Joaquin Valley during the afternoon and evening of May 25 which resulted in the development of scattered thunderstorms. One thunderstorm produced nickel sized hail between Mettler and Maricopa along State Route 166 and also produced roadway flooding in the area. The low moved southward through California on May 26 bringing increased clouds, significant rainfall and mountain snowfall, locally strong winds as well as thunderstorms with heavy rain. Much of the area received between a quarter and three quarters of an inch of liquid precipitation while several stations in the Sierra Nevada picked up between 2 to 5 inches of new snowfall with a few stations picking up 6 to 7 inches. Thunderstorms developed during the afternoon of May 26 across the San Joaquin Valley producing heavy rainfall, roadway flooding and a few funnel clouds. In addition, gusty winds prevailed for much of the day in the Tehachapi and Lake Isabella areas where there were several reports of wind gusts exceeding 35 mph while a few low impact indicator sites measured gusts above 55 mph. Several all time daily record precipitation records were shattered on May 26. Posts on Facebook and Twitter with pictures of a funnel cloud between Shafter and Wasco.", "ts_dict_index": [4905, 4906, 4907]}
+{"event_id": 795408, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2019-02-02 15:45:00", "end_date_time": "2019-02-02 15:55:00", "narrative": "A strong upper low pressure system approached the central California coast during the morning of February 2. Ahead of the low, strong southerly winds impacted the Grapevine area along Interstate 5 for much of the morning. By late morning the strong winds spread northward into the Bakersfield area where there were numerous reports of downed trees and wind damage. As the main low moved inland during the day, moderate to heavy precipitation spread into area and produced several instances of roadway and nuisance flooding. Scattered thunderstorms brought additional rainfall and small hail to the San Joaquin Valley and southern Sierra foothills during the late afternoon. One thunderstorm produced a brief small tornado south of Mariposa. Several stations in the San Joaquin Valley picked up over an inch of rain while several stations in the mountains measured  between 2 and 5 inches of liquid precipitation. The precipitation fell mainly as snow above 5000 feet where heavy snowfall was reported at several stations and several feet of new snowfall was estimated at several SNOTELS from this storm and the following storm which moved through the area on February 4 and 5. Several photos were posted on Facebook of a funnel cloud near the intersection of State Route 99 and Sandrini Road.", "ts_dict_index": [4914, 4915, 4916]}
+{"event_id": 873366, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "KERN", "begin_date_time": "2020-03-25 17:15:00", "end_date_time": "2020-03-25 17:15:00", "narrative": "An unsettled pattern continued over central California between March 20 and March 29 with a mean upper trough over the state and several impulses moving through the area. One system produced moderate to locally heavy precipitation across much of the area on March 22 and March 23 with several stations measuring between a half an inch and an inch of liquid precipitation. The precipitation mainly fell as snow over the Sierra Nevada above 7000 feet with several reporting stations picking up between 8 and 12 inches of new snowfall. Another system moved through on March 25 and March 26 which produced locally strong wind gusts above 45 mph during the morning of March 25, and widespread showers and scattered thunderstorms during the afternoon of March 25. Rainfall totals generally ranged from a quarter inch to a half inch to a half inch of rainfall with widespread snowfall totals of 4 to 8 inches being observed above 6000 feet and as much as 2 inches of new snowfall down to 4000 feet. Some of the thunderstorms on March 25 produced pea sized hail and localized street flooding. In addition, a funnel cloud was briefly observed east of Bakersfield. One more system moved through the area during the morning of March 29 producing an additional tenth to a quarter inch of liquid precipitation over the Sierra Nevada and up to a tenth of an inch of rainfall elsewhere across the area. Video relayed by a Bakersfield television station showed a funnel cloud near Rio Bravo Country Club.", "ts_dict_index": [4896, 4897, 4898]}
+{"event_id": 859405, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-12-08 14:10:00", "end_date_time": "2019-12-08 14:15:00", "narrative": "An upper trough slowly moved across California during the weekend of December 7 and 8 producing widespread precipitation across the area. The heaviest precipitation occurred from Fresno County northward where several stations in the Sierra measured between 1 and 2 inches of liquid precipitation while several stations in the valley measured between a half inch and an inch of rainfall. Further south, much of Kings and Tulare Counties picked up between a quarter inch and a half inch of precipitation and most stations in Kern County picking up less than a quarter inch of rainfall. The snow level ranged between 7000 and 8000 feet for most of this event with several locations in the higher Sierra picking up between 8 ans 12 inches of new snowfall over the weekend. In addition the rain and mountain snowfall, scattered thunderstorms produced some areas of locally heavy rainfall, roadway flooding and small hail from the late morning the early evening of December 8. The precipitation ended by late evening as the trough moved to the east of the area. Public report with photo posted on Twitter of a funnel cloud west of Lemoore NAS.", "ts_dict_index": [4926, 4927, 4928]}
+{"event_id": 1015798, "event_type": "Funnel Cloud", "state": "IOWA", "cz_name": "CASS", "begin_date_time": "2022-03-05 15:55:00", "end_date_time": "2022-03-05 15:55:00", "narrative": "On March 5, 2022 a total of 15 tornadoes occurred across the state of Iowa as a warm front lifted across the area. Supercells initially developed across southwest Iowa in the vicinity of the triple point of the surface low with strong, rotating updrafts. Longevity was initially lacking with the storms, producing funnel clouds, brief tornadoes, and hail in southwest Iowa. As the cells moved northeast and matured, larger hail began to fall with golf ball sized hail falling in Adams county and baseball sized hail into Adair county. Following this period of large hail the storms produced a tornado which would remain on the ground for just over 70 miles, carving a path across central Iowa from southwest of Winterset to just northeast of Newton. The tornado peaked in Winterset, Iowa, producing EF-4 damage with wind speeds estimated near 170 mph. The tornado continued across the southern portion of the Des Moines metro area and to Newton. This is the furthest north EF-4 tornado in the CONUS this early in the year on record, the first EF-4 tornado in Iowa since October 4, 2013 which occurred in Woodbury and Cherokee Counties, and is the second longest tornado in Iowa since 1980, behind the longest occurring on June 7, 1984 at a length of 117 miles across southern Iowa. As the storm skimmed the southern Des Moines metro, cells across south central became tornadic, producing several destructive tornadoes including an EF-3 tornado in Chariton, Iowa. This heartbreaking day resulted in seven fatalities, six in Winterset and one in Chariton, making it the deadliest tornado outbreak in Iowa since 2008. At 15 tornadoes, this is also one of the earliest outbreaks of this magnitude to occur so early in the season. Multiple storm chaser reports of a funnel cloud southeast of Cumberland, IA.", "ts_dict_index": [4854, 4855, 4856]}
+{"event_id": 802792, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-03-20 16:46:00", "end_date_time": "2019-03-20 16:51:00", "narrative": "A slow moving low pressure system near the California coast spread moisture inland during the evening of March 19 and the morning of March 20. This produced a band of mainly light rainfall which was most noticeable north of Fresno County. Skies cleared out in the San Joaquin Valley during the afternoon of March 20 and with a post-frontal unstable airmass present, thunderstorms broke out in the valley during the afternoon through the early evening. The thunderstorms produced some locally heavy rainfall and there were a few reports of flooding in Tulare County with a road washed out near Woodlake. There were also a few reports of funnel clouds which were posted online. Most locations in the San Joaquin Valley picked up a tenth to a third of an inch of rainfall while many locations in the Southern Sierra Nevada picked up between a third of an inch to an inch of liquid precipitation with locally higher amounts measured at a few stations. Pictures posted on Twitter of a funnel cloud east of Woodlake.", "ts_dict_index": [4944, 4945, 4946]}
+{"event_id": 802797, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-03-20 17:10:00", "end_date_time": "2019-03-20 17:10:00", "narrative": "A slow moving low pressure system near the California coast spread moisture inland during the evening of March 19 and the morning of March 20. This produced a band of mainly light rainfall which was most noticeable north of Fresno County. Skies cleared out in the San Joaquin Valley during the afternoon of March 20 and with a post-frontal unstable airmass present, thunderstorms broke out in the valley during the afternoon through the early evening. The thunderstorms produced some locally heavy rainfall and there were a few reports of flooding in Tulare County with a road washed out near Woodlake. There were also a few reports of funnel clouds which were posted online. Most locations in the San Joaquin Valley picked up a tenth to a third of an inch of rainfall while many locations in the Southern Sierra Nevada picked up between a third of an inch to an inch of liquid precipitation with locally higher amounts measured at a few stations. Pictures posted on Twitter of a funnel cloud east of Exeter.", "ts_dict_index": [4938, 4939, 4940]}
+{"event_id": 934789, "event_type": "Funnel Cloud", "state": "FLORIDA", "cz_name": "ST. JOHNS", "begin_date_time": "2021-02-14 14:29:00", "end_date_time": "2021-02-14 14:29:00", "narrative": "A wet, unsettled weather pattern continued over the area with a surface front across central in the morning that lifted north into the afternoon as a warm front as a surface low developed along the boundary in the eastern GOMEX and approached Apalachee Bay. Rainfall and isolated thunderstorms continued across NE FL near the lingering surface front in the morning, then as the front retreated northward toward I-10 into the afternoon, the potential for thunderstorms across NE FL expanded northward |within the warm sector. There was a window for severe storm potential in the afternoon across NE FL where enough instability (1000-1500 J/kg MLCAPE) phased with a 35-40 kt 850 mb jet under about 40-50 kts bulk shear with HREF with STP guidance near 1-1.3  units. These ingredients favor strong wind gust potential in |isolated severe storms during this time frame (40-60 mph gusts) and a low threat of isolated, brief tornadoes with Effective SRH |200 m2/s2. A rain wrapped funnel cloud was reported near State Road 13A.", "ts_dict_index": [4935, 4936, 4937]}
+{"event_id": 801140, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-03-02 12:05:00", "end_date_time": "2019-03-02 12:10:00", "narrative": "A strong Pacific storm system moved through central California on March 2. Light precipitation began ahead of the storm during the evening of March 1 then became moderate to locally heavy during the morning of March 2. As a cold front pushed through the area during the late morning and early afternoon hours, thunderstorms developed in the cooler post-frontal airmass producing areas of flooding as well as a small tornado near Mendota which caused minor roof damage to a few homes. Between 1 and 3 inches of liquid precipitation fell across most of the Southern Sierra Nevada. Snow levels were above 8000 feet for much of the event, but lowered to around 5000 feet behind the cold front on Tuesday afternoon. Much of the San Joaquin Valley and Kern County Mountains picked up half an inch to an inch of rain and the Kern County Deserts generally picked up between a tenth to a half an inch of rainfall. The storm moved east of the area by the morning of March 3. A funnel cloud was spotted 5 miles west of Mendota and was shared on Twitter and on media.", "ts_dict_index": [4932, 4933, 4934]}
+{"event_id": 802604, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2019-03-20 12:00:00", "end_date_time": "2019-03-20 12:10:00", "narrative": "A slow moving low pressure system near the California coast spread moisture inland during the evening of March 19 and the morning of March 20. This produced a band of mainly light rainfall which was most noticeable north of Fresno County. Skies cleared out in the San Joaquin Valley during the afternoon of March 20 and with a post-frontal unstable airmass present, thunderstorms broke out in the valley during the afternoon through the early evening. The thunderstorms produced some locally heavy rainfall and there were a few reports of flooding in Tulare County with a road washed out near Woodlake. There were also a few reports of funnel clouds which were posted online. Most locations in the San Joaquin Valley picked up a tenth to a third of an inch of rainfall while many locations in the Southern Sierra Nevada picked up between a third of an inch to an inch of liquid precipitation with locally higher amounts measured at a few stations. A television station posted a photo of a a funnel cloud near Madera.", "ts_dict_index": [4941, 4942, 4943]}
+{"event_id": 939675, "event_type": "Funnel Cloud", "state": "ARKANSAS", "cz_name": "CLARK", "begin_date_time": "2021-02-28 16:20:00", "end_date_time": "2021-02-28 16:20:00", "narrative": "Heavy rain brought flash flooding to parts of Arkansas on February the 28th. By the 28th, thermometers were in the mid to upper 70s across the central and southern counties. It was 76 degrees at Little Rock (Pulaski County) and Monticello (Drew County). It certainly felt like spring, and thunderstorms were back in the forecast.||Storms were sparked by a new cold front that penetrated into northwest Arkansas by lunchtime on the 28th, and approached the Louisiana border toward evening. Along the way, downpours were widespread, and there was at least a concern for severe weather (damaging winds, large hail, and maybe a tornado or two).||In the end, this was mainly a heavy rain event. Roads were flooded in Malvern (Hot Spring County), Pine Bluff (Jefferson County), and Sheridan (Grant County). Severe storms were few, with trees blown down at Greenbrier (Faulkner County) and Olmstead (Pulaski County), and nickel size hail just west of Wooster (Faulkner County). A funnel cloud was seen near Arkadelphia, near Highway 67.", "ts_dict_index": [4929, 4930, 4931]}
+{"event_id": 882334, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2020-03-19 11:00:00", "end_date_time": "2020-03-19 13:00:00", "narrative": "A series of cold upper lows impacted Southern California on March 16-20th. Widespread precipitation occurred with the first upper low on March 16th, continuing through the 17th. Snow occurred on the 18th in the mountains when the upper low moved south over far northern Baja and into the deserts. A secondary cold upper low dropped south from Lake Tahoe on March 18th and 19th, bringing more widespread precipitation to the area. Heavy showers occurred on March 19th in the inland valleys as well as snow in the mountains. Total rainfall ranged from a few tenths of an inch along the coast, up to 0.75 in the valleys. Mountain areas saw up to 1.20 of precipitation. Hourly rainfall rates of 0.25 to 0.55 inches per hour were observed on March 18th and 19th. Snowfall was mainly confined to the San Bernardino Mountains, where up to 6 inches of snow fell on the highest peaks. Funnel clouds were observed along the coast on March 16th and 19th. Coronado Lifeguards reported 2 funnel clouds/waterspouts off the coast of Coronado on March 19th.", "ts_dict_index": [4947, 4948, 4949]}
+{"event_id": 876222, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2020-04-06 14:30:00", "end_date_time": "2020-04-06 14:40:00", "narrative": "A very cold and moist low pressure system dropped south out of the Gulf of Alaska on April 4 and moved slowly southward off the California coast on April 5 and 6. This system brought moderate to heavy precipitation to the area between the afternoon of April 5 to the afternoon of April 6. Several stations in the Sierra Nevada and adjacent foothills picked up between 1.5 and 3 inches of liquid precipitation while much of the eastern San Joaquin Valley picked up between 0.75 and 1.5 inches of rainfall. The west side of the San Joaquin Valley along with the Kern County Mountains and Deserts generally picked up between half and inch and an inch of rain. Several STOTEL stations in the Sierra Nevada above 5500 feet picked up an estimated 18 to 36 of new snowfall with a few stations above 8000 feet picking up higher amounts. There were reports of localized nuisance flooding, as a few thunderstorms popped up during the afternoon of April 6. One of the thunderstorms produced a funnel cloud near Laton which was observed by several spotters and reported by several media outlets. Several public reports and videos were received of a funnel cloud near Laton.", "ts_dict_index": [4923, 4924, 4925]}
+{"event_id": 795745, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "MADERA", "begin_date_time": "2019-02-04 13:33:00", "end_date_time": "2019-02-04 13:38:00", "narrative": "A very cold Pacific Storm system dropped out of the Gulf of Alaska on February 3 and slowly moved across the regions on February 4 and 5. This system brought moderate to heavy precipitation to portions of the San Joaquin Valley on February 4 and heavy snow to elevations as low as 2000 feet in the southern Sierra Nevada foothills on February 4 and 5. Between 4 and 6 feet of new snow fell above 5000 feet in the Southern Sierra Nevada.  The heavy wet snow also resulted in numerous power outages affecting close to 20300 customers in the Mariposa and Yosemite Park areas. Additionally, all roads leading into Yosemite National Park (including State Routes 120, 140 and 41) were closed due to heavy snowfall. Several other roads had chain requirements above 2000 feet. Several school districts in the southern Sierra foothills closed for the day on February 5 due to roads being close to impassible as a result of heavy snowfall. Public reports of a funnel cloud in Madera.", "ts_dict_index": [4959, 4960, 4961]}
+{"event_id": 817719, "event_type": "Funnel Cloud", "state": "NEW MEXICO", "cz_name": "SANTA FE", "begin_date_time": "2019-06-02 16:22:00", "end_date_time": "2019-06-02 16:28:00", "narrative": "The extended stretch of severe weather continued to impact eastern New Mexico on June 2, 2019 as more dryline thunderstorms shifted northeast through the region. A slow-moving upper level storm system to the west of New Mexico continued to pump deep moisture into the region with strong afternoon heating and instability leading to scattered to numerous showers and storms. Thunderstorms first developed within the Rio Grande Valley and nearby higher terrain during the early afternoon before shifting onto the high plains of eastern New Mexico. A cluster of thunderstorms that developed near Los Lunas moved northeast across the east mountain communities into the Santa Fe area with hail up to the size of golf balls. Large hail, strong winds, very heavy rainfall, and even a tornado were reported with these storms as they progressed into eastern New Mexico through the early evening hours. A well-defined funnel cloud was observed in Santa Fe.", "ts_dict_index": [4968, 4969, 4970]}
+{"event_id": 795744, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-02-04 13:05:00", "end_date_time": "2019-02-04 13:10:00", "narrative": "A very cold Pacific Storm system dropped out of the Gulf of Alaska on February 3 and slowly moved across the regions on February 4 and 5. This system brought moderate to heavy precipitation to portions of the San Joaquin Valley on February 4 and heavy snow to elevations as low as 2000 feet in the southern Sierra Nevada foothills on February 4 and 5. Between 4 and 6 feet of new snow fell above 5000 feet in the Southern Sierra Nevada.  The heavy wet snow also resulted in numerous power outages affecting close to 20300 customers in the Mariposa and Yosemite Park areas. Additionally, all roads leading into Yosemite National Park (including State Routes 120, 140 and 41) were closed due to heavy snowfall. Several other roads had chain requirements above 2000 feet. Several school districts in the southern Sierra foothills closed for the day on February 5 due to roads being close to impassible as a result of heavy snowfall. Public reports of a funnel cloud between Dinuba and Visalia.", "ts_dict_index": [4956, 4957, 4958]}
+{"event_id": 971417, "event_type": "Funnel Cloud", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2021-07-14 17:02:00", "end_date_time": "2021-07-14 17:02:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. Multiple reports of a funnel cloud near Green Mountain near 170th and Wallace Avenue.", "ts_dict_index": [4977, 4978, 4979]}
+{"event_id": 882332, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2020-03-16 10:00:00", "end_date_time": "2020-03-16 12:00:00", "narrative": "A series of cold upper lows impacted Southern California on March 16-20th. Widespread precipitation occurred with the first upper low on March 16th, continuing through the 17th. Snow occurred on the 18th in the mountains when the upper low moved south over far northern Baja and into the deserts. A secondary cold upper low dropped south from Lake Tahoe on March 18th and 19th, bringing more widespread precipitation to the area. Heavy showers occurred on March 19th in the inland valleys as well as snow in the mountains. Total rainfall ranged from a few tenths of an inch along the coast, up to 0.75 in the valleys. Mountain areas saw up to 1.20 of precipitation. Hourly rainfall rates of 0.25 to 0.55 inches per hour were observed on March 18th and 19th. Snowfall was mainly confined to the San Bernardino Mountains, where up to 6 inches of snow fell on the highest peaks. Funnel clouds were observed along the coast on March 16th and 19th. Fire department reported funnel clouds or waterspouts off the coast of Oceanside and Carlsbad. They confirmed that there were funnel clouds, and possibly waterspouts but it was too far offshore to tell.", "ts_dict_index": [4950, 4951, 4952]}
+{"event_id": 795747, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "TULARE", "begin_date_time": "2019-02-05 13:45:00", "end_date_time": "2019-02-05 13:50:00", "narrative": "A very cold Pacific Storm system dropped out of the Gulf of Alaska on February 3 and slowly moved across the regions on February 4 and 5. This system brought moderate to heavy precipitation to portions of the San Joaquin Valley on February 4 and heavy snow to elevations as low as 2000 feet in the southern Sierra Nevada foothills on February 4 and 5. Between 4 and 6 feet of new snow fell above 5000 feet in the Southern Sierra Nevada.  The heavy wet snow also resulted in numerous power outages affecting close to 20300 customers in the Mariposa and Yosemite Park areas. Additionally, all roads leading into Yosemite National Park (including State Routes 120, 140 and 41) were closed due to heavy snowfall. Several other roads had chain requirements above 2000 feet. Several school districts in the southern Sierra foothills closed for the day on February 5 due to roads being close to impassible as a result of heavy snowfall. Photos and reports on Twitter of a funnel cloud 4 miles NE of Goshen.", "ts_dict_index": [4965, 4966, 4967]}
+{"event_id": 971420, "event_type": "Funnel Cloud", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2021-07-14 19:15:00", "end_date_time": "2021-07-14 19:15:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. Trained spotter reports a brief funnel cloud 2 miles ESE of Melbourne.", "ts_dict_index": [4980, 4981, 4982]}
+{"event_id": 895493, "event_type": "Funnel Cloud", "state": "WISCONSIN", "cz_name": "POLK", "begin_date_time": "2020-07-21 15:20:00", "end_date_time": "2020-07-21 15:20:00", "narrative": "During the afternoon of Tuesday, July 21st, a few thunderstorms developed along a frontal boundary over east-central Minnesota. Several spotters and storm chasers were following these storms as the storms moved into Wisconsin. ||The storm that moved into Polk County had a consistent funnel cloud associated with it with a brief tornado touchdown near Clear Lake and then again near Arland. Another storm developed across northern Dunn County and produced an EF0 tornado northeast of Wheeler. More storms developed over southeast Dunn and central Chippewa Counties to produce the majority of the damage. ||The worst damage occurred in the city of Cadott where numerous trees, power lines and a few structures were damaged as it moved through the town before dissipating.||The two tornadoes in Chippewa County had an average path length of 3 to 4 miles and an average width of 75 yards. A brief funnel cloud was observed around Bear Lake in western Polk County. Video was inconclusive as to whether there was any ground circulation.", "ts_dict_index": [4974, 4975, 4976]}
+{"event_id": 842048, "event_type": "Funnel Cloud", "state": "IOWA", "cz_name": "CASS", "begin_date_time": "2019-07-16 13:28:00", "end_date_time": "2019-07-16 13:28:00", "narrative": "A juicy atmosphere with a lack of organizational support (effective bulk shear) made for a messy convective environment across portions of the state on the 16th. During the morning hours convection from central and eastern Nebraska drifted into western Iowa, producing heavy rainfall. Another round of developed across northwest Iowa during the morning and rolled across northern Iowa and southern Minnesota, producing a lone severe wind gust. Later in the afternoon, storms were able to initiate along old outflow boundaries and were able to produce localized heavy rainfall, a weak tornado, and a other funnel cloud reports. ||While support was lackluster, there were indications for the possibility of a funnel cloud or weak tornado during the afternoon with supportive SBCAPE in excess of 2000 J/kg, weak boundaries in the area, and most importantly very supportive 0-3km cape values in excess of 150 J/kg for low level stretching. Trained spotter reported a brief funnel cloud south of Atlantic.", "ts_dict_index": [4953, 4954, 4955]}
+{"event_id": 795746, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "FRESNO", "begin_date_time": "2019-02-04 16:00:00", "end_date_time": "2019-02-04 16:05:00", "narrative": "A very cold Pacific Storm system dropped out of the Gulf of Alaska on February 3 and slowly moved across the regions on February 4 and 5. This system brought moderate to heavy precipitation to portions of the San Joaquin Valley on February 4 and heavy snow to elevations as low as 2000 feet in the southern Sierra Nevada foothills on February 4 and 5. Between 4 and 6 feet of new snow fell above 5000 feet in the Southern Sierra Nevada.  The heavy wet snow also resulted in numerous power outages affecting close to 20300 customers in the Mariposa and Yosemite Park areas. Additionally, all roads leading into Yosemite National Park (including State Routes 120, 140 and 41) were closed due to heavy snowfall. Several other roads had chain requirements above 2000 feet. Several school districts in the southern Sierra foothills closed for the day on February 5 due to roads being close to impassible as a result of heavy snowfall. Reports and pictures posted on Facebook of a rotating and lowering funnel cloud west of Balch Camp. A tornado warning had been previously issued on this storm.", "ts_dict_index": [4962, 4963, 4964]}
+{"event_id": 891027, "event_type": "Funnel Cloud", "state": "FLORIDA", "cz_name": "PALM BEACH", "begin_date_time": "2020-05-21 12:11:00", "end_date_time": "2020-05-21 12:11:00", "narrative": "A rex block characterized by a deep upper-level low across the Tennessee Valley Region and an upper-level high across the Great Lakes Region gave way to an upper-level cold pocket across the southeastern portions of the United states. Simultaneously, a mid-level vorticity lobe rotated across the region which also aided in an increase of convection, especially due to the combination of lingering boundaries and sea breeze formation. Forecast soundings also showed an inverted V as well as favorable DCAPE values, which were supportive for a few damaging wind gusts with the taller, more robust, updrafts contained hail. Furthermore, tornado potential increased with favorable low level winds and shear across land. Finally, with an overall weaker flow aloft and PWATs approaching the 2 inch mark, some localized flooding occurred. A photo of a funnel cloud was reported in Boca Raton, west of I-95 and Spanish River Blvd, looking west toward Military Trail.", "ts_dict_index": [4992, 4993, 4994]}
+{"event_id": 1052763, "event_type": "Funnel Cloud", "state": "FLORIDA", "cz_name": "DUVAL", "begin_date_time": "2022-08-31 14:30:00", "end_date_time": "2022-08-31 14:30:00", "narrative": "A cold front slowly moved across southeast Georgia with high pressure to the southeast. A moist (PWATs around 2 in.) airmass and west-southwesterly flow prevailed across the area ahead of the frontal boundary. This caused the Atlantic sea breeze to only shift as far as the I-95 corridor. An upper shortwave trough passed through the southeastern US into southeast Georgia helping to enhance storms along the frontal boundary. A west to east line of pre-frontal storms moved southeastward and converged with the pinned Atlantic sea breeze in the afternoon. A few severe storms developed at these boundary mergers producing funnel clouds, heavy rain and severe winds downing trees. Later in the evening, the line of storms along the front shifted southward and interacted with the pinned sea breeze boundary. A funnel cloud was observed in downtown Jacksonville over the main street bridge. Videos were relayed via social media.", "ts_dict_index": [5013, 5014, 5015]}
+{"event_id": 949971, "event_type": "Funnel Cloud", "state": "NEW MEXICO", "cz_name": "SANTA FE", "begin_date_time": "2021-05-17 12:06:00", "end_date_time": "2021-05-17 12:08:00", "narrative": "An active stretch of severe weather across eastern New Mexico continued on May 17, 2021 with a significant severe weather outbreak that included multiple tornadoes. As a potent low pressure system approached the state, instability and shear increased across the area, providing a favorable environment for severe thunderstorms. Convective initiation started by late Monday morning over the high terrain of New Mexico. Steering flow generally moved the storms in a northeasterly direction where they intensified over the plains. Several reports of hail and severe winds were received as well as multiple tornado reports. Two supercell tornadoes occurred across eastern New Mexico, but no damage occurred. The environment was even favorable for tornadoes in central New Mexico where three landspout tornadoes were confirmed. A funnel cloud from a strong thunderstorm was spotted near the Santa Fe airport. The funnel cloud never touched down, and no damage was reported.", "ts_dict_index": [5001, 5002, 5003]}
+{"event_id": 1103888, "event_type": "Funnel Cloud", "state": "NEW MEXICO", "cz_name": "UNION", "begin_date_time": "2023-06-11 18:00:00", "end_date_time": "2023-06-11 18:10:00", "narrative": "A backdoor front brought moist easterly upslope flow into northeastern NM on June 11th and June 12th. Discrete supercells fired up along the east slopes of the Sangre de Cristo Mountains during the early afternoon hours of June 11th dropping large to destructive hail as they translated east towards the Texas and Oklahoma Panhandles. More storms developed off the east slopes of the Sangre de Cristo Mountains around sunset dropping more large to destructive hail across the region during the overnight hours into Monday morning. Storms eventually trained over the same areas resulting in major flash flooding over Colfax, Union, Mora and Harding Counties. More discrete supercells fired up midday June 12th tracking east before exiting into the Texas Panhandle around sunset. A resident just west of Capulin shared a photo of a funnel cloud from a strong thunderstorm.", "ts_dict_index": [5028, 5029, 5030]}
+{"event_id": 814200, "event_type": "Funnel Cloud", "state": "CALIFORNIA", "cz_name": "MERCED", "begin_date_time": "2019-05-21 14:30:00", "end_date_time": "2019-05-21 14:30:00", "narrative": "A cold front pushed southward through central California during the morning of May 21. Strong winds accompanied the front and followed the frontal passage over the Kern County Mountains and Deserts. Several stations reported wind gusts between 55 and 65 mph, and a few low impact indicator sites measured gusts above 75 mph. This system  also produced scattered showers across the area although precipitation amounts were generally light. Several stations in Yosemite Park above 6000 feet picked up another 2 to 5 inches of new snowfall. Further south there were several reports of 1 to 3 inches of new snow above 6000 feet. A few thunderstorms popped up in the San Joaquin Valley and Sierra foothills during the afternoon of May 21, but most of them were short lived and did not produce much rainfall. Reports and photos on Facebook and Twitter of a funnel cloud over the northeastern portion of Los Banos.", "ts_dict_index": [5016, 5017, 5018]}
+{"event_id": 886883, "event_type": "Funnel Cloud", "state": "FLORIDA", "cz_name": "PALM BEACH", "begin_date_time": "2020-05-17 17:38:00", "end_date_time": "2020-05-17 17:43:00", "narrative": "Tropical Storm Arthur was forecast by the NHC to continue moving northeastward towards the outer banks of North Carolina while a mid-upper level low over TX moves eastward. This allowed for the wind flow over South FL to be SSW which allowed the Gulf Sea Breeze to form along with the Atlantic Sea Breeze. Plenty of residual tropical moisture across the area, along with the eventual sea breeze collision, lead to scattered to numerous strong showers and thunderstorms that eventually pushed eastward towards the east coast metro areas (thanks to the SSW flow). Heavy rain and flooding along with strong wind gusts and small hail were reported. Enhanced helicity/shear in Palm Beach County even led to the development of a funnel cloud. A trained spotter reported a funnel cloud to the SW of the intersection of Big Blue Trace and Wellington Trace from a thunderstorm moving through the area.", "ts_dict_index": [5046, 5047, 5048]}
+{"event_id": 1047170, "event_type": "Funnel Cloud", "state": "FLORIDA", "cz_name": "DUVAL", "begin_date_time": "2022-08-22 13:41:00", "end_date_time": "2022-08-22 13:41:00", "narrative": "Generally west steering flow along with deep moisture (PWATs 2 inches or more) and impulses of energy in this flow aloft triggered numerous showers and storms during the afternoon and evening hours. Westerly flow pinned the Atlantic coast sea breeze to the coast and gave an early start to the Gulf coast sea breeze shifting inland across northeast Florida. Strong thunderstorms developed in the afternoon as they interacted with the stationary Atlantic sea breeze boundary along the coast before shifting offshore. These storms produced gusts between 45 to 55 mph at Marineland, St. Augustine and Mayport. Also, lightning struck a house in Neptune beach causing a house fire. Street flooding and heavy rain in Jacksonville Beach and Clay county were caused by training storms moving northeastward along a line that set up extending from Jacksonville Beach to Ocala. A funnel cloud was reported near Neptune Beach. It lasted about 3 to 4 minutes.", "ts_dict_index": [4983, 4984, 4985]}
+{"event_id": 1037533, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2022-06-14 21:35:00", "end_date_time": "2022-06-14 21:51:00", "narrative": "For the second consecutive Tuesday evening, a relatively small percentage of the 24-county South Central Nebraska area was ravaged by significant severe thunderstorms that caused countless instances of damage including (but not limited to): broken windows/damaged siding, flipped irrigation pivots, destroyed crops by the thousands of acres, and more isolated occurrences of outright-demolished outbuildings/grain bins along with relatively minor structural damage to a few homes. Unlike the event a week prior on the 7th that featured a few separate swaths of severe weather, this one that played out mainly between 9:30 p.m. CDT on the 14th and 3:30 a.m. CDT on the 15th was highlighted by just one narrow, west-southwest to east-northeast oriented swath of multiple training supercells. In fact, some locations (Hastings and York to name a few) actually endured three to four SEPARATE severe storms over a span of 2-4 hours! With only limited exception, the vast majority of storm reports emanated from a 10-20 mile wide stripe centered roughly along a line from Elwood-Kearney-Doniphan-York. Within this zone there were numerous reports of large hail (many golf ball to tennis ball size) and damaging winds mainly in the 60-75 MPH range (but isolated pockets of 90-100+ MPH...especially east Highway 14). In addition, an EF-2 tornado was confirmed in southwest York County. Also of note was that some very unlucky locales experienced nearly a repeat performance of what just unfolded seven evenings prior...struck by another round of large hail/damaging winds only days after starting to recover from the first event on the 7th. Although this overlapping damage was somewhat evident over northeastern Adams County, it was particularly visible within the southwestern quadrant of York County, where many fields were mostly stripped bare for miles around...creating a visually striking/eerie contrast to what is typically a sea of green under the mid-June sun. ||Taking a deeper dive into storm reports and starting with the EF-2 tornado, storm surveys concluded that it tracked just over seven miles through southwestern York County shortly after midnight CDT, developing west-southwest of Lushton and lifting west of McCool Junction. Along the way, several farmsteads sustained damage (including a garage torn from a home and a wood frame outbuilding completely demolished) and two people sustained minor injuries. Interestingly, an unofficial mesonet station in or very near the tornado path actually measured a 90 MPH gust a few miles east-northeast of Lushton. Turning to the many known (and countless unknown) occurrences of large hail/damaging straight line winds within the primary convective swath, a few of the more noteworthy wind damage/speed reports included: estimated 105 MPH winds in the Waco area that toppled a 60 ft. concrete silo; estimated 95 MPH winds through parts of northeastern Clay County that crumpled a grain bin near Saronville; widespread tree and sporadic structural damage in McCool Junction; separate measured wind gusts of 75 and 65 MPH at Hastings airport (from different storms 45 minutes apart); an unofficial mesonet gust of 79 MPH near Norman. Meanwhile, a few of the most notable hail reports featured: stones up to tennis ball size in York and Trumbull; hail up to 2.25 diameter at the NWS Hastings office that significantly dented the vehicles of on-duty meteorologists working this event; various reports of ping pong ball to golf ball size hail in or near Waco, Riverdale, Lushton, Bertrand, Kearney and seven miles south of Elwood. Rainfall-wise, despite the passage of several storms over the same areas, progressive storm motions mitigated the threat of significant flooding by limiting most totals to no more than 1-2 (highest NeRAIN amount of 2.67 on the east side of York). Although the vast majority of hail/wind reports were tied to the aforementioned west-east corridor bisecting the heart of the area, two severe storms occurred well outside of this zone...one to the south/one to the north. The southern one was a discrete supercell that lumbered through parts of Webster/Nuckolls/Thayer counties but yielded only one report of quarter size hail in Nelson. Meanwhile, the northern-most severe storm was the left-split of a supercell that first developed southwest of Kearney, dropping 1.5-2 diameter hail in the Pleasanton and Loup City areas before weakening. ||Examining event evolution/meteorological background, the first weak convection of the evening within South Central Nebraska bubbled up in the Hastings area shortly before sunset, forming slightly north of a well-defined, southwest-northeast oriented quasi-stationary front stretched from west-central KS through southeast NE (storms that developed directly along this front earlier in the evening remained just southeast of the local area). Between 9-10 p.m. CDT two supercells quickly evolved out of the initial weak activity, one that pounded York with its first round of large hail and drilled the eastern part of the county with significant wind damage, and the other the aforementioned southern supercell that developed over Webster County. Between 10-11 p.m. CDT, these first severe storms either departed the local area into eastern Nebraska (the northern one) or weakened/dissipated (the southern one). However, not far to the west the primary supercell train was just getting warmed up as several severe storms rapidly blossomed along the Highway 6/Interstate 80 corridors within the western half of South Central Nebraska. This slightly-elevated activity developed in response to intensifying nocturnal convergence into a sharpening frontal zone very evident in the 850-700 millibar layer. Given that this low-mid level front was aligned nearly parallel to strong west-southwesterly upper level winds (attendant to a large scale trough centered over the Northern Rockies) and that the mesoscale environment featured a potent combination of very strong deep layer shear (50-70 knots) and decent most-unstable CAPE (1000-2000 J/kg), the stage was set for a somewhat rare episode of several supercells training along the same corridor in close succession. In fact, between 11 p.m. and 2 a.m. CDT, at least 3-5 severe-warned storms marched in tandem along this path, each core spaced out roughly 25 miles from the next. During this three-hour span, places such as Hastings and York endured three separate severe storms (bringing York up to FOUR direct hits...including the initial supercell of the night). While most of these cells remained just elevated enough to preclude a tornado threat, the first storm in the supercell train managed to spawn the EF-2 in southwestern York County...apparently tapping into JUST enough lower-level moisture/instability in the vicinity of the nearby surface front to become tornadic. Finally, between 2:00-3:30 a.m. CDT, the last two training supercells of the night passed through Hamilton, Polk and northern York counties before departing the local area, bringing an end to this unique and (in places) destructive event. There were several reports of hail ranging in size from quarters to golf balls along and near a path from Odessa, to in and near Riverdale, to south of Pleasanton.", "ts_dict_index": [5049, 5050, 5051]}
+{"event_id": 978887, "event_type": "Funnel Cloud", "state": "IOWA", "cz_name": "CERRO GORDO", "begin_date_time": "2021-08-27 16:27:00", "end_date_time": "2021-08-27 16:27:00", "narrative": "A nearly station boundary draped itself across northern Iowa, oriented east-west on the evening of the 27th and allowed isolated supercells and multi cellular storms to initiate and in some cases train/develop over the same area for a number of hours. In total, severe weather (damaging winds, funnel clouds, tornadoes), heavy rain, and flooding occurred. ||The portions of northern Iowa that experienced the severe and hazardous weather resided just south of the surface boundary and included the following environment: SB/MUCAPE in excess of 2000 j/kg, LCLs under 1000m, effective bulk shear around/in excess of 30 kts, precipitable water values in excess of 1.8 inches, supercell composite values in excess of 12, effective SRH around 200 m2/s2, and 0-3km SRH around 200-300 m2/s2. A funnel cloud was reported north of Sheffield. The funnel cloud was low but unclear if it was in contact with the ground.", "ts_dict_index": [5025, 5026, 5027]}
+{"event_id": 1039442, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-14 22:39:00", "end_date_time": "2022-06-14 22:45:00", "narrative": "For the second consecutive Tuesday evening, a relatively small percentage of the 24-county South Central Nebraska area was ravaged by significant severe thunderstorms that caused countless instances of damage including (but not limited to): broken windows/damaged siding, flipped irrigation pivots, destroyed crops by the thousands of acres, and more isolated occurrences of outright-demolished outbuildings/grain bins along with relatively minor structural damage to a few homes. Unlike the event a week prior on the 7th that featured a few separate swaths of severe weather, this one that played out mainly between 9:30 p.m. CDT on the 14th and 3:30 a.m. CDT on the 15th was highlighted by just one narrow, west-southwest to east-northeast oriented swath of multiple training supercells. In fact, some locations (Hastings and York to name a few) actually endured three to four SEPARATE severe storms over a span of 2-4 hours! With only limited exception, the vast majority of storm reports emanated from a 10-20 mile wide stripe centered roughly along a line from Elwood-Kearney-Doniphan-York. Within this zone there were numerous reports of large hail (many golf ball to tennis ball size) and damaging winds mainly in the 60-75 MPH range (but isolated pockets of 90-100+ MPH...especially east Highway 14). In addition, an EF-2 tornado was confirmed in southwest York County. Also of note was that some very unlucky locales experienced nearly a repeat performance of what just unfolded seven evenings prior...struck by another round of large hail/damaging winds only days after starting to recover from the first event on the 7th. Although this overlapping damage was somewhat evident over northeastern Adams County, it was particularly visible within the southwestern quadrant of York County, where many fields were mostly stripped bare for miles around...creating a visually striking/eerie contrast to what is typically a sea of green under the mid-June sun. ||Taking a deeper dive into storm reports and starting with the EF-2 tornado, storm surveys concluded that it tracked just over seven miles through southwestern York County shortly after midnight CDT, developing west-southwest of Lushton and lifting west of McCool Junction. Along the way, several farmsteads sustained damage (including a garage torn from a home and a wood frame outbuilding completely demolished) and two people sustained minor injuries. Interestingly, an unofficial mesonet station in or very near the tornado path actually measured a 90 MPH gust a few miles east-northeast of Lushton. Turning to the many known (and countless unknown) occurrences of large hail/damaging straight line winds within the primary convective swath, a few of the more noteworthy wind damage/speed reports included: estimated 105 MPH winds in the Waco area that toppled a 60 ft. concrete silo; estimated 95 MPH winds through parts of northeastern Clay County that crumpled a grain bin near Saronville; widespread tree and sporadic structural damage in McCool Junction; separate measured wind gusts of 75 and 65 MPH at Hastings airport (from different storms 45 minutes apart); an unofficial mesonet gust of 79 MPH near Norman. Meanwhile, a few of the most notable hail reports featured: stones up to tennis ball size in York and Trumbull; hail up to 2.25 diameter at the NWS Hastings office that significantly dented the vehicles of on-duty meteorologists working this event; various reports of ping pong ball to golf ball size hail in or near Waco, Riverdale, Lushton, Bertrand, Kearney and seven miles south of Elwood. Rainfall-wise, despite the passage of several storms over the same areas, progressive storm motions mitigated the threat of significant flooding by limiting most totals to no more than 1-2 (highest NeRAIN amount of 2.67 on the east side of York). Although the vast majority of hail/wind reports were tied to the aforementioned west-east corridor bisecting the heart of the area, two severe storms occurred well outside of this zone...one to the south/one to the north. The southern one was a discrete supercell that lumbered through parts of Webster/Nuckolls/Thayer counties but yielded only one report of quarter size hail in Nelson. Meanwhile, the northern-most severe storm was the left-split of a supercell that first developed southwest of Kearney, dropping 1.5-2 diameter hail in the Pleasanton and Loup City areas before weakening. ||Examining event evolution/meteorological background, the first weak convection of the evening within South Central Nebraska bubbled up in the Hastings area shortly before sunset, forming slightly north of a well-defined, southwest-northeast oriented quasi-stationary front stretched from west-central KS through southeast NE (storms that developed directly along this front earlier in the evening remained just southeast of the local area). Between 9-10 p.m. CDT two supercells quickly evolved out of the initial weak activity, one that pounded York with its first round of large hail and drilled the eastern part of the county with significant wind damage, and the other the aforementioned southern supercell that developed over Webster County. Between 10-11 p.m. CDT, these first severe storms either departed the local area into eastern Nebraska (the northern one) or weakened/dissipated (the southern one). However, not far to the west the primary supercell train was just getting warmed up as several severe storms rapidly blossomed along the Highway 6/Interstate 80 corridors within the western half of South Central Nebraska. This slightly-elevated activity developed in response to intensifying nocturnal convergence into a sharpening frontal zone very evident in the 850-700 millibar layer. Given that this low-mid level front was aligned nearly parallel to strong west-southwesterly upper level winds (attendant to a large scale trough centered over the Northern Rockies) and that the mesoscale environment featured a potent combination of very strong deep layer shear (50-70 knots) and decent most-unstable CAPE (1000-2000 J/kg), the stage was set for a somewhat rare episode of several supercells training along the same corridor in close succession. In fact, between 11 p.m. and 2 a.m. CDT, at least 3-5 severe-warned storms marched in tandem along this path, each core spaced out roughly 25 miles from the next. During this three-hour span, places such as Hastings and York endured three separate severe storms (bringing York up to FOUR direct hits...including the initial supercell of the night). While most of these cells remained just elevated enough to preclude a tornado threat, the first storm in the supercell train managed to spawn the EF-2 in southwestern York County...apparently tapping into JUST enough lower-level moisture/instability in the vicinity of the nearby surface front to become tornadic. Finally, between 2:00-3:30 a.m. CDT, the last two training supercells of the night passed through Hamilton, Polk and northern York counties before departing the local area, bringing an end to this unique and (in places) destructive event. Hail as large as tennis balls was reported in Trumbull.", "ts_dict_index": [5052, 5053, 5054]}
+{"event_id": 978888, "event_type": "Funnel Cloud", "state": "IOWA", "cz_name": "CERRO GORDO", "begin_date_time": "2021-08-27 16:42:00", "end_date_time": "2021-08-27 16:42:00", "narrative": "A nearly station boundary draped itself across northern Iowa, oriented east-west on the evening of the 27th and allowed isolated supercells and multi cellular storms to initiate and in some cases train/develop over the same area for a number of hours. In total, severe weather (damaging winds, funnel clouds, tornadoes), heavy rain, and flooding occurred. ||The portions of northern Iowa that experienced the severe and hazardous weather resided just south of the surface boundary and included the following environment: SB/MUCAPE in excess of 2000 j/kg, LCLs under 1000m, effective bulk shear around/in excess of 30 kts, precipitable water values in excess of 1.8 inches, supercell composite values in excess of 12, effective SRH around 200 m2/s2, and 0-3km SRH around 200-300 m2/s2. Funnel cloud reported 2 miles northwest of Dougherty, with uncertainty as to whether it was in contact with the ground.", "ts_dict_index": [5022, 5023, 5024]}
+{"event_id": 1035656, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-07 20:00:00", "end_date_time": "2022-06-07 20:00:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. Quarter size hail was reported. Wind gusts were estimated to be near 70 MPH.", "ts_dict_index": [5055, 5056, 5057]}
+{"event_id": 1120249, "event_type": "Funnel Cloud", "state": "IOWA", "cz_name": "BREMER", "begin_date_time": "2023-07-28 17:17:00", "end_date_time": "2023-07-28 17:17:00", "narrative": "A cold front sank south across Iowa during the afternoon and evening of July 28th. The environment was primed for severe storms with warm moist air in place; as temperatures climbed into the 90s and dewpoints into the 70s. By afternoon MLCAPE values of 3000 J/kg were in place across much of Iowa with deep layer shear exceeding 40 kts. Such an environment supported rapid storm development along the boundary by late afternoon. Storms produced ping-pong ball to baseball sized hail along with two tornadoes, damaging confinement pens and creating easily identifiable tracks on high resolution satellite imagery through surrounding fields. As storms pushed south into the evening, the hazards transitioned to a wind threat. A micro burst occurred in Marshall County very near the ASOS, resulting in an isolated pocket of 80 to 90 mph winds. Funnel cloud north of Denver, Iowa.", "ts_dict_index": [4986, 4987, 4988]}
+{"event_id": 883646, "event_type": "Funnel Cloud", "state": "MINNESOTA", "cz_name": "DAKOTA", "begin_date_time": "2020-05-26 18:30:00", "end_date_time": "2020-05-26 18:32:00", "narrative": "The afternoon of Tuesday, May 26th, a surface low was noted in southwest Iowa with a broad area of southeast flow along a surface boundary northward across southern Minnesota. Scattered thunderstorms started to develop in the warm sector by the mid afternoon across western Wisconsin and Iowa. These storms moved northward into an area of MLCAPEs of 1500-2000 J/kg with bulk shear values of around 30 knots. Radar indicated that numerous storms were rotating along the boundary as they moved northward. Most of the storms produced funnel clouds, but two storms caused an EF0 tornado east of Albert Lea, and another in the southeast Twin Cities suburbs of Rosemount. A line of storms that moved northward across southeast Minnesota produced wind damage in Kenyon. Several storm chasers took video of a funnel cloud west of Northfield.", "ts_dict_index": [5040, 5041, 5042]}
+{"event_id": 859868, "event_type": "Funnel Cloud", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-11-21 13:05:00", "end_date_time": "2019-11-21 13:05:00", "narrative": "A strong upper low system passing through the area helped generate convection in western Maricopa county in the afternoon of the 21st. Modest instability and shear was enough to generate isolated strong storms with multiple reports of funnel clouds, hail, and heavy rain. There were two reports of funnel clouds over far western Maricopa County near the county border, one of which was along Interstate 10 just west of the county line. On the southwest side of Phoenix, one especially strong storm became severe and strengthened into a supercell. The storm developed a wall cloud and produced heavy rain as well as several reports of hail at least one inch in diameter.. Hail was reported in communities such as Buckeye, Avondale and Goodyear. A strong thunderstorm developed across the far western portion of Maricopa County during the early afternoon hours on November 21st. In addition to the typical thunderstorm hazards including wind and heavy rain, the storm managed to produce a funnel cloud at about 1305MST. The funnel cloud was observed by a motorist on Interstate 10 about 10 miles to the west of the town of Tonopah; the  motorist also took video of the funnel which was located just north of the interstate. The storm had a history of producing funnel clouds; about one half hour earlier the storm generated another funnel along the interstate and just west of the county line in far eastern La Paz County. Although no damage was produced by the funnel, it was still noteworthy as funnel clouds are rare across the deserts of southern Arizona.", "ts_dict_index": [5043, 5044, 5045]}
+{"event_id": 799411, "event_type": "Funnel Cloud", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-02-22 17:25:00", "end_date_time": "2019-02-22 17:30:00", "narrative": "A powerful and slow moving winter storm moved across Arizona from February 21st into the 22nd; the storm brought locally heavy rain to much of south-central Arizona as well as heavy mountain snow. Although conditions were not overly unstable during the afternoon, they were sufficient to allow for the generation of isolated thunderstorms. On February 21st, a strong storm generated wind damage in Tolleson. On the 22nd, the storms produced a pair of funnel clouds. At 1435MST the public reported one of the funnel clouds in the town of Peoria, near the Padres field. Later that afternoon, at 1730MST, another funnel was captured on video about 4 miles to the northeast of Wittmann. The funnels were noteworthy and generated media attention due to their rarity, not because they caused any damage or other significant impacts. A powerful winter storm continued to slowly push eastward across Arizona on February 22nd. In addition to generating moderate to heavy desert rain and higher elevation snow the storm produced a couple of funnel clouds, one of which occurred near the town of Wittmann. At 1730MST a member of the public captured the funnel cloud on video; the funnel was located about 4 miles northeast of the town. Although the funnel never touched ground and produced no damage, it was noteworthy due to its rarity and as such generated some media attention.", "ts_dict_index": [4995, 4996, 4997]}
+{"event_id": 1051017, "event_type": "Funnel Cloud", "state": "MINNESOTA", "cz_name": "DAKOTA", "begin_date_time": "2022-08-27 21:24:00", "end_date_time": "2022-08-27 21:24:00", "narrative": "Several waves of storms moved across southern Minnesota during the morning and afternoon of Saturday, August 27th. During the late afternoon and early evening, a stronger storm developed over south central Minnesota and quickly moved northeast and produced a bow-echo segment. This bow-echo segment took on the characteristic of a QLCS and produced several circulations across the south and southeastern Twin Cities metro area. Some of these circulations produced EF0 tornado damage from Apple Valley, northeast to Eagan, West St. Paul, and the east side of St. Paul and Maplewood. Most of the damage was associated with large trees blown down or uprooted. A few of the larger trees landed on buildings and a trailer park west of the Minnesota Zoo and caused damage to those structures. A storm chaser took video of a funnel cloud. The funnel may have made ground contact, but it was not possible to verify that. No damage was reported. The location was approximated based on the video.", "ts_dict_index": [5019, 5020, 5021]}
+{"event_id": 894179, "event_type": "Funnel Cloud", "state": "ILLINOIS", "cz_name": "LA SALLE", "begin_date_time": "2020-05-18 12:50:00", "end_date_time": "2020-05-18 12:50:00", "narrative": "Heavy rain fell across many areas of northeast Illinois on May 17th producing widespread flooding which continued into May 18th.  Two brief tornadoes also occurred during the afternoon of May 17th.  Scattered showers produced a few funnel clouds on May 18th.  Some of the highest 48 hour rainfall totals ending Monday morning May 18th included 8.61 inches in River Forest; 5.18 inches near Oak Forest; 4.75 inches near Burr Ridge; 4.70 inches three miles southwest of Midway Airport; 4.59 inches in Palos Heights; 4.14 inches in Burr Ridge; 3.99 inches in Joliet; 3.88 inches in Harwood Heights; 3.80 inches at the National Weather Service office in Romeoville; 3.73 inches in Algonquin; 3.60 inches near Manhattan; 3.59 inches in Minooka; 3.59 inches at Chicago O'Hare Airport (ORD) and 3.32 inches in Cary. A funnel cloud extended about one third of the way to the ground and then dissipated.", "ts_dict_index": [5007, 5008, 5009]}
+{"event_id": 883643, "event_type": "Funnel Cloud", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2020-05-26 16:56:00", "end_date_time": "2020-05-26 16:58:00", "narrative": "The afternoon of Tuesday, May 26th, a surface low was noted in southwest Iowa with a broad area of southeast flow along a surface boundary northward across southern Minnesota. Scattered thunderstorms started to develop in the warm sector by the mid afternoon across western Wisconsin and Iowa. These storms moved northward into an area of MLCAPEs of 1500-2000 J/kg with bulk shear values of around 30 knots. Radar indicated that numerous storms were rotating along the boundary as they moved northward. Most of the storms produced funnel clouds, but two storms caused an EF0 tornado east of Albert Lea, and another in the southeast Twin Cities suburbs of Rosemount. A line of storms that moved northward across southeast Minnesota produced wind damage in Kenyon. A rope funnel was observed and photographed.", "ts_dict_index": [5037, 5038, 5039]}
+{"event_id": 894178, "event_type": "Funnel Cloud", "state": "ILLINOIS", "cz_name": "LA SALLE", "begin_date_time": "2020-05-18 13:28:00", "end_date_time": "2020-05-18 13:28:00", "narrative": "Heavy rain fell across many areas of northeast Illinois on May 17th producing widespread flooding which continued into May 18th.  Two brief tornadoes also occurred during the afternoon of May 17th.  Scattered showers produced a few funnel clouds on May 18th.  Some of the highest 48 hour rainfall totals ending Monday morning May 18th included 8.61 inches in River Forest; 5.18 inches near Oak Forest; 4.75 inches near Burr Ridge; 4.70 inches three miles southwest of Midway Airport; 4.59 inches in Palos Heights; 4.14 inches in Burr Ridge; 3.99 inches in Joliet; 3.88 inches in Harwood Heights; 3.80 inches at the National Weather Service office in Romeoville; 3.73 inches in Algonquin; 3.60 inches near Manhattan; 3.59 inches in Minooka; 3.59 inches at Chicago O'Hare Airport (ORD) and 3.32 inches in Cary. Two funnel clouds were reported in the Tonica and Leonore areas.", "ts_dict_index": [5004, 5005, 5006]}
+{"event_id": 894177, "event_type": "Funnel Cloud", "state": "ILLINOIS", "cz_name": "LA SALLE", "begin_date_time": "2020-05-18 10:50:00", "end_date_time": "2020-05-18 10:50:00", "narrative": "Heavy rain fell across many areas of northeast Illinois on May 17th producing widespread flooding which continued into May 18th.  Two brief tornadoes also occurred during the afternoon of May 17th.  Scattered showers produced a few funnel clouds on May 18th.  Some of the highest 48 hour rainfall totals ending Monday morning May 18th included 8.61 inches in River Forest; 5.18 inches near Oak Forest; 4.75 inches near Burr Ridge; 4.70 inches three miles southwest of Midway Airport; 4.59 inches in Palos Heights; 4.14 inches in Burr Ridge; 3.99 inches in Joliet; 3.88 inches in Harwood Heights; 3.80 inches at the National Weather Service office in Romeoville; 3.73 inches in Algonquin; 3.60 inches near Manhattan; 3.59 inches in Minooka; 3.59 inches at Chicago O'Hare Airport (ORD) and 3.32 inches in Cary. ", "ts_dict_index": [5010, 5011, 5012]}
+{"event_id": 883641, "event_type": "Funnel Cloud", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2020-05-26 16:10:00", "end_date_time": "2020-05-26 16:14:00", "narrative": "The afternoon of Tuesday, May 26th, a surface low was noted in southwest Iowa with a broad area of southeast flow along a surface boundary northward across southern Minnesota. Scattered thunderstorms started to develop in the warm sector by the mid afternoon across western Wisconsin and Iowa. These storms moved northward into an area of MLCAPEs of 1500-2000 J/kg with bulk shear values of around 30 knots. Radar indicated that numerous storms were rotating along the boundary as they moved northward. Most of the storms produced funnel clouds, but two storms caused an EF0 tornado east of Albert Lea, and another in the southeast Twin Cities suburbs of Rosemount. A line of storms that moved northward across southeast Minnesota produced wind damage in Kenyon. A deputy and several others observed a funnel cloud for several minutes. The funnel was also photographed.", "ts_dict_index": [5034, 5035, 5036]}
+{"event_id": 883642, "event_type": "Funnel Cloud", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2020-05-26 16:45:00", "end_date_time": "2020-05-26 16:56:00", "narrative": "The afternoon of Tuesday, May 26th, a surface low was noted in southwest Iowa with a broad area of southeast flow along a surface boundary northward across southern Minnesota. Scattered thunderstorms started to develop in the warm sector by the mid afternoon across western Wisconsin and Iowa. These storms moved northward into an area of MLCAPEs of 1500-2000 J/kg with bulk shear values of around 30 knots. Radar indicated that numerous storms were rotating along the boundary as they moved northward. Most of the storms produced funnel clouds, but two storms caused an EF0 tornado east of Albert Lea, and another in the southeast Twin Cities suburbs of Rosemount. A line of storms that moved northward across southeast Minnesota produced wind damage in Kenyon. Two funnel clouds were observed and photographed. These funnel clouds were observed for approximately 10-15 minutes as the storm associated with the funnel clouds moved northward.", "ts_dict_index": [5031, 5032, 5033]}
+{"event_id": 896793, "event_type": "Funnel Cloud", "state": "WISCONSIN", "cz_name": "POLK", "begin_date_time": "2020-07-21 16:37:00", "end_date_time": "2020-07-21 16:38:00", "narrative": "During the afternoon of Tuesday, July 21st, a few thunderstorms developed along a frontal boundary over east-central Minnesota. Several spotters and storm chasers were following these storms as the storms moved into Wisconsin. ||The storm that moved into Polk County had a consistent funnel cloud associated with it with a brief tornado touchdown near Clear Lake and then again near Arland. Another storm developed across northern Dunn County and produced an EF0 tornado northeast of Wheeler. More storms developed over southeast Dunn and central Chippewa Counties to produce the majority of the damage. ||The worst damage occurred in the city of Cadott where numerous trees, power lines and a few structures were damaged as it moved through the town before dissipating.||The two tornadoes in Chippewa County had an average path length of 3 to 4 miles and an average width of 75 yards. A storm chaser took video of a funnel cloud. It is possible it may have been on the ground, but the video was inconclusive.", "ts_dict_index": [4971, 4972, 4973]}
+{"event_id": 1033061, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2022-06-07 19:00:00", "end_date_time": "2022-06-07 19:05:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. There were several reports of hail ranging from 2-4 inch diameter in and near Ravenna. Widespread home siding and window damage was reported. Vehicles sustained damage, including shattered windows and windshields of the town's fire trucks.", "ts_dict_index": [5061, 5062, 5063]}
+{"event_id": 1044214, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-07 20:26:00", "end_date_time": "2022-06-07 20:26:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. An NeRAIN observer reported hail up to ping pong ball size.", "ts_dict_index": [5058, 5059, 5060]}
+{"event_id": 799410, "event_type": "Funnel Cloud", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-02-22 14:30:00", "end_date_time": "2019-02-22 14:35:00", "narrative": "A powerful and slow moving winter storm moved across Arizona from February 21st into the 22nd; the storm brought locally heavy rain to much of south-central Arizona as well as heavy mountain snow. Although conditions were not overly unstable during the afternoon, they were sufficient to allow for the generation of isolated thunderstorms. On February 21st, a strong storm generated wind damage in Tolleson. On the 22nd, the storms produced a pair of funnel clouds. At 1435MST the public reported one of the funnel clouds in the town of Peoria, near the Padres field. Later that afternoon, at 1730MST, another funnel was captured on video about 4 miles to the northeast of Wittmann. The funnels were noteworthy and generated media attention due to their rarity, not because they caused any damage or other significant impacts. A powerful winter storm continued to push east across Arizona on February 22nd; although the storm mainly generated moderate to heavy desert rain and higher elevation snow, it also produced a couple of funnel clouds during the afternoon hours. One such funnel cloud was reported in the town of Peoria. At 1435MST, a member of the public reported a funnel cloud  just to the southwest of Padres field, about 1 mile northeast of Peoria. Radar data confirmed the rotation within this funnel. As the funnel did not touch the ground, no damage resulted, however due to the rarity of funnel clouds it generated some media attention.", "ts_dict_index": [4998, 4999, 5000]}
+{"event_id": 823518, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2019-05-27 20:59:00", "end_date_time": "2019-05-27 21:09:00", "narrative": "Severe hail and winds occurred in a few spots, along with a brief tornado on this Memorial Day (Monday) evening. However, the biggest story was repeated waves of heavy rain from the 26th that resulted in extensive flooding, and more heavy rain was to come. During the evening, several thunderstorms developed over north central Kansas. All but one of these storms moved northeast into south central Nebraska and affected areas mainly along and east of Highway 281 between 830 and 1130 PM CST. These storms generally remained sub-severe, but a brief EF-0 tornado occurred in Superior at 945 PM CST. The storms had congealed and become quasi-linear, but the low-level and deep-layer shear and SRH were very high, resulting in a shear-dominant line with the most intense cores at the back edge of the line. Along the updraft-downdraft convergence zone, a very small, brief mesovortex formed and produced the tornado. This occurred within a developing bookend vortex, just north of the rear-inflow notch. The one storm that moved different from all the others was a left-moving supercell that originated from a cell split over Rooks county Kansas. That storm moved due north from Alma to Kearney to Loup City from 8 to 945 PM CST, producing quarter size hail in Wilcox and 1 to 2 inch hail in Kearney. Meanwhile, scattered thunderstorms were on-going over southwest Nebraska. These storms entered western Dawson county around 10 PM CST, and during the following two hours these storms organized into a squall line that extended from Ord to Loup City to Lexington to near McCook by 12 AM CST. These storms produced golf ball size hail in and east of Gothenburg, and measured winds of 58 MPH at Cozad. Quarter size hail also occurred in Miller and Ravenna. This line broken into two separate lines, one of which moved east between Interstate 80 and Highway 6, and the other north of the Interstate. The storms remained sub-severe, but a wind gust of 55 MPH was measured at the Hastings airport, and nickel size hail occurred in York. A third cluster of scattered storms developed over southwest Nebraska around midnight. These storms consolidated into a multicell cluster and moved from west to east across the region from 2 to 530 AM CST Tuesday the 28th. These storms were not severe, but they added to the rainfall totals. Total rainfall amounts from all three thunderstorm episodes were not excessive, but given that 2 to 4 inches fell across a large portion of south central Nebraska just 24 hours before, an additional 1 to 2 inches was not needed. ||Water levels were already rising on area creeks and rivers from the heavy rain Sunday night. Flooding began to occur as an increasing number of creeks and rivers overflowed their banks through the day. Minor flooding began around sunrise Monday on the upper portions of the Little Blue River from southeastern Adams county into northern Nuckolls county. The Republican River at Riverton had also risen above flood stage. Thompson Creek, which also passes through Riverton, rapidly increased to moderate flood stage. Whatever impacts might have occurred were not known. In Polk county, extensive flooding resulted in numerous road closures. Bridges on gravel roads had water flowing over them. Highway 81 between Osceola and Shelby was closed because it was impassable. The emergency manager stated that the flooding was worse than what occurred in March of this year. Throughout the day, extensive flooding developed over more and more low-lying areas, creeks, and rivers in south central Nebraska. Numerous mostly gravel roads were impassable. All of the counties along and south of the Platte River were affected, although the Platte River itself did not flood. As flooding worsened along the Little Blue River, the Crystal Lake State Recreation Area near Ayr had to be evacuated and closed. Highway 5 north of Deshler was closed due to the Little Blue River. U.S. Highway 6 near Sutton was closed due to floodwater covering the road. The Republican River also went into flood from Guide Rock to Hardy. Across Hamilton, York, and Polk counties, the West Fork of the Big Blue River, the Big Blue River, Lincoln Creek, and Beaver Creek all flooded. In Merrick county, extensive flooding occurred due to Prairie and Silver Creeks. In Dawson and Buffalo counties, Buffalo and Spring Creeks flooded, as well as Mud Creek near Ravenna. Prairie Dog Creek also flooded southwest of Harlan County Lake. This was the second significant flood to occur since the record and near-record flooding in March 2019.||A quasi-stationary front extended from the Mid-Atlantic across the Midwest to low pressure over Iowa. The front then extended southwest across Nebraska and Kansas to another low over Colorado. In the upper-levels, a longwave trough was over the western U.S., with a fairly flat ridge over the east. An upper low moved from Nevada into Utah through the day with southwest flow over the Central Plains. Just before the storms moved into south central Nebraska, temperatures were in the 70s, with dewpoints in the 60s. Despite low mid-level lapse rates, MUCAPE was between 2000 and 3000 J/kg. Deep layer shear was very strong (60-70 kt), with 0-3 km SRH 250-500 m2/s2, with the highest values on the cool side of the front, where low-level winds were most-backed. The persistence of the atmosphere to initiate multiple thunderstorm episodes was impressive, but even more impressive was that they each moved downstream over the same area, between the surface and 850 mb fronts. The initial storms clearly did not exhaust the instability. Through the night, the low over Colorado moved into western Kansas. This maintained the low-level jet, which terminated at the 850 mb front. The low-level jet did not move. The 850 mb front remained stalled near the Kansas-Nebraska border, along with the terminus of maximum 850 mb moisture transport and the 850 mb theta-e ridge. Hail ranging in size from 1 to 2 inches in diameter was reported across Kearney.", "ts_dict_index": [5091, 5092, 5093]}
+{"event_id": 1013515, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2022-04-29 16:10:00", "end_date_time": "2022-04-29 16:15:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Hail ranging in size from nickels to golf balls was reported in Kearney.", "ts_dict_index": [5064, 5065, 5066]}
+{"event_id": 1013499, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2022-04-29 14:43:00", "end_date_time": "2022-04-29 14:43:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Report from Facebook stated the largest stone was measured at 2.7 inches in diameter.", "ts_dict_index": [5073, 5074, 5075]}
+{"event_id": 823513, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2019-05-27 23:12:00", "end_date_time": "2019-05-27 23:12:00", "narrative": "Severe hail and winds occurred in a few spots, along with a brief tornado on this Memorial Day (Monday) evening. However, the biggest story was repeated waves of heavy rain from the 26th that resulted in extensive flooding, and more heavy rain was to come. During the evening, several thunderstorms developed over north central Kansas. All but one of these storms moved northeast into south central Nebraska and affected areas mainly along and east of Highway 281 between 830 and 1130 PM CST. These storms generally remained sub-severe, but a brief EF-0 tornado occurred in Superior at 945 PM CST. The storms had congealed and become quasi-linear, but the low-level and deep-layer shear and SRH were very high, resulting in a shear-dominant line with the most intense cores at the back edge of the line. Along the updraft-downdraft convergence zone, a very small, brief mesovortex formed and produced the tornado. This occurred within a developing bookend vortex, just north of the rear-inflow notch. The one storm that moved different from all the others was a left-moving supercell that originated from a cell split over Rooks county Kansas. That storm moved due north from Alma to Kearney to Loup City from 8 to 945 PM CST, producing quarter size hail in Wilcox and 1 to 2 inch hail in Kearney. Meanwhile, scattered thunderstorms were on-going over southwest Nebraska. These storms entered western Dawson county around 10 PM CST, and during the following two hours these storms organized into a squall line that extended from Ord to Loup City to Lexington to near McCook by 12 AM CST. These storms produced golf ball size hail in and east of Gothenburg, and measured winds of 58 MPH at Cozad. Quarter size hail also occurred in Miller and Ravenna. This line broken into two separate lines, one of which moved east between Interstate 80 and Highway 6, and the other north of the Interstate. The storms remained sub-severe, but a wind gust of 55 MPH was measured at the Hastings airport, and nickel size hail occurred in York. A third cluster of scattered storms developed over southwest Nebraska around midnight. These storms consolidated into a multicell cluster and moved from west to east across the region from 2 to 530 AM CST Tuesday the 28th. These storms were not severe, but they added to the rainfall totals. Total rainfall amounts from all three thunderstorm episodes were not excessive, but given that 2 to 4 inches fell across a large portion of south central Nebraska just 24 hours before, an additional 1 to 2 inches was not needed. ||Water levels were already rising on area creeks and rivers from the heavy rain Sunday night. Flooding began to occur as an increasing number of creeks and rivers overflowed their banks through the day. Minor flooding began around sunrise Monday on the upper portions of the Little Blue River from southeastern Adams county into northern Nuckolls county. The Republican River at Riverton had also risen above flood stage. Thompson Creek, which also passes through Riverton, rapidly increased to moderate flood stage. Whatever impacts might have occurred were not known. In Polk county, extensive flooding resulted in numerous road closures. Bridges on gravel roads had water flowing over them. Highway 81 between Osceola and Shelby was closed because it was impassable. The emergency manager stated that the flooding was worse than what occurred in March of this year. Throughout the day, extensive flooding developed over more and more low-lying areas, creeks, and rivers in south central Nebraska. Numerous mostly gravel roads were impassable. All of the counties along and south of the Platte River were affected, although the Platte River itself did not flood. As flooding worsened along the Little Blue River, the Crystal Lake State Recreation Area near Ayr had to be evacuated and closed. Highway 5 north of Deshler was closed due to the Little Blue River. U.S. Highway 6 near Sutton was closed due to floodwater covering the road. The Republican River also went into flood from Guide Rock to Hardy. Across Hamilton, York, and Polk counties, the West Fork of the Big Blue River, the Big Blue River, Lincoln Creek, and Beaver Creek all flooded. In Merrick county, extensive flooding occurred due to Prairie and Silver Creeks. In Dawson and Buffalo counties, Buffalo and Spring Creeks flooded, as well as Mud Creek near Ravenna. Prairie Dog Creek also flooded southwest of Harlan County Lake. This was the second significant flood to occur since the record and near-record flooding in March 2019.||A quasi-stationary front extended from the Mid-Atlantic across the Midwest to low pressure over Iowa. The front then extended southwest across Nebraska and Kansas to another low over Colorado. In the upper-levels, a longwave trough was over the western U.S., with a fairly flat ridge over the east. An upper low moved from Nevada into Utah through the day with southwest flow over the Central Plains. Just before the storms moved into south central Nebraska, temperatures were in the 70s, with dewpoints in the 60s. Despite low mid-level lapse rates, MUCAPE was between 2000 and 3000 J/kg. Deep layer shear was very strong (60-70 kt), with 0-3 km SRH 250-500 m2/s2, with the highest values on the cool side of the front, where low-level winds were most-backed. The persistence of the atmosphere to initiate multiple thunderstorm episodes was impressive, but even more impressive was that they each moved downstream over the same area, between the surface and 850 mb fronts. The initial storms clearly did not exhaust the instability. Through the night, the low over Colorado moved into western Kansas. This maintained the low-level jet, which terminated at the 850 mb front. The low-level jet did not move. The 850 mb front remained stalled near the Kansas-Nebraska border, along with the terminus of maximum 850 mb moisture transport and the 850 mb theta-e ridge. ", "ts_dict_index": [5088, 5089, 5090]}
+{"event_id": 1026701, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2022-05-12 13:15:00", "end_date_time": "2022-05-12 13:23:00", "narrative": "Major severe weather event unfolds across south central Nebraska during the afternoon and evening of May 12th, including wind gusts of 80 to 90 MPH. The most significant severe weather event of May 2022 occurred on a Thursday in which multiple rounds of thunderstorms wreaked havoc on essentially all of south central Nebraska at some point. The most intense severe weather, by far, was the first round. This activity actually developed over portions of west/southwest Kansas during the morning hours and moved northeast. Rapid intensification took place between 1PM and 2PM CDT as thunderstorms organized into a long line, and the first Severe Thunderstorm Warnings were issued for areas from Phillipsburg, KS to Lexington, NE. Initial storm reports ranged from quarter to ping pong ball size hail with the southern portion of the line, to widespread damaging wind gusts with the northern portion of the line across a large portion of Dawson County. Wind damage consisted of overturned pivots, uprooted trees, broken power poles, fence and roof damage, large tree limbs downed. Wind damage was widespread over central and western Dawson County where measured wind gusts of 60-70 MPH were common. Even an 82 MPH gust, which is considered ���significant severe���, was measured by a mesonet near Eddyville. Surface temperatures near 90 degrees and mixed layer CAPE values in excess of 3000 J/kg ahead of the line of thunderstorms, amidst 35kt to 50kt of southwesterly deep layer shear, allowed for continued intensification through the mid to late afternoon as the line raced northeast. Additional significant damaging wind impacts were felt across Sherman, Valley, and Greeley Counties. Valley County was another area especially hard hit. Here, several wind gusts in the 80-90 MPH range were reported, and damage was significant. Numerous trees were uprooted, pivots overturned, and outbuildings and grain bins destroyed. Another destructive aspect of this storm is that it also produced ping pong ball sized hail that was blown by the intense winds. This resulted in significant window and body damage to cars, as well as roof, siding, and window damage to homes. Additional significant wind damage was reported in and around Burwell (just barely outside this coverage area). The first round of thunderstorms exited north/northeast of the area around 3:30PM CDT, but the next round was ���hot on its heels���, and entered southern Nebraska around 4PM CDT, and quickly became severe. In fact, brief, but intense, circulations were noted on radar for a time just south and southeast of Hastings. This round affected mainly areas along and east of Highway 281. Since this region was spared from the first round, and a similar thermodynamic and kinematic environment was still in place, it���s no surprise that this round also intensified enough to produce ���significant severe��� wind gusts, most notably in a swath from Clay County northeast to Polk County. Several more 60-70 MPH wind gusts were reported in these areas, causing more overturned pivots, downed power lines, and damage to roofs, outbuildings, and grain bins. Also, intense wind gusts moved over Interstate 80 in Hamilton County, causing multiple overturned semis. This second round exited into eastern Nebraska and out of the Hastings CWA around 7PM CDT. The third and final round began to affect areas along and east Highway 183 between 7PM and 8PM CDT. The majority of this activity remained sub-severe as the greatest instability had been used up by the two previous rounds. However, a marginally severe wind gust of 59 MPH was measured at the Hastings airport shortly before 8PM. Thereafter, weakening ensued as the line became strung out and forward propagation slowed. Thunderstorms finally exited south central Nebraska between 11PM and midnight, ending a roughly 10 hour stretch of seemingly never ending severe weather!||Meteorologically speaking, this event was driven by a particularly volatile combination of intensifying shortwave ejecting from the central Rockies into the northern Plains, very unstable airmass (MUCAPE of 3000-4000 J/kg at it���s peak), and strong deep layer shear driven by 500 mb speed max of 60-70 kt. While this setup is not unheard of for mid-May, it���s certainly not very common, and for three distinct waves of thunderstorms to move through in a 10 hour period (two of which contained significant severe weather phenomena) is also not very common. From a regional perspective, the Hastings CWA was the developing grounds for a significant derecho that would propagate into the Northern Plains and Upper Mississippi Valley and go on to produce hundreds of measured severe wind gusts and wind damage reports, of which over 60 were considered ���significant severe���. Over 75 hail reports and nearly three dozen tornado reports were also reported, with the majority of tornadoes occurring in SD and MN. For 2022, this will likely be remembered as one of the most severe convective events of the year, both locally, and across the greater region. Dime to quarter size hail was accompanied by wind gusts estimated to be near 55 MPH.", "ts_dict_index": [5097, 5098, 5099]}
+{"event_id": 1013502, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2022-04-29 15:05:00", "end_date_time": "2022-04-29 15:30:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Hail ranging anywhere in size from peas to tennis balls was reported along and near this path, including in the towns of Beaver City and Hollinger.", "ts_dict_index": [5070, 5071, 5072]}
+{"event_id": 1045489, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2022-07-16 19:12:00", "end_date_time": "2022-07-16 19:12:00", "narrative": "Several strong to severe thunderstorms, some that eventually merged into a compact mesoscale convective system (MCS), rumbled southeastward across various parts of South Central Nebraska mainly between 6:30-11:30 p.m. CDT on this Saturday evening, prompting assorted reports of large hail (up to baseball size) and damaging winds (estimated up to 80 MPH) and disrupting activities at a handful of local county fairs. The most prominent narrow swath of severe activity cut through the heart of the 24-county area, focusing within 10 miles either side of a line extending from Ord-Cairo-Hastings-Davenport as an initially isolated supercell merged with a separate cluster of severe storms to its west, forming the aforementioned MCS. During it's more supercellular phase near/north of the Highway 92 corridor (mainly 6:30-8:30 p.m. CDT), a combo of both damaging winds and large hail occurred, featuring measured gusts as high as 74 MPH at Ord airport and hail ranging from golf ball to baseball size particularly within western Howard and far northwestern Hall counties. In Howard County, a stripe of significant damage to crops and windows/siding was noted from around Farwell to west of Dannebrog. As this MCS reached areas near/south of Interstate 80 (primarily 9-11 p.m. CDT) the hail threat waned but damaging winds continued, evidenced by a measured 58 MPH gust at Hastings airport and unofficial mesonet-measured gusts of 67 MPH near Nelson and 62 MPH near Davenport. Within Clay County, tree branches were downed in several communities including Trumbull, Deweese, Fairfield and Edgar. Shortly before this storm complex exited the local area to the southeast between 11:00-11:30 p.m. CDT, wind intensity ramped down to slightly sub-severe levels within southern/eastern Thayer County. Although far from the only outdoor event interruption of the evening within South Central Nebraska, one of the more noteworthy ones associated with this MCS involved the Adams County Fairfest in Hastings, where an ongoing Nelly concert was cut short and an evacuation of the grounds was successfully initiated shortly before the storm struck. Although rain totals of 1-2 inches were common within the heart of the MCS track (overall highest inF Clay County), any flooding was of the very short term/nuisance variety. To the west of the aforementioned primary swath of severe weather, a few separate and smaller-scale areas of strong to severe storms impacted portions of primarily Furnas, Buffalo and Dawson counties mainly between 7-9 p.m. CDT. In Furnas County, a relatively small but intense supercell roamed northern and eastern parts of the county, with estimated 80 MPH winds destroying an outbuilding and grain bin at a farmstead between Holbrook and Arapahoe. Meanwhile, other semi-discrete convection within parts of Buffalo/Dawson counties yielded a few wind reports including a mesonet-measured 64 MPH gust near Kearney and a slightly sub-severe 54 MPH speed near Lexington. The eastern reaches of this activity eventually merged with the primary MCS as it charged across the I-80 corridor and into the Hastings area. ||Finishing with some details regarding the evolution and meteorology behind this event, the initial development of isolated to scattered thunderstorms during the mid-late afternoon hours occurred in separate areas slightly off to  the north and also west of South Central Nebraska, with this early activity gradually increasing in both coverage/intensity as it evolved into the local area. In the mid-upper levels, forcing was fairly weak, featuring only subtle shortwave energy working into the region in west-northwest flow, directed around the northeastern periphery of a large-scale ridge centered over the Four Corners region. At the surface, there were also no significant features of note locally, with most of South Central Nebraska simply reporting 5-15 MPH east-southeasterly breezes during the afternoon. However, the initial storm development off to the north and west of the area appeared to be tied to weak convergence along a pair of subtle boundaries. Despite the aforementioned weak forcing and also weak mid level lapse rates, the environment featured plentiful low level moisture/instability and seasonably-decent deep layer wind shear of 30-40 knots. Ahead of the incoming storms, late afternoon temperatures in the upper 80s-low 90s (F) and dewpoints in the upper 60s-mid 70s promoted mixed-layer CAPE 2000-3000 J/kg. ", "ts_dict_index": [5100, 5101, 5102]}
+{"event_id": 1109315, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2023-06-29 02:00:00", "end_date_time": "2023-06-29 02:40:00", "narrative": "Although it only impacted a small portion of South Central Nebraska, this very early Thursday morning was a destructive one within a few far southern counties as one of the fiercest (if not the fiercest) supercell thunderstorm of the local 2023 convective season raged across primarily the southern halves of Furnas/Harlan counties into southwestern Franklin County...laying down a concentrated swath of large hail/damaging winds before mercifully weakening as it slid farther east into southeastern Franklin and southern Webster/Nuckolls counties. This storm/supercell cluster had actually been trucking along for quite some time before invading the local area (see event evolution details below). Per numerous storm reports (and confirmed by post-event satellite imagery), the primary west-east swath of damage was only 5-10 miles across...centered almost directly along a line from Wilsonville-Beaver City-Stamford-Alma-Naponee. Within this corridor, the combination of large hail (some stones to at least baseball size) driven by wind gusts of at least 60-70 MPH prompted countless instances of damage such as: broken windows/damaged siding at homes/businesses, flipped irrigation pivots, crops destroyed by the thousands of acres, and more isolated occurrences of significantly damaged or demolished outbuildings. This was a fairly quick-hitting event within South Central Nebraska, with the vast majority of severe weather in the unfolding over 90 minutes between 3:00-4:30 a.m. CDT. Taking a deeper dive into storm reports and the various documented (and countless undocumented) occurrences of large hail/damaging winds within the primary convective swath, a few of the more noteworthy accounts that garnered local media coverage included: a nasty combination of wind-driven hail (widespread ping pong ball up to isolated baseball size stones and 60-80 MPH winds) that shredded crops and shattered many windows/significantly damaged siding in and near Wilsonville, Beaver City, Stamford and Orleans...including at business such as the Wilsonville Post Office; estimated 80 MPH winds in southern Harlan County that topped several trees/large branches in Alma and destroyed a farm machine shed between Stamford and Orleans. Although the vast majority of severe weather reports occurred with the primary supercell along the aforementioned narrow swath, there were a few outlier occurrences including: estimated 60-70 MPH winds near Cambridge (along the far northern fringes of the main supercell) and ping pong ball size hail in Beaver City from a rogue, isolated storm that briefly flared up a few hours prior to the main event.  ||Breaking down event evolution/timing, and starting from a forecast perspective, this was not an overly-obvious setup for such a significant (albeit rather localized) severe storm event within the local area. Although some necessary ingredients were certainly present, short term/higher-resolution computer models (CAMs) varied considerably regarding how evening High Plains convection would evolve, and to what degree it would impact locales farther east (including South Central Nebraska). The 01 UTC (8 p.m. CDT) Day 1 Convective Outlook from SPC (valid through the early morning of the 29th) highlighted only a Marginal Risk (level 1 of 5) for South Central Nebraska, but also acknowledged very substantial uncertainty. In the mid-upper levels, although lacking any noteworthy, small-scale disturbances, broad and seasonably-strong west-southwesterly flow was in place over the Central Plains...downstream from a large scale, positively-tilted trough centered from the Northern Rockies to the Great Basin. At the surface, South Central Nebraska resided north of a quasi-stationary front stretched across Kansas from southwest-to-northeast, with resultant east-northeasterly breezes to the north of this boundary enhancing High Plains upslope flow. Turning to storm-scale details, the supercell that eventually roared into Furnas County actually initiated/became severe roughly 240 miles off to the west-northwest during the late afternoon of the 28th...in extreme southeast Wyoming. During the evening, the intense storm slowly lumbered southeastward through the far southwestern Nebraska Panhandle into northeast Colorado. By around midnight CDT, this convection had morphed into a powerful supercell cluster/small complex as it entered far southwestern Nebraska and started tracking more due-east...riding along the northern fringes of a tight mid-level temperature gradient (generally hugging the 12C line at 700 millibars). Out ahead of this dominant supercell, increasing low-mid level warm air advection prompted the brief flare-up of a lone strong/marginally-severe storm over Furnas/Harlan counties between 12:30-1:30 a.m. CDT (which produced ping pong ball size hail). However, this was just a small taste of what was to come a few hours later, as the notable supercell cluster reached Furnas/Harlan counties between 3-4 a.m. CDT. During the ensuing hour, this storm complex gradually weakened within Franklin/Webster counties as additional strong storms flared up out ahead of it primarily over Nuckolls/Thayer/Fillmore counties. Between 5-6 a.m. CDT the severe weather threat finally ended within South Central Nebraska for the night, as the main core of the initial supercell cluster slipped slightly south of the state line into northern Kansas, while the more widespread convection to its north remained sub-severe while gradually exiting eastward into eastern Nebraska. Although there had been considerable uncertainty whether South Central Nebraska would even see such an intense storm during the pre-dawn hours of the 29th, once it started approaching the local area from southwest Nebraska the mesoscale environment strongly supported its eastward persistence, given a formidable combination of at least 2000-3000 most-unstable CAPE and at least 50-60 knots of deep-layer wind shear. A cluster of thunderstorms sliding east just north of the Nebraska-Kansas state line produced widespread severe weather across central and southern portions of Furnas County. Hail generally up to the size of golf balls was reported across this area, though isolated larger hail fell west of Wilsonville (3 inches in diameter) and in Beaver City (baseball size). Wind gusts were estimated to be anywhere from 60 to 70 MPH, resulting in numerous reports of tree damage, including whole trees snapped and larger limbs downed. The wind-driven large hail resulted in widespread damage to crops, siding, windows, and vehicles.", "ts_dict_index": [5079, 5080, 5081]}
+{"event_id": 980676, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2021-08-22 16:46:00", "end_date_time": "2021-08-22 16:46:00", "narrative": "Between the late afternoon of Sunday the 22nd and sunrise on Monday the 23rd, primarily some southern-southwestern counties in South Central Nebraska (along with briefly a few northwestern ones) endured an active episode of strong to severe thunderstorms. Within the hardest-hit southern counties (mainly Furnas/Harlan/Franklin) there were several instances of not only severe-criteria wind/hail but also narrow swaths of very heavy rain and localized flash flooding...resulting from the highest official/measured short-fuse rain totals of the 2021 convective season within the 24-county local area. On the hail/wind side of things, a few of the more notable reports (all occurring between 5:30-11:30 p.m. CDT) included: golf ball size hail in rural northwestern Buffalo County; ping pong ball size stones near Wilsonville; several instances of estimated or measured gusts of 60-70 MPH within Furnas/Harlan counties (including a few downed trees in towns such as Alma/Orleans). However, for parts of primarily Furnas, Harlan, Franklin and Webster counties, this event's signature calling card was heavy rain and localized flooding. While the majority of those four counties received modest amounts of no more than 1-2 inches, significant training of storms dumped notably higher totals between 3-7+ in narrow swaths over the course of 6-8 hours. The most significant of these heavy rain bullseyes focused along/near the Highway 136 corridor between Orleans and Oxford, where 5-7+ was common, including an unofficial automated sensor that tallied 7.13 and nearby CoCoRaHS reports of 6.22 and 6.16. Although ground-truth reports of impactful flooding/flash flooding were sparse, a resident six miles north-northwest of Orleans confirmed that School Creek spilled out of its banks overnight, inundating a nearby gravel road for several hours and encroaching within 50 feet of his home. Despite this concentrated batch of very heavy rain falling directly onto the Republican River basin, there was no firm evidence that the Republican itself flooded before excess water flushed out into Harlan County Lake. Outside of this most notable heavy rain bullseye, other impressive area rain totals included 4.76 in Alma and 3.90 near Franklin. ||Breaking down event evolution/timing within South Central Nebraska: things got underway between 5-6 p.m. CDT as a large severe storm infiltrated southern Furnas County after initiating a bit earlier just west of the local area. During the same hour, another severe cell fired up slightly to its east over the Furnas/Harlan County line. Between 6-7 p.m. CDT these two storms merged over Harlan County before drifting slowly east across southern Franklin/Webster counties between 7-9 p.m. CDT. Meanwhile, during this same 7-9 p.m. CDT time frame but roughly 50-80 miles to the north-northeast, a separate area of scattered strong to severe activity briefly blossomed, primarily affecting parts of Buffalo, Sherman and Howard counties (and yielding a few hail reports) before fading away. Getting back to the original southern convection, the main concerns gradually transitioned from hail/wind to hydro/flooding between 9 p.m. and midnight CDT as a persistent, west-east oriented corridor of cell training focused along a line from Furnas through Webster counties (likely as a strengthening low level jet impinged upon the outflow/cold pool trailing from the earlier-evening storms). By midnight CDT this west-east corridor of training convection had thankfully lifted slightly north of its original position (more so along a line from Gosper through Kearney counties), ending the heavy rain threat for the night in the aforementioned places that had already been swamped with impressive amounts. Post-midnight, storms continued to percolate within portions of primarily Gosper/Phelps/Kearney/Webster/Nuckolls counties for a few to several more hours, but this activity was less intense and a bit more transient than the earlier round, keeping heavy rain and flooding concerns in check. By 5 a.m. CDT, the areal coverage of activity within southern local counties had waned considerably, with the last strong storm of the night affecting Nuckolls County before mostly-dissipating by sunrise. In the mid-upper levels, South Central Nebraska received a glancing blow of lift from a compact-but-potent shortwave trough swinging east-northeast from the Dakotas toward northern MN/southern Canada during the afternoon-evening. At the surface, the local area resided within a broad warm sector, slightly east-southeast of a weak cold front stalling out over western/north central Nebraska, and hundreds of miles south of a strong low pressure system (around 998 millibars) centered over southern Manitoba during the evening-overnight. Closer to home, the late afternoon initiation of robust storms near the Furnas County area was likely aided by modest moisture convergence focused slightly northeast of a secondary/weaker surface low (around 1004 millibars) along the CO/KS border. All in all, the mesoscale environment proved rather supportive of severe storms and transient supercell structures, with late afternoon parameters featuring 2000-3000 J/kg mixed layer CAPE and around 40 knots of deep-layer wind shear. ", "ts_dict_index": [5094, 5095, 5096]}
+{"event_id": 1109270, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2023-06-29 02:25:00", "end_date_time": "2023-06-29 02:25:00", "narrative": "Although it only impacted a small portion of South Central Nebraska, this very early Thursday morning was a destructive one within a few far southern counties as one of the fiercest (if not the fiercest) supercell thunderstorm of the local 2023 convective season raged across primarily the southern halves of Furnas/Harlan counties into southwestern Franklin County...laying down a concentrated swath of large hail/damaging winds before mercifully weakening as it slid farther east into southeastern Franklin and southern Webster/Nuckolls counties. This storm/supercell cluster had actually been trucking along for quite some time before invading the local area (see event evolution details below). Per numerous storm reports (and confirmed by post-event satellite imagery), the primary west-east swath of damage was only 5-10 miles across...centered almost directly along a line from Wilsonville-Beaver City-Stamford-Alma-Naponee. Within this corridor, the combination of large hail (some stones to at least baseball size) driven by wind gusts of at least 60-70 MPH prompted countless instances of damage such as: broken windows/damaged siding at homes/businesses, flipped irrigation pivots, crops destroyed by the thousands of acres, and more isolated occurrences of significantly damaged or demolished outbuildings. This was a fairly quick-hitting event within South Central Nebraska, with the vast majority of severe weather in the unfolding over 90 minutes between 3:00-4:30 a.m. CDT. Taking a deeper dive into storm reports and the various documented (and countless undocumented) occurrences of large hail/damaging winds within the primary convective swath, a few of the more noteworthy accounts that garnered local media coverage included: a nasty combination of wind-driven hail (widespread ping pong ball up to isolated baseball size stones and 60-80 MPH winds) that shredded crops and shattered many windows/significantly damaged siding in and near Wilsonville, Beaver City, Stamford and Orleans...including at business such as the Wilsonville Post Office; estimated 80 MPH winds in southern Harlan County that topped several trees/large branches in Alma and destroyed a farm machine shed between Stamford and Orleans. Although the vast majority of severe weather reports occurred with the primary supercell along the aforementioned narrow swath, there were a few outlier occurrences including: estimated 60-70 MPH winds near Cambridge (along the far northern fringes of the main supercell) and ping pong ball size hail in Beaver City from a rogue, isolated storm that briefly flared up a few hours prior to the main event.  ||Breaking down event evolution/timing, and starting from a forecast perspective, this was not an overly-obvious setup for such a significant (albeit rather localized) severe storm event within the local area. Although some necessary ingredients were certainly present, short term/higher-resolution computer models (CAMs) varied considerably regarding how evening High Plains convection would evolve, and to what degree it would impact locales farther east (including South Central Nebraska). The 01 UTC (8 p.m. CDT) Day 1 Convective Outlook from SPC (valid through the early morning of the 29th) highlighted only a Marginal Risk (level 1 of 5) for South Central Nebraska, but also acknowledged very substantial uncertainty. In the mid-upper levels, although lacking any noteworthy, small-scale disturbances, broad and seasonably-strong west-southwesterly flow was in place over the Central Plains...downstream from a large scale, positively-tilted trough centered from the Northern Rockies to the Great Basin. At the surface, South Central Nebraska resided north of a quasi-stationary front stretched across Kansas from southwest-to-northeast, with resultant east-northeasterly breezes to the north of this boundary enhancing High Plains upslope flow. Turning to storm-scale details, the supercell that eventually roared into Furnas County actually initiated/became severe roughly 240 miles off to the west-northwest during the late afternoon of the 28th...in extreme southeast Wyoming. During the evening, the intense storm slowly lumbered southeastward through the far southwestern Nebraska Panhandle into northeast Colorado. By around midnight CDT, this convection had morphed into a powerful supercell cluster/small complex as it entered far southwestern Nebraska and started tracking more due-east...riding along the northern fringes of a tight mid-level temperature gradient (generally hugging the 12C line at 700 millibars). Out ahead of this dominant supercell, increasing low-mid level warm air advection prompted the brief flare-up of a lone strong/marginally-severe storm over Furnas/Harlan counties between 12:30-1:30 a.m. CDT (which produced ping pong ball size hail). However, this was just a small taste of what was to come a few hours later, as the notable supercell cluster reached Furnas/Harlan counties between 3-4 a.m. CDT. During the ensuing hour, this storm complex gradually weakened within Franklin/Webster counties as additional strong storms flared up out ahead of it primarily over Nuckolls/Thayer/Fillmore counties. Between 5-6 a.m. CDT the severe weather threat finally ended within South Central Nebraska for the night, as the main core of the initial supercell cluster slipped slightly south of the state line into northern Kansas, while the more widespread convection to its north remained sub-severe while gradually exiting eastward into eastern Nebraska. Although there had been considerable uncertainty whether South Central Nebraska would even see such an intense storm during the pre-dawn hours of the 29th, once it started approaching the local area from southwest Nebraska the mesoscale environment strongly supported its eastward persistence, given a formidable combination of at least 2000-3000 most-unstable CAPE and at least 50-60 knots of deep-layer wind shear. Extensive home and vehicle damage was reported from hail up to baseball size, driven by wind gusts near 70 MPH.", "ts_dict_index": [5082, 5083, 5084]}
+{"event_id": 1109269, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2023-06-29 02:05:00", "end_date_time": "2023-06-29 02:05:00", "narrative": "Although it only impacted a small portion of South Central Nebraska, this very early Thursday morning was a destructive one within a few far southern counties as one of the fiercest (if not the fiercest) supercell thunderstorm of the local 2023 convective season raged across primarily the southern halves of Furnas/Harlan counties into southwestern Franklin County...laying down a concentrated swath of large hail/damaging winds before mercifully weakening as it slid farther east into southeastern Franklin and southern Webster/Nuckolls counties. This storm/supercell cluster had actually been trucking along for quite some time before invading the local area (see event evolution details below). Per numerous storm reports (and confirmed by post-event satellite imagery), the primary west-east swath of damage was only 5-10 miles across...centered almost directly along a line from Wilsonville-Beaver City-Stamford-Alma-Naponee. Within this corridor, the combination of large hail (some stones to at least baseball size) driven by wind gusts of at least 60-70 MPH prompted countless instances of damage such as: broken windows/damaged siding at homes/businesses, flipped irrigation pivots, crops destroyed by the thousands of acres, and more isolated occurrences of significantly damaged or demolished outbuildings. This was a fairly quick-hitting event within South Central Nebraska, with the vast majority of severe weather in the unfolding over 90 minutes between 3:00-4:30 a.m. CDT. Taking a deeper dive into storm reports and the various documented (and countless undocumented) occurrences of large hail/damaging winds within the primary convective swath, a few of the more noteworthy accounts that garnered local media coverage included: a nasty combination of wind-driven hail (widespread ping pong ball up to isolated baseball size stones and 60-80 MPH winds) that shredded crops and shattered many windows/significantly damaged siding in and near Wilsonville, Beaver City, Stamford and Orleans...including at business such as the Wilsonville Post Office; estimated 80 MPH winds in southern Harlan County that topped several trees/large branches in Alma and destroyed a farm machine shed between Stamford and Orleans. Although the vast majority of severe weather reports occurred with the primary supercell along the aforementioned narrow swath, there were a few outlier occurrences including: estimated 60-70 MPH winds near Cambridge (along the far northern fringes of the main supercell) and ping pong ball size hail in Beaver City from a rogue, isolated storm that briefly flared up a few hours prior to the main event.  ||Breaking down event evolution/timing, and starting from a forecast perspective, this was not an overly-obvious setup for such a significant (albeit rather localized) severe storm event within the local area. Although some necessary ingredients were certainly present, short term/higher-resolution computer models (CAMs) varied considerably regarding how evening High Plains convection would evolve, and to what degree it would impact locales farther east (including South Central Nebraska). The 01 UTC (8 p.m. CDT) Day 1 Convective Outlook from SPC (valid through the early morning of the 29th) highlighted only a Marginal Risk (level 1 of 5) for South Central Nebraska, but also acknowledged very substantial uncertainty. In the mid-upper levels, although lacking any noteworthy, small-scale disturbances, broad and seasonably-strong west-southwesterly flow was in place over the Central Plains...downstream from a large scale, positively-tilted trough centered from the Northern Rockies to the Great Basin. At the surface, South Central Nebraska resided north of a quasi-stationary front stretched across Kansas from southwest-to-northeast, with resultant east-northeasterly breezes to the north of this boundary enhancing High Plains upslope flow. Turning to storm-scale details, the supercell that eventually roared into Furnas County actually initiated/became severe roughly 240 miles off to the west-northwest during the late afternoon of the 28th...in extreme southeast Wyoming. During the evening, the intense storm slowly lumbered southeastward through the far southwestern Nebraska Panhandle into northeast Colorado. By around midnight CDT, this convection had morphed into a powerful supercell cluster/small complex as it entered far southwestern Nebraska and started tracking more due-east...riding along the northern fringes of a tight mid-level temperature gradient (generally hugging the 12C line at 700 millibars). Out ahead of this dominant supercell, increasing low-mid level warm air advection prompted the brief flare-up of a lone strong/marginally-severe storm over Furnas/Harlan counties between 12:30-1:30 a.m. CDT (which produced ping pong ball size hail). However, this was just a small taste of what was to come a few hours later, as the notable supercell cluster reached Furnas/Harlan counties between 3-4 a.m. CDT. During the ensuing hour, this storm complex gradually weakened within Franklin/Webster counties as additional strong storms flared up out ahead of it primarily over Nuckolls/Thayer/Fillmore counties. Between 5-6 a.m. CDT the severe weather threat finally ended within South Central Nebraska for the night, as the main core of the initial supercell cluster slipped slightly south of the state line into northern Kansas, while the more widespread convection to its north remained sub-severe while gradually exiting eastward into eastern Nebraska. Although there had been considerable uncertainty whether South Central Nebraska would even see such an intense storm during the pre-dawn hours of the 29th, once it started approaching the local area from southwest Nebraska the mesoscale environment strongly supported its eastward persistence, given a formidable combination of at least 2000-3000 most-unstable CAPE and at least 50-60 knots of deep-layer wind shear. Hail up to three inches in diameter resulted in numerous broken windows and siding damage. This hail was accompanied by wind gusts near 70 MPH.", "ts_dict_index": [5085, 5086, 5087]}
+{"event_id": 902701, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2020-07-08 22:25:00", "end_date_time": "2020-07-08 22:25:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. ", "ts_dict_index": [5112, 5113, 5114]}
+{"event_id": 1045486, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2022-07-16 18:35:00", "end_date_time": "2022-07-16 18:40:00", "narrative": "Several strong to severe thunderstorms, some that eventually merged into a compact mesoscale convective system (MCS), rumbled southeastward across various parts of South Central Nebraska mainly between 6:30-11:30 p.m. CDT on this Saturday evening, prompting assorted reports of large hail (up to baseball size) and damaging winds (estimated up to 80 MPH) and disrupting activities at a handful of local county fairs. The most prominent narrow swath of severe activity cut through the heart of the 24-county area, focusing within 10 miles either side of a line extending from Ord-Cairo-Hastings-Davenport as an initially isolated supercell merged with a separate cluster of severe storms to its west, forming the aforementioned MCS. During it's more supercellular phase near/north of the Highway 92 corridor (mainly 6:30-8:30 p.m. CDT), a combo of both damaging winds and large hail occurred, featuring measured gusts as high as 74 MPH at Ord airport and hail ranging from golf ball to baseball size particularly within western Howard and far northwestern Hall counties. In Howard County, a stripe of significant damage to crops and windows/siding was noted from around Farwell to west of Dannebrog. As this MCS reached areas near/south of Interstate 80 (primarily 9-11 p.m. CDT) the hail threat waned but damaging winds continued, evidenced by a measured 58 MPH gust at Hastings airport and unofficial mesonet-measured gusts of 67 MPH near Nelson and 62 MPH near Davenport. Within Clay County, tree branches were downed in several communities including Trumbull, Deweese, Fairfield and Edgar. Shortly before this storm complex exited the local area to the southeast between 11:00-11:30 p.m. CDT, wind intensity ramped down to slightly sub-severe levels within southern/eastern Thayer County. Although far from the only outdoor event interruption of the evening within South Central Nebraska, one of the more noteworthy ones associated with this MCS involved the Adams County Fairfest in Hastings, where an ongoing Nelly concert was cut short and an evacuation of the grounds was successfully initiated shortly before the storm struck. Although rain totals of 1-2 inches were common within the heart of the MCS track (overall highest inF Clay County), any flooding was of the very short term/nuisance variety. To the west of the aforementioned primary swath of severe weather, a few separate and smaller-scale areas of strong to severe storms impacted portions of primarily Furnas, Buffalo and Dawson counties mainly between 7-9 p.m. CDT. In Furnas County, a relatively small but intense supercell roamed northern and eastern parts of the county, with estimated 80 MPH winds destroying an outbuilding and grain bin at a farmstead between Holbrook and Arapahoe. Meanwhile, other semi-discrete convection within parts of Buffalo/Dawson counties yielded a few wind reports including a mesonet-measured 64 MPH gust near Kearney and a slightly sub-severe 54 MPH speed near Lexington. The eastern reaches of this activity eventually merged with the primary MCS as it charged across the I-80 corridor and into the Hastings area. ||Finishing with some details regarding the evolution and meteorology behind this event, the initial development of isolated to scattered thunderstorms during the mid-late afternoon hours occurred in separate areas slightly off to  the north and also west of South Central Nebraska, with this early activity gradually increasing in both coverage/intensity as it evolved into the local area. In the mid-upper levels, forcing was fairly weak, featuring only subtle shortwave energy working into the region in west-northwest flow, directed around the northeastern periphery of a large-scale ridge centered over the Four Corners region. At the surface, there were also no significant features of note locally, with most of South Central Nebraska simply reporting 5-15 MPH east-southeasterly breezes during the afternoon. However, the initial storm development off to the north and west of the area appeared to be tied to weak convergence along a pair of subtle boundaries. Despite the aforementioned weak forcing and also weak mid level lapse rates, the environment featured plentiful low level moisture/instability and seasonably-decent deep layer wind shear of 30-40 knots. Ahead of the incoming storms, late afternoon temperatures in the upper 80s-low 90s (F) and dewpoints in the upper 60s-mid 70s promoted mixed-layer CAPE 2000-3000 J/kg. Hail up to the size of half dollars was accompanied by wind gusts in the area ranging between 60-80 MPH. Wind gusts were estimated to be near 60 MPH in Holbrook, where a few large tree limbs were downed. A few miles east of Holbrook, gusts likely closer to 80 MPH caused damage at a farmstead. An outbuilding and grain bin were destroyed, and the roof of a two-car garage was damaged.", "ts_dict_index": [5103, 5104, 5105]}
+{"event_id": 837349, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2019-06-20 21:53:00", "end_date_time": "2019-06-20 21:53:00", "narrative": "The overall most significant, widespread damaging wind event of the 2019 convective season wrought havoc across much of South Central Nebraska between the late evening of Thursday the 20th and around sunrise on Friday the 21st. The culprits were two separate linear mesoscale convective systems (MCS), with the first one by far the most impactful. This first storm complex, which traversed the area between 10:30 p.m. and 3 a.m. CDT, produced a swath of damaging winds ranging anywhere from 60 up to around 90 MPH, particularly within a corridor centered roughly 15 miles either side of a line from Cambridge-Minden-Hastings-Sutton. Within this area, there were countless reports of damage, particularly to the likes of trees (many large trees uprooted), power poles/lines and irrigation pivots, but also to some structures (mainly rural outbuildings). A short list of some of the hardest-hit communities included: Arapahoe, Oxford, Kenesaw and Hastings, with Hastings likely enduring its most widespread tree damage in roughly five years. As just a few specific instances of damage and/or measured winds: a grain bin and outbuilding were destroyed near Holbrook with irrigation pipe blown up to one-half mile; an unofficial mesonet gusted to 95 MPH near Oxford; several farm outbuildings were damaged/destroyed near Phillips with sheet metal hanging in trees. Within the Tri Cities, Hastings clearly bore the brunt of wind issues, as Grand Island and Kearney only received a glancing blow of sub-severe gusts mainly in the 40-55 MPH range. However, some places outside of the main damage swath still weren't spared from storm impacts, including in Farwell, where a lightning-induced fire damaged a portion of the fire hall. This primary linear MCS exhibited impressive radar signatures including a bookend vortex and rear inflow notch, with the system as a whole taking on a notable S-shape on reflectivity. As the initial MCS began departing the local area into eastern Nebraska, a second round of storms got underway back to the west, in response to lift above the residual cold pool. Although not nearly as intense/organized as the earlier system, this convection congealed into a northeast-southwest oriented MCS as it entered southwestern counties such as Furnas/Gosper/Harlan between 3:30-4:30 a.m. CDT. For a while, this second system remained slightly sub-severe, with peak gusts only to around 50 MPH (including 53 MPH at Hastings airport). However, some intensification to marginally-severe levels occurred between 5:30-6:30 a.m. CDT in far southeast counties, evidenced by mesonet wind gusts of 67 MPH near Superior and 60 MPH at Davenport. The back edge of this second MCS departed the local area out of Thayer County by 7 a.m. CDT, finally ending the rocky night. ||Interestingly, severe-criteria hail was very limited during this event, taking a clear backseat to damaging winds. However, a few quarter size stones were reported in and near communities such as Cambridge and Nelson. The Cambridge area was likely the hardest-hit, as copious amounts of mainly small hail combined with winds to promote fairly extensive crop damage. Rainfall-wise, the majority of South Central Nebraska measured between 0.50-1.50, holding flooding issues at bay. However, there were limited corridors of 2-3+, particularly within parts of Furnas/Gosper/Phelps counties. Including more rain that fell on the morning of the 22nd, Thayer County actually dealt with some of the worst flooding issues in the ensuing few days, such as water over several rural roads and a bridge washout north of Chester. ||Looking at the meteorological setup, this was a fairly classic recipe for intense overnight convection in the Central Plains. In the mid-upper levels, seasonably-strong, west-southwesterly flow was in place, downstream from a large-scale trough centered over the Northern Rockies. At the surface, South Central Nebraska resided just north of a west-east oriented front stretched near the Kansas border. As a low-amplitude disturbance entered southern Nebraska during the evening, this forcing combined with a very unstable airmass and increasing moisture convergence within the exit region of a 30-40 knot southerly low level jet to spark the MCS activity. By late-night standards, it was a fairly volatile mesoscale environment, featuring 2000-4000 J/kg most-unstable CAPE and 30-40 knots of deep-layer wind shear. A newspaper story wrote that a tremendous amount of mostly small hail occurred. Drifts of hail still existed at sunrise the following morning on June 21st. One farmer reported 800 to 900 acres of corn were destroyed northeast, east, and southeast of Cambridge. Corn was stripped, leaving just the stalks. Wheat that was not flattened was also damaged. Some of the larger stones near Cambridge were the size of quarters. Furnas County Emergency Management noted that significant crop damage occurred in a swath all the way from south of Cambridge to south of Arapahoe.", "ts_dict_index": [5106, 5107, 5108]}
+{"event_id": 1109267, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2023-06-28 23:45:00", "end_date_time": "2023-06-28 23:45:00", "narrative": "Although it only impacted a small portion of South Central Nebraska, this very early Thursday morning was a destructive one within a few far southern counties as one of the fiercest (if not the fiercest) supercell thunderstorm of the local 2023 convective season raged across primarily the southern halves of Furnas/Harlan counties into southwestern Franklin County...laying down a concentrated swath of large hail/damaging winds before mercifully weakening as it slid farther east into southeastern Franklin and southern Webster/Nuckolls counties. This storm/supercell cluster had actually been trucking along for quite some time before invading the local area (see event evolution details below). Per numerous storm reports (and confirmed by post-event satellite imagery), the primary west-east swath of damage was only 5-10 miles across...centered almost directly along a line from Wilsonville-Beaver City-Stamford-Alma-Naponee. Within this corridor, the combination of large hail (some stones to at least baseball size) driven by wind gusts of at least 60-70 MPH prompted countless instances of damage such as: broken windows/damaged siding at homes/businesses, flipped irrigation pivots, crops destroyed by the thousands of acres, and more isolated occurrences of significantly damaged or demolished outbuildings. This was a fairly quick-hitting event within South Central Nebraska, with the vast majority of severe weather in the unfolding over 90 minutes between 3:00-4:30 a.m. CDT. Taking a deeper dive into storm reports and the various documented (and countless undocumented) occurrences of large hail/damaging winds within the primary convective swath, a few of the more noteworthy accounts that garnered local media coverage included: a nasty combination of wind-driven hail (widespread ping pong ball up to isolated baseball size stones and 60-80 MPH winds) that shredded crops and shattered many windows/significantly damaged siding in and near Wilsonville, Beaver City, Stamford and Orleans...including at business such as the Wilsonville Post Office; estimated 80 MPH winds in southern Harlan County that topped several trees/large branches in Alma and destroyed a farm machine shed between Stamford and Orleans. Although the vast majority of severe weather reports occurred with the primary supercell along the aforementioned narrow swath, there were a few outlier occurrences including: estimated 60-70 MPH winds near Cambridge (along the far northern fringes of the main supercell) and ping pong ball size hail in Beaver City from a rogue, isolated storm that briefly flared up a few hours prior to the main event.  ||Breaking down event evolution/timing, and starting from a forecast perspective, this was not an overly-obvious setup for such a significant (albeit rather localized) severe storm event within the local area. Although some necessary ingredients were certainly present, short term/higher-resolution computer models (CAMs) varied considerably regarding how evening High Plains convection would evolve, and to what degree it would impact locales farther east (including South Central Nebraska). The 01 UTC (8 p.m. CDT) Day 1 Convective Outlook from SPC (valid through the early morning of the 29th) highlighted only a Marginal Risk (level 1 of 5) for South Central Nebraska, but also acknowledged very substantial uncertainty. In the mid-upper levels, although lacking any noteworthy, small-scale disturbances, broad and seasonably-strong west-southwesterly flow was in place over the Central Plains...downstream from a large scale, positively-tilted trough centered from the Northern Rockies to the Great Basin. At the surface, South Central Nebraska resided north of a quasi-stationary front stretched across Kansas from southwest-to-northeast, with resultant east-northeasterly breezes to the north of this boundary enhancing High Plains upslope flow. Turning to storm-scale details, the supercell that eventually roared into Furnas County actually initiated/became severe roughly 240 miles off to the west-northwest during the late afternoon of the 28th...in extreme southeast Wyoming. During the evening, the intense storm slowly lumbered southeastward through the far southwestern Nebraska Panhandle into northeast Colorado. By around midnight CDT, this convection had morphed into a powerful supercell cluster/small complex as it entered far southwestern Nebraska and started tracking more due-east...riding along the northern fringes of a tight mid-level temperature gradient (generally hugging the 12C line at 700 millibars). Out ahead of this dominant supercell, increasing low-mid level warm air advection prompted the brief flare-up of a lone strong/marginally-severe storm over Furnas/Harlan counties between 12:30-1:30 a.m. CDT (which produced ping pong ball size hail). However, this was just a small taste of what was to come a few hours later, as the notable supercell cluster reached Furnas/Harlan counties between 3-4 a.m. CDT. During the ensuing hour, this storm complex gradually weakened within Franklin/Webster counties as additional strong storms flared up out ahead of it primarily over Nuckolls/Thayer/Fillmore counties. Between 5-6 a.m. CDT the severe weather threat finally ended within South Central Nebraska for the night, as the main core of the initial supercell cluster slipped slightly south of the state line into northern Kansas, while the more widespread convection to its north remained sub-severe while gradually exiting eastward into eastern Nebraska. Although there had been considerable uncertainty whether South Central Nebraska would even see such an intense storm during the pre-dawn hours of the 29th, once it started approaching the local area from southwest Nebraska the mesoscale environment strongly supported its eastward persistence, given a formidable combination of at least 2000-3000 most-unstable CAPE and at least 50-60 knots of deep-layer wind shear. ", "ts_dict_index": [5076, 5077, 5078]}
+{"event_id": 1120248, "event_type": "Funnel Cloud", "state": "IOWA", "cz_name": "BREMER", "begin_date_time": "2023-07-28 17:05:00", "end_date_time": "2023-07-28 17:05:00", "narrative": "A cold front sank south across Iowa during the afternoon and evening of July 28th. The environment was primed for severe storms with warm moist air in place; as temperatures climbed into the 90s and dewpoints into the 70s. By afternoon MLCAPE values of 3000 J/kg were in place across much of Iowa with deep layer shear exceeding 40 kts. Such an environment supported rapid storm development along the boundary by late afternoon. Storms produced ping-pong ball to baseball sized hail along with two tornadoes, damaging confinement pens and creating easily identifiable tracks on high resolution satellite imagery through surrounding fields. As storms pushed south into the evening, the hazards transitioned to a wind threat. A micro burst occurred in Marshall County very near the ASOS, resulting in an isolated pocket of 80 to 90 mph winds. Funnel cloud reported north of Highway 3 and east of Highway 63.", "ts_dict_index": [4989, 4990, 4991]}
+{"event_id": 913258, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-08-14 17:10:00", "end_date_time": "2020-08-14 17:10:00", "narrative": "Although it only impacted a small percentage of the 24-county South Central Nebraska area, the large and intense supercell storm that marched south-southwestward for over 90 miles through several eastern counties on this Friday afternoon/early evening was likely the local area's most noteworthy individual storm of the 2020 convective season. In addition to dropping three fairly brief EF-0 tornadoes in southeastern Hamilton and northeastern Clay counties, its main calling card was large hail, with several reports of golf ball to slightly larger than baseball size stones in Clay/Nuckolls counties, and smaller hail to around quarter size as far north as Osceola. Interestingly, damaging winds were not a major player, with no ground-truth gusts in excess of 50 MPH. Focusing on specific storm reports, and starting with the three EF-0 tornadoes, they all occurred between 5-6 p.m. CDT, touching down briefly along a roughly 15-mile long corridor from near Interstate 80 a few miles south of Hampton, down to the Saronville area. Per storm surveys, the first two tornadoes were each on the ground for roughly 2 miles. While the majority of minor damage was confined to crops and trees, a lean-to shed was destroyed and a pivot overturned. As for the hail, the largest reported was 3 diameter between Clay Center and Harvard, but towns including Sutton and Nelson endured stones to at least tennis ball size. Flooding was not much of an issue, as the storm was progressive enough to keep rainfall amounts largely under one inch. ||Breaking down the meteorological background and event timing, this was actually a fairly conditional severe weather setup for South Central Nebraska, with various pros and cons for/against robust activity. In the mid-upper levels, the local area resided a fair distance south of a vigorous shortwave trough swinging across the Dakotas towards northern MN, resulting in fairly limited forcing aloft. Also working against convection (especially widespread severe) was a plume of warm mid level temperatures, with 700 millibar values of 12-14C providing a healthy cap. On the other hand, low-level forcing was seasonably-strong, as a well-defined cold front slid southeastward into the area during the afternoon. Ahead of this boundary, a significantly-unstable airmass awaited, featuring temperatures in the upper 80s-low 90s F/dewpoints upper 60s-mid 70s F, yielding formidable mixed-layer CAPE around 4000 J/kg. This extreme instability, in the presence of sufficient deep-layer wind shear around 35 knots, clearly fostered a mesoscale environment capable of stout convection. As for what actually transpired, the main show was preceded by a broken line of non-severe, likely elevated storms that passed primarily through counties south of Interstate 80 and east of Highway 281 between 12:30-3:30 p.m. CDT. About the time this innocuous early afternoon activity was departing the local area to the southeast, a broken line of true, surface-based storms got going along the front in northeast Nebraska, with the southwestern-most cell building down into the far northeast corner of South Central Nebraska (eastern Nance/northeast Merrick/northern Polk counties) between 3-4 p.m. CDT. Within an hour thereafter, this tail end Charlie storm rapidly grew into a full-blown supercell over Polk/northern York counties, producing its first marginally-severe hail reports. During the following two hours (5-7 p.m. CDT), the storm anchored itself firmly to the surface front, with new updraft generation along its western edge promoting more of a southwestward propagation and causing it to grow larger in both intensity/size, becoming more of a supercell cluster. It was during this time that the brief tornadoes occurred along the storm's far western flank, likely driven by pronounced low-level vorticity stretching along the surface front. While the sporadic tornado touchdowns were brief, the storm continued to be a prolific hail-producer as it gradually exited the local area out of Nuckolls County into northern Kansas between 7-8 p.m. CDT, ending all South Central Nebraska convection for the night. ", "ts_dict_index": [5127, 5128, 5129]}
+{"event_id": 913257, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-08-14 17:10:00", "end_date_time": "2020-08-14 17:15:00", "narrative": "Although it only impacted a small percentage of the 24-county South Central Nebraska area, the large and intense supercell storm that marched south-southwestward for over 90 miles through several eastern counties on this Friday afternoon/early evening was likely the local area's most noteworthy individual storm of the 2020 convective season. In addition to dropping three fairly brief EF-0 tornadoes in southeastern Hamilton and northeastern Clay counties, its main calling card was large hail, with several reports of golf ball to slightly larger than baseball size stones in Clay/Nuckolls counties, and smaller hail to around quarter size as far north as Osceola. Interestingly, damaging winds were not a major player, with no ground-truth gusts in excess of 50 MPH. Focusing on specific storm reports, and starting with the three EF-0 tornadoes, they all occurred between 5-6 p.m. CDT, touching down briefly along a roughly 15-mile long corridor from near Interstate 80 a few miles south of Hampton, down to the Saronville area. Per storm surveys, the first two tornadoes were each on the ground for roughly 2 miles. While the majority of minor damage was confined to crops and trees, a lean-to shed was destroyed and a pivot overturned. As for the hail, the largest reported was 3 diameter between Clay Center and Harvard, but towns including Sutton and Nelson endured stones to at least tennis ball size. Flooding was not much of an issue, as the storm was progressive enough to keep rainfall amounts largely under one inch. ||Breaking down the meteorological background and event timing, this was actually a fairly conditional severe weather setup for South Central Nebraska, with various pros and cons for/against robust activity. In the mid-upper levels, the local area resided a fair distance south of a vigorous shortwave trough swinging across the Dakotas towards northern MN, resulting in fairly limited forcing aloft. Also working against convection (especially widespread severe) was a plume of warm mid level temperatures, with 700 millibar values of 12-14C providing a healthy cap. On the other hand, low-level forcing was seasonably-strong, as a well-defined cold front slid southeastward into the area during the afternoon. Ahead of this boundary, a significantly-unstable airmass awaited, featuring temperatures in the upper 80s-low 90s F/dewpoints upper 60s-mid 70s F, yielding formidable mixed-layer CAPE around 4000 J/kg. This extreme instability, in the presence of sufficient deep-layer wind shear around 35 knots, clearly fostered a mesoscale environment capable of stout convection. As for what actually transpired, the main show was preceded by a broken line of non-severe, likely elevated storms that passed primarily through counties south of Interstate 80 and east of Highway 281 between 12:30-3:30 p.m. CDT. About the time this innocuous early afternoon activity was departing the local area to the southeast, a broken line of true, surface-based storms got going along the front in northeast Nebraska, with the southwestern-most cell building down into the far northeast corner of South Central Nebraska (eastern Nance/northeast Merrick/northern Polk counties) between 3-4 p.m. CDT. Within an hour thereafter, this tail end Charlie storm rapidly grew into a full-blown supercell over Polk/northern York counties, producing its first marginally-severe hail reports. During the following two hours (5-7 p.m. CDT), the storm anchored itself firmly to the surface front, with new updraft generation along its western edge promoting more of a southwestward propagation and causing it to grow larger in both intensity/size, becoming more of a supercell cluster. It was during this time that the brief tornadoes occurred along the storm's far western flank, likely driven by pronounced low-level vorticity stretching along the surface front. While the sporadic tornado touchdowns were brief, the storm continued to be a prolific hail-producer as it gradually exited the local area out of Nuckolls County into northern Kansas between 7-8 p.m. CDT, ending all South Central Nebraska convection for the night. Hail ranging in size from golf balls to baseballs was reported along this path. A vehicle's windshield was cracked approximately 6 miles southeast of Clay Center.", "ts_dict_index": [5130, 5131, 5132]}
+{"event_id": 1093426, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-04-18 20:16:00", "end_date_time": "2023-04-18 20:35:00", "narrative": "On this Tuesday late afternoon and evening, thunderstorms of varying strength rumbled from southwest-to-northeast across portions of South Central Nebraska mainly between 6:00-11:30 p.m. CDT. However, the vast majority of strong to severe activity focused within a 15-30 mile wide swath centered along a line from Franklin-Blue Hill-Sutton-York. Within this corridor, there were a number of reports of large hail ranging from quarter size up to tennis ball size, with the tennis ball (2.5 inch) reports out of Harvard and Stockham. There were also several instances of ping pong ball to golf ball size stones, including in or near the following communities: Blue Hill, Sutton, Edgar and Glenvil. Finally, marginally-severe, quarter to half dollar size hail reports originated from in or near places such as: Franklin, Bladen, Clay Center, Deweese and York. Large hail was clearly the main story of the evening, as there were only a few measured strong to marginally-severe gusts of 50+ MPH, a few of which were several miles removed from obvious thunderstorm outflow and were likely associated with a weak wake low. A few of the strongest detected gusts included 58 MPH in Doniphan (unofficial mesonet) and ASOS-measured gusts of 55 and 52 MPH at Grand Island and Hastings airports, respectively. ||Breaking down event evolution/timing, if anything the intensity of storms (and peak hail size) ended up being a bit surprising given the seasonably-modest and just in time nature of low-level moisture advecting northward into the area along a slow-moving surface warm front. At daybreak on the 18th, this west-east oriented front was aligned across northern Kansas, with South Central Nebraska firmly on its cool/dry side with surface dewpoints mainly only in the 20s (F). Meanwhile, in the mid-upper levels, the Central Plains resided well downstream of a large scale trough centered over the Northern Rockies. Over the course of the day, a subtle wave along the leading edges of the aforementioned parent trough entered the Central High Plains. This prompted a gradual increase in west-southwesterly, mid-upper level flow into South Central Nebraska, along with a gradual increase in south-southeasterly low-level flow, allowing slow-but-steady northward moisture transport into the lifting warm frontal zone. By late afternoon (around the time of convective initiation), a 994 millibar surface low was noted over northwest Kansas, with the attendant warm front extending into far southern Nebraska to its east, and a north-south oriented dryline trailing southward. Although still seasonably-unimpressive, surface dewpoints over the southern half of South Central Nebraska had risen well into the mid-upper 40s by this time (a surge of nearly 20 degrees over early morning values). This meager-but-sufficient low level moisture, combined with steep low-to-mid level lapse rates and convergence near the warm front/dryline intersection, was enough to initiate the first high-based storms of the afternoon over north central Kansas around 5:30 p.m. CDT. Already by 6 p.m. CDT, the first severe-warned storm of the day within South Central Nebraska had entered southern Franklin County. During the next two hours, a series of semi-discrete, strong-to-severe cells affected primarily Franklin/Webster counties. Then, between 8-10 p.m. CDT, intense elevated convection consolidated into a more cohesive line as it tracked northeastward across portions of mainly Adams/Clay/Nuckolls/Hamilton/Fillmore counties, aided by an uptick in a 40-50 knot southerly low level jet (evident at 850 millibars). Finally, between 10:00-11:30 p.m. CDT, this severe storm complex traversed York County before exiting the local area into eastern Nebraska, while other non-severe cells passed through various counties mainly along/north of Highway 92 before also departing South Central Nebraska...thus ending all local thunderstorm activity for the night. As it turned out, despite the unimpressive low level moisture magnitude, the combination of mixed-layer CAPE increasing to as high as 1000-1500 J/kg during the evening, combined with strong effective deep-layer wind shear around 50 knots, proved plenty sufficient to ignite robust updrafts. Hail up to the size of half dollars was reported along and near this path.", "ts_dict_index": [5121, 5122, 5123]}
+{"event_id": 909523, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-08-14 16:50:00", "end_date_time": "2020-08-14 16:52:00", "narrative": "Although it only impacted a small percentage of the 24-county South Central Nebraska area, the large and intense supercell storm that marched south-southwestward for over 90 miles through several eastern counties on this Friday afternoon/early evening was likely the local area's most noteworthy individual storm of the 2020 convective season. In addition to dropping three fairly brief EF-0 tornadoes in southeastern Hamilton and northeastern Clay counties, its main calling card was large hail, with several reports of golf ball to slightly larger than baseball size stones in Clay/Nuckolls counties, and smaller hail to around quarter size as far north as Osceola. Interestingly, damaging winds were not a major player, with no ground-truth gusts in excess of 50 MPH. Focusing on specific storm reports, and starting with the three EF-0 tornadoes, they all occurred between 5-6 p.m. CDT, touching down briefly along a roughly 15-mile long corridor from near Interstate 80 a few miles south of Hampton, down to the Saronville area. Per storm surveys, the first two tornadoes were each on the ground for roughly 2 miles. While the majority of minor damage was confined to crops and trees, a lean-to shed was destroyed and a pivot overturned. As for the hail, the largest reported was 3 diameter between Clay Center and Harvard, but towns including Sutton and Nelson endured stones to at least tennis ball size. Flooding was not much of an issue, as the storm was progressive enough to keep rainfall amounts largely under one inch. ||Breaking down the meteorological background and event timing, this was actually a fairly conditional severe weather setup for South Central Nebraska, with various pros and cons for/against robust activity. In the mid-upper levels, the local area resided a fair distance south of a vigorous shortwave trough swinging across the Dakotas towards northern MN, resulting in fairly limited forcing aloft. Also working against convection (especially widespread severe) was a plume of warm mid level temperatures, with 700 millibar values of 12-14C providing a healthy cap. On the other hand, low-level forcing was seasonably-strong, as a well-defined cold front slid southeastward into the area during the afternoon. Ahead of this boundary, a significantly-unstable airmass awaited, featuring temperatures in the upper 80s-low 90s F/dewpoints upper 60s-mid 70s F, yielding formidable mixed-layer CAPE around 4000 J/kg. This extreme instability, in the presence of sufficient deep-layer wind shear around 35 knots, clearly fostered a mesoscale environment capable of stout convection. As for what actually transpired, the main show was preceded by a broken line of non-severe, likely elevated storms that passed primarily through counties south of Interstate 80 and east of Highway 281 between 12:30-3:30 p.m. CDT. About the time this innocuous early afternoon activity was departing the local area to the southeast, a broken line of true, surface-based storms got going along the front in northeast Nebraska, with the southwestern-most cell building down into the far northeast corner of South Central Nebraska (eastern Nance/northeast Merrick/northern Polk counties) between 3-4 p.m. CDT. Within an hour thereafter, this tail end Charlie storm rapidly grew into a full-blown supercell over Polk/northern York counties, producing its first marginally-severe hail reports. During the following two hours (5-7 p.m. CDT), the storm anchored itself firmly to the surface front, with new updraft generation along its western edge promoting more of a southwestward propagation and causing it to grow larger in both intensity/size, becoming more of a supercell cluster. It was during this time that the brief tornadoes occurred along the storm's far western flank, likely driven by pronounced low-level vorticity stretching along the surface front. While the sporadic tornado touchdowns were brief, the storm continued to be a prolific hail-producer as it gradually exited the local area out of Nuckolls County into northern Kansas between 7-8 p.m. CDT, ending all South Central Nebraska convection for the night. Hail ranging in size from half dollars to baseballs was reported in Sutton.", "ts_dict_index": [5124, 5125, 5126]}
+{"event_id": 1013391, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2022-04-28 23:00:00", "end_date_time": "2022-04-28 23:00:00", "narrative": "From the late afternoon of Thursday the 28th into the very early morning of Friday the 29th, strong to severe thunderstorms impacted a few far southwestern and also northern counties of South Central Nebraska, yielding primarily large hail and localized heavy rain, but also one brief, weak tornado. This tornado, spawned by the most intense supercell storm of the day that primarily impacted Harlan County, consisted of a narrow, dusty circulation that tracked along a short path in a rural area south-southwest of Alma (as captured by storm chaser video). Both zones of local convection yielded severe-criteria hail, with the largest reported stones of 1.5 to 2 inches occurring in the Oxford, Alma, Holbrook and Cambridge vicinities. The northern area of storms featured quarter size hail reports from Loup City and Elba, along with a mesonet-measured 59 MPH wind gust in northeastern Nance County (this was actually the only known severe-criteria gust of the event). Rainfall-wise, while most places affected by storms received no more than 1.50 inches, portions of primarily southern Harlan and northern Furnas counties measured at least 2.50-3.00, including an unofficial mesonet with 3.96 south of Alma and a CoCoRaHS report of 3.05 in Arapahoe. However, there were no ground-truth reports of significant flooding. ||Breaking down event evolution/timing within each main area of convection and starting with the more intense southwestern activity: things got going between 4-5 p.m. CDT as an isolated supercell fired up over the northern Furnas-Harlan County border, initiating in a zone of modest surface moisture convergence along a weak trough axis extending northeastward out of western KS. Over the next few hours, this stout storm drifted very slowly south-southeastward through much of Harlan County, finally exiting the state southward into KS by around 7:30 p.m. CDT. In the wake of the departed supercell, scattered storms began developing (and re-developing) within Furnas, Harlan, southern Gosper and southern Phelps counties for several hours, in response to lift within the nose of a gradually-strengthening low level jet. Through 10:30 p.m. CDT most of this activity remained fairly weak, but especially between 11 p.m-1 a.m. CDT a west-east oriented band intensified over northern Furnas County, dropping hail to at least golf ball size in spots before lifting into southern Gosper County and weakening/dissipating by 2 a.m. CDT. Turning to the completely separate area of strong to severe storms farther north: a broken, east-northeast to west-southwest oriented line of convection first got underway within Valley/Greeley counties between 4:30-6:30 p.m. CDT, focused along a quasi-stationary front draped across central NE. Through 9 p.m. CDT, strong to briefly-severe storms remained mainly north of Highway 92 as they drifted slowly south-southeast, gradually weakening and congealing into a more solid line. Between 9-11 p.m. CDT the eastern reaches of this convection sagged as far south as Hamilton/York counties but was non-severe. By midnight CDT the vast majority of local eastern counties were storm-free, and largely remained so through the rest of the night. In the mid-upper levels, this was a weakly-forced event as South Central Nebraska resided under fairly benign quasi-zonal flow (even subtle weak ridging), well-downstream from a larger-scale trough still well off to the west during the evening (over the Intermountain West). As a result, deep-layer wind shear was not overly-strong, averaging just 30-35 knots. In addition, low-level moisture was seasonably-modest, with surface dewpoints peaking only mid-50s F. However, due in part to afternoon temperatures climbing a bit higher than anticipated (highs mid-80s F), mixed-layer CAPE topped out as high as 1500-2000 J/kg. Ultimately, the combination of healthy instability, modest shear, modest convergence along the aforementioned surface boundaries and eventually an increasing low level jet proved sufficient to drive limited areal coverage of intense convection, most notably the Harlan County supercell. ", "ts_dict_index": [5133, 5134, 5135]}
+{"event_id": 1093416, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-04-18 20:03:00", "end_date_time": "2023-04-18 20:13:00", "narrative": "On this Tuesday late afternoon and evening, thunderstorms of varying strength rumbled from southwest-to-northeast across portions of South Central Nebraska mainly between 6:00-11:30 p.m. CDT. However, the vast majority of strong to severe activity focused within a 15-30 mile wide swath centered along a line from Franklin-Blue Hill-Sutton-York. Within this corridor, there were a number of reports of large hail ranging from quarter size up to tennis ball size, with the tennis ball (2.5 inch) reports out of Harvard and Stockham. There were also several instances of ping pong ball to golf ball size stones, including in or near the following communities: Blue Hill, Sutton, Edgar and Glenvil. Finally, marginally-severe, quarter to half dollar size hail reports originated from in or near places such as: Franklin, Bladen, Clay Center, Deweese and York. Large hail was clearly the main story of the evening, as there were only a few measured strong to marginally-severe gusts of 50+ MPH, a few of which were several miles removed from obvious thunderstorm outflow and were likely associated with a weak wake low. A few of the strongest detected gusts included 58 MPH in Doniphan (unofficial mesonet) and ASOS-measured gusts of 55 and 52 MPH at Grand Island and Hastings airports, respectively. ||Breaking down event evolution/timing, if anything the intensity of storms (and peak hail size) ended up being a bit surprising given the seasonably-modest and just in time nature of low-level moisture advecting northward into the area along a slow-moving surface warm front. At daybreak on the 18th, this west-east oriented front was aligned across northern Kansas, with South Central Nebraska firmly on its cool/dry side with surface dewpoints mainly only in the 20s (F). Meanwhile, in the mid-upper levels, the Central Plains resided well downstream of a large scale trough centered over the Northern Rockies. Over the course of the day, a subtle wave along the leading edges of the aforementioned parent trough entered the Central High Plains. This prompted a gradual increase in west-southwesterly, mid-upper level flow into South Central Nebraska, along with a gradual increase in south-southeasterly low-level flow, allowing slow-but-steady northward moisture transport into the lifting warm frontal zone. By late afternoon (around the time of convective initiation), a 994 millibar surface low was noted over northwest Kansas, with the attendant warm front extending into far southern Nebraska to its east, and a north-south oriented dryline trailing southward. Although still seasonably-unimpressive, surface dewpoints over the southern half of South Central Nebraska had risen well into the mid-upper 40s by this time (a surge of nearly 20 degrees over early morning values). This meager-but-sufficient low level moisture, combined with steep low-to-mid level lapse rates and convergence near the warm front/dryline intersection, was enough to initiate the first high-based storms of the afternoon over north central Kansas around 5:30 p.m. CDT. Already by 6 p.m. CDT, the first severe-warned storm of the day within South Central Nebraska had entered southern Franklin County. During the next two hours, a series of semi-discrete, strong-to-severe cells affected primarily Franklin/Webster counties. Then, between 8-10 p.m. CDT, intense elevated convection consolidated into a more cohesive line as it tracked northeastward across portions of mainly Adams/Clay/Nuckolls/Hamilton/Fillmore counties, aided by an uptick in a 40-50 knot southerly low level jet (evident at 850 millibars). Finally, between 10:00-11:30 p.m. CDT, this severe storm complex traversed York County before exiting the local area into eastern Nebraska, while other non-severe cells passed through various counties mainly along/north of Highway 92 before also departing South Central Nebraska...thus ending all local thunderstorm activity for the night. As it turned out, despite the unimpressive low level moisture magnitude, the combination of mixed-layer CAPE increasing to as high as 1000-1500 J/kg during the evening, combined with strong effective deep-layer wind shear around 50 knots, proved plenty sufficient to ignite robust updrafts. Hail ranging in size from quarters to golf balls was reported along and near this path.", "ts_dict_index": [5118, 5119, 5120]}
+{"event_id": 907658, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2020-07-09 01:00:00", "end_date_time": "2020-07-09 01:10:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Quarter to golf ball size hail was reported.", "ts_dict_index": [5109, 5110, 5111]}
+{"event_id": 848465, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2019-09-30 17:19:00", "end_date_time": "2019-09-30 17:34:00", "narrative": "Thunderstorms produced a lot of severe hail on this Monday afternoon and evening. Thirty-one reports of hail were received with the largest the size of tennis balls. Just after 4 PM CST, the first storm began moving into Harlan county from north central Kansas. This supercell storm dropped quarter size hail west of Alma. Between 415 and 430 PM CST, this storm split. The left-mover moved north-northeast along the Phelps-Kearney county line into Buffalo county. Multiple reports of hail were received over south central Buffalo county, including on the west and north sides of Kearney, where quarter to ping pong ball size hail fell. Hail up to two inches in diameter occurred north of Riverdale and east of Amherst. This long-lived storm continued moving north-northeast, producing severe hail across parts of Sherman, Howard, and Greeley counties through 630 PM CST. The largest hail was the size of tennis balls between Loup City and Rockville. The right-moving storm continued producing severe hail up to ping pong ball size from northern Franklin into southwest Adams county. While these two storms were in progress, other scattered storms developed, forming a broken line from near McCook northeast to near Columbus. Another supercell formed over northern Kansas and moved into Furnas county. Between 515 and 530 PM CST, this supercell split, with the left-mover producing 2 to 2.5 inch hail between Cambridge and Holbrook. This storm moved north-northeast across Gosper and Dawson counties through 630 PM CST. The only other hail reported with this storm was the size of half dollars in the town of Eddyville. The last storm known to produce severe hail occurred at Grand Island, where nickel to quarter size hail occurred between 730 and 800 PM CST. Severe weather was not reported with any of the other storms during this event. Despite the large number of storms, the convective mode remained cellular and supercellular. The entire area of scattered storms moved northeast and out of south central Nebraska by 1030 PM CST.||These storms formed along and just north of a slow-moving cold front. This front was associated with a 1005 mb low over Minnesota. A dryline intersected the front near McCook and extended south through northwest Kansas. In the upper-levels, the longwaves were highly-amplified with an anomalous subtropical high over the Tennessee Valley, and a deep low over the Northern Rockies. Strong southwest flow was over Nebraska. Where the initial thunderstorms erupted, temperatures were in the middle 90s, with dewpoints in the lower to middle 60s. Mid-level lapse rates were poor, but MLCAPE was still between 1500 and 2200 J/kg, with a southwest-northeast gradient along the front. Deep layer shear was 40-50 kt. Effective SRH was between 150 and 200 m2/s2, with even higher values on the cold side of the front. The lack of strong forcing aloft, combined with the low-level and deep-layer shear contributed to a cellular convective mode, some of which were supercells. Most hail stones along and near this path were quarter to half dollar size, but hail up to 2 inches in diameter was reported north of Riverdale.", "ts_dict_index": [5163, 5164, 5165]}
+{"event_id": 1099527, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2023-06-09 14:20:00", "end_date_time": "2023-06-09 14:20:00", "narrative": "Primarily between 2:30-9:30 p.m. CDT on this Friday afternoon and evening, scattered to numerous thunderstorms rumbled across much of South Central Nebraska, including a varied mix of isolated pulse/single cells, multicell clusters and small-scale line segments. Like the more spotty activity the day prior, the majority of this convection was non-severe, simply producing beneficial rainfall, gusty winds of no more than 40-50 MPH and isolated pockets of very small hail. However, a handful of storms became strong to marginally-severe. Ground-truth reports were quite limited, but included nickel size hail near Holbrook and a measured wind gust to 59 MPH near Shickley (unofficial mesonet). Based on radar data, marginally-severe storms might have also affected at least small portions of the following counties, but with no verification: Greeley, Howard, Nance and Gosper. Rainfall-wise, amounts across the 24-county area were highly variable, with most areas receiving no more than one-quarter to one-half inch, but ranging from hardly a drop in some spots, to several small pockets at least 1-2, particularly within portions of several counties along/north of Interstate 80. However, there were no reports of impactful flooding. ||Turning to the meteorological background and event evolution, this was another case of marginally-severe convection forming in a moderately-unstable, but weakly-sheared environment. In the mid-upper levels, wind fields remained unusually weak by early-June standards, thanks to South Central Nebraska residing under broad ridging stretched across the heart of the United States from north-northwest to south-southeast...well-removed from any larger-scale troughs centered over the northeastern and northwestern states. However, on the smaller-scale, a weak disturbance (possible MCV) drifted east into South Central Nebraska during the afternoon-evening, likely supporting more widespread convective coverage versus the day before. At the surface, there were no notable features in the pre-convective environment, only light south-southeasterly breezes and hints of a weak low pressure center over Nebraska. As temperatures climbed into the upper 80s-low 90s (F) by mid-afternoon, storms readily developed in a weakly-capped environment featuring moderate mixed-layer CAPE of of 1500-2500 J/kg, but seasonably-paltry deep-layer wind shear only around 20 knots at best. The majority of convection early in the event (mainly 2:30-5:30 p.m. CDT) was more discrete in nature and focused within northern/western portions of South Central Nebraska. Thereafter, activity trended a bit more upscale/linear over the next few hours as it progressed through mainly south central/southeast local counties, before departing southeastward into mainly northern Kansas by sunset. ", "ts_dict_index": [5166, 5167, 5168]}
+{"event_id": 913696, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2020-08-16 16:53:00", "end_date_time": "2020-08-16 16:53:00", "narrative": "On this late Sunday afternoon and evening, several scattered, strong to severe storms advanced southward across various portions of South Central Nebraska, prompting many accounts of large hail and a few damaging wind gusts. While most hail was in the quarter to golf ball size range, larger stones of 2-3 diameter fell in the Chapman and Marquette areas of Merrick/Hamilton counties. Ping pong to golf ball size hail occurred in or near the following communities/locations: Fullerton, Amherst, Orleans, Harlan County Lake, Naponee and Deweese. In the Tri Cities, only Grand Island saw severe weather, as two rounds of quarter to half dollar size hail moved through, one mainly affecting the north side of town (including the airport) around 6 p.m. CDT, and another about an hour later that clipped more of the city. As for thunderstorm winds, the vast majority of gusts captured by area sensors were non-severe (generally 40-50 MPH), but there were two reports estimated around 60 MPH, one near Hampton and another at Hebron, where a few large trees were downed and a store front sustained minor damage. Given fairly progressive storm motions, rainfall totals in most affected areas were less than 1 inch during the afternoon/evening. However, combined with localized heavy rain that fell during a separate round of early morning/non-severe activity, portions of mainly eastern Clay County registered over 3 for the day (including NWS coop observer total of 3.33 six miles east-southeast of Clay Center). As a result, the later-day storms prompted some isolated flash flooding, as School Creek overtopped the paved spur road south of Saronville. ||This event was characterized by truly scattered, hit-or-miss convection, as afternoon heating and subtle convergence along/ahead of a weak cold front sagging southward into the region prompted several strong to severe storms, mainly in the form of multicells/multicell clusters, but also a few brief supercells. Nearly every county in the 24-county area observed at least a touch of thunderstorm activity. That being said, the majority of ground-truth reports concentrated in two primary areas: 1) parts of Hall/Hamilton/Merrick counties...2) a swath from eastern Furnas to far southwestern Franklin counties. A few of the first severe storms of the event flared up over Furnas/Buffalo counties between 430-530 p.m. CDT, and the final severe storm of the evening was centered over the Nuckolls County area before weakening around 9 p.m. CDT. Thereafter, a smattering of strong storms lingered within counties south of Interstate 80 through around 10:30 pm. CDT before all convection ended for the night. In total, 19 Severe Thunderstorm Warnings were issued within South Central Nebraska over the course of over four hours. Digging deeper into the meteorological setup, it's worth noting that this event exceeded forecast expectations, especially in terms of the number of severe storms. This was due in part to greater-than-expected convective instability, as afternoon surface dewpoints soared into the upper 60s-low 70 F,  promoting significant mixed-layer CAPE of at least 3000-4000 J/kg. In tandem with deep layer wind shear around 35 knots, this CAPE/shear combo proved plenty sufficient for robust convection. In the mid-upper levels, a pronounced north-northwest flow regime resided over the Central Plains, within the interface between a stout western United States ridge and a broad eastern trough. ", "ts_dict_index": [5142, 5143, 5144]}
+{"event_id": 901329, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2020-06-27 23:55:00", "end_date_time": "2020-06-27 23:55:00", "narrative": "This was an active late Saturday evening-early Sunday morning of thunderstorms across much of South Central Nebraska, featuring several reports of large hail and especially damaging winds mainly between midnight-3 a.m. CDT as two storm complexes rolled through and eventually merged. Focusing first on severe winds, most estimated or measured gusts were in the 50-70 MPH range and associated with primarily tree damage. However a few isolated structural damage reports were more suggestive of at least 75-80 MPH, including: 1) 10 power poles blown down and three grain bins destroyed (along with some overturned irrigation pivots) west of Aurora...2) grain bin damage and overturned pivots north of Minden. Hail was more limited overall, but stones reached golf ball size at Pauline and ping pong ball size in Davenport, while Hastings saw nickel to quarter size hail. Rainfall amounts varied considerably (most of South Central Nebraska had less than one-half inch), but a fairly narrow swath of at least 1.50-2.50 targeted parts of primarily Thayer/Nuckolls/Clay counties, with one unofficial report as high as 3.17 near Belvidere. Flooding was fairly minimal, although one rural road along the Fillmore/Thayer County line still had water running across it around sunrise. ||As for storm mode/evolution, this was a somewhat complex event. The first local convection of the night entered the Furnas County area out of northwest Kansas after 11 p.m. CDT, in the form of a compact linear mesoscale convective system (MCS) on a weakening trend. But then, between midnight-1 a.m. CDT, a broken band of intense, semi-discrete storms erupted out ahead of this MCS along a west-east axis centered from Phelps-Adams-Thayer counties (likely in response to the onset of a healthy low level jet). However, these initially semi-discrete storms (which accounted for all large hail reports) quickly consolidated/grew upscale into a new linear MCS that charged north-northeast across the Highway 6/Interstate 80 corridors between 1-2 a.m. CDT, gradually merging with the initial MCS racing up from the southwest in the process. During the ensuing hour, the two complexes completed a full merger; the northern end weakening as it reached far northeastern counties (such as Nance/Polk), while the southern end remained severe through Fillmore/Thayer counties before departing the local area into southeast Nebraska. This ended any severe threat for the night, although weaker storms and broader showers persisted until around sunrise in some spots. This was a ripe setup for severe nocturnal storms, especially with the exit region of a 30-40 knot southerly low level jet (evident at 850 millibars) aimed into the heart of South Central Nebraska after dark, and tapping into a large reservoir of most-unstable CAPE as high as 2000-3000 J/kg. In the mid-upper levels, flow over the region was not overly-strong, but contained various low-amplitude disturbances and was in the process of transitioning more southwesterly in response to a larger-scale trough setting up over the northwestern United States. There were no distinct surface features across the local area, but steady light southeast breezes prior to storm initiation maintained seasonably-high dewpoints in the mid-60s to low-70 F. Likely one of the main limiting factors against a more robust severe threat was only modest deep-layer wind shear around 30 knots. ", "ts_dict_index": [5145, 5146, 5147]}
+{"event_id": 873029, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2020-03-19 14:04:00", "end_date_time": "2020-03-19 14:12:00", "narrative": "On this Thursday, the first severe thunderstorms of the year occurred, followed by windy conditions and even accumulating snow in some areas. A few weak thunderstorms began forming around 1230 PM CST, with two small clusters over Harlan and Clay counties. Other showers and thunderstorms developed south of Interstate 80, and by mid-afternoon, they had moved across and to the north of the Interstate. A couple of these storms became severe and produced large amounts of hail (the freezing level was around 8,000 ft AGL). One storm turned severe from northwest Kearney county into south-central Buffalo county, where hail up to the size of ping pong balls occurred, including in the southwest part of the city of Kearney. There was a narrow swath of Interstate 80 that was covered with hail, and snowplows needed to be deployed. The other severe storm tracked from near Edgar to McCool Junction, where it also produced hail up to the size of ping pong balls. The thunderstorm activity ended by late afternoon. These storms were elevated, on the cold side of a strong cold front. As the colder temperatures near-surface moved in, and lapse rates steepened, north winds increased to 30 to 35 mph, with frequent gusts between 45 and 55 mph. There were a few higher wind gusts, including 63 mph at the Lexington airport, which was the highest gust recorded, 59 mph near Odessa, and 58 mph at Cozad and Hastings. Late in the afternoon, the thunderstorms weakened into showers which eventually morphed into stratiform rain as they encountered stability. This rain moved into increasingly colder air where it changed to snow north of a line from Lexington to Fullerton. One to 5 inches of snow fell, with most areas measuring 1 to 3 inches. The highest amounts were 5 inches near Scotia, 4 inches near Johnson Lake, with 3 inches at Greeley and Ord. Snow began accumulating during the late afternoon, and continued through the evening hours. The snow rapidly dissipated just after midnight CST.||At sunrise, a 1000 mb low pressure system was over southeast Colorado, with a warm front extending east across northern Kansas. A stationary Arctic front was over the northern Rockies and Plains. During the day, the stationary front become mobile and accelerated southward, merging with the occluded low and its fronts. The forward momentum of the Arctic air shoved the combined front south, also forcing the Colorado low to weaken as it migrated along the front into central Kansas. In the upper-levels, the longwave pattern was typical of the mean flow that had stubbornly prevailed since the middle of November. The flow over North America was split, with a trough over the western U.S. and a ridge over the Gulf of Mexico. The flow was from the southwest over the Central Plains, with a potent, intensifying shortwave trough over Colorado and New Mexico during the morning. By sunset, a small closed low had formed along the Nebraska-Kansas border. Due to the confluence of the northern and southern streams, the low quickly dissipated and, by Friday morning, all that was left was a modest shortwave trough over Wisconsin and Illinois. Hail ranged in size from nickels to half dollars. Enough hail fell to cover Interstate 80 and snow plows were dispatched to clear the road.", "ts_dict_index": [5151, 5152, 5153]}
+{"event_id": 1013390, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2022-04-28 22:15:00", "end_date_time": "2022-04-28 22:45:00", "narrative": "From the late afternoon of Thursday the 28th into the very early morning of Friday the 29th, strong to severe thunderstorms impacted a few far southwestern and also northern counties of South Central Nebraska, yielding primarily large hail and localized heavy rain, but also one brief, weak tornado. This tornado, spawned by the most intense supercell storm of the day that primarily impacted Harlan County, consisted of a narrow, dusty circulation that tracked along a short path in a rural area south-southwest of Alma (as captured by storm chaser video). Both zones of local convection yielded severe-criteria hail, with the largest reported stones of 1.5 to 2 inches occurring in the Oxford, Alma, Holbrook and Cambridge vicinities. The northern area of storms featured quarter size hail reports from Loup City and Elba, along with a mesonet-measured 59 MPH wind gust in northeastern Nance County (this was actually the only known severe-criteria gust of the event). Rainfall-wise, while most places affected by storms received no more than 1.50 inches, portions of primarily southern Harlan and northern Furnas counties measured at least 2.50-3.00, including an unofficial mesonet with 3.96 south of Alma and a CoCoRaHS report of 3.05 in Arapahoe. However, there were no ground-truth reports of significant flooding. ||Breaking down event evolution/timing within each main area of convection and starting with the more intense southwestern activity: things got going between 4-5 p.m. CDT as an isolated supercell fired up over the northern Furnas-Harlan County border, initiating in a zone of modest surface moisture convergence along a weak trough axis extending northeastward out of western KS. Over the next few hours, this stout storm drifted very slowly south-southeastward through much of Harlan County, finally exiting the state southward into KS by around 7:30 p.m. CDT. In the wake of the departed supercell, scattered storms began developing (and re-developing) within Furnas, Harlan, southern Gosper and southern Phelps counties for several hours, in response to lift within the nose of a gradually-strengthening low level jet. Through 10:30 p.m. CDT most of this activity remained fairly weak, but especially between 11 p.m-1 a.m. CDT a west-east oriented band intensified over northern Furnas County, dropping hail to at least golf ball size in spots before lifting into southern Gosper County and weakening/dissipating by 2 a.m. CDT. Turning to the completely separate area of strong to severe storms farther north: a broken, east-northeast to west-southwest oriented line of convection first got underway within Valley/Greeley counties between 4:30-6:30 p.m. CDT, focused along a quasi-stationary front draped across central NE. Through 9 p.m. CDT, strong to briefly-severe storms remained mainly north of Highway 92 as they drifted slowly south-southeast, gradually weakening and congealing into a more solid line. Between 9-11 p.m. CDT the eastern reaches of this convection sagged as far south as Hamilton/York counties but was non-severe. By midnight CDT the vast majority of local eastern counties were storm-free, and largely remained so through the rest of the night. In the mid-upper levels, this was a weakly-forced event as South Central Nebraska resided under fairly benign quasi-zonal flow (even subtle weak ridging), well-downstream from a larger-scale trough still well off to the west during the evening (over the Intermountain West). As a result, deep-layer wind shear was not overly-strong, averaging just 30-35 knots. In addition, low-level moisture was seasonably-modest, with surface dewpoints peaking only mid-50s F. However, due in part to afternoon temperatures climbing a bit higher than anticipated (highs mid-80s F), mixed-layer CAPE topped out as high as 1500-2000 J/kg. Ultimately, the combination of healthy instability, modest shear, modest convergence along the aforementioned surface boundaries and eventually an increasing low level jet proved sufficient to drive limited areal coverage of intense convection, most notably the Harlan County supercell. Off and on quarter size hail was reported to have fallen for at least 30 minutes.", "ts_dict_index": [5136, 5137, 5138]}
+{"event_id": 922601, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-10-11 19:19:00", "end_date_time": "2020-10-11 19:19:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. ", "ts_dict_index": [5154, 5155, 5156]}
+{"event_id": 848466, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2019-09-30 17:28:00", "end_date_time": "2019-09-30 17:31:00", "narrative": "Thunderstorms produced a lot of severe hail on this Monday afternoon and evening. Thirty-one reports of hail were received with the largest the size of tennis balls. Just after 4 PM CST, the first storm began moving into Harlan county from north central Kansas. This supercell storm dropped quarter size hail west of Alma. Between 415 and 430 PM CST, this storm split. The left-mover moved north-northeast along the Phelps-Kearney county line into Buffalo county. Multiple reports of hail were received over south central Buffalo county, including on the west and north sides of Kearney, where quarter to ping pong ball size hail fell. Hail up to two inches in diameter occurred north of Riverdale and east of Amherst. This long-lived storm continued moving north-northeast, producing severe hail across parts of Sherman, Howard, and Greeley counties through 630 PM CST. The largest hail was the size of tennis balls between Loup City and Rockville. The right-moving storm continued producing severe hail up to ping pong ball size from northern Franklin into southwest Adams county. While these two storms were in progress, other scattered storms developed, forming a broken line from near McCook northeast to near Columbus. Another supercell formed over northern Kansas and moved into Furnas county. Between 515 and 530 PM CST, this supercell split, with the left-mover producing 2 to 2.5 inch hail between Cambridge and Holbrook. This storm moved north-northeast across Gosper and Dawson counties through 630 PM CST. The only other hail reported with this storm was the size of half dollars in the town of Eddyville. The last storm known to produce severe hail occurred at Grand Island, where nickel to quarter size hail occurred between 730 and 800 PM CST. Severe weather was not reported with any of the other storms during this event. Despite the large number of storms, the convective mode remained cellular and supercellular. The entire area of scattered storms moved northeast and out of south central Nebraska by 1030 PM CST.||These storms formed along and just north of a slow-moving cold front. This front was associated with a 1005 mb low over Minnesota. A dryline intersected the front near McCook and extended south through northwest Kansas. In the upper-levels, the longwaves were highly-amplified with an anomalous subtropical high over the Tennessee Valley, and a deep low over the Northern Rockies. Strong southwest flow was over Nebraska. Where the initial thunderstorms erupted, temperatures were in the middle 90s, with dewpoints in the lower to middle 60s. Mid-level lapse rates were poor, but MLCAPE was still between 1500 and 2200 J/kg, with a southwest-northeast gradient along the front. Deep layer shear was 40-50 kt. Effective SRH was between 150 and 200 m2/s2, with even higher values on the cold side of the front. The lack of strong forcing aloft, combined with the low-level and deep-layer shear contributed to a cellular convective mode, some of which were supercells. Hail stones of 2 to 2.5 inches in diameter was reported along this path.", "ts_dict_index": [5160, 5161, 5162]}
+{"event_id": 837606, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-06-25 17:31:00", "end_date_time": "2019-06-25 17:31:00", "narrative": "Between the mid-afternoon of Tuesday the 25th and early morning of Wednesday the 26th, mainly the eastern half of South Central Nebraska endured two rounds of severe thunderstorms and heavy rainfall, with the first round by far the most impactful as it produced some of the largest hail of 2019 within the area (up to 3 diameter). Examining Round 1 in more detail, it unfolded from 4-8 p.m. CDT within several counties south of Interstate 80 and east of Highway 183, but with the majority of action focused within Adams, Webster and Nuckolls counties. The primary player here was an initially isolated, high-precipitation supercell that developed over western Adams County, gradually growing upscale into more of a supercell cluster as it surged southeastward before departing into northern Kansas. This storm was a prolific hail-producer, particularly within southwestern Adams County where there were numerous reports of stones ranging from quarter to larger than baseball size. The area in and near Holstein was particularly hard-hit, as hail as large as 3 was documented there by an NWS employee (although the vast majority of stones were smaller than this). As this massive storm sank farther south it became increasingly outflow-dominant and more of a wind-producer, with several gusts of 55-70 MPH reported in the Guide Rock and Superior areas. Independent of this storm of the day, other severe storms flared up during the afternoon and early evening within counties such as Clay/Fillmore/Franklin, producing hail of 2 diameter near Ong and golf ball size in Naponee. Rainfall-wise, though not extreme, amounts of 1.50-2.50 fell within much of Adams/Webster counties. This led to minor flooding on the Little Blue River, with the gauge near Deweese cresting at 10.3 feet on the afternoon of the 26th (flood stage 10 ft.). ||After Round 1 departed into Kansas, all was quiet on the local front for several hours. However, Round 2 got underway after 1 a.m. CDT on the 26th and persisted until past sunrise. This round of convection was not as intense, mainly producing heavy rainfall, sub-severe wind gusts and small hail within northeastern portions of the area (mainly northeast of an Ord-York line). However, there were a few severe-criteria reports including quarter size hail in York and a 61 MPH wind gust near Waco. Technically, Round 2 consisted of a few separate areas of storms: one small cluster that blew up over York County along the nose of a nocturnal low level jet and another larger complex that expanded across several northeastern counties between 3-7 a.m. CDT before finally weakening and departing the vast majority of South Central Nebraska by 9 a.m. CDT. Rainfall totals of 1.50-3.00 were fairly common with this early-AM activity, highlighted by NeRAIN totals of 3.60 near York and 3.33 north of Osceola. Resultant flooding was relatively minor, including along the Clear Creek in northern Polk County, which crested at 8.3 feet on the morning of the 27th (flood stage 8 ft.).||For yielding so many severe weather reports, this was actually a fairly weakly-forced event in the mid-upper levels, with Nebraska positioned along the southern periphery of broad westerly flow and no significant shortwave troughs of note. However, the intense afternoon-early evening convection was clearly tied to low-level convergence along a west-east oriented, quasi-stationary surface front. As afternoon temperatures climbed into the upper 80s F, the mesoscale environment became quite supportive of severe storms (including supercells), featuring 2000-3000 J/kg mixed-layer CAPE and 30-40 knots of deep-layer wind shear. Later in the night, Round 2 was fueled by a classic increase in convergence/moisture transport within the exit region of a 30-40 knot southwesterly low-level jet. ", "ts_dict_index": [5139, 5140, 5141]}
+{"event_id": 901023, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-06-04 21:11:00", "end_date_time": "2020-06-04 21:11:00", "narrative": "Albeit not as active as the previous evening, the evening of Thursday the 4th was the third consecutive with at least some severe storm activity in South Central Nebraska. This was truly a hit-and-miss, isolated to scattered event, as while storm coverage was fairly limited across the 24-county area as a whole, all four quadrants of it saw at least some convection. Overall, marginally-severe winds were the main issue, including measured gusts of 61 MPH at the Ord airport and 60 MPH at Waco, and estimated 60 MPH at Shelby, where the NWS cooperative observer reported downed tree branches up to 3 inches in diameter. Various other places clocked slightly sub-severe wind gusts of 50-55 MPH, including in or near Gothenburg, Johnson Lake, Arcadia, Gresham and Clay Center. Hail was less of an issue, with the only severe-criteria report consisting of quarter size stones in Sutton. ||Breaking down event evolution and timing, two small/separate storm clusters entered west-central and northern counties between 7-9 p.m. CDT, a continuation of activity that initiated hours earlier over the Nebraska Panhandle. These early evening storms produced strong-to-marginally severe winds mainly in Valley/Dawson/Gosper counties. Over the next few hours from 9-11:30 p.m. CDT, both of these storm clusters briefly weakened, only to re-intensify and even merge somewhat as they reached eastern portions of the area, prompting various hail/wind reports from counties such as Clay/Polk/York before exiting into eastern Nebraska. Meanwhile, back off to the southwest, a separate area of strong storms blossomed between 10 p.m. and midnight CDT in several counties along the Kansas border, but there were no ground-truth reports from this convection that departed into southeast Nebraska/northeast Kansas after midnight. Finally, one last weaker batch of storms roamed various northern/eastern counties between 1-4 a.m. CDT on Friday the 5th before all local storm activity ended for the night. Both at the surface and aloft, the same general environment that supported severe storms the prior evening remained in place for this round. In the mid-upper levels,  broad west-northwest flow containing various embedded, low-amplitude disturbances persisted over the region. At the surface, the same seasonably-hot and moderately unstable airmass persisted as well, as afternoon temperatures topped out in the low-mid 90s F with dewpoints ranging from upper 50s F in western counties to 65-70 F in the east. As strong to severe storms traversed the area in the evening, mesoscale parameters featured 1000-3000 J/kg mixed-layer CAPE and 40 knots of deep-layer wind shear. ", "ts_dict_index": [5169, 5170, 5171]}
+{"event_id": 829980, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-06-08 22:05:00", "end_date_time": "2019-06-08 22:05:00", "narrative": "Numerous thunderstorms rumbled across much of South Central Nebraska on the evening of Saturday the 8th into the early morning of Sunday the 9th. While most of this activity was sub-severe, producing only small hail and/or wind gusts up to around 50 MPH, a notable exception occurred in several southwestern counties where a briefly-supercellular storm produced a flurry of severe-criteria wind gusts primarily between 8-9 p.m. CDT. These severe winds of mainly 60-70 MPH concentrated within northern Furnas, southern Gosper, northwestern Harlan and southern Phelps counties, including an intense (albeit unofficial) gust of 86 MPH clocked by a personal weather station north-northwest of Oxford. While ground-truth damage reports were limited, they included: 1) a power pole blown onto Highway 6/34 in Arapahoe along with several large tree limbs down around town...2) various reports of mainly minor damage in/near Holdrege, including: damaged power poles, a large tree down at the cemetery, and part of an irrigation pivot blown onto a rural road a few miles west of town. As this storm of the day progressed into eastern Phelps County it weakened while transitioning to more of a multicell cluster mode. However, storm intensity occasionally flared up farther east, as evidenced by estimated 55-60 MPH winds in southeast Adams County. Lightning also made the news during the evening, as a bolt from a non-severe storm in Grand Island blew out a roughly 5-by-5 foot section from the roof of a retail store, sparking a small fire. Somewhat surprisingly, there was no verified severe-criteria hail during this event, with the largest reported stones only nickel size.||Timing-wise, the first severe storms of the day in close proximity to (but slightly west of) South Central Nebraska erupted along a well-defined cold front in west-central Nebraska during the mid-afternoon. A few hours later, the first strong storm to affect the local area entered western Dawson County between 6-7 p.m. CDT, followed a bit later by the main, outflow-dominant severe cell that rapidly intensified over Gosper/northern Furnas counties. As the night wore on a few larger-scale, predominantly sub-severe storm complexes traversed much of the 30-county area, with most places eventually rain-free by 4-5 a.m. CDT on the 9th. Meteorologically, this was a fairly strongly-forced event. In the mid-upper levels, west-southwesterly flow was present, slightly downstream from a seasonably-strong, large-scale trough traversing the Northern Rockies. At the surface, the aforementioned, northeast-southwest oriented cold front gradually made its way through South Central Nebraska during the evening and overnight hours. Ahead of this boundary, the mesoscale environment was clearly supportive of severe storms, with early-evening parameters featuring around 2000 J/kg mixed-layer CAPE and 30-40 knots of deep-layer wind shear. As a testament to the strength of the passing cold front, high temperatures across most of South Central Nebraska dropped from the mid-80s F on the 8th to only the upper-60s on the 9th. ", "ts_dict_index": [5157, 5158, 5159]}
+{"event_id": 1013500, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2022-04-29 14:48:00", "end_date_time": "2022-04-29 15:05:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Largest hail stones at the local golf course ranged in size from ping pong balls to two inches in diameter.", "ts_dict_index": [5067, 5068, 5069]}
+{"event_id": 843927, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2019-08-02 19:45:00", "end_date_time": "2019-08-02 19:45:00", "narrative": "The vast majority of South Central Nebraska experienced very little (if any) notable weather on this Friday. However, there were a couple of significant exceptions, as heavy rains caused extensive flooding in parts of Valley County and a lone severe storm with damaging winds and large hail brushed far western portions of Dawson and Furnas counties. Going into more detail, and starting with the Valley County situation, a small-but-persistent cluster of heavy showers/non-severe storms dumped a roughly 5-10 mile wide swath of heavy rain on northwestern and south central portions of the county, mainly between 10 a.m. and 4 p.m. CDT. These areas received a widespread 2-4 with isolated pockets as high as 5-7, including an unofficial public report of 6.25 nine miles west-southwest of Elyria. Within a few hours after the onset of heavy rain, several rural roads were flooded/washed out, and small creeks such as Turtle Creek spilled out of their banks. An NeRAIN observer southwest of Elyria commented that Turtle Creek flooding was worse than what occurred during the historic March 2019 floods. By the evening and overnight hours, flooding also ramped up on Mira Creek south of Ord, including a bridge washout on a paved county road. During the pre-dawn hours of the 3rd, Mira Creek flooding reached the town of North Loup, prompting mainly minor water issues on the north side of town. Turning to the severe storm aspect of the day (and completely separate from the Valley County flooding), an isolated severe storm tracked almost due south over the western fringes of Dawson and Furnas counties between 6:30-9:30 p.m. CDT, affecting the Gothenburg and Cambridge areas. Near Gothenburg, a mesonet clocked a 66 MPH gust and a flag pole was bent over. A bit later, trained spotters just west of Cambridge reported hail up to golf ball size and a measured wind gust of 71 MPH, with a few power poles downed on Highway 6/34.||In the big picture of the mid-upper levels, forcing was nebulous over the Central Plains as subtle waves passed through northwesterly flow, directed around the edge of an expansive ridge centered over New Mexico. Most notably for the Valley County flooding, precipitable water values averaged nearly 2, fostering impressive rainfall rates in low-topped cells. For the evening severe storm in Dawson/Furnas counties, mesoscale parameters featured around 1500 J/kg mixed-layer CAPE and 35 knots of deep-layer wind shear. At the surface, a nondescript pattern existed over South Central Nebraska, with light southerly-to-easterly breezes and dewpoints in the upper 60s to around 70 F. Golf ball size hail was accompanied by wind gusts near 70 MPH, with a 71 MPH wind gust measured by a mesonet station.", "ts_dict_index": [5172, 5173, 5174]}
+{"event_id": 1093431, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-04-18 20:45:00", "end_date_time": "2023-04-18 20:50:00", "narrative": "On this Tuesday late afternoon and evening, thunderstorms of varying strength rumbled from southwest-to-northeast across portions of South Central Nebraska mainly between 6:00-11:30 p.m. CDT. However, the vast majority of strong to severe activity focused within a 15-30 mile wide swath centered along a line from Franklin-Blue Hill-Sutton-York. Within this corridor, there were a number of reports of large hail ranging from quarter size up to tennis ball size, with the tennis ball (2.5 inch) reports out of Harvard and Stockham. There were also several instances of ping pong ball to golf ball size stones, including in or near the following communities: Blue Hill, Sutton, Edgar and Glenvil. Finally, marginally-severe, quarter to half dollar size hail reports originated from in or near places such as: Franklin, Bladen, Clay Center, Deweese and York. Large hail was clearly the main story of the evening, as there were only a few measured strong to marginally-severe gusts of 50+ MPH, a few of which were several miles removed from obvious thunderstorm outflow and were likely associated with a weak wake low. A few of the strongest detected gusts included 58 MPH in Doniphan (unofficial mesonet) and ASOS-measured gusts of 55 and 52 MPH at Grand Island and Hastings airports, respectively. ||Breaking down event evolution/timing, if anything the intensity of storms (and peak hail size) ended up being a bit surprising given the seasonably-modest and just in time nature of low-level moisture advecting northward into the area along a slow-moving surface warm front. At daybreak on the 18th, this west-east oriented front was aligned across northern Kansas, with South Central Nebraska firmly on its cool/dry side with surface dewpoints mainly only in the 20s (F). Meanwhile, in the mid-upper levels, the Central Plains resided well downstream of a large scale trough centered over the Northern Rockies. Over the course of the day, a subtle wave along the leading edges of the aforementioned parent trough entered the Central High Plains. This prompted a gradual increase in west-southwesterly, mid-upper level flow into South Central Nebraska, along with a gradual increase in south-southeasterly low-level flow, allowing slow-but-steady northward moisture transport into the lifting warm frontal zone. By late afternoon (around the time of convective initiation), a 994 millibar surface low was noted over northwest Kansas, with the attendant warm front extending into far southern Nebraska to its east, and a north-south oriented dryline trailing southward. Although still seasonably-unimpressive, surface dewpoints over the southern half of South Central Nebraska had risen well into the mid-upper 40s by this time (a surge of nearly 20 degrees over early morning values). This meager-but-sufficient low level moisture, combined with steep low-to-mid level lapse rates and convergence near the warm front/dryline intersection, was enough to initiate the first high-based storms of the afternoon over north central Kansas around 5:30 p.m. CDT. Already by 6 p.m. CDT, the first severe-warned storm of the day within South Central Nebraska had entered southern Franklin County. During the next two hours, a series of semi-discrete, strong-to-severe cells affected primarily Franklin/Webster counties. Then, between 8-10 p.m. CDT, intense elevated convection consolidated into a more cohesive line as it tracked northeastward across portions of mainly Adams/Clay/Nuckolls/Hamilton/Fillmore counties, aided by an uptick in a 40-50 knot southerly low level jet (evident at 850 millibars). Finally, between 10:00-11:30 p.m. CDT, this severe storm complex traversed York County before exiting the local area into eastern Nebraska, while other non-severe cells passed through various counties mainly along/north of Highway 92 before also departing South Central Nebraska...thus ending all local thunderstorm activity for the night. As it turned out, despite the unimpressive low level moisture magnitude, the combination of mixed-layer CAPE increasing to as high as 1000-1500 J/kg during the evening, combined with strong effective deep-layer wind shear around 50 knots, proved plenty sufficient to ignite robust updrafts. Quarter to golf ball size hail was reported in Sutton.", "ts_dict_index": [5115, 5116, 5117]}
+{"event_id": 1099537, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2023-06-16 15:37:00", "end_date_time": "2023-06-16 15:37:00", "narrative": "Mainly between 2-9 p.m. CDT on this Friday afternoon and evening, isolated to scattered thunderstorms roamed South Central Nebraska, affecting at least small portions of nearly all 24 local counties. The vast majority of these slow-moving storms (a varied mix of pulse/single-cell and multicell) were non-severe, producing pockets of heavy rain, gusty winds of no more than 40-50 MPH and isolated instances of small hail up to around dime size (as reported in various places such as Holdrege and Waco). However, a few cores intensified enough to prompt Severe Thunderstorm Warnings for small parts of primarily Buffalo, Phelps and Valley counties. Only one of these warnings yielded ground-truth verification: quarter size hail in Amherst around 4:30 p.m. CDT. As for rainfall, although there were no reports of impactful flooding, a combination of radar estimation and measured totals confirmed that at least 1-2 fell in a short time within at least small sections of the following counties: Buffalo, Dawson, Gosper, Furnas, Phelps, Harlan, Valley, Greeley, Sherman and Polk.||As was the case during similar events earlier in the month, this round of diurnally-driven convection unfolded in an environment characterized by moderate instability, but seasonably-weak deep layer wind shear...promoting slow-moving and only-briefly-intense cores. In the mid-upper levels the situation over South Central Nebraska was unremarkable, featuring feeble and mainly westerly flow... well-removed from better-defined shortwave troughs well to the east (northeastern United States) and west (Northern Rockies into Intermountain West). At the surface, there was some focus for storm development in the form of a weak, quasi-stationary front draped across the area from west-southwest to east-northeast. As afternoon temperatures climbed into the mid-80s to low-90s (F), storms readily developed in a weakly-capped airmass featuring mixed-layer CAPE of 1000-2000 J/kg, but meager deep-layer wind shear of no more than 20-25 knots. After this round of storms steadily weakened/faded away with the loss of daytime heating, there was a brief lull in activity across the area. However, between midnight and sunrise on the 17th, an overall-weak storm complex gradually invaded much of South Central Nebraska from the southwest. ", "ts_dict_index": [5193, 5194, 5195]}
+{"event_id": 900017, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2020-06-04 20:38:00", "end_date_time": "2020-06-04 20:38:00", "narrative": "Very hot temperatures combined with a weak upper level disturbance, abundant moisture, and instability led to the development of thunderstorms on the afternoon of the fourth. These thunderstorms produced widespread wind damage and large hail. The hot and well mixed lower atmosphere and high-based nature of the thunderstorms provided ideal conditions for the generation of strong and severe wind gusts. Scattered thunderstorms initially developed in the Texas Panhandle along a surface trough and tracked to the south and southeast through the evening. ||The first reports of severe weather were from Briscoe County with wind gusts up to 72 mph near Silverton. These initial thunderstorms then accelerated to the south forming a strong cold pool out ahead of the storms. Storms repeatedly formed along outflow boundaries in the central South Plains and quickly raced southward. One of these storms produced large hail up to two inches in diameter in Floyd County. This particular storm went on to produce wind damage in Ralls (Crosby County) and finally in Post (Garza County).  In far southwestern Garza County, this storm produced a wind gust to 94 mph near Graham. High precipitable water values contributed to flooding in Garza County along Texas State Highway 207 north of Post. Reports on social media showed the road had been damaged and impassable due to flooding.||Additional thunderstorms developed across the central South Plains and rushed southward from Hale into Lubbock and Lynn Counties. A large swath of severe winds initially affected a portion of Lubbock County and the city of Lubbock. The first severe wind gust was reported by the Automated Surface Observing System at Lubbock Preston Smith International Airport at 2020 CST. The Texas Tech University West Texas mesonet recorded additional severe wind gusts at Reese Center, Texas Tech University, and Slaton. These severe winds mostly affected the eastern portion of the city of Lubbock. In total, 50 power poles were downed along with a tree that fell onto and damaged a residence.||Thunderstorm outflow winds well ahead of the thunderstorms produced a severe wind gust to 58 mph at Amherst (Lamb County) at 1925 CST measured by the Texas Tech University West Texas mesonet. ", "ts_dict_index": [5196, 5197, 5198]}
+{"event_id": 888717, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2020-05-23 16:05:00", "end_date_time": "2020-05-23 16:05:00", "narrative": "Widespread supercell thunderstorms developed across the South Plains on the afternoon and evening of the 23rd producing very large hail, a tornado, and flash flooding. ||From the night of the 22nd through the morning of the 23rd, a dryline surged westward allowing abundant low level moisture to return to the region. This dryline mixed to the east during the afternoon stalling around US Highway 385. A capping inversion initially kept convective initiation from occurring until late in the afternoon under a very unstable atmosphere with CAPE values in excess of 4000 J/kg. Initially, the most intense thunderstorm developed and became anchored over southwestern Garza County. This supercell exhibited strong rotation at low and mid levels of the storm. Several storm chasers observed a tornado over open land that lasted for about 11 minutes. Because of the very slow storm motion of this thunderstorm, the tornado was nearly stationary for its entire lifetime. A lack of roads in the path of the tornado prevented a storm survey from being completed, thus this tornado could not be rated.|Heavy rain fell over an extended period of time in Garza County due to the storm's nearly stationary movement. As a result, a portion of Farm to Market road 669 south of Post was washed out.||The thunderstorms that developed in the southeastern South Plains generated a strong outflow boundary which then moved through the central South Plains. This outflow boundary caused scattered thunderstorms to grow over Lubbock County in which many of these became severe over multiple parts of the city of Lubbock. Hail up to two inches was reported in the city of Lubbock along with wind gusts up to 62 mph. This outflow boundary continued to move northward creating additional severe thunderstorms over the extreme south-central Texas Panhandle. One of these storms produced hail up to three inches in diameter in the city of Silverton (Briscoe County) leading to widespread damage to vehicles.||Trailing stratiform precipitation from decaying thunderstorms generated a couple of non-thunderstorm severe wind gusts. One of these occurred at Caprock Canyons State Park where a Texas Tech University West Texas mesonet site measured a wind gust to 58 mph. The other was at the Automated Surface Observing System at Childress Municipal Airport measuring a gust to 58 mph. Scattered severe thunderstorms developed across Lubbock County on an outflow boundary. The first of these storms produced hail up to golf ball size from near Slaton to Buffalo Springs Lake at 1605 CST.", "ts_dict_index": [5184, 5185, 5186]}
+{"event_id": 875877, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-12 06:25:00", "end_date_time": "2020-04-12 06:25:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. Quarter size hail fell on Northeast Loop 323 in Tyler.", "ts_dict_index": [5202, 5203, 5204]}
+{"event_id": 849739, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2019-08-20 23:40:00", "end_date_time": "2019-08-21 00:25:00", "narrative": "The overnight hours of Tuesday the 20th into the early morning of Wednesday the 21st were quite stormy, especially within the northeast half of South Central Nebraska. However, the vast majority of strong to severe activity (along with heavy rainfall) concentrated within a 10-20 mile wide, northwest-southeast oriented stripe centered from roughly Hazard-Grand Island-Lushton. Despite several radar-indicated signatures of large hail within this zone, various factors (such as the time of day) resulted in hardly any ground-truth verification. The main exception was at a well-known, 45-acre melon and pumpkin patch seven miles east of Ravenna, where 45 minutes of hail (some up to golf ball size) ruined the majority of the season's produce. As for heavy rain, most locations within the main swath tallied between 1.50-3.00 overnight. However, there were very localized higher exceptions, including 3.84 at the aforementioned melon patch east of Ravenna and 3.66 at Dannebrog. There was also an unofficial report of 5.50 in far northeastern Buffalo County, but this was certainly a high-end outlier. There were no ground-truth reports of flash flooding during the night. However, heavy rain over southern Hamilton County pushed the West Fork Big Blue River out of its banks during the day, with minor flooding reported near Stockham (side note: due to repeated rounds of rain, minor flooding ended up persisting along local portions of the West Fork Big Blue River for the next 10 days).||Timing-wise, rapid storm development got underway within the primary northwest-southeast corridor shortly before midnight CDT, with convection peaking in intensity 12-3 a.m. CDT before weakening but expanding in coverage. The initial concentration of storms within such a narrow swath was a classic signature of increasing nocturnal warm air advection/convergence in the 850-700 millibar layer. In the mid-upper levels, broad quasi-zonal flow prevailed over the Central Plains, containing subtle, low-amplitude disturbances. The mesoscale environment was primed for robust-but-slow-moving storms, featuring 2000-3000 J/kg mixed-layer CAPE but only 20-30 knots of deep-layer wind shear. At the surface, South Central Nebraska resided slightly north of a quasi-stationary front draped west-east through northern Kansas, and within a very moist/humid airmass marked by dewpoints well into the 70s F. Hail ranging in size from peas to golf balls fell for approximately 45 minutes, ravaging a 45-acre melon and pumpkin patch east of Ravenna. About a month later, it was reported that the business lost 80-90 percent of its produce from this storm.", "ts_dict_index": [5181, 5182, 5183]}
+{"event_id": 888747, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2020-05-23 17:19:00", "end_date_time": "2020-05-23 17:19:00", "narrative": "Widespread supercell thunderstorms developed across the South Plains on the afternoon and evening of the 23rd producing very large hail, a tornado, and flash flooding. ||From the night of the 22nd through the morning of the 23rd, a dryline surged westward allowing abundant low level moisture to return to the region. This dryline mixed to the east during the afternoon stalling around US Highway 385. A capping inversion initially kept convective initiation from occurring until late in the afternoon under a very unstable atmosphere with CAPE values in excess of 4000 J/kg. Initially, the most intense thunderstorm developed and became anchored over southwestern Garza County. This supercell exhibited strong rotation at low and mid levels of the storm. Several storm chasers observed a tornado over open land that lasted for about 11 minutes. Because of the very slow storm motion of this thunderstorm, the tornado was nearly stationary for its entire lifetime. A lack of roads in the path of the tornado prevented a storm survey from being completed, thus this tornado could not be rated.|Heavy rain fell over an extended period of time in Garza County due to the storm's nearly stationary movement. As a result, a portion of Farm to Market road 669 south of Post was washed out.||The thunderstorms that developed in the southeastern South Plains generated a strong outflow boundary which then moved through the central South Plains. This outflow boundary caused scattered thunderstorms to grow over Lubbock County in which many of these became severe over multiple parts of the city of Lubbock. Hail up to two inches was reported in the city of Lubbock along with wind gusts up to 62 mph. This outflow boundary continued to move northward creating additional severe thunderstorms over the extreme south-central Texas Panhandle. One of these storms produced hail up to three inches in diameter in the city of Silverton (Briscoe County) leading to widespread damage to vehicles.||Trailing stratiform precipitation from decaying thunderstorms generated a couple of non-thunderstorm severe wind gusts. One of these occurred at Caprock Canyons State Park where a Texas Tech University West Texas mesonet site measured a wind gust to 58 mph. The other was at the Automated Surface Observing System at Childress Municipal Airport measuring a gust to 58 mph. Scattered severe thunderstorms developed across Lubbock County on an outflow boundary. One of these storms produced hail up to ping pong ball size in Wolfforth.", "ts_dict_index": [5187, 5188, 5189]}
+{"event_id": 879884, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-12 11:53:00", "end_date_time": "2020-04-12 11:53:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. Penny size hail fell in the Deepwoods subdivision in South Shreveport.", "ts_dict_index": [5178, 5179, 5180]}
+{"event_id": 977990, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2021-08-15 03:10:00", "end_date_time": "2021-08-15 03:10:00", "narrative": "Between 11 p.m. CDT on Saturday the 14th and 8:30 a.m. on Sunday the 15th, numerous elevated thunderstorms occurred in various parts of South Central Nebraska, but with the most concentrated activity focused within a narrow, north-south band centered roughly from Arcadia-Elm Creek-Orleans. While the vast majority of this overnight-early morning activity was not severe, producing only heavy rain and sporadic small hail, there were a few reports of severe-criteria hail including a pocket of quarter to ping pong ball size stones in parts (not all) of Hastings around sunrise, and also copious amounts of hail up to quarter size near Elm Creek around 4 a.m. CDT that caused some crop and vehicle damage. Slightly smaller nickel size hail was also reported in Upland and near Arcadia. While rainfall totals varied widely outside the aforementioned narrow north-south swath, places within the heart of this mainly 10-mile-or-less wide strip averaged 1.50-3.00 inches, with a few of the highest measured totals featuring 3.72��� near Orleans, 2.99��� north-northwest of Holdrege and 2.98��� south-southwest of Elm Creek. However, there were no reports of impactful flooding. ||This mostly-nocturnal event was a fairly classic example of somewhat-subtle low-mid level moisture convergence (evident in the 850-700 millibar layer) and along the eastern fringes of a 30-40 knot southerly low level jet (850 millibars) promoting a mesoscale heavy rain band along with transient hail cores. In the mid-upper levels, South Central Nebraska resided under modest north-northwesterly flow containing a steady stream of embedded subtle perturbations. Timing-wise, the beginning stages of this event got underway around 11 p.m. as a briefly-isolated storm developed in eastern Dawson County. Over the course of the next several hours, the aforementioned north-south band became increasingly established within the western half of South Central Nebraska, while more scattered activity slowly drifted east along its eastern fringes. During the 5-7 a.m. CDT time frame the persistent band finally dissipated, shifting the focus to some of the spottier hail cores closer to the Highway 281 corridor (including the one over Hastings). After 7 a.m., a couple of more small hail cores pulsed up over parts of Clay, Hamilton and southwestern York counties, but by 8:30 a.m. CDT any strong convection had all but faded away. Through the balance of this event, instability/shear parameters featured around 1000-1500 J/kg most-unstable CAPE and 30-40 knots of effective deep-layer shear. Hail up to quarter size caused some damage to vehicles, buildings, and crops.", "ts_dict_index": [5175, 5176, 5177]}
+{"event_id": 888738, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2020-05-23 16:34:00", "end_date_time": "2020-05-23 16:48:00", "narrative": "Widespread supercell thunderstorms developed across the South Plains on the afternoon and evening of the 23rd producing very large hail, a tornado, and flash flooding. ||From the night of the 22nd through the morning of the 23rd, a dryline surged westward allowing abundant low level moisture to return to the region. This dryline mixed to the east during the afternoon stalling around US Highway 385. A capping inversion initially kept convective initiation from occurring until late in the afternoon under a very unstable atmosphere with CAPE values in excess of 4000 J/kg. Initially, the most intense thunderstorm developed and became anchored over southwestern Garza County. This supercell exhibited strong rotation at low and mid levels of the storm. Several storm chasers observed a tornado over open land that lasted for about 11 minutes. Because of the very slow storm motion of this thunderstorm, the tornado was nearly stationary for its entire lifetime. A lack of roads in the path of the tornado prevented a storm survey from being completed, thus this tornado could not be rated.|Heavy rain fell over an extended period of time in Garza County due to the storm's nearly stationary movement. As a result, a portion of Farm to Market road 669 south of Post was washed out.||The thunderstorms that developed in the southeastern South Plains generated a strong outflow boundary which then moved through the central South Plains. This outflow boundary caused scattered thunderstorms to grow over Lubbock County in which many of these became severe over multiple parts of the city of Lubbock. Hail up to two inches was reported in the city of Lubbock along with wind gusts up to 62 mph. This outflow boundary continued to move northward creating additional severe thunderstorms over the extreme south-central Texas Panhandle. One of these storms produced hail up to three inches in diameter in the city of Silverton (Briscoe County) leading to widespread damage to vehicles.||Trailing stratiform precipitation from decaying thunderstorms generated a couple of non-thunderstorm severe wind gusts. One of these occurred at Caprock Canyons State Park where a Texas Tech University West Texas mesonet site measured a wind gust to 58 mph. The other was at the Automated Surface Observing System at Childress Municipal Airport measuring a gust to 58 mph. Scattered severe thunderstorms developed across Lubbock County on an outflow boundary. One of these thunderstorms produced severe hail on the western side of the city of Lubbock. Numerous reports were received of hail up to golf ball size from the southwestern portion of Lubbock through the western side of Lubbock. Hail up to two inches in diameter was reported in Woodrow. No damage was reported.", "ts_dict_index": [5190, 5191, 5192]}
+{"event_id": 875881, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-12 07:32:00", "end_date_time": "2020-04-12 07:32:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. Quarter size hail was reported 2 miles south of the East Texas Regional Airport.", "ts_dict_index": [5205, 5206, 5207]}
+{"event_id": 978076, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-08-07 18:55:00", "end_date_time": "2021-08-07 18:56:00", "narrative": "The 24-hour period between the early mornings of Saturday the 7th and Sunday the 8th featured several rounds of thunderstorms within South Central Nebraska. However, by far the most prominent round focused between 6-10 p.m. CDT, during which time a burst of fairly widespread strong to severe activity affected mainly the southeast half of the area...especially east of a line from Franklin-St. Paul-Fullerton. Although ground-truth reports were somewhat limited considering that 16 Severe Thunderstorm Warnings were issued during these four hours, there were a handful of hail reports up to golf ball size along with a few mesonet-measured severe wind gusts (including 68 MPH near Lawrence and 63 MPH near Polk). A few of the more notable hail reports included: golf ball size near Giltner and Lawrence; ping pong ball size near Fairfield. Within the Tri Cities, parts of both Grand Island and Hastings observed small hail up to dime-nickel size, but for Grand Island the bigger story was actually heavy rain and a few rounds of fairly minor urban flooding as multiple storms cumulatively dumped a widespread 2-3 inches of rain within a bullseye centered directly over the city. However, the overall heaviest rain within South Central Nebraska actually concentrated within a southwest-northeast swath through the heart of Polk County, where amounts of 2.50-3.50 were common (including 3.35 in Osceola). Meanwhile, the vast majority of the 24-county area observed much lower and highly-variable rain amounts ranging from only a few hundredths up to around 1.50. ||Breaking down event evolution/timing and meteorological background, weak/non-severe convection percolated over much of South Central Nebraska throughout much of  the morning and afternoon, downstream from a seasonably-potent mid level shortwave trough slowly approaching from the NE/WY/CO border area. However, this activity diminished enough by late afternoon to allow considerable instability to build, aided by surface temperatures climbing into the mid-80s to around 90 (F) in the presence of healthy dewpoints mainly upper 60s-low 70s. By 6 p.m. CDT, the resultant mesoscale environment featured a fairly potent combination of 3000-4000 J/kg mixed-layer CAPE and 30-35 knots of deep-layer wind shear. Despite a lack of prominent surface boundaries within the area (only a fairly weak trough axis), the first initially-isolated strong-to-severe local storms of the day flared up between 6-7:30 p.m. CDT, one over Polk County (which dumped quarter size hail in Osceola) and another that lifted north out of Kansas into Webster/Nuckolls counties. Then, the ensuing few hours saw quite an uptick in the coverage of strong to severe storms within several central/eastern local counties. By around 10 p.m. CDT this activity quickly weakened below severe limits and started gradually departing off to the east. However, with a modest low level jet acting upon lingering elevated instability, additional flare-ups of spotty strong to perhaps marginally-severe storms (unverified) occurred mainly 1-4 a.m. CDT on the 8th, with a few of the most intense cells over Webster and Hall counties. Once this late-night round weakened/dissipated, most all of South Central Nebraska was finally convection-free by 5:30 a.m. CDT. Hail ranging in size from quarters to ping pong balls was reported.", "ts_dict_index": [5148, 5149, 5150]}
+{"event_id": 1095775, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2023-05-24 16:41:00", "end_date_time": "2023-05-24 17:30:00", "narrative": "Several consecutive days of significant severe weather impacted eastern New Mexico from May 24-26, 2023. Showers and thunderstorms developed along the dryline and east slopes of the Sangre de Cristo Mountains on May 23rd. Storms tracked east and southeast across the eastern plains of New Mexico. Extensive severe weather was reported when these storms encountered greater moisture and lift closer to the Texas border. Hail up to 3.5 inches in diameter, thunderstorm wind gusts of 80 to 90 mph, and three tornados were reported in an area stretching from Union County to Roosevelt County. The largest hail stones and strongest wind gusts focused throughout Curry County during the evening hours. Hail and wind damage was reported in Tucumcari, Grady, and Clovis. Three separate tornadoes were reported in northern Curry County. Thunderstorms also dropped very heavy rainfall of 2 to 4 inches of rain across portions of Quay, De Baca, Curry, and Roosevelt Counties. Urban flooding occurred in Clovis, NM, causing some roads to be closed, and some cars to be stranded. Severe weather continued through the night and into May 25th with numerous reports of large hail, strong winds, and flash flooding. Quay County was particularly hard hit with baseball size hail and torrential rainfall amounts in excess of 5 inches. Significant hail damage was reported across Tucumcari with widespread flooding across the county. Severe wind gusts of 70 to 80 mph were common with these storms with damage reported. Strong to severe storms continued well into the night once again on the 25th with more heavy rainfall around the Caprock. The focus for severe weather shifted farther west on May 26th with large hail and heavy rainfall reported around Torrance County. A tornado and baseball size hail was also reported with a supercell near Encino. This activity spread eastward through the day with large hail, damaging wind gusts, and more torrential rainfall around the Caprock well into the night of May 26th. Three-day rainfall amounts exceeded 6 inches in many parts of Curry and Quay counties. Hail reports ranging in size from dimes to quarters in San Jon.", "ts_dict_index": [5226, 5227, 5228]}
+{"event_id": 1096931, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2023-05-05 21:12:00", "end_date_time": "2023-05-05 21:25:00", "narrative": "Large hail, damaging wind gusts, and an isolated tornado occurred over portions of south central Nebraska, mainly west of Highway 281, during the afternoon through late evening hours. Initial development occurred roughly along the NE/KS state line between 1600-1700CDT, and was mainly in the form of supercells. By around 2200CDT, nearly a half-dozen supercells affected portions of south central Nebraska roughly along and south of Interstate 80 (I-80) and west of Highway 281 and produced scattered instances of large to very large hail. The largest hail reported was tennis ball in Franklin County, which was associated with one of the first supercells to form in the late afternoon. After the initial round of supercells, which weakened mostly below severe limits by 2230CDT, a squall line of thunderstorms moved into far western portions of the CWA between 2230-2300CDT. The primary severe threat with this activity was damaging wind gusts of 60-65MPH. However, embedded within the squall line was a brief EF-1 tornado that impacted the Johnson Lake area around 2300. A bow echo developed within the squall line between 2300-2400CDT over Dawson County then raced northeast and affected areas north of the Platte River over the next 60-90 minutes. This activity weakened as it exited NE portions of the CWA during the early morning hours of May 6th.||While there were no significant synoptic scale fronts or low pressure systems in the area of this event, the first round of scattered supercells developed along a remnant outflow boundary that was stalled near the NE/KS state line. The second round was a result of thunderstorms that developed over the High Plains which was then supported by an increasing low level jet as activity shifted east overnight. Through the entire event, there was moderately strong instability (2000-3000 J/kg of CAPE), strong deep layer shear around 40-45kt, and steep mid level lapse rates of 7-8C/km. 0-3km shear was also strong during this event, around 30kt, which supported the bow echo development across northern portions of the CWA during the evening hours. Hail up to the size of ping pong balls was reported across Kearney.", "ts_dict_index": [5220, 5221, 5222]}
+{"event_id": 907418, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2020-07-29 17:38:00", "end_date_time": "2020-07-29 17:38:00", "narrative": "Slow moving upper low brings multiple rounds of thunderstorms, including locally heavy rain and a few severe thunderstorms, on July 29th. Low to mid level warm air advection ahead of a lead shortwave trough led to the development of scattered showers and thunderstorms roughly along a line from Hastings to Superior between 6-8am CDT. Locally heavy rain rates and slow moving thunderstorms led to areas of heavy rain across portions of Clay, Nuckolls, Fillmore and Thayer Counties during the mid to late morning hours. Soil conditions in these areas were already saturated due to previous heavy rain events over the recent days. Activity decreased in coverage and intensity around midday, and most areas were dry by 1pm CDT. Total rain amounts of 2-3 inches were common across these areas, which led to renewed flooding, particularly over Thayer County. The primary impact was water covering county roads and water flowing over Highway 136 west of Deshler. Conditions were favorable for heavy rain given the aforementioned slow storm motions, but also relatively high precipitable water values near 2���.||Additional thunderstorm activity developed during the afternoon hours from central Nebraska into northwest Kansas. Initial individual and cellular thunderstorms grew upscale into several clusters during the late afternoon and into the evening. One such cluster moved through far western portions of the County Warning Area (CWA), mainly from Cozad down to Beaver City, between 6-8pm CDT. Some of this activity became severe and produced up to ping pong ball sized hail across Furnas County. As this activity weakened around 8pm CDT, new, mainly isolated, thunderstorms developed just to the NE over Phelps and Buffalo Counties between 8-9pm CDT. Up to penny size hail was reported with this activity over Phelps County. Yet another round of thunderstorms developed and organized into a mesoscale convective system (MCS) west of the area, then moved through areas southwest of a line from Lexington, Nebraska to Beloit, Kansas after 10pm CDT. This activity was strong, but remained non-severe, over south central Nebraska. ", "ts_dict_index": [5217, 5218, 5219]}
+{"event_id": 1091721, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2023-05-24 17:00:00", "end_date_time": "2023-05-24 17:30:00", "narrative": "Several consecutive days of significant severe weather impacted eastern New Mexico from May 24-26, 2023. Showers and thunderstorms developed along the dryline and east slopes of the Sangre de Cristo Mountains on May 23rd. Storms tracked east and southeast across the eastern plains of New Mexico. Extensive severe weather was reported when these storms encountered greater moisture and lift closer to the Texas border. Hail up to 3.5 inches in diameter, thunderstorm wind gusts of 80 to 90 mph, and three tornados were reported in an area stretching from Union County to Roosevelt County. The largest hail stones and strongest wind gusts focused throughout Curry County during the evening hours. Hail and wind damage was reported in Tucumcari, Grady, and Clovis. Three separate tornadoes were reported in northern Curry County. Thunderstorms also dropped very heavy rainfall of 2 to 4 inches of rain across portions of Quay, De Baca, Curry, and Roosevelt Counties. Urban flooding occurred in Clovis, NM, causing some roads to be closed, and some cars to be stranded. Severe weather continued through the night and into May 25th with numerous reports of large hail, strong winds, and flash flooding. Quay County was particularly hard hit with baseball size hail and torrential rainfall amounts in excess of 5 inches. Significant hail damage was reported across Tucumcari with widespread flooding across the county. Severe wind gusts of 70 to 80 mph were common with these storms with damage reported. Strong to severe storms continued well into the night once again on the 25th with more heavy rainfall around the Caprock. The focus for severe weather shifted farther west on May 26th with large hail and heavy rainfall reported around Torrance County. A tornado and baseball size hail was also reported with a supercell near Encino. This activity spread eastward through the day with large hail, damaging wind gusts, and more torrential rainfall around the Caprock well into the night of May 26th. Three-day rainfall amounts exceeded 6 inches in many parts of Curry and Quay counties. Two inch hail a few miles west of San Jon along I-40.", "ts_dict_index": [5241, 5242, 5243]}
+{"event_id": 1092113, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2023-05-24 17:18:00", "end_date_time": "2023-05-24 18:00:00", "narrative": "Several consecutive days of significant severe weather impacted eastern New Mexico from May 24-26, 2023. Showers and thunderstorms developed along the dryline and east slopes of the Sangre de Cristo Mountains on May 23rd. Storms tracked east and southeast across the eastern plains of New Mexico. Extensive severe weather was reported when these storms encountered greater moisture and lift closer to the Texas border. Hail up to 3.5 inches in diameter, thunderstorm wind gusts of 80 to 90 mph, and three tornados were reported in an area stretching from Union County to Roosevelt County. The largest hail stones and strongest wind gusts focused throughout Curry County during the evening hours. Hail and wind damage was reported in Tucumcari, Grady, and Clovis. Three separate tornadoes were reported in northern Curry County. Thunderstorms also dropped very heavy rainfall of 2 to 4 inches of rain across portions of Quay, De Baca, Curry, and Roosevelt Counties. Urban flooding occurred in Clovis, NM, causing some roads to be closed, and some cars to be stranded. Severe weather continued through the night and into May 25th with numerous reports of large hail, strong winds, and flash flooding. Quay County was particularly hard hit with baseball size hail and torrential rainfall amounts in excess of 5 inches. Significant hail damage was reported across Tucumcari with widespread flooding across the county. Severe wind gusts of 70 to 80 mph were common with these storms with damage reported. Strong to severe storms continued well into the night once again on the 25th with more heavy rainfall around the Caprock. The focus for severe weather shifted farther west on May 26th with large hail and heavy rainfall reported around Torrance County. A tornado and baseball size hail was also reported with a supercell near Encino. This activity spread eastward through the day with large hail, damaging wind gusts, and more torrential rainfall around the Caprock well into the night of May 26th. Three-day rainfall amounts exceeded 6 inches in many parts of Curry and Quay counties. One inch hail reported south of San Jon. Hail stones likely peaked larger than this based on surrounding 2 inch reports during this timeframe.", "ts_dict_index": [5238, 5239, 5240]}
+{"event_id": 813235, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-07 22:07:00", "end_date_time": "2019-05-07 22:07:00", "narrative": "By 1400 CST on the seventh, another consecutive day of severe weather was underway across the South Plains of West Texas. A dryline mixed into West Texas and stalled around the US Highway 385 corridor. Discrete supercells developed along the entire dryline through the South Plains. Fortunately, many of these thunderstorms did not produce severe hail. The strongest thunderstorm of the day initially developed in Lamb County and slowly moved northeast into Hale and Swisher Counties. Numerous storm chasers observed this storm and documented several tornadoes during its life cycle. The first tornado was observed approximately five miles southwest of Edmonson in Hale County. However, the NWS storm survey team was unable to locate any damage due to its brief duration and lack of damage indicators. Therefore, an EFU rating was assigned. The next tornado was observed several miles southwest of Tulia in Swisher County. Although this multi vortex tornado persisted for several minutes, no damage indicators were impacted, so an EFU rating was assigned to this tornado as well. The third tornado was observed about 4-5 miles northwest of Vigo Park and was the largest of the three. Similar to the other two tornadoes, no damage indicators were found by the NWS storm survey team, so a rating of EFU was assigned. Extremely strong rear flank downdraft winds were observed with this third tornado west of Vigo Park near the intersection of Farm to Market Roads 146 and 2301. A metal barn was partially destroyed and 19 wood transmission lines were snapped. Due to the slow moving nature of these storms, extremely heavy rainfall occurred in central Swisher County which brought an estimated three to six inches of rainfall over a short period of time. A NWS storm survey revealed many paved roads that had four to five feet of water running over the roadway. Several other roads still had mud from nearby fields on the roadway which indicates where water was over the roadway. ", "ts_dict_index": [5244, 5245, 5246]}
+{"event_id": 1091718, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2023-05-24 16:41:00", "end_date_time": "2023-05-24 17:15:00", "narrative": "Several consecutive days of significant severe weather impacted eastern New Mexico from May 24-26, 2023. Showers and thunderstorms developed along the dryline and east slopes of the Sangre de Cristo Mountains on May 23rd. Storms tracked east and southeast across the eastern plains of New Mexico. Extensive severe weather was reported when these storms encountered greater moisture and lift closer to the Texas border. Hail up to 3.5 inches in diameter, thunderstorm wind gusts of 80 to 90 mph, and three tornados were reported in an area stretching from Union County to Roosevelt County. The largest hail stones and strongest wind gusts focused throughout Curry County during the evening hours. Hail and wind damage was reported in Tucumcari, Grady, and Clovis. Three separate tornadoes were reported in northern Curry County. Thunderstorms also dropped very heavy rainfall of 2 to 4 inches of rain across portions of Quay, De Baca, Curry, and Roosevelt Counties. Urban flooding occurred in Clovis, NM, causing some roads to be closed, and some cars to be stranded. Severe weather continued through the night and into May 25th with numerous reports of large hail, strong winds, and flash flooding. Quay County was particularly hard hit with baseball size hail and torrential rainfall amounts in excess of 5 inches. Significant hail damage was reported across Tucumcari with widespread flooding across the county. Severe wind gusts of 70 to 80 mph were common with these storms with damage reported. Strong to severe storms continued well into the night once again on the 25th with more heavy rainfall around the Caprock. The focus for severe weather shifted farther west on May 26th with large hail and heavy rainfall reported around Torrance County. A tornado and baseball size hail was also reported with a supercell near Encino. This activity spread eastward through the day with large hail, damaging wind gusts, and more torrential rainfall around the Caprock well into the night of May 26th. Three-day rainfall amounts exceeded 6 inches in many parts of Curry and Quay counties. One inch hail was reported just west of San Jon, NM.", "ts_dict_index": [5229, 5230, 5231]}
+{"event_id": 1092783, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2023-05-26 23:00:00", "end_date_time": "2023-05-26 23:20:00", "narrative": "Several consecutive days of significant severe weather impacted eastern New Mexico from May 24-26, 2023. Showers and thunderstorms developed along the dryline and east slopes of the Sangre de Cristo Mountains on May 23rd. Storms tracked east and southeast across the eastern plains of New Mexico. Extensive severe weather was reported when these storms encountered greater moisture and lift closer to the Texas border. Hail up to 3.5 inches in diameter, thunderstorm wind gusts of 80 to 90 mph, and three tornados were reported in an area stretching from Union County to Roosevelt County. The largest hail stones and strongest wind gusts focused throughout Curry County during the evening hours. Hail and wind damage was reported in Tucumcari, Grady, and Clovis. Three separate tornadoes were reported in northern Curry County. Thunderstorms also dropped very heavy rainfall of 2 to 4 inches of rain across portions of Quay, De Baca, Curry, and Roosevelt Counties. Urban flooding occurred in Clovis, NM, causing some roads to be closed, and some cars to be stranded. Severe weather continued through the night and into May 25th with numerous reports of large hail, strong winds, and flash flooding. Quay County was particularly hard hit with baseball size hail and torrential rainfall amounts in excess of 5 inches. Significant hail damage was reported across Tucumcari with widespread flooding across the county. Severe wind gusts of 70 to 80 mph were common with these storms with damage reported. Strong to severe storms continued well into the night once again on the 25th with more heavy rainfall around the Caprock. The focus for severe weather shifted farther west on May 26th with large hail and heavy rainfall reported around Torrance County. A tornado and baseball size hail was also reported with a supercell near Encino. This activity spread eastward through the day with large hail, damaging wind gusts, and more torrential rainfall around the Caprock well into the night of May 26th. Three-day rainfall amounts exceeded 6 inches in many parts of Curry and Quay counties. Reports of 1.5 to 2 inch hail stones.", "ts_dict_index": [5235, 5236, 5237]}
+{"event_id": 885048, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2020-05-20 17:46:00", "end_date_time": "2020-05-20 18:19:00", "narrative": "Severe thunderstorms erupted for a second straight day across the South Plains. A large upper level low over the western United States allowed for low level moisture to remain in the region under low level southeasterly flow. A weak short wave moved out of central New Mexico into West Texas during the afternoon hours which aided in convective development along a dryline. Two general areas of convection matured into severe thunderstorms: one in the southwestern Texas Panhandle and another in the southern South Plains into the Permian Basin. Although there was no initial development in the central South Plains, this area saw the largest hail of the afternoon. Storms across the extreme southwestern Texas Panhandle generally produced hail up to ping pong ball size. At the same time, a severe thunderstorm near Post (Garza County) produced hail up to tennis ball size. The initial thunderstorms in the southern South Plains generated an outflow boundary that surged northward lifting very unstable air. Multi cellular thunderstorms developed along this outflow boundary in Lynn County but quickly moved northward into Lubbock County. One of these storms took on a anticyclonic circulation as it moved into southern Lubbock County. This storm would go on to produce a widespread swath of hail with sizes generally between hen eggs and tennis balls. The largest hailstone observed was three inches in diameter around the intersection of Quaker Ave. and 114th Street. The swath of giant hail began on the south side of the city of Lubbock (Lubbock County) and ended around Lubbock Preston Smith International Airport (Lubbock County). One of the other thunderstorms that developed on the outflow boundary also produced severe hail at the same time over the western portion of Lubbock County. This swath of hail was observed from just east of Wolfforth (Lubbock County) to Texas Tech University (Lubbock County) and consisted of hail mostly around golf ball size. Total damages in Lubbock County were estimated at $100 million due to substantial and widespread roof and vehicle damage. A thunderstorm developed along an outflow boundary in Lynn County and rapidly grew into a severe supercell thunderstorm as it moved northward toward the city of Lubbock. This storm quickly began to rotate anticyclonically as it moved into the southern portion of Lubbock County. As the storm entered the southern portion of the city of Lubbock numerous reports were initially received of hail up to baseball size. The largest hail stone reported was three inches in diameter. The storm continued to move northward through the central part of the city producing hail up to tennis ball size. The swath of giant hail ended around Lubbock Preston Smith International Airport at 1819 CST. While this initial storm was affecting the central portion of the city, a second severe thunderstorm developed over Wolfforth and moved to the northeast. This storm produced hail up to two inches in diameter from just east of Wolfforth to Texas Tech University. In the aftermath, numerous vehicles and roofs on homes were damaged, primarily from the initial thunderstorm that moved through the central part of Lubbock. Total losses were estimated at over $100 million.", "ts_dict_index": [5223, 5224, 5225]}
+{"event_id": 964011, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2021-06-15 18:25:00", "end_date_time": "2021-06-15 18:30:00", "narrative": "Despite weak upper forcing and fairly strong convective inhibition (CINH) keeping the vast majority of South Central Nebraska storm-free on this early Tuesday evening, a pair of rogue, slow-moving supercell storms were able to breach the cap and produce hail to at least golf ball size in small portions of Buffalo and Clay counties. The far southeastern Buffalo County storm initiated first, shortly before 7 p.m. CDT, and drifted slowly south before rapidly dissipating only about an hour later. Along the way  though, it dumped hail up to 2 inches in diameter on Shelton. Just as this storm was fading the second one got going in southeastern Clay County around 8 p.m. CDT and followed a very similar life cycle, drifting slowly south-southeast and dissipating 60-90 minutes later, but not before dropping golf ball size hail north of Edgar that reportedly damaged crops and cracked vehicle windshields. A weaker storm that split eastward from the Clay County supercell briefly affected northwestern Thayer County, but once this convection died around 930 p.m. CDT with the onset of diurnal cooling, the remainder of the night was storm-free. ||This somewhat-surprising, albeit brief/localized event was a textbook case of why one can never say never to at least isolated robust convection in a high instability environment during summer peak heating. In the mid-upper levels, South Central Nebraska resided along the northeast periphery of an expansive ridge centered over the Four Corners region. Although deep-layer shear was respectable (around 40 knots), the flow over the Central Plains lacked any notable disturbances and fairly strong capping was present (as indicated by 700 millibar temperatures around 12 C). However, upon closer review, a subtle northwest-southwest oriented surface boundary was draped across the heart of the local area, promoting weak low-level convergence between light easterly breezes and light southerlies. This subtle convergence, in tandem with fairly robust mixed-layer CAPE of 2000-3000 J/kg (owing to temperatures/dewpoints well into the 90s/60s F) proved just sufficient enough to spark the isolated severe activity. Hail up to 2 inches in diameter was reported.", "ts_dict_index": [5214, 5215, 5216]}
+{"event_id": 964013, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-06-15 19:30:00", "end_date_time": "2021-06-15 19:30:00", "narrative": "Despite weak upper forcing and fairly strong convective inhibition (CINH) keeping the vast majority of South Central Nebraska storm-free on this early Tuesday evening, a pair of rogue, slow-moving supercell storms were able to breach the cap and produce hail to at least golf ball size in small portions of Buffalo and Clay counties. The far southeastern Buffalo County storm initiated first, shortly before 7 p.m. CDT, and drifted slowly south before rapidly dissipating only about an hour later. Along the way  though, it dumped hail up to 2 inches in diameter on Shelton. Just as this storm was fading the second one got going in southeastern Clay County around 8 p.m. CDT and followed a very similar life cycle, drifting slowly south-southeast and dissipating 60-90 minutes later, but not before dropping golf ball size hail north of Edgar that reportedly damaged crops and cracked vehicle windshields. A weaker storm that split eastward from the Clay County supercell briefly affected northwestern Thayer County, but once this convection died around 930 p.m. CDT with the onset of diurnal cooling, the remainder of the night was storm-free. ||This somewhat-surprising, albeit brief/localized event was a textbook case of why one can never say never to at least isolated robust convection in a high instability environment during summer peak heating. In the mid-upper levels, South Central Nebraska resided along the northeast periphery of an expansive ridge centered over the Four Corners region. Although deep-layer shear was respectable (around 40 knots), the flow over the Central Plains lacked any notable disturbances and fairly strong capping was present (as indicated by 700 millibar temperatures around 12 C). However, upon closer review, a subtle northwest-southwest oriented surface boundary was draped across the heart of the local area, promoting weak low-level convergence between light easterly breezes and light southerlies. This subtle convergence, in tandem with fairly robust mixed-layer CAPE of 2000-3000 J/kg (owing to temperatures/dewpoints well into the 90s/60s F) proved just sufficient enough to spark the isolated severe activity. Hail up to golf ball size caused vehicle and crop damage in the area.", "ts_dict_index": [5211, 5212, 5213]}
+{"event_id": 1012044, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-04-21 22:43:00", "end_date_time": "2022-04-21 22:43:00", "narrative": "Between 10 p.m. CDT on Thursday the 21st and 3:30 a.m. on Friday the 22nd, a cluster of slightly elevated strong-to-severe thunderstorms rumbled across parts of South Central Nebraska, primarily affecting counties along/north of Highway 6 and also areas mainly east of a line from Holdrege-Loup City. Severe-criteria reports were fairly limited but were highlighted by: estimated 65 MPH winds near Clay Center that snapped a 12-inch diameter cedar tree; mesonet-measured wind gusts of 65 MPH near Clarks and 63 MPH near Kearney; quarter size hail in Grand Island and Sutton. Most places received well under 1 inch of rain except for a fairly narrow, southwest-northeast oriented swath of 1.00-1.50 centered from just west of Grand Island up through much of Merrick/Nance counties. ||Breaking down timing and storm evolution, the initial convection fired up slightly south of the Highway 6 corridor between 10-11 p.m. CDT, taking the form of a broken west-east oriented line. Over the next few hours, this primarily multicell convective line drifted steadily northward across the I-80 corridor, although along the way an embedded supercell briefly took shape over Clay County. Between 1-3 a.m. CDT the broken, west-east line of storms gradually consolidated into more of a compact cluster centered over Merrick/Nance counties, with the back-edge of the last severe-warned core departing the local area into eastern Nebraska by 3:30 a.m. CDT. This nocturnal event was a classic case of slightly elevated storms blossoming within the leading/north edge of low-level moisture advection and convergence within the heart of a strengthening low-level jet (40-60 knots at 850 millibars). In the mid-upper levels, South Central Nebraska resided under broad southwesterly flow, well-downstream from a large-scale trough coming onshore into California. At the surface, this event focused slightly north of a warm front that gradually lifted from northern KS into central NE over the course of the night. Mesoscale parameters featured 1000-2000 J/kg most-unstable CAPE and 40-50 knots of deep-layer shear, promoting the organized multicell and brief/transient supercell storm mode. ", "ts_dict_index": [5208, 5209, 5210]}
+{"event_id": 875876, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-12 06:20:00", "end_date_time": "2020-04-12 06:20:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. Golfball size hail fell at the Broadway Square Mall in Tyler, as well as Golden Road near Loop 323.", "ts_dict_index": [5199, 5200, 5201]}
+{"event_id": 823420, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2019-05-06 09:34:00", "end_date_time": "2019-05-06 09:34:00", "narrative": "Scattered elevated thunderstorms produced severe hail in a couple spots from late morning into early afternoon on this Monday. These storms occurred with surface temperatures usually not associated with thunderstorms. Scattered showers, with an embedded thunderstorm or two, were on-going at sunrise from the Sandhills south to near North Platte. This area of showers and isolated thunderstorms moved east into south central Nebraska. Around 9 AM CST, the thunderstorms began to increase in coverage and number. At 945 AM CST, a thunderstorm over southwest Buffalo county became severe, covering the ground with hail up to the size of quarters. Scattered thunderstorms continued to develop through midday. Around 12 PM CST, a severe storm produced 1.5 inch hail in eastern Franklin county, and another storm produced 1 inch hail in southeast Webster county. The thunderstorms were forming on the southwest edge of an increasing area of rain. New thunderstorm development ended during the afternoon, and the area of rain and thunderstorms moved east and out of the area by 4 PM CST.||A chilly air mass was over south central Nebraska. Temperatures were in the 40s to near 50. A strong, slow-moving cold front had moved through south central Nebraska the previous night, and it had become stationary across Kansas. In the upper-levels, the flow was zonal over the central and eastern U.S., with a broad trough extending into the north central United States from Canada. Mid-level lapse rates were between 7 and 8 C/km, with MUCAPE estimated around 500 J/kg. The freezing level was very low (around 9,000 ft AGL). Effective deep layer shear was 30-35 kt. These storms appeared to be associated with frontogenesis along the 850 mb front, and warm air advection from 850-700 mb. ", "ts_dict_index": [5277, 5278, 5279]}
+{"event_id": 809824, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-04-13 04:25:00", "end_date_time": "2019-04-13 04:25:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing several reports of damaging winds across portions of Northcentral Louisiana. These storms also produced locally heavy rainfall that led to instances of flash flooding, which resulted in two separate fatalities in Ouachita Parish. A 13 year old boy drowned in a drainage canal in the Bawcomville community during the heavy rains, and an 80 year old female drove past barricades on a closed road in Calhoun several hours after the heavy rains had ended, with her car becoming submerged in the flood waters. Unfortunately, she was unable to escape and drowned.  These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Quarter size hail fell south of Highway 160 in Western Bossier Parish.", "ts_dict_index": [5250, 5251, 5252]}
+{"event_id": 880563, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:52:00", "end_date_time": "2020-04-24 20:52:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Hail slightly larger than golfballs fell on Downs Circle in the Brownlee neighborhood of North Bossier City.", "ts_dict_index": [5289, 5290, 5291]}
+{"event_id": 880559, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:45:00", "end_date_time": "2020-04-24 20:45:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. A picture was posted to social media of quarter size hail that fell in the Rocky Mount community.", "ts_dict_index": [5283, 5284, 5285]}
+{"event_id": 835566, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2019-07-13 00:00:00", "end_date_time": "2019-07-13 00:00:00", "narrative": "Low-end severe hail occurred in Dawson and northwest Buffalo counties on this Friday night. During the evening hours, a broken arc of multi-cell thunderstorms was moving east through southwest Nebraska. These storms existed along a common cold pool, but individual cells were prominent rather than a solid squall line. The southern tip of this line entered Dawson county at 1030 PM CST. Shortly after entering the county, hail up to the size of quarters was reported in the extreme northwest corner of the county, 8 miles north of Gothenburg. At 11 PM CST, a new storm formed northeast of Cozad. This storm moved east and intensified over east-central Dawson county. After moving into northwestern Buffalo county, hail up to the size of quarters was reported in Miller at midnight CST. Severe hail probably occurred over east-central Dawson county as well, but no other reports were received given the time of night and location away from any towns.||1003 mb low pressure was advancing through Ontario, Canada. The associated weak cold front extended across northern Nebraska into the Panhandle and was nearly stationary. The storms initially formed along this front. In the upper-levels, a 594 dm subtropical high was over New Mexico and dominated the flow over the western and central United States. Weak, anticyclonic flow was over Nebraska. The westerlies were along the U.S.-Canada border. Immediately ahead of the line, temperatures were in the middle 70s, with dewpoints in the upper 60s. Mid-level lapse rates were very steep, more than 8 deg C/km, resulting in MUCAPE between 2000 and 2500 J/kg. However, effective deep layer shear was very weak, less than 20 kt. So, while there was sufficient instability for thunderstorms, the lack of shear limited storm severity. ", "ts_dict_index": [5274, 5275, 5276]}
+{"event_id": 1043929, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2022-07-22 21:34:00", "end_date_time": "2022-07-22 21:34:00", "narrative": "A slow-moving cluster of strong to severe thunderstorms rumbled along a path from the northwestern corner of Buffalo County to northwestern Adams County between the evening of Friday the 22nd into the very early morning of Saturday the 23rd, yielding a few reports of marginally-severe hail and winds, along with heavy rain and localized flooding. Isolated thunderstorms started developing around 8 PM CDT near the northern edge of the Dawson-Buffalo County line. Over the next few hours, activity gradually increased along a NW-SE swath line as it impacted northern/eastern Buffalo County and eventually entered Adams County. The training of initial storms brought heavy rainfall to northern portions of Buffalo County, with amounts as high as 3 to 4 inches reported, mainly falling between 10PM-1AM CDT. Creeks in the Pleasanton area were reported to be running full, and some rural roads were covered with water. The strongest storms produced quarter to golf ball size hail in the Pleasanton, Gibbon, and Kenesaw areas. Wind gusts near 60 MPH were reported near Shelton.||Upper level flow across the region was west-northwesterly and generally on the weaker side, as the area sat on the north side of high pressure centered over the Four Corners region. By early-late evening, the surface weather map showed low pressure setting up over western Kansas into far southwestern Nebraska, with a weak boundary extending into portions of central Nebraska. Convergence along the nose of an increasing low-level jet was the main driver of this activity. Though instability was plentiful, with MUCAPE values exceeding 3000 J/kg initially, deep layer shear was lacking, with values around 30 knots. With upper level support on the subtle side, overall coverage of thunderstorms in South Central Nebraska remained low through the overnight hours. ", "ts_dict_index": [5268, 5269, 5270]}
+{"event_id": 809827, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-04-13 04:47:00", "end_date_time": "2019-04-13 04:47:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing several reports of damaging winds across portions of Northcentral Louisiana. These storms also produced locally heavy rainfall that led to instances of flash flooding, which resulted in two separate fatalities in Ouachita Parish. A 13 year old boy drowned in a drainage canal in the Bawcomville community during the heavy rains, and an 80 year old female drove past barricades on a closed road in Calhoun several hours after the heavy rains had ended, with her car becoming submerged in the flood waters. Unfortunately, she was unable to escape and drowned.  These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Penny size hail fell in Blanchard.", "ts_dict_index": [5259, 5260, 5261]}
+{"event_id": 901250, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2020-06-20 18:10:00", "end_date_time": "2020-06-20 18:15:00", "narrative": "A smattering of strong to severe thunderstorms roamed South Central Nebraska from the early evening of Saturday the 20th into the very early morning of Sunday the 21st, prompting a few hail reports from widely-varying locations. The largest reported hail, ping pong to golf ball size, occurred in far southwestern Furnas County near Wilsonville. Later, quarter size stones fell from other storms at Wood River, Genoa and Silver Creek, although the late-night report from Silver Creek implied that much larger hail might have transpired (observer unable to confirm a maximum size). ||Isolated storms first drifted into western portions of the 24-county area between 6-8 p.m. CDT, after initiating a few hours prior in west-central Nebraska along a north-south oriented surface trough. These initial storms included the one that produced the large hail in Furnas County. Between 8-11 p.m. CDT the vast majority of limited storm activity was rather weak, with the main exception of the briefly-severe storm that produced the 1-inch hail in Hall County. Then, about the time it appeared that any severe threat had ended for the night, a small cluster of storms began intensifying over eastern Nance County around midnight CDT, likely in response to the onset of a fairly weak southwesterly low level jet. Over the next few hours, this convection briefly morphed into a supercell that drifted southeast across portions of Nance, Merrick and Polk counties (yielding the Genoa and Silver Creek hail reports) before departing the local area around 2 a.m. CDT. In the mid-upper levels, forcing was provided by a low-amplitude shortwave trough translating across Nebraska in west-northwest flow, well-south of a larger-scale trough anchored over south central Canada. Mesoscale parameters over South Central Nebraska during the evening were certainly supportive of severe storms, featuring around 2000 J/kg mixed-layer CAPE and deep layer wind shear of 30-40 knots. Hail ranging in size from ping pong balls to golf balls was reported along this path.", "ts_dict_index": [5247, 5248, 5249]}
+{"event_id": 823278, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2019-05-09 22:30:00", "end_date_time": "2019-05-09 22:30:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in several reports of tornadoes, with two separate tracks found across Northern Harrison and extreme Northeast Panola Counties, before the storms moved into North Louisiana by mid-afternoon. Locally heavy rainfall from the stronger storms within a short period of time also resulted in localized flash flooding across portions of Cass County, with flash flooding also reported across Eastern Harrison and Panola Counties during the early morning hours on May 9th as additional showers and thunderstorms redeveloped and moved repeatedly over the same areas. During the evening hours on the 9th, isolated severe thunderstorms developed over portions of Deep East Texas along old outflow boundaries from the storms earlier in the day. These storms produced large hail in extreme Southern Sabine County and Central Nacogdoches County before diminishing by midnight. Ping pong ball size hail fell along Highway 59 on the southwest side of Nacogdoches.", "ts_dict_index": [5265, 5266, 5267]}
+{"event_id": 880554, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-24 20:25:00", "end_date_time": "2020-04-24 20:25:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. A picture was posted to social media of golf ball size hail that fell on the southeast side of Vivian.", "ts_dict_index": [5280, 5281, 5282]}
+{"event_id": 880471, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-24 20:00:00", "end_date_time": "2020-04-24 20:00:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Quarter size hail fell in Keithville.", "ts_dict_index": [5286, 5287, 5288]}
+{"event_id": 890565, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2020-06-02 21:30:00", "end_date_time": "2020-06-02 21:30:00", "narrative": "On the evening of Tuesday the 2nd into the very early morning of Wednesday the 3rd, a cluster of strong to briefly-severe thunderstorms rumbled through the southwestern quadrant of South Central Nebraska (primarily affecting counties south of Interstate 80 and west of Highway 281). While most of this activity was sub-severe, a briefly-more-intense storm prompted a lone report of quarter size hail near Stamford around 10:45 p.m. CDT (penny size hail occurred in Beaver City shortly before this). ||Initially, South Central Nebraska remained mostly storm-free during the peak heating of late afternoon/early evening, but not by very far, as counties slightly to the west within southwest Nebraska and northwest Kansas saw a few strong to severe storms develop near a slow-moving cold front. Eventually, between 8-10 p.m. CDT, a loosely-organized cluster of multicell convection that evolved from this early activity propagated east into far southwestern local counties. Then, between 10 p.m. and midnight CDT a few embedded cells intensified enough to prompt severe thunderstorm warnings for parts of Furnas/Harlan/Phelps counties (although the quarter size hail near Stamford was the only ground-truth verification). After midnight, the dominant cell within the cluster gradually weakened as it traversed parts of Franklin/Kearney counties, dissipating by 2 a.m. CDT over western Adams County. While the evening mesoscale environment in South Central Nebraska was obviously sufficient for a marginally-severe storm, it was not supportive of widespread severe activity given that respectable mixed-layer CAPE of 1000-2000 J/kg was offset by weak deep-layer wind shear of no more than 25 knots. In the mid-upper levels, the local area resided under fairly anemic quasi-zonal flow, as the primary upper jet (and resultant stronger shear) resided farther north over the Dakotas. ", "ts_dict_index": [5262, 5263, 5264]}
+{"event_id": 809815, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2019-04-13 00:45:00", "end_date_time": "2019-04-13 00:45:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing several reports of damaging winds across portions of Northcentral Louisiana. These storms also produced locally heavy rainfall that led to instances of flash flooding, which resulted in two separate fatalities in Ouachita Parish. A 13 year old boy drowned in a drainage canal in the Bawcomville community during the heavy rains, and an 80 year old female drove past barricades on a closed road in Calhoun several hours after the heavy rains had ended, with her car becoming submerged in the flood waters. Unfortunately, she was unable to escape and drowned.  These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Golfball size hail fell in Florien.", "ts_dict_index": [5256, 5257, 5258]}
+{"event_id": 1092207, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2023-05-25 18:45:00", "end_date_time": "2023-05-25 19:20:00", "narrative": "Several consecutive days of significant severe weather impacted eastern New Mexico from May 24-26, 2023. Showers and thunderstorms developed along the dryline and east slopes of the Sangre de Cristo Mountains on May 23rd. Storms tracked east and southeast across the eastern plains of New Mexico. Extensive severe weather was reported when these storms encountered greater moisture and lift closer to the Texas border. Hail up to 3.5 inches in diameter, thunderstorm wind gusts of 80 to 90 mph, and three tornados were reported in an area stretching from Union County to Roosevelt County. The largest hail stones and strongest wind gusts focused throughout Curry County during the evening hours. Hail and wind damage was reported in Tucumcari, Grady, and Clovis. Three separate tornadoes were reported in northern Curry County. Thunderstorms also dropped very heavy rainfall of 2 to 4 inches of rain across portions of Quay, De Baca, Curry, and Roosevelt Counties. Urban flooding occurred in Clovis, NM, causing some roads to be closed, and some cars to be stranded. Severe weather continued through the night and into May 25th with numerous reports of large hail, strong winds, and flash flooding. Quay County was particularly hard hit with baseball size hail and torrential rainfall amounts in excess of 5 inches. Significant hail damage was reported across Tucumcari with widespread flooding across the county. Severe wind gusts of 70 to 80 mph were common with these storms with damage reported. Strong to severe storms continued well into the night once again on the 25th with more heavy rainfall around the Caprock. The focus for severe weather shifted farther west on May 26th with large hail and heavy rainfall reported around Torrance County. A tornado and baseball size hail was also reported with a supercell near Encino. This activity spread eastward through the day with large hail, damaging wind gusts, and more torrential rainfall around the Caprock well into the night of May 26th. Three-day rainfall amounts exceeded 6 inches in many parts of Curry and Quay counties. There were multiple reports from storm chasers of large hail ranging in size from 2 to 3.5 inches just east-northeast of Tucumcari along U.S. Highway 54. Thankfully there were no reports of damage directly related to the hail.", "ts_dict_index": [5232, 5233, 5234]}
+{"event_id": 880469, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 19:50:00", "end_date_time": "2020-04-24 19:50:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Quarter size hail was reported in the Red Chute community.", "ts_dict_index": [5292, 5293, 5294]}
+{"event_id": 880570, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 21:01:00", "end_date_time": "2020-04-24 21:01:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Golfball size hail fell in the Tall Timbers subdivision.", "ts_dict_index": [5301, 5302, 5303]}
+{"event_id": 880565, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:51:00", "end_date_time": "2020-04-24 20:51:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. A picture was posted to social media of softball size hail that fell in the Legacy subdivision in North Bossier City.", "ts_dict_index": [5295, 5296, 5297]}
+{"event_id": 880468, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 19:17:00", "end_date_time": "2020-04-24 19:17:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. A photo of quarter size hail that fell in the Rocky Mount community was submitted to social media.", "ts_dict_index": [5298, 5299, 5300]}
+{"event_id": 809819, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-04-13 04:25:00", "end_date_time": "2019-04-13 04:25:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing several reports of damaging winds across portions of Northcentral Louisiana. These storms also produced locally heavy rainfall that led to instances of flash flooding, which resulted in two separate fatalities in Ouachita Parish. A 13 year old boy drowned in a drainage canal in the Bawcomville community during the heavy rains, and an 80 year old female drove past barricades on a closed road in Calhoun several hours after the heavy rains had ended, with her car becoming submerged in the flood waters. Unfortunately, she was unable to escape and drowned.  These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Dime to quarter size hail fell in the Woodlake Ridge subdivision just north of Bossier City.", "ts_dict_index": [5253, 5254, 5255]}
+{"event_id": 880462, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-24 19:27:00", "end_date_time": "2020-04-24 19:27:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Half dollar size hail fell off of North Market Street.", "ts_dict_index": [5325, 5326, 5327]}
+{"event_id": 880465, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 19:38:00", "end_date_time": "2020-04-24 19:38:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Ping pong ball size hail fell in the Colony subdivision in North Bossier City.", "ts_dict_index": [5304, 5305, 5306]}
+{"event_id": 880571, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:52:00", "end_date_time": "2020-04-24 20:52:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Golfball size hail fell several miles southeast of Benton, damaging vinyl siding, the roof, and gutters of a home. Large limbs were also downed as well.", "ts_dict_index": [5313, 5314, 5315]}
+{"event_id": 880474, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 19:49:00", "end_date_time": "2020-04-24 19:49:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Quarter size hail fell near the intersection of Stockwell Road and Shed Road in East Bossier City.", "ts_dict_index": [5337, 5338, 5339]}
+{"event_id": 880467, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-24 19:27:00", "end_date_time": "2020-04-24 19:27:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Quarter size hail fell on Forest Cove Drive in North Shreveport.", "ts_dict_index": [5316, 5317, 5318]}
+{"event_id": 880564, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:50:00", "end_date_time": "2020-04-24 20:50:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Baseball size hail fell about 5 miles east of Benton.", "ts_dict_index": [5319, 5320, 5321]}
+{"event_id": 880464, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 19:38:00", "end_date_time": "2020-04-24 19:38:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Quarter size hail fell at the intersection of Benton Road and Interstate 220 in North Bossier City.", "ts_dict_index": [5322, 5323, 5324]}
+{"event_id": 880573, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:57:00", "end_date_time": "2020-04-24 20:57:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Large hail ranging in size from quarters to slightly larger than golf balls fell in the Dogwood subdivision in East Bossier City.", "ts_dict_index": [5328, 5329, 5330]}
+{"event_id": 880578, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:59:00", "end_date_time": "2020-04-24 20:59:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Golfball size hail fell in the Red Chute community just east of Bossier City.", "ts_dict_index": [5307, 5308, 5309]}
+{"event_id": 880557, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:45:00", "end_date_time": "2020-04-24 20:45:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. A picture was posted to social media of golfball size hail that fell in Benton.", "ts_dict_index": [5334, 5335, 5336]}
+{"event_id": 880562, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:50:00", "end_date_time": "2020-04-24 20:50:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Golf ball size hail fell about 3 miles north of Interstate 220 on Benton Road.", "ts_dict_index": [5331, 5332, 5333]}
+{"event_id": 880472, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:02:00", "end_date_time": "2020-04-24 20:02:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Half dollar size hail fell on Coldwater Creek in the Eastwood community.", "ts_dict_index": [5340, 5341, 5342]}
+{"event_id": 867066, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-01-11 01:12:00", "end_date_time": "2020-01-11 01:12:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Nickel size hail fell in East Shreveport.", "ts_dict_index": [5271, 5272, 5273]}
+{"event_id": 1015774, "event_type": "Hail", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2022-03-05 14:06:00", "end_date_time": "2022-03-05 14:06:00", "narrative": "On March 5, 2022 a total of 15 tornadoes occurred across the state of Iowa as a warm front lifted across the area. Supercells initially developed across southwest Iowa in the vicinity of the triple point of the surface low with strong, rotating updrafts. Longevity was initially lacking with the storms, producing funnel clouds, brief tornadoes, and hail in southwest Iowa. As the cells moved northeast and matured, larger hail began to fall with golf ball sized hail falling in Adams county and baseball sized hail into Adair county. Following this period of large hail the storms produced a tornado which would remain on the ground for just over 70 miles, carving a path across central Iowa from southwest of Winterset to just northeast of Newton. The tornado peaked in Winterset, Iowa, producing EF-4 damage with wind speeds estimated near 170 mph. The tornado continued across the southern portion of the Des Moines metro area and to Newton. This is the furthest north EF-4 tornado in the CONUS this early in the year on record, the first EF-4 tornado in Iowa since October 4, 2013 which occurred in Woodbury and Cherokee Counties, and is the second longest tornado in Iowa since 1980, behind the longest occurring on June 7, 1984 at a length of 117 miles across southern Iowa. As the storm skimmed the southern Des Moines metro, cells across south central became tornadic, producing several destructive tornadoes including an EF-3 tornado in Chariton, Iowa. This heartbreaking day resulted in seven fatalities, six in Winterset and one in Chariton, making it the deadliest tornado outbreak in Iowa since 2008. At 15 tornadoes, this is also one of the earliest outbreaks of this magnitude to occur so early in the season. Social media picture of quarter sized hail.", "ts_dict_index": [5361, 5362, 5363]}
+{"event_id": 1064239, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2023-01-03 02:15:00", "end_date_time": "2023-01-03 02:15:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of Deep East Texas, which resulted in areas of flash flooding from the mid-afternoon through the evening hours on the 2nd. Isolated severe thunderstorms continued to develop even during the early morning hours on the 3rd, which produced sporadic reports of large hail. Ping pong ball size hail fell just south of Cushing on FM 225 just north of its intersection with FM 343.", "ts_dict_index": [5364, 5365, 5366]}
+{"event_id": 1018265, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2022-05-23 21:08:00", "end_date_time": "2022-05-23 21:08:00", "narrative": "Returning Gulf of Mexico moisture into the South Plains of West Texas fueled widespread severe thunderstorm development across the region on the afternoon and evening of the 23rd. Moderate to strong instability developed across the western South Plains and eastern New Mexico Monday afternoon and evening as the improving low-level moisture and temperatures warming into the 80s developed beneath an approaching upper level storm system. Relatively strong wind shear caused several of the thunderstorms to rotate as they moved into the western South Plains and western Texas Panhandle. A cluster of thunderstorms moving northeast out of southeastern New Mexico interacted with an outflow boundary moving northwest out of the Permian Basin. This caused a storm on the southern flank of the cluster to begin to rotate and become supercellular and take a more easterly, then southeasterly track. As the storm intensified, it became cyclic in behavior and its forward speed varied from about 5 mph to 20 mph. An NWS storm survey revealed that this supercell produced nine separate tornadoes over an approximately two hour period. The tornadoes occurred over rural areas which limited the overall impacts. Spotty damage did occur including two oil pumpjacks that were toppled by the intense tornadic winds. This damage, along with snapped power poles and flipped center pivots earned a peak damage rating of EF-2. The thunderstorms eventually evolved into a larger complex that brought widespread rain to most of the South Plains, Rolling Plains, and southern Texas Panhandle. The heaviest rain was associated with the slow-moving tornadic storm and was concentrated over Bailey County, where three to as much as seven inches of rain fell. A trained spotter reported quarter size hail along Farm to Market Road 1294 west of Shallowater.", "ts_dict_index": [5355, 5356, 5357]}
+{"event_id": 880561, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-24 20:46:00", "end_date_time": "2020-04-24 20:46:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Half dollar size hail fell near the intersection of Highway 1 and Interstate 49 near Blanchard.", "ts_dict_index": [5349, 5350, 5351]}
+{"event_id": 880477, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:14:00", "end_date_time": "2020-04-24 20:14:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Half dollar size hail fell near Haughton.", "ts_dict_index": [5352, 5353, 5354]}
+{"event_id": 880470, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-24 19:51:00", "end_date_time": "2020-04-24 19:51:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Quarter size hail fell between Greenwood and Bethany.", "ts_dict_index": [5343, 5344, 5345]}
+{"event_id": 880473, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-24 20:01:00", "end_date_time": "2020-04-24 20:01:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Ping pong ball size hail fell in Keithville.", "ts_dict_index": [5346, 5347, 5348]}
+{"event_id": 1015790, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-03-05 17:23:00", "end_date_time": "2022-03-05 17:23:00", "narrative": "On March 5, 2022 a total of 15 tornadoes occurred across the state of Iowa as a warm front lifted across the area. Supercells initially developed across southwest Iowa in the vicinity of the triple point of the surface low with strong, rotating updrafts. Longevity was initially lacking with the storms, producing funnel clouds, brief tornadoes, and hail in southwest Iowa. As the cells moved northeast and matured, larger hail began to fall with golf ball sized hail falling in Adams county and baseball sized hail into Adair county. Following this period of large hail the storms produced a tornado which would remain on the ground for just over 70 miles, carving a path across central Iowa from southwest of Winterset to just northeast of Newton. The tornado peaked in Winterset, Iowa, producing EF-4 damage with wind speeds estimated near 170 mph. The tornado continued across the southern portion of the Des Moines metro area and to Newton. This is the furthest north EF-4 tornado in the CONUS this early in the year on record, the first EF-4 tornado in Iowa since October 4, 2013 which occurred in Woodbury and Cherokee Counties, and is the second longest tornado in Iowa since 1980, behind the longest occurring on June 7, 1984 at a length of 117 miles across southern Iowa. As the storm skimmed the southern Des Moines metro, cells across south central became tornadic, producing several destructive tornadoes including an EF-3 tornado in Chariton, Iowa. This heartbreaking day resulted in seven fatalities, six in Winterset and one in Chariton, making it the deadliest tornado outbreak in Iowa since 2008. At 15 tornadoes, this is also one of the earliest outbreaks of this magnitude to occur so early in the season. Public report of 2.5 inch or greater hail stones in Pleasant Hill via Twitter.", "ts_dict_index": [5358, 5359, 5360]}
+{"event_id": 880575, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-24 20:57:00", "end_date_time": "2020-04-24 20:57:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. Baseball size hail fell near the intersection of Stockwell Road and Shed Road in the Stockwell subdivision of Bossier City.", "ts_dict_index": [5310, 5311, 5312]}
+{"event_id": 881103, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-28 17:30:00", "end_date_time": "2020-04-28 17:30:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Penny to quarter size hail fell near Troup.", "ts_dict_index": [5394, 5395, 5396]}
+{"event_id": 881096, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-28 15:14:00", "end_date_time": "2020-04-28 15:14:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Quarter size hail fell in the Central Heights Community.", "ts_dict_index": [5379, 5380, 5381]}
+{"event_id": 881097, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-28 15:30:00", "end_date_time": "2020-04-28 15:30:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Quarter size hail fell near the Appleby community.", "ts_dict_index": [5400, 5401, 5402]}
+{"event_id": 881094, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-28 14:38:00", "end_date_time": "2020-04-28 14:38:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Photos of golf ball size hail that fell in the Woden community were submitted to social media.", "ts_dict_index": [5376, 5377, 5378]}
+{"event_id": 881101, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-28 16:50:00", "end_date_time": "2020-04-28 16:50:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Golfball size hail fell in the Good Springs community.", "ts_dict_index": [5367, 5368, 5369]}
+{"event_id": 881071, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-28 16:52:00", "end_date_time": "2020-04-28 16:52:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Ping pong ball size hail fell several miles southwest of Henderson.", "ts_dict_index": [5388, 5389, 5390]}
+{"event_id": 881099, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-28 16:45:00", "end_date_time": "2020-04-28 16:45:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Golfball size hail fell on FM 839 near the Compton community.", "ts_dict_index": [5397, 5398, 5399]}
+{"event_id": 881093, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-29 00:16:00", "end_date_time": "2020-04-29 00:16:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Ping pong ball size hail fell in the Laird Hill community.", "ts_dict_index": [5370, 5371, 5372]}
+{"event_id": 881113, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-29 00:38:00", "end_date_time": "2020-04-29 00:38:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Nickel size hail fell near New London.", "ts_dict_index": [5403, 5404, 5405]}
+{"event_id": 859244, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 16:32:00", "end_date_time": "2019-10-01 16:32:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. Public relayed video depicting ping pong ball sized hail.", "ts_dict_index": [5421, 5422, 5423]}
+{"event_id": 859238, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 16:30:00", "end_date_time": "2019-10-01 16:30:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. WHO TV relayed tennis ball sized hail report. Time estimated from radar.", "ts_dict_index": [5409, 5410, 5411]}
+{"event_id": 859243, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 16:32:00", "end_date_time": "2019-10-01 16:32:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. Public reported baseball sized hail via picture from social media.", "ts_dict_index": [5406, 5407, 5408]}
+{"event_id": 859239, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 16:31:00", "end_date_time": "2019-10-01 16:31:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. Trained spotter reported half dollar sized hail.", "ts_dict_index": [5418, 5419, 5420]}
+{"event_id": 881109, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-29 00:27:00", "end_date_time": "2020-04-29 00:27:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Quarter size hail fell a few miles south of the Lakeport community.", "ts_dict_index": [5385, 5386, 5387]}
+{"event_id": 859245, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 16:34:00", "end_date_time": "2019-10-01 16:34:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. Amateur radio operator reported quarter sized hail.", "ts_dict_index": [5412, 5413, 5414]}
+{"event_id": 859242, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 16:32:00", "end_date_time": "2019-10-01 16:32:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. Public reported quarter sized hail via mPING app.", "ts_dict_index": [5415, 5416, 5417]}
+{"event_id": 859237, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 16:27:00", "end_date_time": "2019-10-01 16:27:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. Broadcast media relayed golf ball sized hail report.", "ts_dict_index": [5424, 5425, 5426]}
+{"event_id": 1080880, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-02 17:50:00", "end_date_time": "2023-03-02 17:50:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 1st and through March 2nd. Strong warm and moist air advection was ongoing in advance of the trough preceding the event. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. This environment produced an isolated strong thunderstorm that produced nickel size hail just south of Haworth on the 1st. A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing an isolated tornado in addition to large hail and damaging wind gusts Across McCurtain County Oklahoma. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threat of large hail also continued through the end of the event. Hail up to quarter size covered the ground in Rufe.", "ts_dict_index": [5427, 5428, 5429]}
+{"event_id": 881085, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-28 23:50:00", "end_date_time": "2020-04-28 23:50:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Half dollar size hail fell in Lindale.", "ts_dict_index": [5373, 5374, 5375]}
+{"event_id": 1044296, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2022-08-18 16:05:00", "end_date_time": "2022-08-18 16:35:00", "narrative": "A cold front brought isolated to scattered severe thunderstorms with large hail to portions of South Central Nebraska on the evening of August 18th. The first signs of thunderstorm development along the cold front showed itself in Valley County between 3 PM to 4 PM CDT. Temperatures ahead of the front were in the 80s, which was supportive of moderate instability. As instability increased ahead of the front between 4 PM and 5 PM, thunderstorms strengthened and became severe on an isolated basis roughly near the Highway 92 corridor. By 5 PM, a storm near Ravenna in far northeast Buffalo County developed supercell characteristics and began to produce significant amounts of large hail, including up to golf ball size. This storm weakened as it moved southeast through eastern Buffalo County by 6 PM, but a new intense storm developed over central Buffalo County and also became severe and produced large hail just northeast and east of Kearney in the Gibbon area. Around the same time, a lone/isolated supercell developed just north of Genoa along the Boone/Platte County line and quickly became severe. This storm slowly moved south into eastern Nance County between 6:00-6:30 PM, and ended up producing the largest hail of the evening, up to baseball size, in and around Genoa. Significant damage occurred as a result, particularly to crops, vehicles, and roofs. The storm weakened as it moved into Polk County, but still managed to produce severe hail up to ping pong ball size in western Polk County between 7-7:30 PM. Activity quickly decreased in coverage and severity as nocturnal cooling set in between 7:30-8 PM. Hail ranging in size from quarters to golf balls was reported in this area. Windows were shattered out of a vehicle six miles southwest of Boelus.", "ts_dict_index": [5451, 5452, 5453]}
+{"event_id": 1026406, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2022-05-17 18:16:00", "end_date_time": "2022-05-17 18:42:00", "narrative": "Cold front leads to strong to severe thunderstorms for portions of south central Nebraska during the evening of May 17th. The first thunderstorms of this event developed over southwest Furnas County between 4PM and 5PM CDT. The initial concern was the potential for landspouts, and at least two were reported in the area of Wilsonville and Beaver City. As is often the case with landspouts, these were very brief touchdowns, and no damage indicators could be found, so they were given an EFU, or unknown, rating. This initial setup for landspouts was fairly typical for this region in which steep low level lapse rates coincided with weak deep layer wind shear, weak low level convergence, and a weak surface front that provides abundant ambient surface vorticity. Eventually, between 5PM and 7PM, thunderstorms ���unzipped���, or developed further northeast in Kearney County, along the advancing cold front, which lead to upscale growth into a couple intense thunderstorm clusters. Large hail was the primary hazard with this activity, and for the most part ranged from quarter to golf ball size. However, up to 3 inch in diameter hail was reported in Harlan County. The thunderstorm clusters moved east and southeast, and eventually weakened and/or shifted in northern Kansas around 8PM CDT.||Another separate broken line of thunderstorms developed further north, from around Kearney to Columbus, between 9PM and 10PM. This activity persisted for a couple of hours before weakening. Once again, large hail was the primary threat, with penny to half dollar size hail reported in portions of Hall and Hamilton Counties. Hail between quarter and ping pong ball size was reported in Edison.", "ts_dict_index": [5457, 5458, 5459]}
+{"event_id": 994046, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2022-01-08 16:10:00", "end_date_time": "2022-01-08 16:10:00", "narrative": "A strong upper level low pressure system tracked east across the Red River Valley of Southern Oklahoma and North Texas during the afternoon of January 8th, before shifting across Northeast Texas into Southwest Arkansas during the early morning hours of the 9th. Ahead of this low, strong southerly low level winds rapidly transported low level moisture back north across the region, with large scale forcing and elevated instability ahead of the low contributing to areas of showers and embedded thunderstorms over East Texas, North Louisiana, and Southwest Arkansas. An isolated severe thunderstorm developed during the afternoon of the 8th over Nacogdoches County in East Texas, producing ping pong ball size hail just southeast of Nacogdoches. Meanwhile, a warm front spread north into portions of Deep East Texas and Central Louisiana during the late evening and early morning hours, with increasing instability and low level wind shear fueling the development of strong to severe thunderstorms over these areas. These storms produced damaging winds which downed trees and limbs in Sabine County, with additional severe storms later spawning two tornadoes in Southern Sabine Parish, Louisiana. These storms also continued to develop and move repeatedly over the same areas during the early morning hours across extreme Southeast Angelina, Southern San Augustine, and Central Sabine Counties, producing a narrow swath of heavy rain with amounts ranging from 3-7+ inches. This resulted in extensive flash flooding across Southern San Augustine and Central Sabine Counties, before the storms shifted east into West Central Louisiana just prior to daybreak on the 9th. Ping pong ball size hail fell off of East Main Street near Nottingham and Robin Hood Drives.", "ts_dict_index": [5433, 5434, 5435]}
+{"event_id": 1044301, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2022-08-18 16:51:00", "end_date_time": "2022-08-18 17:29:00", "narrative": "A cold front brought isolated to scattered severe thunderstorms with large hail to portions of South Central Nebraska on the evening of August 18th. The first signs of thunderstorm development along the cold front showed itself in Valley County between 3 PM to 4 PM CDT. Temperatures ahead of the front were in the 80s, which was supportive of moderate instability. As instability increased ahead of the front between 4 PM and 5 PM, thunderstorms strengthened and became severe on an isolated basis roughly near the Highway 92 corridor. By 5 PM, a storm near Ravenna in far northeast Buffalo County developed supercell characteristics and began to produce significant amounts of large hail, including up to golf ball size. This storm weakened as it moved southeast through eastern Buffalo County by 6 PM, but a new intense storm developed over central Buffalo County and also became severe and produced large hail just northeast and east of Kearney in the Gibbon area. Around the same time, a lone/isolated supercell developed just north of Genoa along the Boone/Platte County line and quickly became severe. This storm slowly moved south into eastern Nance County between 6:00-6:30 PM, and ended up producing the largest hail of the evening, up to baseball size, in and around Genoa. Significant damage occurred as a result, particularly to crops, vehicles, and roofs. The storm weakened as it moved into Polk County, but still managed to produce severe hail up to ping pong ball size in western Polk County between 7-7:30 PM. Activity quickly decreased in coverage and severity as nocturnal cooling set in between 7:30-8 PM. Quarter to golf ball size hail was reported in this area.", "ts_dict_index": [5454, 5455, 5456]}
+{"event_id": 953086, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2021-05-17 18:48:00", "end_date_time": "2021-05-17 18:48:00", "narrative": "A widespread severe thunderstorm event occurred on the afternoon and evening of the 17th. Thunderstorms initially formed along a dryline near the Texas/New Mexico state line and along an outflow boundary from previous day storms. The ample instability was complemented by large scale lift moving overhead from an upper level jet moving into the southern High Plains. Very intense supercells developed across the entirety of the South Plains, Rolling Plains, and extreme southern Texas Panhandle due to the abundant amount of unstable air. Several supercells produced hail up to baseball size as they slowly moved across the region. One particularly robust rotating storm developed over Hockley County and moved eastward into Lubbock County and through the city of Lubbock. This storm developed several funnel clouds and a brief tornado in far eastern Hockley County. The low level circulation moved directly over the southern portion of the city of Lubbock but did not produce any additional tornadoes. Decaying thunderstorms also produced two high wind gusts. These high wind gusts were measured by the Texas Tech University West Texas mesonet at Friona (Parmer County) 64 mph and Lesley (Hall County) 59 mph. Lastly, thunderstorms repeatedly formed over central Bailey County causing flash flooding along Farm to Market Road 746 west of Texas Highway 214.||In the early morning hours of the 18th, stratiform precipitation from decaying thunderstorms produced two high wind gusts. One near Graham of 62 mph and the other near Hackberry (Cottle County) of 59 mph. Both of these reports came from the Texas Tech University West Texas mesonet. A trained spotter reported quarter size hail at 108th Street and Indiana Avenue in the city of Lubbock.", "ts_dict_index": [5442, 5443, 5444]}
+{"event_id": 1112412, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-16 03:30:00", "end_date_time": "2023-06-16 03:30:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Golf ball size hail reported near Bullard via social media.", "ts_dict_index": [5448, 5449, 5450]}
+{"event_id": 953089, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2021-05-17 19:12:00", "end_date_time": "2021-05-17 19:32:00", "narrative": "A widespread severe thunderstorm event occurred on the afternoon and evening of the 17th. Thunderstorms initially formed along a dryline near the Texas/New Mexico state line and along an outflow boundary from previous day storms. The ample instability was complemented by large scale lift moving overhead from an upper level jet moving into the southern High Plains. Very intense supercells developed across the entirety of the South Plains, Rolling Plains, and extreme southern Texas Panhandle due to the abundant amount of unstable air. Several supercells produced hail up to baseball size as they slowly moved across the region. One particularly robust rotating storm developed over Hockley County and moved eastward into Lubbock County and through the city of Lubbock. This storm developed several funnel clouds and a brief tornado in far eastern Hockley County. The low level circulation moved directly over the southern portion of the city of Lubbock but did not produce any additional tornadoes. Decaying thunderstorms also produced two high wind gusts. These high wind gusts were measured by the Texas Tech University West Texas mesonet at Friona (Parmer County) 64 mph and Lesley (Hall County) 59 mph. Lastly, thunderstorms repeatedly formed over central Bailey County causing flash flooding along Farm to Market Road 746 west of Texas Highway 214.||In the early morning hours of the 18th, stratiform precipitation from decaying thunderstorms produced two high wind gusts. One near Graham of 62 mph and the other near Hackberry (Cottle County) of 59 mph. Both of these reports came from the Texas Tech University West Texas mesonet. A tornadic supercell produced a swath of mostly quarter size hail from Wolfforth across a small portion of the southern part of the city of Lubbock from 1912 CST through 1932 CST. A photograph on social media showed a maximum hail size of golf ball size in Wolfforth.", "ts_dict_index": [5445, 5446, 5447]}
+{"event_id": 880438, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-24 19:30:00", "end_date_time": "2020-04-24 19:30:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Numerous reports of large hail were reported from these storms, with some isolated instances of damaging winds and funnel clouds across portions of Northeast Texas. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening, thus ending the severe threat for Northeast Texas with the cold frontal passage. A picture of quarter size hail that fell in Tatum was posted to social media.", "ts_dict_index": [5439, 5440, 5441]}
+{"event_id": 880429, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-24 19:12:00", "end_date_time": "2020-04-24 19:12:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Numerous reports of large hail were reported from these storms, with some isolated instances of damaging winds and funnel clouds across portions of Northeast Texas. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening, thus ending the severe threat for Northeast Texas with the cold frontal passage. Quarter size hail was reported near the intersection of County Road 2118 and County Road 2121.", "ts_dict_index": [5436, 5437, 5438]}
+{"event_id": 1086980, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-01 17:35:00", "end_date_time": "2023-03-01 17:35:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 1st and through March 2nd. Strong warm and moist air advection was ongoing in advance of the trough preceding the event. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. This environment produced an isolated strong thunderstorm that produced nickel size hail just south of Haworth on the 1st. A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing an isolated tornado in addition to large hail and damaging wind gusts Across McCurtain County Oklahoma. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threat of large hail also continued through the end of the event. Nickel size hail reported just south of Haworth.", "ts_dict_index": [5430, 5431, 5432]}
+{"event_id": 826934, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-06-24 18:45:00", "end_date_time": "2019-06-24 18:45:00", "narrative": "The evening of the 24th saw very large hail in Lubbock and Lynn Counties as well as a wind turbine completely destroyed near Petersburg (Hale County). Low level moisture streamed into the region early in the morning with low stratus covering the region. However, this low stratus deck burned off quickly which lead to rapid destabilization of the atmosphere. By late in the afternoon, surface based CAPE was analyzed at values between 4000 and 5000 Joules per kg. Despite very little deep layer shear available in the atmosphere, large hail still developed with the substantial amount of instability. Isolated thunderstorms initially developed over the Permian Basin with one of these storms moving northeast into Lynn County. The first storm in Lynn County produced baseball size hail. While baseball size hail was dropping in Tahoka (Lynn County), an isolated thunderstorm rapidly developed over southwestern Lubbock County. This initial thunderstorm moved to the northeast producing hail up to golf ball size. Additional thunderstorms developed along the outflow of this initial thunderstorm. One of these storms moved from the south part of the city of Lubbock to Slaton producing baseball size hail. Another storm developed near New Deal (Lubbock County) and moved northeast into southeastern Hale County. This storm produced hail up to three inches in diameter east of New Deal. However, the most incredible damage from this storm occurred near Petersburg in Hale County. A newly installed wind turbine was completely destroyed by severe thunderstorm winds. Hail up to the size of golf balls were reported on the south side of the city of Lubbock. This hail was from one of several severe thunderstorms that developed off of the outflow of the initial thunderstorm in southwestern Lubbock County.", "ts_dict_index": [5460, 5461, 5462]}
+{"event_id": 826936, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-06-24 18:39:00", "end_date_time": "2019-06-24 18:39:00", "narrative": "The evening of the 24th saw very large hail in Lubbock and Lynn Counties as well as a wind turbine completely destroyed near Petersburg (Hale County). Low level moisture streamed into the region early in the morning with low stratus covering the region. However, this low stratus deck burned off quickly which lead to rapid destabilization of the atmosphere. By late in the afternoon, surface based CAPE was analyzed at values between 4000 and 5000 Joules per kg. Despite very little deep layer shear available in the atmosphere, large hail still developed with the substantial amount of instability. Isolated thunderstorms initially developed over the Permian Basin with one of these storms moving northeast into Lynn County. The first storm in Lynn County produced baseball size hail. While baseball size hail was dropping in Tahoka (Lynn County), an isolated thunderstorm rapidly developed over southwestern Lubbock County. This initial thunderstorm moved to the northeast producing hail up to golf ball size. Additional thunderstorms developed along the outflow of this initial thunderstorm. One of these storms moved from the south part of the city of Lubbock to Slaton producing baseball size hail. Another storm developed near New Deal (Lubbock County) and moved northeast into southeastern Hale County. This storm produced hail up to three inches in diameter east of New Deal. However, the most incredible damage from this storm occurred near Petersburg in Hale County. A newly installed wind turbine was completely destroyed by severe thunderstorm winds. A spotter at the Slaton Municipal Airport reported baseball size hail. This hail was from one of several severe thunderstorms that developed off of the outflow of the initial thunderstorm in southwestern Lubbock County.", "ts_dict_index": [5463, 5464, 5465]}
+{"event_id": 881102, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-28 16:51:00", "end_date_time": "2020-04-28 16:51:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Ping pong ball size hail fell on County Road 475 south of the Price community.", "ts_dict_index": [5382, 5383, 5384]}
+{"event_id": 824146, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-24 18:15:00", "end_date_time": "2019-05-24 18:15:00", "narrative": "A persistent upper level trough over the western United States allowed for another day of convective development across the South Plains of West Texas. Although strong large scale lift was not anticipated on the afternoon of the 24th, widespread severe thunderstorms developed under a very moist and unstable atmosphere. A quasi-stationary warm front began to move northward during the morning hours with a dryline mixing into the South Plains from the west. Very high surface dew points in the warm sector allowed mixed layer instabilities to climb to values greater than 3000 J/kg. Thunderstorms easily blossomed under these conditions and produced widespread hail up to the size of golf balls, in particular, across Lubbock County. The presence of the quasi-stationary front and dryline allowed thunderstorms to train over many areas. The most devastating flooding was observed in Crosby County where numerous roads became flooded and impassable. Flooding was also extreme in Lubbock County where many vehicles became stranded in flood waters on the south side of the city of Lubbock. Late in the evening, a home of a NWS cooperative weather observer became partially inundated by flood waters due to training of thunderstorms. One thunderstorm took on supercell characteristics while moving across Motley County. Although no tornadoes were observed, several severe wind gusts were reported by the Texas Tech University West Texas mesonet and a NSSL mobile mesonet. These winds also caused numerous power poles and trees to be downed in Roaring Springs. A trained spotter reported golf ball size hail near the intersection of US Highway 84 and Farm to Market Road 2528.", "ts_dict_index": [5481, 5482, 5483]}
+{"event_id": 826932, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-06-24 17:50:00", "end_date_time": "2019-06-24 18:32:00", "narrative": "The evening of the 24th saw very large hail in Lubbock and Lynn Counties as well as a wind turbine completely destroyed near Petersburg (Hale County). Low level moisture streamed into the region early in the morning with low stratus covering the region. However, this low stratus deck burned off quickly which lead to rapid destabilization of the atmosphere. By late in the afternoon, surface based CAPE was analyzed at values between 4000 and 5000 Joules per kg. Despite very little deep layer shear available in the atmosphere, large hail still developed with the substantial amount of instability. Isolated thunderstorms initially developed over the Permian Basin with one of these storms moving northeast into Lynn County. The first storm in Lynn County produced baseball size hail. While baseball size hail was dropping in Tahoka (Lynn County), an isolated thunderstorm rapidly developed over southwestern Lubbock County. This initial thunderstorm moved to the northeast producing hail up to golf ball size. Additional thunderstorms developed along the outflow of this initial thunderstorm. One of these storms moved from the south part of the city of Lubbock to Slaton producing baseball size hail. Another storm developed near New Deal (Lubbock County) and moved northeast into southeastern Hale County. This storm produced hail up to three inches in diameter east of New Deal. However, the most incredible damage from this storm occurred near Petersburg in Hale County. A newly installed wind turbine was completely destroyed by severe thunderstorm winds. Numerous reports were received of hail up to golf ball size in the city of Lubbock. The reports in the city of Lubbock were from one of many severe thunderstorms that developed in Lubbock County. Several severe thunderstorms developed off of the outflow of the initial thunderstorm in southwestern Lubbock County. Additionally, a large tree branch was broken off of a tree in the parking lot of the NWS office.", "ts_dict_index": [5469, 5470, 5471]}
+{"event_id": 824127, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-24 12:59:00", "end_date_time": "2019-05-24 13:31:00", "narrative": "A persistent upper level trough over the western United States allowed for another day of convective development across the South Plains of West Texas. Although strong large scale lift was not anticipated on the afternoon of the 24th, widespread severe thunderstorms developed under a very moist and unstable atmosphere. A quasi-stationary warm front began to move northward during the morning hours with a dryline mixing into the South Plains from the west. Very high surface dew points in the warm sector allowed mixed layer instabilities to climb to values greater than 3000 J/kg. Thunderstorms easily blossomed under these conditions and produced widespread hail up to the size of golf balls, in particular, across Lubbock County. The presence of the quasi-stationary front and dryline allowed thunderstorms to train over many areas. The most devastating flooding was observed in Crosby County where numerous roads became flooded and impassable. Flooding was also extreme in Lubbock County where many vehicles became stranded in flood waters on the south side of the city of Lubbock. Late in the evening, a home of a NWS cooperative weather observer became partially inundated by flood waters due to training of thunderstorms. One thunderstorm took on supercell characteristics while moving across Motley County. Although no tornadoes were observed, several severe wind gusts were reported by the Texas Tech University West Texas mesonet and a NSSL mobile mesonet. These winds also caused numerous power poles and trees to be downed in Roaring Springs. A cluster of thunderstorms moving into southwestern Lubbock County brought a widespread swath of severe hail. The first report was from a NWS employee five miles south of Wolfforth at 1259 CST. The final report came at 1331 CST in northwest Lubbock. Hail was mostly quarter to half dollar size with the largest report of golf ball size along US Highway 62/82 southwest of Wolfforth.", "ts_dict_index": [5478, 5479, 5480]}
+{"event_id": 826816, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-06-24 18:50:00", "end_date_time": "2019-06-24 18:59:00", "narrative": "The evening of the 24th saw very large hail in Lubbock and Lynn Counties as well as a wind turbine completely destroyed near Petersburg (Hale County). Low level moisture streamed into the region early in the morning with low stratus covering the region. However, this low stratus deck burned off quickly which lead to rapid destabilization of the atmosphere. By late in the afternoon, surface based CAPE was analyzed at values between 4000 and 5000 Joules per kg. Despite very little deep layer shear available in the atmosphere, large hail still developed with the substantial amount of instability. Isolated thunderstorms initially developed over the Permian Basin with one of these storms moving northeast into Lynn County. The first storm in Lynn County produced baseball size hail. While baseball size hail was dropping in Tahoka (Lynn County), an isolated thunderstorm rapidly developed over southwestern Lubbock County. This initial thunderstorm moved to the northeast producing hail up to golf ball size. Additional thunderstorms developed along the outflow of this initial thunderstorm. One of these storms moved from the south part of the city of Lubbock to Slaton producing baseball size hail. Another storm developed near New Deal (Lubbock County) and moved northeast into southeastern Hale County. This storm produced hail up to three inches in diameter east of New Deal. However, the most incredible damage from this storm occurred near Petersburg in Hale County. A newly installed wind turbine was completely destroyed by severe thunderstorm winds. A picture posted to social media depicted hail up to the size of baseballs at 1850 CST in New Deal. At 1859 CST, three inch hail was reported seven miles east of New Deal by a trained spotter. This hail was from one of several severe thunderstorms that developed off of the outflow of the initial thunderstorm in southwestern Lubbock County.", "ts_dict_index": [5472, 5473, 5474]}
+{"event_id": 947255, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-05-04 10:05:00", "end_date_time": "2021-05-04 10:05:00", "narrative": "Very warm, moist, and humid air spread back north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma during the afternoon hours of May 3rd, along a strong southerly low level jet. This resulted in a moderately unstable air mass across the region, which lingered during the evening hours across Southeast Oklahoma, ahead of a upper trough that moved across the Southern Plains. This trough enhanced large scale forcing along the dryline across Central Oklahoma and North Texas, with scattered strong to severe thunderstorms developing over these areas, which shifted east northeast into the unstable air across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the late evening and early morning hours of the 14th. Numerous reports of damaging winds were received across these areas before the storms diminished during the early morning hours of the 4th.||These storms left behind a cold pool surface boundary across portions of East Texas, extreme Northwest Louisiana, and South-central Arkansas, which focused additional severe thunderstorm development from the late morning through the afternoon hours of the 4th, as large scale forcing again increased with the approaching upper trough atop the moderately unstable air mass along this mesoscale boundary. Additional reports of damaging winds were received across Deep East Texas, North Louisiana, and South-central Arkansas from these storms, before they spread southeast into Eastern and Southern Louisiana and Mississippi by mid and late afternoon. Nickel size hail fell in the St. Charles neighborhood south of the Southern Loop.", "ts_dict_index": [5475, 5476, 5477]}
+{"event_id": 881092, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-29 00:06:00", "end_date_time": "2020-04-29 00:06:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Quarter size hail fell on the northwest side of Tyler.", "ts_dict_index": [5391, 5392, 5393]}
+{"event_id": 881318, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-29 00:22:00", "end_date_time": "2020-04-29 00:22:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Quarter size hail fell in Southeast Shreveport.", "ts_dict_index": [5517, 5518, 5519]}
+{"event_id": 824144, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-24 15:58:00", "end_date_time": "2019-05-24 15:58:00", "narrative": "A persistent upper level trough over the western United States allowed for another day of convective development across the South Plains of West Texas. Although strong large scale lift was not anticipated on the afternoon of the 24th, widespread severe thunderstorms developed under a very moist and unstable atmosphere. A quasi-stationary warm front began to move northward during the morning hours with a dryline mixing into the South Plains from the west. Very high surface dew points in the warm sector allowed mixed layer instabilities to climb to values greater than 3000 J/kg. Thunderstorms easily blossomed under these conditions and produced widespread hail up to the size of golf balls, in particular, across Lubbock County. The presence of the quasi-stationary front and dryline allowed thunderstorms to train over many areas. The most devastating flooding was observed in Crosby County where numerous roads became flooded and impassable. Flooding was also extreme in Lubbock County where many vehicles became stranded in flood waters on the south side of the city of Lubbock. Late in the evening, a home of a NWS cooperative weather observer became partially inundated by flood waters due to training of thunderstorms. One thunderstorm took on supercell characteristics while moving across Motley County. Although no tornadoes were observed, several severe wind gusts were reported by the Texas Tech University West Texas mesonet and a NSSL mobile mesonet. These winds also caused numerous power poles and trees to be downed in Roaring Springs. A picture on social media showed mostly quarter sized hail with some half dollar size hail on the northwest side of the city of Lubbock.", "ts_dict_index": [5484, 5485, 5486]}
+{"event_id": 1014572, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2022-04-12 23:01:00", "end_date_time": "2022-04-12 23:01:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. Quarter size hail was reported in Nacogdoches.", "ts_dict_index": [5508, 5509, 5510]}
+{"event_id": 947073, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-05-04 00:12:00", "end_date_time": "2021-05-04 00:12:00", "narrative": "Very warm, moist, and humid air spread back north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma during the afternoon hours of May 3rd, along a strong southerly low level jet. This resulted in a moderately unstable air mass across the region, which lingered during the evening hours across Southeast Oklahoma, ahead of a upper trough that moved across the Southern Plains. This trough enhanced large scale forcing along the dryline across Central Oklahoma and North Texas, with scattered strong to severe thunderstorms developing over these areas, which shifted east northeast into the unstable air across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the late evening and early morning hours of the 14th. Numerous reports of damaging winds were received across these areas before the storms diminished during the early morning hours of the 4th.||These storms left behind a cold pool surface boundary across portions of East Texas, extreme Northwest Louisiana, and South-central Arkansas, which focused additional severe thunderstorm development from the late morning through the afternoon hours of the 4th, as large scale forcing again increased with the approaching upper trough atop the moderately unstable air mass along this mesoscale boundary. Additional reports of damaging winds were received across Deep East Texas and North Louisiana from these storms, before they spread southeast into Eastern and Southern Louisiana and Mississippi by mid and late afternoon. Nickel size hail fell in the Carroll community.", "ts_dict_index": [5496, 5497, 5498]}
+{"event_id": 813757, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2019-05-20 00:37:00", "end_date_time": "2019-05-20 00:39:00", "narrative": "A powerful spring storm system that moved slowly east through the southwest United States on May 20-21, 2019 produced a variety of spring weather conditions over northern and central New Mexico. The active weather pattern began on the evening of the 19th when a virga bomb impacted the Albuquerque Sunport with a brief wind gust to 64 mph. Power outages were reported across parts of Nob Hill and Ridgecrest. Low level moisture then surged northwest into eastern New Mexico while a potent jet streak moved in from the southwest. Severe thunderstorms develop over the far eastern plains shortly after midnight. Golf ball size hail, strong winds, and heavy rainfall impacted Quay County. Southwest winds then increased quickly after sunrise on the 20th when widespread wind gusts of 45 to 55 mph were reported around south central and eastern New Mexico. The strongest winds impacted Lincoln County where gusts near 60 mph were reported. Meanwhile, several inches of snow fell over northern and western New Mexico through the morning of the 21st, including Farmington, Gallup, and Raton. Strong northwest winds then impacted much of eastern New Mexico on the afternoon of the 21st as the powerful storm system moved into the Great Plains states. Peak wind gusts of 60 to 70 mph were common along the Interstate 40 corridor east of Tijeras Canyon. Temperatures ended up 15 to 25 degrees below normal in many areas in the wake of this storm system. A rapidly moving severe thunderstorm produced golf ball size hail in Logan.", "ts_dict_index": [5538, 5539, 5540]}
+{"event_id": 811375, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-04-13 08:50:00", "end_date_time": "2019-04-13 08:50:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing numerous reports of damaging winds with several tornadoes across portions of East Texas. These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Quarter size hail fell in the Antioch community.", "ts_dict_index": [5511, 5512, 5513]}
+{"event_id": 824142, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-24 15:47:00", "end_date_time": "2019-05-24 15:49:00", "narrative": "A persistent upper level trough over the western United States allowed for another day of convective development across the South Plains of West Texas. Although strong large scale lift was not anticipated on the afternoon of the 24th, widespread severe thunderstorms developed under a very moist and unstable atmosphere. A quasi-stationary warm front began to move northward during the morning hours with a dryline mixing into the South Plains from the west. Very high surface dew points in the warm sector allowed mixed layer instabilities to climb to values greater than 3000 J/kg. Thunderstorms easily blossomed under these conditions and produced widespread hail up to the size of golf balls, in particular, across Lubbock County. The presence of the quasi-stationary front and dryline allowed thunderstorms to train over many areas. The most devastating flooding was observed in Crosby County where numerous roads became flooded and impassable. Flooding was also extreme in Lubbock County where many vehicles became stranded in flood waters on the south side of the city of Lubbock. Late in the evening, a home of a NWS cooperative weather observer became partially inundated by flood waters due to training of thunderstorms. One thunderstorm took on supercell characteristics while moving across Motley County. Although no tornadoes were observed, several severe wind gusts were reported by the Texas Tech University West Texas mesonet and a NSSL mobile mesonet. These winds also caused numerous power poles and trees to be downed in Roaring Springs. Trained spotters in Wolfforth reported hail up to golf ball size.", "ts_dict_index": [5487, 5488, 5489]}
+{"event_id": 824147, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-24 19:27:00", "end_date_time": "2019-05-24 19:27:00", "narrative": "A persistent upper level trough over the western United States allowed for another day of convective development across the South Plains of West Texas. Although strong large scale lift was not anticipated on the afternoon of the 24th, widespread severe thunderstorms developed under a very moist and unstable atmosphere. A quasi-stationary warm front began to move northward during the morning hours with a dryline mixing into the South Plains from the west. Very high surface dew points in the warm sector allowed mixed layer instabilities to climb to values greater than 3000 J/kg. Thunderstorms easily blossomed under these conditions and produced widespread hail up to the size of golf balls, in particular, across Lubbock County. The presence of the quasi-stationary front and dryline allowed thunderstorms to train over many areas. The most devastating flooding was observed in Crosby County where numerous roads became flooded and impassable. Flooding was also extreme in Lubbock County where many vehicles became stranded in flood waters on the south side of the city of Lubbock. Late in the evening, a home of a NWS cooperative weather observer became partially inundated by flood waters due to training of thunderstorms. One thunderstorm took on supercell characteristics while moving across Motley County. Although no tornadoes were observed, several severe wind gusts were reported by the Texas Tech University West Texas mesonet and a NSSL mobile mesonet. These winds also caused numerous power poles and trees to be downed in Roaring Springs. A trained spotter reported quarter size hail along Interstate 27 south of Abernathy.", "ts_dict_index": [5490, 5491, 5492]}
+{"event_id": 940445, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-03-27 22:17:00", "end_date_time": "2021-03-27 22:17:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track across East Texas, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area through the early morning hours of the 28th. Penny size hail fell just southwest of the Eastwood community. Report from mPING.", "ts_dict_index": [5535, 5536, 5537]}
+{"event_id": 817764, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2019-04-26 21:24:00", "end_date_time": "2019-04-26 21:24:00", "narrative": "On this Friday evening, a northeast-southwest oriented line of strong to marginally-severe thunderstorms tracked across primarily portions of Dawson, Buffalo and northern Phelps counties before weakening. These storms yielded a few reports of nickel to quarter size hail, with the quarter size reports in the Gothenburg and Elm Creek areas. In addition, wind gusts were estimated at 50-55 MPH near Gothenburg, but with no ground-truth of severe-criteria speeds. Convection first intensified just west of the local area (over Lincoln County) around 8 p.m. CDT before entering Dawson County around 9 p.m. CDT. During the next few hours this fairly small-scale line of storms tracked east-southeast, weakening below severe thresholds before reaching the Kearney area. Other non-severe storms (a few strong) continued roaming parts of South Central Nebraska into the very early morning of Saturday the 27th, but the entire local area was storm-free by around 3 a.m. CDT. In the mid-upper levels, the main driving force was a progressive shortwave trough tracking east-southeast from the Northern Rockies. At the surface, convection blossomed near the intersection of a northeast-southwest oriented trough axis and a northwest-southeast oriented quasi-stationary front stretched across the heart of Nebraska. Despite meager low-level moisture (surface dewpoints only in the 30s-40s F), the combination of modest most-unstable CAPE of 500-1000 J/kg and strong deep-layer wind shear around 50 knots proved sufficient for marginally-severe storms. ", "ts_dict_index": [5493, 5494, 5495]}
+{"event_id": 940446, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-03-27 22:31:00", "end_date_time": "2021-03-27 22:31:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track across East Texas, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area through the early morning hours of the 28th. Quarter and slightly larger size hail fell in Haughton.", "ts_dict_index": [5532, 5533, 5534]}
+{"event_id": 813756, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2019-05-20 00:15:00", "end_date_time": "2019-05-20 00:17:00", "narrative": "A powerful spring storm system that moved slowly east through the southwest United States on May 20-21, 2019 produced a variety of spring weather conditions over northern and central New Mexico. The active weather pattern began on the evening of the 19th when a virga bomb impacted the Albuquerque Sunport with a brief wind gust to 64 mph. Power outages were reported across parts of Nob Hill and Ridgecrest. Low level moisture then surged northwest into eastern New Mexico while a potent jet streak moved in from the southwest. Severe thunderstorms develop over the far eastern plains shortly after midnight. Golf ball size hail, strong winds, and heavy rainfall impacted Quay County. Southwest winds then increased quickly after sunrise on the 20th when widespread wind gusts of 45 to 55 mph were reported around south central and eastern New Mexico. The strongest winds impacted Lincoln County where gusts near 60 mph were reported. Meanwhile, several inches of snow fell over northern and western New Mexico through the morning of the 21st, including Farmington, Gallup, and Raton. Strong northwest winds then impacted much of eastern New Mexico on the afternoon of the 21st as the powerful storm system moved into the Great Plains states. Peak wind gusts of 60 to 70 mph were common along the Interstate 40 corridor east of Tijeras Canyon. Temperatures ended up 15 to 25 degrees below normal in many areas in the wake of this storm system. A rapidly developing severe thunderstorm produced hail up to the size of golf balls along NM-278 southeast of Tucumcari.", "ts_dict_index": [5544, 5545, 5546]}
+{"event_id": 1096343, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-05-06 19:34:00", "end_date_time": "2023-05-06 19:40:00", "narrative": "Long-track, elevated supercell brings swath of large hail to portions of south central Nebraska during the evening of May 6th with additional elevated storms and large hail over far northern portions of the area late overnight. The main story with this event was a lone, elevated supercell, that cycled several times to produce a nearly continuous swath of large hail from around the Elwood, NE area ESE to around the Hebron, NE area. This supercell initially developed just W of the CWA during the late afternoon hours, well N of the primary outflow boundary that was placed just S of the NE/KS state line, and moved into Gosper Co. around 1800CDT. Despite stable conditions at/near the surface, lingering moderate elevated instability and strong effective shear enabled this supercell to continue ESE through the remainder of the evening. The largest hail reported within this swath was tennis ball size in northern Nuckolls Co. between 2000-2100CDT. The supercell exited Thayer Co. to the E shortly before 2200CDT. This portion of the severe episode was largely unexpected as this area was not included in any of the daytime SPC Day 1 Convective Outlooks.||What was more accurately anticipated was a band of elevated convection during the late overnight and early morning hours of May 6th into May 7th over far N portions of the CWA. These storms affected mainly Valley Co. between 0300-0400CDT and produced a few instances of quarter to ping pong ball size hail. Hail up to the size of tennis balls was reported in Edgar.", "ts_dict_index": [5529, 5530, 5531]}
+{"event_id": 814716, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2019-05-20 00:40:00", "end_date_time": "2019-05-20 00:41:00", "narrative": "A powerful spring storm system that moved slowly east through the southwest United States on May 20-21, 2019 produced a variety of spring weather conditions over northern and central New Mexico. The active weather pattern began on the evening of the 19th when a virga bomb impacted the Albuquerque Sunport with a brief wind gust to 64 mph. Power outages were reported across parts of Nob Hill and Ridgecrest. Low level moisture then surged northwest into eastern New Mexico while a potent jet streak moved in from the southwest. Severe thunderstorms develop over the far eastern plains shortly after midnight. Golf ball size hail, strong winds, and heavy rainfall impacted Quay County. Southwest winds then increased quickly after sunrise on the 20th when widespread wind gusts of 45 to 55 mph were reported around south central and eastern New Mexico. The strongest winds impacted Lincoln County where gusts near 60 mph were reported. Meanwhile, several inches of snow fell over northern and western New Mexico through the morning of the 21st, including Farmington, Gallup, and Raton. Strong northwest winds then impacted much of eastern New Mexico on the afternoon of the 21st as the powerful storm system moved into the Great Plains states. Peak wind gusts of 60 to 70 mph were common along the Interstate 40 corridor east of Tijeras Canyon. Temperatures ended up 15 to 25 degrees below normal in many areas in the wake of this storm system. Penny size hail was reported in Logan.", "ts_dict_index": [5541, 5542, 5543]}
+{"event_id": 821744, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-05-25 21:25:00", "end_date_time": "2019-05-25 21:25:00", "narrative": "A single report of low-end severe hail occurred on this Saturday evening. Around 9 PM CST, an isolated thunderstorm began forming over Webster and Nuckolls county. This storm moved northeast, intensified, and briefly produced quarter size hail in Edgar around 930 PM CST. This storm moved into Fillmore county by 10 PM CST. By that time, a few other showers and thunderstorms had developed in a discontinuous arc from McCook to near Hastings with the storm over Fillmore county at the eastern edge of this arc. A mesoscale convective system had been moving northeast across central and eastern Kansas during the late afternoon and early evening. Given the linear organization of the showers and thunderstorms over south central Nebraska, it is possible they were triggered by an outflow boundary or undular bore. Between midnight and 1 AM CST, these showers and storms dissipated.||Low pressure was near Hudson Bay. The associated cold front extended southwest and became stationary from southeast Nebraska through western Kansas to another low near Pueblo. The flow aloft was moderately amplified with west-southwest flow over the central Plains. A longwave trough was along the west coast, and a subtropical high was over the southeast states. Around the time of thunderstorm initiation, surface temperatures were in the upper 60s with dewpoints around 60. With mid-level lapse rates 7.0-7.5 C/km, MUCAPE was around 1500 J/kg. Effective deep layer shear was near 45 kt. ", "ts_dict_index": [5523, 5524, 5525]}
+{"event_id": 1096340, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-05-06 19:13:00", "end_date_time": "2023-05-06 19:25:00", "narrative": "Long-track, elevated supercell brings swath of large hail to portions of south central Nebraska during the evening of May 6th with additional elevated storms and large hail over far northern portions of the area late overnight. The main story with this event was a lone, elevated supercell, that cycled several times to produce a nearly continuous swath of large hail from around the Elwood, NE area ESE to around the Hebron, NE area. This supercell initially developed just W of the CWA during the late afternoon hours, well N of the primary outflow boundary that was placed just S of the NE/KS state line, and moved into Gosper Co. around 1800CDT. Despite stable conditions at/near the surface, lingering moderate elevated instability and strong effective shear enabled this supercell to continue ESE through the remainder of the evening. The largest hail reported within this swath was tennis ball size in northern Nuckolls Co. between 2000-2100CDT. The supercell exited Thayer Co. to the E shortly before 2200CDT. This portion of the severe episode was largely unexpected as this area was not included in any of the daytime SPC Day 1 Convective Outlooks.||What was more accurately anticipated was a band of elevated convection during the late overnight and early morning hours of May 6th into May 7th over far N portions of the CWA. These storms affected mainly Valley Co. between 0300-0400CDT and produced a few instances of quarter to ping pong ball size hail. Hail up to the size of golf balls was reported along this path.", "ts_dict_index": [5526, 5527, 5528]}
+{"event_id": 1014576, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2022-04-12 22:58:00", "end_date_time": "2022-04-12 22:58:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. Quarter size hail fell on the southwest side of Nacogdoches.", "ts_dict_index": [5505, 5506, 5507]}
+{"event_id": 854760, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-10-20 17:38:00", "end_date_time": "2019-10-20 17:38:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. A video was posted to Facebook of penny to quarter size hail that fell near the intersection of Highways 79 and 42 in Southwest Rusk County.", "ts_dict_index": [5499, 5500, 5501]}
+{"event_id": 880459, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-04-24 18:55:00", "end_date_time": "2020-04-24 18:55:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear had also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Numerous reports of large hail were reported from these storms, with some isolated instances of damaging winds and funnel clouds across portions of Northeast Texas. These storms accelerated southeast into portions of Northwest Louisiana by mid-evening, thus ending the severe threat for Southeast Oklahoma and Northeast Texas with the cold frontal passage. Quarter size hail fell at the intersection of Highways 37 and 98 west of Idabel.", "ts_dict_index": [5514, 5515, 5516]}
+{"event_id": 854761, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-10-20 17:54:00", "end_date_time": "2019-10-20 17:54:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. A picture was posted to Facebook of penny size hail that fell in Henderson.", "ts_dict_index": [5502, 5503, 5504]}
+{"event_id": 826935, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-06-24 18:35:00", "end_date_time": "2019-06-24 18:35:00", "narrative": "The evening of the 24th saw very large hail in Lubbock and Lynn Counties as well as a wind turbine completely destroyed near Petersburg (Hale County). Low level moisture streamed into the region early in the morning with low stratus covering the region. However, this low stratus deck burned off quickly which lead to rapid destabilization of the atmosphere. By late in the afternoon, surface based CAPE was analyzed at values between 4000 and 5000 Joules per kg. Despite very little deep layer shear available in the atmosphere, large hail still developed with the substantial amount of instability. Isolated thunderstorms initially developed over the Permian Basin with one of these storms moving northeast into Lynn County. The first storm in Lynn County produced baseball size hail. While baseball size hail was dropping in Tahoka (Lynn County), an isolated thunderstorm rapidly developed over southwestern Lubbock County. This initial thunderstorm moved to the northeast producing hail up to golf ball size. Additional thunderstorms developed along the outflow of this initial thunderstorm. One of these storms moved from the south part of the city of Lubbock to Slaton producing baseball size hail. Another storm developed near New Deal (Lubbock County) and moved northeast into southeastern Hale County. This storm produced hail up to three inches in diameter east of New Deal. However, the most incredible damage from this storm occurred near Petersburg in Hale County. A newly installed wind turbine was completely destroyed by severe thunderstorm winds. A trained spotter reported ping pong ball size hail at Buffalo Springs Lake. This hail was from one of several severe thunderstorms that developed off of the outflow of the initial thunderstorm in southwestern Lubbock County.", "ts_dict_index": [5466, 5467, 5468]}
+{"event_id": 821741, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2019-05-16 19:05:00", "end_date_time": "2019-05-16 19:05:00", "narrative": "A couple severe wind gusts and small hail occurred over parts of Furnas and Phelps counties on this Thursday evening. During the late afternoon, a couple small thunderstorms developed over northwest Kansas. They moved northeast and by 6 PM CST, they were in the McCook area. These storms congealed into a single storm, and by 630 PM CST the resulting storm moved into northwest Furnas county where winds were measured at 57 MPH at the Cambridge airport, and nickel size hail fell at Holbrook around 700 PM CST. This storm continued moving slightly north of east into southern Phelps county where winds were measured at 61 MPH between Atlanta and Holdrege, and 66 MPH between Loomis and Holdrege. The storm then rapidly weakened and dissipated over eastern Phelps county by 9 PM CST.||These storms formed in the warm sector. High pressure was off the coast of the Carolina's, while a stationary front extended from the Great Lakes across Nebraska to low pressure over eastern Colorado. The upper-level flow was moderately-amplified with a ridge over the Plains and a deep trough along the West Coast. As is typical for this area, these were high based storms that formed due to deep mixing. Just prior to the storms moving in, temperatures were in the lower 90s with dewpoints in the middle to upper 40s. Mid-level lapse rates were steep (8.5 C/km) resulting in MLCAPE around 1500 J/kg. Effective deep layer shear was weak, around 20 kt. ", "ts_dict_index": [5547, 5548, 5549]}
+{"event_id": 881317, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-29 00:20:00", "end_date_time": "2020-04-29 00:20:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Quarter size hail fell in East Shreveport.", "ts_dict_index": [5520, 5521, 5522]}
+{"event_id": 1087019, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-04-26 14:48:00", "end_date_time": "2023-04-26 14:48:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Nickel size hail fell in the New Harmony community.", "ts_dict_index": [5595, 5596, 5597]}
+{"event_id": 816273, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2019-05-26 17:12:00", "end_date_time": "2019-05-26 17:17:00", "narrative": "A potent upper level storm system approaching New Mexico from the west interacted with deep moisture and very unstable conditions along a sharp dryline over eastern New Mexico on May 26, 2019. Dry showers and thunderstorms with strong downburst winds first developed along the Continental Divide by late morning before marching east into the Rio Grande Valley through the afternoon. Several locations within the Rio Grande Valley reported wind gusts in excess of 60 mph, including Los Lunas, Albuquerque, Santa Fe, and Taos. Wind damage was also reported as this activity moved across the central mountain chain into the Estancia Valley. Meanwhile, showers and thunderstorms fired up along the dryline in eastern New Mexico then quickly became severe with large hail, high winds, and several tornados. A violent supercell thunderstorm that moved through Union County during the late afternoon produced at least two tornadoes and three inch hail. Severe thunderstorms then evolved into a quasi-linear convective system over the Caprock region and resulted in a large area of high winds and large hail. Several more tornadoes developed along the southern edge of this line, including a spectacular wedge tornado near Dora. In addition to all the severe thunderstorms that impacted the region, many areas outside of thunderstorm activity in central and western New Mexico also reported strong southwest winds with gusts of 50 to 60 mph. Quarter size hail reported near Wheatland.", "ts_dict_index": [5550, 5551, 5552]}
+{"event_id": 1111965, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-07-04 19:15:00", "end_date_time": "2023-07-04 19:45:00", "narrative": "An upper level trough was over the northern Rocky Mountains and Northern Plains and was bringing a cold front south through Nebraska during the afternoon and evening hours of Independence Day. Temperatures heated up in advance of the front with dewpoints mostly in the 60s. A very moist and unstable atmosphere was present. CAPE values were generally near 4,000 J/kg ahead of the front, and 0 to 6 km wind shear values were around 35 knots. Mid-level lapse rates were generally 7 to 8 degrees C/km. ||Isolated showers and storms were moving across portions of south central Nebraska during the early to mid-afternoon hours. This activity did not produce any severe weather. The main storm activity developed late in the afternoon into the evening hours and was associated with the cold front moving through Nebraska. Storms began developing in central Nebraska in the late afternoon and early evening hours. Then storms developed in south central Nebraska and formed a line with the storms in the central part of the state. The storms in central Nebraska moved southeast during the evening hours while the storms in the south central part of the state remained fairly stationary. The storms produced large hail and wind gusts of 58 to 66 mph between 5:30 PM CDT and 9 PM CDT. The largest hail reported was up to 2.50 inches and was reported in Webster, Fillmore, and Thayer Counties. Hail up to the size of nickels fell off-and-on for approximately 30 minutes.", "ts_dict_index": [5565, 5566, 5567]}
+{"event_id": 1087032, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-04-26 16:00:00", "end_date_time": "2023-04-26 16:00:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Golfball size hail fell on County Road 405D southwest of Henderson.", "ts_dict_index": [5571, 5572, 5573]}
+{"event_id": 1087031, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-04-26 15:50:00", "end_date_time": "2023-04-26 15:50:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Quarter size hail fell in the Carlisle Price community.", "ts_dict_index": [5580, 5581, 5582]}
+{"event_id": 842454, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-07-20 16:20:00", "end_date_time": "2019-07-20 16:20:00", "narrative": "The atmosphere was juiced so to speak ahead of a cold front sliding into the region. MUCAPE values very quickly approached and exceeded 4000 J/kg by mid-morning. With the cold front and previous storm outflows the impetus for new convection, discrete storms were not expected, with the prevailing storm type being the linear or quasi-linear convective system (QLCS) variety. Additional support for the QLCS mode was seen with, once again the cold frontal and outflow forcing, highly unstable atmosphere, and little to no convective inhibition.  Additional support for strong winds was seen with DCAPE values in excess of 1500 J/kg across much of the area  Once a system began to produce a decent cold pool, there would be little to prevent it from progressing. ||That was evident in Iowa as two distinct QLCSs moved through. First in the morning hours across northern Iowa, and second during the late morning through evening hours from central Iowa and on toward south central and southeast Iowa. In both cases, damaging winds widely prevailed. Across northern Iowa the gust front roared out ahead of the line of convection, continuing to produce severe wind reports in areas of no storms well to the south and east. In central and southeast Iowa, widespread reports of 60 to 70 mph winds and various tree damage (from large limbs to entire trees) were received along a path from roughly Perry, IA through Ottumwa, IA. Public reported penny sized hail, as well as sapling trees snapped.", "ts_dict_index": [5559, 5560, 5561]}
+{"event_id": 1087033, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-04-26 16:00:00", "end_date_time": "2023-04-26 16:00:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Quarter size hail fell near the intersection of Van Buren Street and Highway 64 in Henderson.", "ts_dict_index": [5592, 5593, 5594]}
+{"event_id": 1087027, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-04-26 15:48:00", "end_date_time": "2023-04-26 15:48:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Dime to half dollar size hail fell and covered the ground along FM 838 just south of Overton and New London.", "ts_dict_index": [5574, 5575, 5576]}
+{"event_id": 1087028, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-04-26 15:50:00", "end_date_time": "2023-04-26 15:50:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Hail measured slightly larger than 2 inches in diameter (hen egg size) fell in the Turnertown community.", "ts_dict_index": [5568, 5569, 5570]}
+{"event_id": 1087026, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-04-26 15:45:00", "end_date_time": "2023-04-26 15:45:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Golfball size hail fell in the Selman City community.", "ts_dict_index": [5589, 5590, 5591]}
+{"event_id": 1087035, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-04-26 16:05:00", "end_date_time": "2023-04-26 16:05:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Hail up the size of baseballs fell throughout the city of Henderson. Several reports were received of windshields and skylights broken, along with damaged traffic signals with power outages.", "ts_dict_index": [5577, 5578, 5579]}
+{"event_id": 1064264, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-01-07 23:30:00", "end_date_time": "2023-01-07 23:30:00", "narrative": "An upper trough ejected east across the Central Plains on January 7th and into Iowa/Northern Missouri during the evening, inducing surface low development farther south over Southern Oklahoma which moved east into Central Arkansas by the evening. This system reinforced a cold front southeast across the Southern Plains during the afternoon, and into East Texas during the mid and late evening hours. Meanwhile, another shortwave trough rapidly traversed east from Northern Baja and merged with the southern extent of the upper trough axis over East Texas, increasing large scale forcing along and ahead of the front. Low level moisture return was already underway across East Texas and North Louisiana ahead of the front, and was sufficient enough for the development of scattered to numerous showers and thunderstorms across these areas during the evening and overnight hours. While shear ahead of the front was strong, instability was not particularly high across the area, but was adequate enough for the development of isolated strong to severe thunderstorms across portions of Lower East Texas, which moved east-southeast into Western Louisiana during the late evening hours. Damaging winds downed trees and power lines across portions of North-central Sabine Parish, with multiple reports of large hail falling as well before the storms exiting the region into Central Louisiana during the early morning hours on the 8th. Pictures of quarter size hail that fell in the Ebarb community were posted to social media.", "ts_dict_index": [5553, 5554, 5555]}
+{"event_id": 1064269, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-01-07 23:40:00", "end_date_time": "2023-01-07 23:40:00", "narrative": "An upper trough ejected east across the Central Plains on January 7th and into Iowa/Northern Missouri during the evening, inducing surface low development farther south over Southern Oklahoma which moved east into Central Arkansas by the evening. This system reinforced a cold front southeast across the Southern Plains during the afternoon, and into East Texas during the mid and late evening hours. Meanwhile, another shortwave trough rapidly traversed east from Northern Baja and merged with the southern extent of the upper trough axis over East Texas, increasing large scale forcing along and ahead of the front. Low level moisture return was already underway across East Texas and North Louisiana ahead of the front, and was sufficient enough for the development of scattered to numerous showers and thunderstorms across these areas during the evening and overnight hours. While shear ahead of the front was strong, instability was not particularly high across the area, but was adequate enough for the development of isolated strong to severe thunderstorms across portions of Lower East Texas, which moved east-southeast into Western Louisiana during the late evening hours. Damaging winds downed trees and power lines across portions of North-central Sabine Parish, with multiple reports of large hail falling as well before the storms exiting the region into Central Louisiana during the early morning hours on the 8th. Nickle size hail fell in the Noble community.", "ts_dict_index": [5556, 5557, 5558]}
+{"event_id": 1018733, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2022-05-24 16:13:00", "end_date_time": "2022-05-24 16:13:00", "narrative": "Following severe weather the previous afternoon of the 23rd, another batch of thunderstorms originating from the higher terrain of eastern New Mexico swept through the region. This complex of thunderstorms moved much more quickly than the previous evening's storms, though additional slow-moving storms also formed along a weak frontal zone over the central South Plains late Tuesday afternoon which brought torrential rainfall to a portion of the South Plains. The thunderstorms that formed above the quasi-stationary frontal zone were able to concentrate the spin along the front, which resulted in the development of several landspout type tornadoes. At one point as many as three landspouts were observed at the same time near the community of Meadow (Terry County). The landspouts moved very little, dissipated relatively quickly, and inflicted no known damage. In contrast to the limited and short-lived landspouts, the bulging cluster of storms generated widespread severe wind gusts across the central and southern South Plains. Severe wind gusts developed in the southern South Plains underneath stratiform precipitation well behind the main convective line.||High wind gusts from stratiform precipitation were measured by the Texas Tech University West Texas mesonet shown below:||69 mph at Graham (Garza County),|67 mph at Post (Garza County), and|60 mph at O'Donnell (Lynn County). An off duty NWS employee measured quarter size hail south of Wolfforth.", "ts_dict_index": [5562, 5563, 5564]}
+{"event_id": 888984, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2020-05-24 17:24:00", "end_date_time": "2020-05-24 17:32:00", "narrative": "Severe thunderstorms erupted for a second straight day across the South Plains. A weak short wave moved out of central New Mexico into West Texas during the afternoon hours which aided in convective development along a dryline. Two general areas of convection matured into severe thunderstorms: one in the south central South Plains and another across the southeastern Texas Panhandle. Multi-cellular thunderstorms developed in Hockley County but quickly moved eastward into Lubbock and Lynn Counties. These storms produced mostly one inch sized hail, but hail as big as an inch and a half was reported by a weather spotter in the southern part of the city of Lubbock (Lubbock County). As the storms matured they began to form a line and produced more inch size hail in the central Rolling Plains as well as severe wind gusts near Guthrie (King County). A few reports of damage were reported including downed power poles in Briscoe County and a demolished office trailer in Hockley County. No injuries were reported.||Late that same day after storms has moved through the Southern Texas Panhandle,  severe non-thunderstorm winds were recorded near the city of Lesley (Hall County). Severe non-thunderstorm severe wind gusts are listed below from the Texas Tech University West Texas mesonet:||65 mph at Lesley (Hall County) and 64 mph at Turkey (Hall County). A severe thunderstorm moved across Lubbock County. This thunderstorm produced severe hail on the southern side of the city of Lubbock. Numerous reports were received of hail up to golf ball size across the southern portion of Lubbock. Hail up to one and a half inches in diameter was reported by a trained weather spotter. No damage was reported.", "ts_dict_index": [5598, 5599, 5600]}
+{"event_id": 946932, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-13 15:55:00", "end_date_time": "2021-04-13 15:55:00", "narrative": "A warm front began to lift north across East Texas and North Louisiana during the afternoon of April 13th, with warm, moist, and unstable air shifting back north across these areas. Meanwhile, a weak upper level disturbance in the zonal flow aloft helped enhance scattered thunderstorm development along and north of the front across portions of East Texas. Given the adequate shear and extent of instability aloft, isolated severe thunderstorms developed and produced reports of large hail across these areas before diminishing during the evening with the loss of heating. However, another more significant shortwave trough traversed the Red River Valley of Southern Oklahoma and North Texas, as the warm front shifted farther north across East Texas to near the Louisiana/Arkansas border. Large scale forcing ahead of this trough and elevated instability aloft resulted in an increase in shower and thunderstorm development during the early morning hours of April 14th, near and ahead of an associated cold front that had begun to enter the region from the northwest. A few isolated severe thunderstorms developed over portions of Northeast Texas, Southwest Arkansas, and North Louisiana, producing instances of large hail before these storms weakened and became more numerous after daybreak, before eventually diminishing from west to east by afternoon. Quarter size hail fell several miles south of Appleby.", "ts_dict_index": [5613, 5614, 5615]}
+{"event_id": 946933, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-13 16:32:00", "end_date_time": "2021-04-13 16:32:00", "narrative": "A warm front began to lift north across East Texas and North Louisiana during the afternoon of April 13th, with warm, moist, and unstable air shifting back north across these areas. Meanwhile, a weak upper level disturbance in the zonal flow aloft helped enhance scattered thunderstorm development along and north of the front across portions of East Texas. Given the adequate shear and extent of instability aloft, isolated severe thunderstorms developed and produced reports of large hail across these areas before diminishing during the evening with the loss of heating. However, another more significant shortwave trough traversed the Red River Valley of Southern Oklahoma and North Texas, as the warm front shifted farther north across East Texas to near the Louisiana/Arkansas border. Large scale forcing ahead of this trough and elevated instability aloft resulted in an increase in shower and thunderstorm development during the early morning hours of April 14th, near and ahead of an associated cold front that had begun to enter the region from the northwest. A few isolated severe thunderstorms developed over portions of Northeast Texas, Southwest Arkansas, and North Louisiana, producing instances of large hail before these storms weakened and became more numerous after daybreak, before eventually diminishing from west to east by afternoon. Quarter size hail fell near the Shady Grove community east of Nacogdoches.", "ts_dict_index": [5607, 5608, 5609]}
+{"event_id": 946931, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-13 15:53:00", "end_date_time": "2021-04-13 15:53:00", "narrative": "A warm front began to lift north across East Texas and North Louisiana during the afternoon of April 13th, with warm, moist, and unstable air shifting back north across these areas. Meanwhile, a weak upper level disturbance in the zonal flow aloft helped enhance scattered thunderstorm development along and north of the front across portions of East Texas. Given the adequate shear and extent of instability aloft, isolated severe thunderstorms developed and produced reports of large hail across these areas before diminishing during the evening with the loss of heating. However, another more significant shortwave trough traversed the Red River Valley of Southern Oklahoma and North Texas, as the warm front shifted farther north across East Texas to near the Louisiana/Arkansas border. Large scale forcing ahead of this trough and elevated instability aloft resulted in an increase in shower and thunderstorm development during the early morning hours of April 14th, near and ahead of an associated cold front that had begun to enter the region from the northwest. A few isolated severe thunderstorms developed over portions of Northeast Texas, Southwest Arkansas, and North Louisiana, producing instances of large hail before these storms weakened and became more numerous after daybreak, before eventually diminishing from west to east by afternoon. Ping pong ball size hail fell off of Appleby Sand Road in Northeast Nacogdoches.", "ts_dict_index": [5610, 5611, 5612]}
+{"event_id": 880049, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-22 11:44:00", "end_date_time": "2020-04-22 11:44:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Quarter size hail fell in Vivian.", "ts_dict_index": [5625, 5626, 5627]}
+{"event_id": 946939, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2021-04-14 04:27:00", "end_date_time": "2021-04-14 04:27:00", "narrative": "A warm front began to lift north across East Texas and North Louisiana during the afternoon of April 13th, with warm, moist, and unstable air shifting back north across these areas. Meanwhile, a weak upper level disturbance in the zonal flow aloft helped enhance scattered thunderstorm development along and north of the front across portions of East Texas. Given the adequate shear and extent of instability aloft, isolated severe thunderstorms developed and produced reports of large hail across these areas before diminishing during the evening with the loss of heating. However, another more significant shortwave trough traversed the Red River Valley of Southern Oklahoma and North Texas, as the warm front shifted farther north across East Texas to near the Louisiana/Arkansas border. Large scale forcing ahead of this trough and elevated instability aloft resulted in an increase in shower and thunderstorm development during the early morning hours of April 14th, near and ahead of an associated cold front that had begun to enter the region from the northwest. A few isolated severe thunderstorms developed over portions of Northeast Texas, Southwest Arkansas, and North Louisiana, producing instances of large hail before these storms weakened and became more numerous after daybreak, before eventually diminishing from west to east by afternoon. Quarter size hail fell near the De Kalb Church of Christ on the east side of De Kalb.", "ts_dict_index": [5604, 5605, 5606]}
+{"event_id": 880239, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-22 14:28:00", "end_date_time": "2020-04-22 14:28:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. A picture was posted to social media of half dollar size hail that fell just south of the Douglass community.", "ts_dict_index": [5634, 5635, 5636]}
+{"event_id": 880061, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-22 17:07:00", "end_date_time": "2020-04-22 17:07:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Half dollar size hail fell in East Shreveport. Report from mPING.", "ts_dict_index": [5628, 5629, 5630]}
+{"event_id": 880241, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-22 14:28:00", "end_date_time": "2020-04-22 14:28:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Golfball size hail was reported near the Douglass community.", "ts_dict_index": [5631, 5632, 5633]}
+{"event_id": 880242, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-22 14:39:00", "end_date_time": "2020-04-22 14:39:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Golfball size hail fell several miles west of Nacogdoches.", "ts_dict_index": [5619, 5620, 5621]}
+{"event_id": 880245, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-22 14:41:00", "end_date_time": "2020-04-22 14:41:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Quarter size hail fell several miles southwest of Nacogdoches. Report from mPING.", "ts_dict_index": [5622, 5623, 5624]}
+{"event_id": 880243, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-22 14:34:00", "end_date_time": "2020-04-22 14:34:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Hen egg size hail fell at the intersection of FM 2782 and FM 225 in the Alazan community.", "ts_dict_index": [5637, 5638, 5639]}
+{"event_id": 880244, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-22 14:41:00", "end_date_time": "2020-04-22 14:41:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. At least quarter size hail fell on Old Lufkin Road.", "ts_dict_index": [5640, 5641, 5642]}
+{"event_id": 1087025, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-04-26 15:40:00", "end_date_time": "2023-04-26 15:40:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Golfball size hail fell in Arp.", "ts_dict_index": [5583, 5584, 5585]}
+{"event_id": 1114456, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-07-28 17:18:00", "end_date_time": "2023-07-28 17:20:00", "narrative": "An upper ridge was over most of the southern half of the country. A weak upper level disturbance was moving across northern Nebraska. A weak surface low pressure was across parts of south central Nebraska during the afternoon hours. Temperatures were in the mid 90s to triple digits, and dewpoints were in the upper 60s to lower 70s. Effective bulk shear values generally ranged from 30 to 45 knots, and most unstable CAPE was generally 4,000 to 6,000 J/kg. ||A storm developed and strengthened over south central Nebraska and produced 1.50 inch hail in Nuckolls County after 4 PM CDT. This storm went on to produce quarter and nickel size hail in the same county then moved south towards the Kansas border. The storm split as it was crossing the border with the northern storm remaining in Nebraska then weakening and the southern half of the storm moving into Kansas. Another storm moved into Hamilton County and produced hail up to two inches at 5:40 PM CDT. This storm moved into Clay County after 6 PM CDT and produced two inch hail along with 60 mph wind gusts. The storm continued to move south through Clay County and produced hail ranging in size from two to four inches. Finally, the storm crossed over into Fillmore County and produced golf ball sized hail at 7 PM CDT. Reports received via social media and broadcast media of hail between three and four inches in diameter in and around Saronville.", "ts_dict_index": [5643, 5644, 5645]}
+{"event_id": 1114451, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-07-28 17:15:00", "end_date_time": "2023-07-28 17:25:00", "narrative": "An upper ridge was over most of the southern half of the country. A weak upper level disturbance was moving across northern Nebraska. A weak surface low pressure was across parts of south central Nebraska during the afternoon hours. Temperatures were in the mid 90s to triple digits, and dewpoints were in the upper 60s to lower 70s. Effective bulk shear values generally ranged from 30 to 45 knots, and most unstable CAPE was generally 4,000 to 6,000 J/kg. ||A storm developed and strengthened over south central Nebraska and produced 1.50 inch hail in Nuckolls County after 4 PM CDT. This storm went on to produce quarter and nickel size hail in the same county then moved south towards the Kansas border. The storm split as it was crossing the border with the northern storm remaining in Nebraska then weakening and the southern half of the storm moving into Kansas. Another storm moved into Hamilton County and produced hail up to two inches at 5:40 PM CDT. This storm moved into Clay County after 6 PM CDT and produced two inch hail along with 60 mph wind gusts. The storm continued to move south through Clay County and produced hail ranging in size from two to four inches. Finally, the storm crossed over into Fillmore County and produced golf ball sized hail at 7 PM CDT. Hail up to the size of tennis balls was reported along and near this path.", "ts_dict_index": [5646, 5647, 5648]}
+{"event_id": 1087034, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-04-26 16:00:00", "end_date_time": "2023-04-26 16:00:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Quarter to golfball size hail fell throughout the city of Henderson.", "ts_dict_index": [5586, 5587, 5588]}
+{"event_id": 859073, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2019-11-30 10:56:00", "end_date_time": "2019-11-30 10:56:00", "narrative": "A warm front lifted north across the Ark-La-Tex area during the afternoon and evening hours of November 29th, returning a warm and humid air mass back north into the region. A large closed upper low pressure system drifted east over the Central Plains during the daytime hours of November 30th, with the attendant upper trough shifting east across the Southern Plains and into the Mississippi Valley. Very strong wind shear spread east ahead of this trough, which reinforced a dryline east across the Ark-La-Tex throughout the day. Temperatures climbed into the mid 70s to near 80 degrees across the warm sector of East Texas and North Louisiana, which resulted in adequate instability to generate a narrow line of showers and thunderstorms along the dryline. The storms during the morning remained slightly elevated, with isolated severe thunderstorms producing large hail across portions of Northeast Texas. As the day progressed, the storms became more surface based, with additional scattered strong to severe thunderstorms developing just ahead of this line as well across portions of Deep East Texas and Northcentral Louisiana. These storms weakened during the late afternoon hours with the loss of instability, with the dryline exiting the area during the early evening. Pictures of quarter to half dollar size hail that fell in Maud were posted to Facebook.", "ts_dict_index": [5655, 5656, 5657]}
+{"event_id": 1114447, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-07-28 17:03:00", "end_date_time": "2023-07-28 17:03:00", "narrative": "An upper ridge was over most of the southern half of the country. A weak upper level disturbance was moving across northern Nebraska. A weak surface low pressure was across parts of south central Nebraska during the afternoon hours. Temperatures were in the mid 90s to triple digits, and dewpoints were in the upper 60s to lower 70s. Effective bulk shear values generally ranged from 30 to 45 knots, and most unstable CAPE was generally 4,000 to 6,000 J/kg. ||A storm developed and strengthened over south central Nebraska and produced 1.50 inch hail in Nuckolls County after 4 PM CDT. This storm went on to produce quarter and nickel size hail in the same county then moved south towards the Kansas border. The storm split as it was crossing the border with the northern storm remaining in Nebraska then weakening and the southern half of the storm moving into Kansas. Another storm moved into Hamilton County and produced hail up to two inches at 5:40 PM CDT. This storm moved into Clay County after 6 PM CDT and produced two inch hail along with 60 mph wind gusts. The storm continued to move south through Clay County and produced hail ranging in size from two to four inches. Finally, the storm crossed over into Fillmore County and produced golf ball sized hail at 7 PM CDT. Hail up to two inches in diameter was accompanied by wind gusts estimated to be near 60 MPH.", "ts_dict_index": [5649, 5650, 5651]}
+{"event_id": 884317, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2020-05-20 15:26:00", "end_date_time": "2020-05-20 15:26:00", "narrative": "A warm front lifting northeast into portions of East Texas and Westcentral Louisiana near or just east of the Sabine River during the morning hours of May 20th became stationary by midday, as a weak upper level disturbance rounded a closed upper low pressure system over the Tennessee Valley. Convergence and moisture pooling near this surface boundary and weak large scale forcing aloft contributed to areas of showers and thunderstorms developing from late morning through much of the afternoon near and just south of the front, as they continued to move southeast repeatedly over the same areas of Westcentral Louisiana. This environment resulted in efficient rainfall producers, with a narrow axis of 2-6 inch rains falling over Eastern Sabine, Southeast Desoto, and Western Natchitoches Parishes, with isolated higher amounts exceeding 11 inches along the Sabine/Natchitoches Parish line. Flash flooding was observed across these areas, before the rains diminished by late afternoon/early evening. In addition, some diurnal heating occurred within this area, contributing to moderate instability near the front as well, with isolated severe thunderstorms producing large hail over portions of Eastern Sabine and Western Natchitoches Parishes during the mid-afternoon hours. Golf ball size hail fell along Highway 6 near the Fort Jesup community.", "ts_dict_index": [5652, 5653, 5654]}
+{"event_id": 946938, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-04-14 00:28:00", "end_date_time": "2021-04-14 00:28:00", "narrative": "A warm front began to lift north across East Texas and North Louisiana during the afternoon of April 13th, with warm, moist, and unstable air shifting back north across these areas. Meanwhile, a weak upper level disturbance in the zonal flow aloft helped enhance scattered thunderstorm development along and north of the front across portions of East Texas. Given the adequate shear and extent of instability aloft, isolated severe thunderstorms developed and produced reports of large hail across these areas before diminishing during the evening with the loss of heating. However, another more significant shortwave trough traversed the Red River Valley of Southern Oklahoma and North Texas, as the warm front shifted farther north across East Texas to near the Louisiana/Arkansas border. Large scale forcing ahead of this trough and elevated instability aloft resulted in an increase in shower and thunderstorm development during the early morning hours of April 14th, near and ahead of an associated cold front that had begun to enter the region from the northwest. A few isolated severe thunderstorms developed over portions of Northeast Texas, Southwest Arkansas, and North Louisiana, producing instances of large hail before these storms weakened and became more numerous after daybreak, before eventually diminishing from west to east by afternoon. Quarter size hail fell several miles south-southwest of Winona.", "ts_dict_index": [5601, 5602, 5603]}
+{"event_id": 859074, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2019-11-30 11:03:00", "end_date_time": "2019-11-30 11:03:00", "narrative": "A warm front lifted north across the Ark-La-Tex area during the afternoon and evening hours of November 29th, returning a warm and humid air mass back north into the region. A large closed upper low pressure system drifted east over the Central Plains during the daytime hours of November 30th, with the attendant upper trough shifting east across the Southern Plains and into the Mississippi Valley. Very strong wind shear spread east ahead of this trough, which reinforced a dryline east across the Ark-La-Tex throughout the day. Temperatures climbed into the mid 70s to near 80 degrees across the warm sector of East Texas and North Louisiana, which resulted in adequate instability to generate a narrow line of showers and thunderstorms along the dryline. The storms during the morning remained slightly elevated, with isolated severe thunderstorms producing large hail across portions of Northeast Texas. As the day progressed, the storms became more surface based, with additional scattered strong to severe thunderstorms developing just ahead of this line as well across portions of Deep East Texas and Northcentral Louisiana. These storms weakened during the late afternoon hours with the loss of instability, with the dryline exiting the area during the early evening. Penny size hail fell near Redwater. Report via MPING.", "ts_dict_index": [5658, 5659, 5660]}
+{"event_id": 971363, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 12:58:00", "end_date_time": "2021-07-09 12:58:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Report via mping app.", "ts_dict_index": [5670, 5671, 5672]}
+{"event_id": 971374, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:03:00", "end_date_time": "2021-07-09 13:03:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Baseball sized hail report relayed via WHO TV.", "ts_dict_index": [5676, 5677, 5678]}
+{"event_id": 971380, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:15:00", "end_date_time": "2021-07-09 13:15:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Most hail at 31st and Ingersoll Avenue was dime to nickel sized, however up to 1.5 inch hail fell at time of report.", "ts_dict_index": [5679, 5680, 5681]}
+{"event_id": 971381, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:15:00", "end_date_time": "2021-07-09 13:15:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Picture via social media of 3.25 inch hail in Beaverdale. Time estimated via radar.", "ts_dict_index": [5682, 5683, 5684]}
+{"event_id": 971382, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:16:00", "end_date_time": "2021-07-09 13:16:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Half dollar sized hail at the state capitol.", "ts_dict_index": [5661, 5662, 5663]}
+{"event_id": 971367, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:01:00", "end_date_time": "2021-07-09 13:01:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. ", "ts_dict_index": [5664, 5665, 5666]}
+{"event_id": 971379, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:14:00", "end_date_time": "2021-07-09 13:14:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Hail sized ranged from three quarters of an inch to as large as ping pong ball sized.", "ts_dict_index": [5685, 5686, 5687]}
+{"event_id": 971384, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:23:00", "end_date_time": "2021-07-09 13:23:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Hail was ongoing at time of report.", "ts_dict_index": [5691, 5692, 5693]}
+{"event_id": 971366, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:01:00", "end_date_time": "2021-07-09 13:01:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Golf ball to egg sized hail at the NWS office in Johnston. Minor damage to vehicles.", "ts_dict_index": [5667, 5668, 5669]}
+{"event_id": 971376, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:06:00", "end_date_time": "2021-07-09 13:06:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Largest hail was golf ball sized and fell around 206pm local time.", "ts_dict_index": [5673, 5674, 5675]}
+{"event_id": 971377, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:08:00", "end_date_time": "2021-07-09 13:08:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. NWS Employee reports half dollar to golf ball sized hail.", "ts_dict_index": [5694, 5695, 5696]}
+{"event_id": 871209, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-03-04 06:50:00", "end_date_time": "2020-03-04 06:50:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across East Texas during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Given the still saturated grounds in wake of much above normal rains that had fallen since mid-January, the locally heavy rainfall produced isolated reports of flash flooding as well, before rain rates diminished during the afternoon. Quarter size hail was reported along Highway 259 between Henderson and Mount Enterprise.", "ts_dict_index": [5616, 5617, 5618]}
+{"event_id": 1085005, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-05 20:20:00", "end_date_time": "2023-04-05 20:20:00", "narrative": "An upper low pressure system over the Four Corners Region ejected northeast through the Southern Rockies into the Central Plains by the afternoon of April 5th, which reinforced a cold front southeast into East Texas, Southwest Arkansas, and North Louisiana before stalling out late in the day. Large scale ascent increased along and ahead of the front and the ejecting upper low, which had tapped into a warm and moderately unstable air mass that had pooled north from the Gulf of Mexico ahead of the front. This resulted in numerous shower and thunderstorm development during the morning around and after daybreak over Northeast Texas and Southwest Arkansas, which eventually moved into portions of extreme Northwest Louisiana by late morning/early afternoon. Some of these storms became severe, with damaging winds and large hail observed. While these storms eventually weakened by mid-afternoon, additional redevelopment occurred along the slowing front farther south of I-20 in East Texas and North Louisiana by late afternoon and early evening as they tapped stronger instability, with isolated severe thunderstorms producing large hail affecting portions of Western Caddo Parish before weakening. Quarter size hail fell in Greenwood.", "ts_dict_index": [5718, 5719, 5720]}
+{"event_id": 1085002, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-05 11:29:00", "end_date_time": "2023-04-05 11:29:00", "narrative": "An upper low pressure system over the Four Corners Region ejected northeast through the Southern Rockies into the Central Plains by the afternoon of April 5th, which reinforced a cold front southeast into East Texas, Southwest Arkansas, and North Louisiana before stalling out late in the day. Large scale ascent increased along and ahead of the front and the ejecting upper low, which had tapped into a warm and moderately unstable air mass that had pooled north from the Gulf of Mexico ahead of the front. This resulted in numerous shower and thunderstorm development during the morning around and after daybreak over Northeast Texas and Southwest Arkansas, which eventually moved into portions of extreme Northwest Louisiana by late morning/early afternoon. Some of these storms became severe, with damaging winds and large hail observed. While these storms eventually weakened by mid-afternoon, additional redevelopment occurred along the slowing front farther south of I-20 in East Texas and North Louisiana by late afternoon and early evening as they tapped stronger instability, with isolated severe thunderstorms producing large hail affecting portions of Western Caddo Parish before weakening. Quarter size hail fell along Highway 71 between Elm Grove and Ninock.", "ts_dict_index": [5721, 5722, 5723]}
+{"event_id": 823608, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-20 15:08:00", "end_date_time": "2019-05-20 15:08:00", "narrative": "The afternoon of the 20th was the beginning of an extended period of several weeks of severe weather for the South Plains and Rolling Plains of West Texas. A high risk of severe weather was issued by the Storm Prediction Center in the morning for the afternoon of the 20th. Southwest flow aloft with an embedded mid level jet streak contributed to an ample amount of lift across the region. Numerous thunderstorms developed east of the dryline which was located west of the Interstate 27/US Highway 87 corridor. Very strong instability developed out ahead of the dryline in the warm sector along with favorable shear for supercell and tornado development. Although no long track tornadoes were observed, there were several weak tornadoes that developed. The most destructive storm of the afternoon was a supercell that moved through parts of the city of Lubbock (Lubbock County). A widespread swath of wind gusts in excess of 60 mph and extensive wind damage was seen from southern Lubbock County up through the south side of Lubbock and into Idalou. Due to the fast moving nature of the thunderstorms, this damage occurred over a period of only nine minutes from 1504 through 1513 CST. Most damage reports consisted of downed trees and power lines. Hail up to golf ball size was reported near the intersection of 114th Street and Quaker Avenue in the city of Lubbock. This hail report was among the widespread swath of thunderstorm wind damage as the same time.", "ts_dict_index": [5703, 5704, 5705]}
+{"event_id": 1085003, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-05 11:30:00", "end_date_time": "2023-04-05 11:30:00", "narrative": "An upper low pressure system over the Four Corners Region ejected northeast through the Southern Rockies into the Central Plains by the afternoon of April 5th, which reinforced a cold front southeast into East Texas, Southwest Arkansas, and North Louisiana before stalling out late in the day. Large scale ascent increased along and ahead of the front and the ejecting upper low, which had tapped into a warm and moderately unstable air mass that had pooled north from the Gulf of Mexico ahead of the front. This resulted in numerous shower and thunderstorm development during the morning around and after daybreak over Northeast Texas and Southwest Arkansas, which eventually moved into portions of extreme Northwest Louisiana by late morning/early afternoon. Some of these storms became severe, with damaging winds and large hail observed. While these storms eventually weakened by mid-afternoon, additional redevelopment occurred along the slowing front farther south of I-20 in East Texas and North Louisiana by late afternoon and early evening as they tapped stronger instability, with isolated severe thunderstorms producing large hail affecting portions of Western Caddo Parish before weakening. Quarter size hail fell just east of the Atkins community in Southern Bossier Parish.", "ts_dict_index": [5715, 5716, 5717]}
+{"event_id": 806406, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-03-25 02:09:00", "end_date_time": "2019-03-25 02:09:00", "narrative": "Warm and moist air began to return north across the Ark-La-Tex during the daytime hours on March 24th, ahead of an upper level shortwave trough that traversed east across Southern Oklahoma and North Texas. This resulted in scattered showers and thunderstorms developing during the evening over Southeast Oklahoma and portions of North Texas, where better instability developed earlier in the day in response to daytime heating. Despite the marginal instability near the surface, ample shear and forcing were noted aloft ahead of this approaching disturbance and associated cold front, where several supercell thunderstorms developed over these areas during the evening. Additional scattered severe thunderstorms spread east southeast into Northeast Texas and Southern McCurtain County Oklahoma during the late evening hours. Large hail reports were received across portions of these areas, before the storms organized into a cluster and surged southeast across portions of East Texas and Northwest Louisiana during the early morning hours on the 25th. Damaging winds became prevalent along this line of storms, although occasional reports of large hail were also received, before the storms weakened after 330 am once instability diminished even further. A home security camera captured images of near ping pong ball size hail that fell in North Bossier City.", "ts_dict_index": [5700, 5701, 5702]}
+{"event_id": 806398, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-03-25 00:10:00", "end_date_time": "2019-03-25 00:10:00", "narrative": "Warm and moist air began to return north across the Ark-La-Tex during the daytime hours on March 24th, ahead of an upper level shortwave trough that traversed east across Southern Oklahoma and North Texas. This resulted in scattered showers and thunderstorms developing during the evening over Southeast Oklahoma and portions of North Texas, where better instability developed earlier in the day in response to daytime heating. Despite the marginal instability near the surface, ample shear and forcing were noted aloft ahead of this approaching disturbance and associated cold front, where several supercell thunderstorms developed over these areas during the evening. As a result, some of these storms produced large hail initially over Northern McCurtain County Oklahoma, and well as across portions of the Dallas-Fort Worth Metroplex, before the scattered severe thunderstorms spread east southeast into Northeast Texas and Southern McCurtain County Oklahoma during the late evening through the early morning hours on the 25th. Additional large hail reports were received across portions of these areas, before the storms organized into a cluster and surged southeast across portions of East Texas and Northwest Louisiana. A picture of half-dollar size hail that fell in Broken Bow was posted to social media.", "ts_dict_index": [5712, 5713, 5714]}
+{"event_id": 806397, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-03-25 00:02:00", "end_date_time": "2019-03-25 00:02:00", "narrative": "Warm and moist air began to return north across the Ark-La-Tex during the daytime hours on March 24th, ahead of an upper level shortwave trough that traversed east across Southern Oklahoma and North Texas. This resulted in scattered showers and thunderstorms developing during the evening over Southeast Oklahoma and portions of North Texas, where better instability developed earlier in the day in response to daytime heating. Despite the marginal instability near the surface, ample shear and forcing were noted aloft ahead of this approaching disturbance and associated cold front, where several supercell thunderstorms developed over these areas during the evening. As a result, some of these storms produced large hail initially over Northern McCurtain County Oklahoma, and well as across portions of the Dallas-Fort Worth Metroplex, before the scattered severe thunderstorms spread east southeast into Northeast Texas and Southern McCurtain County Oklahoma during the late evening through the early morning hours on the 25th. Additional large hail reports were received across portions of these areas, before the storms organized into a cluster and surged southeast across portions of East Texas and Northwest Louisiana. The Holly Creek Fire Department reported quarter size hail in the Holly Creek community.", "ts_dict_index": [5709, 5710, 5711]}
+{"event_id": 806396, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-03-24 18:00:00", "end_date_time": "2019-03-24 18:00:00", "narrative": "Warm and moist air began to return north across the Ark-La-Tex during the daytime hours on March 24th, ahead of an upper level shortwave trough that traversed east across Southern Oklahoma and North Texas. This resulted in scattered showers and thunderstorms developing during the evening over Southeast Oklahoma and portions of North Texas, where better instability developed earlier in the day in response to daytime heating. Despite the marginal instability near the surface, ample shear and forcing were noted aloft ahead of this approaching disturbance and associated cold front, where several supercell thunderstorms developed over these areas during the evening. As a result, some of these storms produced large hail initially over Northern McCurtain County Oklahoma, and well as across portions of the Dallas-Fort Worth Metroplex, before the scattered severe thunderstorms spread east southeast into Northeast Texas and Southern McCurtain County Oklahoma during the late evening through the early morning hours on the 25th. Additional large hail reports were received across portions of these areas, before the storms organized into a cluster and surged southeast across portions of East Texas and Northwest Louisiana. Pictures of golfball to hen egg size hail was submitted to the National Weather Service near the Mountain Country Store in Smithville.", "ts_dict_index": [5706, 5707, 5708]}
+{"event_id": 971383, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 13:21:00", "end_date_time": "2021-07-09 13:21:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Golf balled sized hail at the state capitol.", "ts_dict_index": [5688, 5689, 5690]}
+{"event_id": 1085648, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2023-04-20 18:25:00", "end_date_time": "2023-04-20 18:25:00", "narrative": "An upper level low pressure system shifted east from Montana east into the Dakotas on April 20th, with the attendant trough extending southward through the Rockies before ejecting east through the Central and Southern Plains during the afternoon and evening. A strong southerly low level flow ahead of this trough ushered very warm and humid air back north into the Four State Region on the 19th-20th, which primed the area with moderate instability ahead of an associated cold front that entered the region during the afternoon. Large scale forcing increased by mid and late afternoon through the evening along and ahead of the front and upper trough within the warm, moist, and unstable sector, enhancing scattered to numerous shower and thunderstorm development across portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple reports of damaging winds and large hail were observed, with an isolated tornado also touching down in Midtown Tyler in Smith County. Localized flash flooding was also reported on the Texas side of Texarkana before the storms weakened during the evening with the loss of heating and reduced instability. Quarter size hail fell several miles east-northeast of Redwater.", "ts_dict_index": [5733, 5734, 5735]}
+{"event_id": 1085646, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2023-04-20 18:20:00", "end_date_time": "2023-04-20 18:20:00", "narrative": "An upper level low pressure system shifted east from Montana east into the Dakotas on April 20th, with the attendant trough extending southward through the Rockies before ejecting east through the Central and Southern Plains during the afternoon and evening. A strong southerly low level flow ahead of this trough ushered very warm and humid air back north into the Four State Region on the 19th-20th, which primed the area with moderate instability ahead of an associated cold front that entered the region during the afternoon. Large scale forcing increased by mid and late afternoon through the evening along and ahead of the front and upper trough within the warm, moist, and unstable sector, enhancing scattered to numerous shower and thunderstorm development across portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple reports of damaging winds and large hail were observed, with an isolated tornado also touching down in Midtown Tyler in Smith County. Localized flash flooding was also reported on the Texas side of Texarkana before the storms weakened during the evening with the loss of heating and reduced instability. Penny size hail fell just southeast of Leary. Report from m-PING.", "ts_dict_index": [5736, 5737, 5738]}
+{"event_id": 994162, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2022-01-19 18:31:00", "end_date_time": "2022-01-19 18:31:00", "narrative": "A strong southwesterly low level jet, which developed ahead of an area of low pressure along a cold front over Southern Oklahoma, quickly resulted in the transport of low level moisture north-northeast into East Texas, Southwest Arkansas, and North Louisiana, ahead of a shortwave trough that traversed the Red River Valley into Southern Arkansas and North Louisiana during the afternoon of January 19th. This cold front was reinforced south into Northeast Texas and Southwest Arkansas during the afternoon, with breaks in the cloud cover ahead of the front resulting in some destabilization near the surface. Mid level lapse rates steepened in the expanding warm sector ahead of the approaching shortwave trough, with increased large scale forcing resulting in expanding coverage of showers and thunderstorms. Some of these storms became severe across portions of East Texas, with reports of large hail over Gregg and Harrison Counties. Hail as large as tennis balls fell across portions of Marshall in Harrison County, before the storms weakened considerably as they entered extreme Northwest Louisiana during the late afternoon and early evening. Quarter size hail fell just north of the Angelina/Nacogdoches County line on Highway 59.", "ts_dict_index": [5739, 5740, 5741]}
+{"event_id": 948494, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-05-09 15:25:00", "end_date_time": "2021-05-09 15:25:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. Nickel size hail fell on Highway 21 and West Loop 224.", "ts_dict_index": [5727, 5728, 5729]}
+{"event_id": 1113931, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-07-30 07:08:00", "end_date_time": "2023-07-30 07:08:00", "narrative": "An upper level ridge extended from the Desert Southwest and south Texas northward to Nebraska and Wyoming. During the early to mid-morning hours, the temperature was in the mid to upper 60s and the dewpoint was also in the mid to upper 60s across south central Nebraska. In the early evening hours, the temperature was in the 80s and the dewpoint was in the mid 60s to lower 70s. There was subtle low to mid-level warm air advection/isentropic ascent across portions of eastern Nebraska during the morning hours. During the early evening hours, the effective wind shear was generally 40 to 50 knots and the most unstable CAPE was 3,000 to 5,000 J/kg. Mid-level lapse rates were generally between 7 to 8 degrees C/km. ||Storms developed and moved across south central Nebraska during the morning hours. One storm moved into Clay County and produced one inch hail just after 8 AM CDT. This storm weakened and moved out of the area later in the morning. Storms redeveloped across south central Nebraska during the afternoon hours. One storm strengthened and moved into Thayer County and produced one inch hail just after 7 PM CDT. This storm then moved southward into Kansas. ", "ts_dict_index": [5724, 5725, 5726]}
+{"event_id": 948462, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2021-05-09 17:45:00", "end_date_time": "2021-05-09 17:45:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. Nickel size hail fell in the Florien community.", "ts_dict_index": [5730, 5731, 5732]}
+{"event_id": 1060604, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2022-11-29 15:57:00", "end_date_time": "2022-11-29 15:57:00", "narrative": "A large upper trough progressed east out of the Rockies and into the Plains during the afternoon and evening of November 29th, which reinforced a cold front southeast into the Ozarks and portions of the Southern Plains. Meanwhile, a dryline developed over West Texas ahead of the trough and front, and rapidly mixed east into East Texas and Southeast Oklahoma during the afternoon. Very warm and humid air quickly spread north with the strong low level southerly flow throughout the day on the 29th, resulting in moderately unstable conditions developing within a strongly sheared environment ahead of the approaching dryline and upper trough. Isolated strong to severe thunderstorms were able to develop near the dryline over portions of Deep East Texas by mid to late afternoon, which eventually spread across portions of North-Central Louisiana during the late afternoon and evening while becoming more numerous. Instances of damaging winds which downed trees as well as large hail occurred with these storms, with an isolated strong tornado spawning over Southeast Caldwell Parish before moving into Eastern Louisiana by late evening. Nickel to quarter size hail fell just north of Many.", "ts_dict_index": [5745, 5746, 5747]}
+{"event_id": 1060602, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2022-11-29 15:39:00", "end_date_time": "2022-11-29 15:39:00", "narrative": "A large upper trough progressed east out of the Rockies and into the Plains during the afternoon and evening of November 29th, which reinforced a cold front southeast into the Ozarks and portions of the Southern Plains. Meanwhile, a dryline developed over West Texas ahead of the trough and front, and rapidly mixed east into East Texas and Southeast Oklahoma during the afternoon. Very warm and humid air quickly spread north with the strong low level southerly flow throughout the day on the 29th, resulting in moderately unstable conditions developing within a strongly sheared environment ahead of the approaching dryline and upper trough. Isolated strong to severe thunderstorms were able to develop near the dryline over portions of Deep East Texas by mid to late afternoon, which eventually spread across portions of North-Central Louisiana during the late afternoon and evening while becoming more numerous. Instances of damaging winds which downed trees as well as large hail occurred with these storms, with an isolated strong tornado spawning over Southeast Caldwell Parish before moving into Eastern Louisiana by late evening. Nickel to quarter size hail fell southwest of Zwolle along Toledo Bend Reservoir.", "ts_dict_index": [5742, 5743, 5744]}
+{"event_id": 1060603, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2022-11-29 15:50:00", "end_date_time": "2022-11-29 15:50:00", "narrative": "A large upper trough progressed east out of the Rockies and into the Plains during the afternoon and evening of November 29th, which reinforced a cold front southeast into the Ozarks and portions of the Southern Plains. Meanwhile, a dryline developed over West Texas ahead of the trough and front, and rapidly mixed east into East Texas and Southeast Oklahoma during the afternoon. Very warm and humid air quickly spread north with the strong low level southerly flow throughout the day on the 29th, resulting in moderately unstable conditions developing within a strongly sheared environment ahead of the approaching dryline and upper trough. Isolated strong to severe thunderstorms were able to develop near the dryline over portions of Deep East Texas by mid to late afternoon, which eventually spread across portions of North-Central Louisiana during the late afternoon and evening while becoming more numerous. Instances of damaging winds which downed trees as well as large hail occurred with these storms, with an isolated strong tornado spawning over Southeast Caldwell Parish before moving into Eastern Louisiana by late evening. A photo was posted to social media of ping pong ball size hail that fell east of Zwolle along Highway 120.", "ts_dict_index": [5748, 5749, 5750]}
+{"event_id": 806408, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-03-25 02:13:00", "end_date_time": "2019-03-25 02:13:00", "narrative": "Warm and moist air began to return north across the Ark-La-Tex during the daytime hours on March 24th, ahead of an upper level shortwave trough that traversed east across Southern Oklahoma and North Texas. This resulted in scattered showers and thunderstorms developing during the evening over Southeast Oklahoma and portions of North Texas, where better instability developed earlier in the day in response to daytime heating. Despite the marginal instability near the surface, ample shear and forcing were noted aloft ahead of this approaching disturbance and associated cold front, where several supercell thunderstorms developed over these areas during the evening. Additional scattered severe thunderstorms spread east southeast into Northeast Texas and Southern McCurtain County Oklahoma during the late evening hours. Large hail reports were received across portions of these areas, before the storms organized into a cluster and surged southeast across portions of East Texas and Northwest Louisiana during the early morning hours on the 25th. Damaging winds became prevalent along this line of storms, although occasional reports of large hail were also received, before the storms weakened after 330 am once instability diminished even further. Nickel size hail fell near the intersection of Kings Highway and Mansfield Road.", "ts_dict_index": [5697, 5698, 5699]}
+{"event_id": 1032800, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2022-06-09 22:32:00", "end_date_time": "2022-06-09 22:32:00", "narrative": "Although isolated strong thunderstorms also affected parts of Valley, Sherman, Dawson and Gosper counties within South Central Nebraska on this Thursday evening, the only verified severe storm clipped portions of Furnas County, with golf ball size hail reported in Holbrook. ||Upper level flow across the Central Plains was northwesterly, set up between a broad trough over the eastern CONUS and a ridge axis extending from the Desert Southwest northward into the Northern Rockies. A shortwave disturbance embedded in this northwesterly flow sparked off thunderstorms during the early evening hours over the Sandhills of western Nebraska. These storms developed along an inverted surface trough extending northward from low pressure set up over eastern Colorado. Through the evening and overnight hours, this activity pushed south-southeast, generally following an axis of higher instability. Mixed-layer CAPE values of 1000-2000 J/kg stretched northward into far western portions of the coverage area, while most-unstable/elevated CAPE values exceeded 2000 J/kg. Deep layer shear was not lacking, with 0-6 km values between 50-60 knots. ", "ts_dict_index": [5754, 5755, 5756]}
+{"event_id": 1098453, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2023-06-23 17:07:00", "end_date_time": "2023-06-23 17:42:00", "narrative": "Strong daytime heating and good moisture levels proved sufficient for scattered thunderstorm development up and down much of the High Plains on the afternoon and evening of the 23rd. In addition, a storm system emerging from the northern Rockies provided moderate to strong vertical wind shear over this same corridor, which promoted storm organization. Several of the thunderstorms gained strong mid-level rotation. These supercell thunderstorms generated very large hail and torrential downpours as they tracked eastward through the evening hours. One storm took aim at the south side of Lubbock (Lubbock County), producing golf ball to baseball size hail, and even larger in spots. The giant stones were widely spaced, but inflicted property damage where they impacted objects like cars and buildings.||High wind reports from the Texas Tech University West Texas mesonet site are listed below:||67 mph at Paducah (Cottle County),|58 mph at Hackberry (Cottle County), and|58 mph at Childress (Childress County).||Maximum wind gusts from area ASOS stations are listed below:||59 mph at Childress Municipal Airport (Childress County). A large swath of giant hail occurred over an extensive portion of the city of Lubbock causing widespread damage to roofs and vehicles. The largest hailstone observed was 4.50 inches in diameter.", "ts_dict_index": [5760, 5761, 5762]}
+{"event_id": 1010142, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-04-05 00:28:00", "end_date_time": "2022-04-05 00:28:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited East Texas shortly after 1 am on the 5th. Penny size hail fell in Southwest Tyler. Report from mPING.", "ts_dict_index": [5775, 5776, 5777]}
+{"event_id": 1098455, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2023-06-23 18:12:00", "end_date_time": "2023-06-23 18:12:00", "narrative": "Strong daytime heating and good moisture levels proved sufficient for scattered thunderstorm development up and down much of the High Plains on the afternoon and evening of the 23rd. In addition, a storm system emerging from the northern Rockies provided moderate to strong vertical wind shear over this same corridor, which promoted storm organization. Several of the thunderstorms gained strong mid-level rotation. These supercell thunderstorms generated very large hail and torrential downpours as they tracked eastward through the evening hours. One storm took aim at the south side of Lubbock (Lubbock County), producing golf ball to baseball size hail, and even larger in spots. The giant stones were widely spaced, but inflicted property damage where they impacted objects like cars and buildings.||High wind reports from the Texas Tech University West Texas mesonet site are listed below:||67 mph at Paducah (Cottle County),|58 mph at Hackberry (Cottle County), and|58 mph at Childress (Childress County).||Maximum wind gusts from area ASOS stations are listed below:||59 mph at Childress Municipal Airport (Childress County). A report was received of golf ball size hail just south of Slaton.", "ts_dict_index": [5757, 5758, 5759]}
+{"event_id": 1087265, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-04-26 18:10:00", "end_date_time": "2023-04-26 18:10:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with multiple reports of large hail observed across Sabine Parish before diminishing after midnight. Dime to quarter size hail covered the ground in Converse.", "ts_dict_index": [5787, 5788, 5789]}
+{"event_id": 1010203, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-04-04 21:30:00", "end_date_time": "2022-04-04 21:30:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas and Southeast Oklahoma during the late evening hours of the 4th. Given the extent of elevated instability and the strong southerly low level jet in place across Southeast Oklahoma, these storms became severe as they spread east across McCurtain County, resulting in multiple reports of hail as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited Southeast Oklahoma by midnight that night. Quarter size hail fell in the Garvin community.", "ts_dict_index": [5766, 5767, 5768]}
+{"event_id": 1010205, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-04-04 21:40:00", "end_date_time": "2022-04-04 21:40:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas and Southeast Oklahoma during the late evening hours of the 4th. Given the extent of elevated instability and the strong southerly low level jet in place across Southeast Oklahoma, these storms became severe as they spread east across McCurtain County, resulting in multiple reports of hail as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited Southeast Oklahoma by midnight that night. Quarter size hail fell in Idabel.", "ts_dict_index": [5769, 5770, 5771]}
+{"event_id": 1010204, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-04-04 21:54:00", "end_date_time": "2022-04-04 21:54:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas and Southeast Oklahoma during the late evening hours of the 4th. Given the extent of elevated instability and the strong southerly low level jet in place across Southeast Oklahoma, these storms became severe as they spread east across McCurtain County, resulting in multiple reports of hail as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited Southeast Oklahoma by midnight that night. Nickel size hail fell in the Haworth community.", "ts_dict_index": [5772, 5773, 5774]}
+{"event_id": 1087268, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-04-26 18:18:00", "end_date_time": "2023-04-26 18:18:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with multiple reports of large hail observed across Sabine Parish before diminishing after midnight. Quarter size hail fell in Zwolle.", "ts_dict_index": [5796, 5797, 5798]}
+{"event_id": 1010202, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-04-04 21:26:00", "end_date_time": "2022-04-04 21:26:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas and Southeast Oklahoma during the late evening hours of the 4th. Given the extent of elevated instability and the strong southerly low level jet in place across Southeast Oklahoma, these storms became severe as they spread east across McCurtain County, resulting in multiple reports of hail as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited Southeast Oklahoma by midnight that night. Nickel size hail fell a couple of miles south of Garvin.", "ts_dict_index": [5763, 5764, 5765]}
+{"event_id": 1087266, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-04-26 18:10:00", "end_date_time": "2023-04-26 18:10:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with multiple reports of large hail observed across Sabine Parish before diminishing after midnight. Half dollar size hail covered the ground in Noble.", "ts_dict_index": [5793, 5794, 5795]}
+{"event_id": 1087260, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-04-26 18:05:00", "end_date_time": "2023-04-26 18:05:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with multiple reports of large hail observed across Sabine Parish before diminishing after midnight. Quarter size hail fell between Noble and Converse.", "ts_dict_index": [5790, 5791, 5792]}
+{"event_id": 1087271, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-04-26 18:20:00", "end_date_time": "2023-04-26 18:20:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with multiple reports of large hail observed across Sabine Parish before diminishing after midnight. Ping pong ball size hail covered the ground several miles northeast of Zwolle.", "ts_dict_index": [5778, 5779, 5780]}
+{"event_id": 1087257, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-04-26 17:55:00", "end_date_time": "2023-04-26 17:55:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with multiple reports of large hail observed across Sabine Parish before diminishing after midnight. Pictures were submitted to social media of baseball size hail that fell near Highway 191 along Toledo Bend Reservoir west of Noble and Converse. Multiple vehicles were damaged from the large hail.", "ts_dict_index": [5784, 5785, 5786]}
+{"event_id": 851260, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-10-06 17:09:00", "end_date_time": "2019-10-06 17:09:00", "narrative": "A strong upper level trough of low pressure over the Central Plains shifted east into the Mississippi Valley during the afternoon and evening hours on October 6th, which reinforced a strong cold front southeast across Oklahoma and Western Arkansas. This resulted in upper level ridging to gradually begin to retreat east and weaken over the Southeastern U.S., but not until afternoon temperatures again climbed back well above normal into the lower 90s across Southeast Oklahoma and Southwest Arkansas. Increasing gulf moisture was ushered north ahead of the front with the southerly winds, which allowed for a moderately unstable air mass to develop ahead of the approaching front. Large scale forcing along the front and ahead of the approaching upper trough resulted in scattered to numerous showers and thunderstorms developing over Southeast Oklahoma and Western Arkansas, some of which became severe over McCurtain County Oklahoma. These storms produced large hail and damaging winds during the late afternoon and early evening hours before weakening during the mid and late evening with the loss of heating and reduced instability. Quarter size hail was reported in the Mount Herman community.", "ts_dict_index": [5751, 5752, 5753]}
+{"event_id": 832637, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2019-06-29 08:05:00", "end_date_time": "2019-06-29 08:05:00", "narrative": "An upper level trough over Northern Mississippi drifted west into Southern Arkansas, Northern Louisiana, and extreme Northeast Texas during June 28th, which helped to ignite scattered showers and thunderstorms over Southcentral Arkansas and Northcentral Louisiana during the afternoon, evening, through the early morning hours on the 29th with the aid of available heating and ample low level moisture. While this resulted in a brief period of isolated strong to severe thunderstorms during the mid and late afternoon hours on the 28th across portions of Southcentral Arkansas and Northcentral Louisiana, these storms diminished during the evening but left behind residual outflow boundaries which ignited additional isolated to scattered showers and thunderstorms during the morning hours of June 29th across portions of Southwest Arkansas, Northwest Louisiana, and extreme Northeast Texas. A couple of isolated thunderstorms briefly became severe over Eastern Bowie County Texas, producing quarter size hail in the Leary community and just northeast of Maud before diminishing. Nickel to quarter size hail fell off of Highway 67 between Redwater and Maud.", "ts_dict_index": [5805, 5806, 5807]}
+{"event_id": 871233, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-03-04 06:25:00", "end_date_time": "2020-03-04 06:25:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across North Louisiana during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Nickel size hail fell near Pierre Bossier Mall in Bossier City.", "ts_dict_index": [5820, 5821, 5822]}
+{"event_id": 1086498, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2023-05-10 16:05:00", "end_date_time": "2023-05-10 16:08:00", "narrative": "A strong upper level storm system accompanied by a strong portion of the jetstream brought high winds to portions of central and eastern NM. These southwest winds reached nearly the entire state with high wind gusts being reported from Santa Fe to Albuquerque and through the highlands from Las Vegas to Clines Corners and Vaughn. Areas of blowing dust resulted from these winds, slightly dropping visibilities. The high winds also aided in the rapid spread of a new wildfire near Sapello, NM during the afternoon. There were no reports of damage or injuries directly related to the high winds. Meanwhile, severe weather broke out across far eastern NM along the TX border during the afternoon and evening hours. Thunderstorm activity favored a dryline feature with individual storm cells producing mostly pea to nickel size hail and severe wind gusts. Several severe wind gusts were reported in portions of northeastern NM with one report of one inch size hail near Clovis. Nickel size hail was also reported in San Jon, NM. There were no reports of wind or hail damage. A trained spotter estimated a few nickel size hail stones fell at San Jon. Strong wind gusts also were ripping through their trees, but no damage was reported.", "ts_dict_index": [5826, 5827, 5828]}
+{"event_id": 939731, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2021-02-25 22:35:00", "end_date_time": "2021-02-25 22:35:00", "narrative": "A shallow cold front moved south through East Texas and North Louisiana during the morning hours of February 25th, before becoming stationary during the afternoon over Southeast Texas and Central Louisiana. Meanwhile, a moist southwest flow aloft continued over the Ark-La-Tex ahead of an upper trough that ejected east out of the Southern Rockies and into the Southern Plains, with ripples in this flow contributing to the development of scattered to numerous showers and thunderstorms across North and Northeast Texas, Southwest Arkansas, and extreme Northern Louisiana well north of the stalled surface front. Elevated instability ahead of the upper trough enhanced large scale ascent, resulting in some of these storms to become severe across Red River and Bowie Counties in Northeast Texas during the mid and late evening hours. Large hail fell from these storms, with hail larger than golfballs falling in Bogota before weakening as it entered Bowie County. These storms weakened after midnight as the elevated instability weakened, and showers became widespread across the area. Quarter size hail fell at I-30 and Kings Highway.", "ts_dict_index": [5802, 5803, 5804]}
+{"event_id": 871231, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-03-04 06:15:00", "end_date_time": "2020-03-04 06:15:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across North Louisiana during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. A retired NWS employee reported nickel size hail on Hedges Drive in South Shreveport.", "ts_dict_index": [5817, 5818, 5819]}
+{"event_id": 871236, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-03-04 07:45:00", "end_date_time": "2020-03-04 07:45:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across North Louisiana during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Quarter size hail fell along Barron Road in Keithville.", "ts_dict_index": [5823, 5824, 5825]}
+{"event_id": 871238, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-03-04 07:53:00", "end_date_time": "2020-03-04 07:53:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across North Louisiana during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Dime to quarter size hail fell at Brookwood Baptist Church in South Shreveport.", "ts_dict_index": [5814, 5815, 5816]}
+{"event_id": 871232, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-03-04 06:18:00", "end_date_time": "2020-03-04 06:18:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across North Louisiana during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Quarter size hail fell in Central Shreveport. Report from mPING.", "ts_dict_index": [5811, 5812, 5813]}
+{"event_id": 1006925, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-03-14 20:39:00", "end_date_time": "2022-03-14 20:39:00", "narrative": "A strong shortwave trough traversed east across the Southern Plains during the afternoon and evening of March 14th, which reinforced a cold front southeast across Eastern Oklahoma, Western Arkansas, and North Texas during the afternoon and evening. A strong southerly low level flow allowed for low level moisture and increasing instability to return back north along a warm front, as it entered portions of Deep East Texas and the Lower Toledo Bend Country of Western Louisiana during the evening. Strong large scale forcing ahead of the approaching trough occurred along the cold front, allowing for a line of strong thunderstorms to develop and push east into East Texas during the mid and late evening. Isolated supercell thunderstorms also developed ahead of this line of storms over portions of Deep East Texas, and produced multiple instances of large hail over portions of Angelina, San Augustine, and Rusk Counties. These storms eventually weakened by late evening as they became more elevated and moved away from the waning instability away from the warm front. Pictures of quarter to half-dollar size hail that fell in the Pinehill community were posted to social media.", "ts_dict_index": [5829, 5830, 5831]}
+{"event_id": 939732, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2021-02-25 22:37:00", "end_date_time": "2021-02-25 22:37:00", "narrative": "A shallow cold front moved south through East Texas and North Louisiana during the morning hours of February 25th, before becoming stationary during the afternoon over Southeast Texas and Central Louisiana. Meanwhile, a moist southwest flow aloft continued over the Ark-La-Tex ahead of an upper trough that ejected east out of the Southern Rockies and into the Southern Plains, with ripples in this flow contributing to the development of scattered to numerous showers and thunderstorms across North and Northeast Texas, Southwest Arkansas, and extreme Northern Louisiana well north of the stalled surface front. Elevated instability ahead of the upper trough enhanced large scale ascent, resulting in some of these storms to become severe across Red River and Bowie Counties in Northeast Texas during the mid and late evening hours. Large hail fell from these storms, with hail larger than golfballs falling in Bogota before weakening as it entered Bowie County. These storms weakened after midnight as the elevated instability weakened, and showers became widespread across the area. Penny size hail fell on the northwest side of Texarkana, TX.", "ts_dict_index": [5799, 5800, 5801]}
+{"event_id": 887337, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2020-05-26 20:25:00", "end_date_time": "2020-05-26 20:25:00", "narrative": "A slow moving upper low pressure system over Southern Oklahoma and Northeast Texas drifted east along the Red River Valley during the afternoon and evening hours of May 26th. This system contributed to a decayed complex of showers and thunderstorms that moved through portions of East Texas and North Louisiana during the morning hours, thus stabilizing the air mass through much of the day. However, diurnal heating did contribute to the development of some instability during the late afternoon through the evening hours from Southeast Texas north into portions of East Texas and Northwest Louisiana, as another spoke of upper level energy rotated north-northeast around the center of the upper level low pressure area. This resulted in scattered shower and thunderstorm development by late afternoon through much of the evening hours, with some of these storms becoming severe, resulting in several reports of large hail. These storms persisted into the early morning hours of May 27th, but weakened given the loss of instability. Quarter size hail fell in Hooks.", "ts_dict_index": [5847, 5848, 5849]}
+{"event_id": 1095477, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 15:40:00", "end_date_time": "2023-06-03 15:40:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Dime to nickel size hail fell for approximately 15 to 20 minutes at the NWS Shreveport office with some brief accumulation on grass surfaces.", "ts_dict_index": [5835, 5836, 5837]}
+{"event_id": 1006928, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-03-14 19:21:00", "end_date_time": "2022-03-14 19:21:00", "narrative": "A strong shortwave trough traversed east across the Southern Plains during the afternoon and evening of March 14th, which reinforced a cold front southeast across Eastern Oklahoma, Western Arkansas, and North Texas during the afternoon and evening. A strong southerly low level flow allowed for low level moisture and increasing instability to return back north along a warm front, as it entered portions of Deep East Texas and the Lower Toledo Bend Country of Western Louisiana during the evening. Strong large scale forcing ahead of the approaching trough occurred along the cold front, allowing for a line of strong thunderstorms to develop and push east into East Texas during the mid and late evening. Isolated supercell thunderstorms also developed ahead of this line of storms over portions of Deep East Texas, and produced multiple instances of large hail over portions of Angelina, San Augustine, and Rusk Counties. These storms eventually weakened by late evening as they became more elevated and moved away from the waning instability away from the warm front. Nickel size hail fell on the south side of Tyler.", "ts_dict_index": [5832, 5833, 5834]}
+{"event_id": 1023715, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-05-05 12:52:00", "end_date_time": "2022-05-05 12:52:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, this led to widespread strong to severe thunderstorms during the latter half of the day on May 5th with peak daytime heating aiding in a very unstable environment ahead of the cold front and upper low which were both advancing eastward from the Southern Plains. Nickel-sized hail reported just outside of Valliant northeast of downtown.", "ts_dict_index": [5844, 5845, 5846]}
+{"event_id": 828825, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-06-19 16:45:00", "end_date_time": "2019-06-19 16:45:00", "narrative": "A complex of severe thunderstorms that tracked across portions of East Texas and Northwest Louisiana during the early morning hours of July 19th left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across portions of McCurtain County Oklahoma. These storms produced damaging winds which downed trees near Wright City and along the McCurtain County Oklahoma/Little River County Arkansas line, and produced large hail that fell in Idabel and near Broken Bow before moving into portions of Northeast Texas and Southwest Arkansas late in the afternoon. A brief, isolated tornado also touched down in the Haworth community. Quarter size hail fell in Idabel.", "ts_dict_index": [5841, 5842, 5843]}
+{"event_id": 828826, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-06-19 16:50:00", "end_date_time": "2019-06-19 16:50:00", "narrative": "A complex of severe thunderstorms that tracked across portions of East Texas and Northwest Louisiana during the early morning hours of July 19th left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across portions of McCurtain County Oklahoma. These storms produced damaging winds which downed trees near Wright City and along the McCurtain County Oklahoma/Little River County Arkansas line, and produced large hail that fell in Idabel and near Broken Bow before moving into portions of Northeast Texas and Southwest Arkansas late in the afternoon. A brief, isolated tornado also touched down in the Haworth community. Half dollar size hail fell just south of Broken Bow.", "ts_dict_index": [5838, 5839, 5840]}
+{"event_id": 1087277, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-04-26 18:34:00", "end_date_time": "2023-04-26 18:34:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with multiple reports of large hail observed across Sabine Parish before diminishing after midnight. Half dollar size hail covered the ground in the Belmont area, including a portion of Highway 175 between Belmont and Many.", "ts_dict_index": [5781, 5782, 5783]}
+{"event_id": 949137, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-05-11 14:15:00", "end_date_time": "2021-05-11 14:15:00", "narrative": "A shallow cold front which moved through the Four State Region on May 9th lifted back north as a warm front into portions of Lower East Texas south of Interstate 20 during the afternoon of the 11th, with warm, humid, and unstable air spilling back north into this area ahead of an upper trough that shifted east into the Central and Southern Plains. This trough and associated large scale forcing contributed to a large area of elevated showers and thunderstorms that developed over West Texas during the morning, and spread east into East Texas during the mid and late afternoon. These storms became more surface based as they moved into the warm sector of Lower East Texas, and quickly became severe, producing damaging winds and large hail. However, the storms quickly weakened by late afternoon as they moved back into a more stable air mass near and east of the Sabine River into North Louisiana, but continued to produce widespread moderate to heavy rainfall before exiting the area during the early and mid evening hours. Nickel to quarter size hail fell in Whitehouse.", "ts_dict_index": [5853, 5854, 5855]}
+{"event_id": 823314, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-05-18 17:20:00", "end_date_time": "2019-05-18 17:20:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas. An isolated tornado also touched down just southeast of Tyler with one supercell thunderstorm. These storms began to move repeatedly over the same areas during the evening, with instances of flash flooding reported as well. These storms eventually spread into portions of North Louisiana during the early morning hours of the 19th. Quarter size hail fell in Arp.", "ts_dict_index": [5850, 5851, 5852]}
+{"event_id": 1089182, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-03-16 20:14:00", "end_date_time": "2023-03-16 20:14:00", "narrative": "A long-lived cluster of supercell thunderstorms advanced across northeast Texas into northwest Louisiana on the evening of March 16th just ahead of an accelerating band of thunderstorms along a cold front. As the evening progressed, the cold front gradually overtook the ongoing supercell cluster with the primary threat of hail transitioning to damaging winds within the expanding QLCS. Initially within the far eastern edge of the warm sector, supercell thunderstorms over Sabine County/Parish in Deep East Texas and far western Louisiana produced large hail. The QLCS continued to evolve along the cold front, with an embedded long-lived supercell over Rusk County Texas later in the evening. The environment favored a continuation of the severe threat downstream, with the greatest threat expected along the QLCS segment and with the embedded supercell. As that portion of the line moved southeastward, the threat for damaging winds persisted with a few additional reports of damage in East Texas and Northwest Louisiana. Penny size hail reported via m-PING.", "ts_dict_index": [5874, 5875, 5876]}
+{"event_id": 811779, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-05 16:19:00", "end_date_time": "2019-05-05 16:34:00", "narrative": "Very strong instability developed across the South Plains this afternoon east of a sharp dryline. Scattered thunderstorms developed along the length of this dryline by 1600 CST and slowly matured into severe thunderstorms, including supercells. A remnant outflow boundary near the US Highway 84 corridor drifted west and interacted with an already stout supercell in southwest Lubbock County. This supercell proceeded to anchor to this boundary as it moved slowly southward and supported at least two sizable tornadoes in Lynn County over the next two hours. One of these tornadoes lasted 65 minutes and grew very intense with over 150 knots of gate-to-gate rotation noted per the Lubbock WSR-88D. These tornadoes narrowly missed population centers such as Tahoka and O'Donnell, but extensive lead time from warnings and excellent storm spotter reports gave the public plenty of time to seek shelter. This prolific supercell also produced very large hail to tennis ball size, intense RFD winds over 80 mph, and flash flooding. On the heels of the earlier hail, a second hailstorm affected much of the same areas of southern Lubbock, this time with hailstones only to the size of half dollars. Damage estimates from this second hailstorm were impossible to estimate given the earlier damage.", "ts_dict_index": [5859, 5860, 5861]}
+{"event_id": 1089181, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-03-16 20:07:00", "end_date_time": "2023-03-16 20:07:00", "narrative": "A long-lived cluster of supercell thunderstorms advanced across northeast Texas into northwest Louisiana on the evening of March 16th just ahead of an accelerating band of thunderstorms along a cold front. As the evening progressed, the cold front gradually overtook the ongoing supercell cluster with the primary threat of hail transitioning to damaging winds within the expanding QLCS. Initially within the far eastern edge of the warm sector, supercell thunderstorms over Sabine County/Parish in Deep East Texas and far western Louisiana produced large hail. The QLCS continued to evolve along the cold front, with an embedded long-lived supercell over Rusk County Texas later in the evening. The environment favored a continuation of the severe threat downstream, with the greatest threat expected along the QLCS segment and with the embedded supercell. As that portion of the line moved southeastward, the threat for damaging winds persisted with a few additional reports of damage in East Texas and Northwest Louisiana. Quarter size hail reported and winds estimated near 60 mph in Southeast Tyler.", "ts_dict_index": [5871, 5872, 5873]}
+{"event_id": 823315, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-05-18 17:35:00", "end_date_time": "2019-05-18 17:35:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas. An isolated tornado also touched down just southeast of Tyler with one supercell thunderstorm. These storms began to move repeatedly over the same areas during the evening, with instances of flash flooding reported as well. These storms eventually spread into portions of North Louisiana during the early morning hours of the 19th. Quarter size hail fell just east of New London.", "ts_dict_index": [5856, 5857, 5858]}
+{"event_id": 1089184, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-03-16 20:55:00", "end_date_time": "2023-03-16 20:55:00", "narrative": "A long-lived cluster of supercell thunderstorms advanced across northeast Texas into northwest Louisiana on the evening of March 16th just ahead of an accelerating band of thunderstorms along a cold front. As the evening progressed, the cold front gradually overtook the ongoing supercell cluster with the primary threat of hail transitioning to damaging winds within the expanding QLCS. Initially within the far eastern edge of the warm sector, supercell thunderstorms over Sabine County/Parish in Deep East Texas and far western Louisiana produced large hail. The QLCS continued to evolve along the cold front, with an embedded long-lived supercell over Rusk County Texas later in the evening. The environment favored a continuation of the severe threat downstream, with the greatest threat expected along the QLCS segment and with the embedded supercell. As that portion of the line moved southeastward, the threat for damaging winds persisted with a few additional reports of damage in East Texas and Northwest Louisiana. Nickel size hail reported on County Road 405D.", "ts_dict_index": [5877, 5878, 5879]}
+{"event_id": 1089168, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-03-16 18:47:00", "end_date_time": "2023-03-16 18:47:00", "narrative": "A long-lived cluster of supercell thunderstorms advanced across northeast Texas into northwest Louisiana on the evening of March 16th just ahead of an accelerating band of thunderstorms along a cold front. As the evening progressed, the cold front gradually overtook the ongoing supercell cluster with the primary threat of hail transitioning to damaging winds within the expanding QLCS. Initially within the far eastern edge of the warm sector, supercell thunderstorms over Sabine County/Parish in Deep East Texas and far western Louisiana produced large hail. The QLCS continued to evolve along the cold front, with an embedded long-lived supercell over Rusk County Texas later in the evening. The environment favored a continuation of the severe threat downstream, with the greatest threat expected along the QLCS segment and with the embedded supercell. As that portion of the line moved southeastward, the threat for damaging winds persisted with a few additional reports of damage in East Texas and Northwest Louisiana. Quarter size hail reported at the Fisherman's Fast Stop south of the Negreet community.", "ts_dict_index": [5865, 5866, 5867]}
+{"event_id": 1089167, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-03-16 18:17:00", "end_date_time": "2023-03-16 18:17:00", "narrative": "A long-lived cluster of supercell thunderstorms advanced across northeast Texas into northwest Louisiana on the evening of March 16th just ahead of an accelerating band of thunderstorms along a cold front. As the evening progressed, the cold front gradually overtook the ongoing supercell cluster with the primary threat of hail transitioning to damaging winds within the expanding QLCS. Initially within the far eastern edge of the warm sector, supercell thunderstorms over Sabine County/Parish in Deep East Texas and far western Louisiana produced large hail. The QLCS continued to evolve along the cold front, with an embedded long-lived supercell over Rusk County Texas later in the evening. The environment favored a continuation of the severe threat downstream, with the greatest threat expected along the QLCS segment and with the embedded supercell. As that portion of the line moved southeastward, the threat for damaging winds persisted with a few additional reports of damage in East Texas and Northwest Louisiana. Quarter size hail reported in Florien.", "ts_dict_index": [5868, 5869, 5870]}
+{"event_id": 832639, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2019-06-29 02:50:00", "end_date_time": "2019-06-29 02:50:00", "narrative": "An upper level trough over Northern Mississippi drifted west into Southern Arkansas, Northern Louisiana, and extreme Northeast Texas during June 28th, which helped to ignite scattered showers and thunderstorms over Southcentral Arkansas and Northcentral Louisiana during the afternoon, evening, through the early morning hours on the 29th with the aid of available heating and ample low level moisture. While this resulted in a brief period of isolated strong to severe thunderstorms during the mid and late afternoon hours on the 28th across portions of Southcentral Arkansas and Northcentral Louisiana, these storms diminished during the evening but left behind residual outflow boundaries which ignited additional isolated to scattered showers and thunderstorms during the morning hours of June 29th across portions of Southwest Arkansas, Northwest Louisiana, and extreme Northeast Texas. A couple of isolated thunderstorms briefly became severe over Eastern Bowie County Texas, producing quarter size hail in the Leary community and just northeast of Maud before diminishing. Quarter size hail fell in the Leary community.", "ts_dict_index": [5808, 5809, 5810]}
+{"event_id": 1085428, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-15 16:21:00", "end_date_time": "2023-04-15 16:21:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. Ping pong ball size hail fell in the Eastwood community.", "ts_dict_index": [5892, 5893, 5894]}
+{"event_id": 825082, "event_type": "Hail", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2019-06-15 16:50:00", "end_date_time": "2019-06-15 16:50:00", "narrative": "Increasingly humid conditions, a weak low pressure system, and an impinging northern weak cold front combined to create an environment ripe for strong to severe storms across northern and central Iowa, with much of the severe activity through central Iowa. ||The resulting environment from the aforementioned ingredients included SBCAPE values in the 2000-3000+ J/kg range, marginal effective bulk shear around 30 kts, 400-600 J/kg CAPE in the hail growth region, and at least a few hours with steep low level lapse rates around or greater than 8 deg C/km. All in all while the environment did not lend much support to long lived strong to severe storms, it was more than enough for brief periods of severe storms as many pulsed up and down prior to congealing into multi-cellular clusters and eventually an mesoscale convective system by the evening. Most reports revolved around severe and damaging winds, with a few instances of hail, heavy rainfall, and a land-spout reported north of Whitten in Hardin county. Public reported nickel sized hail.", "ts_dict_index": [5886, 5887, 5888]}
+{"event_id": 1089183, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-03-16 20:45:00", "end_date_time": "2023-03-16 20:45:00", "narrative": "A long-lived cluster of supercell thunderstorms advanced across northeast Texas into northwest Louisiana on the evening of March 16th just ahead of an accelerating band of thunderstorms along a cold front. As the evening progressed, the cold front gradually overtook the ongoing supercell cluster with the primary threat of hail transitioning to damaging winds within the expanding QLCS. Initially within the far eastern edge of the warm sector, supercell thunderstorms over Sabine County/Parish in Deep East Texas and far western Louisiana produced large hail. The QLCS continued to evolve along the cold front, with an embedded long-lived supercell over Rusk County Texas later in the evening. The environment favored a continuation of the severe threat downstream, with the greatest threat expected along the QLCS segment and with the embedded supercell. As that portion of the line moved southeastward, the threat for damaging winds persisted with a few additional reports of damage in East Texas and Northwest Louisiana. Quarter size hail reported.", "ts_dict_index": [5880, 5881, 5882]}
+{"event_id": 1089185, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-03-16 21:07:00", "end_date_time": "2023-03-16 21:07:00", "narrative": "A long-lived cluster of supercell thunderstorms advanced across northeast Texas into northwest Louisiana on the evening of March 16th just ahead of an accelerating band of thunderstorms along a cold front. As the evening progressed, the cold front gradually overtook the ongoing supercell cluster with the primary threat of hail transitioning to damaging winds within the expanding QLCS. Initially within the far eastern edge of the warm sector, supercell thunderstorms over Sabine County/Parish in Deep East Texas and far western Louisiana produced large hail. The QLCS continued to evolve along the cold front, with an embedded long-lived supercell over Rusk County Texas later in the evening. The environment favored a continuation of the severe threat downstream, with the greatest threat expected along the QLCS segment and with the embedded supercell. As that portion of the line moved southeastward, the threat for damaging winds persisted with a few additional reports of damage in East Texas and Northwest Louisiana. Dime to nickel size hail reported on the southeast side of Henderson along Highway 259.", "ts_dict_index": [5883, 5884, 5885]}
+{"event_id": 811767, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-05 15:30:00", "end_date_time": "2019-05-05 16:04:00", "narrative": "Very strong instability developed across the South Plains this afternoon east of a sharp dryline. Scattered thunderstorms developed along the length of this dryline by 1600 CST and slowly matured into severe thunderstorms, including supercells. A remnant outflow boundary near the US Highway 84 corridor drifted west and interacted with an already stout supercell in southwest Lubbock County. This supercell proceeded to anchor to this boundary as it moved slowly southward and supported at least two sizable tornadoes in Lynn County over the next two hours. One of these tornadoes lasted 65 minutes and grew very intense with over 150 knots of gate-to-gate rotation noted per the Lubbock WSR-88D. These tornadoes narrowly missed population centers such as Tahoka and O'Donnell, but extensive lead time from warnings and excellent storm spotter reports gave the public plenty of time to seek shelter. This prolific supercell also produced very large hail to tennis ball size, intense RFD winds over 80 mph, and flash flooding. This was the first of at least two hail swaths that impacted many areas of south and southwest Lubbock. Fortunately, the hail fell without any strong winds, but minor hail damage was likely inflicted to thousands of vehicles across the area.", "ts_dict_index": [5862, 5863, 5864]}
+{"event_id": 1085430, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-15 16:11:00", "end_date_time": "2023-04-15 16:11:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. Quarter to half dollar size hail fell in Bossier City just northeast of Barksdale Air Force Base.", "ts_dict_index": [5901, 5902, 5903]}
+{"event_id": 879916, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-19 10:05:00", "end_date_time": "2020-04-19 10:05:00", "narrative": "A warm front lifted north into Deep East Texas and the southern sections of North Central Louisiana by afternoon on April 19th, ahead of a vigorous upper level trough that ejected east from New Mexico across Texas. Large scale forcing increased by afternoon ahead of the trough as it approached the expanding warm sector, characteristic of moderate instability and strong wind shear. Areas of showers and thunderstorms developed and became widespread near and north of the warm front, and limited the northward progress of the front, but severe thunderstorms still developed within the warm sector across Deep East Texas and Northcentral Louisiana, resulting in areas of damaging winds across these areas. An isolated elevated severe thunderstorm also developed over portions of Lamar County Texas, which moved into Red River County and produced quarter size hail near Clarksville. These storms eventually weakened during the mid evening hours with the passage of the trough through the area. Nickel size hail fell along Highway 259 northwest of Appleby.", "ts_dict_index": [5916, 5917, 5918]}
+{"event_id": 1113721, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2023-06-26 06:40:00", "end_date_time": "2023-06-26 06:40:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Quarter size hail reported in the Red Springs community north of West 7th Street and west of FM Road 2148.", "ts_dict_index": [5940, 5941, 5942]}
+{"event_id": 1085465, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-15 19:05:00", "end_date_time": "2023-04-15 19:05:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. Nickel to quarter size hail fell at a gas station at the corner of Sligo Road and Highway 157 in the Oakland community.", "ts_dict_index": [5895, 5896, 5897]}
+{"event_id": 1085432, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-15 16:05:00", "end_date_time": "2023-04-15 16:05:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. Half dollar size hail fell in Bossier City.", "ts_dict_index": [5910, 5911, 5912]}
+{"event_id": 1085434, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-15 16:41:00", "end_date_time": "2023-04-15 16:41:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. Ping pong ball size hail fell across the southern sections of Haughton.", "ts_dict_index": [5904, 5905, 5906]}
+{"event_id": 956665, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2021-06-26 15:48:00", "end_date_time": "2021-06-26 15:52:00", "narrative": "After several days of relatively drier air at the surface resulted in more gusty winds than wetting precipitation, a moist backdoor cold front that invaded eastern New Mexico early on June 26, 2021. This boundary tracked westward through the state before stronger westerly flow aloft stalled it along the east slopes of the central mountain chain. Behind this boundary, deeper moisture across the plains of New Mexico resulted in an uptick in storm coverage. With a destabilizing atmosphere and increasing wind shear, the environment was supportive for strong to severe thunderstorms during the afternoon and evening hours. The greatest severe weather threat was across the southeastern portion of the area where these thunderstorms produced large hail and severe winds. A particularly strong thunderstorm near Logan, New Mexico produced several inches of hail accumulation while 70 mph wind speeds downed power lines, caused mobile home damage, and overturned a tractor trailer in the area. A strong thunderstorm moving southeast through Ragland produced nickel size hail.", "ts_dict_index": [5925, 5926, 5927]}
+{"event_id": 879914, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2020-04-19 09:57:00", "end_date_time": "2020-04-19 09:57:00", "narrative": "A warm front lifted north into Deep East Texas and the southern sections of North Central Louisiana by afternoon on April 19th, ahead of a vigorous upper level trough that ejected east from New Mexico across Texas. Large scale forcing increased by afternoon ahead of the trough as it approached the expanding warm sector, characteristic of moderate instability and strong wind shear. Areas of showers and thunderstorms developed and became widespread near and north of the warm front, and limited the northward progress of the front, but severe thunderstorms still developed within the warm sector across Deep East Texas and Northcentral Louisiana, resulting in areas of damaging winds across these areas. An isolated elevated severe thunderstorm also developed over portions of Lamar County Texas, which moved into Red River County and produced quarter size hail near Clarksville. These storms eventually weakened during the mid evening hours with the passage of the trough through the area. Ping pong ball size hail fell in the Lilbert community.", "ts_dict_index": [5919, 5920, 5921]}
+{"event_id": 1113725, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2023-06-26 07:17:00", "end_date_time": "2023-06-26 07:17:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Golf ball size hail reported just west of Hooks via social media.", "ts_dict_index": [5931, 5932, 5933]}
+{"event_id": 956663, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2021-06-26 14:50:00", "end_date_time": "2021-06-26 15:10:00", "narrative": "After several days of relatively drier air at the surface resulted in more gusty winds than wetting precipitation, a moist backdoor cold front that invaded eastern New Mexico early on June 26, 2021. This boundary tracked westward through the state before stronger westerly flow aloft stalled it along the east slopes of the central mountain chain. Behind this boundary, deeper moisture across the plains of New Mexico resulted in an uptick in storm coverage. With a destabilizing atmosphere and increasing wind shear, the environment was supportive for strong to severe thunderstorms during the afternoon and evening hours. The greatest severe weather threat was across the southeastern portion of the area where these thunderstorms produced large hail and severe winds. A particularly strong thunderstorm near Logan, New Mexico produced several inches of hail accumulation while 70 mph wind speeds downed power lines, caused mobile home damage, and overturned a tractor trailer in the area. Trained spotters and law enforcement in Logan reported estimated quarter size hail from a severe thunderstorm tracking southeast through the area. The hail tore holes in mobile home siding. This thunderstorm also produced six to twelve inches of hail accumulation across Logan, including along New Mexico State Highway 54. Damages are estimated for the hail damage to the mobile homes.", "ts_dict_index": [5928, 5929, 5930]}
+{"event_id": 1085426, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-15 16:05:00", "end_date_time": "2023-04-15 16:05:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. Ping pong ball size hail fell at Barksdale Air Force Base.", "ts_dict_index": [5898, 5899, 5900]}
+{"event_id": 1113724, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2023-06-26 07:24:00", "end_date_time": "2023-06-26 07:24:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Golf ball size hail reported at Red River Army Depot.", "ts_dict_index": [5937, 5938, 5939]}
+{"event_id": 1085637, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-04-20 15:42:00", "end_date_time": "2023-04-20 15:42:00", "narrative": "An upper level low pressure system shifted east from Montana east into the Dakotas on April 20th, with the attendant trough extending southward through the Rockies before ejecting east through the Central and Southern Plains during the afternoon and evening. A strong southerly low level flow ahead of this trough ushered very warm and humid air back north into the Four State Region on the 19th-20th, which primed the area with moderate instability ahead of an associated cold front that entered the region during the afternoon. Large scale forcing increased by mid and late afternoon through the evening along and ahead of the front and upper trough within the warm, moist, and unstable sector, enhancing scattered to numerous shower and thunderstorm development across portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. An isolated strong thunderstorm developed over Southern McCurtain County Oklahoma along the front, with nickel size hail reported in Haworth before weakening. Dime to nickel size hail fell at the Country Store Convenience Store in Haworth.", "ts_dict_index": [5913, 5914, 5915]}
+{"event_id": 946629, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-04-09 21:50:00", "end_date_time": "2021-04-09 21:50:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with these storms affecting McCurtain County Oklahoma along the cold front during the late evening hours. Damaging winds were measured at 70 mph from the Idabel Mesonet station, with golfball size hail falling in the Harris community, before exiting the county to the southeast just prior to midnight with the passage of the cold front. Golfball size hail fell in the Harris community.", "ts_dict_index": [5922, 5923, 5924]}
+{"event_id": 1085461, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-04-15 18:00:00", "end_date_time": "2023-04-15 18:00:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. Half dollar size hail fell just southwest of Noble. Report from m-PING.", "ts_dict_index": [5907, 5908, 5909]}
+{"event_id": 1085470, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-04-15 17:35:00", "end_date_time": "2023-04-15 17:35:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. Hen egg size hail fell west of Converse near the intersection of Highways 191 and 174.", "ts_dict_index": [5889, 5890, 5891]}
+{"event_id": 1085471, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2023-04-15 16:25:00", "end_date_time": "2023-04-15 16:25:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of large hail across portions of East Texas before exiting the area during the mid-evening hours. Penny size hail fell in the Appleby community.", "ts_dict_index": [5955, 5956, 5957]}
+{"event_id": 952668, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2021-05-26 01:20:00", "end_date_time": "2021-05-26 01:20:00", "narrative": "Following a decaying complex of showers and thunderstorms that moved east across East Texas, extreme Southwest Arkansas, and Northwest Louisiana during the afternoon and evening on May 25th, additional showers and thunderstorms redeveloped across portions of extreme Northeast Texas and Southwest Arkansas during the late evening through the early morning hours of May 26th, along and ahead of a shortwave trough and associated weak surface front that moved into these areas. A very moist air mass was present as these showers and thunderstorms developed, with these storms redeveloping and moving over the same areas of Bowie County in Northeast Texas and Miller County in Southwest Arkansas. Widespread rainfall amounts of three to six inches fell over these areas during the early morning hours of the 26th, resulting in extensive flash flooding especially throughout the city of Texarkana. These storms finally diminished shortly after daybreak. Nickel size hail fell in the Wake Village community.", "ts_dict_index": [5973, 5974, 5975]}
+{"event_id": 953192, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2021-05-24 23:06:00", "end_date_time": "2021-05-24 23:06:00", "narrative": "Scattered thunderstorms initially developed over the western South Plains on the afternoon of the 24th under a very unstable atmosphere. Relatively weak atmospheric flow for late May kept most of these storms from becoming severe. These storms produced mostly heavy rainfall but were also able to generate a few severe hail and wind reports. Most hail reports were only up to the size of quarters but one report of golf balls was reported in Hockley County near Whitharral. More notably, heavy rain caused flash flooding in the city of Lubbock and along the Double Mountain Fork of the Brazos in Lubbock County. Heavy rain over the northeastern portion of the city of Lubbock flowed through Mackenzie Park into the Double Mountain Fork of the Brazos. This water made its way downstream into Buffalo Springs Lake flowing over Farm to Market Road 835 west of the lake. The road was shut down on the 25th due to water flowing over the roadway making it impassable. An off duty NWS employee measured quarter size hail around the intersection of 42nd Street and Indiana Avenue in the city of Lubbock.", "ts_dict_index": [5961, 5962, 5963]}
+{"event_id": 1113892, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2023-07-14 09:40:00", "end_date_time": "2023-07-14 09:47:00", "narrative": "A broad upper trough was centered over Canada and extended southward over the Central Plains to the East Coast. Upper level disturbances had moved over the Central Plains at the base of the trough and provided lift. One of the upper disturbances moved over south central Nebraska in the late morning to early afternoon hours. CAPE was fairly high across the area and zero to six km wind shear was generally between 30 to 45 knots. Mid-level lapse rates were generally between 7 to 8 degrees C/km. ||Showers and thunderstorms developed across Nebraska during the morning hours. A cluster of storms moved into south central Nebraska from the west. One storm produced penny sized hail in Dawson County just after 10 AM CDT. Another storm strengthened as it moved in from the west and impacted Furnas County. This storm began by producing nickel sized hail at 10:40 AM CDT and ended by producing quarter size hail at 11:18 AM CDT. This storm had also produced a wind gust up to 64 mph. Penny to nickel size hail was reported in the area, accompanied by wind gusts near 45 MPH.", "ts_dict_index": [5949, 5950, 5951]}
+{"event_id": 1019312, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2022-06-07 19:00:00", "end_date_time": "2022-06-07 19:15:00", "narrative": "A backdoor cold front that moved through eastern New Mexico early on June 6, 2022, set the stage for a round of severe thunderstorms across northeast and east central New Mexico as it ushered it beneficial low-level moisture. With plentiful instability and wind shear across this area, the atmosphere quickly became supportive of strong to severe thunderstorms. Thunderstorms developed first across the Sangre de Cristo Mountains and then tracked in an easterly direction onto the plains where they strengthened. The strongest thunderstorm of the day started near Wagon Mound and then made a right turn before tracking southeastward through Harding, San Miguel, and Quay counties. When the thunderstorm was southwest of Roy, it developed a strong mesocyclone. While no mesocyclonic tornado was observed, a brief and weak landspout was. This thunderstorm's main hazard then was very large hail with hail up to baseball size reported near Bell Ranch. A CoCoRaHS observer near Ute Lake State Park reported quarter size hail.", "ts_dict_index": [5976, 5977, 5978]}
+{"event_id": 808885, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-04-04 01:38:00", "end_date_time": "2019-04-04 01:38:00", "narrative": "Warmer, more humid and unstable air began to return north across East Texas and North Louisiana during the evening hours on April 3rd, and continued through much of the day on the 4th, well east of an area of surface low development over the Oklahoma Panhandle. This was in response to an upper level trough that began to pivot east from the Rockies and across the Plains during the early morning hours of the 4th. Upper level disturbances ejecting northeast ahead of the trough tapped into some elevated instability aloft which resulted in isolated elevated severe thunderstorms developing over portions of extreme Eastern Texas, which quickly shifted northeast into portions of Northwest Louisiana. Additional scattered strong to severe thunderstorms containing large hail developed farther east across portions of North Louisiana, which resulted in several instances of hail over this area before weakening late in the morning and early afternoon. Half dollar size hail fell in the Bethany community along the Louisiana/Texas border.", "ts_dict_index": [5970, 5971, 5972]}
+{"event_id": 808888, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-04-06 10:40:00", "end_date_time": "2019-04-06 10:40:00", "narrative": "Warmer, more humid and unstable air began to return north across East Texas and North Louisiana during the evening hours on April 3rd, and continued through much of the day on the 4th, well east of an area of surface low development over the Oklahoma Panhandle. This was in response to an upper level trough that began to pivot east from the Rockies and across the Plains during the early morning hours of the 4th. Upper level disturbances ejecting northeast ahead of the trough tapped into some elevated instability aloft which resulted in isolated elevated severe thunderstorms developing over portions of extreme Eastern Texas, which quickly shifted northeast into portions of Northwest Louisiana. Additional scattered strong to severe thunderstorms containing large hail developed farther east across portions of North Louisiana, which resulted in several instances of hail over this area before weakening late in the morning and early afternoon. Quarter size hail fell in the Elm Grove community. Report received via Facebook by KSLA-TV.", "ts_dict_index": [5967, 5968, 5969]}
+{"event_id": 1113717, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-26 03:28:00", "end_date_time": "2023-06-26 03:28:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Quarter size hail reported near Valliant via mPING.", "ts_dict_index": [5946, 5947, 5948]}
+{"event_id": 1104308, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-06-10 14:35:00", "end_date_time": "2023-06-10 14:35:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. Nickel size hail south of Highway 6.", "ts_dict_index": [5952, 5953, 5954]}
+{"event_id": 1113487, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-23 16:06:00", "end_date_time": "2023-06-23 16:06:00", "narrative": "Scattered strong to severe thunderstorms developed across parts of East Texas on the afternoon of June 23rd, aided by forcing for ascent from weak warm air advection and downstream of a significant but weakening cluster of storms shifting southeast from the middle Red River Valley. This was also focused along the eastern periphery of a plume of warm, capping elevated mixed-layer air, which supported instability up to 4000 J/kg for boundary layer moisture characterized by mid 70s dew points. Under 25-30 knots of northwesterly flow around 500 millibars, deep-layer shear was marginally supportive for the evolution of supercells, and an upscale growing organized cluster as convective inhibition weakened in the peak late afternoon heating. The environment was at least conditionally supportive of large hail and increasing damaging winds, which ultimately occurred across parts of Rusk County and adjacent Panola County with multiple local storm reports. Nickel size hail reported in Henderson.", "ts_dict_index": [5964, 5965, 5966]}
+{"event_id": 1113722, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2023-06-26 07:18:00", "end_date_time": "2023-06-26 07:18:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Quarter size hail reported just west of Hooks via mPING.", "ts_dict_index": [5934, 5935, 5936]}
+{"event_id": 1053214, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 13:47:00", "end_date_time": "2022-08-19 13:47:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. Report from mping.", "ts_dict_index": [5979, 5980, 5981]}
+{"event_id": 1053211, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 13:45:00", "end_date_time": "2022-08-19 13:45:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. WOI-5 reported three inch hail at the station in West Des Moines.", "ts_dict_index": [5985, 5986, 5987]}
+{"event_id": 1053205, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 13:40:00", "end_date_time": "2022-08-19 13:40:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. WOI-5 storm team reports ping pong ball sized hail at studio.", "ts_dict_index": [5991, 5992, 5993]}
+{"event_id": 1053213, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 13:46:00", "end_date_time": "2022-08-19 13:46:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. Delayed report via social media of two inch diameter hail reported at Valley High School. Many cars with broken windshields. Hail damage to school resulted in water falling into the library with damage to books. Time estimated via radar.", "ts_dict_index": [5982, 5983, 5984]}
+{"event_id": 1053206, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 13:40:00", "end_date_time": "2022-08-19 13:40:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. Golf balled sized hail reported breaking windshields.", "ts_dict_index": [5988, 5989, 5990]}
+{"event_id": 1113723, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2023-06-26 07:35:00", "end_date_time": "2023-06-26 07:35:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Half dollar size hail reported northeast of Redwater on Shavers Lane just off Highway 67 via mPING.", "ts_dict_index": [5943, 5944, 5945]}
+{"event_id": 1053221, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 14:10:00", "end_date_time": "2022-08-19 14:10:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. Delayed report of quarter sized hail. Time estimated form radar.", "ts_dict_index": [5994, 5995, 5996]}
+{"event_id": 1053207, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 13:40:00", "end_date_time": "2022-08-19 13:40:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. One and a half to two inch hail in Clive.", "ts_dict_index": [5997, 5998, 5999]}
+{"event_id": 1110565, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-06-14 13:15:00", "end_date_time": "2023-06-14 13:15:00", "narrative": "Supercell thunderstorms developed toward midday across the middle Red River Valley along and south of a stalled frontal boundary. These thunderstorms progressed east southeast with upper 80s temperatures on the warm side of the boundary with dew points exceeding 75 degrees. Mid-level lapse rates of 7-8 C/km overspread this very moist low-level air mass over a rather broad west-to-east corridor, supporting extreme instability upwards of 4500 J/kg well downstream of the upscale-growing convection. Coinciding this corridor of extreme buoyancy was very strong effective bulk shear near 65 kts along with hodographs that were modestly curved at the low levels and elongated above 3 km AGL. Numerous local storm reports were documented of large hail and damaging wind gusts across parts of North Louisiana throughout the event. Unfortunately, a 73 year old male was killed in a fire ignited after lightning struck his home near Shongaloo in Northern Webster Parish. Quarter size hail reported via mPING.", "ts_dict_index": [5958, 5959, 5960]}
+{"event_id": 822139, "event_type": "Hail", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2019-05-16 18:38:00", "end_date_time": "2019-05-16 18:38:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Emergency manager reported ping pong ball sized hail.", "ts_dict_index": [6021, 6022, 6023]}
+{"event_id": 822153, "event_type": "Hail", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2019-05-16 19:03:00", "end_date_time": "2019-05-16 19:03:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Public reported quarter sized hail, via social media.", "ts_dict_index": [6042, 6043, 6044]}
+{"event_id": 822140, "event_type": "Hail", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2019-05-16 18:44:00", "end_date_time": "2019-05-16 18:44:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported ping pong ball sized hail ongoing.", "ts_dict_index": [6027, 6028, 6029]}
+{"event_id": 822142, "event_type": "Hail", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2019-05-16 18:46:00", "end_date_time": "2019-05-16 18:46:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported pea, nickel and a few quarter sized hail stones.", "ts_dict_index": [6036, 6037, 6038]}
+{"event_id": 822138, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 18:37:00", "end_date_time": "2019-05-16 18:37:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported nickel to quarter sized hail along with strong winds. No damage seen from winds at the time.", "ts_dict_index": [6018, 6019, 6020]}
+{"event_id": 822136, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 18:35:00", "end_date_time": "2019-05-16 18:35:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Public reported quarter sized hail via social media.", "ts_dict_index": [6033, 6034, 6035]}
+{"event_id": 822134, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 18:32:00", "end_date_time": "2019-05-16 18:32:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported penny sized hail at Urbandale High School.", "ts_dict_index": [6045, 6046, 6047]}
+{"event_id": 816089, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-04-28 20:28:00", "end_date_time": "2019-04-28 20:28:00", "narrative": "After a rather chilly overnight, complete with reports of up to 3.5 inches of snow in northern Iowa, storms initiated across portions of central Iowa and produced multiple instances of severe hail. ||Throughout the day, surface high pressure centered over the state slid eastward, placing the western half of the state back in warm air advection by the evening hours, especially above surface levels. The environment was not extremely conducive to sustained severe weather, but did have indications of hail potential, including a freezing level below 10kft, moderate to steep lapse rates above the near surface inversion, and a few hundred J/kg CAPE in the hail growth zone. Elevated storms roughly initiated along the 850mb front along and near I-80 across western Des Moines and west of the metro area. Storms were not long lived, but were able to produce a number of reports of severe hail, including up to half dollar in size. Public reported quarter sized hail via the mPING app.", "ts_dict_index": [6015, 6016, 6017]}
+{"event_id": 1053209, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 13:45:00", "end_date_time": "2022-08-19 13:45:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. Delayed report via social media of ping pong ball sized hail in West Des Moines. Time estimated via radar.", "ts_dict_index": [6003, 6004, 6005]}
+{"event_id": 822132, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 18:31:00", "end_date_time": "2019-05-16 18:31:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported penny sized hail at 48th and Forest Ave in Des Moines.", "ts_dict_index": [6039, 6040, 6041]}
+{"event_id": 1053215, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 13:50:00", "end_date_time": "2022-08-19 13:50:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. Hail at least 1.5 to 2 inches with many cars damaged at Valley West Mall. Delayed report, time estimated via radar.", "ts_dict_index": [6006, 6007, 6008]}
+{"event_id": 816088, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-04-28 20:24:00", "end_date_time": "2019-04-28 20:24:00", "narrative": "After a rather chilly overnight, complete with reports of up to 3.5 inches of snow in northern Iowa, storms initiated across portions of central Iowa and produced multiple instances of severe hail. ||Throughout the day, surface high pressure centered over the state slid eastward, placing the western half of the state back in warm air advection by the evening hours, especially above surface levels. The environment was not extremely conducive to sustained severe weather, but did have indications of hail potential, including a freezing level below 10kft, moderate to steep lapse rates above the near surface inversion, and a few hundred J/kg CAPE in the hail growth zone. Elevated storms roughly initiated along the 850mb front along and near I-80 across western Des Moines and west of the metro area. Storms were not long lived, but were able to produce a number of reports of severe hail, including up to half dollar in size. Public relayed estimated quarter sized hail via the mPING app, and was located right underneath the hail core via radar.", "ts_dict_index": [6012, 6013, 6014]}
+{"event_id": 1053208, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 13:43:00", "end_date_time": "2022-08-19 13:43:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. Dime up to golf ball sized hail.", "ts_dict_index": [6009, 6010, 6011]}
+{"event_id": 822133, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 18:32:00", "end_date_time": "2019-05-16 18:32:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. NWS Employee reported up to nickel sized hail.", "ts_dict_index": [6048, 6049, 6050]}
+{"event_id": 826917, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 19:55:00", "end_date_time": "2019-05-16 20:00:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. The local media reported hail caused damage to the roofs of Hoover High School and Meredith Middle School, making some spaces unusable. Some classes had to be moved, and some ofthe classes were dismissed early on Friday for repairs to be made. Some of the classrooms were flooded as well.", "ts_dict_index": [6024, 6025, 6026]}
+{"event_id": 1053210, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2022-08-19 13:45:00", "end_date_time": "2022-08-19 13:45:00", "narrative": "A surface low sinking south into the area allowed for scattered storms to develop across central Iowa in the afternoon. Steep lapse rates and deep layer shear allowed for the development of organized updrafts while low melting levels supported larger hail development. Several storms strengthened and prompted warnings, though few resulted in any severe reports. The strongest quickly developed over the Des Moines metro, where the time between a clear radar image and golf ball sized hail was just over 20 minutes. Hail pummeled the west side of the metro for nearly 30 minutes, resulting in hundreds of vehicles with significant damage. One high school in West Des Moines also reported damage to the building which resulted in water leaking into the library and a rush to protect the books. After the hail ended the storms continued to train across the metro, resulting in flash flooding a a couple of water rescues due to stranded vehicles. Delayed report of egg sized hail in West Des Moines. Time estimated by radar.", "ts_dict_index": [6000, 6001, 6002]}
+{"event_id": 822160, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 20:00:00", "end_date_time": "2019-05-16 20:00:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Public reported half dollar sized hail, via pictures on social media.", "ts_dict_index": [6030, 6031, 6032]}
+{"event_id": 1140454, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:54:00", "end_date_time": "2023-09-24 19:54:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced baseball size hail in Round Rock.", "ts_dict_index": [6096, 6097, 6098]}
+{"event_id": 1140453, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:52:00", "end_date_time": "2023-09-24 19:52:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail at the intersection of FM 1431 and I-35 in Round Rock.", "ts_dict_index": [6108, 6109, 6110]}
+{"event_id": 823744, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-23 19:30:00", "end_date_time": "2019-05-23 19:34:00", "narrative": "Another day of long-lived widespread severe weather was observed on the South Plains of West Texas on the afternoon and evening of the 23rd. The first report of severe weather was received at 1518 CST with the final report at 2309 CST. A persistent long wave trough over the western United States remained in place with a dryline moving into the South Plains in the afternoon. Numerous thunderstorms developed east of the dryline and took advantage of strong shear and instability and rapidly became severe. Most reports consisted of large hail with the largest report of baseball size hail near Shallowater (Lubbock County). Despite the strong shear and low cloud bases, only one report was received of a tornado. A brief anticyclonic tornado was observed west of Brownfield (Terry County). Additionally, very heavy rainfall caused flooding in portions of the southwestern part of the city of Lubbock (Lubbock County). A swath of hail was reported with hail sizes ranging from golf ball up to baseball. No damage was reported.", "ts_dict_index": [6066, 6067, 6068]}
+{"event_id": 822149, "event_type": "Hail", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2019-05-16 18:54:00", "end_date_time": "2019-05-16 18:54:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported ongoing hail from nickels to ping pong ball in size.", "ts_dict_index": [6054, 6055, 6056]}
+{"event_id": 823836, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-23 20:57:00", "end_date_time": "2019-05-23 20:57:00", "narrative": "Another day of long-lived widespread severe weather was observed on the South Plains of West Texas on the afternoon and evening of the 23rd. The first report of severe weather was received at 1518 CST with the final report at 2309 CST. A persistent long wave trough over the western United States remained in place with a dryline moving into the South Plains in the afternoon. Numerous thunderstorms developed east of the dryline and took advantage of strong shear and instability and rapidly became severe. Most reports consisted of large hail with the largest report of baseball size hail near Shallowater (Lubbock County). Despite the strong shear and low cloud bases, only one report was received of a tornado. A brief anticyclonic tornado was observed west of Brownfield (Terry County). Additionally, very heavy rainfall caused flooding in portions of the southwestern part of the city of Lubbock (Lubbock County). A member of the public submitted a picture that showed 2.25 inch diameter hail. No damage was reported.", "ts_dict_index": [6072, 6073, 6074]}
+{"event_id": 1140534, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:21:00", "end_date_time": "2023-09-24 20:21:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced four inch diameter hail in Round Rock. This storm was part of a complex that caused 700 million dollars in hail damage in Texas. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system and totaled upwards of 600 million dollars in damage across Williamson and Travis counties.  Thus 300 million dollars of damage is being listed on this Williamson County entry.  An article from the Austin American Statesman tells that Round Rock school district estimated losses of 70 million in damages to 62 facilities.", "ts_dict_index": [6087, 6088, 6089]}
+{"event_id": 1140472, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:03:00", "end_date_time": "2023-09-24 20:03:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail in Brushy Creek.", "ts_dict_index": [6105, 6106, 6107]}
+{"event_id": 1140463, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:58:00", "end_date_time": "2023-09-24 19:58:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced golf ball size hail at the intersection of E. Bowman Dr. and Sunrise Rd. in Round Rock.", "ts_dict_index": [6132, 6133, 6134]}
+{"event_id": 1140487, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:13:00", "end_date_time": "2023-09-24 20:13:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced golf ball size hail in Round Rock.", "ts_dict_index": [6102, 6103, 6104]}
+{"event_id": 1140451, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:50:00", "end_date_time": "2023-09-24 19:50:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced 2.25 inch diameter hail in Georgetown.", "ts_dict_index": [6075, 6076, 6077]}
+{"event_id": 1140408, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:39:00", "end_date_time": "2023-09-24 19:39:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail along Leander Rd. around 1/2 mile southwest of the Southwest Bypass in Georgetown.", "ts_dict_index": [6138, 6139, 6140]}
+{"event_id": 1140460, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:57:00", "end_date_time": "2023-09-24 19:57:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced 3.5 inch diameter hail in Round Rock. The hail dropped over a car dealership and broke windows and windshields.", "ts_dict_index": [6099, 6100, 6101]}
+{"event_id": 1140471, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:03:00", "end_date_time": "2023-09-24 20:03:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail at the intersection of FM 620 and O'Connor Dr. in Brushy Creek.", "ts_dict_index": [6123, 6124, 6125]}
+{"event_id": 1142710, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:55:00", "end_date_time": "2023-09-24 19:55:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced 3.5 inch diameter hail in Round Rock.", "ts_dict_index": [6117, 6118, 6119]}
+{"event_id": 823737, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-23 17:30:00", "end_date_time": "2019-05-23 17:35:00", "narrative": "Another day of long-lived widespread severe weather was observed on the South Plains of West Texas on the afternoon and evening of the 23rd. The first report of severe weather was received at 1518 CST with the final report at 2309 CST. A persistent long wave trough over the western United States remained in place with a dryline moving into the South Plains in the afternoon. Numerous thunderstorms developed east of the dryline and took advantage of strong shear and instability and rapidly became severe. Most reports consisted of large hail with the largest report of baseball size hail near Shallowater (Lubbock County). Despite the strong shear and low cloud bases, only one report was received of a tornado. A brief anticyclonic tornado was observed west of Brownfield (Terry County). Additionally, very heavy rainfall caused flooding in portions of the southwestern part of the city of Lubbock (Lubbock County). Several reports of penny size hail were received on the west side of the city of Lubbock. One report of quarter size hail was observed at 19th Street and Upland Ave.", "ts_dict_index": [6060, 6061, 6062]}
+{"event_id": 1140404, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:24:00", "end_date_time": "2023-09-24 19:24:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced nickel size hail in northern Georgetown.", "ts_dict_index": [6078, 6079, 6080]}
+{"event_id": 1140570, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:27:00", "end_date_time": "2023-09-24 20:27:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced 3.75 inch diameter hail in Round Rock.", "ts_dict_index": [6114, 6115, 6116]}
+{"event_id": 1140528, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:18:00", "end_date_time": "2023-09-24 20:18:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced two inch diameter hail at the intersection of CR 172 and TX 45 in Round Rock.", "ts_dict_index": [6084, 6085, 6086]}
+{"event_id": 1140452, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:50:00", "end_date_time": "2023-09-24 19:50:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced pea to golf ball size hail near the intersection of Sam Bass Rd. and Old Settlers Blvd. in Round Rock.", "ts_dict_index": [6129, 6130, 6131]}
+{"event_id": 822159, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 19:51:00", "end_date_time": "2019-05-16 19:51:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported hail larger than quarters and water covering the roads up to and over the curbs.", "ts_dict_index": [6057, 6058, 6059]}
+{"event_id": 822162, "event_type": "Hail", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 20:15:00", "end_date_time": "2019-05-16 20:15:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Public reported quarter sized hail, via picture on social media.", "ts_dict_index": [6051, 6052, 6053]}
+{"event_id": 1140488, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:13:00", "end_date_time": "2023-09-24 20:13:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail in Wells Branch.", "ts_dict_index": [6090, 6091, 6092]}
+{"event_id": 1140591, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:11:00", "end_date_time": "2023-09-24 21:11:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail in northeastern Austin.", "ts_dict_index": [6120, 6121, 6122]}
+{"event_id": 1140574, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:31:00", "end_date_time": "2023-09-24 20:31:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced hen egg size hail in northern Austin.", "ts_dict_index": [6081, 6082, 6083]}
+{"event_id": 1140593, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:17:00", "end_date_time": "2023-09-24 21:17:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced tennis ball size hail in central Austin.", "ts_dict_index": [6126, 6127, 6128]}
+{"event_id": 1140592, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:17:00", "end_date_time": "2023-09-24 21:17:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced tennis ball size hail in Austin.", "ts_dict_index": [6135, 6136, 6137]}
+{"event_id": 823739, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-23 18:07:00", "end_date_time": "2019-05-23 18:30:00", "narrative": "Another day of long-lived widespread severe weather was observed on the South Plains of West Texas on the afternoon and evening of the 23rd. The first report of severe weather was received at 1518 CST with the final report at 2309 CST. A persistent long wave trough over the western United States remained in place with a dryline moving into the South Plains in the afternoon. Numerous thunderstorms developed east of the dryline and took advantage of strong shear and instability and rapidly became severe. Most reports consisted of large hail with the largest report of baseball size hail near Shallowater (Lubbock County). Despite the strong shear and low cloud bases, only one report was received of a tornado. A brief anticyclonic tornado was observed west of Brownfield (Terry County). Additionally, very heavy rainfall caused flooding in portions of the southwestern part of the city of Lubbock (Lubbock County). Numerous reports were received of hail ranging from nickel size to golf ball size from south of Wolfforth to southwestern portions of the city of Lubbock. No damage was reported.", "ts_dict_index": [6063, 6064, 6065]}
+{"event_id": 1140575, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:35:00", "end_date_time": "2023-09-24 20:35:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail just west of Pflugerville.", "ts_dict_index": [6141, 6142, 6143]}
+{"event_id": 823743, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2019-05-23 18:58:00", "end_date_time": "2019-05-23 19:04:00", "narrative": "Another day of long-lived widespread severe weather was observed on the South Plains of West Texas on the afternoon and evening of the 23rd. The first report of severe weather was received at 1518 CST with the final report at 2309 CST. A persistent long wave trough over the western United States remained in place with a dryline moving into the South Plains in the afternoon. Numerous thunderstorms developed east of the dryline and took advantage of strong shear and instability and rapidly became severe. Most reports consisted of large hail with the largest report of baseball size hail near Shallowater (Lubbock County). Despite the strong shear and low cloud bases, only one report was received of a tornado. A brief anticyclonic tornado was observed west of Brownfield (Terry County). Additionally, very heavy rainfall caused flooding in portions of the southwestern part of the city of Lubbock (Lubbock County). An emergency management official and the Lubbock Fire Department reported hail ranging from quarter size to golf ball size between 19th and 50th Streets along Interstate 27.", "ts_dict_index": [6069, 6070, 6071]}
+{"event_id": 1140466, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:00:00", "end_date_time": "2023-09-24 20:00:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced three inch diameter hail near the intersection of TX 45 and I-35 in Round Rock.", "ts_dict_index": [6165, 6166, 6167]}
+{"event_id": 1140403, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 18:50:00", "end_date_time": "2023-09-24 18:50:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail at the intersection of Tomlinson St. and Patterson Ave. in Florence.", "ts_dict_index": [6168, 6169, 6170]}
+{"event_id": 1140411, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:44:00", "end_date_time": "2023-09-24 19:44:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced golf ball size hail in Serenada.", "ts_dict_index": [6159, 6160, 6161]}
+{"event_id": 1140450, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:49:00", "end_date_time": "2023-09-24 19:49:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail in Serenada.", "ts_dict_index": [6180, 6181, 6182]}
+{"event_id": 1140568, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:23:00", "end_date_time": "2023-09-24 20:23:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced two inch diameter hail in northern Austin.", "ts_dict_index": [6144, 6145, 6146]}
+{"event_id": 1140590, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:10:00", "end_date_time": "2023-09-24 21:10:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced two inch diameter hail in northeastern Austin.", "ts_dict_index": [6171, 6172, 6173]}
+{"event_id": 1140596, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:44:00", "end_date_time": "2023-09-24 21:44:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced hen egg size hail in the Mueller area of Austin.", "ts_dict_index": [6153, 6154, 6155]}
+{"event_id": 1140580, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:55:00", "end_date_time": "2023-09-24 20:55:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced three inch diameter hail on Burnet Ln. in the Brentwood area of Austin.  This storm was part of a complex that caused 700 million dollars in hail damage in Texas. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system and totaled upwards of 600 million dollars in damage across Williamson and Travis counties.  Thus 300 million dollars of damage is being listed on this Travis County entry.", "ts_dict_index": [6174, 6175, 6176]}
+{"event_id": 1140571, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:30:00", "end_date_time": "2023-09-24 20:30:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced half dollar size hail in the North Oaks area of Austin.", "ts_dict_index": [6147, 6148, 6149]}
+{"event_id": 1140586, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:07:00", "end_date_time": "2023-09-24 21:07:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced hail up to two inches in diameter near the intersection of Kirkwood Rd. and Wrightwood Rd. in northeastern Austin. The hail broke two house windows, cracked a car windshield, and dented the car.", "ts_dict_index": [6183, 6184, 6185]}
+{"event_id": 1140589, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:10:00", "end_date_time": "2023-09-24 21:10:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced tennis ball size hail in northeastern Austin.", "ts_dict_index": [6156, 6157, 6158]}
+{"event_id": 1140587, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:08:00", "end_date_time": "2023-09-24 21:08:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced golf ball size hail at the intersection of 38th St. and Duval St. in northern Austin.", "ts_dict_index": [6186, 6187, 6188]}
+{"event_id": 1140573, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:31:00", "end_date_time": "2023-09-24 20:31:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail in the North Oaks area of Austin.", "ts_dict_index": [6162, 6163, 6164]}
+{"event_id": 1140588, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:10:00", "end_date_time": "2023-09-24 21:10:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced 2.25 inches diameter hail in the Brentwood area of Austin.", "ts_dict_index": [6150, 6151, 6152]}
+{"event_id": 1140473, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:03:00", "end_date_time": "2023-09-24 20:03:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail in Round Rock.", "ts_dict_index": [6198, 6199, 6200]}
+{"event_id": 1140405, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:32:00", "end_date_time": "2023-09-24 19:32:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced dime to quarter size hail near the intersection of Serenada Dr. and Williams Dr. in Georgetown.", "ts_dict_index": [6195, 6196, 6197]}
+{"event_id": 1140512, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:15:00", "end_date_time": "2023-09-24 20:15:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced three inch diameter hail on Heather Dr. in Round Rock.", "ts_dict_index": [6201, 6202, 6203]}
+{"event_id": 1140409, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:43:00", "end_date_time": "2023-09-24 19:43:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail between Georgetown and Weir.", "ts_dict_index": [6207, 6208, 6209]}
+{"event_id": 1140594, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:19:00", "end_date_time": "2023-09-24 21:19:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced ping pong ball size hail in the Mueller area of Austin.", "ts_dict_index": [6189, 6190, 6191]}
+{"event_id": 1140533, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:20:00", "end_date_time": "2023-09-24 20:20:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced tea cup size hail in Pflugerville.", "ts_dict_index": [6192, 6193, 6194]}
+{"event_id": 1140576, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:40:00", "end_date_time": "2023-09-24 20:40:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced hail up to the size of golf balls near the intersection of N. Lamar Blvd. and Hwy 183 in northern Austin.", "ts_dict_index": [6204, 6205, 6206]}
+{"event_id": 1140519, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:16:00", "end_date_time": "2023-09-24 20:16:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail in Pflugerville.", "ts_dict_index": [6111, 6112, 6113]}
+{"event_id": 1140536, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:22:00", "end_date_time": "2023-09-24 20:22:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced ping pong ball size hail in northern Austin.", "ts_dict_index": [6210, 6211, 6212]}
+{"event_id": 1140412, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:45:00", "end_date_time": "2023-09-24 19:45:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced golf ball size hail in Georgetown.", "ts_dict_index": [6231, 6232, 6233]}
+{"event_id": 1140407, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:36:00", "end_date_time": "2023-09-24 19:36:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced penny size hail in Georgetown.", "ts_dict_index": [6228, 6229, 6230]}
+{"event_id": 1140532, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:20:00", "end_date_time": "2023-09-24 20:20:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced 2.25 inch diameter hail in Brushy Creek.", "ts_dict_index": [6216, 6217, 6218]}
+{"event_id": 1140406, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 19:35:00", "end_date_time": "2023-09-24 19:35:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced 2.5 inch diameter hail in western Georgetown.", "ts_dict_index": [6237, 6238, 6239]}
+{"event_id": 1140524, "event_type": "Hail", "state": "TEXAS", "cz_name": "WILLIAMSON", "begin_date_time": "2023-09-24 20:17:00", "end_date_time": "2023-09-24 20:17:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced hail up to the size of ping pong balls in Round Rock.", "ts_dict_index": [6225, 6226, 6227]}
+{"event_id": 1140584, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:03:00", "end_date_time": "2023-09-24 21:03:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced hail up to the size of quarters near the intersection of N. Lamar Blvd. and Hwy 183 in northern Austin.", "ts_dict_index": [6219, 6220, 6221]}
+{"event_id": 1140535, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:22:00", "end_date_time": "2023-09-24 20:22:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced ping pong size hail at Metric Blvd. and W. Braker Ln. in North Austin.", "ts_dict_index": [6234, 6235, 6236]}
+{"event_id": 879910, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-18 19:12:00", "end_date_time": "2020-04-18 19:12:00", "narrative": "A weak cold front moved south through the Ark-La-Tex to the Texas and Louisiana coasts on the morning of April 18th, although this front was shallow with its remnant elevated front stalling along the I-20 corridor of East Texas and North Louisiana. Elevated moisture return commenced during the afternoon hours atop this shallow post-frontal air mass, as weak shortwave energy ejected east northeast over the region ahead of an upper trough over the Four Corners Region. Ample instability aloft remained ahead of this approaching disturbance, with isolated to widely scattered showers and thunderstorms developing during the late afternoon and early evening hours. One of these storms briefly became severe, producing quarter size hail north of Cushing in Southern Rusk County. Additional scattered showers and thunderstorms developed overnight ahead of a northward moving warm front, but these remained sub-severe. Nickel to quarter size hail fell at a Plant Nursery north of Cushing off of Highway 84.", "ts_dict_index": [6240, 6241, 6242]}
+{"event_id": 1140582, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:00:00", "end_date_time": "2023-09-24 21:00:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced golf ball size hail on Lamar Blvd. in Austin.", "ts_dict_index": [6213, 6214, 6215]}
+{"event_id": 1140595, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 21:29:00", "end_date_time": "2023-09-24 21:29:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced tennis ball size hail in the Brentwood area of Austin.", "ts_dict_index": [6093, 6094, 6095]}
+{"event_id": 873741, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2020-03-18 16:29:00", "end_date_time": "2020-03-18 16:54:00", "narrative": "Several consecutive days of southwesterly flow aloft were capped off by a final day of severe convection on the 18th. A short wave moved from southwest to northeast over the region ahead of a large upper level low off the southern California coast. Strong low level moisture was present in the region which created a very unstable atmosphere. Although convection was fairly unorganized, a few strong updrafts were able to generate very large hail. One of these thunderstorms developed over the southwestern portion of Lubbock County and tracked through Wolfforth (Lubbock County) and western portions of the city of Lubbock (Lubbock County). A swath of severe hail was reported through this track with a maximum hail size of 2.25 inches. A second severe thunderstorm tracked from the southeastern side of Childress (Childress County) northward up US Highway 83. This storm produced hail up to golf ball size. Numerous reports of hail from off-duty NWS employees and social media were received as a severe thunderstorm tracked from south of Wolfforth to western Lubbock. Hail ranged in size from quarters to one report of tennis ball size. No damage was reported.", "ts_dict_index": [6249, 6250, 6251]}
+{"event_id": 1109867, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-13 18:29:00", "end_date_time": "2023-06-13 18:29:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds and isolated tornadoes slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across North Louisiana. Quarter size hail reported at a gas station in Mira.", "ts_dict_index": [6255, 6256, 6257]}
+{"event_id": 960227, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2021-07-06 16:00:00", "end_date_time": "2021-07-06 16:04:00", "narrative": "The area of high pressure that had been centered over the Four Corners shifted slightly westward on July 6, 2021. Meanwhile, low level return flow continued which aided in keeping moisture values high across New Mexico. With sufficient instability and shear, another crop of thunderstorms developed first across the high terrain before becoming more widespread across lower elevations. With numerous days of widespread thunderstorms and heavy rainfall, soils across northern and central New Mexico were saturated and primed for more flash flooding. Numerous flash floods were reported across the area with the most significant flash flooding occurring in the Belen area and farther south into Socorro County. Several inches of rainfall breached a canal in Belen which flooded low-water crossings as well as numerous homes and businesses. A State of Emergency was declared in Valencia County due to the flooding. A COOP observer near Tucumcari reported nickel size hail from a strong thunderstorm tracking southwestward through the area.", "ts_dict_index": [6246, 6247, 6248]}
+{"event_id": 1114377, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2023-07-22 15:28:00", "end_date_time": "2023-07-22 15:28:00", "narrative": "Nebraska was on the backside of an upper trough. A weak shortwave trough moved over the Central Plains and resulted in an increase in atmospheric lift. Most unstable CAPE was around 3,000 J/kg and effective bulk shear was around 35 knots. Mid-level lapse rates were around 7 degrees C/km. Temperatures were between 85 and 90 degrees across south central Nebraska. Dewpoint temperatures were between 60 and 65 degrees. ||A storm strengthened over Gosper County and moved into Furnas County and produced nickel sized hail at 2:44 PM CDT. This storm went on to produce two inch hail in Furnas County. Additional storms developed across south central Nebraska and produced large hail during the afternoon and early evening hours of July 22nd. The largest hail of 2.50 inches occurred in Buffalo and Phelps Counties. The storms ended by producing nickel size hail in Clay County at 6:40 PM CDT. ", "ts_dict_index": [6261, 6262, 6263]}
+{"event_id": 873742, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2020-03-18 17:20:00", "end_date_time": "2020-03-18 17:20:00", "narrative": "Several consecutive days of southwesterly flow aloft were capped off by a final day of severe convection on the 18th. A short wave moved from southwest to northeast over the region ahead of a large upper level low off the southern California coast. Strong low level moisture was present in the region which created a very unstable atmosphere. Although convection was fairly unorganized, a few strong updrafts were able to generate very large hail. One of these thunderstorms developed over the southwestern portion of Lubbock County and tracked through Wolfforth (Lubbock County) and western portions of the city of Lubbock (Lubbock County). A swath of severe hail was reported through this track with a maximum hail size of 2.25 inches. A second severe thunderstorm tracked from the southeastern side of Childress (Childress County) northward up US Highway 83. This storm produced hail up to golf ball size. A picture on social media depicted half dollar size hail along US Highway 62/82 northeast of Wolfforth. No damage was reported.", "ts_dict_index": [6252, 6253, 6254]}
+{"event_id": 990845, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2021-12-10 22:45:00", "end_date_time": "2021-12-10 22:45:00", "narrative": "A strong upper trough advanced east out of the Rockies and into the Central and Southern Plains during the afternoon and evening of December 10th, which reinforced a strong cold front southeast into the Ozarks and Southern Plains. An expansive area of very warm and moist air had spread north into all of the Four State Region into Southeast Oklahoma and Central Arkansas, with afternoon heating contributing to moderate instability within a strongly sheared air mass. Scattered strong to severe thunderstorms developed during the evening over portions of Northeast Texas and Southwest Arkansas ahead of the approaching cold front, before organizing into a narrow squall line and shifting southeast into North Louisiana during the late evening and early morning hours on the 11th. These storms produced reports of large hail and damaging winds across portions of Northeast Texas before exiting into North Louisiana. Numerous reports of quarter size hail fell across the northwest sections of Texarkana.", "ts_dict_index": [6243, 6244, 6245]}
+{"event_id": 1015815, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2022-05-01 16:45:00", "end_date_time": "2022-05-01 16:45:00", "narrative": "Moisture quickly returned to West Texas during the day on the first ahead of an approaching upper level short wave. In response, scattered thunderstorms rapidly developed late Sunday afternoon. Relatively strong wind shear and moderate instability spurred several of the storms to rotate and produce very large hail. The configuration of the increasing and turning winds with height were right to favor splitting supercell storms. The left splits raced north-northeastward bringing brief heavy rain, large hail, and sporadic wind gusts. Golf ball to baseball size hail fell from the strongest of these northward-racing storms. Western portions of Levelland experienced extensive damage, primarily from shattered glass. The right splits moved slowly to the east, producing locally heavy rains. These storms also dropped huge hail with one greater than baseball size near O'Donnell (Lynn County). A member of the public sent a picture of quarter size hail at the intersection of Erskine Street and Dover Avenue in Lubbock.", "ts_dict_index": [6258, 6259, 6260]}
+{"event_id": 1114375, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2023-07-22 15:00:00", "end_date_time": "2023-07-22 15:00:00", "narrative": "Nebraska was on the backside of an upper trough. A weak shortwave trough moved over the Central Plains and resulted in an increase in atmospheric lift. Most unstable CAPE was around 3,000 J/kg and effective bulk shear was around 35 knots. Mid-level lapse rates were around 7 degrees C/km. Temperatures were between 85 and 90 degrees across south central Nebraska. Dewpoint temperatures were between 60 and 65 degrees. ||A storm strengthened over Gosper County and moved into Furnas County and produced nickel sized hail at 2:44 PM CDT. This storm went on to produce two inch hail in Furnas County. Additional storms developed across south central Nebraska and produced large hail during the afternoon and early evening hours of July 22nd. The largest hail of 2.50 inches occurred in Buffalo and Phelps Counties. The storms ended by producing nickel size hail in Clay County at 6:40 PM CDT. Most hail was nickel to golf ball size, with a few up to the size of tennis balls.", "ts_dict_index": [6267, 6268, 6269]}
+{"event_id": 1114367, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2023-07-22 14:17:00", "end_date_time": "2023-07-22 14:20:00", "narrative": "Nebraska was on the backside of an upper trough. A weak shortwave trough moved over the Central Plains and resulted in an increase in atmospheric lift. Most unstable CAPE was around 3,000 J/kg and effective bulk shear was around 35 knots. Mid-level lapse rates were around 7 degrees C/km. Temperatures were between 85 and 90 degrees across south central Nebraska. Dewpoint temperatures were between 60 and 65 degrees. ||A storm strengthened over Gosper County and moved into Furnas County and produced nickel sized hail at 2:44 PM CDT. This storm went on to produce two inch hail in Furnas County. Additional storms developed across south central Nebraska and produced large hail during the afternoon and early evening hours of July 22nd. The largest hail of 2.50 inches occurred in Buffalo and Phelps Counties. The storms ended by producing nickel size hail in Clay County at 6:40 PM CDT. Hail up to the size of quarters was reported in Beaver City.", "ts_dict_index": [6264, 6265, 6266]}
+{"event_id": 1114362, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2023-07-22 13:50:00", "end_date_time": "2023-07-22 14:05:00", "narrative": "Nebraska was on the backside of an upper trough. A weak shortwave trough moved over the Central Plains and resulted in an increase in atmospheric lift. Most unstable CAPE was around 3,000 J/kg and effective bulk shear was around 35 knots. Mid-level lapse rates were around 7 degrees C/km. Temperatures were between 85 and 90 degrees across south central Nebraska. Dewpoint temperatures were between 60 and 65 degrees. ||A storm strengthened over Gosper County and moved into Furnas County and produced nickel sized hail at 2:44 PM CDT. This storm went on to produce two inch hail in Furnas County. Additional storms developed across south central Nebraska and produced large hail during the afternoon and early evening hours of July 22nd. The largest hail of 2.50 inches occurred in Buffalo and Phelps Counties. The storms ended by producing nickel size hail in Clay County at 6:40 PM CDT. Hail up to two inches in diameter was reported in the area, with hail covering part of Highway 283 south of Arapahoe.", "ts_dict_index": [6270, 6271, 6272]}
+{"event_id": 1109888, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 15:00:00", "end_date_time": "2023-06-13 15:00:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Tennis ball size hail reported via social media in the Swan community.", "ts_dict_index": [6276, 6277, 6278]}
+{"event_id": 1109881, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2023-06-13 12:57:00", "end_date_time": "2023-06-13 12:57:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Half dollar size hail reported via mPING.", "ts_dict_index": [6297, 6298, 6299]}
+{"event_id": 1109892, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 15:50:00", "end_date_time": "2023-06-13 15:50:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Ping pong ball size hail reported on the southeast side of Tyler.", "ts_dict_index": [6279, 6280, 6281]}
+{"event_id": 1109883, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 14:47:00", "end_date_time": "2023-06-13 14:47:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Hen egg size hail reported via social media along Interstate 20 in western Smith County.", "ts_dict_index": [6282, 6283, 6284]}
+{"event_id": 1109890, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 15:15:00", "end_date_time": "2023-06-13 15:15:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Golf ball size hail reported via social media along Highway 64 between the Bascom and Chapel Hill communities.", "ts_dict_index": [6288, 6289, 6290]}
+{"event_id": 1109887, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 15:18:00", "end_date_time": "2023-06-13 15:18:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Golf ball size hail reported 7 miles northeast of Tyler.", "ts_dict_index": [6291, 6292, 6293]}
+{"event_id": 1109895, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 14:52:00", "end_date_time": "2023-06-13 14:52:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Half dollar size hail reported along Highway 110 in far western Smith County.", "ts_dict_index": [6294, 6295, 6296]}
+{"event_id": 1109882, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 13:41:00", "end_date_time": "2023-06-13 13:41:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Hail slightly larger than hen egg size reported via social media along Highway 69 between Lindale and Mineola.", "ts_dict_index": [6285, 6286, 6287]}
+{"event_id": 1109891, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-13 15:45:00", "end_date_time": "2023-06-13 15:45:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Quarter size hail reported at FM Road 850 and U.S. Highway 259.", "ts_dict_index": [6273, 6274, 6275]}
+{"event_id": 1140579, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:50:00", "end_date_time": "2023-09-24 20:50:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced 2.25 inch diameter hail near Hyde Park in Austin.", "ts_dict_index": [6222, 6223, 6224]}
+{"event_id": 1109894, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 15:15:00", "end_date_time": "2023-06-13 15:15:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Ping pong ball size hail reported along Highway 271 northeast of Tyler.", "ts_dict_index": [6303, 6304, 6305]}
+{"event_id": 1109889, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 15:07:00", "end_date_time": "2023-06-13 15:07:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Baseball size hail reported via social media 6 miles northeast of Tyler.", "ts_dict_index": [6300, 6301, 6302]}
+{"event_id": 1109898, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 16:05:00", "end_date_time": "2023-06-13 16:05:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Hail up to quarter size reported along Old Jacksonville Highway just inside the loop south of Tyler.", "ts_dict_index": [6306, 6307, 6308]}
+{"event_id": 1109897, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-13 15:45:00", "end_date_time": "2023-06-13 15:45:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Tennis ball size hail reported along Highway 259 near Pyrtle.", "ts_dict_index": [6315, 6316, 6317]}
+{"event_id": 1107848, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-13 15:51:00", "end_date_time": "2023-06-13 15:51:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds and isolated tornadoes slightly lower on the threat scale. Numerous local storm reports of large hail were documented throughout the event across Southeast Oklahoma. Hen egg size hail reported along Highway 259.", "ts_dict_index": [6318, 6319, 6320]}
+{"event_id": 1109899, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-13 16:50:00", "end_date_time": "2023-06-13 16:50:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Baseball size hail reported at Henderson High School.", "ts_dict_index": [6309, 6310, 6311]}
+{"event_id": 1107851, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-13 16:18:00", "end_date_time": "2023-06-13 16:18:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds and isolated tornadoes slightly lower on the threat scale. Numerous local storm reports of large hail were documented throughout the event across Southeast Oklahoma. Quarter size hail reported just east of Idabel.", "ts_dict_index": [6321, 6322, 6323]}
+{"event_id": 1140581, "event_type": "Hail", "state": "TEXAS", "cz_name": "TRAVIS", "begin_date_time": "2023-09-24 20:57:00", "end_date_time": "2023-09-24 20:57:00", "narrative": "Thunderstorms developed along a cold front as it moved southward through South Central Texas. Some of these storms produced large hail and damaging wind gusts. One supercell produced giant hail that caused considerable damage from Georgetown to Austin. This storm was part of a complex that caused $1.3 billion in hail damage in Texas, Oklahoma, and Missouri. The damage in Austin, Georgetown, and Round Rock was the most impactful from this system. Estimates from NCEI indicate that 700 million dollars in damages occurred in Texas from these storms.  It is being estimated that 300 million dollars of damage occurred in Travis County and 300 million dollars of damage occurred in Williamson County since a county breakdown of damage is not given to NCEI and is not given by insurance companies. Austin American Statesman tells that Round Rock School District estimates 70 million dollars in damages to 62 facilities. A thunderstorm produced quarter size hail in northern Austin.", "ts_dict_index": [6177, 6178, 6179]}
+{"event_id": 1090206, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2023-03-31 14:48:00", "end_date_time": "2023-03-31 14:48:00", "narrative": "Elevated convection initially developed early in the day on March 31st within a plume of rich low-level moisture and along the periphery of a lead shortwave moving across the Southern Plains. By early afternoon, more widespread severe convection developed and expanded farther along an eastward advancing dryline and associated cold front from Northeast Texas into Southeast Oklahoma and eventually Southwest Arkansas into Northern Louisiana. Strong surface heating within a moist low-level environment resulted in MLCAPE values of 1500-2500 J/kg across the region along with deep layer shear of 50-70 knots, more than sufficient for organized thunderstorms. In this type environment, strong large-scale ascent also promoted some supercell thunderstorms as well with numerous reports of large hail and damaging wind gusts across East Texas during the afternoon and evening hours. Penny size hail reported in the Dalby Springs community.", "ts_dict_index": [6351, 6352, 6353]}
+{"event_id": 1056607, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2022-09-25 15:27:00", "end_date_time": "2022-09-25 15:27:00", "narrative": "Northwesterly flow aloft aided in pushing a cold front southward into the region on the afternoon of September 25th. Despite only weak upper-level support, frontal forcing was sufficient to generate scattered convection along the frontal boundary during the afternoon. The atmosphere was relatively uncapped, and with afternoon temperatures climbing into the mid 90s, moderate surface-based instability developed. However, a lack of deep layer moisture appeared to be a limiting factor for any severe weather although classic inverted-V forecast soundings indicated the potential for isolated damaging wind gusts from thunderstorm downbursts in the afternoon. Moisture proved to be sufficient for storms to rapidly develop by mid to late afternoon, quickly accelerating southward and producing sporadic damaging wind gusts and large hail across parts of Bowie County Texas. Social media photo showed half dollar sized hail near the intersection of US Highway 59 and FM 2148.", "ts_dict_index": [6354, 6355, 6356]}
+{"event_id": 1090208, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-03-31 15:11:00", "end_date_time": "2023-03-31 15:11:00", "narrative": "Elevated convection initially developed early in the day on March 31st within a plume of rich low-level moisture and along the periphery of a lead shortwave moving across the Southern Plains. By early afternoon, more widespread severe convection developed and expanded farther along an eastward advancing dryline and associated cold front from Northeast Texas into Southeast Oklahoma and eventually Southwest Arkansas into Northern Louisiana. Strong surface heating within a moist low-level environment resulted in MLCAPE values of 1500-2500 J/kg across the region along with deep layer shear of 50-70 knots, more than sufficient for organized thunderstorms. In this type environment, strong large-scale ascent also promoted some supercell thunderstorms as well with numerous reports of large hail and damaging wind gusts across East Texas during the afternoon and evening hours. Penny size hail reported south of Tyler via m-PING.", "ts_dict_index": [6348, 6349, 6350]}
+{"event_id": 1090207, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-03-31 15:07:00", "end_date_time": "2023-03-31 15:07:00", "narrative": "Elevated convection initially developed early in the day on March 31st within a plume of rich low-level moisture and along the periphery of a lead shortwave moving across the Southern Plains. By early afternoon, more widespread severe convection developed and expanded farther along an eastward advancing dryline and associated cold front from Northeast Texas into Southeast Oklahoma and eventually Southwest Arkansas into Northern Louisiana. Strong surface heating within a moist low-level environment resulted in MLCAPE values of 1500-2500 J/kg across the region along with deep layer shear of 50-70 knots, more than sufficient for organized thunderstorms. In this type environment, strong large-scale ascent also promoted some supercell thunderstorms as well with numerous reports of large hail and damaging wind gusts across East Texas during the afternoon and evening hours. Hail up to penny size reported on Paluxy Drive in south Tyler.", "ts_dict_index": [6345, 6346, 6347]}
+{"event_id": 1056606, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2022-09-25 15:15:00", "end_date_time": "2022-09-25 15:15:00", "narrative": "Northwesterly flow aloft aided in pushing a cold front southward into the region on the afternoon of September 25th. Despite only weak upper-level support, frontal forcing was sufficient to generate scattered convection along the frontal boundary during the afternoon. The atmosphere was relatively uncapped, and with afternoon temperatures climbing into the mid 90s, moderate surface-based instability developed. However, a lack of deep layer moisture appeared to be a limiting factor for any severe weather although classic inverted-V forecast soundings indicated the potential for isolated damaging wind gusts from thunderstorm downbursts in the afternoon. Moisture proved to be sufficient for storms to rapidly develop by mid to late afternoon, quickly accelerating southward and producing sporadic damaging wind gusts and large hail across parts of Bowie County Texas. Social media pictures showed quarter to half dollar sized hail near Texarkana in the Liberty Eylau area.", "ts_dict_index": [6357, 6358, 6359]}
+{"event_id": 949521, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2021-05-15 15:15:00", "end_date_time": "2021-05-15 15:20:00", "narrative": "Surface southeasterly flow continued over eastern New Mexico which trended moisture upward across the area. With another day of warming temperatures and an unstable atmosphere, strong to severe thunderstorms once again impacted the eastern plains of New Mexico on May 15, 2021. By early afternoon, thunderstorms developed along the northern and southern high terrain of New Mexico. As they tracked eastward onto lower elevations, they moved into a more unstable and sheared environment where they quickly intensified. The most significant damage occurred in Portales where hail up to the size of half dollars was reported. Additionally, the general slow movement of these thunderstorms near the New Mexico and Texas state line resulted in heavy rainfall and flash flooding in Portales. A water rescue was conducted for a family who attempted to drive through the flooded roadways. A CoCoRaHS observer reported penny size hail from a strong thunderstorm east-southeast of Tucumcari.", "ts_dict_index": [6336, 6337, 6338]}
+{"event_id": 1107849, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-13 15:55:00", "end_date_time": "2023-06-13 15:55:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds and isolated tornadoes slightly lower on the threat scale. Numerous local storm reports of large hail were documented throughout the event across Southeast Oklahoma. Tennis ball size hail reported in the Tom community.", "ts_dict_index": [6324, 6325, 6326]}
+{"event_id": 1107852, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-13 20:51:00", "end_date_time": "2023-06-13 20:51:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds and isolated tornadoes slightly lower on the threat scale. Numerous local storm reports of large hail were documented throughout the event across Southeast Oklahoma. Quarter size hail reported in Garvin.", "ts_dict_index": [6330, 6331, 6332]}
+{"event_id": 1090179, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-31 13:46:00", "end_date_time": "2023-03-31 13:46:00", "narrative": "Elevated convection initially developed early in the day on March 31st within a plume of rich low-level moisture and along the periphery of a lead shortwave moving across the Southern Plains. By early afternoon, more widespread severe convection developed and expanded farther along an eastward advancing dryline and associated cold front from Northeast Texas into Southeast Oklahoma and eventually Southwest Arkansas into Northern Louisiana. Strong surface heating within a moist low-level environment resulted in MLCAPE values of 1500-2500 J/kg across the region along with deep layer shear of 50-70 knots, more than sufficient for organized thunderstorms. In this type environment, strong large-scale ascent also promoted isolated supercell thunderstorms across portions of McCurtain County Oklahoma which produced isolated instances of  large hail during the afternoon hours. Hail up to nickel size reported just west of Idabel.", "ts_dict_index": [6339, 6340, 6341]}
+{"event_id": 1090178, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-31 13:24:00", "end_date_time": "2023-03-31 13:24:00", "narrative": "Elevated convection initially developed early in the day on March 31st within a plume of rich low-level moisture and along the periphery of a lead shortwave moving across the Southern Plains. By early afternoon, more widespread severe convection developed and expanded farther along an eastward advancing dryline and associated cold front from Northeast Texas into Southeast Oklahoma and eventually Southwest Arkansas into Northern Louisiana. Strong surface heating within a moist low-level environment resulted in MLCAPE values of 1500-2500 J/kg across the region along with deep layer shear of 50-70 knots, more than sufficient for organized thunderstorms. In this type environment, strong large-scale ascent also promoted isolated supercell thunderstorms across portions of McCurtain County Oklahoma which produced isolated instances of  large hail during the afternoon hours. Quarter size hail reported near and just east of Battiest.", "ts_dict_index": [6342, 6343, 6344]}
+{"event_id": 1107850, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-13 15:55:00", "end_date_time": "2023-06-13 15:55:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds and isolated tornadoes slightly lower on the threat scale. Numerous local storm reports of large hail were documented throughout the event across Southeast Oklahoma. Ping pong ball size hail reported near the intersection of Pleasant Hill Road and Red Slough Road.", "ts_dict_index": [6333, 6334, 6335]}
+{"event_id": 1109885, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-13 15:21:00", "end_date_time": "2023-06-13 15:21:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds slightly lower on the threat scale. Numerous local storm reports of large hail and damaging winds were documented throughout the event across East and Northeast Texas. Golf ball size hail northwest of Lindale along Highway 69.", "ts_dict_index": [6312, 6313, 6314]}
+{"event_id": 1081341, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2023-04-09 17:15:00", "end_date_time": "2023-04-09 17:34:00", "narrative": "Easter Sunday brought severe thunderstorms to the region during the late afternoon into the early evening. The initial thunderstorm development was concentrated along several low-level boundaries stretching across the southern Texas Panhandle and northern South and Rolling Plains. The storms were fueled by just enough moisture and instability, that when coupled with cold air and a weak disturbance aloft, several of the storms became strong to severe. Given the relatively dry, warm, and deeply mixed lower levels of the atmosphere, favorable for significant sub-cloud evaporation, the activity generated several strong wind gusts with a few exceeding severe thresholds. Most of these thunderstorms brought copious amount of hail. Although most of the hail was sub-severe, a few of the storms produced hail accumulations, covering the ground several inches deep or more. A swath of severe hail was observed beginning northwest of Shallowater and continuing through western and southern portions of the city of Lubbock. Most hail ranged from dime to quarter size but hail up to half dollar size was reported. Additionally, copious amount of hail fell with this storm covering the ground in and around Shallowater. Area roadways became ice covered and made it look like snowfall. In some spots the hail didn't completely melt off until the next morning.", "ts_dict_index": [6360, 6361, 6362]}
+{"event_id": 949003, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-05-10 14:37:00", "end_date_time": "2021-05-10 14:37:00", "narrative": "A shallow cold front settled south into portions of Southeast Texas and Central Louisiana by the morning hours of May 10th, although a weak shortwave trough traversed east across the Red River Valley of Southern Oklahoma and North Texas, enhancing scattered shower and thunderstorm development over this area. Steep lapse rates aloft contributed to adequate instability such that some of these storms become severe, as they tracked southeast into Northeast Texas and Northwest Louisiana during the afternoon. These storms remained elevated across much of these areas, producing large hail before becoming more surface based across portions of Northwest Louisiana, where damaging winds were the more dominant mode. Numerous trees were uprooted in Red River Parish before the storms weakened as they moved away from the area of best forcing and instability aloft. Nickel size hail fell about 2.5 miles south of the Shreveport Regional Airport off of Walker Road. Report from retired NWS employee.", "ts_dict_index": [6387, 6388, 6389]}
+{"event_id": 946755, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-04-09 13:13:00", "end_date_time": "2021-04-09 13:13:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across North Louisiana. These storms finally exited North Louisiana during the early morning hours of April 10th with the passage of the cold front. Penny size hail fell several miles northeast of Blanchard. Report from mPING.", "ts_dict_index": [6369, 6370, 6371]}
+{"event_id": 949002, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-05-10 13:50:00", "end_date_time": "2021-05-10 13:50:00", "narrative": "A shallow cold front settled south into portions of Southeast Texas and Central Louisiana by the morning hours of May 10th, although a weak shortwave trough traversed east across the Red River Valley of Southern Oklahoma and North Texas, enhancing scattered shower and thunderstorm development over this area. Steep lapse rates aloft contributed to adequate instability such that some of these storms become severe, as they tracked southeast into Northeast Texas and Northwest Louisiana during the afternoon. These storms remained elevated across much of these areas, producing large hail before becoming more surface based across portions of Northwest Louisiana, where damaging winds were the more dominant mode. Numerous trees were uprooted in Red River Parish before the storms weakened as they moved away from the area of best forcing and instability aloft. Quarter size hail fell in Vivian.", "ts_dict_index": [6393, 6394, 6395]}
+{"event_id": 1051950, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "FURNAS", "begin_date_time": "2022-09-15 17:03:00", "end_date_time": "2022-09-15 17:03:00", "narrative": "Marginally-severe thunderstorms affected Gosper and Furnas counties during the evening hours of September 15th. A weak upper level shortwave along with a surface trough combined with moderate instability and abundant moisture to spark off clusters of thunderstorms during the late afternoon and early evening hours. The strongest storms impacted portions of Gosper and Furnas Counties between 6-8 PM CDT, with localized instances of penny to nickel size hail reported. A lone severe wind gust of 65 MPH was also reported. While instability was moderate and moisture was plentiful, weak deep layer wind shear of only 20 knots or less likely precluded a greater, or more widespread, severe weather threat. Scattered to widespread showers and thunderstorms continued well into the late evening hours, but thunderstorm intensity greatly decreased with loss of daytime heating. ", "ts_dict_index": [6363, 6364, 6365]}
+{"event_id": 1084762, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-04-02 17:00:00", "end_date_time": "2023-04-02 17:00:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Nickle size hail fell on the west side of Lindale.", "ts_dict_index": [6372, 6373, 6374]}
+{"event_id": 1084955, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-02 21:10:00", "end_date_time": "2023-04-02 21:10:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Penny size hail fell on Woodlake Drive just southeast of Benton.", "ts_dict_index": [6375, 6376, 6377]}
+{"event_id": 949005, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-05-10 14:50:00", "end_date_time": "2021-05-10 14:50:00", "narrative": "A shallow cold front settled south into portions of Southeast Texas and Central Louisiana by the morning hours of May 10th, although a weak shortwave trough traversed east across the Red River Valley of Southern Oklahoma and North Texas, enhancing scattered shower and thunderstorm development over this area. Steep lapse rates aloft contributed to adequate instability such that some of these storms become severe, as they tracked southeast into Northeast Texas and Northwest Louisiana during the afternoon. These storms remained elevated across much of these areas, producing large hail before becoming more surface based across portions of Northwest Louisiana, where damaging winds were the more dominant mode. Numerous trees were uprooted in Red River Parish before the storms weakened as they moved away from the area of best forcing and instability aloft. Quarter size hail fell in the Ellerbe Road Estates. Report from retired NWS employee.", "ts_dict_index": [6384, 6385, 6386]}
+{"event_id": 949009, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-05-10 14:44:00", "end_date_time": "2021-05-10 14:44:00", "narrative": "A shallow cold front settled south into portions of Southeast Texas and Central Louisiana by the morning hours of May 10th, although a weak shortwave trough traversed east across the Red River Valley of Southern Oklahoma and North Texas, enhancing scattered shower and thunderstorm development over this area. Steep lapse rates aloft contributed to adequate instability such that some of these storms become severe, as they tracked southeast into Northeast Texas and Northwest Louisiana during the afternoon. These storms remained elevated across much of these areas, producing large hail before becoming more surface based across portions of Northwest Louisiana, where damaging winds were the more dominant mode. Numerous trees were uprooted in Red River Parish before the storms weakened as they moved away from the area of best forcing and instability aloft. Quarter size hail fell in South Bossier off of Barksdale Blvd.", "ts_dict_index": [6390, 6391, 6392]}
+{"event_id": 1090163, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-03-26 13:54:00", "end_date_time": "2023-03-26 13:54:00", "narrative": "A shortwave trough moving across Central Texas on the morning of March 26th made its way into Ark-La-Tex region by the afternoon. Meanwhile, a surface warm front was lifting back northward from the coast, providing the leading edge of near 70 degree dewpoints and ample surface-based instability. Strengthening southeasterly low-level winds ahead of the upper trough, combined with the favorable thermodynamic environment, resulted in the potential for supercell thunderstorms capable of large hail and damaging winds across much of the Ark-La-Tex. By early in the afternoon, increasing lift and moisture associated with these synoptic features led to scattered thunderstorm development with a cluster of supercells resulting in numerous reports of severe hail and damaging wind gusts across North Louisiana, but more isolated across East Texas and Southwest Arkansas. Quarter size hail reported in Many.", "ts_dict_index": [6378, 6379, 6380]}
+{"event_id": 1107853, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-13 21:07:00", "end_date_time": "2023-06-13 21:07:00", "narrative": "A nearly stationary frontal boundary maintained a focus for widespread severe weather across Southeast Oklahoma into the Ark-La-Tex region throughout the day on June 13th. Northwesterly flow aloft, ahead of an upper trough over the Great Lakes, combined with this stalled frontal boundary to funnel a series of embedded shortwave disturbances across the entire region. This included one strong shortwave in particular that maintained the threat of severe thunderstorms throughout most of the afternoon and evening hours, producing multiple rounds of thunderstorms. With ample ingredients for severe weather, including mid-level lapse rates near 7-8C/km or greater, large hail was the primary threat with damaging winds and isolated tornadoes slightly lower on the threat scale. Numerous local storm reports of large hail were documented throughout the event across Southeast Oklahoma. Quarter size hail reported in Broken Bow.", "ts_dict_index": [6327, 6328, 6329]}
+{"event_id": 1110867, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-14 17:29:00", "end_date_time": "2023-06-14 17:29:00", "narrative": "Supercell thunderstorms developed toward midday across the middle Red River Valley along and south of a stalled frontal boundary. These thunderstorms progressed east southeast with upper 80s temperatures on the warm side of the boundary with dew points exceeding 75 degrees. Mid-level lapse rates of 7-8 C/km overspread this very moist low-level air mass over a rather broad west-to-east corridor, supporting extreme instability upwards of 4500 J/kg well downstream of the upscale-growing convection. Coinciding this corridor of extreme buoyancy was very strong effective bulk shear near 65 kts along with hodographs that were modestly curved at the low levels and elongated above 3 km AGL. Numerous local storm reports were documented of large hail, damaging wind gusts, and an isolated tornado across parts of East and Northeast Texas throughout the event. Quarter size hail reported near Hideaway via social media.", "ts_dict_index": [6405, 6406, 6407]}
+{"event_id": 1111836, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2023-07-11 23:04:00", "end_date_time": "2023-07-11 23:10:00", "narrative": "West to northwest upper winds were across south central and central Nebraska. There was a shortwave disturbance along the Montana and Canada border that moved east. A surface low was across the High Plains with a warm frontal boundary that extended east across northern Nebraska. Deep layer wind shear was around 40+ knots and mid-level lapse rates were between 7 and 8 degrees C/km. Most unstable CAPE was between 2,000 to 3,000 J/kg and dewpoints were generally in the upper 60s. ||In the late evening hours of July 11th, a supercell storm moved southeast from central Nebraska. This storm started off by producing 1.50 inch hail in Sherman County around 11:30 PM CDT and went on to produce baseball sized hail in both Sherman and Buffalo Counties. The last hail report occurred just after midnight. The baseball size hail resulted in damage to vehicles. Golf ball to baseball size hail was reported in the area. One spotter reported a broken windshield.", "ts_dict_index": [6417, 6418, 6419]}
+{"event_id": 884512, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2020-05-13 18:16:00", "end_date_time": "2020-05-13 18:16:00", "narrative": "A very moist and unstable atmosphere developed on the 13th ahead of an approaching upper level short wave. Virga showers had developed out ahead of this upper level feature during the morning and early afternoon. This caused a severe wind gust to 65 mph from a heat burst at the Texas Tech University West Texas mesonet site near Graham (Garza County). When thunderstorms developed in the late afternoon, the initial activity was somewhat disorganized. But these initial storms were intense enough to produce pockets of hail as large as ping pong ball size. Eventually the scattered thunderstorms amalgamated into a line and accelerated eastward through the Rolling Plains and into western North Texas during the late evening hours. Several reports of small hail, strong to severe wind gusts and very heavy rainfall were received as the line moved through. Numerous reports were received of hail ranging in size from quarters to ping pong balls in the southwestern portion of the city of Lubbock.", "ts_dict_index": [6420, 6421, 6422]}
+{"event_id": 949004, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-05-10 14:43:00", "end_date_time": "2021-05-10 14:43:00", "narrative": "A shallow cold front settled south into portions of Southeast Texas and Central Louisiana by the morning hours of May 10th, although a weak shortwave trough traversed east across the Red River Valley of Southern Oklahoma and North Texas, enhancing scattered shower and thunderstorm development over this area. Steep lapse rates aloft contributed to adequate instability such that some of these storms become severe, as they tracked southeast into Northeast Texas and Northwest Louisiana during the afternoon. These storms remained elevated across much of these areas, producing large hail before becoming more surface based across portions of Northwest Louisiana, where damaging winds were the more dominant mode. Numerous trees were uprooted in Red River Parish before the storms weakened as they moved away from the area of best forcing and instability aloft. Ping pong ball size hail fell a few miles north of Benton. This resulted in severe damage to vehicles.", "ts_dict_index": [6396, 6397, 6398]}
+{"event_id": 1110868, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-14 17:19:00", "end_date_time": "2023-06-14 17:19:00", "narrative": "Supercell thunderstorms developed toward midday across the middle Red River Valley along and south of a stalled frontal boundary. These thunderstorms progressed east southeast with upper 80s temperatures on the warm side of the boundary with dew points exceeding 75 degrees. Mid-level lapse rates of 7-8 C/km overspread this very moist low-level air mass over a rather broad west-to-east corridor, supporting extreme instability upwards of 4500 J/kg well downstream of the upscale-growing convection. Coinciding this corridor of extreme buoyancy was very strong effective bulk shear near 65 kts along with hodographs that were modestly curved at the low levels and elongated above 3 km AGL. Numerous local storm reports were documented of large hail, damaging wind gusts, and an isolated tornado across parts of East and Northeast Texas throughout the event. Hen egg size hail reported.", "ts_dict_index": [6411, 6412, 6413]}
+{"event_id": 1110872, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-14 17:20:00", "end_date_time": "2023-06-14 17:20:00", "narrative": "Supercell thunderstorms developed toward midday across the middle Red River Valley along and south of a stalled frontal boundary. These thunderstorms progressed east southeast with upper 80s temperatures on the warm side of the boundary with dew points exceeding 75 degrees. Mid-level lapse rates of 7-8 C/km overspread this very moist low-level air mass over a rather broad west-to-east corridor, supporting extreme instability upwards of 4500 J/kg well downstream of the upscale-growing convection. Coinciding this corridor of extreme buoyancy was very strong effective bulk shear near 65 kts along with hodographs that were modestly curved at the low levels and elongated above 3 km AGL. Numerous local storm reports were documented of large hail, damaging wind gusts, and an isolated tornado across parts of East and Northeast Texas throughout the event. Hen egg size hail reported in the Stallion Park Place and Stallion Lake Ranch areas in northwest Smith County.", "ts_dict_index": [6414, 6415, 6416]}
+{"event_id": 1110811, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-14 17:10:00", "end_date_time": "2023-06-14 17:10:00", "narrative": "Supercell thunderstorms developed toward midday across the middle Red River Valley along and south of a stalled frontal boundary. These thunderstorms progressed east southeast with upper 80s temperatures on the warm side of the boundary with dew points exceeding 75 degrees. Mid-level lapse rates of 7-8 C/km overspread this very moist low-level air mass over a rather broad west-to-east corridor, supporting extreme instability upwards of 4500 J/kg well downstream of the upscale-growing convection. Coinciding this corridor of extreme buoyancy was very strong effective bulk shear near 65 kts along with hodographs that were modestly curved at the low levels and elongated above 3 km AGL. Numerous local storm reports were documented of large hail, damaging wind gusts, and an isolated tornado across parts of East and Northeast Texas throughout the event. Nickel size hail reported in the Jamestown community.", "ts_dict_index": [6408, 6409, 6410]}
+{"event_id": 946612, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-04-09 17:35:00", "end_date_time": "2021-04-09 17:35:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Ping pong ball size hail fell near the Brachfield community.", "ts_dict_index": [6423, 6424, 6425]}
+{"event_id": 1100453, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-07-03 17:05:00", "end_date_time": "2023-07-03 17:05:00", "narrative": "A broad positively tilted upper trough continued to extend from the Great Lakes Region and Mid-Mississippi Valley southwest into North Texas during the afternoon of July 3rd, while an associated weak surface front lifted back north before becoming stationary across Southeast Oklahoma and Western/Central Arkansas. Strong heating within a moist air mass resulted in strong instability developing during the afternoon, with large scale forcing ahead of the trough adequate enough for the development of scattered showers and thunderstorms across portions of Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and Northwest Louisiana during the afternoon. One isolated severe thunderstorm developed over Northeast McCurtain County Oklahoma, producing damaging winds which downed multiple trees near Smithville. Large hail was also observed from this storm. Quarter size hail fell near Smithville.", "ts_dict_index": [6402, 6403, 6404]}
+{"event_id": 946607, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-04-09 15:55:00", "end_date_time": "2021-04-09 15:55:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Quarter size hail fell in Mount Enterprise.", "ts_dict_index": [6426, 6427, 6428]}
+{"event_id": 946611, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-04-09 17:25:00", "end_date_time": "2021-04-09 17:25:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Ping pong ball size hail fell in the Minden community.", "ts_dict_index": [6432, 6433, 6434]}
+{"event_id": 946614, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-04-09 17:35:00", "end_date_time": "2021-04-09 17:35:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Teacup size hail fell several miles southeast of Henderson. Report from mPING.", "ts_dict_index": [6435, 6436, 6437]}
+{"event_id": 946610, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-04-09 17:01:00", "end_date_time": "2021-04-09 17:01:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Half dollar size hail fell in the Glenfawn community.", "ts_dict_index": [6429, 6430, 6431]}
+{"event_id": 946756, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-04-09 13:24:00", "end_date_time": "2021-04-09 13:24:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across North Louisiana. These storms finally exited North Louisiana during the early morning hours of April 10th with the passage of the cold front. Nickel size hail fell east of Benton Road and just north of Kingston Road.", "ts_dict_index": [6366, 6367, 6368]}
+{"event_id": 946606, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-09 15:32:00", "end_date_time": "2021-04-09 15:32:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Quarter size hail fell in the Lilbert community.", "ts_dict_index": [6444, 6445, 6446]}
+{"event_id": 946622, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-09 22:08:00", "end_date_time": "2021-04-09 22:08:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Penny size hail fell on the west side of Nacogdoches.", "ts_dict_index": [6447, 6448, 6449]}
+{"event_id": 946625, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-04-09 23:20:00", "end_date_time": "2021-04-09 23:20:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Penny size hail fell on County Road 431 near Lindale.", "ts_dict_index": [6450, 6451, 6452]}
+{"event_id": 946613, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-04-09 17:35:00", "end_date_time": "2021-04-09 17:35:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Baseball size hail fell at the intersection of Highway 259 and County Road 317.", "ts_dict_index": [6441, 6442, 6443]}
+{"event_id": 949006, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-05-10 15:16:00", "end_date_time": "2021-05-10 15:16:00", "narrative": "A shallow cold front settled south into portions of Southeast Texas and Central Louisiana by the morning hours of May 10th, although a weak shortwave trough traversed east across the Red River Valley of Southern Oklahoma and North Texas, enhancing scattered shower and thunderstorm development over this area. Steep lapse rates aloft contributed to adequate instability such that some of these storms become severe, as they tracked southeast into Northeast Texas and Northwest Louisiana during the afternoon. These storms remained elevated across much of these areas, producing large hail before becoming more surface based across portions of Northwest Louisiana, where damaging winds were the more dominant mode. Numerous trees were uprooted in Red River Parish before the storms weakened as they moved away from the area of best forcing and instability aloft. Half dollar size and larger hail fell at the Caddo Parish entrance to the Lock and Dam #5 south of Caspiana, which broke windows of vehicles.", "ts_dict_index": [6381, 6382, 6383]}
+{"event_id": 946599, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-04-09 11:40:00", "end_date_time": "2021-04-09 11:40:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Half dollar size hail fell in the Red Springs community.", "ts_dict_index": [6456, 6457, 6458]}
+{"event_id": 946598, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-04-09 11:20:00", "end_date_time": "2021-04-09 11:20:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Penny size hail fell in the Hideaway community.", "ts_dict_index": [6453, 6454, 6455]}
+{"event_id": 946603, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2021-04-09 11:56:00", "end_date_time": "2021-04-09 11:56:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Ping pong ball size hail fell on the northwest side of De Kalb.", "ts_dict_index": [6465, 6466, 6467]}
+{"event_id": 961304, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2021-07-20 11:15:00", "end_date_time": "2021-07-20 11:20:00", "narrative": "It was another active monsoon day across northern and central New Mexico on July 20, 2021. With an area of high pressure centered over the Four Corners and high amounts of atmospheric moisture across western and central New Mexico, thunderstorms developed by late morning across the mountainous terrain. With the upper-level high pressure's location, thunderstorms moved in a southerly direction and expanded in coverage across lower elevations. These thunderstorms produced very heavy rainfall, and several reports of flash flooding were received across urban areas. The most significant flash flooding occurred in Albuquerque where rainfall rates of 3 to 4 inches per hour quickly filled the city's arroyos. Three water rescues had to be conducted in Albuquerque due to people in the arroyos, but unfortunately, rescue efforts were not successful. A CoCoRaHS observer in House reported nickel size hail with a strong thunderstorm tracking southward through the area. The observer also reported some minor damage with dents in their car from the hail. Damages are estimated for the car dents.", "ts_dict_index": [6474, 6475, 6476]}
+{"event_id": 946604, "event_type": "Hail", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-04-09 12:40:00", "end_date_time": "2021-04-09 12:40:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Quarter size hail fell a few miles west of the Hideaway community.", "ts_dict_index": [6468, 6469, 6470]}
+{"event_id": 939786, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2021-03-17 06:58:00", "end_date_time": "2021-03-17 06:58:00", "narrative": "A strong closed upper low pressure system ejected northeast through the Oklahoma/Texas Panhandle region during the afternoon and evening hours of March 16th, which helped mix a dry line east across Oklahoma and Texas. Ahead of this dry line, a broad warm and moist sector spread north across the Ark-La-Tex, which allowed for greater instability to overspread into the area ahead of this surface feature. A complex of showers and thunderstorms developed over West Texas during the late afternoon through the evening hours on the 16th, before advancing east across the state during the overnight and early morning hours of the 17th. Some of these storms remained severe as they moved through East Texas around and shortly after daybreak, where damaging winds downed trees and power lines before gradually weakening as they moved into Western Louisiana. Nickel size hail fell in Maud.", "ts_dict_index": [6471, 6472, 6473]}
+{"event_id": 946602, "event_type": "Hail", "state": "TEXAS", "cz_name": "BOWIE", "begin_date_time": "2021-04-09 11:55:00", "end_date_time": "2021-04-09 11:55:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Half dollar size hail fell near De kalb.", "ts_dict_index": [6462, 6463, 6464]}
+{"event_id": 946626, "event_type": "Hail", "state": "TEXAS", "cz_name": "NACOGDOCHES", "begin_date_time": "2021-04-10 01:22:00", "end_date_time": "2021-04-10 01:22:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Nickel size hail fell in the Appleby community.", "ts_dict_index": [6459, 6460, 6461]}
+{"event_id": 949010, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-05-10 14:35:00", "end_date_time": "2021-05-10 14:35:00", "narrative": "A shallow cold front settled south into portions of Southeast Texas and Central Louisiana by the morning hours of May 10th, although a weak shortwave trough traversed east across the Red River Valley of Southern Oklahoma and North Texas, enhancing scattered shower and thunderstorm development over this area. Steep lapse rates aloft contributed to adequate instability such that some of these storms become severe, as they tracked southeast into Northeast Texas and Northwest Louisiana during the afternoon. These storms remained elevated across much of these areas, producing large hail before becoming more surface based across portions of Northwest Louisiana, where damaging winds were the more dominant mode. Numerous trees were uprooted in Red River Parish before the storms weakened as they moved away from the area of best forcing and instability aloft. Quarter size hail fell near LSU-Shreveport.", "ts_dict_index": [6399, 6400, 6401]}
+{"event_id": 1120217, "event_type": "Hail", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2023-07-28 18:55:00", "end_date_time": "2023-07-28 18:55:00", "narrative": "A cold front sank south across Iowa during the afternoon and evening of July 28th. The environment was primed for severe storms with warm moist air in place; as temperatures climbed into the 90s and dewpoints into the 70s. By afternoon MLCAPE values of 3000 J/kg were in place across much of Iowa with deep layer shear exceeding 40 kts. Such an environment supported rapid storm development along the boundary by late afternoon. Storms produced ping-pong ball to baseball sized hail along with two tornadoes, damaging confinement pens and creating easily identifiable tracks on high resolution satellite imagery through surrounding fields. As storms pushed south into the evening, the hazards transitioned to a wind threat. A micro burst occurred in Marshall County very near the ASOS, resulting in an isolated pocket of 80 to 90 mph winds. Delayed report via mping.", "ts_dict_index": [6483, 6484, 6485]}
+{"event_id": 815855, "event_type": "Hail", "state": "IOWA", "cz_name": "MARSHALL", "begin_date_time": "2019-04-17 15:31:00", "end_date_time": "2019-04-17 15:31:00", "narrative": "A surface low pressure system developed in the southern Colorado front range area on April 16th and slid east northeast through Kansas, Nebraska, and into Iowa through the 17th of April. By mid afternoon on the 17th, the surface low was situated over north central Iowa/south central Minnesota and the accompanying surface low extending back south southwest through the state. In the warm sector, SBCAPE values were in the 1000-2000 J/kg range, effective bulk shear around 30 to 40 kts, nominal hail CAPE values in the 200 to 300 J/kg range, and nearly negligible DCAPE. Storms were driven by the cold front and were pulse storms in nature in most cases. Storms were predominantly sub-severe with gusty winds and small hail, though two instances of severe reports were seen in the form of a destroyed farm shed and quarter inch hail. Trained spotter reported quarter inch hail.", "ts_dict_index": [6486, 6487, 6488]}
+{"event_id": 1092973, "event_type": "Hail", "state": "TEXAS", "cz_name": "LUBBOCK", "begin_date_time": "2023-05-23 17:10:00", "end_date_time": "2023-05-23 17:21:00", "narrative": "Another consecutive evening of severe storms occurred on the Caprock on the evening of the 23rd as the atmosphere again became very unstable. Several of the thunderstorms were able to gain significant mid-level rotation which allowed them to generate very large hail. Hailstones as large as baseballs damaged multiple vehicles northwest of Shallowater (Lubbock County) along US Highway 84, while many other spots incurred impacts from hail as large as golf ball size. In addition to producing large hail, the slow moving storms also dumped torrential rainfall. One such pocket of torrential rain occurred just to the north of Plainview (Hale County), where several roads were underwater. Activity then shifted into the Rolling Plains late in the evening as activity morphed into upscale clusters of storms producing a few severe wind gusts. Numerous reports were received of a swath of hail from north of Shallowater westward to the Lubbock/Hockley County line. Hail ranged in size from quarters to as large as baseballs. Multiple vehicles were reported as damaged along US Highway 84.", "ts_dict_index": [6480, 6481, 6482]}
+{"event_id": 1103682, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-07-22 16:05:00", "end_date_time": "2023-07-22 16:05:00", "narrative": "A large upper level ridge of high pressure over the Rockies and Southern Plains began to retreat west of the Four State Region on July 22nd, as a weak upper level disturbance shifted southeast into the region and Lower Mississippi Valley. This disturbance reinforced a weak cool front south through the area, and focused scattered showers and thunderstorms during the mid and late afternoon hours over portions of Deep East Texas and Central Louisiana during peak heating. This heating and the available low level moisture in place contributed to strong instability which enhanced this thunderstorm development, contributing to a couple of these storms becoming briefly severe. One severe thunderstorm produced quarter size hail in the Ebarb community in Western Sabine Parish before weakening as it moved into Vernon Parish late in the afternoon. Quarter size hail fell in the Ebarb community.", "ts_dict_index": [6477, 6478, 6479]}
+{"event_id": 946615, "event_type": "Hail", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-04-09 17:51:00", "end_date_time": "2021-04-09 17:51:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma, resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with numerous reports of large hail and occasional damaging winds across East Texas. These storms finally diminished during the early morning hours of April 10th with the passage of the cold front. Half dollar size hail fell several miles southeast of Henderson. Report from mPING.", "ts_dict_index": [6438, 6439, 6440]}
+{"event_id": 952203, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2021-05-28 15:06:00", "end_date_time": "2021-05-28 15:15:00", "narrative": "A backdoor cold front tracked south and west through New Mexico early on May 28, 2021, which reinforced low-level moisture across much of eastern and central portions of the state. Upslope flow aided in the early onset of afternoon thunderstorms across the higher terrain, and these thunderstorms then tracked east to southeast onto the plains. With plenty of instability and shear, these storms quickly intensified through the afternoon and evening hours. Large hail was the main hazard with numerous reports of hail ranging from 2 to 3 inches. A variety of weather hazards particularly impacted southeast New Mexico with large hail and severe winds resulting in property damage and minor street flooding in Portales and Clovis disrupting traffic. A couple tornadoes and landspouts were also reported, but did not do any damage. A trained spotter reported 1 inch hail along Interstate 40 from a severe thunderstorm that tracked southeastward over the area.", "ts_dict_index": [6501, 6502, 6503]}
+{"event_id": 949599, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2021-05-17 14:00:00", "end_date_time": "2021-05-17 14:20:00", "narrative": "An active stretch of severe weather across eastern New Mexico continued on May 17, 2021 with a significant severe weather outbreak that included multiple tornadoes. As a potent low pressure system approached the state, instability and shear increased across the area, providing a favorable environment for severe thunderstorms. Convective initiation started by late Monday morning over the high terrain of New Mexico. Steering flow generally moved the storms in a northeasterly direction where they intensified over the plains. Several reports of hail and severe winds were received as well as multiple tornado reports. Two supercell tornadoes occurred across eastern New Mexico, but no damage occurred. The environment was even favorable for tornadoes in central New Mexico where three landspout tornadoes were confirmed. A trained spotter reported nickel size hail from a strong thunderstorm near House.", "ts_dict_index": [6510, 6511, 6512]}
+{"event_id": 952601, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2021-05-28 15:55:00", "end_date_time": "2021-05-28 16:00:00", "narrative": "A backdoor cold front tracked south and west through New Mexico early on May 28, 2021, which reinforced low-level moisture across much of eastern and central portions of the state. Upslope flow aided in the early onset of afternoon thunderstorms across the higher terrain, and these thunderstorms then tracked east to southeast onto the plains. With plenty of instability and shear, these storms quickly intensified through the afternoon and evening hours. Large hail was the main hazard with numerous reports of hail ranging from 2 to 3 inches. A variety of weather hazards particularly impacted southeast New Mexico with large hail and severe winds resulting in property damage and minor street flooding in Portales and Clovis disrupting traffic. A couple tornadoes and landspouts were also reported, but did not do any damage. A trained spotter reported 1 inch hail as they were driving along U.S. Highway 209 near Quay.", "ts_dict_index": [6498, 6499, 6500]}
+{"event_id": 1096282, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "BUFFALO", "begin_date_time": "2023-05-10 21:03:00", "end_date_time": "2023-05-10 21:03:00", "narrative": "Southwest upper winds were over south central Nebraska with an upper level trough moving towards the Four Corners region. A surface low was over eastern Colorado with storms that developed over the High Plains during the afternoon. CAPE values were around 2,000 J/kg, but wind shear was fairly weak across south central Nebraska. Dewpoint temperatures were generally in the lower 60s and the air temperature cooled to near 70 degrees during the evening hours. ||Storms were across eastern Colorado, western and southern Nebraska, and northeast Kansas during the evening hours of May 10th. An area of storms across southern Nebraska moved eastward while a line of storms developed across south central Nebraska. These storms that developed produced quarter and half dollar sized hail between 10 and 10:30 pm in Buffalo County. ", "ts_dict_index": [6507, 6508, 6509]}
+{"event_id": 938045, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2021-03-13 11:30:00", "end_date_time": "2021-03-13 11:35:00", "narrative": "A slow-moving Pacific storm system finally arrived to New Mexico on March 13-14, 2021, and this dynamic low pressure system brought a wide variety of weather hazards to the area. Strengthening southwest flow from a strong upper-level jet resulted in high winds to much of eastern and southern New Mexico. This system also brought heavy snow to the northern mountains with the highest totals of 15 to 27 inches across the Sangre de Cristo Mountains. Meanwhile, return flow across the eastern plains ahead of this low pressure system combined with an unstable atmosphere to produce severe weather from the 13th through the morning of the 14th. Scattered strong to severe thunderstorms developed along a dryline across eastern New Mexico which resulted in large hail and strong thunderstorm wind gusts in Quay County. One inch hail was reported with a severe thunderstorm near Tucumcari on the morning of March 13th.", "ts_dict_index": [6522, 6523, 6524]}
+{"event_id": 951837, "event_type": "Hail", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-05-05 14:59:00", "end_date_time": "2021-05-05 14:59:00", "narrative": "A swift moving cold front brought a brief bout of strong storms to south central Nebraska during the afternoon hours on May 5th. Thunderstorms developed along the cold front from SW to NE, generally along a line from Franklin County to Nance County around 3pm, and moved SE. Most of this activity was fairly weak and poorly organized. However, shortly before 4pm CDT, a stronger storm developed over Clay County and managed to produce nickel size hail and a brief landspout tornado. This became the second event in only a few days where landspout tornadoes were reported in this general area of south central Nebraska. No damage or impacts from the landspout were reported, so it was given an EFU rating. The line of thunderstorms continued SE with no additional severe reports, and exited the area around 6pm CDT. ", "ts_dict_index": [6519, 6520, 6521]}
+{"event_id": 881330, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-05-05 04:15:00", "end_date_time": "2020-05-05 04:15:00", "narrative": "A weak cold front drifted south across Central and Eastern Oklahoma into Western and Central Arkansas during the early morning hours of May 5th, as a series of weak upper level disturbances traversed east across these areas. Pockets of cold air aloft contributed to steep lapse rates, with large scale forcing ahead of these disturbances contributing to scattered showers and thunderstorms which shifted south southeast with the front over Southeast Oklahoma and the northern sections of Southwest Arkansas prior to daybreak. Given the extent of instability and wind shear ahead of the front, some of these storms became severe, producing large hail over portions of Northern and Eastern McCurtain County. These storms eventually weakened by daybreak as instability diminished over the area with the departure of these disturbances. A picture of golf ball size hail that fell between Broken Bow and Eagletown was posted to social media.", "ts_dict_index": [6495, 6496, 6497]}
+{"event_id": 881328, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-05-05 00:55:00", "end_date_time": "2020-05-05 00:55:00", "narrative": "A weak cold front drifted south across Central and Eastern Oklahoma into Western and Central Arkansas during the early morning hours of May 5th, as a series of weak upper level disturbances traversed east across these areas. Pockets of cold air aloft contributed to steep lapse rates, with large scale forcing ahead of these disturbances contributing to scattered showers and thunderstorms which shifted south southeast with the front over Southeast Oklahoma and the northern sections of Southwest Arkansas prior to daybreak. Given the extent of instability and wind shear ahead of the front, some of these storms became severe, producing large hail over portions of Northern and Eastern McCurtain County. These storms eventually weakened by daybreak as instability diminished over the area with the departure of these disturbances. Golf ball size size hail mixed with some ping pong ball and half dollar size hail fell in Smithville. Report from a trained spotter via social media.", "ts_dict_index": [6492, 6493, 6494]}
+{"event_id": 1015171, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-04-24 20:10:00", "end_date_time": "2022-04-24 20:10:00", "narrative": "A broad upper trough extended south from Southern Minnesota into the Ozarks during the afternoon of April 24th, with a secondary shortwave trough swinging southeast over Eastern Colorado and Western Kansas, which entered Oklahoma during the evening hours. A cold front moved slowly southeast across Northwest Arkansas, Southeast Oklahoma, into Northern and West-central Texas during the afternoon, with large scale forcing ahead of this second shortwave trough focusing showers and thunderstorms along the frontal zone where daytime heating resulted in increased instability over Southeast Oklahoma. Thus, strong to severe thunderstorms developed as a result, which moved across portions of McCurtain County downing trees and power lines and also producing large hail before exiting the area by mid-evening. Quarter size hail fell in the Hochatown community near Beavers Bend State Park.", "ts_dict_index": [6531, 6532, 6533]}
+{"event_id": 1107588, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-06-12 13:18:00", "end_date_time": "2023-06-12 13:18:00", "narrative": "Robust convection developed across northern and central portions of Louisiana with multiple multicellular structures and supercells ahead of a surface cold front. Surface temperatures in the 90s along with dew points in the 70s contributed to 4000 J/kg MLCAPE. Strong mid-level flow also supported over 40 knots of effective bulk shear. As such, storms organized into multicellular clusters and transient supercells, with damaging gusts and large hail the main threats. Furthermore, MRMS MESH depicted storms with hail approaching 2 inches in diameter, with a couple of 1 inch hail/wind damage reports also received. Given the heated, well-mixed boundary layer (and associated 3500+ J/kg MLCAPE) preceding the storms, supercell structures persisted into the evening hours with a large hail/damaging gust threat. Quarter size hail reported in Zwolle.", "ts_dict_index": [6525, 6526, 6527]}
+{"event_id": 954693, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-17 16:47:00", "end_date_time": "2021-06-17 16:47:00", "narrative": "A broad ridge of high pressure aloft was anchored from the Four Corners Region east into the Southern Plains on June 17th. Meanwhile, an upper level disturbance rounded the ridge and drifted southwest across Western Arkansas and Southeast Oklahoma during the afternoon, over an area where moderate instability developed once temperatures climbed into the lower and mid 90s. Given the higher terrain over this area, orographic ascent helped to increase large scale forcing beneath this disturbance such that isolated showers and thunderstorms developed during the mid and late afternoon, and became severe as they entered Northern McCurtain County Oklahoma. Reports of quarter size hail and damaging winds which downed trees were received from this storm as it spread west, before entering Southern Pushmataha County. Quarter size hail fell near Battiest.", "ts_dict_index": [6516, 6517, 6518]}
+{"event_id": 1107592, "event_type": "Hail", "state": "LOUISIANA", "cz_name": "SABINE", "begin_date_time": "2023-06-12 14:10:00", "end_date_time": "2023-06-12 14:10:00", "narrative": "Robust convection developed across northern and central portions of Louisiana with multiple multicellular structures and supercells ahead of a surface cold front. Surface temperatures in the 90s along with dew points in the 70s contributed to 4000 J/kg MLCAPE. Strong mid-level flow also supported over 40 knots of effective bulk shear. As such, storms organized into multicellular clusters and transient supercells, with damaging gusts and large hail the main threats. Furthermore, MRMS MESH depicted storms with hail approaching 2 inches in diameter, with a couple of 1 inch hail/wind damage reports also received. Given the heated, well-mixed boundary layer (and associated 3500+ J/kg MLCAPE) preceding the storms, supercell structures persisted into the evening hours with a large hail/damaging gust threat. Quarter size hail reported along Highway 191.", "ts_dict_index": [6528, 6529, 6530]}
+{"event_id": 954692, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-17 16:22:00", "end_date_time": "2021-06-17 16:22:00", "narrative": "A broad ridge of high pressure aloft was anchored from the Four Corners Region east into the Southern Plains on June 17th. Meanwhile, an upper level disturbance rounded the ridge and drifted southwest across Western Arkansas and Southeast Oklahoma during the afternoon, over an area where moderate instability developed once temperatures climbed into the lower and mid 90s. Given the higher terrain over this area, orographic ascent helped to increase large scale forcing beneath this disturbance such that isolated showers and thunderstorms developed during the mid and late afternoon, and became severe as they entered Northern McCurtain County Oklahoma. Reports of quarter size hail and damaging winds which downed trees were received from this storm as it spread west, before entering Southern Pushmataha County. Quarter size hail fell in the community of Bethel.", "ts_dict_index": [6513, 6514, 6515]}
+{"event_id": 881329, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-05-05 01:05:00", "end_date_time": "2020-05-05 01:05:00", "narrative": "A weak cold front drifted south across Central and Eastern Oklahoma into Western and Central Arkansas during the early morning hours of May 5th, as a series of weak upper level disturbances traversed east across these areas. Pockets of cold air aloft contributed to steep lapse rates, with large scale forcing ahead of these disturbances contributing to scattered showers and thunderstorms which shifted south southeast with the front over Southeast Oklahoma and the northern sections of Southwest Arkansas prior to daybreak. Given the extent of instability and wind shear ahead of the front, some of these storms became severe, producing large hail over portions of Northern and Eastern McCurtain County. These storms eventually weakened by daybreak as instability diminished over the area with the departure of these disturbances. Half dollar size hail damaged vehicles north of Watson near the Mountain Fork River.", "ts_dict_index": [6489, 6490, 6491]}
+{"event_id": 1020837, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:15:00", "end_date_time": "2022-04-12 17:15:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. Broadcast media reported golf ball sized hail about 2 miles west-northwest of Killeen, TX.", "ts_dict_index": [6549, 6550, 6551]}
+{"event_id": 1020991, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:29:00", "end_date_time": "2022-04-12 17:29:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. Military personnel reported golf ball sized hail at Phantom Warrior Lanes on Fort Hood in Killeen Texas.", "ts_dict_index": [6552, 6553, 6554]}
+{"event_id": 1020949, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:12:00", "end_date_time": "2022-04-12 17:12:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. Amateur radio reported golf ball sized hail about 3 miles north-northwest of Salado, TX.", "ts_dict_index": [6558, 6559, 6560]}
+{"event_id": 1021017, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 18:32:00", "end_date_time": "2022-04-12 18:32:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. Amateur radio reported quarter sized hail in Zabcikville, TX.", "ts_dict_index": [6567, 6568, 6569]}
+{"event_id": 1021009, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 18:50:00", "end_date_time": "2022-04-12 18:50:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A public report indicated quarter sized hail about 3 miles west-northwest of Temple, TX.", "ts_dict_index": [6573, 6574, 6575]}
+{"event_id": 1020942, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:27:00", "end_date_time": "2022-04-12 17:27:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A public report indicated half-dollar sized hail just southwest of Killeen, TX.", "ts_dict_index": [6570, 6571, 6572]}
+{"event_id": 1020947, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:10:00", "end_date_time": "2022-04-12 17:20:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A trained spotter reported 3-inch diameter hail just southwest of Belton, TX.", "ts_dict_index": [6555, 6556, 6557]}
+{"event_id": 1021018, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 18:49:00", "end_date_time": "2022-04-12 18:49:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A trained spotter reported quarter sized hail about 4 miles north-northeast of Salado, TX.", "ts_dict_index": [6564, 6565, 6566]}
+{"event_id": 1088590, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-11 21:57:00", "end_date_time": "2023-03-11 21:57:00", "narrative": "A cold front advanced southeastward across Oklahoma and western North Texas on the afternoon of March 11th, interacting with a roughly west-to-east warm front extending across southeast Oklahoma and into southern Arkansas. This resulted in an organized complex of thunderstorms moving to the east/southeast from southeast Oklahoma into southwest Arkansas. A few embedded supercells tracked on the southwest portion of the line with large hail as the primary threat. Further intensification along the southwestern flank of the convection was observed as the complex moved southeastward along the frontal boundary and into a slightly more buoyant air mass characterized by surface temperatures and dewpoints in the low to mid 60s. Consequently, some isolated severe wind gusts also produced sporadic damage. Quarter size hail reported just north of Eagletown via social media.", "ts_dict_index": [6543, 6544, 6545]}
+{"event_id": 1088588, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-11 21:40:00", "end_date_time": "2023-03-11 21:40:00", "narrative": "A cold front advanced southeastward across Oklahoma and western North Texas on the afternoon of March 11th, interacting with a roughly west-to-east warm front extending across southeast Oklahoma and into southern Arkansas. This resulted in an organized complex of thunderstorms moving to the east/southeast from southeast Oklahoma into southwest Arkansas. A few embedded supercells tracked on the southwest portion of the line with large hail as the primary threat. Further intensification along the southwestern flank of the convection was observed as the complex moved southeastward along the frontal boundary and into a slightly more buoyant air mass characterized by surface temperatures and dewpoints in the low to mid 60s. Consequently, some isolated severe wind gusts also produced sporadic damage. Quarter size hail reported near the intersection of US Highway 259 and State Highway 259 A.", "ts_dict_index": [6537, 6538, 6539]}
+{"event_id": 1088586, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-11 19:51:00", "end_date_time": "2023-03-11 19:51:00", "narrative": "A cold front advanced southeastward across Oklahoma and western North Texas on the afternoon of March 11th, interacting with a roughly west-to-east warm front extending across southeast Oklahoma and into southern Arkansas. This resulted in an organized complex of thunderstorms moving to the east/southeast from southeast Oklahoma into southwest Arkansas. A few embedded supercells tracked on the southwest portion of the line with large hail as the primary threat. Further intensification along the southwestern flank of the convection was observed as the complex moved southeastward along the frontal boundary and into a slightly more buoyant air mass characterized by surface temperatures and dewpoints in the low to mid 60s. Consequently, some isolated severe wind gusts also produced sporadic damage. Nickel size hail reported in the Tablerville community via social media.", "ts_dict_index": [6534, 6535, 6536]}
+{"event_id": 1088587, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-11 21:33:00", "end_date_time": "2023-03-11 21:33:00", "narrative": "A cold front advanced southeastward across Oklahoma and western North Texas on the afternoon of March 11th, interacting with a roughly west-to-east warm front extending across southeast Oklahoma and into southern Arkansas. This resulted in an organized complex of thunderstorms moving to the east/southeast from southeast Oklahoma into southwest Arkansas. A few embedded supercells tracked on the southwest portion of the line with large hail as the primary threat. Further intensification along the southwestern flank of the convection was observed as the complex moved southeastward along the frontal boundary and into a slightly more buoyant air mass characterized by surface temperatures and dewpoints in the low to mid 60s. Consequently, some isolated severe wind gusts also produced sporadic damage. Half dollar size hail reported in the Hochatown area.", "ts_dict_index": [6540, 6541, 6542]}
+{"event_id": 952616, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2021-05-28 03:08:00", "end_date_time": "2021-05-28 03:28:00", "narrative": "A backdoor cold front tracked south and west through New Mexico early on May 28, 2021, which reinforced low-level moisture across much of eastern and central portions of the state. Upslope flow aided in the early onset of afternoon thunderstorms across the higher terrain, and these thunderstorms then tracked east to southeast onto the plains. With plenty of instability and shear, these storms quickly intensified through the afternoon and evening hours. Large hail was the main hazard with numerous reports of hail ranging from 2 to 3 inches. A variety of weather hazards particularly impacted southeast New Mexico with large hail and severe winds resulting in property damage and minor street flooding in Portales and Clovis disrupting traffic. A couple tornadoes and landspouts were also reported, but did not do any damage. An early morning severe thunderstorm near Ragland produced a mixture of quarter to golf ball size hail.", "ts_dict_index": [6504, 6505, 6506]}
+{"event_id": 1034410, "event_type": "Hail", "state": "NEW MEXICO", "cz_name": "QUAY", "begin_date_time": "2022-07-29 15:30:00", "end_date_time": "2022-07-29 15:40:00", "narrative": "An abundant amount of moisture in the atmosphere led to another very active monsoon day for northern and central New Mexico on July 29, 2022. Thunderstorms developed early in the day across the high terrain areas before becoming more widespread as the day progressed. Heavy rain was common with these thunderstorms, especially on the Calf Canyon burn scar which reported more burn scar flash flooding and debris flow. The Gallup area also received heavy rainfall which forced the closure of a few area roadways. Meanwhile, a few thunderstorms across the eastern plains briefly turned strong to severe which prompted a few Severe Thunderstorm Warnings. One thunderstorm near Logan looked like it was producing baseball size hail according to radar, but a trained spotter only reported quarter size hail. A trained spotter near Logan reported quarter size hail. The hail did damage to tree leaves and destroyed their garden. Damages are estimated.", "ts_dict_index": [6585, 6586, 6587]}
+{"event_id": 1020995, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:40:00", "end_date_time": "2022-04-12 17:40:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A public report indicated 2 inch diameter hail about 2 miles west-southwest of Belton, TX.", "ts_dict_index": [6579, 6580, 6581]}
+{"event_id": 1020997, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:46:00", "end_date_time": "2022-04-12 17:46:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A public report indicated 2.25 inch diameter hail about 4 miles west-southwest of Belton, TX.", "ts_dict_index": [6582, 6583, 6584]}
+{"event_id": 1020994, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:30:00", "end_date_time": "2022-04-12 17:30:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A public report indicated golf ball sized hail 3 miles south-southwest of Belton, TX.", "ts_dict_index": [6576, 6577, 6578]}
+{"event_id": 1020838, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:19:00", "end_date_time": "2022-04-12 17:19:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A public report indicated golf ball sized hail just south of Belton, TX.", "ts_dict_index": [6561, 6562, 6563]}
+{"event_id": 1020998, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:46:00", "end_date_time": "2022-04-12 17:46:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A public report indicated golf ball sized hail about 2 miles north-northwest of Killeen, TX.", "ts_dict_index": [6588, 6589, 6590]}
+{"event_id": 1020551, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:00:00", "end_date_time": "2022-04-12 17:00:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A social media picture indicated a 5.6+ inch diameter hail stone in Salado, TX. Swift actions were taken by NWS Fort Worth and the IBHS (Insurance Institute for Business & Home Safety) to preserve and document this record hailstone. The IBHS officially measured the hailstone at: Maximum diameter ��� 5.676 in, Mass ��� 409.3 g, Volume ��� 29.5 in3 making it the largest hail stone on record in the FWD CWA to date. Other large hailstones also fell in this same area.", "ts_dict_index": [6606, 6607, 6608]}
+{"event_id": 1021013, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 18:03:00", "end_date_time": "2022-04-12 18:03:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A trained spotter reported golf ball sized hail about 3 miles east of Temple, TX.", "ts_dict_index": [6597, 6598, 6599]}
+{"event_id": 1021012, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:53:00", "end_date_time": "2022-04-12 17:53:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. Amateur radio reported half-dollar sized hail just east of Killeen, TX.", "ts_dict_index": [6600, 6601, 6602]}
+{"event_id": 1020559, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 16:50:00", "end_date_time": "2022-04-12 17:15:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. Many social media reports of large hail ranging up to 4 inch in diameter hail was reported in and around the Salado, TX area. This was in addition to the 5.6+ inch hail stone that is noted separately. The large hail fell for several minutes.", "ts_dict_index": [6609, 6610, 6611]}
+{"event_id": 1021010, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 19:10:00", "end_date_time": "2022-04-12 19:10:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A trained spotter reported half-dollar sized hail about 4 miles north of Rogers, TX.", "ts_dict_index": [6591, 6592, 6593]}
+{"event_id": 1020835, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:14:00", "end_date_time": "2022-04-12 17:14:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. Amateur radio reported half dollar sized hail near the intersection of Highways 2484 and 1670 in Bell County.", "ts_dict_index": [6612, 6613, 6614]}
+{"event_id": 1021011, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:40:00", "end_date_time": "2022-04-12 17:40:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A public report indicated dime sized hail about a mile west of Nolanville, TX.", "ts_dict_index": [6603, 6604, 6605]}
+{"event_id": 1021016, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 18:25:00", "end_date_time": "2022-04-12 18:25:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. Amateur radio reported golf ball sized hail about 3 miles southeast of Temple, TX.", "ts_dict_index": [6618, 6619, 6620]}
+{"event_id": 1021015, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 18:18:00", "end_date_time": "2022-04-12 18:18:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. Amateur radio reported quarter sized hail about a mile north-northeast of Belton, TX.", "ts_dict_index": [6621, 6622, 6623]}
+{"event_id": 1021014, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 18:07:00", "end_date_time": "2022-04-12 18:07:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. Amateur radio reported quarter sized hail about 3 miles west-southwest of Belton, TX.", "ts_dict_index": [6615, 6616, 6617]}
+{"event_id": 1128952, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2023-08-27 11:00:00", "end_date_time": "2023-08-28 11:00:00", "narrative": "A series of training thunderstorms produced extremely high rainfall across portions of Patrick and Carroll Counties during the predawn hours of August 28th. This resulted in areas of flash flooding, mainly in the headwaters of the Smith River and the Ararat River. ||The event began with a stationary front draped near the border of Virginia and North Carolina early on the 28th as an upper level disturbance began passing across the lower Great Lakes, placing the central Appalachians in an area of lift. The disturbance triggered a southeasterly wind shift across the foothills of the Blue Ridge in southern Virginia and northern North Carolina, bringing an increase of deep moisture northeast from the Piedmont of North Carolina. Precipitable water values were estimated to|be 1.9 to 2.1 inches across Patrick and Carroll counties by 3:00 am on the 28th, while Mixed-Layer CAPE values remained around 500 J/Kg through much of the night.||Convection initiated after sunset on the 27th as a few slow-moving showers across southern Patrick County. Coverage and intensity of the slow-moving activity only increased as the evening progressed, with a band of showers and embedded storms forming along the Highway 58 corridor by midnight, that was advancing northeast toward the crest of the Blue Ridge. Deep moisture combined with orographic lift to produce extremely efficient rainfall rates that were, at times, ranging from 3 to 5 inches per hour across Patrick County into neighboring Carroll County. Doppler Radar estimated rainfall totals of nearly 11 inches of rainfall in northern Patrick County across the Smith River basin, which was confirmed by one CoCoRaHS report of 10.70 inches, as well as a Cooperative Observer report from Woolwine of 10.62 inches. The stream gage at the Smith River near Woolwine (SMWV2) rose to 11.04 feet, just above moderate flood stage due to this rainfall, however radar estimates put the highest amounts downstream of this gage.  Few reports of flooding impacts were received, however it was noted that Philpott Reservoir rose 3 feet in response to the inflows from the Smith River. In western Patrick County and southeast Carroll County, 4 to 7 inches of rain fell across the entire headwaters of the Ararat River, with radar estimates of around 9 inches near the town of Ararat, VA. Flash flooding in this area resulted in several roads being destroyed or heavily damaged where they passed over flooded creeks and rivers, including the Ararat River. A personal weather station (Weather Underground: KVAHILLS12) recorded a 24 hour rainfall amount, ending at 11 am EST on the 28th, of 6.91 inches.  This 24-hour total is between a 10-year and a 25-year Average Recurrence Interval event per NOAA Atlas 14 Point Precipitation Frequency estimates.", "ts_dict_index": [6627, 6628, 6629]}
+{"event_id": 1128947, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2023-08-27 07:00:00", "end_date_time": "2023-08-28 07:00:00", "narrative": "A series of training thunderstorms produced extremely high rainfall across portions of Patrick and Carroll Counties during the predawn hours of August 28th. This resulted in areas of flash flooding, mainly in the headwaters of the Smith River and the Ararat River. ||The event began with a stationary front draped near the border of Virginia and North Carolina early on the 28th as an upper level disturbance began passing across the lower Great Lakes, placing the central Appalachians in an area of lift. The disturbance triggered a southeasterly wind shift across the foothills of the Blue Ridge in southern Virginia and northern North Carolina, bringing an increase of deep moisture northeast from the Piedmont of North Carolina. Precipitable water values were estimated to|be 1.9 to 2.1 inches across Patrick and Carroll counties by 3:00 am on the 28th, while Mixed-Layer CAPE values remained around 500 J/Kg through much of the night.||Convection initiated after sunset on the 27th as a few slow-moving showers across southern Patrick County. Coverage and intensity of the slow-moving activity only increased as the evening progressed, with a band of showers and embedded storms forming along the Highway 58 corridor by midnight, that was advancing northeast toward the crest of the Blue Ridge. Deep moisture combined with orographic lift to produce extremely efficient rainfall rates that were, at times, ranging from 3 to 5 inches per hour across Patrick County into neighboring Carroll County. Doppler Radar estimated rainfall totals of nearly 11 inches of rainfall in northern Patrick County across the Smith River basin, which was confirmed by one CoCoRaHS report of 10.70 inches, as well as a Cooperative Observer report from Woolwine of 10.62 inches. The stream gage at the Smith River near Woolwine (SMWV2) rose to 11.04 feet, just above moderate flood stage due to this rainfall, however radar estimates put the highest amounts downstream of this gage.  Few reports of flooding impacts were received, however it was noted that Philpott Reservoir rose 3 feet in response to the inflows from the Smith River. In western Patrick County and southeast Carroll County, 4 to 7 inches of rain fell across the entire headwaters of the Ararat River, with radar estimates of around 9 inches near the town of Ararat, VA. Flash flooding in this area resulted in several roads being destroyed or heavily damaged where they passed over flooded creeks and rivers, including the Ararat River. The Cooperative Weather Observer at Woolwine, VA (WLWV2) measured a 24-hour rainfall total of 10.62 inches, a new all-time record for a 24-hour precipitation total for this station. However, the vast majority of this rainfall fell within a 6-hour window per MRMS data, which would make this total greater than a 1,000-year rainfall event per NOAA Atlas 14 point precipitation frequency estimates.  Runoff from this location flows into the Smith River.", "ts_dict_index": [6636, 6637, 6638]}
+{"event_id": 1128950, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2023-08-27 07:00:00", "end_date_time": "2023-08-28 07:00:00", "narrative": "A series of training thunderstorms produced extremely high rainfall across portions of Patrick and Carroll Counties during the predawn hours of August 28th. This resulted in areas of flash flooding, mainly in the headwaters of the Smith River and the Ararat River. ||The event began with a stationary front draped near the border of Virginia and North Carolina early on the 28th as an upper level disturbance began passing across the lower Great Lakes, placing the central Appalachians in an area of lift. The disturbance triggered a southeasterly wind shift across the foothills of the Blue Ridge in southern Virginia and northern North Carolina, bringing an increase of deep moisture northeast from the Piedmont of North Carolina. Precipitable water values were estimated to|be 1.9 to 2.1 inches across Patrick and Carroll counties by 3:00 am on the 28th, while Mixed-Layer CAPE values remained around 500 J/Kg through much of the night.||Convection initiated after sunset on the 27th as a few slow-moving showers across southern Patrick County. Coverage and intensity of the slow-moving activity only increased as the evening progressed, with a band of showers and embedded storms forming along the Highway 58 corridor by midnight, that was advancing northeast toward the crest of the Blue Ridge. Deep moisture combined with orographic lift to produce extremely efficient rainfall rates that were, at times, ranging from 3 to 5 inches per hour across Patrick County into neighboring Carroll County. Doppler Radar estimated rainfall totals of nearly 11 inches of rainfall in northern Patrick County across the Smith River basin, which was confirmed by one CoCoRaHS report of 10.70 inches, as well as a Cooperative Observer report from Woolwine of 10.62 inches. The stream gage at the Smith River near Woolwine (SMWV2) rose to 11.04 feet, just above moderate flood stage due to this rainfall, however radar estimates put the highest amounts downstream of this gage.  Few reports of flooding impacts were received, however it was noted that Philpott Reservoir rose 3 feet in response to the inflows from the Smith River. In western Patrick County and southeast Carroll County, 4 to 7 inches of rain fell across the entire headwaters of the Ararat River, with radar estimates of around 9 inches near the town of Ararat, VA. Flash flooding in this area resulted in several roads being destroyed or heavily damaged where they passed over flooded creeks and rivers, including the Ararat River. A CoCoRaHS observer (VA-PR-1) measured a 24-hour rainfall total of 6.30 inches. However, the vast majority of this rainfall fell within a 6-hour window per MRMS data, which would make this total between a 50-year and a 100-year rainfall event per NOAA Atlas 14 point precipitation frequency estimates.", "ts_dict_index": [6639, 6640, 6641]}
+{"event_id": 1128949, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2023-08-27 07:00:00", "end_date_time": "2023-08-28 07:00:00", "narrative": "A series of training thunderstorms produced extremely high rainfall across portions of Patrick and Carroll Counties during the predawn hours of August 28th. This resulted in areas of flash flooding, mainly in the headwaters of the Smith River and the Ararat River. ||The event began with a stationary front draped near the border of Virginia and North Carolina early on the 28th as an upper level disturbance began passing across the lower Great Lakes, placing the central Appalachians in an area of lift. The disturbance triggered a southeasterly wind shift across the foothills of the Blue Ridge in southern Virginia and northern North Carolina, bringing an increase of deep moisture northeast from the Piedmont of North Carolina. Precipitable water values were estimated to|be 1.9 to 2.1 inches across Patrick and Carroll counties by 3:00 am on the 28th, while Mixed-Layer CAPE values remained around 500 J/Kg through much of the night.||Convection initiated after sunset on the 27th as a few slow-moving showers across southern Patrick County. Coverage and intensity of the slow-moving activity only increased as the evening progressed, with a band of showers and embedded storms forming along the Highway 58 corridor by midnight, that was advancing northeast toward the crest of the Blue Ridge. Deep moisture combined with orographic lift to produce extremely efficient rainfall rates that were, at times, ranging from 3 to 5 inches per hour across Patrick County into neighboring Carroll County. Doppler Radar estimated rainfall totals of nearly 11 inches of rainfall in northern Patrick County across the Smith River basin, which was confirmed by one CoCoRaHS report of 10.70 inches, as well as a Cooperative Observer report from Woolwine of 10.62 inches. The stream gage at the Smith River near Woolwine (SMWV2) rose to 11.04 feet, just above moderate flood stage due to this rainfall, however radar estimates put the highest amounts downstream of this gage.  Few reports of flooding impacts were received, however it was noted that Philpott Reservoir rose 3 feet in response to the inflows from the Smith River. In western Patrick County and southeast Carroll County, 4 to 7 inches of rain fell across the entire headwaters of the Ararat River, with radar estimates of around 9 inches near the town of Ararat, VA. Flash flooding in this area resulted in several roads being destroyed or heavily damaged where they passed over flooded creeks and rivers, including the Ararat River. A CoCoRaHS observer (VA-PR-8) measured a 24-hour rainfall total of 10.70 inches. However, the vast majority of this rainfall fell within a 6-hour window per MRMS data, which would make this total greater than a 1,000-year rainfall event per NOAA Atlas 14 point precipitation frequency estimates. Runoff from this location flows into the Smith River.", "ts_dict_index": [6624, 6625, 6626]}
+{"event_id": 1128954, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2023-08-27 11:00:00", "end_date_time": "2023-08-28 11:00:00", "narrative": "A series of training thunderstorms produced extremely high rainfall across portions of Patrick and Carroll Counties during the predawn hours of August 28th. This resulted in areas of flash flooding, mainly in the headwaters of the Smith River and the Ararat River. ||The event began with a stationary front draped near the border of Virginia and North Carolina early on the 28th as an upper level disturbance began passing across the lower Great Lakes, placing the central Appalachians in an area of lift. The disturbance triggered a southeasterly wind shift across the foothills of the Blue Ridge in southern Virginia and northern North Carolina, bringing an increase of deep moisture northeast from the Piedmont of North Carolina. Precipitable water values were estimated to|be 1.9 to 2.1 inches across Patrick and Carroll counties by 3:00 am on the 28th, while Mixed-Layer CAPE values remained around 500 J/Kg through much of the night.||Convection initiated after sunset on the 27th as a few slow-moving showers across southern Patrick County. Coverage and intensity of the slow-moving activity only increased as the evening progressed, with a band of showers and embedded storms forming along the Highway 58 corridor by midnight, that was advancing northeast toward the crest of the Blue Ridge. Deep moisture combined with orographic lift to produce extremely efficient rainfall rates that were, at times, ranging from 3 to 5 inches per hour across Patrick County into neighboring Carroll County. Doppler Radar estimated rainfall totals of nearly 11 inches of rainfall in northern Patrick County across the Smith River basin, which was confirmed by one CoCoRaHS report of 10.70 inches, as well as a Cooperative Observer report from Woolwine of 10.62 inches. The stream gage at the Smith River near Woolwine (SMWV2) rose to 11.04 feet, just above moderate flood stage due to this rainfall, however radar estimates put the highest amounts downstream of this gage.  Few reports of flooding impacts were received, however it was noted that Philpott Reservoir rose 3 feet in response to the inflows from the Smith River. In western Patrick County and southeast Carroll County, 4 to 7 inches of rain fell across the entire headwaters of the Ararat River, with radar estimates of around 9 inches near the town of Ararat, VA. Flash flooding in this area resulted in several roads being destroyed or heavily damaged where they passed over flooded creeks and rivers, including the Ararat River. A personal weather station (Weather Underground: KVAPATRI8) recorded a 24 hour rainfall amount, ending at 11 am EST on the 28th, of 6.08 inches.", "ts_dict_index": [6630, 6631, 6632]}
+{"event_id": 1088589, "event_type": "Hail", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-11 21:45:00", "end_date_time": "2023-03-11 21:45:00", "narrative": "A cold front advanced southeastward across Oklahoma and western North Texas on the afternoon of March 11th, interacting with a roughly west-to-east warm front extending across southeast Oklahoma and into southern Arkansas. This resulted in an organized complex of thunderstorms moving to the east/southeast from southeast Oklahoma into southwest Arkansas. A few embedded supercells tracked on the southwest portion of the line with large hail as the primary threat. Further intensification along the southwestern flank of the convection was observed as the complex moved southeastward along the frontal boundary and into a slightly more buoyant air mass characterized by surface temperatures and dewpoints in the low to mid 60s. Consequently, some isolated severe wind gusts also produced sporadic damage. Half dollar size hail reported near Broken Bow Reservoir in the Hochatown area.", "ts_dict_index": [6546, 6547, 6548]}
+{"event_id": 1093252, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2023-05-28 11:00:00", "end_date_time": "2023-05-29 11:00:00", "narrative": "A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region. Areas of rain developed across the mountains by late morning, and gradually increased in coverage due to the sustained 25 to 30 knot (850mb) moisture inflow. Precipitable water values were observed in the 1.2 to 1.3 inch range through the day into the early morning hours of the 29th, which is around the 75th percentile for late May. Through the 28th into the early morning hours of the 29th, the upper low drifted eastward, allowing instability to increase across the central Appalachians as the associated pocket of cooler upper level temperatures approached. While Surface-based CAPE levels remained minimal during the event, Most-Unstable CAPE (MUCAPE) values were observed climbing across the mountains through the evening of the 28th into morning of the 29th, reaching into the 600 to 850 J/Kg range. Combined with orographic lift, this instability supported the development of low-topped thunderstorms with enhanced rainfall rates.  As rainfall totals increased across the mountains and soils approached saturation, flash flood guidance values were lowered to under an inch at the 1- and 3-hour time periods. Training of low-topped cells passed across the Bluefield area between 6 AM and 7 AM with sustained 1.5 to locally 2 inch per hour rates. High runoff resulted in rapid street flooding, with water then quickly surrounding and entering homes. Between 500 and 1,000 homes received some form of water damage. The heavy rain then led to flooding of the Bluestone and East Rivers. A personal weather station (Weather Underground: KWVEDISO2) recorded a 24-rainfall amount of 4.18 inches. This is between a 25-year (4% AEP) and a 50-year (2% AEP) Average Recurrence Interval event per NOAA Atlas 14 Point Precipitation Frequency estimates. This includes about 1.6 inches that fell between 7am and 9am on the 29th, with rainfall rates of up to 2 inches per hour during this time.  Runoff from this location flows into Brush Creek.", "ts_dict_index": [6657, 6658, 6659]}
+{"event_id": 1092236, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2023-05-28 11:00:00", "end_date_time": "2023-05-29 11:00:00", "narrative": "A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region. Areas of rain developed across the mountains by late morning, and gradually increased in coverage due to the sustained 25 to 30 knot (850mb) moisture inflow. Precipitable water values were observed in the 1.2 to 1.3 inch range through the day into the early morning hours of the 29th, which is around the 75th percentile for late May. Through the 28th into the early morning hours of the 29th, the upper low drifted eastward, allowing instability to increase across the central Appalachians as the associated pocket of cooler upper level temperatures approached. While Surface-based CAPE levels remained minimal during the event, Most-Unstable CAPE (MUCAPE) values were observed climbing across the mountains through the evening of the 28th into morning of the 29th, reaching into the 600 to 850 J/Kg range. Combined with orographic lift, this instability supported the development of low-topped thunderstorms with enhanced rainfall rates.  As rainfall totals increased across the mountains and soils approached saturation, flash flood guidance values were lowered to under an inch at the 1- and 3-hour time periods. Training of low-topped cells passed across the Bluefield area between 6 AM and 7 AM with sustained 1.5 to locally 2 inch per hour rates. High runoff resulted in rapid street flooding, with water then quickly surrounding and entering homes. Between 500 and 1,000 homes received some form of water damage. The heavy rain then led to flooding of the Bluestone and East Rivers. A personal weather station (Weather Underground: KWVBLUEF23) recorded a 24-rainfall amount of 5.25 inches. This is about a 200-year Average Recurrence Interval event per NOAA Atlas 14 Point Precipitation Frequency estimates. Runoff from this location flows into the East River.", "ts_dict_index": [6654, 6655, 6656]}
+{"event_id": 1093261, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2023-05-28 06:00:00", "end_date_time": "2023-05-30 06:00:00", "narrative": "A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region. Areas of rain developed across the mountains by late morning, and gradually increased in coverage due to the sustained 25 to 30 knot (850mb) moisture inflow. Precipitable water values were observed in the 1.2 to 1.3 inch range through the day into the early morning hours of the 29th, which is around the 75th percentile for late May. Through the 28th into the early morning hours of the 29th, the upper low drifted eastward, allowing instability to increase across the central Appalachians as the associated pocket of cooler upper level temperatures approached. While Surface-based CAPE levels remained minimal during the event, Most-Unstable CAPE (MUCAPE) values were observed climbing across the mountains through the evening of the 28th into morning of the 29th, reaching into the 600 to 850 J/Kg range. Combined with orographic lift, this instability supported the development of low-topped thunderstorms with enhanced rainfall rates.  As rainfall totals increased across the mountains and soils approached saturation, flash flood guidance values were lowered to under an inch at the 1- and 3-hour time periods. Training of low-topped cells passed across the Bluefield area between 6 AM and 7 AM with sustained 1.5 to locally 2 inch per hour rates. High runoff resulted in rapid street flooding, with water then quickly surrounding and entering homes. Between 500 and 1,000 homes received some form of water damage. The heavy rain then led to flooding of the Bluestone and East Rivers. The Cooperative Weather Observer at Bluefield, WV (BLFW2) observed a 2-day rainfall total of 4.58 inches.  Dating back to December 1998, this is the highest 2-day total in the history of this Cooperative Observer station.", "ts_dict_index": [6642, 6643, 6644]}
+{"event_id": 1093254, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2023-05-27 23:00:00", "end_date_time": "2023-05-29 23:00:00", "narrative": "A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region. Areas of rain developed across the mountains by late morning, and gradually increased in coverage due to the sustained 25 to 30 knot (850mb) moisture inflow. Precipitable water values were observed in the 1.2 to 1.3 inch range through the day into the early morning hours of the 29th, which is around the 75th percentile for late May. Through the 28th into the early morning hours of the 29th, the upper low drifted eastward, allowing instability to increase across the central Appalachians as the associated pocket of cooler upper level temperatures approached. While Surface-based CAPE levels remained minimal during the event, Most-Unstable CAPE (MUCAPE) values were observed climbing across the mountains through the evening of the 28th into morning of the 29th, reaching into the 600 to 850 J/Kg range. Combined with orographic lift, this instability supported the development of low-topped thunderstorms with enhanced rainfall rates.  As rainfall totals increased across the mountains and soils approached saturation, flash flood guidance values were lowered to under an inch at the 1- and 3-hour time periods. Training of low-topped cells passed across the Bluefield area between 6 AM and 7 AM with sustained 1.5 to locally 2 inch per hour rates. High runoff resulted in rapid street flooding, with water then quickly surrounding and entering homes. Between 500 and 1,000 homes received some form of water damage. The heavy rain then led to flooding of the Bluestone and East Rivers. The ASOS (Automated Surface Observing Station) at the Mercer County Regional Airport (KBLF) recorded a 48-hour rainfall total of 4.45 inches.  This includes a 3-hour total of 1.86 inches that fell between around 530 AM and 830 AM EST, which is between a 5-year (20% AEP) and a 10-year (10% AEP) Average Recurrence Interval event per NOAA Atlas 14 Point Precipitation Frequency estimates. This is the second highest two-day total of rainfall for this station since September 1959.", "ts_dict_index": [6645, 6646, 6647]}
+{"event_id": 1092237, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2023-05-28 11:00:00", "end_date_time": "2023-05-29 12:00:00", "narrative": "A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region. Areas of rain developed across the mountains by late morning, and gradually increased in coverage due to the sustained 25 to 30 knot (850mb) moisture inflow. Precipitable water values were observed in the 1.2 to 1.3 inch range through the day into the early morning hours of the 29th, which is around the 75th percentile for late May. Through the 28th into the early morning hours of the 29th, the upper low drifted eastward, allowing instability to increase across the central Appalachians as the associated pocket of cooler upper level temperatures approached. While Surface-based CAPE levels remained minimal during the event, Most-Unstable CAPE (MUCAPE) values were observed climbing across the mountains through the evening of the 28th into morning of the 29th, reaching into the 600 to 850 J/Kg range. Combined with orographic lift, this instability supported the development of low-topped thunderstorms with enhanced rainfall rates.  As rainfall totals increased across the mountains and soils approached saturation, flash flood guidance values were lowered to under an inch at the 1- and 3-hour time periods. Training of low-topped cells passed across the Bluefield area between 6 AM and 7 AM with sustained 1.5 to locally 2 inch per hour rates. High runoff resulted in rapid street flooding, with water then quickly surrounding and entering homes. Between 500 and 1,000 homes received some form of water damage. The heavy rain then led to flooding of the Bluestone and East Rivers. A personal weather station (Weather Underground: KWVBLUEF26) recorded a 24-rainfall amount of 4.48 inches. This is about a 50-year Average Recurrence Interval event per NOAA Atlas 14 Point Precipitation Frequency estimates. Runoff from this location flows into the East River.", "ts_dict_index": [6648, 6649, 6650]}
+{"event_id": 1093253, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2023-05-28 11:00:00", "end_date_time": "2023-05-29 11:00:00", "narrative": "A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region. Areas of rain developed across the mountains by late morning, and gradually increased in coverage due to the sustained 25 to 30 knot (850mb) moisture inflow. Precipitable water values were observed in the 1.2 to 1.3 inch range through the day into the early morning hours of the 29th, which is around the 75th percentile for late May. Through the 28th into the early morning hours of the 29th, the upper low drifted eastward, allowing instability to increase across the central Appalachians as the associated pocket of cooler upper level temperatures approached. While Surface-based CAPE levels remained minimal during the event, Most-Unstable CAPE (MUCAPE) values were observed climbing across the mountains through the evening of the 28th into morning of the 29th, reaching into the 600 to 850 J/Kg range. Combined with orographic lift, this instability supported the development of low-topped thunderstorms with enhanced rainfall rates.  As rainfall totals increased across the mountains and soils approached saturation, flash flood guidance values were lowered to under an inch at the 1- and 3-hour time periods. Training of low-topped cells passed across the Bluefield area between 6 AM and 7 AM with sustained 1.5 to locally 2 inch per hour rates. High runoff resulted in rapid street flooding, with water then quickly surrounding and entering homes. Between 500 and 1,000 homes received some form of water damage. The heavy rain then led to flooding of the Bluestone and East Rivers. A personal weather station (Weather Underground: KWVPRINC14) recorded a 24-rainfall amount of 3.48 inches. This is about a 10-year (10% AEP) Average Recurrence Interval event per NOAA Atlas 14 Point Precipitation Frequency estimates. This includes about one inch that fell between 7am and 8am on the 29th, with rainfall rates of up to 1.5 inches per hour during this time.  Runoff from this location flows into Brush Creek.", "ts_dict_index": [6651, 6652, 6653]}
+{"event_id": 1020561, "event_type": "Hail", "state": "TEXAS", "cz_name": "BELL", "begin_date_time": "2022-04-12 17:06:00", "end_date_time": "2022-04-12 17:06:00", "narrative": "Thunderstorms developed along a dryline across the Big Country the afternoon of Tuesday April 12, then spread east across North and Central Texas, producing all modes of severe weather. Extremely large hail occurred over parts of our Central Texas counties, where a record-breaking hailstone over 5.6 inches in length was documented in the Salado area of Bell County. This hailstone is now the largest recorded hailstone in our CWA to date. Two tornadoes also occurred across Central Texas in Bell County. An EF-3 tornado started in Williamson County and moved northeast and then northerly across the Salado area. Twenty-three people were injured but no fatalities occurred. Additional storms developed overnight into Wednesday as a cold front pushed through the area, some of which also became severe. A public report indicated quarter sized hail just south of Fort Hood in Bell County.", "ts_dict_index": [6594, 6595, 6596]}
+{"event_id": 859260, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-10-01 05:00:00", "end_date_time": "2019-10-02 05:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 2.10 inches over the past 24 hours.", "ts_dict_index": [6678, 6679, 6680]}
+{"event_id": 859273, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-10-01 06:00:00", "end_date_time": "2019-10-02 06:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 3.40 inches over the past 24 hours.", "ts_dict_index": [6672, 6673, 6674]}
+{"event_id": 859281, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 06:00:00", "end_date_time": "2019-10-02 06:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 2.22 inches over the past 24 hours.", "ts_dict_index": [6684, 6685, 6686]}
+{"event_id": 1078286, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2023-02-16 07:00:00", "end_date_time": "2023-02-18 07:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of western Virginia. Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area. However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior. On the morning of the 16th, western Virginia was located on the south side of a stationary front draped near the Ohio River. Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th. PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain. Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough. Total rainfall amounts through the event ranged from 1.75 to locally 2.50 inches, resulting in minor river flooding along the Cowpasture, Bluestone and Clinch Rivers.  Other smaller tributaries experienced minor flooding as well.  Multiple other rivers and creeks rose to Action stage, but remained within their banks.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. The Cooperative Weather Observer at Burkes Garden, VA (BURV2) recorded 1.65 inches or rain during a 2-day period ending at 7 am EST on February 18th.", "ts_dict_index": [6660, 6661, 6662]}
+{"event_id": 859262, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-10-01 15:30:00", "end_date_time": "2019-10-01 23:30:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. Retired NWS employee reported heavy rainfall of 2.70 inches. Beginning and ending times estimated from radar.", "ts_dict_index": [6681, 6682, 6683]}
+{"event_id": 859282, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 06:00:00", "end_date_time": "2019-10-02 06:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 2.58 inches over the past 24 hours.", "ts_dict_index": [6687, 6688, 6689]}
+{"event_id": 859259, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-10-01 04:00:00", "end_date_time": "2019-10-02 04:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 2.17 inches over the past 24 hours.", "ts_dict_index": [6675, 6676, 6677]}
+{"event_id": 1078285, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2023-02-16 07:00:00", "end_date_time": "2023-02-17 08:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of western Virginia. Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area. However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior. On the morning of the 16th, western Virginia was located on the south side of a stationary front draped near the Ohio River. Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th. PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain. Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough. Total rainfall amounts through the event ranged from 1.75 to locally 2.50 inches, resulting in minor river flooding along the Cowpasture, Bluestone and Clinch Rivers.  Other smaller tributaries experienced minor flooding as well.  Multiple other rivers and creeks rose to Action stage, but remained within their banks.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. A personal weather station (Weather Underground:KVANORTH36) near North Tazewell, VA recorded 1.91 inches of rainfall during at 25 hour period ending 8:00 AM EST on 2/17/2023. This was across ground already highly moistened from periods of heavy rain during the 12th & 13th a few days before. Rainfall rates at times were observed up to 0.5 inch per hour. This amount was a 1-year event (100% AEP) per NOAA Atlas 14 point precipitation frequency estimates. Runoff from this location flows into the Clinch River.", "ts_dict_index": [6666, 6667, 6668]}
+{"event_id": 859268, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 15:30:00", "end_date_time": "2019-10-01 23:30:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. Public reported storm total heavy rainfall of 2.5 inches. Beginning and ending times estimated from radar.", "ts_dict_index": [6669, 6670, 6671]}
+{"event_id": 1128955, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2023-08-27 11:00:00", "end_date_time": "2023-08-28 11:00:00", "narrative": "A series of training thunderstorms produced extremely high rainfall across portions of Patrick and Carroll Counties during the predawn hours of August 28th. This resulted in areas of flash flooding, mainly in the headwaters of the Smith River and the Ararat River. ||The event began with a stationary front draped near the border of Virginia and North Carolina early on the 28th as an upper level disturbance began passing across the lower Great Lakes, placing the central Appalachians in an area of lift. The disturbance triggered a southeasterly wind shift across the foothills of the Blue Ridge in southern Virginia and northern North Carolina, bringing an increase of deep moisture northeast from the Piedmont of North Carolina. Precipitable water values were estimated to|be 1.9 to 2.1 inches across Patrick and Carroll counties by 3:00 am on the 28th, while Mixed-Layer CAPE values remained around 500 J/Kg through much of the night.||Convection initiated after sunset on the 27th as a few slow-moving showers across southern Patrick County. Coverage and intensity of the slow-moving activity only increased as the evening progressed, with a band of showers and embedded storms forming along the Highway 58 corridor by midnight, that was advancing northeast toward the crest of the Blue Ridge. Deep moisture combined with orographic lift to produce extremely efficient rainfall rates that were, at times, ranging from 3 to 5 inches per hour across Patrick County into neighboring Carroll County. Doppler Radar estimated rainfall totals of nearly 11 inches of rainfall in northern Patrick County across the Smith River basin, which was confirmed by one CoCoRaHS report of 10.70 inches, as well as a Cooperative Observer report from Woolwine of 10.62 inches. The stream gage at the Smith River near Woolwine (SMWV2) rose to 11.04 feet, just above moderate flood stage due to this rainfall, however radar estimates put the highest amounts downstream of this gage.  Few reports of flooding impacts were received, however it was noted that Philpott Reservoir rose 3 feet in response to the inflows from the Smith River. In western Patrick County and southeast Carroll County, 4 to 7 inches of rain fell across the entire headwaters of the Ararat River, with radar estimates of around 9 inches near the town of Ararat, VA. Flash flooding in this area resulted in several roads being destroyed or heavily damaged where they passed over flooded creeks and rivers, including the Ararat River. A personal weather station (Weather Underground: KVADOBYN2) recorded a 24 hour rainfall amount, ending at 11 am EST on the 28th, of 5.90 inches.", "ts_dict_index": [6633, 6634, 6635]}
+{"event_id": 859274, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-10-01 06:00:00", "end_date_time": "2019-10-02 06:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 3.49 inches over the past 24 hours.", "ts_dict_index": [6711, 6712, 6713]}
+{"event_id": 859292, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-10-01 07:00:00", "end_date_time": "2019-10-02 07:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 2.12 inches over the past 24 hours.", "ts_dict_index": [6705, 6706, 6707]}
+{"event_id": 1098997, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2023-05-28 11:00:00", "end_date_time": "2023-05-29 11:00:00", "narrative": "A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region. Areas of rain developed across the mountains by late morning, and gradually increased in coverage due to the sustained 25 to 30 knot (850mb) moisture inflow. Precipitable water values were observed in the 1.2 to 1.3 inch range through the day into the early morning hours of the 29th, which is around the 75th percentile for late May. Through the 28th into the early morning hours of the 29th, the upper low drifted eastward, allowing instability to increase across the central Appalachians as the associated pocket of cooler upper level temperatures approached. While Surface-based CAPE levels remained minimal during the event, Most-Unstable CAPE (MUCAPE) values were observed climbing across the mountains through the evening of the 28th into morning of the 29th, reaching into the 600 to 850 J/Kg range. Combined with orographic lift, this instability supported the development of low-topped thunderstorms with enhanced rainfall rates.  As rainfall totals increased across the mountains and soils approached saturation, flash flood guidance values were lowered to under an inch at the 1- and 3-hour time periods. ||The heavy rain then led to flooding of Wolf Creek and Walker Creek. Elsewhere, training cells across Floyd and Franklin Counties resulted in minor flooding of the South Fork of the Roanoke River, which brought the Roanoke River up to Action Stage as it passed through the Cities of Roanoke and Salem. A personal weather station (Weather Underground: KVABLUEF19) recorded a 24-rainfall amount of 3.29 inches. This is about a 10-year Average Recurrence Interval event per NOAA Atlas 14 Point Precipitation Frequency estimates. Runoff from this location flows into the Bluestone River.", "ts_dict_index": [6723, 6724, 6725]}
+{"event_id": 859290, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 07:00:00", "end_date_time": "2019-10-02 07:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. NWS employee recorded heavy rainfall of 2.48 inches in their rain gage this morning. This is a 24 hour report.", "ts_dict_index": [6720, 6721, 6722]}
+{"event_id": 859277, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 06:00:00", "end_date_time": "2019-10-02 06:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 2.05 inches over the past 24 hours.", "ts_dict_index": [6696, 6697, 6698]}
+{"event_id": 859276, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 06:00:00", "end_date_time": "2019-10-02 06:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 2.14 inches over the past 24 hours.", "ts_dict_index": [6693, 6694, 6695]}
+{"event_id": 859291, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 07:00:00", "end_date_time": "2019-10-02 07:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 3.28 inches over the past 24 hours.", "ts_dict_index": [6690, 6691, 6692]}
+{"event_id": 859289, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 06:54:00", "end_date_time": "2019-10-02 06:54:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. Des Moines International Airport ASOS recorded heavy rainfall of 2.74 inches over the last 24 hours.", "ts_dict_index": [6699, 6700, 6701]}
+{"event_id": 859280, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 06:00:00", "end_date_time": "2019-10-02 06:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 2.32 inches over the past 24 hours.", "ts_dict_index": [6702, 6703, 6704]}
+{"event_id": 859279, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 06:00:00", "end_date_time": "2019-10-02 06:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 2.23 inches over the past 24 hours.", "ts_dict_index": [6714, 6715, 6716]}
+{"event_id": 1078279, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2023-02-16 07:00:00", "end_date_time": "2023-02-17 08:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of western Virginia. Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area. However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior. On the morning of the 16th, western Virginia was located on the south side of a stationary front draped near the Ohio River. Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th. PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain. Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough. Total rainfall amounts through the event ranged from 1.75 to locally 2.50 inches, resulting in minor river flooding along the Cowpasture, Bluestone and Clinch Rivers.  Other smaller tributaries experienced minor flooding as well.  Multiple other rivers and creeks rose to Action stage, but remained within their banks.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. A personal weather station (Weather Underground:KVAJEWEL2) recorded 2.67 inches of rainfall during at 25 hour period ending 8:00 AM EST on 2/17/2023. This was across ground already highly moistened from periods of heavy rain during the 12th & 13th a few days before. Rainfall rates at times were observed up to 0.5 inch per hour. This amount was around a 2-year event (50% AEP) per NOAA Atlas 14 point precipitation frequency estimates. Runoff from this location flows into the Clinch River.", "ts_dict_index": [6663, 6664, 6665]}
+{"event_id": 849764, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2019-08-20 01:15:00", "end_date_time": "2019-08-20 05:00:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. Public reported heavy rainfall of 3.1 inches. Beginning time estimated from radar.", "ts_dict_index": [6756, 6757, 6758]}
+{"event_id": 1077843, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-16 08:00:00", "end_date_time": "2023-02-17 08:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. A personal weather station (Weather Underground:KWVCRAWL8) recorded 2.89 inches of rainfall during at 24 hour period ending 8:00 AM EST on 2/17/2023. This was across ground already highly moistened from periods of heavy rain during the 12th & 13th a few days before. Rainfall rates at times were observed up to 0.5 inch per hour. This amount was between a 2-year and a 5-year event (50%-20% AEP) per NOAA Atlas 14 point precipitation frequency estimates. Runoff from this location flows into the Meadow River.", "ts_dict_index": [6735, 6736, 6737]}
+{"event_id": 1078219, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2023-02-16 07:30:00", "end_date_time": "2023-02-17 08:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. A personal weather station (Weather Underground:KWVBLUEF24) recorded 2.39 inches of rainfall during a little more than 24 hours ending 8:00 AM EST on 2/17/2023. This was across ground already highly moistened from periods of heavy rain during the 12th & 13th a few days before. Rainfall rates at times were observed up to 0.5 inch per hour. This amount was about a 2-year event (50%-10% AEP) per NOAA Atlas 14 point precipitation frequency estimates. Runoff from this location flows into the Bluestone River.", "ts_dict_index": [6744, 6745, 6746]}
+{"event_id": 1098989, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2023-05-28 11:00:00", "end_date_time": "2023-05-29 11:00:00", "narrative": "A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region. Areas of rain developed across the mountains by late morning, and gradually increased in coverage due to the sustained 25 to 30 knot (850mb) moisture inflow. Precipitable water values were observed in the 1.2 to 1.3 inch range through the day into the early morning hours of the 29th, which is around the 75th percentile for late May. Through the 28th into the early morning hours of the 29th, the upper low drifted eastward, allowing instability to increase across the central Appalachians as the associated pocket of cooler upper level temperatures approached. While Surface-based CAPE levels remained minimal during the event, Most-Unstable CAPE (MUCAPE) values were observed climbing across the mountains through the evening of the 28th into morning of the 29th, reaching into the 600 to 850 J/Kg range. Combined with orographic lift, this instability supported the development of low-topped thunderstorms with enhanced rainfall rates.  As rainfall totals increased across the mountains and soils approached saturation, flash flood guidance values were lowered to under an inch at the 1- and 3-hour time periods. ||The heavy rain then led to flooding of Wolf Creek and Walker Creek. Elsewhere, training cells across Floyd and Franklin Counties resulted in minor flooding of the South Fork of the Roanoke River, which brought the Roanoke River up to Action Stage as it passed through the Cities of Roanoke and Salem. A personal weather station (Weather Underground: KVABASTI15) recorded a 24-rainfall amount of 2.38 inches. This is between a 2-year and a 5-year Average Recurrence Interval event per NOAA Atlas 14 Point Precipitation Frequency estimates. Runoff from this location flows into Wolf Creek.", "ts_dict_index": [6732, 6733, 6734]}
+{"event_id": 849793, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-08-20 04:00:00", "end_date_time": "2019-08-20 05:40:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. Trained spotter reported storm total heavy rainfall of 2 inches. Beginning and end times estimated from radar.", "ts_dict_index": [6753, 6754, 6755]}
+{"event_id": 1077841, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-16 08:00:00", "end_date_time": "2023-02-17 08:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. A personal weather station (Weather Underground:KWVWHITE7) recorded 2.35 inches of rainfall during at 24 hour period ending 8:00 AM EST on 2/17/2023. This was across ground already highly moistened from periods of heavy rain during the 12th & 13th a few days before.  Rainfall rates at times were observed between 0.5 inch per hour to nearly an inch per hour. This amount is only a 1-year event per NOAA Atlas 14 point precipitation frequency estimates.  Runoff from this location flows into Anthony Creek.", "ts_dict_index": [6738, 6739, 6740]}
+{"event_id": 1077847, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-16 07:00:00", "end_date_time": "2023-02-17 08:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. A personal weather station (Weather Underground:KWVCHARM1) recorded 3.44 inches of rainfall during at 25 hour period ending 8:00 AM EST on 2/17/2023. This was across ground already highly moistened from periods of heavy rain during the 12th & 13th a few days before. Rainfall rates at times were observed up to 1.5 inch per hour. This amount was between a 5-year and a 10-year event (20%-10% AEP) per NOAA Atlas 14 point precipitation frequency estimates. Runoff from this location flows into the Meadow River.", "ts_dict_index": [6741, 6742, 6743]}
+{"event_id": 849789, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-19 06:00:00", "end_date_time": "2019-08-20 06:00:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. Public reported heavy rainfall of 2.07 inches over the last 24 hours.", "ts_dict_index": [6759, 6760, 6761]}
+{"event_id": 1098203, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2023-05-28 07:00:00", "end_date_time": "2023-05-30 07:00:00", "narrative": "A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region. Areas of rain developed across the mountains by late morning, and gradually increased in coverage due to the sustained 25 to 30 knot (850mb) moisture inflow. Precipitable water values were observed in the 1.2 to 1.3 inch range through the day into the early morning hours of the 29th, which is around the 75th percentile for late May. Through the 28th into the early morning hours of the 29th, the upper low drifted eastward, allowing instability to increase across the central Appalachians as the associated pocket of cooler upper level temperatures approached. While Surface-based CAPE levels remained minimal during the event, Most-Unstable CAPE (MUCAPE) values were observed climbing across the mountains through the evening of the 28th into morning of the 29th, reaching into the 600 to 850 J/Kg range. Combined with orographic lift, this instability supported the development of low-topped thunderstorms with enhanced rainfall rates.  As rainfall totals increased across the mountains and soils approached saturation, flash flood guidance values were lowered to under an inch at the 1- and 3-hour time periods. ||The heavy rain then led to flooding of Wolf Creek and Walker Creek. Elsewhere, training cells across Floyd and Franklin Counties resulted in minor flooding of the South Fork of the Roanoke River, which brought the Roanoke River up to Action Stage as it passed through the Cities of Roanoke and Salem. The Cooperative Weather Observer at Burkes Garden, VA (BURV2) recorded a 48-rainfall amount of 2.84 inches. This is between a 1-year and a 2-year Average Recurrence Interval event per NOAA Atlas 14 Point Precipitation Frequency estimates. Runoff from this location flows into Wolf Creek.", "ts_dict_index": [6729, 6730, 6731]}
+{"event_id": 1077852, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2023-02-16 07:00:00", "end_date_time": "2023-02-17 08:00:00", "narrative": "Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).  Unusual warmth during most of the river meant no frozen ground, snow cover or river ice in the area.  However, MRMS CREST indicated that the ground was still 50 to 75 percent saturated from widespread rainfall during the 12th and 13th, just a few days prior.  On the morning of the 16th, SEWV was located on the south side of a stationary front draped near the Ohio River.  Strong southwesterly windflow carried deep moisture from the Gulf of Mexico across the area, with precipitable water values (PWATs) in excess of 1.0 inch through much of the day on the 16th.  PWATs would increase to around 1.2 inches by sunrise of the 17th, just as a supporting upper level trough began to push across the Appalachian chain.  Rainfall rates were generally under a quarter inch per hour on the 16th, but began to increase during the overnight hours as the trough approached, in some instances exceeding an inch per hour for brief periods of time as a few thunderstorms developed, supported by Most-Unstable Layer CAPE values increasing to over 1,000 J/Kg ahead of the approaching trough.  Total rainfall amounts through the event ranged from 2.25 to locally 3.50 inches, resulting in minor river flooding along the Greenbrier, Bluestone and Meadow Rivers, as well as Anthony Creek.  Other smaller tributaries experienced minor flooding as well.  No flash flooding occurred.  Reported impacts were limited to flooded roads with little to no damage. A personal weather station (Weather Underground:KWVRAINE18) recorded 2.52 inches of rainfall during at 25 hour period ending 8:00 AM EST on 2/17/2023. This was across ground already highly moistened from periods of heavy rain during the 12th & 13th a few days before. Rainfall rates at times were observed up to 0.5 inch per hour. This amount was between a 5-year and a 10-year event (20%-10% AEP) per NOAA Atlas 14 point precipitation frequency estimates. Runoff from this location flows into Sewell Creek.", "ts_dict_index": [6747, 6748, 6749]}
+{"event_id": 849797, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-20 03:45:00", "end_date_time": "2019-08-20 06:15:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. Public reported storm total heavy rainfall of 2.30 inches. Beginning and end time estimated from radar.", "ts_dict_index": [6750, 6751, 6752]}
+{"event_id": 859278, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-10-01 06:00:00", "end_date_time": "2019-10-02 06:00:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. CoCoRaHS observer recorded heavy rainfall of 2.44 inches over the past 24 hours.", "ts_dict_index": [6708, 6709, 6710]}
+{"event_id": 1042271, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2022-07-26 07:00:00", "end_date_time": "2022-07-27 13:00:00", "narrative": "A stationary front was observed situated south of the Ohio River across northern Kentucky and West Virginia during July 26th when an upper level disturbance approached the state from the west late that evening. A 30 to 35 mph nocturnal low level jet developed just south of the boundary, tapping deep moisture in place across central Kentucky, carrying it northeast toward Greenbrier County, resulting in deep moisture convergence across the area. Precipitable water values were estimated to have risen from around 1.7 inches around 10 pm on the 26th to nearly 2 inches by around 6 am on the 27th, or two standard deviations above normal for late July. Given the latent heat of the tropical air being carried toward southeast West Virginia, most-unstable layer CAPE values were estimated to be between 500 and 1,000 J/Kg just after midnight on the 27th. Soils were already moistened from 0.5 to locally 1.5 inches of rain that fell during early afternoon on the 26th when another round of storms developed across the western part of the county beginning around 10 pm. Perhaps enhanced by upsloping as the storms entered the higher terrain across the western half of the county, the low-topped convection proved to be efficient, producing prolonged 1 to 2 inch per hour rainfall rates in multiple waves. The heaviest rainfall began to diminish by 5 am on the 27th, leaving only residual shower activity after dropping a large swath of 2 to over 4 inches within the 7 hour period. A personal weather station (Weather Underground: KWVWILLI26) recorded 5.27 inches of on-and-off rainfall during a 30-hour period, measured from 8 am on the 26th to 2 pm on the 27th. Rainfall rates were observed to be nearly 2 inches per hour at times.", "ts_dict_index": [6789, 6790, 6791]}
+{"event_id": 1042275, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2022-07-26 07:00:00", "end_date_time": "2022-07-27 13:00:00", "narrative": "A stationary front was observed situated south of the Ohio River across northern Kentucky and West Virginia during July 26th when an upper level disturbance approached the state from the west late that evening. A 30 to 35 mph nocturnal low level jet developed just south of the boundary, tapping deep moisture in place across central Kentucky, carrying it northeast toward Greenbrier County, resulting in deep moisture convergence across the area. Precipitable water values were estimated to have risen from around 1.7 inches around 10 pm on the 26th to nearly 2 inches by around 6 am on the 27th, or two standard deviations above normal for late July. Given the latent heat of the tropical air being carried toward southeast West Virginia, most-unstable layer CAPE values were estimated to be between 500 and 1,000 J/Kg just after midnight on the 27th. Soils were already moistened from 0.5 to locally 1.5 inches of rain that fell during early afternoon on the 26th when another round of storms developed across the western part of the county beginning around 10 pm. Perhaps enhanced by upsloping as the storms entered the higher terrain across the western half of the county, the low-topped convection proved to be efficient, producing prolonged 1 to 2 inch per hour rainfall rates in multiple waves. The heaviest rainfall began to diminish by 5 am on the 27th, leaving only residual shower activity after dropping a large swath of 2 to over 4 inches within the 7 hour period. A personal weather station (Weather Underground: KWVCHARM1) recorded 6.23 inches of rainfall during a 30-hour period of on-and-off thunderstorm activity from 8 am on the 26th to 2 pm on the 27th. Rainfall rates at times were 2 to 2.5 inches per hour. Runoff from this location eventually flows into the Meadow River.", "ts_dict_index": [6786, 6787, 6788]}
+{"event_id": 1042245, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2022-07-26 07:00:00", "end_date_time": "2022-07-27 13:00:00", "narrative": "A stationary front was observed situated south of the Ohio River across northern Kentucky and West Virginia during July 26th when an upper level disturbance approached the state from the west late that evening. A 30 to 35 mph nocturnal low level jet developed just south of the boundary, tapping deep moisture in place across central Kentucky, carrying it northeast toward Greenbrier County, resulting in deep moisture convergence across the area. Precipitable water values were estimated to have risen from around 1.7 inches around 10 pm on the 26th to nearly 2 inches by around 6 am on the 27th, or two standard deviations above normal for late July. Given the latent heat of the tropical air being carried toward southeast West Virginia, most-unstable layer CAPE values were estimated to be between 500 and 1,000 J/Kg just after midnight on the 27th. Soils were already moistened from 0.5 to locally 1.5 inches of rain that fell during early afternoon on the 26th when another round of storms developed across the western part of the county beginning around 10 pm. Perhaps enhanced by upsloping as the storms entered the higher terrain across the western half of the county, the low-topped convection proved to be efficient, producing prolonged 1 to 2 inch per hour rainfall rates in multiple waves. The heaviest rainfall began to diminish by 5 am on the 27th, leaving only residual shower activity after dropping a large swath of 2 to over 4 inches within the 7 hour period. A personal weather station (Weather Underground: KWVCRAWL8) recorded 3.70 inches of rainfall during on-and-off thunderstorms from 8 am on the 26th to 2 pm on the 27th. Rainfall rates were observed to be 1.5 to 2 inches per hour at times. Runoff from this location eventually reaches the Meadow River.", "ts_dict_index": [6783, 6784, 6785]}
+{"event_id": 849782, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-08-19 06:00:00", "end_date_time": "2019-08-20 06:00:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. Coop observer recorded heavy rainfall of 2.15 inches over the last 24 hours.", "ts_dict_index": [6768, 6769, 6770]}
+{"event_id": 849773, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-08-20 03:30:00", "end_date_time": "2019-08-20 05:00:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. Trained spotter reported heavy rainfall of 2.55 inches. Beginning and end time estimated from radar.", "ts_dict_index": [6765, 6766, 6767]}
+{"event_id": 849788, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-19 06:00:00", "end_date_time": "2019-08-20 06:00:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. Des Moines International Airport ASOS recorded heavy rainfall of 2.35 inches over the last 24 hours.", "ts_dict_index": [6762, 6763, 6764]}
+{"event_id": 885156, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2020-04-12 06:00:00", "end_date_time": "2020-04-13 06:00:00", "narrative": "A strong cold front extending from a complex surface low pressure system, |brought intense thunderstorms which produced damaging winds and very heavy rain on April 12-13.  The heavy rains resulted from a deep plume of tropical moisture lifted northward ahead of the cold front. Heavy rain began during the evening of April 12th and exited the region shortly after sunrise on the 13th, lasting roughly a 12-hour period. Between 1.5 and 4 inches of rain fell across the mountains and foothills, with pockets of 4 to 7.5 inches observed near the crest of the Blue Ridge. ||Given the heavy rainfall rates, the result was mainly flash flooding of small creeks and streams.  Hardest hit were portions of Watauga County, NC, where 4 to 7.5 inches fell county-wide.  Extensive flooding was observed along the East Fork of the South Fork of the New River, near the Hidden Hills neighborhood.  Multiple homes were evacuated due flooding, with many long-time residents reporting that this event was the highest that river had risen in at least 20 years. Flooding elsewhere across Watauga County was not as severe, with some roads flooded. National Water Model simulations of this basin indicate that the flooding may have risen to a 25 to 50-year recurrence interval.    ||Flooding extended into Ashe County, NC where multiple roads sustained severe damage, being either partially or totally collapsed/washed out where they intersected smaller creeks. Many other counties across the mountains and foothills reported mainly flooded roads with little to no other damage. The CoCoRaHS station at Boone 4.5 SE (NC-WT-24) measured 7.50 inches in 24 hours ending at 600 AM EST. According to NOAA Atlas 14 this falls in the 90 percent confidence interval (7.02 to 8.49 inches) for a 25-year rainfall event (0.04 annual chance of occurrence).", "ts_dict_index": [6777, 6778, 6779]}
+{"event_id": 885159, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2020-04-12 07:00:00", "end_date_time": "2020-04-13 07:00:00", "narrative": "A strong cold front extending from a complex surface low pressure system, |brought intense thunderstorms which produced damaging winds and very heavy rain on April 12-13.  The heavy rains resulted from a deep plume of tropical moisture lifted northward ahead of the cold front. Heavy rain began during the evening of April 12th and exited the region shortly after sunrise on the 13th, lasting roughly a 12-hour period. Between 1.5 and 4 inches of rain fell across the mountains and foothills, with pockets of 4 to 7.5 inches observed near the crest of the Blue Ridge. ||Given the heavy rainfall rates, the result was mainly flash flooding of small creeks and streams.  Hardest hit were portions of Watauga County, NC, where 4 to 7.5 inches fell county-wide.  Extensive flooding was observed along the East Fork of the South Fork of the New River, near the Hidden Hills neighborhood.  Multiple homes were evacuated due flooding, with many long-time residents reporting that this event was the highest that river had risen in at least 20 years. Flooding elsewhere across Watauga County was not as severe, with some roads flooded. National Water Model simulations of this basin indicate that the flooding may have risen to a 25 to 50-year recurrence interval.    ||Flooding extended into Ashe County, NC where multiple roads sustained severe damage, being either partially or totally collapsed/washed out where they intersected smaller creeks. Many other counties across the mountains and foothills reported mainly flooded roads with little to no other damage. The CoCoRaHS station at Boone 4.6 E (NC-WT-37) measured 6.40 inches in 24 hours ending at 600 AM EST. According to NOAA Atlas 14 this falls in the 90 percent confidence interval (5.43 to 6.53 inches) for a 10-year rainfall event (0.1 annual chance of occurrence).", "ts_dict_index": [6771, 6772, 6773]}
+{"event_id": 885158, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2020-04-12 06:00:00", "end_date_time": "2020-04-13 06:00:00", "narrative": "A strong cold front extending from a complex surface low pressure system, |brought intense thunderstorms which produced damaging winds and very heavy rain on April 12-13.  The heavy rains resulted from a deep plume of tropical moisture lifted northward ahead of the cold front. Heavy rain began during the evening of April 12th and exited the region shortly after sunrise on the 13th, lasting roughly a 12-hour period. Between 1.5 and 4 inches of rain fell across the mountains and foothills, with pockets of 4 to 7.5 inches observed near the crest of the Blue Ridge. ||Given the heavy rainfall rates, the result was mainly flash flooding of small creeks and streams.  Hardest hit were portions of Watauga County, NC, where 4 to 7.5 inches fell county-wide.  Extensive flooding was observed along the East Fork of the South Fork of the New River, near the Hidden Hills neighborhood.  Multiple homes were evacuated due flooding, with many long-time residents reporting that this event was the highest that river had risen in at least 20 years. Flooding elsewhere across Watauga County was not as severe, with some roads flooded. National Water Model simulations of this basin indicate that the flooding may have risen to a 25 to 50-year recurrence interval.    ||Flooding extended into Ashe County, NC where multiple roads sustained severe damage, being either partially or totally collapsed/washed out where they intersected smaller creeks. Many other counties across the mountains and foothills reported mainly flooded roads with little to no other damage. The CoCoRaHS station at Blowing Rock 2.2 ENE (NC-WT-10) measured 7.38 inches in 24 hours ending at 600 AM EST. According to NOAA Atlas 14 this falls just below the 90 percent confidence interval (7.40 to 8.94) for a 25-year rainfall event (0.04 annual chance of occurrence).", "ts_dict_index": [6774, 6775, 6776]}
+{"event_id": 884826, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2020-04-12 07:00:00", "end_date_time": "2020-04-13 07:00:00", "narrative": "A strong cold front extending from a complex surface low pressure system, |brought intense thunderstorms which produced damaging winds and very heavy rain on April 12-13.  The heavy rains resulted from a deep plume of tropical moisture lifted northward ahead of the cold front. Heavy rain began during the evening of April 12th and exited the region shortly after sunrise on the 13th, lasting roughly a 12-hour period. Between 1.5 and 4 inches of rain fell across the mountains and foothills, with pockets of 4 to 7.5 inches observed near the crest of the Blue Ridge. ||Given the heavy rainfall rates, the result was mainly flash flooding of small creeks and streams.  Hardest hit were portions of Watauga County, NC, where 4 to 7.5 inches fell county-wide.  Extensive flooding was observed along the East Fork of the South Fork of the New River, near the Hidden Hills neighborhood.  Multiple homes were evacuated due flooding, with many long-time residents reporting that this event was the highest that river had risen in at least 20 years. Flooding elsewhere across Watauga County was not as severe, with some roads flooded. National Water Model simulations of this basin indicate that the flooding may have risen to a 25 to 50-year recurrence interval.    ||Flooding extended into Ashe County, NC where multiple roads sustained severe damage, being either partially or totally collapsed/washed out where they intersected smaller creeks. Many other counties across the mountains and foothills reported mainly flooded roads with little to no other damage. The NWS Cooperative station at Boone 1 SE (BOON7) set a daily April rainfall record of 4.71 inches for the 24-hour period ending 700 AM EST on April 13, 2020. The old record was 3.94 inches on April 24, 2018 (complete data since 1981). It was also the highest April one-day rainfall at Boone if the previous COOP site in the Boone area is included, the old record was 4.68 inches April 5, 1957. The previous site has nearly complete data back to 1929.", "ts_dict_index": [6780, 6781, 6782]}
+{"event_id": 1042261, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2022-07-26 07:00:00", "end_date_time": "2022-07-27 13:00:00", "narrative": "A stationary front was observed situated south of the Ohio River across northern Kentucky and West Virginia during July 26th when an upper level disturbance approached the state from the west late that evening. A 30 to 35 mph nocturnal low level jet developed just south of the boundary, tapping deep moisture in place across central Kentucky, carrying it northeast toward Greenbrier County, resulting in deep moisture convergence across the area. Precipitable water values were estimated to have risen from around 1.7 inches around 10 pm on the 26th to nearly 2 inches by around 6 am on the 27th, or two standard deviations above normal for late July. Given the latent heat of the tropical air being carried toward southeast West Virginia, most-unstable layer CAPE values were estimated to be between 500 and 1,000 J/Kg just after midnight on the 27th. Soils were already moistened from 0.5 to locally 1.5 inches of rain that fell during early afternoon on the 26th when another round of storms developed across the western part of the county beginning around 10 pm. Perhaps enhanced by upsloping as the storms entered the higher terrain across the western half of the county, the low-topped convection proved to be efficient, producing prolonged 1 to 2 inch per hour rainfall rates in multiple waves. The heaviest rainfall began to diminish by 5 am on the 27th, leaving only residual shower activity after dropping a large swath of 2 to over 4 inches within the 7 hour period. A personal weather station (Weather Underground: KWVRENIC7) recorded 4.11 inches of rainfall during a 30-hour period of on-and-off rain from 8 am on the 26th to 2 pm on the 27th. Rainfall rates at times were in excess of 2 inches per hour.", "ts_dict_index": [6792, 6793, 6794]}
+{"event_id": 1042256, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2022-07-26 07:00:00", "end_date_time": "2022-07-27 13:00:00", "narrative": "A stationary front was observed situated south of the Ohio River across northern Kentucky and West Virginia during July 26th when an upper level disturbance approached the state from the west late that evening. A 30 to 35 mph nocturnal low level jet developed just south of the boundary, tapping deep moisture in place across central Kentucky, carrying it northeast toward Greenbrier County, resulting in deep moisture convergence across the area. Precipitable water values were estimated to have risen from around 1.7 inches around 10 pm on the 26th to nearly 2 inches by around 6 am on the 27th, or two standard deviations above normal for late July. Given the latent heat of the tropical air being carried toward southeast West Virginia, most-unstable layer CAPE values were estimated to be between 500 and 1,000 J/Kg just after midnight on the 27th. Soils were already moistened from 0.5 to locally 1.5 inches of rain that fell during early afternoon on the 26th when another round of storms developed across the western part of the county beginning around 10 pm. Perhaps enhanced by upsloping as the storms entered the higher terrain across the western half of the county, the low-topped convection proved to be efficient, producing prolonged 1 to 2 inch per hour rainfall rates in multiple waves. The heaviest rainfall began to diminish by 5 am on the 27th, leaving only residual shower activity after dropping a large swath of 2 to over 4 inches within the 7 hour period. A personal weather station (Weather Underground: KWVRAINE9) recorded 4.19 inches of rainfall during a 30-hour period of on-and-off thunderstorms from 8 am on the 26th to 2 pm on the 27th. Rainfall rates at times exceeded 2 inches per hour.", "ts_dict_index": [6795, 6796, 6797]}
+{"event_id": 1042247, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2022-07-26 07:00:00", "end_date_time": "2022-07-27 13:00:00", "narrative": "A stationary front was observed situated south of the Ohio River across northern Kentucky and West Virginia during July 26th when an upper level disturbance approached the state from the west late that evening. A 30 to 35 mph nocturnal low level jet developed just south of the boundary, tapping deep moisture in place across central Kentucky, carrying it northeast toward Greenbrier County, resulting in deep moisture convergence across the area. Precipitable water values were estimated to have risen from around 1.7 inches around 10 pm on the 26th to nearly 2 inches by around 6 am on the 27th, or two standard deviations above normal for late July. Given the latent heat of the tropical air being carried toward southeast West Virginia, most-unstable layer CAPE values were estimated to be between 500 and 1,000 J/Kg just after midnight on the 27th. Soils were already moistened from 0.5 to locally 1.5 inches of rain that fell during early afternoon on the 26th when another round of storms developed across the western part of the county beginning around 10 pm. Perhaps enhanced by upsloping as the storms entered the higher terrain across the western half of the county, the low-topped convection proved to be efficient, producing prolonged 1 to 2 inch per hour rainfall rates in multiple waves. The heaviest rainfall began to diminish by 5 am on the 27th, leaving only residual shower activity after dropping a large swath of 2 to over 4 inches within the 7 hour period. A personal weather station (Weather Underground: KWVWHITE7) recorded 3.70 inches of rain during a 30-hr period of on and off rainfall from 8 am on 7/26 to 2 pm on 7/27. Rainfall rates were in excess of 2 inches per hour at times during this period.", "ts_dict_index": [6798, 6799, 6800]}
+{"event_id": 1098984, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2023-05-28 11:00:00", "end_date_time": "2023-05-29 11:00:00", "narrative": "A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region. Areas of rain developed across the mountains by late morning, and gradually increased in coverage due to the sustained 25 to 30 knot (850mb) moisture inflow. Precipitable water values were observed in the 1.2 to 1.3 inch range through the day into the early morning hours of the 29th, which is around the 75th percentile for late May. Through the 28th into the early morning hours of the 29th, the upper low drifted eastward, allowing instability to increase across the central Appalachians as the associated pocket of cooler upper level temperatures approached. While Surface-based CAPE levels remained minimal during the event, Most-Unstable CAPE (MUCAPE) values were observed climbing across the mountains through the evening of the 28th into morning of the 29th, reaching into the 600 to 850 J/Kg range. Combined with orographic lift, this instability supported the development of low-topped thunderstorms with enhanced rainfall rates.  As rainfall totals increased across the mountains and soils approached saturation, flash flood guidance values were lowered to under an inch at the 1- and 3-hour time periods. ||The heavy rain then led to flooding of Wolf Creek and Walker Creek. Elsewhere, training cells across Floyd and Franklin Counties resulted in minor flooding of the South Fork of the Roanoke River, which brought the Roanoke River up to Action Stage as it passed through the Cities of Roanoke and Salem. A personal weather station (Weather Underground: KVATAZEW19) recorded a 24-rainfall amount of 2.78 inches. This is between a 2-year and a 5-year Average Recurrence Interval event per NOAA Atlas 14 Point Precipitation Frequency estimates. Runoff from this location flows into Wolf Creek.", "ts_dict_index": [6726, 6727, 6728]}
+{"event_id": 822614, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2019-05-28 00:30:00", "end_date_time": "2019-05-28 18:47:00", "narrative": "The hits just kept on rolling, with yet another pair of rounds of strong to severe storms, heavy rainfall, and flooding. Through much of the end of May, the synoptic setup across the region remained relatively unchanged, including this event. Upper level flow continued to be out of the SW, precipitable water values remained in excess of 1.5 inches, and a relatively stationary boundary remained over the area. In addition to that broad setup, MUCAPE values hovered in the 1000-2000 J/kg range, bulk effective shear was supportive in the 40 to 60 kts range, and low level moisture flow continued to move into the area.  ||The 28th saw two rounds of strong to severe storms move through from the west and southwest, each causing at least a few severe reports and contributing to overall heavy rainfall and eventually flash flooding. Severe reports were generally relegated to west central and southwest Iowa, where storms were strongest and able to utilize the greatest amounts of effective bulk shear, while heavy rainfall and flash flooding prevailed over already wet areas of south-central and southeastern Iowa. Fortunately flash flooding was predominantly relegated to road closures, though some flooding did linger into the 29th.||Note, the morning round of strong to severe storms is covered in another Storm Data event entry (27-28 May 2019). Trained spotter reported heavy rainfall of 3.22 inches. Beginning time estimated from radar.", "ts_dict_index": [6801, 6802, 6803]}
+{"event_id": 971406, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2021-07-09 10:08:00", "end_date_time": "2021-07-10 10:08:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. A 24 hour rain total of 2.40 inches.", "ts_dict_index": [6819, 6820, 6821]}
+{"event_id": 971395, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2021-07-09 06:00:00", "end_date_time": "2021-07-10 06:00:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. A 24 hour rain total of 2.29 inches.", "ts_dict_index": [6831, 6832, 6833]}
+{"event_id": 822613, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2019-05-28 00:30:00", "end_date_time": "2019-05-28 16:42:00", "narrative": "The hits just kept on rolling, with yet another pair of rounds of strong to severe storms, heavy rainfall, and flooding. Through much of the end of May, the synoptic setup across the region remained relatively unchanged, including this event. Upper level flow continued to be out of the SW, precipitable water values remained in excess of 1.5 inches, and a relatively stationary boundary remained over the area. In addition to that broad setup, MUCAPE values hovered in the 1000-2000 J/kg range, bulk effective shear was supportive in the 40 to 60 kts range, and low level moisture flow continued to move into the area.  ||The 28th saw two rounds of strong to severe storms move through from the west and southwest, each causing at least a few severe reports and contributing to overall heavy rainfall and eventually flash flooding. Severe reports were generally relegated to west central and southwest Iowa, where storms were strongest and able to utilize the greatest amounts of effective bulk shear, while heavy rainfall and flash flooding prevailed over already wet areas of south-central and southeastern Iowa. Fortunately flash flooding was predominantly relegated to road closures, though some flooding did linger into the 29th.||Note, the morning round of strong to severe storms is covered in another Storm Data event entry (27-28 May 2019). Trained spotter reported heavy rainfall of 2.20 inches so far today, and 1.7 inches since 330pm. Beginning time estimated from radar.", "ts_dict_index": [6804, 6805, 6806]}
+{"event_id": 971404, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2021-07-09 08:22:00", "end_date_time": "2021-07-10 08:22:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. A 24 hour rain total of 2.67 inches.", "ts_dict_index": [6825, 6826, 6827]}
+{"event_id": 971403, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 23:00:00", "end_date_time": "2021-07-10 07:37:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. Public report of 2.14 inches of rain since midnight, made via social media.", "ts_dict_index": [6828, 6829, 6830]}
+{"event_id": 871056, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2020-02-06 07:00:00", "end_date_time": "2020-02-07 07:00:00", "narrative": "A deep upper-level trough moved slowly across the central and eastern U.S. drawing abundant moisture northward. At the same time, a complex frontal boundary with several waves of low pressure brought repeated rounds of heavy rainfall to the region. Rainfall totals for the 72-hour period ending at 700 AM on February 7th ranged from 2 to 6 inches with isolated higher amounts mainly along the Blue Ridge Mountains, but most of the rain fell within a 48-hour period. Numerous NWS Cooperative stations recorded all time one-day February rainfall amounts ending on the morning of February 6th and/or the 7th, and numerous two-day February records were also set. Some flash flooding occurred early in the the event as higher rates of rainfall were embedded within the overall rain pattern. Numerous rivers and streams flooded, some reaching crests mainly in the 5- to 10-year flood recurrence interval and many roads were flooded. A state of emergency was declared by the Virginia Governor for several counties in southwest Virginia due to the flooding, including Tazewell and Smyth counties. Flooding was most severe along the Clinch River and tributaries in Richlands, VA where a Flash Flood Emergency was issued in consultation with local officials. The NWS Cooperative station at Stuart (STUV2) set a daily February rainfall record of 3.40 inches for the 24-hour period ending 700 AM EST on February 7th. The previous February record was 2.82 inches on Feb. 19, 1927 (nearly complete data since 1923).", "ts_dict_index": [6843, 6844, 6845]}
+{"event_id": 929381, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2020-11-10 07:00:00", "end_date_time": "2020-11-13 07:00:00", "narrative": "One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.  In the wake of high pressure passing east off the mid-Atlantic coast, a plume of deep tropical moisture was rapidly carried inland to the central Appalachians ahead of a slow-moving cold front.  Though this plume was of tropical origin, it was not directly related to Tropical Storm Eta, which was off the coast of southern Florida.  Precipitable Water values were in the extremely high range of 1.9 to 2.2 inches with this airmass, around the 99th percentile for mid-November.  In addition, evapotranspiration was significantly lower than during the previous few months given lower daytime heating and the fact that most vegetation had become dormant for the upcoming winter months.  Despite dry conditions for almost two weeks leading up to the event, numerous instances of flooding and flash flooding occurred as 4 to 6 inches of rain fell across portions of the Piedmont on the 11th, followed by an additional 1 to 3 inches on the 12th.  Some of the activity was convective in nature, producing locally 2 to 4 inch per hour rainfall rates.  The rainfall produces numerous instances of flooding and flash flooding, followed shortly by river flooding. The Cooperative Weather Observer at Woolwine 4 S, VA (WLWV2) observed a 72-hour (ending 12Z on November 13th) precipitation amount of 5.62 inches.  This was the 6th-highest 72-hour total for this station during the month of November.  The 48-hour total (ending 12Z on November 12th) of 5.32 inches was the 4th-highest 48-hour total for November.  Records date back to June 1951.", "ts_dict_index": [6816, 6817, 6818]}
+{"event_id": 971391, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-09 05:35:00", "end_date_time": "2021-07-10 05:35:00", "narrative": "A shortwave pushed across the area in the overnight to morning hours of July 9th, triggering severe storms over portions of western Iowa in the early morning hours. Storms weakened as they moved east into more stable air, however one cell did develop quarter to golf ball sized hail in Adair county.  As the early morning convection continued to weaken and move southeast, additional cells developed in late morning along outflow boundaries left across northern Iowa. By midday a single dominant cell strengthened over central Iowa and dove south southeast. This cell dropped golf ball to baseball sized hail northwest of and across the Des Moines metro through early afternoon. It then dissipated quickly just southeast of the Des Moines metro. The atmosphere recovered through the rest of the afternoon as surface based cape soared to 5000+ J/kg in southwest Iowa paired with 50 knots of 0-6 km shear.  Storms developed once more in the late afternoon across eastern Iowa along the outflow boundary put out by the midday supercell. Though the environment was supportive, no storms reached severe thresholds. Overnight yet another round of convection rolled across southern Iowa, producing heavy rain and pushing all lingering convection across eastern Iowa out of the area. A 24 hour rain total of 2.62 inches.", "ts_dict_index": [6822, 6823, 6824]}
+{"event_id": 875197, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2020-02-05 07:00:00", "end_date_time": "2020-02-07 07:00:00", "narrative": "A deep upper-level trough moved slowly across the central and eastern U.S. drawing abundant moisture northward. At the same time, a complex frontal boundary with several waves of low pressure brought repeated rounds of heavy rainfall to the region. Rainfall totals for the 72-hour period ending at 700 AM on February 7th ranged from 2 to 6 inches with isolated higher amounts mainly along the Blue Ridge Mountains, but most of the rain fell within a 48-hour period. Numerous NWS Cooperative stations recorded all time one-day February rainfall amounts ending on the morning of February 6th and/or the 7th, and numerous two-day February records were also set. Some flash flooding occurred early in the the event as higher rates of rainfall were embedded within the overall rain pattern. Numerous rivers and streams flooded, some reaching crests mainly in the 5- to 10-year flood recurrence interval and many roads were flooded. A state of emergency was declared by the Virginia Governor for several counties in southwest Virginia due to the flooding, including Tazewell and Smyth counties. Flooding was most severe along the Clinch River and tributaries in Richlands, VA where a Flash Flood Emergency was issued in consultation with local officials. The NWS Cooperative station at Meadows of Dan (MODV2) set a date rainfall record of 3.33 inches for the 24-hour period ending 700 AM EST on February 7th. The previous date record was 2.27 inches on Feb. 23, 1984 (nearly complete data since 1951). The station also set a two-day February rainfall record with 5.41 inches for the period ending 700 AM on the 7th, breaking the previous February record of 4.42 inches set Feb. 17-18, 1966.", "ts_dict_index": [6834, 6835, 6836]}
+{"event_id": 929382, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2020-11-10 07:00:00", "end_date_time": "2020-11-13 07:00:00", "narrative": "One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.  In the wake of high pressure passing east off the mid-Atlantic coast, a plume of deep tropical moisture was rapidly carried inland to the central Appalachians ahead of a slow-moving cold front.  Though this plume was of tropical origin, it was not directly related to Tropical Storm Eta, which was off the coast of southern Florida.  Precipitable Water values were in the extremely high range of 1.9 to 2.2 inches with this airmass, around the 99th percentile for mid-November.  In addition, evapotranspiration was significantly lower than during the previous few months given lower daytime heating and the fact that most vegetation had become dormant for the upcoming winter months.  Despite dry conditions for almost two weeks leading up to the event, numerous instances of flooding and flash flooding occurred as 4 to 6 inches of rain fell across portions of the Piedmont on the 11th, followed by an additional 1 to 3 inches on the 12th.  Some of the activity was convective in nature, producing locally 2 to 4 inch per hour rainfall rates.  The rainfall produces numerous instances of flooding and flash flooding, followed shortly by river flooding. The Cooperative Weather Observer at Stuart, VA (STUV2) observed a 72-hour (ending 12Z on November 13th) precipitation amount of 7.30 inches.  This was the highest 72-hour total for this station during the month of November, and the 6th highest all-time.  The 48-hour total (ending 12Z on November 12th) of 6.59 inches was also the highest 48-hour total for November and 4th highest all-time.  The 24-hour total of 5.41 inches measured at 12Z on the 12th is the highest 24-hour measurement for November and 4th-highest all-time 24-hour amount.  All of these amounts are 5- to 10-year ARI events per NOAA Atlas 14 point precipitation estimates.  Records date back to May 1913.", "ts_dict_index": [6807, 6808, 6809]}
+{"event_id": 929785, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2020-11-10 07:00:00", "end_date_time": "2020-11-13 07:00:00", "narrative": "One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.  In the wake of high pressure passing east off the mid-Atlantic coast, a plume of deep tropical moisture was rapidly carried inland to the central Appalachians ahead of a slow-moving cold front.  Though this plume was of tropical origin, it was not directly related to Tropical Storm Eta, which was off the coast of southern Florida.  Precipitable Water values were in the extremely high range of 1.9 to 2.2 inches with this airmass, around the 99th percentile for mid-November.  In addition, evapotranspiration was significantly lower than during the previous few months given lower daytime heating and the fact that most vegetation had become dormant for the upcoming winter months.  Despite dry conditions for almost two weeks leading up to the event, numerous instances of flooding and flash flooding occurred as 4 to 6 inches of rain fell across portions of the Piedmont on the 11th, followed by an additional 1 to 3 inches on the 12th.  Some of the activity was convective in nature, producing locally 2 to 4 inch per hour rainfall rates.  The rainfall produces numerous instances of flooding and flash flooding, followed shortly by river flooding. Personal weather station KVAHILLS8 recorded a 72-hour storm-total rainfall amount, ending 12Z on November 13th, of 5.25 inches.", "ts_dict_index": [6810, 6811, 6812]}
+{"event_id": 929384, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2020-11-10 07:00:00", "end_date_time": "2020-11-13 07:00:00", "narrative": "One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.  In the wake of high pressure passing east off the mid-Atlantic coast, a plume of deep tropical moisture was rapidly carried inland to the central Appalachians ahead of a slow-moving cold front.  Though this plume was of tropical origin, it was not directly related to Tropical Storm Eta, which was off the coast of southern Florida.  Precipitable Water values were in the extremely high range of 1.9 to 2.2 inches with this airmass, around the 99th percentile for mid-November.  In addition, evapotranspiration was significantly lower than during the previous few months given lower daytime heating and the fact that most vegetation had become dormant for the upcoming winter months.  Despite dry conditions for almost two weeks leading up to the event, numerous instances of flooding and flash flooding occurred as 4 to 6 inches of rain fell across portions of the Piedmont on the 11th, followed by an additional 1 to 3 inches on the 12th.  Some of the activity was convective in nature, producing locally 2 to 4 inch per hour rainfall rates.  The rainfall produces numerous instances of flooding and flash flooding, followed shortly by river flooding. The Cooperative Weather Observer at Meadows of Dan, VA (MODV2) observed a 72-hour (ending 12Z on November 13th) precipitation amount of 5.49 inches. This was the 2nd-highest 72-hour total for this station during the month of November.  The 48-hour total (ending 12Z on November 12th) of 5.05 inches was also the highest 48-hour total for November and 10th highest all-time.  The 24-hour total of 5.10 inches measured at 12Z on the 12th is the highest 24-hour measurement for November and 7th-highest all-time 24-hour amount.  All of these amounts are 10- to 25-year ARI events per NOAA Atlas 14 point precipitation estimates.  Records date back to April 1894.", "ts_dict_index": [6813, 6814, 6815]}
+{"event_id": 871062, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2020-02-05 07:00:00", "end_date_time": "2020-02-07 07:00:00", "narrative": "A deep upper-level trough moved slowly across the central and eastern U.S. drawing abundant moisture northward. At the same time, a complex frontal boundary with several waves of low pressure brought repeated rounds of heavy rainfall to the region. Rainfall totals for the 72-hour period ending at 700 AM on February 7th ranged from 2 to 6 inches with isolated higher amounts mainly along the Blue Ridge Mountains, but most of the rain fell within a 48-hour period. Numerous NWS Cooperative stations recorded all time one-day February rainfall amounts ending on the morning of February 6th and/or the 7th, and numerous two-day February records were also set. Some flash flooding occurred early in the the event as higher rates of rainfall were embedded within the overall rain pattern. Numerous rivers and streams flooded, some reaching crests mainly in the 5- to 10-year flood recurrence interval and many roads were flooded. A state of emergency was declared by the Virginia Governor for several counties in southwest Virginia due to the flooding, including Tazewell and Smyth counties. Flooding was most severe along the Clinch River and tributaries in Richlands, VA where a Flash Flood Emergency was issued in consultation with local officials. The NWS Cooperative station at Richlands (RCLV2) set a daily February rainfall record of 2.38 inches for the 24-hour period ending 700 AM EST on February 6th. The previous February record was 2.05 inches on Feb. 11, 2018 (complete data since 1990). This station also set a date record for the 24-hours ending 700 AM on the 7th of 1.05 inches, breaking the old record of 0.90 inches set in 2019. The two-day total of 3.43 inches ending on the 7th was also a February record for the site, beating the previous record of 2.99 inches set the day before, February 6, 2020 and previously in 2018 at 2.59 inches.", "ts_dict_index": [6840, 6841, 6842]}
+{"event_id": 949131, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 08:00:00", "narrative": "Multiple waves of low pressure passing along a cold front approaching from near the Ohio River resulted in several rounds of prolonged and, at times, heavy rain across northern and western portions of Greenbrier County.  In the 72-hour period ending 7 am on March 1st, the northwestern half of the county had received between 2.5 to locally 4 inches of rainfall from shower and thunderstorm activity. Snow pack prior to the arrival of the rainfall was confined to the highest elevations of the western half of the county, where 2 to locally 4 inches was on the ground.  Portions of Pocahontas County to the north, where the upstream reaches of the Greenbrier River are located, had up to 9 inches of snow pack.  Nearly all remaining snow in both counties melted with this rainfall, contributing to the runoff entering the local rivers by the morning of the 1st, when widespread minor to moderate river flooding occurred.  On March 3rd, Gov. Jim Justice included Greenbrier County among eighteen total West Virginia counties in a declared State of Emergency due of the flood damage.  Heavy rain moved south during the early hours of the 1st, impacting Mercer County with more localized flooding that caused a road closure. A local mesonet weather station (KWVPRINC17) recorded 1.02 inches of rain between 9 pm on February 28th and 8 am on March 1st.  The 72-hour storm total rainfall amount for this station, ending 8 am on the 1st, was 2.69 inches.", "ts_dict_index": [6846, 6847, 6848]}
+{"event_id": 846215, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2019-07-18 20:10:00", "end_date_time": "2019-07-18 21:10:00", "narrative": "Several rounds of thunderstorms moved across western Wisconsin during the late evening of July 18th into the early morning hours of July 19th. As the initial round of storms moved through, a brief tornado touched down northeast of Westby (Vernon County). The tornado destroyed a barn, flipped a trailer and damaged numerous trees. A fatal accident occurred near Whitehall (Trempealeau County) during the storms. Authorities indicated that weather was likely a factor in a head-on two vehicle crash. Rainfall totals from the storms ranged from 3 to 5 inches across portions of La Crosse, Monroe and Vernon Counties that resulted in some flash flooding. Campers had to be evacuated from the Kickapoo Valley Reserve. Flood waters covered County Road P north of Coon Valley (Vernon County) and east of Westby (Vernon County) where a mudslide also occurred. U.S. Highway 14 was closed near Coon Valley where flood waters from Coon Creek covered the road.  The initial storms also produced some 60 mph wind gusts near Mindoro (La Crosse County) and Tomah (Monroe County) and blew down trees near Barre Mills (La Crosse County). A fatal accident occurred during a thunderstorm with heavy rain south of Whitehall. Authorities believe weather was a factor in the head-on two vehicle crash. One person was killed with the other driver sustaining serious injuries.", "ts_dict_index": [6876, 6877, 6878]}
+{"event_id": 837957, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2019-06-08 11:00:00", "end_date_time": "2019-06-09 11:00:00", "narrative": "An unusual long-duration event occurred June 7-11 as a very slow-moving upper trough and surface high across New England combined to produce several days of cool-air damming and persistent rainfall along the frontal boundary and in orographically favored areas of the Blue Ridge with the heaviest rainfall focused over eastern Watauga and Ashe and western Wilkes counties where rain gauges showed 2 to 3 inches in the 24-hour period ending at 0800 EDT on June 8th. The rain continued much of the 8th even heavier amounts with an additional 4 to 8 inches across parts of the area and another 2 to 3 inches ending 0700 on the 10th. Numerous official sites set daily rainfall records on both June 8 and June 9. Four-day totals by the morning of the 10th ranged from 5 to 15 inches, with isolated amounts at unofficial sites approaching 20 inches. The tremendous inflow from various tributaries in the upper Yadkin basin pushed the pool elevation at W. Kerr Scott Reservoir (WLKN7) to its highest level since the dam was completed in 1962, reaching 1062.61 feet on June 10th, eclipsing the previous record of 1061.20 feet in November, 1977. The Boone 1 SE COOP station (BOON7) had 4.60 inches in the 24-hour period ending 700 AM EDT on June 9th, the highest ever for a day in June. The old record was 2.81 inches set in 1992.  Nearly complete records date back to 1980 at this site.", "ts_dict_index": [6873, 6874, 6875]}
+{"event_id": 1056650, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2022-11-10 07:00:00", "end_date_time": "2022-11-12 07:00:00", "narrative": "After making landfall along the Florida Panhandle early on November 11th, the remnants of Tropical Storm Nicole progressed north toward far western North Carolina and Virginia. Moisture radiated well ahead of the storm, resulting in light rainfall during early morning hours, which gradually intensified as dawn approached and winds shifted from a east-northeast direction to become increasingly southeasterly by late morning. This direction is favorable for efficient orographic lift along the crest of the Blue Ridge with the southeasterly windflow tapping into deep moisture across the central Carolinas, where precipitable water values were measured in the 1.7 to 1.9 inch range.  Thirty-five to forty-five mph winds carried this moisture toward the mountains.  Rainfall rates for stations along the crest of the Blue Ridge, particularly in northwest North Carolina were observed in the 0.5 to 1 inch per hour range from around sunrise on the 11th until about 3 pm when winds began to shift more southwesterly.  Most significantly-impacted was the headwaters of the Watauga River, with significant flooding was observed along the river in the communities of Valle Crucis and Sugar Grove. A personal weather station (Weather Underground: KNCBLOWI104) recorded a 48-hour storm rainfall total of 5.42 inches. 5 inches fell in a 24 hour period between 4 pm on 11/10 and 4 pm on 11/11, which is between a 2- and 5-year rainfall event per NOAA Atlas 14 Point Precipitation Frequency estimates for this duration.", "ts_dict_index": [6858, 6859, 6860]}
+{"event_id": 1056560, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2022-11-10 07:00:00", "end_date_time": "2022-11-12 07:00:00", "narrative": "After making landfall along the Florida Panhandle early on November 11th, the remnants of Tropical Storm Nicole progressed north toward far western North Carolina and Virginia. Moisture radiated well ahead of the storm, resulting in light rainfall during early morning hours, which gradually intensified as dawn approached and winds shifted from a east-northeast direction to become increasingly southeasterly by late morning. This direction is favorable for efficient orographic lift along the crest of the Blue Ridge with the southeasterly windflow tapping into deep moisture across the central Carolinas, where precipitable water values were measured in the 1.7 to 1.9 inch range.  Thirty-five to forty-five mph winds carried this moisture toward the mountains.  Rainfall rates for stations along the crest of the Blue Ridge, particularly in northwest North Carolina were observed in the 0.5 to 1 inch per hour range from around sunrise on the 11th until about 3 pm when winds began to shift more southwesterly.  Most significantly-impacted was the headwaters of the Watauga River, with significant flooding was observed along the river in the communities of Valle Crucis and Sugar Grove. A personal weather station (Weather Underground: KNCSEVEN24) recorded a 48-hour storm rainfall total of 7.31 inches. 6.06 inches fell in a 24 hour period between 3 pm on 11/10 and 3 pm on 11/11, which is between a 5- and 10-year rainfall event per NOAA Atlas 14 Point Precipitation Frequency estimates for this duration.", "ts_dict_index": [6861, 6862, 6863]}
+{"event_id": 947517, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2021-03-01 00:00:00", "end_date_time": "2021-03-01 07:00:00", "narrative": "Multiple waves of low pressure passing along a cold front approaching from near the Ohio River resulted in several rounds of prolonged and, at times, heavy rain across northern and western portions of Greenbrier County.  In the 72-hour period ending 7 am on March 1st, the northwestern half of the county had received between 2.5 to locally 4 inches of rainfall from shower and thunderstorm activity. Snow pack prior to the arrival of the rainfall was confined to the highest elevations of the western half of the county, where 2 to locally 4 inches was on the ground.  Portions of Pocahontas County to the north, where the upstream reaches of the Greenbrier River are located, had up to 9 inches of snow pack.  Nearly all remaining snow in both counties melted with this rainfall, contributing to the runoff entering the local rivers by the morning of the 1st, when widespread minor to moderate river flooding occurred.  On March 3rd, Gov. Jim Justice included Greenbrier County among eighteen total West Virginia counties in a declared State of Emergency due of the flood damage.  Heavy rain moved south during the early hours of the 1st, impacting Mercer County with more localized flooding that caused a road closure. The Cooperative Weather Observer at Rupert 4N observed a 24-hour rainfall total, ending 12Z (7 am EST) on March 1st, of 2.30 inches.  The 72-hour, storm total rainfall amount, also ending 12Z (7 am EST) on March 1st, was 3.35 inches.", "ts_dict_index": [6849, 6850, 6851]}
+{"event_id": 837983, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2019-06-08 07:00:00", "end_date_time": "2019-06-09 07:00:00", "narrative": "An unusual long-duration event occurred June 7-11 as a very slow-moving upper trough and surface high across New England combined to produce several days of cool-air damming and persistent rainfall along the frontal boundary and in orographically favored areas of the Blue Ridge with the heaviest rainfall focused over eastern Watauga and Ashe and western Wilkes counties where rain gauges showed 2 to 3 inches in the 24-hour period ending at 0800 EDT on June 8th. The rain continued much of the 8th even heavier amounts with an additional 4 to 8 inches across parts of the area and another 2 to 3 inches ending 0700 on the 10th. Numerous official sites set daily rainfall records on both June 8 and June 9. Four-day totals by the morning of the 10th ranged from 5 to 15 inches, with isolated amounts at unofficial sites approaching 20 inches. The tremendous inflow from various tributaries in the upper Yadkin basin pushed the pool elevation at W. Kerr Scott Reservoir (WLKN7) to its highest level since the dam was completed in 1962, reaching 1062.61 feet on June 10th, eclipsing the previous record of 1061.20 feet in November, 1977. The CoCoRaHS station at Boone 4.6 E (NC-WT-37) measured 9.05 inches for the 24 hours ending 700 AM EDT. The 3-day total ending at 700 AM on the 10th was 15.24 inches. This 3-day total is within the 90 percent confidence interval for a 500-year (.002 annual chance occurrence) rainfall event at this location per NOAA Atlas 14.", "ts_dict_index": [6870, 6871, 6872]}
+{"event_id": 1027805, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2022-07-12 19:40:00", "end_date_time": "2022-07-13 00:00:00", "narrative": "A broken line of thunderstorms developed ahead of a cold front extending from a low pressure system over the eastern Great Lakes through the mid-Mississippi River Valley.  Leading up to the event, strong afternoon heating supported surface-based CAPE values rising into the 2,500 to 3,000 J/Kg range, while precipitable water values were observed climbing from 1.4 inches earlier in the day to around 1.8 inches across these counties as southwesterly winds tapped into deep moisture across the Tennessee River Valley, riding in on a 20-25 mph low level jet.  In addition, Meso-Analysis per the Storm Prediction center also indicated wind flow within the lowest several thousand feet of the atmosphere shifting unidirectional from the west, which can contribute to training of thunderstorm cells over an area.  Storms then trained across the northern half of Tazewell County from around 8 pm on the 12th through about 1 am on the 13th, producing rounds of heavy rainfall rates as high as 4 inches per hour.  Two to locally six inches of rain fell across Tazewell County within 6 hours, with the heaviest amounts representing between a 500- and a 1,000-year rainfall event. A personal weather station (Weather Underground: KVAJEWEL2) recorded a storm-total amount of 5.60 inches during a 4 hour and 20 minute period, with 5.08 inches observed falling in a 3-hour period.  Either case represents between a 500- and 1,000-year rainfall event per NOAA Atlas 14 Point Precipitation Frequency estimates.", "ts_dict_index": [6867, 6868, 6869]}
+{"event_id": 1056651, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2022-11-10 07:00:00", "end_date_time": "2022-11-12 07:00:00", "narrative": "After making landfall along the Florida Panhandle early on November 11th, the remnants of Tropical Storm Nicole progressed north toward far western North Carolina and Virginia. Moisture radiated well ahead of the storm, resulting in light rainfall during early morning hours, which gradually intensified as dawn approached and winds shifted from a east-northeast direction to become increasingly southeasterly by late morning. This direction is favorable for efficient orographic lift along the crest of the Blue Ridge with the southeasterly windflow tapping into deep moisture across the central Carolinas, where precipitable water values were measured in the 1.7 to 1.9 inch range.  Thirty-five to forty-five mph winds carried this moisture toward the mountains.  Rainfall rates for stations along the crest of the Blue Ridge, particularly in northwest North Carolina were observed in the 0.5 to 1 inch per hour range from around sunrise on the 11th until about 3 pm when winds began to shift more southwesterly.  Most significantly-impacted was the headwaters of the Watauga River, with significant flooding was observed along the river in the communities of Valle Crucis and Sugar Grove. A personal weather station (Weather Underground: KNCBLOWI92) recorded a 48-hour storm rainfall total of 4.90 inches. 4.50 inches fell in a 24 hour period between 4 pm on 11/10 and 4 pm on 11/11, which is between a 2- and 5-year rainfall event per NOAA Atlas 14 Point Precipitation Frequency estimates for this duration.", "ts_dict_index": [6855, 6856, 6857]}
+{"event_id": 986896, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2021-09-21 20:00:00", "end_date_time": "2021-09-21 23:00:00", "narrative": "Deep tropical moisture associated with the remnants of Tropical Storm Nicholas was lifted northward ahead of a strong cold front.  Precipitable water values ranging from 1.9 to 2.2 inches were carried into southern Virginia during the evening of the 21st. Warm rain processes produced localized rainfall rates of 2- to 3-inches per hour during the late evening of the 21st into early on the 22nd, enhanced by orographic lift up the Blue Ridge.  FLASH (Flooded Locations And Simulated Hydrographs Project) data indicated bands of rainfall were producing amounts of 1.5 times flash flood guidance across Floyd and Montgomery Counties, with 10-year annual return intervals in spots near the crest of the Blue Ridge before rainfall diminished toward dawn.  During late afternoon into the evening on the 22nd, a line of thunderstorms developed further east as the cold front advanced across the mountains.   The line of storms stalled across portions of Botetourt and Bedford Counties, while CAPE values of 1,500 J/Kg, provided enough instability to support rainfall rates of 2 to 3 inches per hour.  Despite antecedent dry conditions, the areas heavy rain was sufficient to produce localized flash flooding. An automated weather station (Weather Underground: KVAHILLS12) observed a 3-hour rainfall total of 4.29 inches, which is between a 50- and a 100-year rainfall event per NOAA Atlas 14 point frequency estimates for this duration. Rainfall rates between this 3-hour period peaked at a little over 2.6 inches per hour, and remained above 1 inch per hour for nearly the entire 3-hour duration.", "ts_dict_index": [6852, 6853, 6854]}
+{"event_id": 874332, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2020-02-05 07:00:00", "end_date_time": "2020-02-06 07:00:00", "narrative": "A deep upper-level trough moved slowly across the central and eastern U.S. drawing abundant moisture northward. At the same time, a complex frontal boundary with several waves of low pressure brought repeated rounds of heavy rainfall to the region. Rainfall totals for the 72-hour period ending at 700 AM on February 7th ranged from 2 to 6 inches with isolated higher amounts mainly along the Blue Ridge Mountains, but most of the rain fell within a 48-hour period. Numerous NWS Cooperative stations recorded all time one-day February rainfall amounts ending on the morning of February 6th and/or the 7th, and numerous two-day February records were also set. Some flash flooding occurred early in the the event as higher rates of rainfall were embedded within the overall rain pattern. Numerous rivers and streams flooded, some reaching crests mainly in the 5- to 10-year flood recurrence interval and many roads were flooded. A state of emergency was declared by the Virginia Governor for several counties in southwest Virginia due to the flooding, including Tazewell and Smyth counties. Flooding was most severe along the Clinch River and tributaries in Richlands, VA where a Flash Flood Emergency was issued in consultation with local officials. The NWS Cooperative station at Burkes Garden (BURV2) set a date rainfall record of 1.86 inches for the 24-hour period ending 700 AM EST on February 6th. The previous February 6th record was 1.608 inches in 2010 (nearly complete data since 1896). This station also set a date record the following day, for the 24-hours ending 700 AM on the 7th of 1.70 inches, breaking the old record of 1.18 inches set in 1965. The two-day total of 3.56 inches was a February record for the site, breaking the previous two-day high of 3.55 inches set in 1897.", "ts_dict_index": [6837, 6838, 6839]}
+{"event_id": 856079, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-09-29 07:00:00", "end_date_time": "2019-09-29 14:30:00", "narrative": "After a moderate to heavy rainfall event providing 2 to 3 inches just prior to this, the pump was primed so to speak for flooding potential. A generally stationary front resided south of the area into Missouri, but upper level and mid level flow strongly suggested storms would track north of the surface boundary and across portions of southern and central Iowa. The initial wave of rain was initiated by a mid-upper level short wave riding the parent flow, triggering storms in the Oklahoma-Kansas region by late morning and traveled northeast throughout the day, eventually reaching Iowa by the late afternoon and evening. The initial round exited and subsided by midnight, only to see a second round initiated by the low level jet back in northeast and central Kansas. That second round made its way into southern Iowa by around 6 am and continued throughout the morning. When all said and done, heavy rainfall in excess of 5 inches was reported in a few locations, as well as multiple reports of flash flooding. Public reported heavy rainfall of 1.50 inches from 8am to 3:30pm.", "ts_dict_index": [6888, 6889, 6890]}
+{"event_id": 858104, "event_type": "Heavy Rain", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2019-09-05 15:00:00", "end_date_time": "2019-09-05 17:00:00", "narrative": "Upper level high pressure centered over the Four Corners ushered in moisture from the southeast into SoCal starting on Labor Day. Monsoon thunderstorms impacted the mountains and deserts September 2 through 5th. The event started with a nocturnal MCS over the Coachella Valley early in the morning on September 2nd, dumping 1-1.5 inches over a couple of hours. Even more thunderstorms formed Monday afternoon, especially in the mountains. Hail was reported on I-8 Monday afternoon. Storms continued each afternoon and evening in the mountains through September 5th. Some thunderstorms even reached the San Diego County coast on September 4th. Widespread outflow wind gusts of 30-45 mph were reported on the coast and in the valleys on September 4th.|At the end of September, 24-26, tropical moisture was wrapped into southern California from a closed upper low. This initially brought Santa Ana winds and very warm temperatures to the coast and on 25-26 brought scattered thunderstorms to the San Diego mountains. The flooding rains were confined to the Mojave Desert and Imperial Valley. Heavy rain for 20 minutes ending at 1515 PST with accumulations around 3/4 of an inch.  Road flooding in Chihuahua Valley.", "ts_dict_index": [6879, 6880, 6881]}
+{"event_id": 856078, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2019-09-28 16:25:00", "end_date_time": "2019-09-29 16:25:00", "narrative": "After a moderate to heavy rainfall event providing 2 to 3 inches just prior to this, the pump was primed so to speak for flooding potential. A generally stationary front resided south of the area into Missouri, but upper level and mid level flow strongly suggested storms would track north of the surface boundary and across portions of southern and central Iowa. The initial wave of rain was initiated by a mid-upper level short wave riding the parent flow, triggering storms in the Oklahoma-Kansas region by late morning and traveled northeast throughout the day, eventually reaching Iowa by the late afternoon and evening. The initial round exited and subsided by midnight, only to see a second round initiated by the low level jet back in northeast and central Kansas. That second round made its way into southern Iowa by around 6 am and continued throughout the morning. When all said and done, heavy rainfall in excess of 5 inches was reported in a few locations, as well as multiple reports of flash flooding. CoCoRaHS observer recorded heavy rainfall of 5.77 inches over the past 24 hours.", "ts_dict_index": [6894, 6895, 6896]}
+{"event_id": 1109647, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2023-07-12 04:30:00", "end_date_time": "2023-07-12 10:14:00", "narrative": "Two rounds of convection moved across Iowa in quick succession beginning in the pre-dawn hours of July 12th. This first was an area of convection that developed along an elevated boundary into northwest Iowa. While this area of storms mainly remained sub-severe, severe hail did fall across central Iowa near 6 am. At the same time a MCS moved out of the Dakotas and into western Iowa, moving quickly and eventually merging with the first area of storms. This second round developed into a line of storms with winds gusting up to 70 mph, fueled by the low level jet. Orientation of 0-3 km shear was favorable for quick spin-ups and two weaker tornadoes did form in Cass county that morning. With deep warm cloud layers over 4000 meters and precipitable water nearing 2, areas that received rain in both rounds received two to four inches by the time storms ended late in the morning. An isolated pocket of four to six inches fell in Greene and Boone counties, creating flash flooding in the area. Event total of 2.75 inches.", "ts_dict_index": [6903, 6904, 6905]}
+{"event_id": 856076, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2019-09-28 15:10:00", "end_date_time": "2019-09-29 15:10:00", "narrative": "After a moderate to heavy rainfall event providing 2 to 3 inches just prior to this, the pump was primed so to speak for flooding potential. A generally stationary front resided south of the area into Missouri, but upper level and mid level flow strongly suggested storms would track north of the surface boundary and across portions of southern and central Iowa. The initial wave of rain was initiated by a mid-upper level short wave riding the parent flow, triggering storms in the Oklahoma-Kansas region by late morning and traveled northeast throughout the day, eventually reaching Iowa by the late afternoon and evening. The initial round exited and subsided by midnight, only to see a second round initiated by the low level jet back in northeast and central Kansas. That second round made its way into southern Iowa by around 6 am and continued throughout the morning. When all said and done, heavy rainfall in excess of 5 inches was reported in a few locations, as well as multiple reports of flash flooding. Trained spotter reported a 24 hour heavy rainfall total of 2.09 inches. The two full day total, Saturday and Sunday, was 2.79 inches.", "ts_dict_index": [6891, 6892, 6893]}
+{"event_id": 1019304, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2022-05-23 06:00:00", "end_date_time": "2022-05-24 06:00:00", "narrative": "Tropical moisture was forced northward from the Gulf of Mexico on May 23rd, overrunning a cold front draped across central North Carolina.  High pressure extended southward across the Mid-Atlantic, wedged against the eastern face of the Appalachian chain, resulting in upslope east to southeasterly windflow from the Piedmont into the mountains. Atmospheric moisture was abundant, given strong southerly flow around low pressure near the Gulf coast transporting moist air rapidly northward, resulting in precipitable water values ranging from 1.3 to 1.5 inches across the mountains of West Virginia, roughly 2 standard deviations above normal for the month of May.  Rainfall totals across the East River basin varied from 2.5 to 3.5 inches over an 18 hour period. However, the stabilizing effect of the high pressure kept CAPE values low, strictly limiting to preventing convective development.  As such, rainfall was prolonged, however rainfall rates seldom exceeded 0.5 inches per hour. The Cooperative Weather Observer at Bluefield, WV (BLFW2) observed a 24-hour (ending 11Z on May 24th) precipitation amount of 2.73 inches. This was the 5th-highest 24-hour total for this station all-time, and 2nd highest during the month of May. This 24-hour amount is about a 5-year ARI event per NOAA Atlas 14 point precipitation estimates. Records date back to December 1998.", "ts_dict_index": [6924, 6925, 6926]}
+{"event_id": 1109644, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2023-07-12 04:00:00", "end_date_time": "2023-07-12 09:15:00", "narrative": "Two rounds of convection moved across Iowa in quick succession beginning in the pre-dawn hours of July 12th. This first was an area of convection that developed along an elevated boundary into northwest Iowa. While this area of storms mainly remained sub-severe, severe hail did fall across central Iowa near 6 am. At the same time a MCS moved out of the Dakotas and into western Iowa, moving quickly and eventually merging with the first area of storms. This second round developed into a line of storms with winds gusting up to 70 mph, fueled by the low level jet. Orientation of 0-3 km shear was favorable for quick spin-ups and two weaker tornadoes did form in Cass county that morning. With deep warm cloud layers over 4000 meters and precipitable water nearing 2, areas that received rain in both rounds received two to four inches by the time storms ended late in the morning. An isolated pocket of four to six inches fell in Greene and Boone counties, creating flash flooding in the area. Event total of 3.50 inches.", "ts_dict_index": [6909, 6910, 6911]}
+{"event_id": 1109646, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2023-07-12 04:00:00", "end_date_time": "2023-07-12 09:52:00", "narrative": "Two rounds of convection moved across Iowa in quick succession beginning in the pre-dawn hours of July 12th. This first was an area of convection that developed along an elevated boundary into northwest Iowa. While this area of storms mainly remained sub-severe, severe hail did fall across central Iowa near 6 am. At the same time a MCS moved out of the Dakotas and into western Iowa, moving quickly and eventually merging with the first area of storms. This second round developed into a line of storms with winds gusting up to 70 mph, fueled by the low level jet. Orientation of 0-3 km shear was favorable for quick spin-ups and two weaker tornadoes did form in Cass county that morning. With deep warm cloud layers over 4000 meters and precipitable water nearing 2, areas that received rain in both rounds received two to four inches by the time storms ended late in the morning. An isolated pocket of four to six inches fell in Greene and Boone counties, creating flash flooding in the area. Event total of 3.30 inches.", "ts_dict_index": [6912, 6913, 6914]}
+{"event_id": 856075, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2019-09-28 14:31:00", "end_date_time": "2019-09-29 14:31:00", "narrative": "After a moderate to heavy rainfall event providing 2 to 3 inches just prior to this, the pump was primed so to speak for flooding potential. A generally stationary front resided south of the area into Missouri, but upper level and mid level flow strongly suggested storms would track north of the surface boundary and across portions of southern and central Iowa. The initial wave of rain was initiated by a mid-upper level short wave riding the parent flow, triggering storms in the Oklahoma-Kansas region by late morning and traveled northeast throughout the day, eventually reaching Iowa by the late afternoon and evening. The initial round exited and subsided by midnight, only to see a second round initiated by the low level jet back in northeast and central Kansas. That second round made its way into southern Iowa by around 6 am and continued throughout the morning. When all said and done, heavy rainfall in excess of 5 inches was reported in a few locations, as well as multiple reports of flash flooding. Public reported 24 hour heavy rainfall of 5.90 inches 1 mile south of Bridgeview, near Rathbun Lake.", "ts_dict_index": [6897, 6898, 6899]}
+{"event_id": 1109642, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2023-07-12 04:00:00", "end_date_time": "2023-07-12 08:52:00", "narrative": "Two rounds of convection moved across Iowa in quick succession beginning in the pre-dawn hours of July 12th. This first was an area of convection that developed along an elevated boundary into northwest Iowa. While this area of storms mainly remained sub-severe, severe hail did fall across central Iowa near 6 am. At the same time a MCS moved out of the Dakotas and into western Iowa, moving quickly and eventually merging with the first area of storms. This second round developed into a line of storms with winds gusting up to 70 mph, fueled by the low level jet. Orientation of 0-3 km shear was favorable for quick spin-ups and two weaker tornadoes did form in Cass county that morning. With deep warm cloud layers over 4000 meters and precipitable water nearing 2, areas that received rain in both rounds received two to four inches by the time storms ended late in the morning. An isolated pocket of four to six inches fell in Greene and Boone counties, creating flash flooding in the area. Event total of 2.51 inches.", "ts_dict_index": [6906, 6907, 6908]}
+{"event_id": 998362, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2022-01-01 20:00:00", "end_date_time": "2022-01-02 06:00:00", "narrative": "Deep moisture from the Gulf of Mexico pooled ahead of a slow moving cold front during January 1st into the early morning hours of January 2nd.  Precipitable water values across the upper Clinch River Basin were observed to be in excess of 1.3 inches, which is several standard deviations above the normal value for early January in western Virginia.  This deep moisture resulted in rainfall amounts ranging between 1.87 and 2.10 inches fell across the upper Clinch River basin along Highway 460, with close to 3 inches of rain observed near the community of Jewell Ridge in the northern portion of the basin. All of this rain fell during a 7- to 8-hour period, with rainfall rates seldom exceeding 0.5 inches per hour. Antecedent conditions prior to the event were unusually dry, with low streamflows along the Clinch River and its tributaries, low soil moisture and ground that was not frozen due to unusually warm temperatures through the month of December.  This rainfall resulted in minor flooding along the Clinch River. An automated weather station (Weather Underground: KVAJEWEL2) in the northern part of the Clinch River Basin observed a 10-hour rainfall total, ending 6 AM EST on the 2nd, of 2.88 inches.  This amount is estimated to be between a 5- and 10-year rainfall event per NOAA Atlas 14 point frequency estimates for this duration.", "ts_dict_index": [6885, 6886, 6887]}
+{"event_id": 892083, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2020-05-20 07:00:00", "end_date_time": "2020-05-21 07:00:00", "narrative": "An upper-level low became cut-off over the southern Appalachian region for several days leading to persistent rainfall and eventually some flooding. Four-day (96-hour) rainfall amounts ending at 800 AM EDT on May 22nd ranged from 3 to over 12 inches in the most favored locations. Some of the 11-inch+, 4-day rain totals in Roanoke County were within the 200-year recurrence interval (9.78 to 11.8 inches) per NOAA Atlas 14. The flooding that ensued was almost all in the form of river flooding that took several days to develop. Nearly every major river basin saw some flooding, but the most notable occurred in the New River basin where crests ranged from the 4th to 8th highest on record at the Virginia gaging stations along the river. Stages on the upper New were higher than in October 2018 when the remains of Hurricane Michael transited the region. The incredible rainfall, runoff and numerous debris flows produced widespread damage to roads in the region with VDOT reporting over $5 million in damages. The NWS Cooperative station at Woolwine 4 S (WLWV2) had its wettest May day on record with 5.52 inches for the 24-hour period ending 700 AM EST on May 21st. The previous May record was 3.61 inches on May 12, 1961. An all-time record for 3-day rainfall at 10.25 inches ending 700 AM on May 22nd was also established at this site. For a 3-day period this rainfall total is in the 90 percent confidence interval (9.57 to 11.50 inches) for a 50-year recurrence event (.02 annual exceedance probability). At a 4-day duration this station measured 11.90 inches, the 2nd highest of any 4-day period on record (after September 27-30, 2015 at 13.34 inches).  For a 4-day period this rainfall total is in the 90 percent confidence interval (11.4 to 13.7 inches) for a 100-year recurrence event (.01 annual exceedance probability). Complete data extends back to 1952 at this site. Considerable damage occurred to roads and transportation infrastructure in Patrick County according to VDOT.", "ts_dict_index": [6900, 6901, 6902]}
+{"event_id": 998366, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2022-01-01 07:00:00", "end_date_time": "2022-01-02 07:00:00", "narrative": "Deep moisture from the Gulf of Mexico pooled ahead of a slow moving cold front during January 1st into the early morning hours of January 2nd.  Precipitable water values across the upper Clinch River Basin were observed to be in excess of 1.3 inches, which is several standard deviations above the normal value for early January in western Virginia.  This deep moisture resulted in rainfall amounts ranging between 1.87 and 2.10 inches fell across the upper Clinch River basin along Highway 460, with close to 3 inches of rain observed near the community of Jewell Ridge in the northern portion of the basin. All of this rain fell during a 7- to 8-hour period, with rainfall rates seldom exceeding 0.5 inches per hour. Antecedent conditions prior to the event were unusually dry, with low streamflows along the Clinch River and its tributaries, low soil moisture and ground that was not frozen due to unusually warm temperatures through the month of December.  This rainfall resulted in minor flooding along the Clinch River. The Cooperative Weather Observer at Richlands, VA (RCLV2) observed a 24-hour precipitation total ending 12Z (7:00 AM EST) of 1.84 inches, a new station record total for that date.", "ts_dict_index": [6882, 6883, 6884]}
+{"event_id": 1019962, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2022-05-23 07:00:00", "end_date_time": "2022-05-24 07:00:00", "narrative": "Tropical moisture was forced northward from the Gulf of Mexico on May 23rd, overrunning a cold front draped across central North Carolina. High pressure extended southward across the Mid-Atlantic, wedged against the eastern face of the Appalachian chain, resulting in upslope east to southeasterly windflow from the Piedmont into the mountains. Atmospheric moisture was abundant, given strong southerly flow around low pressure near the Gulf coast transporting moist air rapidly northward, resulting in precipitable water values ranging from 1.3 to 1.5 inches across the mountains of western Virginia, roughly 2 standard deviations above normal for the month of May. Rainfall totals across the Upper Bluestone River and Wolf Creek basins varied from 2.5 to 3.5 inches over an 18 hour period. However, the stabilizing effect of the high pressure limited instability, preventing convective development. As such, rainfall was prolonged, however rainfall rates seldom exceeded 0.5 inches per hour. The Cooperative Weather Observer at Burkes Garden, VA (BURV2) recorded at 24-hour rainfall total of 3.58 inches, which is the highest 1-day total ever for this station during the month of May, and the 6th-highest 1-day total all-time.  This 24-hour rainfall total is between a 5- and a 10-year event per NOAA Atlas 14 Point Precipitation Frequency estimates.  Runoff from this rainfall flows into the headwaters of Wolf Creek.", "ts_dict_index": [6921, 6922, 6923]}
+{"event_id": 1109643, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2023-07-12 04:00:00", "end_date_time": "2023-07-12 08:59:00", "narrative": "Two rounds of convection moved across Iowa in quick succession beginning in the pre-dawn hours of July 12th. This first was an area of convection that developed along an elevated boundary into northwest Iowa. While this area of storms mainly remained sub-severe, severe hail did fall across central Iowa near 6 am. At the same time a MCS moved out of the Dakotas and into western Iowa, moving quickly and eventually merging with the first area of storms. This second round developed into a line of storms with winds gusting up to 70 mph, fueled by the low level jet. Orientation of 0-3 km shear was favorable for quick spin-ups and two weaker tornadoes did form in Cass county that morning. With deep warm cloud layers over 4000 meters and precipitable water nearing 2, areas that received rain in both rounds received two to four inches by the time storms ended late in the morning. An isolated pocket of four to six inches fell in Greene and Boone counties, creating flash flooding in the area. Event total of 2.25 inches.", "ts_dict_index": [6915, 6916, 6917]}
+{"event_id": 859297, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-10-01 07:35:00", "end_date_time": "2019-10-02 07:35:00", "narrative": "A surface low pressure system that moved across South Dakota and Minnesota, dragging behind it a cold front that moved into portions of northwest and central Iowa on the 30th of September. As the surface front moved through Iowa, it stalled out and effectively divided the state in half as it oriented it self from southwest to northeast across the state. While the itself stalled, it separated two distinctly different air masses with temperatures in the 50s to low 70s prevailing on the north side and 80s to around 90 prevailing to the south. Surface moisture was also divided with dew points in the 50s on the cool side and low to mid 70s on the warm side. ||Showers and storms persisted north of the front overnight of the 30th into the 1st and during much of the day of the 1st. That activity yielded little more than periods of moderate to heavy rain and sub-severe thunderstorms. Along and south of the front, thermodynamic and kinematics yielded much more vigorous storms and ultimately heavy rainfall and severe weather. SBCAPE profiles yielded 2000 to 3000+ J/kg by early to mid afternoon along with effective bulk shear around 50 to 60 kts, and persistent strong moisture flow yielding precipitable water values around 1.75 to 2.0 inches. Additionally, in the lowest 1 to 3 km, CAPE values exceed 100 J/kg and was accompanied by enhanced low level helicity due to frontal proximity. As a result, virtually all modes of severe weather were possible. In the end, the majority of reports revolved around severe hail, nearing 3 inches in diameter, and heavy rainfall in excess of 3 to 4 inches. A handful of funnel cloud and damaging wind reports were also received. Perry Municipal Airport AWOS recorded heavy rainfall of 2.07 inches over the last 24 hours.", "ts_dict_index": [6717, 6718, 6719]}
+{"event_id": 1145500, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 02:12:00", "end_date_time": "2023-10-25 02:12:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). An automated weather observation station reported 3.74 inches of rainfall in Blair.", "ts_dict_index": [6930, 6931, 6932]}
+{"event_id": 1056559, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2022-11-10 07:00:00", "end_date_time": "2022-11-12 07:00:00", "narrative": "After making landfall along the Florida Panhandle early on November 11th, the remnants of Tropical Storm Nicole progressed north toward far western North Carolina and Virginia. Moisture radiated well ahead of the storm, resulting in light rainfall during early morning hours, which gradually intensified as dawn approached and winds shifted from a east-northeast direction to become increasingly southeasterly by late morning. This direction is favorable for efficient orographic lift along the crest of the Blue Ridge with the southeasterly windflow tapping into deep moisture across the central Carolinas, where precipitable water values were measured in the 1.7 to 1.9 inch range.  Thirty-five to forty-five mph winds carried this moisture toward the mountains.  Rainfall rates for stations along the crest of the Blue Ridge, particularly in northwest North Carolina were observed in the 0.5 to 1 inch per hour range from around sunrise on the 11th until about 3 pm when winds began to shift more southwesterly.  Most significantly-impacted was the headwaters of the Watauga River, with significant flooding was observed along the river in the communities of Valle Crucis and Sugar Grove. A personal weather station (Weather Underground: KNCBANNE130) recorded a 48-hour storm rainfall total of 8.97 inches.  8.45 inches fell in a 24 hour period between 3 pm on 11/10 and 3 pm on 11/11, which is between a 25- and 50-year rainfall event per NOAA Atlas 14 Point Precipitation Frequency estimates for this duration.", "ts_dict_index": [6864, 6865, 6866]}
+{"event_id": 846113, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-08-18 02:45:00", "end_date_time": "2019-08-18 06:19:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Mesonet station recorded heavy rainfall of 2.03 inches. Beginning time estimated from radar.", "ts_dict_index": [6945, 6946, 6947]}
+{"event_id": 1145488, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 03:30:00", "end_date_time": "2023-10-25 03:30:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). A volunteer observer reported 5.30 inches of rainfall near Ettrick.", "ts_dict_index": [6951, 6952, 6953]}
+{"event_id": 1145533, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-24 22:15:00", "end_date_time": "2023-10-24 22:15:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). An automated weather observation station reported 4.89 inches of rainfall near Centerville.", "ts_dict_index": [6936, 6937, 6938]}
+{"event_id": 1145498, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 03:26:00", "end_date_time": "2023-10-25 03:26:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). An automated weather observation station near Centerville reported 4.24 inches of rainfall.", "ts_dict_index": [6933, 6934, 6935]}
+{"event_id": 1145497, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 03:36:00", "end_date_time": "2023-10-25 03:36:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). An automated weather observation station reported 4.16 inches of rainfall near Centerville.", "ts_dict_index": [6948, 6949, 6950]}
+{"event_id": 846122, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-08-18 02:20:00", "end_date_time": "2019-08-18 07:48:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Public reported heavy rainfall of 2.10 inches. Beginning time estimated from radar.", "ts_dict_index": [6939, 6940, 6941]}
+{"event_id": 846115, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-18 02:20:00", "end_date_time": "2019-08-18 06:20:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Mesonet station recorded heavy rainfall of 2.07 inches. Beginning time estimated from radar.", "ts_dict_index": [6942, 6943, 6944]}
+{"event_id": 1019967, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "TAZEWELL", "begin_date_time": "2022-05-23 07:00:00", "end_date_time": "2022-05-24 07:00:00", "narrative": "Tropical moisture was forced northward from the Gulf of Mexico on May 23rd, overrunning a cold front draped across central North Carolina. High pressure extended southward across the Mid-Atlantic, wedged against the eastern face of the Appalachian chain, resulting in upslope east to southeasterly windflow from the Piedmont into the mountains. Atmospheric moisture was abundant, given strong southerly flow around low pressure near the Gulf coast transporting moist air rapidly northward, resulting in precipitable water values ranging from 1.3 to 1.5 inches across the mountains of western Virginia, roughly 2 standard deviations above normal for the month of May. Rainfall totals across the Upper Bluestone River and Wolf Creek basins varied from 2.5 to 3.5 inches over an 18 hour period. However, the stabilizing effect of the high pressure limited instability, preventing convective development. As such, rainfall was prolonged, however rainfall rates seldom exceeded 0.5 inches per hour. An automated weather station (Weather Underground: KVABLUEF10) observed a 24-hour rainfall total, ending 8 AM EDT, of 3.40 inches. Rainfall rates remained mostly below 0.5 per hour, though at times increased to nearly 1 per hour. This amount is around a 10-year rainfall event per NOAA Atlas 14 point frequency estimates for this duration.", "ts_dict_index": [6918, 6919, 6920]}
+{"event_id": 1145543, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 09:00:00", "end_date_time": "2023-10-25 09:00:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). A volunteer observer reported 2.20 inches of rainfall near Hale.", "ts_dict_index": [6966, 6967, 6968]}
+{"event_id": 1145491, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 06:00:00", "end_date_time": "2023-10-25 06:00:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). A volunteer observer reported 5.20 inches of rainfall near the Town of Trempealeau.", "ts_dict_index": [6975, 6976, 6977]}
+{"event_id": 846135, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-08-18 02:45:00", "end_date_time": "2019-08-18 08:00:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Mesonet station recorded heavy rainfall of 2.11 inches. Beginning and ending times estimated from radar.", "ts_dict_index": [6993, 6994, 6995]}
+{"event_id": 1145537, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 03:34:00", "end_date_time": "2023-10-25 03:34:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). An automated weather observation station reported 2.32 inches of rainfall near Pigeon Falls.", "ts_dict_index": [6960, 6961, 6962]}
+{"event_id": 1145539, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 04:45:00", "end_date_time": "2023-10-25 04:45:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). A volunteer observer reported 2.46 inches of rainfall in Osseo.", "ts_dict_index": [6963, 6964, 6965]}
+{"event_id": 1145535, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 02:17:00", "end_date_time": "2023-10-25 02:17:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). An automated weather observation station reported 2.84 inches of rainfall in Whitehall.", "ts_dict_index": [6957, 6958, 6959]}
+{"event_id": 1145486, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 03:18:00", "end_date_time": "2023-10-25 03:18:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). A volunteer observer reported 3.45 inches of storm total rainfall near Arcadia.", "ts_dict_index": [6972, 6973, 6974]}
+{"event_id": 846139, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-08-18 03:30:00", "end_date_time": "2019-08-18 08:45:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Trained spotter reported heavy rainfall of 2.10 inches. Beginning and ending times estimated from radar.", "ts_dict_index": [6999, 7000, 7001]}
+{"event_id": 846125, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2019-08-18 01:35:00", "end_date_time": "2019-08-18 06:30:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Trained spotter, via social media, reported heavy rainfall of 3.43 inches. Beginning and ending times estimated from radar.", "ts_dict_index": [6996, 6997, 6998]}
+{"event_id": 846133, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-18 02:30:00", "end_date_time": "2019-08-18 07:30:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Public reported heavy rainfall of 2.25 inches. Beginning and ending times estimated from radar.", "ts_dict_index": [6984, 6985, 6986]}
+{"event_id": 846120, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-18 02:20:00", "end_date_time": "2019-08-18 07:25:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Public reported heavy rainfall of 2.25 inches. Beginning time estimated from radar.", "ts_dict_index": [6954, 6955, 6956]}
+{"event_id": 846145, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-18 02:25:00", "end_date_time": "2019-08-18 07:00:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Trained spotter reported heavy rainfall of 2.52 inches. Beginning and ending times estimated from radar.", "ts_dict_index": [6981, 6982, 6983]}
+{"event_id": 846119, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-08-18 02:00:00", "end_date_time": "2019-08-18 07:17:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Public reported heavy rainfall of 2.6 inches from the home weather station. Beginning time estimated from radar.", "ts_dict_index": [6978, 6979, 6980]}
+{"event_id": 846105, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-18 02:25:00", "end_date_time": "2019-08-18 05:59:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Mesonet station recorded heavy rainfall of 2.17 inches. Beginning time estimated from radar.", "ts_dict_index": [6990, 6991, 6992]}
+{"event_id": 1019311, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2022-05-23 07:00:00", "end_date_time": "2022-05-24 07:00:00", "narrative": "Tropical moisture was forced northward from the Gulf of Mexico on May 23rd, overrunning a cold front draped across central North Carolina.  High pressure extended southward across the Mid-Atlantic, wedged against the eastern face of the Appalachian chain, resulting in upslope east to southeasterly windflow from the Piedmont into the mountains. Atmospheric moisture was abundant, given strong southerly flow around low pressure near the Gulf coast transporting moist air rapidly northward, resulting in precipitable water values ranging from 1.3 to 1.5 inches across the mountains of West Virginia, roughly 2 standard deviations above normal for the month of May.  Rainfall totals across the East River basin varied from 2.5 to 3.5 inches over an 18 hour period. However, the stabilizing effect of the high pressure kept CAPE values low, strictly limiting to preventing convective development.  As such, rainfall was prolonged, however rainfall rates seldom exceeded 0.5 inches per hour. An automated weather station (Weather Underground: KNCMOUNT12) observed a 24-hour rainfall total, ending 8 AM EDT, of 3.13 inches, most of which fell in a little over 12 hours.  Rainfall rates remained mostly below 0.5 per hour, but at times were near 1 per hour.  This amount is almost a 10-year rainfall event per NOAA Atlas 14 point frequency estimates for this duration.  Runoff from this rainfall eventually flows into the East River.", "ts_dict_index": [6927, 6928, 6929]}
+{"event_id": 846142, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-08-18 02:00:00", "end_date_time": "2019-08-18 05:00:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Trained spotter reported heavy rainfall of 2.1 inches roughly between 3am and 6am local time.", "ts_dict_index": [7005, 7006, 7007]}
+{"event_id": 846109, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-17 06:00:00", "end_date_time": "2019-08-18 06:00:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. CoCoRaHS observer recorded heavy rainfall of 2.05 inches over the last 24 hours.", "ts_dict_index": [7014, 7015, 7016]}
+{"event_id": 846131, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-18 02:05:00", "end_date_time": "2019-08-18 07:30:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Public reported heavy rainfall of 2.00 inches. Beginning and ending times estimated from radar.", "ts_dict_index": [7002, 7003, 7004]}
+{"event_id": 846098, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-18 02:37:00", "end_date_time": "2019-08-18 03:07:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. CoCoRaHS observer reported heavy rainfall of 1.04 inches in 30 minutes.", "ts_dict_index": [7008, 7009, 7010]}
+{"event_id": 846123, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-18 02:10:00", "end_date_time": "2019-08-18 06:15:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Public reported heavy rainfall of 2.15 inches. Beginning time estimated from radar.", "ts_dict_index": [7011, 7012, 7013]}
+{"event_id": 1145496, "event_type": "Heavy Rain", "state": "WISCONSIN", "cz_name": "TREMPEALEAU", "begin_date_time": "2023-10-25 03:15:00", "end_date_time": "2023-10-25 03:15:00", "narrative": "A series of strong to severe storms traversed western into central Wisconsin from the morning hours of October 24th into October 25th, producing heavy rain and mostly small hail. Rainfall amounts ranged from 2 to 4 inches with highest reports of 6.23 inches in Black River Falls (Jackson County), 5.71 inches near Black River Falls (Jackson County), 5.30 inches in Ettrick (Trempealeau County), and 5.20 inches near Centerville (Trempealeau County). The increased rainfall resulted in flooding over roadways in west-central Wisconsin during the early morning hours of October 25th. A rapid response along the Black River resulted in major to moderate flooding from October 25th through the 27th. The Yellow River in Necedah (Juneau County) also flooded from October 28th into October 30th. Besides heavy rainfall, small hail reports frequented the area, with two severe ping pong sized hail reports recorded in the Town of Trempealeau (Trempealeau County) and Neillsville (Clark County). A volunteer observer reported 4.84 inches of rainfall near Galesville.", "ts_dict_index": [6969, 6970, 6971]}
+{"event_id": 1128094, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 17:30:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILCHICA790, recorded 7.36 inches of storm total rainfall.", "ts_dict_index": [7026, 7027, 7028]}
+{"event_id": 1128103, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 17:30:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILBROOK16, recorded 4.99 inches of storm total rainfall.", "ts_dict_index": [7053, 7054, 7055]}
+{"event_id": 1128099, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 17:30:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILCICER16, recorded 8.96 inches of storm total rainfall.", "ts_dict_index": [7017, 7018, 7019]}
+{"event_id": 1128073, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 00:00:00", "end_date_time": "2023-07-02 11:42:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A member of the public recorded 5.27 inches of rain in Berwyn from the start of the day through roughly 11:30 AM CST.", "ts_dict_index": [7029, 7030, 7031]}
+{"event_id": 1128092, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 14:04:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILCHICA677 , recorded 7.23 inches of rainfall between roughly 6 AM and 2 PM CST.", "ts_dict_index": [7038, 7039, 7040]}
+{"event_id": 1128098, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 17:30:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILCHICA498, recorded 8.12 inches of storm total rainfall.", "ts_dict_index": [7023, 7024, 7025]}
+{"event_id": 1128070, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 00:00:00", "end_date_time": "2023-07-02 11:17:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A personal weather station picked up 4.35 inches of rain from the start of the day through roughly 11AM CST. The owner of the weather station confirmed the observation with a standard rain gauge.", "ts_dict_index": [7041, 7042, 7043]}
+{"event_id": 1128101, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 17:30:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILCHICA920, recorded 5.9 inches of storm total rainfall.", "ts_dict_index": [7047, 7048, 7049]}
+{"event_id": 1128093, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 14:09:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILCICER16 , recorded 8.21 inches of rainfall between roughly 6 AM and 2 PM CST.", "ts_dict_index": [7020, 7021, 7022]}
+{"event_id": 1128074, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 00:00:00", "end_date_time": "2023-07-02 11:58:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. The weather station at the Latin School of Chicago recorded 4.76 inches of rainfall from the start of the day through roughly 12:00 PM CST.", "ts_dict_index": [7044, 7045, 7046]}
+{"event_id": 1128095, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 17:30:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILCHICA656, recorded 6.34 inches of storm total rainfall.", "ts_dict_index": [7050, 7051, 7052]}
+{"event_id": 846104, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-18 02:35:00", "end_date_time": "2019-08-18 05:54:00", "narrative": "An upper level trough was pivoting across the Northern Plains and the Canadian Plains August 17th, with a surface low reflection dragging a cold front through the Dakotas and northern Minnesota.  The aforementioned cold front triggered widespread storms during the afternoon hours of the 17th, slowly propagating eastward. By late evening, a portion of the line of storms formed into an organized linear convective system, with bowing segments, that entered northwest Iowa. Through the overnight hours, the system continued to move across Iowa from northwest to southeast, slowly losing its overall organization and threat for damaging winds. Even though it lost overall strength, with MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.7 inches, and strong low level moisture influx, efficient and heavy rainfall continued as it moved across the state. Many areas received between 2 and 3 inches, with the majority of it falling in around 90 minutes or less. Des Moines International Airport ASOS recorded heavy rainfall of 1.97 inches. Beginning time estimated from radar.", "ts_dict_index": [6987, 6988, 6989]}
+{"event_id": 1128075, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 14:04:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILCHICA498, recorded 6.85 inches of rainfall between roughly 6 AM and 2 PM CST.", "ts_dict_index": [7062, 7063, 7064]}
+{"event_id": 1128096, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 17:30:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILSTICK6, recorded 7.47 inches of storm total rainfall.", "ts_dict_index": [7059, 7060, 7061]}
+{"event_id": 840056, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-07-02 06:46:00", "end_date_time": "2019-07-03 06:46:00", "narrative": "Traditional severe weather parameters were lackluster during this event with MUCAPE values predominantly in the 500 to 1500 J/kg range and negligible effective bulk shear. Even precipitable water values, low level moisture transport, and low level jet strength were on the lower end of the spectrum. One item that was in favor of storm initiation and heavy rainfall though was the presence of a stationary boundary across central Iowa much of July 2nd and 3rd. With the boundary in place and moist low levels, it did not take much to initiate multiple rounds of storms. The primary rounds were seen during the mid to late afternoon on the 2nd, near peak heating, and then overnight, aided by a weak low level jet. By the morning of the 3rd, a number of stations around Fort Dodge and down towards Ames had reported between 2 and 4.5 inches of rainfall. While most locations did not have any water issues, the Fort Dodge urban area did experience a period of flash flooding. Coop observer reported heavy rainfall of 2.47 inches over the last 24 hours.", "ts_dict_index": [7071, 7072, 7073]}
+{"event_id": 1128068, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 09:53:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. The ASOS at Chicago Midway Airport recorded 2.94 inches of rain between approximately 6 AM and 9:50 AM CST. Of those 2.94 inches, 1.6 fell within the latest hour.", "ts_dict_index": [7056, 7057, 7058]}
+{"event_id": 840051, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-07-02 16:00:00", "end_date_time": "2019-07-02 19:55:00", "narrative": "Traditional severe weather parameters were lackluster during this event with MUCAPE values predominantly in the 500 to 1500 J/kg range and negligible effective bulk shear. Even precipitable water values, low level moisture transport, and low level jet strength were on the lower end of the spectrum. One item that was in favor of storm initiation and heavy rainfall though was the presence of a stationary boundary across central Iowa much of July 2nd and 3rd. With the boundary in place and moist low levels, it did not take much to initiate multiple rounds of storms. The primary rounds were seen during the mid to late afternoon on the 2nd, near peak heating, and then overnight, aided by a weak low level jet. By the morning of the 3rd, a number of stations around Fort Dodge and down towards Ames had reported between 2 and 4.5 inches of rainfall. While most locations did not have any water issues, the Fort Dodge urban area did experience a period of flash flooding. Public reported heavy rainfall of 2.60 inches. Beginning time estimated from radar.", "ts_dict_index": [7065, 7066, 7067]}
+{"event_id": 840052, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-07-02 16:00:00", "end_date_time": "2019-07-02 20:00:00", "narrative": "Traditional severe weather parameters were lackluster during this event with MUCAPE values predominantly in the 500 to 1500 J/kg range and negligible effective bulk shear. Even precipitable water values, low level moisture transport, and low level jet strength were on the lower end of the spectrum. One item that was in favor of storm initiation and heavy rainfall though was the presence of a stationary boundary across central Iowa much of July 2nd and 3rd. With the boundary in place and moist low levels, it did not take much to initiate multiple rounds of storms. The primary rounds were seen during the mid to late afternoon on the 2nd, near peak heating, and then overnight, aided by a weak low level jet. By the morning of the 3rd, a number of stations around Fort Dodge and down towards Ames had reported between 2 and 4.5 inches of rainfall. While most locations did not have any water issues, the Fort Dodge urban area did experience a period of flash flooding. Mesonet rain gage along the Des Moines River recorded heavy rainfall of 2.23 inches. Beginning time estimated from radar.", "ts_dict_index": [7080, 7081, 7082]}
+{"event_id": 840048, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-07-02 16:00:00", "end_date_time": "2019-07-02 19:35:00", "narrative": "Traditional severe weather parameters were lackluster during this event with MUCAPE values predominantly in the 500 to 1500 J/kg range and negligible effective bulk shear. Even precipitable water values, low level moisture transport, and low level jet strength were on the lower end of the spectrum. One item that was in favor of storm initiation and heavy rainfall though was the presence of a stationary boundary across central Iowa much of July 2nd and 3rd. With the boundary in place and moist low levels, it did not take much to initiate multiple rounds of storms. The primary rounds were seen during the mid to late afternoon on the 2nd, near peak heating, and then overnight, aided by a weak low level jet. By the morning of the 3rd, a number of stations around Fort Dodge and down towards Ames had reported between 2 and 4.5 inches of rainfall. While most locations did not have any water issues, the Fort Dodge urban area did experience a period of flash flooding. Public reported heavy rainfall of 4.5 inches via rain gage picture. Beginning time estimated from radar.", "ts_dict_index": [7068, 7069, 7070]}
+{"event_id": 840050, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-07-02 16:00:00", "end_date_time": "2019-07-02 19:52:00", "narrative": "Traditional severe weather parameters were lackluster during this event with MUCAPE values predominantly in the 500 to 1500 J/kg range and negligible effective bulk shear. Even precipitable water values, low level moisture transport, and low level jet strength were on the lower end of the spectrum. One item that was in favor of storm initiation and heavy rainfall though was the presence of a stationary boundary across central Iowa much of July 2nd and 3rd. With the boundary in place and moist low levels, it did not take much to initiate multiple rounds of storms. The primary rounds were seen during the mid to late afternoon on the 2nd, near peak heating, and then overnight, aided by a weak low level jet. By the morning of the 3rd, a number of stations around Fort Dodge and down towards Ames had reported between 2 and 4.5 inches of rainfall. While most locations did not have any water issues, the Fort Dodge urban area did experience a period of flash flooding. Public reported heavy rainfall of 2.45 inches via home weather station. Beginning time estimated from radar.", "ts_dict_index": [7083, 7084, 7085]}
+{"event_id": 840057, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2019-07-02 07:00:00", "end_date_time": "2019-07-03 07:00:00", "narrative": "Traditional severe weather parameters were lackluster during this event with MUCAPE values predominantly in the 500 to 1500 J/kg range and negligible effective bulk shear. Even precipitable water values, low level moisture transport, and low level jet strength were on the lower end of the spectrum. One item that was in favor of storm initiation and heavy rainfall though was the presence of a stationary boundary across central Iowa much of July 2nd and 3rd. With the boundary in place and moist low levels, it did not take much to initiate multiple rounds of storms. The primary rounds were seen during the mid to late afternoon on the 2nd, near peak heating, and then overnight, aided by a weak low level jet. By the morning of the 3rd, a number of stations around Fort Dodge and down towards Ames had reported between 2 and 4.5 inches of rainfall. While most locations did not have any water issues, the Fort Dodge urban area did experience a period of flash flooding. Mesonet station recorded heavy rainfall of 2.19 inches over the last 24 hours.", "ts_dict_index": [7074, 7075, 7076]}
+{"event_id": 1128106, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 17:00:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A USGS rain gauge at Cicero recorded 8.6 inches of storm total rainfall.", "ts_dict_index": [7035, 7036, 7037]}
+{"event_id": 824682, "event_type": "Heavy Rain", "state": "MISSOURI", "cz_name": "JASPER", "begin_date_time": "2019-05-22 08:00:00", "end_date_time": "2019-05-23 08:00:00", "narrative": "Multiple rounds of storms producing heavy rainfall, severe winds, hail and tornadoes moved across the Missouri Ozarks from May 20th and into the early morning hours of May 24th as upper level disturbances interacted with a slow moving but powerful storm system over the central Plains. Tornadoes occurred with each round, with the strongest and most numerous tornadoes occurring during the late afternoon and evening of the 22nd. On the anniversary of the Joplin Tornado off 2011, another tornado, rated EF-3 struck the north side of Joplin. This storm system eventually produced subsequent tornadoes in Golden City, Eldon and Jefferson City. Unfortunately there were three fatalities as a result of the tornado in Golden City.  The cumulative rainfall caused areas of flash flooding with some flooding lingering across the region. Some locations in southeastern Kansas and southwestern Missouri reported in excess of 8 inches of rainfall over the 72 hour period. . A public observer measured a 24 hour rainfall total of 4.40 inches. The report was received via social media.", "ts_dict_index": [7119, 7120, 7121]}
+{"event_id": 824626, "event_type": "Heavy Rain", "state": "MISSOURI", "cz_name": "JASPER", "begin_date_time": "2019-05-20 20:30:00", "end_date_time": "2019-05-20 20:30:00", "narrative": "Multiple rounds of storms producing heavy rainfall, severe winds, hail and tornadoes moved across the Missouri Ozarks from May 20th and into the early morning hours of May 24th as upper level disturbances interacted with a slow moving but powerful storm system over the central Plains. Tornadoes occurred with each round, with the strongest and most numerous tornadoes occurring during the late afternoon and evening of the 22nd. On the anniversary of the Joplin Tornado off 2011, another tornado, rated EF-3 struck the north side of Joplin. This storm system eventually produced subsequent tornadoes in Golden City, Eldon and Jefferson City. Unfortunately there were three fatalities as a result of the tornado in Golden City.  The cumulative rainfall caused areas of flash flooding with some flooding lingering across the region. Some locations in southeastern Kansas and southwestern Missouri reported in excess of 8 inches of rainfall over the 72 hour period. . Rainfall of 4.17 inches was reported.", "ts_dict_index": [7095, 7096, 7097]}
+{"event_id": 824669, "event_type": "Heavy Rain", "state": "MISSOURI", "cz_name": "JASPER", "begin_date_time": "2019-05-22 05:53:00", "end_date_time": "2019-05-23 05:53:00", "narrative": "Multiple rounds of storms producing heavy rainfall, severe winds, hail and tornadoes moved across the Missouri Ozarks from May 20th and into the early morning hours of May 24th as upper level disturbances interacted with a slow moving but powerful storm system over the central Plains. Tornadoes occurred with each round, with the strongest and most numerous tornadoes occurring during the late afternoon and evening of the 22nd. On the anniversary of the Joplin Tornado off 2011, another tornado, rated EF-3 struck the north side of Joplin. This storm system eventually produced subsequent tornadoes in Golden City, Eldon and Jefferson City. Unfortunately there were three fatalities as a result of the tornado in Golden City.  The cumulative rainfall caused areas of flash flooding with some flooding lingering across the region. Some locations in southeastern Kansas and southwestern Missouri reported in excess of 8 inches of rainfall over the 72 hour period. . The Joplin (JLN) ASOS recorded a 24 HOUR rianfall accumulation of 3.59 inches.", "ts_dict_index": [7098, 7099, 7100]}
+{"event_id": 824617, "event_type": "Heavy Rain", "state": "MISSOURI", "cz_name": "JASPER", "begin_date_time": "2019-05-20 17:15:00", "end_date_time": "2019-05-20 17:15:00", "narrative": "Multiple rounds of storms producing heavy rainfall, severe winds, hail and tornadoes moved across the Missouri Ozarks from May 20th and into the early morning hours of May 24th as upper level disturbances interacted with a slow moving but powerful storm system over the central Plains. Tornadoes occurred with each round, with the strongest and most numerous tornadoes occurring during the late afternoon and evening of the 22nd. On the anniversary of the Joplin Tornado off 2011, another tornado, rated EF-3 struck the north side of Joplin. This storm system eventually produced subsequent tornadoes in Golden City, Eldon and Jefferson City. Unfortunately there were three fatalities as a result of the tornado in Golden City.  The cumulative rainfall caused areas of flash flooding with some flooding lingering across the region. Some locations in southeastern Kansas and southwestern Missouri reported in excess of 8 inches of rainfall over the 72 hour period. . Rainfall of 2.15 inches was reported over a two hour period.", "ts_dict_index": [7107, 7108, 7109]}
+{"event_id": 824611, "event_type": "Heavy Rain", "state": "MISSOURI", "cz_name": "JASPER", "begin_date_time": "2019-05-20 14:57:00", "end_date_time": "2019-05-20 16:57:00", "narrative": "Multiple rounds of storms producing heavy rainfall, severe winds, hail and tornadoes moved across the Missouri Ozarks from May 20th and into the early morning hours of May 24th as upper level disturbances interacted with a slow moving but powerful storm system over the central Plains. Tornadoes occurred with each round, with the strongest and most numerous tornadoes occurring during the late afternoon and evening of the 22nd. On the anniversary of the Joplin Tornado off 2011, another tornado, rated EF-3 struck the north side of Joplin. This storm system eventually produced subsequent tornadoes in Golden City, Eldon and Jefferson City. Unfortunately there were three fatalities as a result of the tornado in Golden City.  The cumulative rainfall caused areas of flash flooding with some flooding lingering across the region. Some locations in southeastern Kansas and southwestern Missouri reported in excess of 8 inches of rainfall over the 72 hour period. . The Emergency Manager reported rainfall of 1.23 inches over a two hour period.", "ts_dict_index": [7113, 7114, 7115]}
+{"event_id": 824680, "event_type": "Heavy Rain", "state": "MISSOURI", "cz_name": "JASPER", "begin_date_time": "2019-05-22 07:00:00", "end_date_time": "2019-05-23 07:00:00", "narrative": "Multiple rounds of storms producing heavy rainfall, severe winds, hail and tornadoes moved across the Missouri Ozarks from May 20th and into the early morning hours of May 24th as upper level disturbances interacted with a slow moving but powerful storm system over the central Plains. Tornadoes occurred with each round, with the strongest and most numerous tornadoes occurring during the late afternoon and evening of the 22nd. On the anniversary of the Joplin Tornado off 2011, another tornado, rated EF-3 struck the north side of Joplin. This storm system eventually produced subsequent tornadoes in Golden City, Eldon and Jefferson City. Unfortunately there were three fatalities as a result of the tornado in Golden City.  The cumulative rainfall caused areas of flash flooding with some flooding lingering across the region. Some locations in southeastern Kansas and southwestern Missouri reported in excess of 8 inches of rainfall over the 72 hour period. . A CoCoRaHS observer measured a 24 hour rainfall total of 3.30 inches.", "ts_dict_index": [7116, 7117, 7118]}
+{"event_id": 824641, "event_type": "Heavy Rain", "state": "MISSOURI", "cz_name": "JASPER", "begin_date_time": "2019-05-20 06:00:00", "end_date_time": "2019-05-21 05:42:00", "narrative": "Multiple rounds of storms producing heavy rainfall, severe winds, hail and tornadoes moved across the Missouri Ozarks from May 20th and into the early morning hours of May 24th as upper level disturbances interacted with a slow moving but powerful storm system over the central Plains. Tornadoes occurred with each round, with the strongest and most numerous tornadoes occurring during the late afternoon and evening of the 22nd. On the anniversary of the Joplin Tornado off 2011, another tornado, rated EF-3 struck the north side of Joplin. This storm system eventually produced subsequent tornadoes in Golden City, Eldon and Jefferson City. Unfortunately there were three fatalities as a result of the tornado in Golden City.  The cumulative rainfall caused areas of flash flooding with some flooding lingering across the region. Some locations in southeastern Kansas and southwestern Missouri reported in excess of 8 inches of rainfall over the 72 hour period. . Rainfall of 4.64 inches was reported over a 24 hour period.", "ts_dict_index": [7122, 7123, 7124]}
+{"event_id": 840058, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-07-02 07:00:00", "end_date_time": "2019-07-03 07:00:00", "narrative": "Traditional severe weather parameters were lackluster during this event with MUCAPE values predominantly in the 500 to 1500 J/kg range and negligible effective bulk shear. Even precipitable water values, low level moisture transport, and low level jet strength were on the lower end of the spectrum. One item that was in favor of storm initiation and heavy rainfall though was the presence of a stationary boundary across central Iowa much of July 2nd and 3rd. With the boundary in place and moist low levels, it did not take much to initiate multiple rounds of storms. The primary rounds were seen during the mid to late afternoon on the 2nd, near peak heating, and then overnight, aided by a weak low level jet. By the morning of the 3rd, a number of stations around Fort Dodge and down towards Ames had reported between 2 and 4.5 inches of rainfall. While most locations did not have any water issues, the Fort Dodge urban area did experience a period of flash flooding. Mesonet station recorded heavy rainfall of 2.35 inches over the last 24 hours.", "ts_dict_index": [7092, 7093, 7094]}
+{"event_id": 824678, "event_type": "Heavy Rain", "state": "MISSOURI", "cz_name": "JASPER", "begin_date_time": "2019-05-23 07:00:00", "end_date_time": "2019-05-23 07:00:00", "narrative": "Multiple rounds of storms producing heavy rainfall, severe winds, hail and tornadoes moved across the Missouri Ozarks from May 20th and into the early morning hours of May 24th as upper level disturbances interacted with a slow moving but powerful storm system over the central Plains. Tornadoes occurred with each round, with the strongest and most numerous tornadoes occurring during the late afternoon and evening of the 22nd. On the anniversary of the Joplin Tornado off 2011, another tornado, rated EF-3 struck the north side of Joplin. This storm system eventually produced subsequent tornadoes in Golden City, Eldon and Jefferson City. Unfortunately there were three fatalities as a result of the tornado in Golden City.  The cumulative rainfall caused areas of flash flooding with some flooding lingering across the region. Some locations in southeastern Kansas and southwestern Missouri reported in excess of 8 inches of rainfall over the 72 hour period. . A CoCoRaHS observer measured a 24 hour rainfall total of 3.43 inches.", "ts_dict_index": [7101, 7102, 7103]}
+{"event_id": 840053, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-07-02 16:00:00", "end_date_time": "2019-07-02 20:01:00", "narrative": "Traditional severe weather parameters were lackluster during this event with MUCAPE values predominantly in the 500 to 1500 J/kg range and negligible effective bulk shear. Even precipitable water values, low level moisture transport, and low level jet strength were on the lower end of the spectrum. One item that was in favor of storm initiation and heavy rainfall though was the presence of a stationary boundary across central Iowa much of July 2nd and 3rd. With the boundary in place and moist low levels, it did not take much to initiate multiple rounds of storms. The primary rounds were seen during the mid to late afternoon on the 2nd, near peak heating, and then overnight, aided by a weak low level jet. By the morning of the 3rd, a number of stations around Fort Dodge and down towards Ames had reported between 2 and 4.5 inches of rainfall. While most locations did not have any water issues, the Fort Dodge urban area did experience a period of flash flooding. Public reported heavy rainfall of about 3 inches from picture of their rain gage. Beginning time estimated from radar.", "ts_dict_index": [7089, 7090, 7091]}
+{"event_id": 824683, "event_type": "Heavy Rain", "state": "MISSOURI", "cz_name": "JASPER", "begin_date_time": "2019-05-23 00:00:00", "end_date_time": "2019-05-23 08:20:00", "narrative": "Multiple rounds of storms producing heavy rainfall, severe winds, hail and tornadoes moved across the Missouri Ozarks from May 20th and into the early morning hours of May 24th as upper level disturbances interacted with a slow moving but powerful storm system over the central Plains. Tornadoes occurred with each round, with the strongest and most numerous tornadoes occurring during the late afternoon and evening of the 22nd. On the anniversary of the Joplin Tornado off 2011, another tornado, rated EF-3 struck the north side of Joplin. This storm system eventually produced subsequent tornadoes in Golden City, Eldon and Jefferson City. Unfortunately there were three fatalities as a result of the tornado in Golden City.  The cumulative rainfall caused areas of flash flooding with some flooding lingering across the region. Some locations in southeastern Kansas and southwestern Missouri reported in excess of 8 inches of rainfall over the 72 hour period. . The public reported that 5 inches of rain fall across the eastern portions of town.", "ts_dict_index": [7110, 7111, 7112]}
+{"event_id": 824624, "event_type": "Heavy Rain", "state": "MISSOURI", "cz_name": "JASPER", "begin_date_time": "2019-05-20 20:10:00", "end_date_time": "2019-05-20 20:10:00", "narrative": "Multiple rounds of storms producing heavy rainfall, severe winds, hail and tornadoes moved across the Missouri Ozarks from May 20th and into the early morning hours of May 24th as upper level disturbances interacted with a slow moving but powerful storm system over the central Plains. Tornadoes occurred with each round, with the strongest and most numerous tornadoes occurring during the late afternoon and evening of the 22nd. On the anniversary of the Joplin Tornado off 2011, another tornado, rated EF-3 struck the north side of Joplin. This storm system eventually produced subsequent tornadoes in Golden City, Eldon and Jefferson City. Unfortunately there were three fatalities as a result of the tornado in Golden City.  The cumulative rainfall caused areas of flash flooding with some flooding lingering across the region. Some locations in southeastern Kansas and southwestern Missouri reported in excess of 8 inches of rainfall over the 72 hour period. . Daily rainfall of 3.46 inches was reported.", "ts_dict_index": [7104, 7105, 7106]}
+{"event_id": 985026, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-10-24 02:15:00", "end_date_time": "2021-10-25 07:15:00", "narrative": "Southwesterly flow allowed for deep moisture transport from the Gulf coast region and into the Midwest. At the same time a shortwave trough moved across the central plains and into the Midwest. While severe storms were limited by deep saturation and only modest shear, widespread moderate to heavy rain fell across the entire state. Rain began across southern Iowa shortly after midnight on October 24th and quickly expanded across the state through the early morning hours. This rain lasted through the day before tapering off across the state on the morning of October 25th. Widespread rain totals of over 2 inches were common with the heaviest rain falling across southern to eastern Iowa. A few pockets of 3.5 to over 4 inches fell in this region. Thanks to the long duration and antecedent exceedingly dry conditions, there was no flood impact. In fact, even area rivers showed little change as most of the rain soaked into the ground rather than running off. A storm total rainfall of 3.50 inches.", "ts_dict_index": [7125, 7126, 7127]}
+{"event_id": 871009, "event_type": "Heavy Rain", "state": "NORTH CAROLINA", "cz_name": "WATAUGA", "begin_date_time": "2020-02-05 07:00:00", "end_date_time": "2020-02-07 07:00:00", "narrative": "A deep upper-level trough moved slowly across the central and eastern U.S. bringing abundant moisture northward and combined with a complex frontal boundary with several waves of low pressure to bring repeated rounds of heavy rainfall. Rainfall totals for the 72-hour period ending at 700 AM EST on February 7th ranged from 2 to 6 inches with isolated higher amounts along the Blue Ridge Mountains, but most of the rain fell within a 48-hour period. Numerous NWS Cooperative stations reported record one-day February rainfall amounts ending on the morning of February 6th and/or the 7th and numerous two-day all-time February records were also set. Some flash flooding occurred early during the event as higher rates of rainfall were embedded within the overall rain pattern. Numerous rivers and streams flooded, some reaching crests in the 25- to 50-year flood recurrence interval and many roads were flooded with significant damage to some infrastructure. The NWS Cooperative station at Boone 1 SE (BOON7) set a date rainfall record of 1.52 inches for the 24-hour period ending 700 AM EST on February 6th, the old record was 1.37 inches in 2010. The next day the station set a February rainfall record of 4.35 inches for the 24-hour period ending 700 AM EST on February 7th. The previous February record was 3.91 inches on Feb. 14, 1984 (complete data since 1981). It was the 2nd highest February one-day rainfall at Boone if the previous COOP site in Boone is included (after Feb. 13, 1966 with 4.46 inches). That has nearly complete data back to 1929. The two-day rainfall total of 5.87 inches ending 700 AM on the 7th was also a February two-day record at both Boone COOP sites. That broke the old record of 4.06 inches in 1984, which itself was eclipsed the next day, Feb. 8th at 4.46 inches.", "ts_dict_index": [7128, 7129, 7130]}
+{"event_id": 832564, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 19:32:00", "end_date_time": "2019-06-22 22:15:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. KCCI relayed social media report of 4.50 inches of heavy rainfall so far.  Beginning time estimated from radar.", "ts_dict_index": [7137, 7138, 7139]}
+{"event_id": 1128097, "event_type": "Heavy Rain", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2023-07-02 06:00:00", "end_date_time": "2023-07-02 17:30:00", "narrative": "An extreme rainfall event occurred on July 2 in the Chicago metropolitan area caused by multiple nearly stationary bands of showers and thunderstorms near a slow-moving low pressure area. Rainfall occurred over from approximately 12 AM CST to 6 PM CST, with peak rainfall rates exceeding 2 inches per hour and storm total accumulations nearing 9.0 inches in Cook County. Individual showers and thunderstorms moved very slowly during the event, with storm motions of 15 mph or less, leading to extended periods of heavy rainfall. The area of peak rainfall just west of Chicago was estimated to have less than a 1% chance of occurring annually, and led to widespread flooding of basements, streets, and expressways. Also happening on this day was the first annual NASCAR Chicago street race downtown. The storm temporarily flooded portions of the race course, caused a number of delays and cancellations of events, and made conditions terribly slick for the drivers on the course. A private weather station, KILCHICA677, recorded 7.89 inches of storm total rainfall.", "ts_dict_index": [7032, 7033, 7034]}
+{"event_id": 832572, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 06:00:00", "end_date_time": "2019-06-23 06:00:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. CoCoRaHS report of heavy rainfall of 2.32 inches over the last 24 hours.", "ts_dict_index": [7140, 7141, 7142]}
+{"event_id": 840055, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-07-02 16:00:00", "end_date_time": "2019-07-02 20:45:00", "narrative": "Traditional severe weather parameters were lackluster during this event with MUCAPE values predominantly in the 500 to 1500 J/kg range and negligible effective bulk shear. Even precipitable water values, low level moisture transport, and low level jet strength were on the lower end of the spectrum. One item that was in favor of storm initiation and heavy rainfall though was the presence of a stationary boundary across central Iowa much of July 2nd and 3rd. With the boundary in place and moist low levels, it did not take much to initiate multiple rounds of storms. The primary rounds were seen during the mid to late afternoon on the 2nd, near peak heating, and then overnight, aided by a weak low level jet. By the morning of the 3rd, a number of stations around Fort Dodge and down towards Ames had reported between 2 and 4.5 inches of rainfall. While most locations did not have any water issues, the Fort Dodge urban area did experience a period of flash flooding. Public reported heavy rainfall of 3.8 inches via picture of rain gage. Beginning time estimated from radar.", "ts_dict_index": [7077, 7078, 7079]}
+{"event_id": 832570, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 06:00:00", "end_date_time": "2019-06-23 06:00:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. Des Moines International Airport ASOS recorded heavy rainfall of 2.48 inches over the last 24 hours.", "ts_dict_index": [7152, 7153, 7154]}
+{"event_id": 832571, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 06:00:00", "end_date_time": "2019-06-23 06:00:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. CoCoRaHS report of heavy rainfall of 2.06 inches over the last 24 hours.", "ts_dict_index": [7155, 7156, 7157]}
+{"event_id": 832562, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 19:52:00", "end_date_time": "2019-06-22 21:20:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. Public reported heavy rainfall of 4.60 inches so far today. Beginning time estimated from radar.", "ts_dict_index": [7146, 7147, 7148]}
+{"event_id": 832554, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 19:56:00", "end_date_time": "2019-06-22 20:56:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. Broadcast media relayed heavy rainfall of 2.39 inches in one hour.", "ts_dict_index": [7149, 7150, 7151]}
+{"event_id": 832573, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 06:00:00", "end_date_time": "2019-06-23 06:00:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. Public report of heavy rainfall of 3.72 inches over the last 24 hours.", "ts_dict_index": [7161, 7162, 7163]}
+{"event_id": 832575, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 06:00:00", "end_date_time": "2019-06-23 06:00:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. CoCoRaHS report of heavy rainfall of 2.37 inches over the last 24 hours.", "ts_dict_index": [7164, 7165, 7166]}
+{"event_id": 832551, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 19:50:00", "end_date_time": "2019-06-22 20:54:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. Trained spotter reported heavy rainfall of about 3.80 inches. Beginning time estimated from radar.", "ts_dict_index": [7158, 7159, 7160]}
+{"event_id": 840054, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-07-02 16:00:00", "end_date_time": "2019-07-02 20:01:00", "narrative": "Traditional severe weather parameters were lackluster during this event with MUCAPE values predominantly in the 500 to 1500 J/kg range and negligible effective bulk shear. Even precipitable water values, low level moisture transport, and low level jet strength were on the lower end of the spectrum. One item that was in favor of storm initiation and heavy rainfall though was the presence of a stationary boundary across central Iowa much of July 2nd and 3rd. With the boundary in place and moist low levels, it did not take much to initiate multiple rounds of storms. The primary rounds were seen during the mid to late afternoon on the 2nd, near peak heating, and then overnight, aided by a weak low level jet. By the morning of the 3rd, a number of stations around Fort Dodge and down towards Ames had reported between 2 and 4.5 inches of rainfall. While most locations did not have any water issues, the Fort Dodge urban area did experience a period of flash flooding. WHO TV relayed a viewer report of heavy rainfall of about 3 inches. Report came in via social media. Beginning time estimated from radar.", "ts_dict_index": [7086, 7087, 7088]}
+{"event_id": 832577, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-06-22 06:00:00", "end_date_time": "2019-06-23 06:00:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. CoCoRaHS report of heavy rainfall of 2.19 inches over the last 24 hours.", "ts_dict_index": [7167, 7168, 7169]}
+{"event_id": 832530, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-06-21 04:00:00", "end_date_time": "2019-06-21 12:00:00", "narrative": "Periods of moderate to heavy rainfall are not uncommon throughout the spring and summer months, but given the very wet spring across Iowa, soils were primed and unable to hold copious amounts of new rainfall. The overall setup for this event was somewhat typical with a shortwave moving through the parent flow, and 850 mb low level jet aiding in convective initiation and moisture transport, precipitable water values around 1.5 to 1.75 inches, and other marginal supporting factors. ||Convection initiated across portions of southwest Nebraska and northwest Kansas late in the evening on the 20th and quickly propagated eastward through the overnight and morning hours. Eventually, two decaying waves of storms moved through portions of western Iowa and predominantly provided small hail and efficient heavy rainfall. A few locations reported as much as 3 to 5 inches of rainfall, which helped initiate flash flooding in the area. Trained spotter reported heavy rainfall of 2.75 inches from Thursday night into Friday morning. This is a delayed report. Beginning time estimated.", "ts_dict_index": [7179, 7180, 7181]}
+{"event_id": 822168, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-05-16 20:00:00", "end_date_time": "2019-05-17 06:00:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported heavy rainfall between 11pm Thursday and 7am Friday.", "ts_dict_index": [7185, 7186, 7187]}
+{"event_id": 822169, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-05-16 07:00:00", "end_date_time": "2019-05-17 07:00:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Coop observer reported heavy rainfall of 3.22 inches over the last 24 hours.", "ts_dict_index": [7188, 7189, 7190]}
+{"event_id": 870477, "event_type": "Heavy Rain", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2019-12-26 00:00:00", "end_date_time": "2019-12-27 23:59:00", "narrative": "A series of low pressure systems from the north and northwest, plus a weak tap into atmospheric river moisture, brought rain, mountain snow, and gusty winds to Southern California. Snow levels reached as low as 2000 feet, and brought high impact snow to locations above 4000 feet. Both I-8 through the San Diego Mountains and I-15 through the Cajon Pass were closed due to heavy snowfall. Between December 22-24, the coastal areas received 1-1.5 inches of rainfall, the valleys received 0.50-1 inch, and the mountain areas received up to 1 inch of rainfall. Again on December 26 through 27, coast and valley areas received 1 to 1.5 inches. Mountain areas received up to an inch. There were many water rescues, particularly in the Tijuana River Valley due to individuals driving through flooded roads and getting stuck. The San Diego River at Fashion Valley reached 10.5 feet on December 26. San Diego County coastal areas and valley areas received 1 to 1.5 inches between December 26 and 27. The mountain areas received up to 1 inch. There were many reports of water rescues, especially along the coast. The San Diego River at Fashion Valley reached 10.5 feet on December 26th.", "ts_dict_index": [7209, 7210, 7211]}
+{"event_id": 832579, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-06-22 06:00:00", "end_date_time": "2019-06-23 06:00:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. CoCoRaHS report of heavy rainfall of 2.35 inches over the last 24 hours.", "ts_dict_index": [7170, 7171, 7172]}
+{"event_id": 822166, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 06:00:00", "end_date_time": "2019-05-17 06:00:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. CoCoRaHS observer recorded heavy rainfall of 2.26 inches over the last 24 hours.", "ts_dict_index": [7200, 7201, 7202]}
+{"event_id": 822172, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 08:44:00", "end_date_time": "2019-05-17 08:44:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported heavy rainfall of 2.75 inches over the last 24 hours.", "ts_dict_index": [7206, 7207, 7208]}
+{"event_id": 822171, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-05-16 06:00:00", "end_date_time": "2019-05-17 08:00:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported heavy rainfall of 2.38 inches from 7am Thursday through 9am Friday.", "ts_dict_index": [7197, 7198, 7199]}
+{"event_id": 822174, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 17:00:00", "end_date_time": "2019-05-17 09:56:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Amateur radio operator reported heavy rainfall of 3.07 inches since 6 pm Thursday.", "ts_dict_index": [7191, 7192, 7193]}
+{"event_id": 832581, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 06:22:00", "end_date_time": "2019-06-23 06:22:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. Ankeny Regional Airport AWOS recorded heavy rainfall of 2.06 inches over the last 24 hours.", "ts_dict_index": [7176, 7177, 7178]}
+{"event_id": 832582, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-06-22 07:00:00", "end_date_time": "2019-06-23 07:00:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. Coop observer recorded heavy rainfall of 2.10 inches over the last 24 hours.", "ts_dict_index": [7173, 7174, 7175]}
+{"event_id": 822173, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-05-16 18:15:00", "end_date_time": "2019-05-17 09:00:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. WHO TV reported heavy rainfall of 2.95 inches. Beginning time estimated from radar.", "ts_dict_index": [7194, 7195, 7196]}
+{"event_id": 832568, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 19:50:00", "end_date_time": "2019-06-23 02:00:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. Trained spotter reported heavy rainfall of 4.75 inches overnight. Beginning and ending times estimated from radar.", "ts_dict_index": [7143, 7144, 7145]}
+{"event_id": 971428, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2021-07-14 23:30:00", "end_date_time": "2021-07-15 01:27:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. Report of 2.22 inches of rain in 2 hours.", "ts_dict_index": [7224, 7225, 7226]}
+{"event_id": 971424, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2021-07-14 17:00:00", "end_date_time": "2021-07-14 19:40:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. Trained spotter reports 5.60 inches of rain since 6 pm local time.", "ts_dict_index": [7227, 7228, 7229]}
+{"event_id": 870463, "event_type": "Heavy Rain", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2019-12-22 00:00:00", "end_date_time": "2019-12-24 23:59:00", "narrative": "A series of low pressure systems from the north and northwest, plus a weak tap into atmospheric river moisture, brought rain, mountain snow, and gusty winds to Southern California. Snow levels reached as low as 2000 feet, and brought high impact snow to locations above 4000 feet. Both I-8 through the San Diego Mountains and I-15 through the Cajon Pass were closed due to heavy snowfall. Between December 22-24, the coastal areas received 1-1.5 inches of rainfall, the valleys received 0.50-1 inch, and the mountain areas received up to 1 inch of rainfall. Again on December 26 through 27, coast and valley areas received 1 to 1.5 inches. Mountain areas received up to an inch. There were many water rescues, particularly in the Tijuana River Valley due to individuals driving through flooded roads and getting stuck. The San Diego River at Fashion Valley reached 10.5 feet on December 26. Many locations across coastal San Diego County reported 1 to 1.5 inches of precipitation (2-day storm total) from December 22 through 24.", "ts_dict_index": [7212, 7213, 7214]}
+{"event_id": 971435, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2021-07-14 07:00:00", "end_date_time": "2021-07-15 07:00:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. A 24 hour rain total of 3.02 inches.", "ts_dict_index": [7218, 7219, 7220]}
+{"event_id": 971436, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2021-07-14 07:03:00", "end_date_time": "2021-07-15 07:03:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. A 24 hour rain total of 2.10 inches with ponding in low lying areas.", "ts_dict_index": [7215, 7216, 7217]}
+{"event_id": 971451, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2021-07-14 09:23:00", "end_date_time": "2021-07-15 09:23:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. A 24 hour rain total of 3.26 inches with rain still in progress.", "ts_dict_index": [7221, 7222, 7223]}
+{"event_id": 822167, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 06:00:00", "end_date_time": "2019-05-17 06:00:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. CoCoRaHS observer recorded heavy rainfall of 2.00 inches over the last 24 hours.", "ts_dict_index": [7203, 7204, 7205]}
+{"event_id": 855777, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2019-09-21 07:00:00", "end_date_time": "2019-09-22 07:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. CoCoRaHS observer recorded heavy rainfall of 2.35 inches over the last 24 hours.", "ts_dict_index": [7272, 7273, 7274]}
+{"event_id": 855774, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2019-09-21 07:00:00", "end_date_time": "2019-09-22 07:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. CoCoRaHS observer recorded heavy rainfall of 2.57 inches over the last 24 hours.", "ts_dict_index": [7251, 7252, 7253]}
+{"event_id": 971427, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2021-07-14 17:00:00", "end_date_time": "2021-07-14 20:29:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. Public report of 5.20 inches of rain.", "ts_dict_index": [7230, 7231, 7232]}
+{"event_id": 855767, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2019-09-21 06:00:00", "end_date_time": "2019-09-22 06:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. Coop observer recorded heavy rainfall of 2.09 inches over the last 24 hours.", "ts_dict_index": [7266, 7267, 7268]}
+{"event_id": 855775, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2019-09-21 07:00:00", "end_date_time": "2019-09-22 07:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. Coop observer recorded heavy rainfall of 2.60 inches over the last 24 hours.", "ts_dict_index": [7254, 7255, 7256]}
+{"event_id": 855776, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2019-09-21 07:00:00", "end_date_time": "2019-09-22 07:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. CoCoRaHS observer recorded heavy rainfall of 2.70 inches over the last 24 hours.", "ts_dict_index": [7260, 7261, 7262]}
+{"event_id": 855783, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WARREN", "begin_date_time": "2019-09-21 08:00:00", "end_date_time": "2019-09-22 08:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. Mesonet station recorded heavy rainfall of 2.08 inches over the last 24 hours.", "ts_dict_index": [7269, 7270, 7271]}
+{"event_id": 971448, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2021-07-14 08:00:00", "end_date_time": "2021-07-15 08:00:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. A 24 hour rain total of 2.35 inches.", "ts_dict_index": [7233, 7234, 7235]}
+{"event_id": 855760, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2019-09-21 06:00:00", "end_date_time": "2019-09-22 06:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. Coop observer recorded heavy rainfall of 3.60 inches over the last 24 hours.", "ts_dict_index": [7248, 7249, 7250]}
+{"event_id": 855784, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2019-09-21 12:00:00", "end_date_time": "2019-09-22 12:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. Trained spotter reported heavy rainfall of 2.25 inches. Time duration unknown. Set at 24 hours for the report.", "ts_dict_index": [7257, 7258, 7259]}
+{"event_id": 971445, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2021-07-14 08:00:00", "end_date_time": "2021-07-15 08:00:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. A 24 hour rain total of 2.61 inches.", "ts_dict_index": [7245, 7246, 7247]}
+{"event_id": 855770, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2019-09-21 07:00:00", "end_date_time": "2019-09-22 07:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. CoCoRaHS observer recorded heavy rainfall of 2.13 inches over the last 24 hours.", "ts_dict_index": [7263, 7264, 7265]}
+{"event_id": 971426, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-07-14 17:00:00", "end_date_time": "2021-07-14 20:07:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. Trained spotter reported 3.40 inches of rain.", "ts_dict_index": [7236, 7237, 7238]}
+{"event_id": 822170, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-05-16 18:00:00", "end_date_time": "2019-05-17 07:30:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Trained spotter reported heavy rainfall of 3.10 inches during the event. Beginning time estimated from radar.", "ts_dict_index": [7182, 7183, 7184]}
+{"event_id": 855769, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2019-09-21 07:00:00", "end_date_time": "2019-09-22 07:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. CoCoRaHS observer recorded heavy rainfall of 2.80 inches over the last 24 hours.", "ts_dict_index": [7275, 7276, 7277]}
+{"event_id": 971439, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2021-07-14 08:00:00", "end_date_time": "2021-07-15 08:00:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. A 24 hour rain total of 4.44 inches.", "ts_dict_index": [7239, 7240, 7241]}
+{"event_id": 855782, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2019-09-21 07:56:00", "end_date_time": "2019-09-22 07:56:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. Fort Dodge Regional Airport AWOS recorded heavy rainfall of 2.56 inches over the last 24 hours.", "ts_dict_index": [7284, 7285, 7286]}
+{"event_id": 873450, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2020-02-06 00:00:00", "end_date_time": "2020-02-07 00:00:00", "narrative": "A deep upper-level trough moved slowly across the central and eastern U.S. bringing abundant moisture northward and combined with a complex frontal boundary and several waves of low pressure to bring repeated rounds of heavy rainfall. Rainfall totals in a 72-hour period ending at 700 AM EST on February 7th ranged from 2 to 4 inches with isolated higher amounts, but most of the rain fell within a 48-hour period. Numerous NWS Cooperative stations reported record one-day February rainfall amounts ending on the morning of February 6th and/or 7th and numerous two-day all-time February records were also set. Some flash flooding occurred during the event as higher rates of rainfall occurred embedded within the overall rain pattern. A state of emergency was declared by the West Virginia Governor in Monroe and Greenbrier counties due to the flooding. The ASOS climate station at Bluefield Airport (BLF) set a daily rainfall record of 2.09 inches for the 24-hour period ending at midnight on February 7th. The old record was 1.55 inches set in 1955. It was also the 2nd highest February one-day rain since records began in 1909, the record is 2.66 inches set February 27th , 1987. In addition, it was the 2nd wettest two-day event in in February at Bluefield with 2.69 inches, behind 1987 at 2.95 inches.", "ts_dict_index": [7305, 7306, 7307]}
+{"event_id": 1055838, "event_type": "Heavy Rain", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2022-09-12 09:26:00", "end_date_time": "2022-09-12 09:26:00", "narrative": "Tropical Cyclone Kay formed on September 4th, 2022 and made its closest approach to Southern California on the 9th and 10th, with the center of Kay coming within 120 miles of San Diego. Tropical moisture associated with Kay managed to produce heavy rainfall leading to flooding across mountainous terrain in Southern California on September 9th and 10th. This led to a number of wind damage and flooding events in the mountains and desert foothill locations in Southern California. Kay transitioned to a Post-Tropical Cyclone that weekend, but left enough lingering moisture to support additional rounds of heavy thunderstorms through the 11th and 12th of September. These later rounds of heavy rain would lead to multiple significant debris flow events in the San Bernardino County Mountains, namely in and around the Apple and El Dorado burn scars. Mesonet station CMFC1 Campo measured 0.87 inch of rainfall.", "ts_dict_index": [7326, 7327, 7328]}
+{"event_id": 1055839, "event_type": "Heavy Rain", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2022-09-12 06:00:00", "end_date_time": "2022-09-12 06:00:00", "narrative": "Tropical Cyclone Kay formed on September 4th, 2022 and made its closest approach to Southern California on the 9th and 10th, with the center of Kay coming within 120 miles of San Diego. Tropical moisture associated with Kay managed to produce heavy rainfall leading to flooding across mountainous terrain in Southern California on September 9th and 10th. This led to a number of wind damage and flooding events in the mountains and desert foothill locations in Southern California. Kay transitioned to a Post-Tropical Cyclone that weekend, but left enough lingering moisture to support additional rounds of heavy thunderstorms through the 11th and 12th of September. These later rounds of heavy rain would lead to multiple significant debris flow events in the San Bernardino County Mountains, namely in and around the Apple and El Dorado burn scars. CoCoRAHS station CA-SD-186 1.8 miles west-southwest of Ramona measured 0.95 inch of rainfall.", "ts_dict_index": [7323, 7324, 7325]}
+{"event_id": 1055823, "event_type": "Heavy Rain", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2022-09-10 14:07:00", "end_date_time": "2022-09-10 14:07:00", "narrative": "Tropical Cyclone Kay formed on September 4th, 2022 and made its closest approach to Southern California on the 9th and 10th, with the center of Kay coming within 120 miles of San Diego. Tropical moisture associated with Kay managed to produce heavy rainfall leading to flooding across mountainous terrain in Southern California on September 9th and 10th. This led to a number of wind damage and flooding events in the mountains and desert foothill locations in Southern California. Kay transitioned to a Post-Tropical Cyclone that weekend, but left enough lingering moisture to support additional rounds of heavy thunderstorms through the 11th and 12th of September. These later rounds of heavy rain would lead to multiple significant debris flow events in the San Bernardino County Mountains, namely in and around the Apple and El Dorado burn scars. Mesonet station RCHC1 Ranchita measured 4.62 inches of storm total rainfall.", "ts_dict_index": [7317, 7318, 7319]}
+{"event_id": 873452, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "MERCER", "begin_date_time": "2020-02-05 07:00:00", "end_date_time": "2020-02-07 07:00:00", "narrative": "A deep upper-level trough moved slowly across the central and eastern U.S. bringing abundant moisture northward and combined with a complex frontal boundary and several waves of low pressure to bring repeated rounds of heavy rainfall. Rainfall totals in a 72-hour period ending at 700 AM EST on February 7th ranged from 2 to 4 inches with isolated higher amounts, but most of the rain fell within a 48-hour period. Numerous NWS Cooperative stations reported record one-day February rainfall amounts ending on the morning of February 6th and/or 7th and numerous two-day all-time February records were also set. Some flash flooding occurred during the event as higher rates of rainfall occurred embedded within the overall rain pattern. A state of emergency was declared by the West Virginia Governor in Monroe and Greenbrier counties due to the flooding. The NWS Cooperative station at Princeton (PRIW2) set a daily rainfall record of 1.37 inches for the 24-hour period ending at 700 AM on February 6th. The previous date record was 1.14 inches in 1955. The station set another date record in the ensuing 24-hour period ending at 700 AM on the 7th, with 1.53 inches, breaking the previous record of 0.76 inches in 1955. Nearly complete station data exists back to 1941, with some additional records back to 1900.", "ts_dict_index": [7302, 7303, 7304]}
+{"event_id": 1055819, "event_type": "Heavy Rain", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2022-09-09 12:17:00", "end_date_time": "2022-09-09 12:17:00", "narrative": "Tropical Cyclone Kay formed on September 4th, 2022 and made its closest approach to Southern California on the 9th and 10th, with the center of Kay coming within 120 miles of San Diego. Tropical moisture associated with Kay managed to produce heavy rainfall leading to flooding across mountainous terrain in Southern California on September 9th and 10th. This led to a number of wind damage and flooding events in the mountains and desert foothill locations in Southern California. Kay transitioned to a Post-Tropical Cyclone that weekend, but left enough lingering moisture to support additional rounds of heavy thunderstorms through the 11th and 12th of September. These later rounds of heavy rain would lead to multiple significant debris flow events in the San Bernardino County Mountains, namely in and around the Apple and El Dorado burn scars. Mesonet Station LGMC1 Mt. Laguna at 6,000 Feet measured 0.98 inch of rainfall in one hour, and 3.23 inches total.", "ts_dict_index": [7308, 7309, 7310]}
+{"event_id": 1057006, "event_type": "Heavy Rain", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2022-09-09 10:35:00", "end_date_time": "2022-09-09 14:00:00", "narrative": "Tropical Cyclone Kay formed on September 4th, 2022 and made its closest approach to Southern California on the 9th and 10th, with the center of Kay coming within 120 miles of San Diego. Tropical moisture associated with Kay managed to produce heavy rainfall leading to flooding across mountainous terrain in Southern California on September 9th and 10th. This led to a number of wind damage and flooding events in the mountains and desert foothill locations in Southern California. Kay transitioned to a Post-Tropical Cyclone that weekend, but left enough lingering moisture to support additional rounds of heavy thunderstorms through the 11th and 12th of September. These later rounds of heavy rain would lead to multiple significant debris flow events in the San Bernardino County Mountains, namely in and around the Apple and El Dorado burn scars. Heavy rain associated with Tropical Cyclone Kay produced heavy rainfall across the San Diego County Mountains on September 9. The following are the heaviest rain reports from the day:||Mesonet station LGMC1 Mt. Laguna: 4.25 inch.|Mesonet Station MLGC1 Mt. Laguna Observatory RAWS, 2 NNW Mt. Laguna: 3.79 inch.|Mesonet Station AGUC1 Agua Caliente, 10 NE Mt. Laguna: 2.06 inch.|Mesonet Station TRRC1 Tierra Del Sol, 9 ENE Campo: 1.02 inch, 0.45 inch which occurred in one hour.", "ts_dict_index": [7311, 7312, 7313]}
+{"event_id": 855779, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "WAYNE", "begin_date_time": "2019-09-21 07:00:00", "end_date_time": "2019-09-22 07:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. CoCoRaHS observer recorded heavy rainfall of 2.00 inches over the last 24 hours.", "ts_dict_index": [7278, 7279, 7280]}
+{"event_id": 1055849, "event_type": "Heavy Rain", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2022-09-12 18:36:00", "end_date_time": "2022-09-12 18:36:00", "narrative": "Tropical Cyclone Kay formed on September 4th, 2022 and made its closest approach to Southern California on the 9th and 10th, with the center of Kay coming within 120 miles of San Diego. Tropical moisture associated with Kay managed to produce heavy rainfall leading to flooding across mountainous terrain in Southern California on September 9th and 10th. This led to a number of wind damage and flooding events in the mountains and desert foothill locations in Southern California. Kay transitioned to a Post-Tropical Cyclone that weekend, but left enough lingering moisture to support additional rounds of heavy thunderstorms through the 11th and 12th of September. These later rounds of heavy rain would lead to multiple significant debris flow events in the San Bernardino County Mountains, namely in and around the Apple and El Dorado burn scars. Mesonet station TR120 Mt Laguna Portable measured 1.46 inches of storm total rainfall.", "ts_dict_index": [7314, 7315, 7316]}
+{"event_id": 1055840, "event_type": "Heavy Rain", "state": "CALIFORNIA", "cz_name": "SAN DIEGO", "begin_date_time": "2022-09-12 11:52:00", "end_date_time": "2022-09-12 11:52:00", "narrative": "Tropical Cyclone Kay formed on September 4th, 2022 and made its closest approach to Southern California on the 9th and 10th, with the center of Kay coming within 120 miles of San Diego. Tropical moisture associated with Kay managed to produce heavy rainfall leading to flooding across mountainous terrain in Southern California on September 9th and 10th. This led to a number of wind damage and flooding events in the mountains and desert foothill locations in Southern California. Kay transitioned to a Post-Tropical Cyclone that weekend, but left enough lingering moisture to support additional rounds of heavy thunderstorms through the 11th and 12th of September. These later rounds of heavy rain would lead to multiple significant debris flow events in the San Bernardino County Mountains, namely in and around the Apple and El Dorado burn scars. Mesonet station ANEC1 Alpine RAWS site measured 0.64 inch of rainfall.", "ts_dict_index": [7320, 7321, 7322]}
+{"event_id": 855780, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2019-09-21 07:10:00", "end_date_time": "2019-09-22 07:10:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. CoCoRaHS observer recorded heavy rainfall of 3.75 inches over the last 24 hours.", "ts_dict_index": [7287, 7288, 7289]}
+{"event_id": 842054, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-07-17 10:45:00", "end_date_time": "2019-07-17 11:45:00", "narrative": "Overnight convection originating in south central South Dakota made its way across southern South Dakota overnight and eventually turned southeast as it approached Iowa. Through the morning hours conditions along and ahead of the line of convection included 30 to 40+ kts of 0-6km shear roughly orthogonal to the line, MUCAPE values in excess of 2000 J/kg, precipitable water values in excess of 1.5 to 1.75 inches, and consistent moisture transport into the region. All in all, a setup for consistent and sustained convection through the morning and afternoon hours. Fortunately, with the progressive nature no updrafts were able to produce severe hail. Given the linear nature, numerous reports of strong winds were received, but only a couple severe level reports. Additionally, heavy rainfall was reported with a few locations picking up in excess of 2 inches. Trained spotter reported storm total of 2.6 inches. Beginning and ending times estimated from radar.", "ts_dict_index": [7290, 7291, 7292]}
+{"event_id": 822570, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2019-05-23 06:00:00", "end_date_time": "2019-05-24 06:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. CoCoRaHS observer recorded heavy rainfall of 2.28 inches over the last 24 hours.", "ts_dict_index": [7332, 7333, 7334]}
+{"event_id": 822567, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-23 06:00:00", "end_date_time": "2019-05-24 06:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. CoCoRaHS observer recorded heavy rainfall of 2.45 inches over the last 24 hours.", "ts_dict_index": [7329, 7330, 7331]}
+{"event_id": 971437, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2021-07-14 08:00:00", "end_date_time": "2021-07-15 08:00:00", "narrative": "A surface low pressure system was centered over Kansas and Nebraska with attendant warm front draped across north central Iowa. This was bisected by an outflow boundary from morning convection across western Iowa. As morning activity exited the are the atmosphere quickly recovered steep low and mid level lapse rates exceeded 8 C/km with 0-6 km shear over 40 knots. Near the remnant outflow boundary 0-1 km SRH exceeded 150 m2/s2. Storms developed along this boundary and moved east along the warm front, spawning a number of tornadoes across the state. In fact, this is in the top 5 for tornadoes occurring in a single day for the state of Iowa since reliable records began in the 1980s. By evening convection congealed into an MCS, bringing heavy rain to portions of the state. A line of training storms set up north of the Des Moines metro, resulting in localized flash flooding. A 24 hour rain total of 5.50 inches.", "ts_dict_index": [7242, 7243, 7244]}
+{"event_id": 822566, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-23 06:00:00", "end_date_time": "2019-05-24 06:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. CoCoRaHS observer recorded heavy rainfall of 3.12 inches over the last 24 hours.", "ts_dict_index": [7338, 7339, 7340]}
+{"event_id": 822563, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-23 06:00:00", "end_date_time": "2019-05-24 06:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. CoCoRaHS observer recorded heavy rainfall of 2.00 inches over the last 24 hours.", "ts_dict_index": [7341, 7342, 7343]}
+{"event_id": 822584, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-23 22:00:00", "end_date_time": "2019-05-24 08:13:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. Who TV meteorologist reported heavy rainfall of 2.85 inches. Beginning time estimated from radar.", "ts_dict_index": [7335, 7336, 7337]}
+{"event_id": 874729, "event_type": "Heavy Rain", "state": "WEST VIRGINIA", "cz_name": "GREENBRIER", "begin_date_time": "2020-02-05 07:00:00", "end_date_time": "2020-02-07 07:00:00", "narrative": "A deep upper-level trough moved slowly across the central and eastern U.S. bringing abundant moisture northward and combined with a complex frontal boundary and several waves of low pressure to bring repeated rounds of heavy rainfall. Rainfall totals in a 72-hour period ending at 700 AM EST on February 7th ranged from 2 to 4 inches with isolated higher amounts, but most of the rain fell within a 48-hour period. Numerous NWS Cooperative stations reported record one-day February rainfall amounts ending on the morning of February 6th and/or 7th and numerous two-day all-time February records were also set. Some flash flooding occurred during the event as higher rates of rainfall occurred embedded within the overall rain pattern. A state of emergency was declared by the West Virginia Governor in Monroe and Greenbrier counties due to the flooding. The NWS Cooperative station at White Sulphur Springs (WSUW2) set a date rainfall record of 1.34 inches for the 24-hour period ending at 700 AM on February 7th. The previous date record was 1.15 inches in 1956 and 1933. It was the 3rd wettest two-day rainfall in February with 2.18 inches ending at 700 AM on the 7th.  Nearly complete station data exists back to 1921 with broken data back to 1888 at this site.", "ts_dict_index": [7299, 7300, 7301]}
+{"event_id": 822585, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "STORY", "begin_date_time": "2019-05-23 22:00:00", "end_date_time": "2019-05-24 08:29:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. Public reported heavy rainfall of 2.25 inches. Beginning time estimated from radar.", "ts_dict_index": [7356, 7357, 7358]}
+{"event_id": 875875, "event_type": "Lightning", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-12 05:57:00", "end_date_time": "2020-04-12 05:57:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. A home was struck by lightning in Flint. No injuries were reported.", "ts_dict_index": [7395, 7396, 7397]}
+{"event_id": 916583, "event_type": "Lightning", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-08-29 14:57:00", "end_date_time": "2020-08-29 14:57:00", "narrative": "The heat/humidity energized the environment on the 29th, and this happened as a cold front slowly approached from Missouri. Ahead of the front, strong to severe thunderstorms popped up in northern Arkansas in the afternoon. There was an estimated 60 mph wind gust just northeast of Damascus (Van Buren County) and a 70 mph gust at Alicia (Lawrence County). Trees were blown down at the latter location, and also at Lynn (Lawrence County). As storms dropped to the south toward Little Rock (Pulaski County), a building on a school campus was struck by lightning in Pulaski Heights (Pulaski County). This started a fire that damaged the roof.||Later in the evening, the focus shifted to the west. A storm near Boothe (Scott County) cranked out golf ball size hail at the intersection of Highways 23 and 71. Trees were pushed onto Highway 28 just east of Hon (Scott County) and Mena (Polk County).||Two to more than four inches of rain fell in west central Arkansas. Since this part of the state had already been pounded with deluge after deluge in August, the soil was saturated and could not hold much liquid. A flash flood event unfolded in a hurry, and it was serious. Water was over Highway 23 at Elm Park (Scott County). Several roads were under water and impassible at Mena (Polk County). At the airport just southeast of town, 2.74 inches of rain fell in an hour. People on all-terrain vehicles were stranded by high water at Wolfpen Gap Campground just west of Big Fork (Polk County). Sections of Highways 270 and 27 were flooded near Mount Ida (Montgomery County).||Early on the 31st, the sky opened again in the west. Many roads were inundated with water at Waldron (Scott County). Flooding was also experienced on Highway 298 near Story (Montgomery County), and along several thoroughfares in Hot Springs (Garland County). Lightning struck the roof of a building on a school campus in Little Rock. The fire that resulted caused additional damage to the roof structure.", "ts_dict_index": [7398, 7399, 7400]}
+{"event_id": 836437, "event_type": "Lightning", "state": "ARKANSAS", "cz_name": "JEFFERSON", "begin_date_time": "2019-06-23 15:30:00", "end_date_time": "2019-06-23 15:30:00", "narrative": "On the 23rd, the focus was on a couple of big thunderstorm clusters. The first cluster hammered areas north and west of Little Rock (Pulaski County) during the early morning hours, and it had a little of everything. Two weak tornadoes were spawned to the southeast of Paris (Logan County). The tornadoes uprooted or snapped trees, with one of the trees falling through a house. A mobile home roof and porch were also damaged. At Russellville (Pope County), thunderstorm gusts reached an estimated 90 mph at Arkansas Tech. Winds this strong tore up an outfield wall and first base dugout at a baseball field.||There was a lot of rain and reports of flash flooding. Creeks and small streams were on the rise, and roads were under water. At Waldron (Scott County), Highways 28 and 71 were closed. Culverts were washed out along Highway 80 southwest of Danville (Yell County). Closer to town, there was plenty of standing water at the airport. County roads were impassible or washed out around Ozone (Johnson County) and Parthenon (Newton County).||The first round of storms was followed quickly by another round in the late morning and afternoon hours. Between 1200 pm and 300 pm CDT, trees and/or power lines were toppled at Calico Rock (Izard County), Clarkridge (Baxter County), Evening Shade (Sharp County), Harmony (Johnson County), Melbourne (Izard County), Pocahontas (Randolph County), north of Strawberry (Lawrence County), Swifton (Jackson County), and Toad Suck (Perry County). There were instances of trees on homes, on vehicles, and blocking roads. A 61 mph wind gust was measured at Walnut Ridge (Lawrence County), with a 60 mph gust estimated at Bradford (White County).||More than a month's worth of rain fell in portions of northern and western Arkansas in the forty eight hour period ending at 700 am CDT on the 24th. Nine miles west of Waldron (Scott County). One rain gauge collected 11.35 inches of precipitation! Abbott (Scott County) had 8.10 inches, with 7.50 inches at Devils Knob (Johnson County), 7.38 inches at Nunley (Polk County), and 6.20 inches at Jasper (Newton County).||As the month came to a close, a storm system aloft visited from Missouri on the 26th. Cooler air overhead associated with the system moved over much warmer conditions near the ground. This agitated the atmosphere, and hit and miss thunderstorms flared up across the north.||Storms were mostly non-severe, but there was a report of golf ball size hail just northwest of Cherokee Village (Sharp County). A low water crossing was flooded near Compton (Newton County). Lightning struck a two-family duplex, causing it to catch fire.", "ts_dict_index": [7389, 7390, 7391]}
+{"event_id": 836439, "event_type": "Lightning", "state": "ARKANSAS", "cz_name": "JEFFERSON", "begin_date_time": "2019-06-23 16:30:00", "end_date_time": "2019-06-23 16:30:00", "narrative": "On the 23rd, the focus was on a couple of big thunderstorm clusters. The first cluster hammered areas north and west of Little Rock (Pulaski County) during the early morning hours, and it had a little of everything. Two weak tornadoes were spawned to the southeast of Paris (Logan County). The tornadoes uprooted or snapped trees, with one of the trees falling through a house. A mobile home roof and porch were also damaged. At Russellville (Pope County), thunderstorm gusts reached an estimated 90 mph at Arkansas Tech. Winds this strong tore up an outfield wall and first base dugout at a baseball field.||There was a lot of rain and reports of flash flooding. Creeks and small streams were on the rise, and roads were under water. At Waldron (Scott County), Highways 28 and 71 were closed. Culverts were washed out along Highway 80 southwest of Danville (Yell County). Closer to town, there was plenty of standing water at the airport. County roads were impassible or washed out around Ozone (Johnson County) and Parthenon (Newton County).||The first round of storms was followed quickly by another round in the late morning and afternoon hours. Between 1200 pm and 300 pm CDT, trees and/or power lines were toppled at Calico Rock (Izard County), Clarkridge (Baxter County), Evening Shade (Sharp County), Harmony (Johnson County), Melbourne (Izard County), Pocahontas (Randolph County), north of Strawberry (Lawrence County), Swifton (Jackson County), and Toad Suck (Perry County). There were instances of trees on homes, on vehicles, and blocking roads. A 61 mph wind gust was measured at Walnut Ridge (Lawrence County), with a 60 mph gust estimated at Bradford (White County).||More than a month's worth of rain fell in portions of northern and western Arkansas in the forty eight hour period ending at 700 am CDT on the 24th. Nine miles west of Waldron (Scott County). One rain gauge collected 11.35 inches of precipitation! Abbott (Scott County) had 8.10 inches, with 7.50 inches at Devils Knob (Johnson County), 7.38 inches at Nunley (Polk County), and 6.20 inches at Jasper (Newton County).||As the month came to a close, a storm system aloft visited from Missouri on the 26th. Cooler air overhead associated with the system moved over much warmer conditions near the ground. This agitated the atmosphere, and hit and miss thunderstorms flared up across the north.||Storms were mostly non-severe, but there was a report of golf ball size hail just northwest of Cherokee Village (Sharp County). A low water crossing was flooded near Compton (Newton County). Lightning hit a power pole at 7th and Dakota streets and broke the power pole in half.", "ts_dict_index": [7392, 7393, 7394]}
+{"event_id": 822577, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-05-23 07:00:00", "end_date_time": "2019-05-24 07:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. Trained spotter reported heavy rainfall of 2.52 inches.", "ts_dict_index": [7344, 7345, 7346]}
+{"event_id": 822561, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-05-23 06:00:00", "end_date_time": "2019-05-24 06:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. CoCoRaHS observer recorded heavy rainfall of 2.12 inches over the last 24 hours.", "ts_dict_index": [7371, 7372, 7373]}
+{"event_id": 822580, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-23 07:00:00", "end_date_time": "2019-05-24 07:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. Coop observer recorded heavy rainfall of 2.45 inches over the last 24 hours.", "ts_dict_index": [7368, 7369, 7370]}
+{"event_id": 822569, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-23 06:00:00", "end_date_time": "2019-05-24 06:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. CoCoRaHS observer recorded heavy rainfall of 2.23 inches over the last 24 hours.", "ts_dict_index": [7365, 7366, 7367]}
+{"event_id": 822557, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-05-23 06:00:00", "end_date_time": "2019-05-24 06:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. CoCoRaHS observer recorded heavy rainfall of 2.43 inches over the last 24 hours.", "ts_dict_index": [7353, 7354, 7355]}
+{"event_id": 822583, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-23 22:00:00", "end_date_time": "2019-05-24 08:09:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. Trained spotter reported heavy rainfall of 2.48 inches. Beginning time estimated from radar.", "ts_dict_index": [7374, 7375, 7376]}
+{"event_id": 822560, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-05-23 06:00:00", "end_date_time": "2019-05-24 06:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. CoCoRaHS observer recorded heavy rainfall of 3.06 inches over the last 24 hours.", "ts_dict_index": [7350, 7351, 7352]}
+{"event_id": 822579, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-23 07:00:00", "end_date_time": "2019-05-24 07:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. Coop observer recorded heavy rainfall of 2.82 inches over the last 24 hours.", "ts_dict_index": [7362, 7363, 7364]}
+{"event_id": 856059, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2019-09-27 06:00:00", "end_date_time": "2019-09-28 06:00:00", "narrative": "A relatively stationary front found it self draped across portions of northern Missouri and southern and southeast Iowa during the evening and overnight hours of the 27th. Fortunately, given the evening event, severe weather was fairly limited, yielding larger concerns for heavy rainfall. Environmentally, MUCAPE values were around 1000 J/kg, effective bulk shear around 40-50 kts and fading over time, precipitable water values around 1.5 to 1.8 inches, and at least moderate moisture transport into the area. While the best conditions for any severe weather potential and excessive rainfall were down into northern Missouri, areas of southern Iowa saw multiple rounds of showers and storms during the evening and overnight, resulting in heavy rainfall around 2 to 3 inches. Fortunately, little to no water issues were reported. CoCoRaHS observer recorded heavy rainfall of 2.40 inches over the last 24 hours.", "ts_dict_index": [7383, 7384, 7385]}
+{"event_id": 822564, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-23 06:00:00", "end_date_time": "2019-05-24 06:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. CoCoRaHS observer recorded heavy rainfall of 2.24 inches over the last 24 hours.", "ts_dict_index": [7347, 7348, 7349]}
+{"event_id": 822568, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-23 06:00:00", "end_date_time": "2019-05-24 06:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. CoCoRaHS observer recorded heavy rainfall of 2.54 inches over the last 24 hours.", "ts_dict_index": [7377, 7378, 7379]}
+{"event_id": 1061583, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 10:00:00", "end_date_time": "2022-10-15 10:00:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A video showed a significant fire broke out on top of the roof of a home in the area of Happy Valley Road and 95th Avenue in Peoria due to lightning. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [7401, 7402, 7403]}
+{"event_id": 1061370, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 14:00:00", "end_date_time": "2022-10-15 14:00:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A 12 year old girl, who lives in the Sun City West Retirement Community, was struck by lightning while playing outside, causing her heart to stop. Her father was able to successfully resuscitate her. The girl was taken to the hospital afterwards. Timing of the lightning strike was estimated by radar.", "ts_dict_index": [7404, 7405, 7406]}
+{"event_id": 856062, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2019-09-27 07:00:00", "end_date_time": "2019-09-28 07:00:00", "narrative": "A relatively stationary front found it self draped across portions of northern Missouri and southern and southeast Iowa during the evening and overnight hours of the 27th. Fortunately, given the evening event, severe weather was fairly limited, yielding larger concerns for heavy rainfall. Environmentally, MUCAPE values were around 1000 J/kg, effective bulk shear around 40-50 kts and fading over time, precipitable water values around 1.5 to 1.8 inches, and at least moderate moisture transport into the area. While the best conditions for any severe weather potential and excessive rainfall were down into northern Missouri, areas of southern Iowa saw multiple rounds of showers and storms during the evening and overnight, resulting in heavy rainfall around 2 to 3 inches. Fortunately, little to no water issues were reported. Coop observer recorded heavy rainfall of 2.10 inches over the last 24 hours.", "ts_dict_index": [7386, 7387, 7388]}
+{"event_id": 1114879, "event_type": "Heavy Rain", "state": "VIRGINIA", "cz_name": "PATRICK", "begin_date_time": "2023-06-19 07:00:00", "end_date_time": "2023-06-20 07:00:00", "narrative": "A stacked upper level low pressure system drifted from the Ohio River Valley to eastern Kentucky during the early morning hours of the 20th. South-southeasterly windflow around the low was efficient in transporting deep moisture into the area from the coastal Carolinas, allowing precipitable water values to rise into the 1.5 to 1.7 inch range along the crest of the Blue Ridge in Virginia south of Roanoke. Winds were nearly unidirectional with height around the low, with speeds varying between 15kt and 25kt between 925mb and 500mb per Storm Prediction Center Mesoscale Analysis.  Most-Unstable CAPEs along the Blue Ridge varied between 500 and 750 J/Kg through the night, but increased to around 1,000 J/Kg at around 5 AM/09 UTC as a wave of energy passed across the area. Multiple bands of training cells developed along the Blue Ridge. A personal weather station recorded a 24-hour rainfall total ending 8:00 AM EDT on the 20th of 3.66 inches. Runoff from this location flows into the Smith River.", "ts_dict_index": [7380, 7381, 7382]}
+{"event_id": 908484, "event_type": "Lightning", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2020-08-15 10:15:00", "end_date_time": "2020-08-15 10:20:00", "narrative": "A prolonged and oppressive heat wave swept the Central Coast and Bay Area for almost a week from August 14th to August 19th with widespread record breaking temperatures observed across the region. This was caused by a strong high pressure system over the Desert Southwest that expanded westward into California. This dome of heat brought hot temperatures to the area for several days. Multiple days of triple digit afternoon highs were recorded inland with some coastal locations even reaching the mid 90s. Several days of hot and dry weather further dried fuels over the area increasing fire danger. During this event, a surge of monsoonal and tropical moisture from a former Tropical Storm advected northward with sufficient instability to generate multiple high based and dry thunderstorms that produced several thousand lightning strikes over the Greater Bay Area. Many locations saw wind gusts of 40-50 mph with isolated areas seeing gusts of 60-75 mph. This prompted the San Francisco Bay Area forecast office to issue a rare severe thunderstorm warning. These lightning strikes in combination with gusty and erratic outflow winds sparked hundreds of wildfires across the state of California. Several smaller fires combined to form complexes some of which are now among the largest wildfires in state history. Most of which were still actively burning at the end of August. Hundreds of thousands of acres have been burned with several hundred structures destroyed as well as a handful of deaths and injuries. Tens of thousands of residents were also forced to evacuate. Additionally, all of these wildfires burning simultaneously across the state gave the Bay Area the worst air quality in the world at one point. Report of lightning striking a tree near San Ardo sparking a small fire.", "ts_dict_index": [7407, 7408, 7409]}
+{"event_id": 849774, "event_type": "Lightning", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-20 05:19:00", "end_date_time": "2019-08-20 05:19:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. Emergency manager reported a house fire started by lightning.", "ts_dict_index": [7410, 7411, 7412]}
+{"event_id": 960717, "event_type": "Lightning", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-07-11 08:15:00", "end_date_time": "2021-07-11 08:15:00", "narrative": "A mesoscale convective system (MCS) developed during the late afternoon and evening hours across Central and Eastern Oklahoma on July 10th, ahead of a weak cold front and associated upper level trough digging through the Central Plains into the Mid Mississippi Valley. The air mass ahead of this front and associated trough was moderately unstable even through the evening, with this complex of storms developing a strong cold pool as it shifted south through Southern Oklahoma, Southern Arkansas, and into East Texas and North Louisiana. Low level southerly winds ahead of this thunderstorm complex was sufficient enough to sustain this storm organization as it moved south through East Texas and North Louisiana during the morning hours of July 11th, which brought about gusty winds of 30-40 mph, heavy rainfall, and frequent lightning. As these storms moved through Lindale in Northern Smith County, Texas, lightning struck the roof of a Posada's Mexican Restaurant, causing a small fire which resulted in localized damage in the building. Lightning struck the roof of the Posadas Mexican Restaurant in Lindale, causing a small fire which was contained to an isolated area. Only minimal damage was caused to the business.", "ts_dict_index": [7446, 7447, 7448]}
+{"event_id": 1031269, "event_type": "Lightning", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-05-21 20:00:00", "end_date_time": "2022-05-21 20:00:00", "narrative": "Scattered strong to severe storms formed into a line across portions of northwestern and northern Arkansas along and ahead of an advancing cold front. The line made it into central sections of the state by early evening, and into the south during the overnight hours of the 21st.||Dry weather and above normal temperatures returned to the state for a few days before yet another storm system would impact the state on the 21st. Ahead of a strong cold front, there was a risk of severe weather stretching from the Texas/Mexico border northeastward to the Maine/Canada border. Thunderstorms initially developed across north/northwest Arkansas before forming into a line and marching east. While a brief, weak tornado occurred across Newton County, the most widespread damage occurred across portions of north central into northeast Arkansas. Numerous trees were blown down from Sharp County into portions of Lawrence and Randolph Counties. Additional storms developed later during the evening of May 21st across portions of western into central and southern Arkansas. Severe weather reports weren't widespread, but a second brief tornado developed near Royal in Garland County. The Emergency Manager reported a structure fire on Ridge Rd. due to a lightning strike.", "ts_dict_index": [7437, 7438, 7439]}
+{"event_id": 823313, "event_type": "Lightning", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-05-18 16:30:00", "end_date_time": "2019-05-18 16:30:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas. An isolated tornado also touched down just southeast of Tyler with one supercell thunderstorm. These storms began to move repeatedly over the same areas during the evening, with instances of flash flooding reported as well. These storms eventually spread into portions of North Louisiana during the early morning hours of the 19th. A house was struck by lightning and set on fire.", "ts_dict_index": [7449, 7450, 7451]}
+{"event_id": 834165, "event_type": "Lightning", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-06-19 20:20:00", "end_date_time": "2019-06-19 20:20:00", "narrative": "Severe weather returned on the 19th, and one of the largest severe weather events in Arkansas of 2019 unfolded. The event began with softball size hail or larger around Vandervoort and Cove (both in Polk County) between 630 pm and 700 pm CDT. Evidence from photos showed that some hailstones were close to five inches in diameter, potentially tying the state record set on January 21, 1999 and April 2, 2006. Records go back to the 1950s.||As the evening progressed, two clusters of storms evolved across the central and southern counties. They moved quickly to the east at 50 to more than 60 mph. This usually increases the chances of wind damage.||Trees and/or power lines were downed at many locations including Camden (Ouachita County), Harrell (Calhoun County), Little Rock (Pulaski County), Mount Ida and Norman (both in Montgomery County), Cabot and Lonoke (both in Lonoke County), Florence and Montongo (both in Drew County), and McGehee (Desha County). Lightning struck a home in the Indian Hills Neighborhood of North Little Rock, catching the structure on fire.", "ts_dict_index": [7455, 7456, 7457]}
+{"event_id": 1122000, "event_type": "Lightning", "state": "NEW YORK", "cz_name": "SARATOGA", "begin_date_time": "2023-07-09 14:45:00", "end_date_time": "2023-07-09 14:45:00", "narrative": "A strong upper-level system brought widespread rounds of showers and thunderstorms to eastern New York on July 9-11, 2023. The steadiest and heaviest rainfall occurred during the afternoon hours on July 9, the early morning hours on July 10 and during the evening hours on July 10 into the overnight hours on July 11. Rainfall totals varied greatly from region to region but the hardest hit areas (Hudson Valley and into northeastern Hamilton County) received 3 to 6 inches of rainfall.||Areal and flash flooding was primarily focused across areas along the Hudson River on July 9-10. Damage consisted of closed and washed out roads. A section of Metro-North's railroad tracks were washed out due to flood waters from Poughkeepsie southward.||The combination of heavy rain and beaver dam failures resulted in destruction of roads, bridges and sidewalks across northeastern Hamilton County during the early morning hours on July 11 focused on the areas of Long Lake and Blue Mountain Lake. A State of Emergency was declared for the towns of Long Lake and Indian Lake. New York Governor Kathy Hochul declared a State of Emergency for Hamilton County. Hamilton County Emergency Manager estimated damage to be in the millions of dollars.||In addition to the heavy rainfall, a few severe thunderstorms also developed across portions of the Hudson Valley leading to downed trees and wires. A lightning strike caused an auto body shop to catch fire. Lightning struck a propane tank and caused an automotive body shop to catch fire.", "ts_dict_index": [7419, 7420, 7421]}
+{"event_id": 832419, "event_type": "Lightning", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-06-23 16:18:00", "end_date_time": "2019-06-23 16:18:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. Lightning struck a home along Highway 79 East, starting a fire in the attic.", "ts_dict_index": [7428, 7429, 7430]}
+{"event_id": 1047576, "event_type": "Lightning", "state": "FLORIDA", "cz_name": "DUVAL", "begin_date_time": "2022-08-23 18:48:00", "end_date_time": "2022-08-23 18:48:00", "narrative": "Deep westerly flow prevailed over the region with an upper trough to the north and a ridge axis to the south. The anomalously moist airmass, with PWATs near 2.2 inches, remained over the region. Dense clouds were advected across much of the area Tuesday morning in the westerly flow. Cloudiness limited heating across southeast Georgia whereas northeast Florida experienced breaks in the cloud deck allowing for delayed diurnal destabilization. Storms were diurnally initiated across north central Florida in the afternoon due to less cloud cover over that area. Late start for the sea breezes, with them pushing inland late afternoon into evening.  Weak westerly flow allowed the Atlantic sea breeze to move inland to the St. Johns River basin. Diurnally driven storms in north central Florida lifted north and interacted with the sea breeze boundary in the evening. Slow-moving storms produced heavy rainfall and caused street flooding in Marion, Alachua and Clay counties. These storms produced about 2.5 to 4 inches of rain. A stronger storm in Marion county damaged a metal roof. Another stronger storm produced penny sized hail in Duval. Lightning struck a teenager in Duval causing injuries. A teenager was electrocuted by a lightning strike on Roosevelt Blvd resulting in an injury.", "ts_dict_index": [7434, 7435, 7436]}
+{"event_id": 1000118, "event_type": "Lightning", "state": "CALIFORNIA", "cz_name": "MONTEREY", "begin_date_time": "2021-12-13 22:00:00", "end_date_time": "2021-12-13 23:00:00", "narrative": "A low pressure system descended from the Gulf of Alaska southward along the entire Pacific Coast and tapped into sub-tropical moisture originating from the Central Pacific to drop heavy rain throughout the state. A stalled frontal boundary over the Santa Cruz Mountains along with strong southerly winds from a coastal low-level jet, enhanced orographic rainfall over this region, leading to rainfall totals over a 2 day period (Dec 12th-13th) of up to ten inches in the coastal mountains. The stalled boundary was reinvigorated by a secondary boundary bringing in a cold unstable airmass that set off convective showers and lowered snow levels below 2000 ft. A wind advisory, later upgraded to a high wind warning was issued for the southern half of the region from the SF Peninsula down to the Big Sur Coast including the inland zones due to the coastal jet bringing sustained winds up to 40 mph with gusts up to 55 mph. A high surf advisory was issued for the entire coast due to the arrival of a strong NW swell train, along with Gale Warning throughout the coastal waters. A flash flood watch was issued for the Santa Lucia Mountains and Dolan Burn Scar area, where up to 12 inches of rain fell. A lightning strike blew out a transformer along Del Monte Blvd. Eight power poles fell down but no injuries were reported. https://kion546.com/news/2021/12/14/a-look-at-the-damage-from-the-rain-storm/.", "ts_dict_index": [7431, 7432, 7433]}
+{"event_id": 976649, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-22 21:30:00", "end_date_time": "2021-07-22 21:30:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Lightning struck a house and sparked a fire in in the attic. No one was home at the time of the strike. Fire crews were able to keep the damage at a minimum. Time estimated from radar. No injuries reported.", "ts_dict_index": [7416, 7417, 7418]}
+{"event_id": 1132537, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:10:00", "end_date_time": "2023-08-31 21:10:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A palm tree caught on fire due to a lightning strike in the area of North Timberland Drive located in the Gainey Ranch area of Scottsdale. No injuries were reported.", "ts_dict_index": [7443, 7444, 7445]}
+{"event_id": 902423, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2020-07-06 19:45:00", "end_date_time": "2020-07-06 19:45:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A structure fire due to a lightning strike was reported on Amandas Teal Dr.", "ts_dict_index": [7452, 7453, 7454]}
+{"event_id": 1014552, "event_type": "Lightning", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-12 19:44:00", "end_date_time": "2022-04-12 19:44:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. Lightning struck a tree near Loop 571 and the Bradshaw State Jail in Henderson. A nearby field was set afire and burned.", "ts_dict_index": [7413, 7414, 7415]}
+{"event_id": 983859, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-16 22:40:00", "end_date_time": "2021-08-16 22:40:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Photos on social media show a charred pickup truck after catching on fire from being struck by lightning in a neighborhood near Ocotillo Road and Schnepf Road. No injuries were reported. Timing was estimated using radar.", "ts_dict_index": [7425, 7426, 7427]}
+{"event_id": 1057823, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-02 22:42:00", "end_date_time": "2022-09-02 22:42:00", "narrative": "Under a classic setup for storm motion from the Northern Arizona high terrain to Southern Arizona lower deserts, with the monsoon 500mb high positioned over Nevada and Utah, a few multicell storm clusters developed and progressed west-southwest through the lower deserts in the afternoon and evening hours of the 2nd. Increased east-northeast steering flow resulted in relatively high shear values for the monsoon (Sfc-6km shear around 25-30 kts) and very steep mid-level lapse rate (8-8.5 C/km) supported the organized multicellular storm mode with robust updrafts. Inversely, very high DCAPE values, up to 1500-1800 J/kg, supported very strong downbursts. Moisture levels were also above normal which, in combination with the strong updrafts, supported high rainfall rates (1.5-2 inches per hour average). There were a few multicell clusters that moved through Southern Arizona. One through the southeast parts of the greater Phoenix area, another that developed in Yavapai County before descending southwest along US-60 in Maricopa and La Paz Counties, and a third that developed off the Kofa Wilderness terrain south of Quartzsite before being caught by the cluster descending along US-60. Each cluster produced damaging winds, dense blowing dust, small to severe hail, and localized flash flooding. Local media reported a home was struck by lightning near Hunt Highway and Peace Pipe Place. The home caught fire and was fully destroyed. No injuries were reported.", "ts_dict_index": [7422, 7423, 7424]}
+{"event_id": 835201, "event_type": "Lightning", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 20:35:00", "end_date_time": "2019-06-22 20:35:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. Lightning struck a tree and the tree fell on a deck and car in Ankeny.", "ts_dict_index": [7458, 7459, 7460]}
+{"event_id": 816218, "event_type": "Lightning", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-04-28 20:00:00", "end_date_time": "2019-04-28 20:00:00", "narrative": "After a rather chilly overnight, complete with reports of up to 3.5 inches of snow in northern Iowa, storms initiated across portions of central Iowa and produced multiple instances of severe hail. ||Throughout the day, surface high pressure centered over the state slid eastward, placing the western half of the state back in warm air advection by the evening hours, especially above surface levels. The environment was not extremely conducive to sustained severe weather, but did have indications of hail potential, including a freezing level below 10kft, moderate to steep lapse rates above the near surface inversion, and a few hundred J/kg CAPE in the hail growth zone. Elevated storms roughly initiated along the 850mb front along and near I-80 across western Des Moines and west of the metro area. Storms were not long lived, but were able to produce a number of reports of severe hail, including up to half dollar in size. Public relayed picture of tree split via social media, possibly set on fire initially, from lightning strike. Location and time estimated from information provided.", "ts_dict_index": [7461, 7462, 7463]}
+{"event_id": 820249, "event_type": "Lightning", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-04-28 20:00:00", "end_date_time": "2019-04-28 20:00:00", "narrative": "After a rather chilly overnight, complete with reports of up to 3.5 inches of snow in northern Iowa, storms initiated across portions of central Iowa and produced multiple instances of severe hail. ||Throughout the day, surface high pressure centered over the state slid eastward, placing the western half of the state back in warm air advection by the evening hours, especially above surface levels. The environment was not extremely conducive to sustained severe weather, but did have indications of hail potential, including a freezing level below 10kft, moderate to steep lapse rates above the near surface inversion, and a few hundred J/kg CAPE in the hail growth zone. Elevated storms roughly initiated along the 850mb front along and near I-80 across western Des Moines and west of the metro area. Storms were not long lived, but were able to produce a number of reports of severe hail, including up to half dollar in size. Lightning struck a tree splitting the tree in half and downing about a 2-3 foot diameter limb/trunk portion of the tree.", "ts_dict_index": [7464, 7465, 7466]}
+{"event_id": 826920, "event_type": "Lightning", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 20:25:00", "end_date_time": "2019-05-16 20:25:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Lightning struck a power pole and knocked out power to the area.", "ts_dict_index": [7467, 7468, 7469]}
+{"event_id": 1132527, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:00:00", "end_date_time": "2023-08-31 21:00:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A lightning strike sparked a fire half an acre in size along the TV towers in South Mountain in Phoenix. Firefighters were able to extinguish fire successfully with structural damage reported.", "ts_dict_index": [7440, 7441, 7442]}
+{"event_id": 1047175, "event_type": "Lightning", "state": "FLORIDA", "cz_name": "DUVAL", "begin_date_time": "2022-08-22 13:45:00", "end_date_time": "2022-08-22 13:45:00", "narrative": "Generally west steering flow along with deep moisture (PWATs 2 inches or more) and impulses of energy in this flow aloft triggered numerous showers and storms during the afternoon and evening hours. Westerly flow pinned the Atlantic coast sea breeze to the coast and gave an early start to the Gulf coast sea breeze shifting inland across northeast Florida. Strong thunderstorms developed in the afternoon as they interacted with the stationary Atlantic sea breeze boundary along the coast before shifting offshore. These storms produced gusts between 45 to 55 mph at Marineland, St. Augustine and Mayport. Also, lightning struck a house in Neptune beach causing a house fire. Street flooding and heavy rain in Jacksonville Beach and Clay county were caused by training storms moving northeastward along a line that set up extending from Jacksonville Beach to Ocala. A lightning struck a home in Neptune Beach which caused damage to the exterior of the house and power outage but no fire was reported.", "ts_dict_index": [7473, 7474, 7475]}
+{"event_id": 1052800, "event_type": "Lightning", "state": "FLORIDA", "cz_name": "DUVAL", "begin_date_time": "2022-08-31 17:15:00", "end_date_time": "2022-08-31 17:15:00", "narrative": "A cold front slowly moved across southeast Georgia with high pressure to the southeast. A moist (PWATs around 2 in.) airmass and west-southwesterly flow prevailed across the area ahead of the frontal boundary. This caused the Atlantic sea breeze to only shift as far as the I-95 corridor. An upper shortwave trough passed through the southeastern US into southeast Georgia helping to enhance storms along the frontal boundary. A west to east line of pre-frontal storms moved southeastward and converged with the pinned Atlantic sea breeze in the afternoon. A few severe storms developed at these boundary mergers producing funnel clouds, heavy rain and severe winds downing trees. Later in the evening, the line of storms along the front shifted southward and interacted with the pinned sea breeze boundary. A power pole transformer was directly struck by lightning which resulted in loss of power to a small area near Oceanway. JEA then reported approximately 12 gallons of non-pcb mineral oil was released from the struck transformer. A nearby storm drain that discharges into the caney branch was impacted. Clean-up actions were completed.", "ts_dict_index": [7479, 7480, 7481]}
+{"event_id": 1041371, "event_type": "Lightning", "state": "INDIANA", "cz_name": "ALLEN", "begin_date_time": "2022-06-13 21:18:00", "end_date_time": "2022-06-13 21:19:00", "narrative": "A volatile environment of over 4000 J/KG of SBCAPE, combined with 45 to 60 knots of effective shear set the stage for multiple rounds of thunderstorm during the afternoon and evening hours of June 13th. Initial storms remained poorly organized, but did produce sporadic wind damage or hail. More substantial thunderstorm development evolved during the evening hours in northwestern Indiana and southwestern Lower Michigan and progressed east, eventually producing several swaths of wind damage. The most intense cluster of storms evolved in Berrien county Michigan and dropped rapidly southeast impacting locations extending from South Bend to Fort Wayne. Southwestern portions of Fort Wayne suffered the greatest impacts with widespread tree and structure damage from 80 to nearly 100 mph winds. Local media reported lightning struck a building at the Canterbury Green apartment complex. While no specific details or amount was provided, an estimate of $25,000 has been entered.", "ts_dict_index": [7482, 7483, 7484]}
+{"event_id": 1047180, "event_type": "Lightning", "state": "FLORIDA", "cz_name": "DUVAL", "begin_date_time": "2022-08-22 13:45:00", "end_date_time": "2022-08-22 13:45:00", "narrative": "Generally west steering flow along with deep moisture (PWATs 2 inches or more) and impulses of energy in this flow aloft triggered numerous showers and storms during the afternoon and evening hours. Westerly flow pinned the Atlantic coast sea breeze to the coast and gave an early start to the Gulf coast sea breeze shifting inland across northeast Florida. Strong thunderstorms developed in the afternoon as they interacted with the stationary Atlantic sea breeze boundary along the coast before shifting offshore. These storms produced gusts between 45 to 55 mph at Marineland, St. Augustine and Mayport. Also, lightning struck a house in Neptune beach causing a house fire. Street flooding and heavy rain in Jacksonville Beach and Clay county were caused by training storms moving northeastward along a line that set up extending from Jacksonville Beach to Ocala. A house on Fiddlers Ln was struck by lightning which led to a house fire. It seems like it started in the garage and spread into the rest of the house. The house and car sustained significant damage. Jacksonville fire rescue responded to the scene and reported no injuries.", "ts_dict_index": [7470, 7471, 7472]}
+{"event_id": 1041372, "event_type": "Lightning", "state": "INDIANA", "cz_name": "ALLEN", "begin_date_time": "2022-06-13 21:26:00", "end_date_time": "2022-06-13 21:27:00", "narrative": "A volatile environment of over 4000 J/KG of SBCAPE, combined with 45 to 60 knots of effective shear set the stage for multiple rounds of thunderstorm during the afternoon and evening hours of June 13th. Initial storms remained poorly organized, but did produce sporadic wind damage or hail. More substantial thunderstorm development evolved during the evening hours in northwestern Indiana and southwestern Lower Michigan and progressed east, eventually producing several swaths of wind damage. The most intense cluster of storms evolved in Berrien county Michigan and dropped rapidly southeast impacting locations extending from South Bend to Fort Wayne. Southwestern portions of Fort Wayne suffered the greatest impacts with widespread tree and structure damage from 80 to nearly 100 mph winds. Local fire  officials reported lightning struck a house on the 1200 block of Harvest Bay Drive. Damage was caused to the attic of the house as well as the loss of the garage. No injuries were reported. Damage is estimated at $40,000.", "ts_dict_index": [7485, 7486, 7487]}
+{"event_id": 947584, "event_type": "Lightning", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2021-03-25 13:54:00", "end_date_time": "2021-03-25 13:54:00", "narrative": "Clusters and line segments of heavy thunderstorms, a couple of which turned severe, overspread north Alabama during the predawn hours of the 25th.  These storms produced 2 to 3 inches of rain, mainly south of the Tennessee River, resulting in excessive runoff and flash flooding. Flash flooding closed a portion of I-65 in Cullman and several other roads were flooded or washed out in Cullman County. Also, isolated large hail and damaging winds were reported with a couple of these thunderstorms in northeast Alabama.  During the afternoon hours, additional strong thunderstorms produced additional excessive rainfall resulting in more flooding.  Rainfall totals were in the 3 to 5 inch range, generally south of the Tennessee River corridor. A law enforcement officer was struck by lightning while evaluating flooding at Mars Hill Bible School and putting up barricades at the intersection of Chisolm Road and Gresham Road. The officer suffered burns and was treated at a local hospital.", "ts_dict_index": [7491, 7492, 7493]}
+{"event_id": 1041375, "event_type": "Lightning", "state": "INDIANA", "cz_name": "ALLEN", "begin_date_time": "2022-06-13 21:32:00", "end_date_time": "2022-06-13 21:33:00", "narrative": "A volatile environment of over 4000 J/KG of SBCAPE, combined with 45 to 60 knots of effective shear set the stage for multiple rounds of thunderstorm during the afternoon and evening hours of June 13th. Initial storms remained poorly organized, but did produce sporadic wind damage or hail. More substantial thunderstorm development evolved during the evening hours in northwestern Indiana and southwestern Lower Michigan and progressed east, eventually producing several swaths of wind damage. The most intense cluster of storms evolved in Berrien county Michigan and dropped rapidly southeast impacting locations extending from South Bend to Fort Wayne. Southwestern portions of Fort Wayne suffered the greatest impacts with widespread tree and structure damage from 80 to nearly 100 mph winds. The public reported lightning struck a house on Wallen Road, between Coldwater and Lima Roads. Minor roof and siding damage was noted, but injuries were reported. Damage is estimated at $10,000.", "ts_dict_index": [7488, 7489, 7490]}
+{"event_id": 822578, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "DALLAS", "begin_date_time": "2019-05-23 07:00:00", "end_date_time": "2019-05-24 07:00:00", "narrative": "The setup over Iowa was primed for a heavy rainfall event for a few reasons, including persistent SW 500 mb flow, a strong and SW oriented 850 mb jet, strong low level moisture transport, and elevated CAPE around 1000-2000 J/kg. Precipitable water values, given the strong moisture transport into the area, rose into the neighborhood of 1.7 inches throughout the event as well. While effective bulk shear values were supportive of organized convection, that generally did not come to fruition given the widespread lifting with persistent low level warm air/theta-e advection and 850 mb jet into the region. As a result, the vast majority of reports and general consequences revolved around heavy rainfall and flooding, including a number of road closures. A couple severe wind gusts and damage reports were received in addition to the water issues. Coop observer recorded heavy rainfall of 2.36 inches over the last 24 hours.", "ts_dict_index": [7359, 7360, 7361]}
+{"event_id": 887672, "event_type": "Lightning", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-05-22 13:20:00", "end_date_time": "2020-05-22 13:20:00", "narrative": "Thunderstorm gusts from 60 to more than 80 mph blew through eastern sections of the state during the afternoon of the 22nd. Trees were toppled (some on houses) in Morton (Woodruff County). Earlier in the day, at least six house fires were triggered by lightning in the Little Rock (Pulaski County) area.||Scattered afternoon and evening severe storms unleashed more wind on the 25th from southwest into central Arkansas. Trees were uprooted or snapped at Fordyce (Dallas County) and Sheridan (Grant County). West of Mena (Polk County), a chicken house was damaged. Small outbuildings were destroyed at Ludwig Lake near Hillcrest (Johnson County). A 55 mph gust was measured at the Little Rock Air Force Base (Pulaski County). Lightning caused a house fire located 3.7 miles east of Mablevale.", "ts_dict_index": [7494, 7495, 7496]}
+{"event_id": 887673, "event_type": "Lightning", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-05-22 13:25:00", "end_date_time": "2020-05-22 13:25:00", "narrative": "Thunderstorm gusts from 60 to more than 80 mph blew through eastern sections of the state during the afternoon of the 22nd. Trees were toppled (some on houses) in Morton (Woodruff County). Earlier in the day, at least six house fires were triggered by lightning in the Little Rock (Pulaski County) area.||Scattered afternoon and evening severe storms unleashed more wind on the 25th from southwest into central Arkansas. Trees were uprooted or snapped at Fordyce (Dallas County) and Sheridan (Grant County). West of Mena (Polk County), a chicken house was damaged. Small outbuildings were destroyed at Ludwig Lake near Hillcrest (Johnson County). A 55 mph gust was measured at the Little Rock Air Force Base (Pulaski County). Lightning cause a house fire 3 miles northeast of Macon. Two people then had to be rescued.", "ts_dict_index": [7497, 7498, 7499]}
+{"event_id": 855761, "event_type": "Heavy Rain", "state": "IOWA", "cz_name": "APPANOOSE", "begin_date_time": "2019-09-21 06:00:00", "end_date_time": "2019-09-22 06:00:00", "narrative": "Generally speaking, there was not much to write home about with regards to the synoptic setup for severe or highly impactful weather. Even so, an environment with nominal MUCAPE (often under 1000 J/kg), high shear (0-1km shear in excess of 30 kts, 0-1km helicity in excess of 200 m2/s2), and consistent low level moisture transport was able to produce weak, brief tornadoes and sustained periods of moderate to heavy rainfall. ||Specifically on the tornadoes, two brief weak tornadoes occurred in the relatively low CAPE, high shear environment in central Iowa.  Little impact was observed from the tornadoes as they stayed in rural areas and away from structures and towns. ||On the rainfall front, multiple rounds of showers and storms produced numerous reports of 2 to 3 inches of rainfall throughout southern Iowa, even trickling north into central Iowa in a few instances. Centerville Municipal Airport AWOS recorded heavy rainfall of 3.01 inches over the last 24 hours.", "ts_dict_index": [7281, 7282, 7283]}
+{"event_id": 953521, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2021-06-09 14:40:00", "end_date_time": "2021-06-09 14:40:00", "narrative": "A very hot and humid air mass remained in place over the mid-Atlantic on June 9, following several days of unusually hot and humid conditions for the season. Similar to the previous day, afternoon thunderstorm development occurred in the mid-Atlantic mainly due to the influence of a weak cold front to the north and a weak surface trough. Like the previous day, storms were disorganized due to weak wind fields and a lack of forcing. However, the strong to extreme instability allowed some storms to briefly become severe with a threat for damaging winds, hail, and torrential rain. Convection gradually dissipated during the evening hours with the loss of daytime heating. Fire departments responded to a structure fire due to lightning on Oakwood Rd. Time estimated from dispatch calls.", "ts_dict_index": [7521, 7522, 7523]}
+{"event_id": 953527, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2021-06-09 15:59:00", "end_date_time": "2021-06-09 15:59:00", "narrative": "A very hot and humid air mass remained in place over the mid-Atlantic on June 9, following several days of unusually hot and humid conditions for the season. Similar to the previous day, afternoon thunderstorm development occurred in the mid-Atlantic mainly due to the influence of a weak cold front to the north and a weak surface trough. Like the previous day, storms were disorganized due to weak wind fields and a lack of forcing. However, the strong to extreme instability allowed some storms to briefly become severe with a threat for damaging winds, hail, and torrential rain. Convection gradually dissipated during the evening hours with the loss of daytime heating. An outbuilding fire due to a lightning strike was reported on Oakwood Rd. Time estimated from dispatch calls.", "ts_dict_index": [7539, 7540, 7541]}
+{"event_id": 1131960, "event_type": "Lightning", "state": "NEW YORK", "cz_name": "SARATOGA", "begin_date_time": "2023-08-04 15:46:00", "end_date_time": "2023-08-04 15:46:00", "narrative": "A slow moving low pressure system brought multiple rounds of scattered showers and thunderstorms across eastern New York from August 3 to August 4, 2023. Isolated thunderstorms developed during the afternoon hours on August 3 in the system's warm sector producing locally damaging wind gusts, small hail and also a funnel cloud. Additional thunderstorm activity developed ahead of a cold front during the morning hours on August 4, especially across Herkimer County, with activity shifting eastward into the Hudson Valley during the afternoon and evening. Additional wind damage and large hail was observed with these storms as well as localized areas of flooding and flash flooding. A tree was downed due to a lightning strike along Route 423 near Stillwater.", "ts_dict_index": [7515, 7516, 7517]}
+{"event_id": 953525, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2021-06-09 16:08:00", "end_date_time": "2021-06-09 16:08:00", "narrative": "A very hot and humid air mass remained in place over the mid-Atlantic on June 9, following several days of unusually hot and humid conditions for the season. Similar to the previous day, afternoon thunderstorm development occurred in the mid-Atlantic mainly due to the influence of a weak cold front to the north and a weak surface trough. Like the previous day, storms were disorganized due to weak wind fields and a lack of forcing. However, the strong to extreme instability allowed some storms to briefly become severe with a threat for damaging winds, hail, and torrential rain. Convection gradually dissipated during the evening hours with the loss of daytime heating. Residential structure fire due to lightning on Layton Rd. Time estimated from dispatch calls.", "ts_dict_index": [7536, 7537, 7538]}
+{"event_id": 953522, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2021-06-09 14:55:00", "end_date_time": "2021-06-09 14:55:00", "narrative": "A very hot and humid air mass remained in place over the mid-Atlantic on June 9, following several days of unusually hot and humid conditions for the season. Similar to the previous day, afternoon thunderstorm development occurred in the mid-Atlantic mainly due to the influence of a weak cold front to the north and a weak surface trough. Like the previous day, storms were disorganized due to weak wind fields and a lack of forcing. However, the strong to extreme instability allowed some storms to briefly become severe with a threat for damaging winds, hail, and torrential rain. Convection gradually dissipated during the evening hours with the loss of daytime heating. There was a residential structure fire due to a lightning strike on Henlopen Dr in Bethany Beach. Time estimated from dispatch reports.", "ts_dict_index": [7527, 7528, 7529]}
+{"event_id": 1045726, "event_type": "Lightning", "state": "FLORIDA", "cz_name": "DUVAL", "begin_date_time": "2022-08-18 16:45:00", "end_date_time": "2022-08-18 16:45:00", "narrative": "A weak area of low surface low pressure formed along a frontal boundary that was draped across the local area. Aloft, shortwave impulses traversed with the better dynamic |forcing over southeast GA. The entire airmass was primed (PWAT over 2 inches) and prevailing westerly steering flow focused the strongest convection along the sea breezes mergers toward the I-95 corridor in the afternoon and into the evening. A cluster of storms formed along the front across NE FL and Duval county. When these slow moving storms encountered the east coast sea breeze as it moved inland, very heavy rainfall rates produced local flooding across portions of downtown Jacksonville, including the Hogans Creek basin near UF Shands. A home was struck by lightning. The cost of damage was unknown and was estimated (likely low estimate) for inclusion of the event in Storm Data.", "ts_dict_index": [7506, 7507, 7508]}
+{"event_id": 953526, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2021-06-09 15:00:00", "end_date_time": "2021-06-09 15:00:00", "narrative": "A very hot and humid air mass remained in place over the mid-Atlantic on June 9, following several days of unusually hot and humid conditions for the season. Similar to the previous day, afternoon thunderstorm development occurred in the mid-Atlantic mainly due to the influence of a weak cold front to the north and a weak surface trough. Like the previous day, storms were disorganized due to weak wind fields and a lack of forcing. However, the strong to extreme instability allowed some storms to briefly become severe with a threat for damaging winds, hail, and torrential rain. Convection gradually dissipated during the evening hours with the loss of daytime heating. Residential structure fire due to lightning on Carrol Dr. Time estimated from dispatch calls.", "ts_dict_index": [7530, 7531, 7532]}
+{"event_id": 887674, "event_type": "Lightning", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-05-22 13:26:00", "end_date_time": "2020-05-22 13:26:00", "narrative": "Thunderstorm gusts from 60 to more than 80 mph blew through eastern sections of the state during the afternoon of the 22nd. Trees were toppled (some on houses) in Morton (Woodruff County). Earlier in the day, at least six house fires were triggered by lightning in the Little Rock (Pulaski County) area.||Scattered afternoon and evening severe storms unleashed more wind on the 25th from southwest into central Arkansas. Trees were uprooted or snapped at Fordyce (Dallas County) and Sheridan (Grant County). West of Mena (Polk County), a chicken house was damaged. Small outbuildings were destroyed at Ludwig Lake near Hillcrest (Johnson County). A 55 mph gust was measured at the Little Rock Air Force Base (Pulaski County). Lightning caused a house fire located 2 miles north of Macon.", "ts_dict_index": [7500, 7501, 7502]}
+{"event_id": 953528, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2021-06-09 13:34:00", "end_date_time": "2021-06-09 13:34:00", "narrative": "A very hot and humid air mass remained in place over the mid-Atlantic on June 9, following several days of unusually hot and humid conditions for the season. Similar to the previous day, afternoon thunderstorm development occurred in the mid-Atlantic mainly due to the influence of a weak cold front to the north and a weak surface trough. Like the previous day, storms were disorganized due to weak wind fields and a lack of forcing. However, the strong to extreme instability allowed some storms to briefly become severe with a threat for damaging winds, hail, and torrential rain. Convection gradually dissipated during the evening hours with the loss of daytime heating. Barn fire due to a lightning strike on Hollyville Rd. Time estimated from dispatch calls.", "ts_dict_index": [7533, 7534, 7535]}
+{"event_id": 1052716, "event_type": "Lightning", "state": "NEW YORK", "cz_name": "SARATOGA", "begin_date_time": "2022-08-30 14:20:00", "end_date_time": "2022-08-30 14:20:00", "narrative": "Hot and humid weather ahead of an approaching cold front led to heat indices reaching between 95F and 100F degrees as well as a few severe thunderstorms across eastern New York on August 30, 2022. Heat indices in excess of 95F degrees were concentrated along the Hudson River Valley. Severe thunderstorms were focused across the Upper Hudson Valley as well as southern Herkimer County. Damage was mainly due to downed trees and wires, though lightning strikes caused two separate house fires. Heavy rainfall also led to some minor street flooding around Glens Falls. A few power outages occurred across the Upper Hudson Valley as a result of the storms. Lightning struck a house on Redmond Road in Moreau causing a fire.", "ts_dict_index": [7551, 7552, 7553]}
+{"event_id": 953520, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2021-06-09 14:35:00", "end_date_time": "2021-06-09 14:35:00", "narrative": "A very hot and humid air mass remained in place over the mid-Atlantic on June 9, following several days of unusually hot and humid conditions for the season. Similar to the previous day, afternoon thunderstorm development occurred in the mid-Atlantic mainly due to the influence of a weak cold front to the north and a weak surface trough. Like the previous day, storms were disorganized due to weak wind fields and a lack of forcing. However, the strong to extreme instability allowed some storms to briefly become severe with a threat for damaging winds, hail, and torrential rain. Convection gradually dissipated during the evening hours with the loss of daytime heating. A person was struck by lightning in Angola, receiving non-fatal injuries. Time estimated from dispatch calls.", "ts_dict_index": [7518, 7519, 7520]}
+{"event_id": 953519, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2021-06-09 14:30:00", "end_date_time": "2021-06-09 14:30:00", "narrative": "A very hot and humid air mass remained in place over the mid-Atlantic on June 9, following several days of unusually hot and humid conditions for the season. Similar to the previous day, afternoon thunderstorm development occurred in the mid-Atlantic mainly due to the influence of a weak cold front to the north and a weak surface trough. Like the previous day, storms were disorganized due to weak wind fields and a lack of forcing. However, the strong to extreme instability allowed some storms to briefly become severe with a threat for damaging winds, hail, and torrential rain. Convection gradually dissipated during the evening hours with the loss of daytime heating. There was a structure fire due to lightning on Seagrass Plantation Ln. Time estimated from dispatch calls.", "ts_dict_index": [7524, 7525, 7526]}
+{"event_id": 1052715, "event_type": "Lightning", "state": "NEW YORK", "cz_name": "SARATOGA", "begin_date_time": "2022-08-30 14:38:00", "end_date_time": "2022-08-30 14:38:00", "narrative": "Hot and humid weather ahead of an approaching cold front led to heat indices reaching between 95F and 100F degrees as well as a few severe thunderstorms across eastern New York on August 30, 2022. Heat indices in excess of 95F degrees were concentrated along the Hudson River Valley. Severe thunderstorms were focused across the Upper Hudson Valley as well as southern Herkimer County. Damage was mainly due to downed trees and wires, though lightning strikes caused two separate house fires. Heavy rainfall also led to some minor street flooding around Glens Falls. A few power outages occurred across the Upper Hudson Valley as a result of the storms. A home near the Bend of the River Golf Club was struck by lightning which sparked a small electrical fire. The property owner later called the home unlivable.", "ts_dict_index": [7554, 7555, 7556]}
+{"event_id": 910191, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2020-09-03 21:20:00", "end_date_time": "2020-09-03 21:20:00", "narrative": "A frontal boundary stalled over the mid-Atlantic on the overnight of September 2 and lifted northward slightly during the day on September 3. A robust shortwave trough was also approaching during the day. This combination caused a high shear environment to develop, with good moisture also present. However, instability was marginal due to considerable cloud cover over the area. In addition, multiple rounds of storms associated with different sources of lift tended to work against each other, as storms generally struggled to organize and become dominant. However, given the high shear some storms still became strong to severe and produced instances of damaging wind. A residential fire occurred due to a lightning strike on Barksdale Court. Time estimated from radar.", "ts_dict_index": [7545, 7546, 7547]}
+{"event_id": 910190, "event_type": "Lightning", "state": "DELAWARE", "cz_name": "SUSSEX", "begin_date_time": "2020-09-03 18:35:00", "end_date_time": "2020-09-03 18:35:00", "narrative": "A frontal boundary stalled over the mid-Atlantic on the overnight of September 2 and lifted northward slightly during the day on September 3. A robust shortwave trough was also approaching during the day. This combination caused a high shear environment to develop, with good moisture also present. However, instability was marginal due to considerable cloud cover over the area. In addition, multiple rounds of storms associated with different sources of lift tended to work against each other, as storms generally struggled to organize and become dominant. However, given the high shear some storms still became strong to severe and produced instances of damaging wind. A structure fire was reported due to a lightning strike on Sunnyside Rd. Time estimated from radar.", "ts_dict_index": [7542, 7543, 7544]}
+{"event_id": 1045729, "event_type": "Lightning", "state": "FLORIDA", "cz_name": "DUVAL", "begin_date_time": "2022-08-18 17:26:00", "end_date_time": "2022-08-18 17:26:00", "narrative": "A weak area of low surface low pressure formed along a frontal boundary that was draped across the local area. Aloft, shortwave impulses traversed with the better dynamic |forcing over southeast GA. The entire airmass was primed (PWAT over 2 inches) and prevailing westerly steering flow focused the strongest convection along the sea breezes mergers toward the I-95 corridor in the afternoon and into the evening. A cluster of storms formed along the front across NE FL and Duval county. When these slow moving storms encountered the east coast sea breeze as it moved inland, very heavy rainfall rates produced local flooding across portions of downtown Jacksonville, including the Hogans Creek basin near UF Shands. Lightning struck an electrical pole and a transformer. This caused the transformer to leak oil onto the pavement. The cost of damage was unknown but estimated for inclusion of the event in Storm Data. It is likely an underestimate.", "ts_dict_index": [7503, 7504, 7505]}
+{"event_id": 810978, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-04-29 22:20:00", "end_date_time": "2019-04-29 22:20:00", "narrative": "During the evening hours on April 29th, an unseasonably strong upper level low pressure system moved across Arizona; during the late evening hours a well defined band of showers and isolated thunderstorms moved ahead of the main upper low and across much of the greater Phoenix metropolitan area. Although thunderstorms were rather isolated, some of them generated a number of cloud to ground lightning strokes, one of which struck a home in central Phoenix at about 2220MST. The lightning strike caused a fire to begin on the roof of a home near 32nd Street and Campbell Avenue. Firefighters were quick to arrive at the scene and put out the fire, limiting damage to the home. No injuries were reported. During the late evening hours on April 29th, a band of showers and isolated thunderstorms pushed east across the central portion of the greater Phoenix area. The convection was developing ahead of an unseasonably strong upper level low pressure system moving through Arizona. Although thunderstorms were isolated, a couple of the stronger storms generated several cloud to ground lightning strikes, one of which struck a home in central Phoenix. According to local broadcast media, at 2220MST a lightning strike hit the roof of a two story home in Phoenix, causing a fire to break out on the roof. The home was located near the intersection of 32nd Street and Campbell Avenue. Fortunately, the Phoenix Fire Department was able to quickly respond to the fire and put out the flames, limiting damage to the home. There were no injuries reported.", "ts_dict_index": [7509, 7510, 7511]}
+{"event_id": 967116, "event_type": "Lightning", "state": "NEW YORK", "cz_name": "SARATOGA", "begin_date_time": "2021-06-21 19:44:00", "end_date_time": "2021-06-21 19:44:00", "narrative": "A lifting warm front across the region brought a hot and humid air mass into the region, leading to maximum heat indices reaching 95 to 98 degrees across some valley locations of eastern New York.||An approaching cold front from the west led to numerous showers and thunderstorms during the afternoon and evening hours. Some of these storms became severe with several reports of downed trees and power lines. A couple trees fell onto homes with another falling onto a camper trailer. No injuries were reported. A funnel cloud was spotted by an observer in Warren County looking northward toward Lake George. A lightning strike hit a structure near Galway, causing a fire. Sporadic power outages occurred as a result of these storms with more than 1,000 National Grid customers without power in Washington County. Lightning hit a structure, causing a fire, on Lake Road in the Town of Galway.", "ts_dict_index": [7476, 7477, 7478]}
+{"event_id": 1127560, "event_type": "Lightning", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-08-07 13:09:00", "end_date_time": "2023-08-07 13:09:00", "narrative": "Clusters of strong to severe thunderstorms entered north Alabama during the late morning and early afternoon hours, moving east-southeast through the area. One of the thunderstorms produced a lightning strike, fatally injuring a male in north Florence in Lauderdale County. Lightning also killed 19 cattle at a farm in Ruth in Marshall County. As the thunderstorms progressed, several reports of wind damage were received, mainly south of Tennessee River in Morgan, Cullman, Marshall and DeKalb Counties.  Over 13,000 were left without power in north Alabama from the thunderstorms, including over 11,000 alone in Cullman County. At approximately 13:09 LST, lightning fatally injured a 28 year old male in the parking lot of a business at 3155 Kendall Drive in Florence.", "ts_dict_index": [7560, 7561, 7562]}
+{"event_id": 975282, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-14 05:10:00", "end_date_time": "2021-07-14 05:10:00", "narrative": "A weak shortwave trough moving across the state aided in the development of showers and thunderstorms across south-central Arizona on the morning of the 14th. With anomalously high amounts of moisture in place, showers and thunderstorms produced locally heavy rainfall which led to some flash flooding. Flash flooding was reported in northern Pinal County near Florence where Maricopa County Flood Control gages recorded over 1.50 of rainfall. Flash flooding was also reported in the Globe area as heavy rainfall over the recent Telegraph burn scar led to enhanced runoff in Pinal Creek. No injuries or damage were reported. Lightning was reported to have started a house fire in a neighborhood near 91st Avenue and Lower Buckeye Road. Firefighters discovered a small fire in the attic of the home, which was quickly extinguished. No injuries were reported.", "ts_dict_index": [7566, 7567, 7568]}
+{"event_id": 899898, "event_type": "Lightning", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-08-05 07:25:00", "end_date_time": "2020-08-05 07:25:00", "narrative": "A complex of showers and thunderstorms shifted southeast into Southeast Oklahoma, Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the morning hours of August 5th, along a weak upper level shortwave trough that progressed southeast over Arkansas. While these showers and thunderstorms gradually weakened as they moved southeast across East Texas and Northwest Louisiana in response to weakening instability over these areas, lightning struck a groundskeeper at the Henderson Country Club in Central Rusk County. Fortunately, the male victim suffered only minor injuries and was released from the hospital the next day. A 54 year old male groundskeeper was struck by lightning near a shed at the Henderson Country Club in Henderson. The lightning entered his head and came out through his left hand and leg. The victim suffered only minor injuries, and was released from the hospital the next day.", "ts_dict_index": [7557, 7558, 7559]}
+{"event_id": 1056463, "event_type": "Lightning", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-09-07 09:20:00", "end_date_time": "2022-09-07 09:20:00", "narrative": "An upper trough extended from the Great Lakes Region southwest into the Red River Valley during the morning hours of September 7th, which began to shift east across the Four State Region during the day. This trough reinforced a weak surface front south from Southeast Oklahoma and Southwest Arkansas into East Texas and North Louisiana throughout the day, with adequate moisture and instability present ahead of the front to help enhance scattered shower and thunderstorm development along and south of the front and ahead of the ejecting trough. Some of these storms became severe, with reports of damaging winds across portions of East Texas during the morning hours. Lightning struck a building near Noonday, setting it on fire.", "ts_dict_index": [7548, 7549, 7550]}
+{"event_id": 883907, "event_type": "Lightning", "state": "FLORIDA", "cz_name": "DUVAL", "begin_date_time": "2020-05-28 13:13:00", "end_date_time": "2020-05-28 13:13:00", "narrative": "A diffuse surface trough axis was north of the Altamaha River basin with very high dew pts in the low/mid 70s across the entire forecast area south of the boundary. The 12z|JAX RAOB showed less deep layer moisture (PWAT 1.6 inches) and stronger SW steering flow across the entire area from 10-15 kts south of I-10 across NE FL to 20 kts across our SE GA zones. There was drier air in the low/mid levels where the steepest lapse rates were near 6.8 C/km between 790 mb and 617 mb roughly. SE GA 0-6 km bulk shear was 20-25 kts. Ingredients favored pulse strong to severe storms with gusty downburst winds the main hazard. A lightning strike caused a house fire on the 2500 block of Dellwood Avenue in Riverside.  The cost of damage was unknown but it was estimated  for inclusion of the event in Storm Data.", "ts_dict_index": [7569, 7570, 7571]}
+{"event_id": 994790, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-12-15 14:32:00", "end_date_time": "2021-12-15 14:32:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 68 MPH was measured by a mesonet station located four miles north of Shickley.", "ts_dict_index": [7605, 7606, 7607]}
+{"event_id": 994792, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-12-15 14:31:00", "end_date_time": "2021-12-15 14:31:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 63 MPH was measured by a mesonet station located three miles south-southwest of Shickley.", "ts_dict_index": [7590, 7591, 7592]}
+{"event_id": 883910, "event_type": "Lightning", "state": "FLORIDA", "cz_name": "CLAY", "begin_date_time": "2020-05-28 13:50:00", "end_date_time": "2020-05-28 13:50:00", "narrative": "A diffuse surface trough axis was north of the Altamaha River basin with very high dew pts in the low/mid 70s across the entire forecast area south of the boundary. The 12z|JAX RAOB showed less deep layer moisture (PWAT 1.6 inches) and stronger SW steering flow across the entire area from 10-15 kts south of I-10 across NE FL to 20 kts across our SE GA zones. There was drier air in the low/mid levels where the steepest lapse rates were near 6.8 C/km between 790 mb and 617 mb roughly. SE GA 0-6 km bulk shear was 20-25 kts. Ingredients favored pulse strong to severe storms with gusty downburst winds the main hazard. A home was struck by lightning near Blanding Blvd and Doctors Inlet. The cost of damage was unknown but estimated for Storm Data.", "ts_dict_index": [7578, 7579, 7580]}
+{"event_id": 883909, "event_type": "Lightning", "state": "FLORIDA", "cz_name": "CLAY", "begin_date_time": "2020-05-28 13:45:00", "end_date_time": "2020-05-28 13:45:00", "narrative": "A diffuse surface trough axis was north of the Altamaha River basin with very high dew pts in the low/mid 70s across the entire forecast area south of the boundary. The 12z|JAX RAOB showed less deep layer moisture (PWAT 1.6 inches) and stronger SW steering flow across the entire area from 10-15 kts south of I-10 across NE FL to 20 kts across our SE GA zones. There was drier air in the low/mid levels where the steepest lapse rates were near 6.8 C/km between 790 mb and 617 mb roughly. SE GA 0-6 km bulk shear was 20-25 kts. Ingredients favored pulse strong to severe storms with gusty downburst winds the main hazard. A home was struck by lightning near U.S. Highway 17 and Varney Road. A significant house fire occurred. The cost of damage was unknown but estimated for Storm Data.", "ts_dict_index": [7572, 7573, 7574]}
+{"event_id": 994791, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-12-15 14:36:00", "end_date_time": "2021-12-15 14:36:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 79 MPH was measured by a mesonet station located four miles northeast of Shickley.", "ts_dict_index": [7602, 7603, 7604]}
+{"event_id": 994780, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-12-15 14:02:00", "end_date_time": "2021-12-15 14:02:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 63 MPH was measured by a mesonet station located two miles north-northwest of Inland.", "ts_dict_index": [7584, 7585, 7586]}
+{"event_id": 883908, "event_type": "Lightning", "state": "FLORIDA", "cz_name": "CLAY", "begin_date_time": "2020-05-28 13:40:00", "end_date_time": "2020-05-28 13:40:00", "narrative": "A diffuse surface trough axis was north of the Altamaha River basin with very high dew pts in the low/mid 70s across the entire forecast area south of the boundary. The 12z|JAX RAOB showed less deep layer moisture (PWAT 1.6 inches) and stronger SW steering flow across the entire area from 10-15 kts south of I-10 across NE FL to 20 kts across our SE GA zones. There was drier air in the low/mid levels where the steepest lapse rates were near 6.8 C/km between 790 mb and 617 mb roughly. SE GA 0-6 km bulk shear was 20-25 kts. Ingredients favored pulse strong to severe storms with gusty downburst winds the main hazard. Three people working for Red Stag Contracting were struck by a lightning strike along Iris Street in Middleburg while working on a roof. All victims were transported to Orange Park Medical Center. One victim, a 35 year old male, was struck directly and went into cardiac arrest. He was revived via CPR on scene and was later transferred to the UF Health Shands Hospital in Gainesville, FL. He remained in a coma until his passing on 6/9/2020, at 15:45 EDT.", "ts_dict_index": [7575, 7576, 7577]}
+{"event_id": 994786, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-12-15 14:40:00", "end_date_time": "2021-12-15 14:40:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 58 MPH was measured by a mesonet station located three miles northwest of Fairmont.", "ts_dict_index": [7608, 7609, 7610]}
+{"event_id": 1121446, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-30 20:30:00", "end_date_time": "2023-07-30 20:30:00", "narrative": "A strong thunderstorm complex known as a Mesoscale Convective System developed across southern Arizona and migrated westward into southern California during the evening and overnight hours on the 30th-31st. The mesoscale convective system developed in an environment characterized by MLCAPE of 1000-1500 J/KG as well as around 30 knots of deep-layer shear from an inverted mid-level trough that was situated over northern Sonora in Mexico. Isolated damaging winds were reported in the Yuma area as well as a lightning induced fire in a tree farm located southwest of the City of Maricopa. A lightning strike sparked a fire in a tree farm located in the area of Ralston and Peters & Nall Roads southwest of Maricopa. The fire burned for nearly 24 hours after the lightning strike. No property damage nor injuries were reported with this fire.", "ts_dict_index": [7581, 7582, 7583]}
+{"event_id": 994808, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-12-15 14:55:00", "end_date_time": "2021-12-15 14:55:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 63 MPH was measured by a mesonet station located five miles north-northwest of Alexandria.", "ts_dict_index": [7599, 7600, 7601]}
+{"event_id": 994777, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2021-12-15 13:54:00", "end_date_time": "2021-12-15 13:54:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 59 MPH was measured by a mesonet station located one mile south of Prosser.", "ts_dict_index": [7593, 7594, 7595]}
+{"event_id": 994807, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-12-15 14:40:00", "end_date_time": "2021-12-15 14:40:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 60 MPH was measured by a mesonet station located three miles east-southeast of Carleton.", "ts_dict_index": [7596, 7597, 7598]}
+{"event_id": 808684, "event_type": "Lightning", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-02-19 23:55:00", "end_date_time": "2019-02-19 23:55:00", "narrative": "Rain was heavy at times on the 19th, and there were hit and miss thunderstorms as well. There was no severe weather, but there was plenty of lightning. During the evening, an employee at Little Rock National Airport (Pulaski County) was struck by lightning while loading a plane. He was knocked unconscious for several minutes before being treated at a local hospital.||At 600 pm CST on the 19th, it was 31 degrees at Harrison (Boone County) and 32 degrees at Mountain Home (Baxter County). Pockets of freezing rain were reported. Ice coated exposed objects, with quarter to half inch accruals from Harrison (Boone County) to Western Grove (Newton County). This led to power outages in places. Just before midnight on the 19th, an employee, a 52 year old male, at Little Rock National Airport (Pulaski County) was struck by lightning while loading a plane. He was knocked unconscious for several minutes before being treated at a local hospital. The strike left a baseball-sized char mark on the top of his head.", "ts_dict_index": [7512, 7513, 7514]}
+{"event_id": 994782, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-12-15 14:13:00", "end_date_time": "2021-12-15 14:13:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 59 MPH was measured by a mesonet station located two miles north-northeast of Deweese.", "ts_dict_index": [7611, 7612, 7613]}
+{"event_id": 975283, "event_type": "Lightning", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-14 05:16:00", "end_date_time": "2021-07-14 05:16:00", "narrative": "A weak shortwave trough moving across the state aided in the development of showers and thunderstorms across south-central Arizona on the morning of the 14th. With anomalously high amounts of moisture in place, showers and thunderstorms produced locally heavy rainfall which led to some flash flooding. Flash flooding was reported in northern Pinal County near Florence where Maricopa County Flood Control gages recorded over 1.50 of rainfall. Flash flooding was also reported in the Globe area as heavy rainfall over the recent Telegraph burn scar led to enhanced runoff in Pinal Creek. No injuries or damage were reported. Lightning was reported to have struck a 3-inch above-ground gas line near 35th Avenue and Durango causing a fire. No injuries were reported.", "ts_dict_index": [7563, 7564, 7565]}
+{"event_id": 994789, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-12-15 14:37:00", "end_date_time": "2021-12-15 14:45:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 63 MPH was measured by a mesonet station located four miles west of Geneva and a wind gust of 60 MPH was measured by a mesonet station located three miles southwest of Geneva.", "ts_dict_index": [7635, 7636, 7637]}
+{"event_id": 994784, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-12-15 14:20:00", "end_date_time": "2021-12-15 14:20:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 68 MPH was measured by a mesonet station located three miles north of Edgar.", "ts_dict_index": [7623, 7624, 7625]}
+{"event_id": 991338, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-12-15 14:21:00", "end_date_time": "2021-12-15 14:23:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. Wind gusts were estimated to be near 70 MPH. Visibility was near zero due to rain and wind. A wind gusts of 63 MPH was measured by a mesonet station located four miles southeast of Clay Center.", "ts_dict_index": [7641, 7642, 7643]}
+{"event_id": 994785, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-12-15 14:25:00", "end_date_time": "2021-12-15 14:25:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 62 MPH was measured by a mesonet station located four miles north-northeast of Ong.", "ts_dict_index": [7626, 7627, 7628]}
+{"event_id": 994787, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-12-15 14:40:00", "end_date_time": "2021-12-15 14:40:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 70 MPH was measured by a mesonet station located two miles north-northwest of Geneva.", "ts_dict_index": [7629, 7630, 7631]}
+{"event_id": 994788, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-12-15 14:45:00", "end_date_time": "2021-12-15 14:45:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 59 MPH was measured by a mesonet station located two miles east-southeast of Fairmont.", "ts_dict_index": [7632, 7633, 7634]}
+{"event_id": 994783, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-12-15 14:15:00", "end_date_time": "2021-12-15 14:15:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 68 MPH was measured by a mesonet station located three miles west of Edgar.", "ts_dict_index": [7620, 7621, 7622]}
+{"event_id": 994779, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2021-12-15 14:00:00", "end_date_time": "2021-12-15 14:00:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 67 MPH was measured by a mesonet station located four miles northwest of Glenvil.", "ts_dict_index": [7614, 7615, 7616]}
+{"event_id": 991361, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-12-15 14:40:00", "end_date_time": "2021-12-15 14:40:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. Wind gusts estimated to be near 80 MPH lofted a carport up into nearby power lines. Tree limbs of at least 3-4 inches in diameter were downed. Blowing dust caused visibility to drop down to near one-half mile.", "ts_dict_index": [7644, 7645, 7646]}
+{"event_id": 994778, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2021-12-15 13:55:00", "end_date_time": "2021-12-15 13:55:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 61 MPH was measured by a mesonet station located on the north side of Hastings.", "ts_dict_index": [7617, 7618, 7619]}
+{"event_id": 991351, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-12-15 14:29:00", "end_date_time": "2021-12-15 14:29:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 84 MPH was measured by a mesonet station located two miles west of Shickley.", "ts_dict_index": [7587, 7588, 7589]}
+{"event_id": 991360, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-12-15 14:40:00", "end_date_time": "2021-12-15 14:40:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. Wind gusts estimated to be near 75 MPH resulted in tree damage in Geneva. A semi-truck was blown over on Highway 81.", "ts_dict_index": [7653, 7654, 7655]}
+{"event_id": 991342, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-12-15 14:25:00", "end_date_time": "2021-12-15 14:25:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. Wind gusts were estimated to be near 80 MPH. Power lines and trees were downed in Sutton.", "ts_dict_index": [7650, 7651, 7652]}
+{"event_id": 994809, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-12-15 14:45:00", "end_date_time": "2021-12-15 14:45:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 59 MPH was measured by a mesonet station located three miles east-southeast of Belvidere.", "ts_dict_index": [7656, 7657, 7658]}
+{"event_id": 991359, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-12-15 14:37:00", "end_date_time": "2021-12-15 14:37:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. Emergency management reported that two large pine trees were uprooted at the courthouse.", "ts_dict_index": [7662, 7663, 7664]}
+{"event_id": 991349, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-12-15 14:25:00", "end_date_time": "2021-12-15 14:28:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. Wind gusts in the area included 83 MPH, measured by a mesonet station located one mile north-northeast of Davenport, and 72 MPH, measured by a mesonet station located two miles south-southeast of Davenport. Photos received from Facebook showed damaged irrigation pivots in the area.", "ts_dict_index": [7647, 7648, 7649]}
+{"event_id": 991327, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2021-12-15 13:52:00", "end_date_time": "2021-12-15 13:52:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 66 MPH was measured by mesonet station located three miles northeast of Ayr.", "ts_dict_index": [7638, 7639, 7640]}
+{"event_id": 994781, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-12-15 14:15:00", "end_date_time": "2021-12-15 14:15:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 63 MPH was measured by a mesonet station located four miles northeast of Fairfield.", "ts_dict_index": [7668, 7669, 7670]}
+{"event_id": 991340, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-12-15 14:23:00", "end_date_time": "2021-12-15 14:23:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. Wind gusts were estimated to be near 80 MPH based on area measured gusts. Power lines were blown down in Ong.", "ts_dict_index": [7671, 7672, 7673]}
+{"event_id": 1035652, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-07 20:24:00", "end_date_time": "2022-06-07 20:24:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 63 MPH was measured by a mesonet station located two miles west of Ong.", "ts_dict_index": [7722, 7723, 7724]}
+{"event_id": 1039478, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-14 23:02:00", "end_date_time": "2022-06-14 23:07:00", "narrative": "For the second consecutive Tuesday evening, a relatively small percentage of the 24-county South Central Nebraska area was ravaged by significant severe thunderstorms that caused countless instances of damage including (but not limited to): broken windows/damaged siding, flipped irrigation pivots, destroyed crops by the thousands of acres, and more isolated occurrences of outright-demolished outbuildings/grain bins along with relatively minor structural damage to a few homes. Unlike the event a week prior on the 7th that featured a few separate swaths of severe weather, this one that played out mainly between 9:30 p.m. CDT on the 14th and 3:30 a.m. CDT on the 15th was highlighted by just one narrow, west-southwest to east-northeast oriented swath of multiple training supercells. In fact, some locations (Hastings and York to name a few) actually endured three to four SEPARATE severe storms over a span of 2-4 hours! With only limited exception, the vast majority of storm reports emanated from a 10-20 mile wide stripe centered roughly along a line from Elwood-Kearney-Doniphan-York. Within this zone there were numerous reports of large hail (many golf ball to tennis ball size) and damaging winds mainly in the 60-75 MPH range (but isolated pockets of 90-100+ MPH...especially east Highway 14). In addition, an EF-2 tornado was confirmed in southwest York County. Also of note was that some very unlucky locales experienced nearly a repeat performance of what just unfolded seven evenings prior...struck by another round of large hail/damaging winds only days after starting to recover from the first event on the 7th. Although this overlapping damage was somewhat evident over northeastern Adams County, it was particularly visible within the southwestern quadrant of York County, where many fields were mostly stripped bare for miles around...creating a visually striking/eerie contrast to what is typically a sea of green under the mid-June sun. ||Taking a deeper dive into storm reports and starting with the EF-2 tornado, storm surveys concluded that it tracked just over seven miles through southwestern York County shortly after midnight CDT, developing west-southwest of Lushton and lifting west of McCool Junction. Along the way, several farmsteads sustained damage (including a garage torn from a home and a wood frame outbuilding completely demolished) and two people sustained minor injuries. Interestingly, an unofficial mesonet station in or very near the tornado path actually measured a 90 MPH gust a few miles east-northeast of Lushton. Turning to the many known (and countless unknown) occurrences of large hail/damaging straight line winds within the primary convective swath, a few of the more noteworthy wind damage/speed reports included: estimated 105 MPH winds in the Waco area that toppled a 60 ft. concrete silo; estimated 95 MPH winds through parts of northeastern Clay County that crumpled a grain bin near Saronville; widespread tree and sporadic structural damage in McCool Junction; separate measured wind gusts of 75 and 65 MPH at Hastings airport (from different storms 45 minutes apart); an unofficial mesonet gust of 79 MPH near Norman. Meanwhile, a few of the most notable hail reports featured: stones up to tennis ball size in York and Trumbull; hail up to 2.25 diameter at the NWS Hastings office that significantly dented the vehicles of on-duty meteorologists working this event; various reports of ping pong ball to golf ball size hail in or near Waco, Riverdale, Lushton, Bertrand, Kearney and seven miles south of Elwood. Rainfall-wise, despite the passage of several storms over the same areas, progressive storm motions mitigated the threat of significant flooding by limiting most totals to no more than 1-2 (highest NeRAIN amount of 2.67 on the east side of York). Although the vast majority of hail/wind reports were tied to the aforementioned west-east corridor bisecting the heart of the area, two severe storms occurred well outside of this zone...one to the south/one to the north. The southern one was a discrete supercell that lumbered through parts of Webster/Nuckolls/Thayer counties but yielded only one report of quarter size hail in Nelson. Meanwhile, the northern-most severe storm was the left-split of a supercell that first developed southwest of Kearney, dropping 1.5-2 diameter hail in the Pleasanton and Loup City areas before weakening. ||Examining event evolution/meteorological background, the first weak convection of the evening within South Central Nebraska bubbled up in the Hastings area shortly before sunset, forming slightly north of a well-defined, southwest-northeast oriented quasi-stationary front stretched from west-central KS through southeast NE (storms that developed directly along this front earlier in the evening remained just southeast of the local area). Between 9-10 p.m. CDT two supercells quickly evolved out of the initial weak activity, one that pounded York with its first round of large hail and drilled the eastern part of the county with significant wind damage, and the other the aforementioned southern supercell that developed over Webster County. Between 10-11 p.m. CDT, these first severe storms either departed the local area into eastern Nebraska (the northern one) or weakened/dissipated (the southern one). However, not far to the west the primary supercell train was just getting warmed up as several severe storms rapidly blossomed along the Highway 6/Interstate 80 corridors within the western half of South Central Nebraska. This slightly-elevated activity developed in response to intensifying nocturnal convergence into a sharpening frontal zone very evident in the 850-700 millibar layer. Given that this low-mid level front was aligned nearly parallel to strong west-southwesterly upper level winds (attendant to a large scale trough centered over the Northern Rockies) and that the mesoscale environment featured a potent combination of very strong deep layer shear (50-70 knots) and decent most-unstable CAPE (1000-2000 J/kg), the stage was set for a somewhat rare episode of several supercells training along the same corridor in close succession. In fact, between 11 p.m. and 2 a.m. CDT, at least 3-5 severe-warned storms marched in tandem along this path, each core spaced out roughly 25 miles from the next. During this three-hour span, places such as Hastings and York endured three separate severe storms (bringing York up to FOUR direct hits...including the initial supercell of the night). While most of these cells remained just elevated enough to preclude a tornado threat, the first storm in the supercell train managed to spawn the EF-2 in southwestern York County...apparently tapping into JUST enough lower-level moisture/instability in the vicinity of the nearby surface front to become tornadic. Finally, between 2:00-3:30 a.m. CDT, the last two training supercells of the night passed through Hamilton, Polk and northern York counties before departing the local area, bringing an end to this unique and (in places) destructive event. Peak wind gusts estimated to be around 95 MPH caused widespread damage along and near this path. Numerous power poles were damaged, including several that were snapped. Tree damage was reported, and several irrigation pivots were overturned. Outbuilding damage occurred, and a grain bin just west of Saronville was shifted off its foundation and crumpled. A shed was overturned north of Sutton.", "ts_dict_index": [7698, 7699, 7700]}
+{"event_id": 1035651, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-07 20:19:00", "end_date_time": "2022-06-07 20:19:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 58 MPH was measured by a mesonet station located four miles northeast of Fairfield.", "ts_dict_index": [7719, 7720, 7721]}
+{"event_id": 1039538, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-14 23:36:00", "end_date_time": "2022-06-14 23:36:00", "narrative": "For the second consecutive Tuesday evening, a relatively small percentage of the 24-county South Central Nebraska area was ravaged by significant severe thunderstorms that caused countless instances of damage including (but not limited to): broken windows/damaged siding, flipped irrigation pivots, destroyed crops by the thousands of acres, and more isolated occurrences of outright-demolished outbuildings/grain bins along with relatively minor structural damage to a few homes. Unlike the event a week prior on the 7th that featured a few separate swaths of severe weather, this one that played out mainly between 9:30 p.m. CDT on the 14th and 3:30 a.m. CDT on the 15th was highlighted by just one narrow, west-southwest to east-northeast oriented swath of multiple training supercells. In fact, some locations (Hastings and York to name a few) actually endured three to four SEPARATE severe storms over a span of 2-4 hours! With only limited exception, the vast majority of storm reports emanated from a 10-20 mile wide stripe centered roughly along a line from Elwood-Kearney-Doniphan-York. Within this zone there were numerous reports of large hail (many golf ball to tennis ball size) and damaging winds mainly in the 60-75 MPH range (but isolated pockets of 90-100+ MPH...especially east Highway 14). In addition, an EF-2 tornado was confirmed in southwest York County. Also of note was that some very unlucky locales experienced nearly a repeat performance of what just unfolded seven evenings prior...struck by another round of large hail/damaging winds only days after starting to recover from the first event on the 7th. Although this overlapping damage was somewhat evident over northeastern Adams County, it was particularly visible within the southwestern quadrant of York County, where many fields were mostly stripped bare for miles around...creating a visually striking/eerie contrast to what is typically a sea of green under the mid-June sun. ||Taking a deeper dive into storm reports and starting with the EF-2 tornado, storm surveys concluded that it tracked just over seven miles through southwestern York County shortly after midnight CDT, developing west-southwest of Lushton and lifting west of McCool Junction. Along the way, several farmsteads sustained damage (including a garage torn from a home and a wood frame outbuilding completely demolished) and two people sustained minor injuries. Interestingly, an unofficial mesonet station in or very near the tornado path actually measured a 90 MPH gust a few miles east-northeast of Lushton. Turning to the many known (and countless unknown) occurrences of large hail/damaging straight line winds within the primary convective swath, a few of the more noteworthy wind damage/speed reports included: estimated 105 MPH winds in the Waco area that toppled a 60 ft. concrete silo; estimated 95 MPH winds through parts of northeastern Clay County that crumpled a grain bin near Saronville; widespread tree and sporadic structural damage in McCool Junction; separate measured wind gusts of 75 and 65 MPH at Hastings airport (from different storms 45 minutes apart); an unofficial mesonet gust of 79 MPH near Norman. Meanwhile, a few of the most notable hail reports featured: stones up to tennis ball size in York and Trumbull; hail up to 2.25 diameter at the NWS Hastings office that significantly dented the vehicles of on-duty meteorologists working this event; various reports of ping pong ball to golf ball size hail in or near Waco, Riverdale, Lushton, Bertrand, Kearney and seven miles south of Elwood. Rainfall-wise, despite the passage of several storms over the same areas, progressive storm motions mitigated the threat of significant flooding by limiting most totals to no more than 1-2 (highest NeRAIN amount of 2.67 on the east side of York). Although the vast majority of hail/wind reports were tied to the aforementioned west-east corridor bisecting the heart of the area, two severe storms occurred well outside of this zone...one to the south/one to the north. The southern one was a discrete supercell that lumbered through parts of Webster/Nuckolls/Thayer counties but yielded only one report of quarter size hail in Nelson. Meanwhile, the northern-most severe storm was the left-split of a supercell that first developed southwest of Kearney, dropping 1.5-2 diameter hail in the Pleasanton and Loup City areas before weakening. ||Examining event evolution/meteorological background, the first weak convection of the evening within South Central Nebraska bubbled up in the Hastings area shortly before sunset, forming slightly north of a well-defined, southwest-northeast oriented quasi-stationary front stretched from west-central KS through southeast NE (storms that developed directly along this front earlier in the evening remained just southeast of the local area). Between 9-10 p.m. CDT two supercells quickly evolved out of the initial weak activity, one that pounded York with its first round of large hail and drilled the eastern part of the county with significant wind damage, and the other the aforementioned southern supercell that developed over Webster County. Between 10-11 p.m. CDT, these first severe storms either departed the local area into eastern Nebraska (the northern one) or weakened/dissipated (the southern one). However, not far to the west the primary supercell train was just getting warmed up as several severe storms rapidly blossomed along the Highway 6/Interstate 80 corridors within the western half of South Central Nebraska. This slightly-elevated activity developed in response to intensifying nocturnal convergence into a sharpening frontal zone very evident in the 850-700 millibar layer. Given that this low-mid level front was aligned nearly parallel to strong west-southwesterly upper level winds (attendant to a large scale trough centered over the Northern Rockies) and that the mesoscale environment featured a potent combination of very strong deep layer shear (50-70 knots) and decent most-unstable CAPE (1000-2000 J/kg), the stage was set for a somewhat rare episode of several supercells training along the same corridor in close succession. In fact, between 11 p.m. and 2 a.m. CDT, at least 3-5 severe-warned storms marched in tandem along this path, each core spaced out roughly 25 miles from the next. During this three-hour span, places such as Hastings and York endured three separate severe storms (bringing York up to FOUR direct hits...including the initial supercell of the night). While most of these cells remained just elevated enough to preclude a tornado threat, the first storm in the supercell train managed to spawn the EF-2 in southwestern York County...apparently tapping into JUST enough lower-level moisture/instability in the vicinity of the nearby surface front to become tornadic. Finally, between 2:00-3:30 a.m. CDT, the last two training supercells of the night passed through Hamilton, Polk and northern York counties before departing the local area, bringing an end to this unique and (in places) destructive event. A wind gust of 64 MPH was measured by a mesonet station located four miles northeast of Fairfield.", "ts_dict_index": [7695, 7696, 7697]}
+{"event_id": 1039443, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-14 22:40:00", "end_date_time": "2022-06-14 22:40:00", "narrative": "For the second consecutive Tuesday evening, a relatively small percentage of the 24-county South Central Nebraska area was ravaged by significant severe thunderstorms that caused countless instances of damage including (but not limited to): broken windows/damaged siding, flipped irrigation pivots, destroyed crops by the thousands of acres, and more isolated occurrences of outright-demolished outbuildings/grain bins along with relatively minor structural damage to a few homes. Unlike the event a week prior on the 7th that featured a few separate swaths of severe weather, this one that played out mainly between 9:30 p.m. CDT on the 14th and 3:30 a.m. CDT on the 15th was highlighted by just one narrow, west-southwest to east-northeast oriented swath of multiple training supercells. In fact, some locations (Hastings and York to name a few) actually endured three to four SEPARATE severe storms over a span of 2-4 hours! With only limited exception, the vast majority of storm reports emanated from a 10-20 mile wide stripe centered roughly along a line from Elwood-Kearney-Doniphan-York. Within this zone there were numerous reports of large hail (many golf ball to tennis ball size) and damaging winds mainly in the 60-75 MPH range (but isolated pockets of 90-100+ MPH...especially east Highway 14). In addition, an EF-2 tornado was confirmed in southwest York County. Also of note was that some very unlucky locales experienced nearly a repeat performance of what just unfolded seven evenings prior...struck by another round of large hail/damaging winds only days after starting to recover from the first event on the 7th. Although this overlapping damage was somewhat evident over northeastern Adams County, it was particularly visible within the southwestern quadrant of York County, where many fields were mostly stripped bare for miles around...creating a visually striking/eerie contrast to what is typically a sea of green under the mid-June sun. ||Taking a deeper dive into storm reports and starting with the EF-2 tornado, storm surveys concluded that it tracked just over seven miles through southwestern York County shortly after midnight CDT, developing west-southwest of Lushton and lifting west of McCool Junction. Along the way, several farmsteads sustained damage (including a garage torn from a home and a wood frame outbuilding completely demolished) and two people sustained minor injuries. Interestingly, an unofficial mesonet station in or very near the tornado path actually measured a 90 MPH gust a few miles east-northeast of Lushton. Turning to the many known (and countless unknown) occurrences of large hail/damaging straight line winds within the primary convective swath, a few of the more noteworthy wind damage/speed reports included: estimated 105 MPH winds in the Waco area that toppled a 60 ft. concrete silo; estimated 95 MPH winds through parts of northeastern Clay County that crumpled a grain bin near Saronville; widespread tree and sporadic structural damage in McCool Junction; separate measured wind gusts of 75 and 65 MPH at Hastings airport (from different storms 45 minutes apart); an unofficial mesonet gust of 79 MPH near Norman. Meanwhile, a few of the most notable hail reports featured: stones up to tennis ball size in York and Trumbull; hail up to 2.25 diameter at the NWS Hastings office that significantly dented the vehicles of on-duty meteorologists working this event; various reports of ping pong ball to golf ball size hail in or near Waco, Riverdale, Lushton, Bertrand, Kearney and seven miles south of Elwood. Rainfall-wise, despite the passage of several storms over the same areas, progressive storm motions mitigated the threat of significant flooding by limiting most totals to no more than 1-2 (highest NeRAIN amount of 2.67 on the east side of York). Although the vast majority of hail/wind reports were tied to the aforementioned west-east corridor bisecting the heart of the area, two severe storms occurred well outside of this zone...one to the south/one to the north. The southern one was a discrete supercell that lumbered through parts of Webster/Nuckolls/Thayer counties but yielded only one report of quarter size hail in Nelson. Meanwhile, the northern-most severe storm was the left-split of a supercell that first developed southwest of Kearney, dropping 1.5-2 diameter hail in the Pleasanton and Loup City areas before weakening. ||Examining event evolution/meteorological background, the first weak convection of the evening within South Central Nebraska bubbled up in the Hastings area shortly before sunset, forming slightly north of a well-defined, southwest-northeast oriented quasi-stationary front stretched from west-central KS through southeast NE (storms that developed directly along this front earlier in the evening remained just southeast of the local area). Between 9-10 p.m. CDT two supercells quickly evolved out of the initial weak activity, one that pounded York with its first round of large hail and drilled the eastern part of the county with significant wind damage, and the other the aforementioned southern supercell that developed over Webster County. Between 10-11 p.m. CDT, these first severe storms either departed the local area into eastern Nebraska (the northern one) or weakened/dissipated (the southern one). However, not far to the west the primary supercell train was just getting warmed up as several severe storms rapidly blossomed along the Highway 6/Interstate 80 corridors within the western half of South Central Nebraska. This slightly-elevated activity developed in response to intensifying nocturnal convergence into a sharpening frontal zone very evident in the 850-700 millibar layer. Given that this low-mid level front was aligned nearly parallel to strong west-southwesterly upper level winds (attendant to a large scale trough centered over the Northern Rockies) and that the mesoscale environment featured a potent combination of very strong deep layer shear (50-70 knots) and decent most-unstable CAPE (1000-2000 J/kg), the stage was set for a somewhat rare episode of several supercells training along the same corridor in close succession. In fact, between 11 p.m. and 2 a.m. CDT, at least 3-5 severe-warned storms marched in tandem along this path, each core spaced out roughly 25 miles from the next. During this three-hour span, places such as Hastings and York endured three separate severe storms (bringing York up to FOUR direct hits...including the initial supercell of the night). While most of these cells remained just elevated enough to preclude a tornado threat, the first storm in the supercell train managed to spawn the EF-2 in southwestern York County...apparently tapping into JUST enough lower-level moisture/instability in the vicinity of the nearby surface front to become tornadic. Finally, between 2:00-3:30 a.m. CDT, the last two training supercells of the night passed through Hamilton, Polk and northern York counties before departing the local area, bringing an end to this unique and (in places) destructive event. A wind gust of 61 MPH was measured by a mesonet station located two miles north-northwest of Inland.", "ts_dict_index": [7704, 7705, 7706]}
+{"event_id": 991326, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2021-12-15 13:50:00", "end_date_time": "2021-12-15 13:50:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A semi-truck was overturned along Highway 6 near Adams Central Schools.", "ts_dict_index": [7665, 7666, 7667]}
+{"event_id": 994812, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-12-15 14:30:00", "end_date_time": "2021-12-15 14:30:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 65 MPH was measured by a mesonet station located four miles west-northwest of Deshler.", "ts_dict_index": [7677, 7678, 7679]}
+{"event_id": 994813, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-12-15 14:30:00", "end_date_time": "2021-12-15 14:30:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 61 MPH was measured by a mesonet station located three miles northwest of Deshler.", "ts_dict_index": [7680, 7681, 7682]}
+{"event_id": 1035665, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-06-07 20:45:00", "end_date_time": "2022-06-07 20:45:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 75 MPH was measured by a mesonet station located one mile south-southeast of Davenport.", "ts_dict_index": [7713, 7714, 7715]}
+{"event_id": 1035666, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-06-07 20:45:00", "end_date_time": "2022-06-07 20:45:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 61 MPH was measured by a mesonet station located in Davenport.", "ts_dict_index": [7710, 7711, 7712]}
+{"event_id": 1039525, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-06-14 23:16:00", "end_date_time": "2022-06-14 23:16:00", "narrative": "For the second consecutive Tuesday evening, a relatively small percentage of the 24-county South Central Nebraska area was ravaged by significant severe thunderstorms that caused countless instances of damage including (but not limited to): broken windows/damaged siding, flipped irrigation pivots, destroyed crops by the thousands of acres, and more isolated occurrences of outright-demolished outbuildings/grain bins along with relatively minor structural damage to a few homes. Unlike the event a week prior on the 7th that featured a few separate swaths of severe weather, this one that played out mainly between 9:30 p.m. CDT on the 14th and 3:30 a.m. CDT on the 15th was highlighted by just one narrow, west-southwest to east-northeast oriented swath of multiple training supercells. In fact, some locations (Hastings and York to name a few) actually endured three to four SEPARATE severe storms over a span of 2-4 hours! With only limited exception, the vast majority of storm reports emanated from a 10-20 mile wide stripe centered roughly along a line from Elwood-Kearney-Doniphan-York. Within this zone there were numerous reports of large hail (many golf ball to tennis ball size) and damaging winds mainly in the 60-75 MPH range (but isolated pockets of 90-100+ MPH...especially east Highway 14). In addition, an EF-2 tornado was confirmed in southwest York County. Also of note was that some very unlucky locales experienced nearly a repeat performance of what just unfolded seven evenings prior...struck by another round of large hail/damaging winds only days after starting to recover from the first event on the 7th. Although this overlapping damage was somewhat evident over northeastern Adams County, it was particularly visible within the southwestern quadrant of York County, where many fields were mostly stripped bare for miles around...creating a visually striking/eerie contrast to what is typically a sea of green under the mid-June sun. ||Taking a deeper dive into storm reports and starting with the EF-2 tornado, storm surveys concluded that it tracked just over seven miles through southwestern York County shortly after midnight CDT, developing west-southwest of Lushton and lifting west of McCool Junction. Along the way, several farmsteads sustained damage (including a garage torn from a home and a wood frame outbuilding completely demolished) and two people sustained minor injuries. Interestingly, an unofficial mesonet station in or very near the tornado path actually measured a 90 MPH gust a few miles east-northeast of Lushton. Turning to the many known (and countless unknown) occurrences of large hail/damaging straight line winds within the primary convective swath, a few of the more noteworthy wind damage/speed reports included: estimated 105 MPH winds in the Waco area that toppled a 60 ft. concrete silo; estimated 95 MPH winds through parts of northeastern Clay County that crumpled a grain bin near Saronville; widespread tree and sporadic structural damage in McCool Junction; separate measured wind gusts of 75 and 65 MPH at Hastings airport (from different storms 45 minutes apart); an unofficial mesonet gust of 79 MPH near Norman. Meanwhile, a few of the most notable hail reports featured: stones up to tennis ball size in York and Trumbull; hail up to 2.25 diameter at the NWS Hastings office that significantly dented the vehicles of on-duty meteorologists working this event; various reports of ping pong ball to golf ball size hail in or near Waco, Riverdale, Lushton, Bertrand, Kearney and seven miles south of Elwood. Rainfall-wise, despite the passage of several storms over the same areas, progressive storm motions mitigated the threat of significant flooding by limiting most totals to no more than 1-2 (highest NeRAIN amount of 2.67 on the east side of York). Although the vast majority of hail/wind reports were tied to the aforementioned west-east corridor bisecting the heart of the area, two severe storms occurred well outside of this zone...one to the south/one to the north. The southern one was a discrete supercell that lumbered through parts of Webster/Nuckolls/Thayer counties but yielded only one report of quarter size hail in Nelson. Meanwhile, the northern-most severe storm was the left-split of a supercell that first developed southwest of Kearney, dropping 1.5-2 diameter hail in the Pleasanton and Loup City areas before weakening. ||Examining event evolution/meteorological background, the first weak convection of the evening within South Central Nebraska bubbled up in the Hastings area shortly before sunset, forming slightly north of a well-defined, southwest-northeast oriented quasi-stationary front stretched from west-central KS through southeast NE (storms that developed directly along this front earlier in the evening remained just southeast of the local area). Between 9-10 p.m. CDT two supercells quickly evolved out of the initial weak activity, one that pounded York with its first round of large hail and drilled the eastern part of the county with significant wind damage, and the other the aforementioned southern supercell that developed over Webster County. Between 10-11 p.m. CDT, these first severe storms either departed the local area into eastern Nebraska (the northern one) or weakened/dissipated (the southern one). However, not far to the west the primary supercell train was just getting warmed up as several severe storms rapidly blossomed along the Highway 6/Interstate 80 corridors within the western half of South Central Nebraska. This slightly-elevated activity developed in response to intensifying nocturnal convergence into a sharpening frontal zone very evident in the 850-700 millibar layer. Given that this low-mid level front was aligned nearly parallel to strong west-southwesterly upper level winds (attendant to a large scale trough centered over the Northern Rockies) and that the mesoscale environment featured a potent combination of very strong deep layer shear (50-70 knots) and decent most-unstable CAPE (1000-2000 J/kg), the stage was set for a somewhat rare episode of several supercells training along the same corridor in close succession. In fact, between 11 p.m. and 2 a.m. CDT, at least 3-5 severe-warned storms marched in tandem along this path, each core spaced out roughly 25 miles from the next. During this three-hour span, places such as Hastings and York endured three separate severe storms (bringing York up to FOUR direct hits...including the initial supercell of the night). While most of these cells remained just elevated enough to preclude a tornado threat, the first storm in the supercell train managed to spawn the EF-2 in southwestern York County...apparently tapping into JUST enough lower-level moisture/instability in the vicinity of the nearby surface front to become tornadic. Finally, between 2:00-3:30 a.m. CDT, the last two training supercells of the night passed through Hamilton, Polk and northern York counties before departing the local area, bringing an end to this unique and (in places) destructive event. Wind gusts estimated to be near 60 MPH resulted in minor tree damage.", "ts_dict_index": [7686, 7687, 7688]}
+{"event_id": 1039445, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-06-14 22:41:00", "end_date_time": "2022-06-14 22:41:00", "narrative": "For the second consecutive Tuesday evening, a relatively small percentage of the 24-county South Central Nebraska area was ravaged by significant severe thunderstorms that caused countless instances of damage including (but not limited to): broken windows/damaged siding, flipped irrigation pivots, destroyed crops by the thousands of acres, and more isolated occurrences of outright-demolished outbuildings/grain bins along with relatively minor structural damage to a few homes. Unlike the event a week prior on the 7th that featured a few separate swaths of severe weather, this one that played out mainly between 9:30 p.m. CDT on the 14th and 3:30 a.m. CDT on the 15th was highlighted by just one narrow, west-southwest to east-northeast oriented swath of multiple training supercells. In fact, some locations (Hastings and York to name a few) actually endured three to four SEPARATE severe storms over a span of 2-4 hours! With only limited exception, the vast majority of storm reports emanated from a 10-20 mile wide stripe centered roughly along a line from Elwood-Kearney-Doniphan-York. Within this zone there were numerous reports of large hail (many golf ball to tennis ball size) and damaging winds mainly in the 60-75 MPH range (but isolated pockets of 90-100+ MPH...especially east Highway 14). In addition, an EF-2 tornado was confirmed in southwest York County. Also of note was that some very unlucky locales experienced nearly a repeat performance of what just unfolded seven evenings prior...struck by another round of large hail/damaging winds only days after starting to recover from the first event on the 7th. Although this overlapping damage was somewhat evident over northeastern Adams County, it was particularly visible within the southwestern quadrant of York County, where many fields were mostly stripped bare for miles around...creating a visually striking/eerie contrast to what is typically a sea of green under the mid-June sun. ||Taking a deeper dive into storm reports and starting with the EF-2 tornado, storm surveys concluded that it tracked just over seven miles through southwestern York County shortly after midnight CDT, developing west-southwest of Lushton and lifting west of McCool Junction. Along the way, several farmsteads sustained damage (including a garage torn from a home and a wood frame outbuilding completely demolished) and two people sustained minor injuries. Interestingly, an unofficial mesonet station in or very near the tornado path actually measured a 90 MPH gust a few miles east-northeast of Lushton. Turning to the many known (and countless unknown) occurrences of large hail/damaging straight line winds within the primary convective swath, a few of the more noteworthy wind damage/speed reports included: estimated 105 MPH winds in the Waco area that toppled a 60 ft. concrete silo; estimated 95 MPH winds through parts of northeastern Clay County that crumpled a grain bin near Saronville; widespread tree and sporadic structural damage in McCool Junction; separate measured wind gusts of 75 and 65 MPH at Hastings airport (from different storms 45 minutes apart); an unofficial mesonet gust of 79 MPH near Norman. Meanwhile, a few of the most notable hail reports featured: stones up to tennis ball size in York and Trumbull; hail up to 2.25 diameter at the NWS Hastings office that significantly dented the vehicles of on-duty meteorologists working this event; various reports of ping pong ball to golf ball size hail in or near Waco, Riverdale, Lushton, Bertrand, Kearney and seven miles south of Elwood. Rainfall-wise, despite the passage of several storms over the same areas, progressive storm motions mitigated the threat of significant flooding by limiting most totals to no more than 1-2 (highest NeRAIN amount of 2.67 on the east side of York). Although the vast majority of hail/wind reports were tied to the aforementioned west-east corridor bisecting the heart of the area, two severe storms occurred well outside of this zone...one to the south/one to the north. The southern one was a discrete supercell that lumbered through parts of Webster/Nuckolls/Thayer counties but yielded only one report of quarter size hail in Nelson. Meanwhile, the northern-most severe storm was the left-split of a supercell that first developed southwest of Kearney, dropping 1.5-2 diameter hail in the Pleasanton and Loup City areas before weakening. ||Examining event evolution/meteorological background, the first weak convection of the evening within South Central Nebraska bubbled up in the Hastings area shortly before sunset, forming slightly north of a well-defined, southwest-northeast oriented quasi-stationary front stretched from west-central KS through southeast NE (storms that developed directly along this front earlier in the evening remained just southeast of the local area). Between 9-10 p.m. CDT two supercells quickly evolved out of the initial weak activity, one that pounded York with its first round of large hail and drilled the eastern part of the county with significant wind damage, and the other the aforementioned southern supercell that developed over Webster County. Between 10-11 p.m. CDT, these first severe storms either departed the local area into eastern Nebraska (the northern one) or weakened/dissipated (the southern one). However, not far to the west the primary supercell train was just getting warmed up as several severe storms rapidly blossomed along the Highway 6/Interstate 80 corridors within the western half of South Central Nebraska. This slightly-elevated activity developed in response to intensifying nocturnal convergence into a sharpening frontal zone very evident in the 850-700 millibar layer. Given that this low-mid level front was aligned nearly parallel to strong west-southwesterly upper level winds (attendant to a large scale trough centered over the Northern Rockies) and that the mesoscale environment featured a potent combination of very strong deep layer shear (50-70 knots) and decent most-unstable CAPE (1000-2000 J/kg), the stage was set for a somewhat rare episode of several supercells training along the same corridor in close succession. In fact, between 11 p.m. and 2 a.m. CDT, at least 3-5 severe-warned storms marched in tandem along this path, each core spaced out roughly 25 miles from the next. During this three-hour span, places such as Hastings and York endured three separate severe storms (bringing York up to FOUR direct hits...including the initial supercell of the night). While most of these cells remained just elevated enough to preclude a tornado threat, the first storm in the supercell train managed to spawn the EF-2 in southwestern York County...apparently tapping into JUST enough lower-level moisture/instability in the vicinity of the nearby surface front to become tornadic. Finally, between 2:00-3:30 a.m. CDT, the last two training supercells of the night passed through Hamilton, Polk and northern York counties before departing the local area, bringing an end to this unique and (in places) destructive event. A wind gust of 65 MPH was measured by a mesonet station located four miles east-southeast of Hastings.", "ts_dict_index": [7701, 7702, 7703]}
+{"event_id": 1035663, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-06-07 20:36:00", "end_date_time": "2022-06-07 20:36:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 61 MPH was measured by a mesonet station located one mile north-northeast of Davenport.", "ts_dict_index": [7716, 7717, 7718]}
+{"event_id": 994811, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-12-15 14:32:00", "end_date_time": "2021-12-15 14:32:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 67 MPH was measured by a mesonet station located four miles east-southeast of Ruskin.", "ts_dict_index": [7674, 7675, 7676]}
+{"event_id": 846447, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-07-08 17:30:00", "end_date_time": "2019-07-08 17:30:00", "narrative": "Excessive rainfall, flash flooding, and severe winds occurred on this Monday afternoon and evening. Widely scattered thunderstorms began forming around 1 PM CST along and west of Highway 183. By 2 PM CST, a persistent line segment of thunderstorms began affecting western Dawson county. Over the following four hours, this southwest-northeast oriented line slowly crept east across Dawson county into western Buffalo county, with its southwest end moving from Gosper county into Phelps county. A downburst occurred in Cozad where winds were measured at 63 mph. Further east, trees were damaged near Elm Creek. This line of storms subsequently weakened as it moved into eastern Buffalo county. However, between 5 and 9 PM CST, numerous small thunderstorms formed over Gosper, Furnas, Phelps, and Harlan counties. Storms kept forming over these counties until a multi-county area of persistent heavy rain enveloped these counties and expanded north to include Dawson and Buffalo counties. By 9 PM CST, the heaviest rain had morphed to the southeast side of a large, expanding rain shield, with a nearly stationary band stretching from southwest to northeast across Furnas, Phelps, and Buffalo counties. After 10 PM CST, a large squall line that had developed far to the west, over the high plains, began moving into south-central Nebraska. It brought a third period of heavy rain to these counties, but its cold pool aided in shoving the training, slow-moving mass of heavy rain eastward. The two areas of rain merged with a progressive squall line subsequently advancing across the rest of the south central Nebraska. The squall line exited into southeast Nebraska by 230 AM CST. Severe downburst winds occurred a few spots with this squall line. A few tree limbs were snapped off in Oxford and Kearney, and 36 power poles were snapped off over a 2-mile stretch southeast of Holdrege. The highest rainfall total reported was 10.65 inches 3 miles southwest of Odessa. The second highest was 8.88 inches in Loomis. 8.33 fell near Hildreth, 7.66 in Riverdale, 7.60 near Lexington, 6.50 near Cozad, 5.90 near Minden, and 5.64 on the southwest side of Kearney.||Late in the afternoon, a few thunderstorms moved north from Kansas ahead of the storms west of Highway 183. These storms produced some spotty tree damage in Webster and Kearney counties, and damage two livestock sheds in the town of Ayr. A brief rope tornado was also reported near Roseland. ||At the surface, a stalled front extended from the Mid-Atlantic states west to the southern Kansas border. Throughout the day, this front gradually lifted north as a warm front. Meanwhile, low pressure over eastern Colorado moved into northwest Kansas, joining the western end of the front. In the upper-levels weak southwest flow was over Nebraska with a longwave trough advancing eastward through the western U.S., and a ridge over the Upper Midwest. An embedded shortwave trough moved out of Colorado and crossed Nebraska, creating a favorable environment for thunderstorms. As the initial thunderstorms developed, the environment was characterized by surface temperatures in the lower to middle 80s, with dewpoints in the lower 70s. Mid-level lapse rates were poor, but despite that, MLCAPE was 2500-3000 J/kg. Deep layer shear was weak at less than 20 kt. Precipitable water values were around 1.70 inches, which was close to a record. ||The excessive rainfall resulted in flash flooding in parts of Dawson, Gosper, Furnas, Harlan, Phelps, and Buffalo counties, including flooding across parts of U.S. Highways 6, 30, 183, and 283. Numerous gravel county roads were inundated by flood waters and impassible. Many of them were severely damaged. Roads in the city of Kearney were flooded from one curb to the other, and in at least two separate places, water was 3 to 4 ft deep. Almost 40 vehicles were stranded in Kearney streets. Basements were flooded in some homes due to egress windows breaking. The student union was flooded on the University of Nebraska campus in Kearney. Two to three feet of water was reported in the lower level of the food court. In Lexington, cars were stalled in flood waters and 23 people were evacuated from an apartment building due to flooding. The Red Cross opened a shelter to care for those evacuated.||In some areas, the impacts worsened the following day as creeks swelled out of their banks. Gibbon, Kearney, Odessa, Elm Creek, and Lexington were all severely impacted. U.S. highway 30 was closed due to floodwater from Shelton to Kearney to Elm Creek, as well as near Lexington. Turkey Creek drains into the North Channel of the Platte River, which runs through the south side of Kearney. Water rapidly rose on the south side of the city Tuesday morning, inundating numerous hotels, restaurants, businesses, and basements. At least 200 people had to be evacuated from hotels using construction grade front-end loaders. Approximately 100 other nearby residents needed to be evacuated as well. At its peak, water was 2 to 4 feet high inside the hotels, and 4 to 5 feet high in the parking lots. The water rose so quickly that many people staying at the hotels did not have time to move their vehicles. Most vehicles at the hotels were a total loss. Hundreds of vehicles in the city had to be towed. Some businesses were closed for weeks, others for months, as repairs and remodeling were completed. Kitchen equipment was ruined at some restaurants. Of the 1800 hotels rooms in Kearney, only about 600 were available for use because first floor services, such as check-in desks, laundry facilities, and kitchens were damaged. Stagecoach souvenir shop lost 2,000 pounds of merchandise. Second avenue, which is the main north-south thoroughfare through the city, was closed from Interstate 80 to 11th avenue. The Interstate 80 off ramp was also closed. All traffic to and from the Interstate, from the city, had to use the Kearney East Expressway. Approximately 400 Kearney homes were damaged by the flood, and many more beyond city limits. Just as one example, an egress window gave way in a home on the southeast side of Kearney. Water rushed into the basement, filling it nearly to the ceiling. Extensive flooding resulted in the closure of Yanney Park. A power substation flooded and resulted in power outages to about 450 customers. Flood waters began to subside Wednesday, July 10th, which allowed for one lane of 2nd avenue to be reopened in each direction.||In Odessa, flooding was significant. Water was 4 feet deep on Webb street. A little further south, the Odessa exit from Interstate 80 was closed because of significant flooding. Water was about 3 feet deep at the truck stop adjacent to the Interstate. Semi trucks and cars pulled into the truck stop due to the heavy rain Monday evening, but by 630 AM CST Tuesday, water was up to the top of the wheel wells on several semi's. Flooded vehicles had to be towed. The Platte River, which is very wide and shallow, rose 3 feet in 12 hours from 6 PM CST Monday to 6 AM CST Tuesday, and 4 feet in 24 hours. It is very difficult for the Platte River to flood, but it crested at 8.3 feet at 515 PM CST Tuesday. Flood stage is 7 feet.||In the town of Elm Creek, many roads and basements were flooded. A gauge on Elm Creek indicated that the water level rose 8 feet in 2 hours Monday evening.||The city of Lexington issued a disaster declaration due to the disruption of utility services. Streets and homes were flooded with sewers backing up into homes. ||Flooding was extensive along the Wood River. Moderate flooding occurred at Riverdale with water covering the bridge just north of town. Further to the north, flooding forced the closure of state highway 10 between Pleasanton and Hazard.||In Gibbon, water flooded streets and basements for the second time this year. The northeast side of town was impacted the worst with at least 30 homes and several businesses inundated by floodwater. People had to sandbag their homes and businesses. It is believed that flooding on the Wood River was wider with this event, due to changes in the riverbed from the prior flood in March. Some places that did not flood in that event, flooded this time. Many people commented, I can't believe this has happened twice. Several businesses affected by the March flood still remained closed due to damage.||Amtrak trains that travel between Chicago and Emeryville, CA were halted in Lincoln and McCook due to the flooding. There were probably many more impacts that were not documented here as it is not possible to include everything. Widespread flooding of low-lying areas, creeks, and rivers continued for several days following the excessive rain. Flood waters did not recede in some locations until Monday, July 15th. This devastating flood occurred just four months after a catastrophic flood occurred nearby in mid-to-late March. That flood affected areas primarily along and north of the Platte River. Two livestock sheds sustained minor damage. Report relayed via KSNB Local 4.", "ts_dict_index": [7683, 7684, 7685]}
+{"event_id": 1039487, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-06-14 23:11:00", "end_date_time": "2022-06-14 23:16:00", "narrative": "For the second consecutive Tuesday evening, a relatively small percentage of the 24-county South Central Nebraska area was ravaged by significant severe thunderstorms that caused countless instances of damage including (but not limited to): broken windows/damaged siding, flipped irrigation pivots, destroyed crops by the thousands of acres, and more isolated occurrences of outright-demolished outbuildings/grain bins along with relatively minor structural damage to a few homes. Unlike the event a week prior on the 7th that featured a few separate swaths of severe weather, this one that played out mainly between 9:30 p.m. CDT on the 14th and 3:30 a.m. CDT on the 15th was highlighted by just one narrow, west-southwest to east-northeast oriented swath of multiple training supercells. In fact, some locations (Hastings and York to name a few) actually endured three to four SEPARATE severe storms over a span of 2-4 hours! With only limited exception, the vast majority of storm reports emanated from a 10-20 mile wide stripe centered roughly along a line from Elwood-Kearney-Doniphan-York. Within this zone there were numerous reports of large hail (many golf ball to tennis ball size) and damaging winds mainly in the 60-75 MPH range (but isolated pockets of 90-100+ MPH...especially east Highway 14). In addition, an EF-2 tornado was confirmed in southwest York County. Also of note was that some very unlucky locales experienced nearly a repeat performance of what just unfolded seven evenings prior...struck by another round of large hail/damaging winds only days after starting to recover from the first event on the 7th. Although this overlapping damage was somewhat evident over northeastern Adams County, it was particularly visible within the southwestern quadrant of York County, where many fields were mostly stripped bare for miles around...creating a visually striking/eerie contrast to what is typically a sea of green under the mid-June sun. ||Taking a deeper dive into storm reports and starting with the EF-2 tornado, storm surveys concluded that it tracked just over seven miles through southwestern York County shortly after midnight CDT, developing west-southwest of Lushton and lifting west of McCool Junction. Along the way, several farmsteads sustained damage (including a garage torn from a home and a wood frame outbuilding completely demolished) and two people sustained minor injuries. Interestingly, an unofficial mesonet station in or very near the tornado path actually measured a 90 MPH gust a few miles east-northeast of Lushton. Turning to the many known (and countless unknown) occurrences of large hail/damaging straight line winds within the primary convective swath, a few of the more noteworthy wind damage/speed reports included: estimated 105 MPH winds in the Waco area that toppled a 60 ft. concrete silo; estimated 95 MPH winds through parts of northeastern Clay County that crumpled a grain bin near Saronville; widespread tree and sporadic structural damage in McCool Junction; separate measured wind gusts of 75 and 65 MPH at Hastings airport (from different storms 45 minutes apart); an unofficial mesonet gust of 79 MPH near Norman. Meanwhile, a few of the most notable hail reports featured: stones up to tennis ball size in York and Trumbull; hail up to 2.25 diameter at the NWS Hastings office that significantly dented the vehicles of on-duty meteorologists working this event; various reports of ping pong ball to golf ball size hail in or near Waco, Riverdale, Lushton, Bertrand, Kearney and seven miles south of Elwood. Rainfall-wise, despite the passage of several storms over the same areas, progressive storm motions mitigated the threat of significant flooding by limiting most totals to no more than 1-2 (highest NeRAIN amount of 2.67 on the east side of York). Although the vast majority of hail/wind reports were tied to the aforementioned west-east corridor bisecting the heart of the area, two severe storms occurred well outside of this zone...one to the south/one to the north. The southern one was a discrete supercell that lumbered through parts of Webster/Nuckolls/Thayer counties but yielded only one report of quarter size hail in Nelson. Meanwhile, the northern-most severe storm was the left-split of a supercell that first developed southwest of Kearney, dropping 1.5-2 diameter hail in the Pleasanton and Loup City areas before weakening. ||Examining event evolution/meteorological background, the first weak convection of the evening within South Central Nebraska bubbled up in the Hastings area shortly before sunset, forming slightly north of a well-defined, southwest-northeast oriented quasi-stationary front stretched from west-central KS through southeast NE (storms that developed directly along this front earlier in the evening remained just southeast of the local area). Between 9-10 p.m. CDT two supercells quickly evolved out of the initial weak activity, one that pounded York with its first round of large hail and drilled the eastern part of the county with significant wind damage, and the other the aforementioned southern supercell that developed over Webster County. Between 10-11 p.m. CDT, these first severe storms either departed the local area into eastern Nebraska (the northern one) or weakened/dissipated (the southern one). However, not far to the west the primary supercell train was just getting warmed up as several severe storms rapidly blossomed along the Highway 6/Interstate 80 corridors within the western half of South Central Nebraska. This slightly-elevated activity developed in response to intensifying nocturnal convergence into a sharpening frontal zone very evident in the 850-700 millibar layer. Given that this low-mid level front was aligned nearly parallel to strong west-southwesterly upper level winds (attendant to a large scale trough centered over the Northern Rockies) and that the mesoscale environment featured a potent combination of very strong deep layer shear (50-70 knots) and decent most-unstable CAPE (1000-2000 J/kg), the stage was set for a somewhat rare episode of several supercells training along the same corridor in close succession. In fact, between 11 p.m. and 2 a.m. CDT, at least 3-5 severe-warned storms marched in tandem along this path, each core spaced out roughly 25 miles from the next. During this three-hour span, places such as Hastings and York endured three separate severe storms (bringing York up to FOUR direct hits...including the initial supercell of the night). While most of these cells remained just elevated enough to preclude a tornado threat, the first storm in the supercell train managed to spawn the EF-2 in southwestern York County...apparently tapping into JUST enough lower-level moisture/instability in the vicinity of the nearby surface front to become tornadic. Finally, between 2:00-3:30 a.m. CDT, the last two training supercells of the night passed through Hamilton, Polk and northern York counties before departing the local area, bringing an end to this unique and (in places) destructive event. A wind gust of 75 MPH was measured by the Hastings Airport ASOS. Wind gusts were estimated to be closer to 60 MPH by a NWS Employee on the far south-southeast side of Hastings. Emergency management reported power pole damage and downed power lines in the area of the intersection of 14th and Baltimore streets.", "ts_dict_index": [7689, 7690, 7691]}
+{"event_id": 994810, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-12-15 14:35:00", "end_date_time": "2021-12-15 14:35:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. A wind gust of 63 MPH was measured by a mesonet station located three miles southeast of Deshler.", "ts_dict_index": [7659, 7660, 7661]}
+{"event_id": 1035655, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-06-07 20:30:00", "end_date_time": "2022-06-07 20:30:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 59 MPH was measured by a mesonet station located two miles south-southeast of Ong.", "ts_dict_index": [7728, 7729, 7730]}
+{"event_id": 1035644, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-06-07 19:58:00", "end_date_time": "2022-06-07 19:58:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 63 MPH was measured by a mesonet station located three miles northeast of Ayr.", "ts_dict_index": [7731, 7732, 7733]}
+{"event_id": 1035632, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-06-07 19:45:00", "end_date_time": "2022-06-07 19:50:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. Wind gusts estimated to be near 70 MPH were observed at the NWS Hastings office, located four miles north of Hastings, and likely occurred northeast of Juniata based on radar and surrounding reports. This wind was accompanied by hail up to the size of golf balls. Vehicle damage was reported at the NWS Hastings office. Several homes northeast of Juniata had broken windows from the wind-driven hail.", "ts_dict_index": [7740, 7741, 7742]}
+{"event_id": 1035669, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-06-07 21:01:00", "end_date_time": "2022-06-07 21:01:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 61 MPH was measured by a mesonet station located three miles north of Chester.", "ts_dict_index": [7734, 7735, 7736]}
+{"event_id": 1035671, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-06-07 21:10:00", "end_date_time": "2022-06-07 21:10:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. Wind gusts estimated to be near 60 MPH resulted in some downed tree limbs in Hubbell.", "ts_dict_index": [7737, 7738, 7739]}
+{"event_id": 1040179, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-06-14 23:55:00", "end_date_time": "2022-06-15 00:11:00", "narrative": "For the second consecutive Tuesday evening, a relatively small percentage of the 24-county South Central Nebraska area was ravaged by significant severe thunderstorms that caused countless instances of damage including (but not limited to): broken windows/damaged siding, flipped irrigation pivots, destroyed crops by the thousands of acres, and more isolated occurrences of outright-demolished outbuildings/grain bins along with relatively minor structural damage to a few homes. Unlike the event a week prior on the 7th that featured a few separate swaths of severe weather, this one that played out mainly between 9:30 p.m. CDT on the 14th and 3:30 a.m. CDT on the 15th was highlighted by just one narrow, west-southwest to east-northeast oriented swath of multiple training supercells. In fact, some locations (Hastings and York to name a few) actually endured three to four SEPARATE severe storms over a span of 2-4 hours! With only limited exception, the vast majority of storm reports emanated from a 10-20 mile wide stripe centered roughly along a line from Elwood-Kearney-Doniphan-York. Within this zone there were numerous reports of large hail (many golf ball to tennis ball size) and damaging winds mainly in the 60-75 MPH range (but isolated pockets of 90-100+ MPH...especially east Highway 14). In addition, an EF-2 tornado was confirmed in southwest York County. Also of note was that some very unlucky locales experienced nearly a repeat performance of what just unfolded seven evenings prior...struck by another round of large hail/damaging winds only days after starting to recover from the first event on the 7th. Although this overlapping damage was somewhat evident over northeastern Adams County, it was particularly visible within the southwestern quadrant of York County, where many fields were mostly stripped bare for miles around...creating a visually striking/eerie contrast to what is typically a sea of green under the mid-June sun. ||Taking a deeper dive into storm reports and starting with the EF-2 tornado, storm surveys concluded that it tracked just over seven miles through southwestern York County shortly after midnight CDT, developing west-southwest of Lushton and lifting west of McCool Junction. Along the way, several farmsteads sustained damage (including a garage torn from a home and a wood frame outbuilding completely demolished) and two people sustained minor injuries. Interestingly, an unofficial mesonet station in or very near the tornado path actually measured a 90 MPH gust a few miles east-northeast of Lushton. Turning to the many known (and countless unknown) occurrences of large hail/damaging straight line winds within the primary convective swath, a few of the more noteworthy wind damage/speed reports included: estimated 105 MPH winds in the Waco area that toppled a 60 ft. concrete silo; estimated 95 MPH winds through parts of northeastern Clay County that crumpled a grain bin near Saronville; widespread tree and sporadic structural damage in McCool Junction; separate measured wind gusts of 75 and 65 MPH at Hastings airport (from different storms 45 minutes apart); an unofficial mesonet gust of 79 MPH near Norman. Meanwhile, a few of the most notable hail reports featured: stones up to tennis ball size in York and Trumbull; hail up to 2.25 diameter at the NWS Hastings office that significantly dented the vehicles of on-duty meteorologists working this event; various reports of ping pong ball to golf ball size hail in or near Waco, Riverdale, Lushton, Bertrand, Kearney and seven miles south of Elwood. Rainfall-wise, despite the passage of several storms over the same areas, progressive storm motions mitigated the threat of significant flooding by limiting most totals to no more than 1-2 (highest NeRAIN amount of 2.67 on the east side of York). Although the vast majority of hail/wind reports were tied to the aforementioned west-east corridor bisecting the heart of the area, two severe storms occurred well outside of this zone...one to the south/one to the north. The southern one was a discrete supercell that lumbered through parts of Webster/Nuckolls/Thayer counties but yielded only one report of quarter size hail in Nelson. Meanwhile, the northern-most severe storm was the left-split of a supercell that first developed southwest of Kearney, dropping 1.5-2 diameter hail in the Pleasanton and Loup City areas before weakening. ||Examining event evolution/meteorological background, the first weak convection of the evening within South Central Nebraska bubbled up in the Hastings area shortly before sunset, forming slightly north of a well-defined, southwest-northeast oriented quasi-stationary front stretched from west-central KS through southeast NE (storms that developed directly along this front earlier in the evening remained just southeast of the local area). Between 9-10 p.m. CDT two supercells quickly evolved out of the initial weak activity, one that pounded York with its first round of large hail and drilled the eastern part of the county with significant wind damage, and the other the aforementioned southern supercell that developed over Webster County. Between 10-11 p.m. CDT, these first severe storms either departed the local area into eastern Nebraska (the northern one) or weakened/dissipated (the southern one). However, not far to the west the primary supercell train was just getting warmed up as several severe storms rapidly blossomed along the Highway 6/Interstate 80 corridors within the western half of South Central Nebraska. This slightly-elevated activity developed in response to intensifying nocturnal convergence into a sharpening frontal zone very evident in the 850-700 millibar layer. Given that this low-mid level front was aligned nearly parallel to strong west-southwesterly upper level winds (attendant to a large scale trough centered over the Northern Rockies) and that the mesoscale environment featured a potent combination of very strong deep layer shear (50-70 knots) and decent most-unstable CAPE (1000-2000 J/kg), the stage was set for a somewhat rare episode of several supercells training along the same corridor in close succession. In fact, between 11 p.m. and 2 a.m. CDT, at least 3-5 severe-warned storms marched in tandem along this path, each core spaced out roughly 25 miles from the next. During this three-hour span, places such as Hastings and York endured three separate severe storms (bringing York up to FOUR direct hits...including the initial supercell of the night). While most of these cells remained just elevated enough to preclude a tornado threat, the first storm in the supercell train managed to spawn the EF-2 in southwestern York County...apparently tapping into JUST enough lower-level moisture/instability in the vicinity of the nearby surface front to become tornadic. Finally, between 2:00-3:30 a.m. CDT, the last two training supercells of the night passed through Hamilton, Polk and northern York counties before departing the local area, bringing an end to this unique and (in places) destructive event. Measured and estimated wind gusts exceeding 60 MPH were reported in and around Hastings. A peak wind gust of 71 MPH was measured by a mesonet station located four miles east-southeast of Hastings. Other wind gusts included: 71 MPH measured by a mesonet station located two miles north of Hastings; 65 MPH measured by the Hastings Airport ASOS; 60 MPH estimated by a NWS employee on the far southeast side of Hastings.", "ts_dict_index": [7692, 7693, 7694]}
+{"event_id": 1035657, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-06-07 19:55:00", "end_date_time": "2022-06-07 19:55:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. Wind gusts estimated to be near 65 MPH resulted in minor tree damage across town, with one larger limb blocking a street.", "ts_dict_index": [7749, 7750, 7751]}
+{"event_id": 1015428, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-04-29 18:35:00", "end_date_time": "2022-04-29 18:35:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A wind gust of 58 MPH was measured by a mesonet station located three miles south-southeast of Strang.", "ts_dict_index": [7767, 7768, 7769]}
+{"event_id": 1035650, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-07 20:19:00", "end_date_time": "2022-06-07 20:25:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. Wind gusts were estimated to be near 60 MPH, resulting in minor tree damage.", "ts_dict_index": [7758, 7759, 7760]}
+{"event_id": 1035647, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-07 20:00:00", "end_date_time": "2022-06-07 20:00:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. Wind gusts were estimated to be near 70 MPH. Quarter size hail was also reported.", "ts_dict_index": [7743, 7744, 7745]}
+{"event_id": 1013561, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-04-29 17:46:00", "end_date_time": "2022-04-29 17:46:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A wind gust of 68 MPH was measured by a mesonet station located four miles east of Pauline.", "ts_dict_index": [7782, 7783, 7784]}
+{"event_id": 1035630, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-06-07 19:51:00", "end_date_time": "2022-06-07 19:51:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 71 MPH was measured by a mesonet station located two miles east-southeast of Fairmont.", "ts_dict_index": [7755, 7756, 7757]}
+{"event_id": 1015430, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-04-29 18:41:00", "end_date_time": "2022-04-29 18:41:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A wind gust of 59 MPH was measured by a mesonet station located five miles southeast of McCool Junction.", "ts_dict_index": [7773, 7774, 7775]}
+{"event_id": 1015426, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-04-29 18:29:00", "end_date_time": "2022-04-29 18:29:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A wind gust of 60 MPH was measured by a mesonet station located one mile north-northwest of Strang.", "ts_dict_index": [7779, 7780, 7781]}
+{"event_id": 1035654, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-07 20:26:00", "end_date_time": "2022-06-07 20:26:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 69 MPH was measured by a mesonet station located one mile north-northwest of Edgar. An NeRAIN comment noted that there was crop damage in the area.", "ts_dict_index": [7761, 7762, 7763]}
+{"event_id": 1035648, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-06-07 20:11:00", "end_date_time": "2022-06-07 20:11:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 65 MPH was measured by a mesonet station located two miles west-northwest of Fairfield.", "ts_dict_index": [7764, 7765, 7766]}
+{"event_id": 1015417, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-04-29 18:20:00", "end_date_time": "2022-04-29 18:20:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Wind gusts estimated to be near 75 MPH resulted in the destruction of a grain bin, with its debris scattered. A high voltage transmission line was also downed in the area.", "ts_dict_index": [7776, 7777, 7778]}
+{"event_id": 1035628, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-06-07 19:40:00", "end_date_time": "2022-06-07 19:45:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 62 MPH was measured by a mesonet station located five miles west of Hansen. A wind gust of 60 MPH was measured by a mesonet station located two miles south-southeast of Prosser.", "ts_dict_index": [7752, 7753, 7754]}
+{"event_id": 1035668, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-06-07 21:00:00", "end_date_time": "2022-06-07 21:01:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. Wind gusts estimated to be near 70 MPH resulted in a the destruction of a wood frame outbuilding. A semi truck was also overturned. An irrigation pivot was flipped and a few power poles were leaning.", "ts_dict_index": [7746, 7747, 7748]}
+{"event_id": 1015413, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-04-29 18:15:00", "end_date_time": "2022-04-29 18:40:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Measured wind gusts along this path included the following: 65 MPH from four miles east-southeast of Davenport; 62 MPH from four miles south-southwest of Carleton; 61 MPH from two miles west-southwest of Bruning. Fire department spotters in Carleton estimated that wind gusts were at least 65 MPH and that power was out in town.", "ts_dict_index": [7770, 7771, 7772]}
+{"event_id": 1015422, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-04-29 18:25:00", "end_date_time": "2022-04-29 18:35:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Measured wind gusts along this path included the following: 61 MPH from three miles east-northeast of Geneva; 60 MPH from four west of Geneva; 58 MPH from five miles west of Geneva. Power outages were reported in Geneva.", "ts_dict_index": [7785, 7786, 7787]}
+{"event_id": 1015418, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-04-29 18:25:00", "end_date_time": "2022-04-29 18:45:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Wind gusts of 58 MPH were measured by mesonets located four miles northeast of Belvidere and five miles north-northwest of Alexandria. Power lines were downed just south of Belvidere.", "ts_dict_index": [7788, 7789, 7790]}
+{"event_id": 1035638, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-06-07 19:45:00", "end_date_time": "2022-06-07 20:00:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. Wind gusts exceeding 60 MPH were reported all across the city of Hastings. Peak measured wind gusts included 66 MPH at the Hastings Airport ASOS and 59 MPH by a mesonet station located on the far eastern edge of Hastings. This wind was accompanied by hail as large as golf ball size to 2.5 inches in diameter. Reports of damage across town included broken windows, siding damage, downed tree limbs, and power outages.", "ts_dict_index": [7725, 7726, 7727]}
+{"event_id": 1015427, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-04-29 18:30:00", "end_date_time": "2022-04-29 18:30:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A wind gust 61 MPH was measured by a mesonet station located three miles northwest of Shickley.", "ts_dict_index": [7800, 7801, 7802]}
+{"event_id": 1013550, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-04-29 17:35:00", "end_date_time": "2022-04-29 17:45:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Wind gusts were estimated to be between 60 and 70 MPH in Glenvil.", "ts_dict_index": [7818, 7819, 7820]}
+{"event_id": 1013570, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-04-29 17:50:00", "end_date_time": "2022-04-29 18:00:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Wind gusts estimated to be near 70 MPH resulted in grain bins being destroyed as well as a nearby outbuilding located two miles west-northwest of Clay Center. A wind gust of 66 MPH was measured by a mesonet station located one mile north of Clay Center.", "ts_dict_index": [7815, 7816, 7817]}
+{"event_id": 1013569, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-04-29 17:55:00", "end_date_time": "2022-04-29 17:55:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Wind gusts estimated to be near 65 MPH resulted in tree damaged and downed power lines in Harvard. The larger trees were approximately two feet in diameter.", "ts_dict_index": [7812, 7813, 7814]}
+{"event_id": 1013573, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-04-29 18:00:00", "end_date_time": "2022-04-29 18:00:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A wind gust of 58 MPH was measured by a mesonet station located four miles northeast of Fairfield.", "ts_dict_index": [7803, 7804, 7805]}
+{"event_id": 1014763, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-04-29 18:05:00", "end_date_time": "2022-04-29 18:15:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A large swath of wind gusts estimated to be between 70 and 85 MPH, with localized gusts near 95 MPH, swept across far southeastern Clay County into southern Fillmore County. Along and near this path, widespread tree damage and power outages occurred, with emergency management reporting at least 250 pivots overturned. Numerous power poles were snapped, several grain bins were destroyed, and a few outbuildings were destroyed. The strongest of these gusts concentrated in an area from near the Clay-Fillmore County line west of Shickley to approximately three miles northeast of Shickley. This area had the majority of the power pole, grain bin, and outbuilding damage. Mesonets in this area measured the following gusts: 78 MPH four miles northeast of Shickley; 77 MPH four miles south of Geneva; 76 MPH three miles east of Shickley; 68 MPH three miles south-southeast of Geneva.", "ts_dict_index": [7809, 7810, 7811]}
+{"event_id": 1013547, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-04-29 17:30:00", "end_date_time": "2022-04-29 17:30:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). Wind gusts estimated to be near 65 MPH blew a small-but-sturdy storage shed from behind a home into the front yard (it had been sitting on concrete blocks).", "ts_dict_index": [7794, 7795, 7796]}
+{"event_id": 1013555, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-04-29 17:35:00", "end_date_time": "2022-04-29 17:35:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A small grain bin was blown between the house and a workshop. Damage was reported to a hydrant and fencing.", "ts_dict_index": [7797, 7798, 7799]}
+{"event_id": 1013546, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-04-29 17:28:00", "end_date_time": "2022-04-29 17:28:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A wind gust of 64 MPH was measured by a mesonet station located three miles northeast of Ayr.", "ts_dict_index": [7791, 7792, 7793]}
+{"event_id": 1035667, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-06-07 20:49:00", "end_date_time": "2022-06-07 20:49:00", "narrative": "While nearly all of South Central Nebraska experienced thunderstorms on this Tuesday evening, the majority of severe storms (significantly severe in places) concentrated within two distinct, northwest-southeast swaths mainly no more than 10-20 miles across...both associated with discrete supercells (one of which eventually morphed into more of a quasi-linear convective system/QLCS). The primary/longest corridor of severe weather primarily impacted the the following local counties: southern/western Sherman, northern/eastern Buffalo, southern/western Hall, northern/eastern Adams (including Hastings), southern/western Clay and much of Nuckolls/Thayer. The other notable (but shorter-in-length) swath of storm damage wrought havoc across parts of eastern Hamilton, southern/western York and northern Fillmore counties. Within each of these corridors, there were numerous reports of severe winds and/or large hail (some at least 2-3 inch diameter), causing countless instances of damage such as: broken windows in homes and vehicles, significant damage to siding/roofs, innumerable flipped irrigation pivots, and the destruction of many thousands of acres of young crops. In addition to the considerable hail/damaging winds that impacted several counties, one QLCS tornado was also confirmed in Nuckolls/Thayer counties (rated EF-0). This event marked the fourth-consecutive day of severe storms within the 24-county area, and was the overall most significant round of all. Duration-wise, this event was actually fairly quick-hitting, with all South Central Nebraska severe storms unfolding during a 3.5 hour span between 7:00-10:30 p.m. CDT...starting off in northern counties and eventually exiting far south-southeast counties. ||Digging deeper into storm reports, and starting with the QLCS EF-0 tornado, it was determined to have tracked for nearly 10 miles through southeastern Nuckolls/southwestern Thayer counties shortly before 10 p.m. CDT, causing tree damage in Ruskin and then destroying/damaging several grain bins, irrigation pivots and a few outbuildings before lifting north of Byron. However, by far the biggest impacts of the evening resulted from large hail/damaging winds. Within the aforementioned longer corridor of damage extending along a line from Sherman through Nuckolls/Thayer counties, a sampling of some of the more noteworthy reports included: 2.5-3.5 diameter hail and 70 MPH winds in the Litchfield and Hazard areas (considerable window/siding damage); hail stones 2-4 diameter through the Ravenna/Pleasanton areas (considerable window/siding damage including shattered windows on a few fire trucks); combo of hail 1.75-2.50 diameter and measured 66 MPH winds in Hastings (considerable window/siding damage especially on north/west sides of the city); widespread 60-70 MPH winds through southern/western Clay County with over a dozen toppled irrigation pivots; wood frame outbuilding destroyed and a semi truck overturned near Hebron. Within the shorter swath of concentrated damage that tore through Hamilton/York/Fillmore counties, various reports included: a semi truck blown over on Interstate 80 and areas of complete crop destruction and many overturned irrigation pivots due to a combo of 60-70 MPH winds and hail up to 2 diameter (particularly in the Hampton, Henderson and McCool Junction areas). While these two main swaths accounted for the vast majority of South Central Nebraska storm reports during the evening, there were also a few more isolated pockets of severe weather well-removed from both of them. These included a mesonet-measured 64 MPH wind gust near Lexington and also a handful of reports associated with a supercell that barely skirted the northeast fringes of the local area (including golf ball size hail near Genoa and a measured 65 MPH gust near Shelby (with pivots reported overturned). ||Examining event evolution/timing, the first scattered storms of the evening (initially non-severe) formed between 6-7 p.m. CDT along a west-east oriented band across far northern local counties. Then, the action really ramped up/intensified during the next hour as: 1) a long-lived supercell that developed several hours prior in the northern NE Panhandle entered the local area into Sherman County (the beginning stages of the primary swath of severe weather)...2) a new intense supercell flared up over central/eastern Hamilton County (along the southern fringes of the initial weak northern activity)...3) another comparably shorter-lived supercell developed out of the eastern fringes of the northern storms and clipped the northeast fringes of the local area in Nance/Merrick/Polk counties. Between 8-10 p.m. CDT, the two primary South Central Nebraska supercells continued east-southeast, with the eastern one exiting the local area out of York/Fillmore counties, while the western one gradually merged with a developing convective line that extended off to its west-southwest. Shortly after this powerful storm tore through eastern Adams/western Clay counties, a gradual storm mode transition from semi-discrete supercell to small-scale severe QLCS was complete, leading to a reduced large hail threat but a continued threat of damaging winds (along with the aforementioned tornado). Finally, between 10-11 p.m. CDT the main QLCS segment over Thayer County, along with weaker linear storms trailing westward along the Nebraska-Kansas border, completely exited South Central Nebraska to the south-southeast, ending a very active 3-4 hours. Wrapping up with a closer look at the meteorological setup, this event was the grand finale to a multiple-day stretch of at least spotty severe storms within South Central Nebraska. But compared to prior days, forcing was stronger both aloft and at the surface, leading to an overall-more impactful event. In the mid-upper levels, west-northwest flow prevailed, featuring a fairly potent (albeit low amplitude) shortwave trough zipping eastward across northern NE/southern SD during the afternoon-evening. At the surface, the day began with an initially weakly-defined, west-east oriented front draped across southern portions of the local area. But during the evening, this boundary sharpened up and made a more pronounced southward surge into Kansas in response to a combination of pressure rises driven by the aforementioned upper wave and also convective outflow. Although quite a bit of daytime cloud cover helped hold afternoon temperatures across most of South Central Nebraska down in the mid-upper 70s (F) and low level moisture levels were only only seasonably-modest (dewpoints low-mid 60s F), an impressive combination of strong deep layer wind shear of at least 50-60 knots and mixed-layer CAPE of 1000-2000 J/kg clearly supported higher-end severe weather. From a forecast/messaging perspective this was a well-anticipated event, as SPC's second Day 2 Outlook (issued on the 6th) upgraded most of South Central Nebraska to an Enhanced Risk (level 3 of 5), with this Enhanced category then maintained throughout the subsequent Day 1 cycle. A wind gust of 71 MPH was measured by a mesonet station located five miles southeast of Ruskin.", "ts_dict_index": [7707, 7708, 7709]}
+{"event_id": 975076, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-07-09 22:28:00", "end_date_time": "2021-07-09 22:34:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. A wind gust of 60 MPH was recorded by mesonet station located three miles south-southwest of Shickley between 11:28-11:30 PM CDT. A wind gust of 58 MPH was recorded by a mesonet station located three miles southeast of Shickley at 11:34 PM CDT.", "ts_dict_index": [7851, 7852, 7853]}
+{"event_id": 974141, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-07-09 22:04:00", "end_date_time": "2021-07-09 22:04:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. A wind gust of 59 MPH was recorded by a Nebraska Mesonet station located four miles southwest of Harvard.", "ts_dict_index": [7845, 7846, 7847]}
+{"event_id": 1014772, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-04-29 18:15:00", "end_date_time": "2022-04-29 18:40:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A large swath of wind gusts estimated to be between 70 and 85 MPH, with localized gusts near 95 MPH, swept across far southeastern Clay County into southern Fillmore County. Along and near this path, widespread tree damage and power outages occurred, with emergency management reporting at least 250 pivots overturned. Numerous power poles were snapped, several grain bins were destroyed, and a few outbuildings were destroyed. The strongest of these gusts was focused in an area from near the Clay/Fillmore County line west of Shickley to approximately three miles northeast of Shickley. This area had the majority of the power pole, grain bin, and outbuilding damage. Mesonets in this area measured the following gusts: 78 MPH, four miles northeast of Shickley; 77 MPH, four miles south of Geneva; 76 MPH, three miles east of Shickley; 68 MPH, three miles south-southeast of Geneva.", "ts_dict_index": [7821, 7822, 7823]}
+{"event_id": 975080, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-07-09 22:30:00", "end_date_time": "2021-07-09 22:45:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. Wind gusts estimated to be near 70 MPH resulted in roof damage at the school building in Strang. Public reported damage to outbuildings and large trees downed in the area. A wind gust of 59 MPH was recorded by a mesonet station located one mile north-northwest of Strang. A wind gust of 62 MPH was recorded by a mesonet station located three miles east of Strang.", "ts_dict_index": [7836, 7837, 7838]}
+{"event_id": 975079, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-07-09 22:45:00", "end_date_time": "2021-07-09 22:45:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. A wind gust of 69 MPH was recorded by a mesonet station located four miles east-southeast of Geneva.", "ts_dict_index": [7848, 7849, 7850]}
+{"event_id": 975073, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-07-09 22:05:00", "end_date_time": "2021-07-09 22:11:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. A wind gust of 76 MPH was recorded by a mesonet station located two miles west-northwest of Fairfield at 11:09 PM CDT. A wind gust of 61 MPH was recorded by a mesonet station located four miles northeast of Fairfield at 11:11 PM CDT. The Cooperative Observer located six miles east-southeast of Clay Center estimated wind speeds of at least 70 MPH.", "ts_dict_index": [7842, 7843, 7844]}
+{"event_id": 962426, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2021-06-10 17:59:00", "end_date_time": "2021-06-10 17:59:00", "narrative": "Hit and miss thunderstorms ramped up on the 6th. Two to more than three inches of rain was measured at Cane Creek State Park (Lincoln County), Fordyce (Dallas County), Monticello (Drew County), Nashville (Howard County), and Pine Bluff (Jefferson County). Several roads were under water between Avilla (Saline County) and Ferndale (Pulaski County), and also at Monticello (Drew County).||During the predawn hours of the 7th, thunderstorm winds downed a tree on Highway 53 just south of Gurdon (Clark County). This caused a log truck to overturn. In the afternoon, more trees were toppled in Camden and East Camden (both in Ouachita County). A chapel roof was damaged just southwest of Cummins (Lincoln County), and part of a roof was blown off close to Sorrells (Jefferson County).||At least a dozen Tornado Warnings were issued in portions of Calhoun, Clark, Cleveland, Dallas, Garland, Hot Spring, Montgomery, Ouachita, and Pike Counties. A funnel cloud was spotted by law enforcement at Gum Springs (Clark County). There was a brief tornado reported (rated EFU, where U is unknown because there was no damage to evaluate) to the west of Calion (Union County) at 426 pm CDT. The tornado apparently did little more than kick up some dust.||On the 8th, there was a life threatening deluge in southeast Arkansas. Showers and thunderstorms became widespread, and moved over the same areas for several hours.||Too much rain flooded roads at Star City and Varner (both in Lincoln County), Pine Bluff (Jefferson County), Stuttgart (Arkansas County), and also at Dumas and McGehee (both in Desha County). Water got into many homes. Crop and road damage (washouts) was reported in Bradley County. A creek was out of its banks just southeast of Timber Ridge (Pulaski County).||There was high water along Highway 114 between Calmer and Rison (both in Cleveland County), Highway 425 near Yorktown (Lincoln County), Highway 293 east of Garrett Bridge (Lincoln County), Highway 46 not far from Ebb (Grant County), Highway 276 on the south side of Stuttgart (Arkansas County), and Highway 1 at Kelso (Desha County). These highways were eventually closed temporarily.||The situation was the most serious in Desha and Drew Counties, and a Flash Flood Emergency was issued for the communities of Dumas, Pickens, Rohwer (all in Desha County), and Winchester (Drew County) at 1142 am CDT on the 8th. Radar estimated 10 to more than 15 inches of rain, and there was water everywhere. Some folks indicated (through social media) they had never witnessed flooding of this magnitude.||From an historic perspective, Rohwer (Desha County) received 9.25 inches of rain in the twenty four hour period ending at 700 am CDT on the 8th. This was the most rain in one day at the site, and the fourth largest one day total across the state in June. If that was not enough, 9.97 inches of liquid was measured the next day! Adding the numbers, the whopping 19.22 inches on the 8th/9th was the second biggest two day amount in Arkansas. It was just behind the 21.45 inches at Danville (Yell County) on December 3-4, 1982.||Relentless cloudbursts continued to start the 9th in eastern Arkansas. A rain gauge near DeValls Bluff (Prairie County) completely filled (to six inches) between 400 am and 700 am CST. Buildings were flooded and cars were stalled in Clarendon (Monroe County). It was the same story in Humnoke (Lonoke County), and sandbags were ordered to stop the water.||It was just getting worse in Stuttgart (Arkansas County), with one picture showing more water in a home than ever before (in the life of the photographer/42 years). That claim was likely true because the 7.50 inches of rain that caused the problem easily surpassed the previous one day June record of 4.07 inches on the 29th in 1939. At least fifteen homes were impacted by flooding at Altheimer (Jefferson County). Highway 302 from Highway 17 to Highway 79 was shut down in Monroe County, as was Highway 15 near Sherrill (Jefferson County), Highway 33 east of Tollville (Prairie County), and Highways 85 and 318 near Oneida (Phillips County).||As the weather calmed down in the east by the afternoon of the 9th, temperatures warmed well into the 80s to around 90 degrees across the northern and central counties. Heating and lots of humidity were enough to fuel isolated strong to severe storms toward evening.||Just after 700 pm CDT, a video showed a tornado (rated EFU) that lasted two minutes in a field near Blakemore (Lonoke County). Between 700 pm and 800 pm CDT, there was quarter size hail just east of College Station (Pulaski County). Little Rock (Pulaski County) got a quick 1.10 inches of rain. Trees were blown down at Cave City (Sharp County). At 805 pm CDT, there was a brief weak tornado (rated EF0) a few miles southeast of England (Lonoke County).||The focus shifted back to the southeast early on the 10th. You guessed it...the sky was falling again. Rain plus runoff from the soaking on the 8th/9th in northern and central Desha County inundated farms toward Halley (Desha County) in the south. At 200 pm CDT, an irrigation canal east of Pickens (Desha County) was breached, and adjacent farmland became a lake. The canal was patched by evening. At Florence (Drew County), residents were forced to use boats to get around. Water threatened structures at Dermott and Eudora (both in Chicot County), and sandbagging was in progress. It was clear that assistance was needed, and Arkansas Governor Asa Hutchinson declared a state of emergency. ||All was quiet quiet in Little Rock (Pulaski County) on the 10th, and the sun was out. For the first time in 2021, the temperature touched 90 degrees (the high was 92 degrees), and it was three weeks late (it normally happens by May 18th). Toward evening, it got loud toward Pinnacle Mountain (Pulaski County). A severe storm pumped out quarter size hail, winds strong enough to push over a few trees, and up to six inches of rain in less than two hours. The terrain accentuated the flow of water across roads and into neighborhoods. A tree was downed on Chalamont Drive.", "ts_dict_index": [7830, 7831, 7832]}
+{"event_id": 974142, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-07-09 21:47:00", "end_date_time": "2021-07-09 22:15:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. Wind gusts estimated to be near 95 MPH occurred along this path. The main reports of damage came from the Harvard and Sutton areas. Widespread tree damage was reported, along with large areas of flattened crops. Minor roof damage occurred in Sutton. Numerous power outages were reported. Emergency management reported multiple irrigation pivots overturned in the area, along with 3 large grain bins destroyed and an outbuilding damaged along N Road near Harvard.", "ts_dict_index": [7833, 7834, 7835]}
+{"event_id": 1026870, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-05-12 16:59:00", "end_date_time": "2022-05-12 17:06:00", "narrative": "Major severe weather event unfolds across south central Nebraska during the afternoon and evening of May 12th, including wind gusts of 80 to 90 MPH. The most significant severe weather event of May 2022 occurred on a Thursday in which multiple rounds of thunderstorms wreaked havoc on essentially all of south central Nebraska at some point. The most intense severe weather, by far, was the first round. This activity actually developed over portions of west/southwest Kansas during the morning hours and moved northeast. Rapid intensification took place between 1PM and 2PM CDT as thunderstorms organized into a long line, and the first Severe Thunderstorm Warnings were issued for areas from Phillipsburg, KS to Lexington, NE. Initial storm reports ranged from quarter to ping pong ball size hail with the southern portion of the line, to widespread damaging wind gusts with the northern portion of the line across a large portion of Dawson County. Wind damage consisted of overturned pivots, uprooted trees, broken power poles, fence and roof damage, large tree limbs downed. Wind damage was widespread over central and western Dawson County where measured wind gusts of 60-70 MPH were common. Even an 82 MPH gust, which is considered ���significant severe���, was measured by a mesonet near Eddyville. Surface temperatures near 90 degrees and mixed layer CAPE values in excess of 3000 J/kg ahead of the line of thunderstorms, amidst 35kt to 50kt of southwesterly deep layer shear, allowed for continued intensification through the mid to late afternoon as the line raced northeast. Additional significant damaging wind impacts were felt across Sherman, Valley, and Greeley Counties. Valley County was another area especially hard hit. Here, several wind gusts in the 80-90 MPH range were reported, and damage was significant. Numerous trees were uprooted, pivots overturned, and outbuildings and grain bins destroyed. Another destructive aspect of this storm is that it also produced ping pong ball sized hail that was blown by the intense winds. This resulted in significant window and body damage to cars, as well as roof, siding, and window damage to homes. Additional significant wind damage was reported in and around Burwell (just barely outside this coverage area). The first round of thunderstorms exited north/northeast of the area around 3:30PM CDT, but the next round was ���hot on its heels���, and entered southern Nebraska around 4PM CDT, and quickly became severe. In fact, brief, but intense, circulations were noted on radar for a time just south and southeast of Hastings. This round affected mainly areas along and east of Highway 281. Since this region was spared from the first round, and a similar thermodynamic and kinematic environment was still in place, it���s no surprise that this round also intensified enough to produce ���significant severe��� wind gusts, most notably in a swath from Clay County northeast to Polk County. Several more 60-70 MPH wind gusts were reported in these areas, causing more overturned pivots, downed power lines, and damage to roofs, outbuildings, and grain bins. Also, intense wind gusts moved over Interstate 80 in Hamilton County, causing multiple overturned semis. This second round exited into eastern Nebraska and out of the Hastings CWA around 7PM CDT. The third and final round began to affect areas along and east Highway 183 between 7PM and 8PM CDT. The majority of this activity remained sub-severe as the greatest instability had been used up by the two previous rounds. However, a marginally severe wind gust of 59 MPH was measured at the Hastings airport shortly before 8PM. Thereafter, weakening ensued as the line became strung out and forward propagation slowed. Thunderstorms finally exited south central Nebraska between 11PM and midnight, ending a roughly 10 hour stretch of seemingly never ending severe weather!||Meteorologically speaking, this event was driven by a particularly volatile combination of intensifying shortwave ejecting from the central Rockies into the northern Plains, very unstable airmass (MUCAPE of 3000-4000 J/kg at it���s peak), and strong deep layer shear driven by 500 mb speed max of 60-70 kt. While this setup is not unheard of for mid-May, it���s certainly not very common, and for three distinct waves of thunderstorms to move through in a 10 hour period (two of which contained significant severe weather phenomena) is also not very common. From a regional perspective, the Hastings CWA was the developing grounds for a significant derecho that would propagate into the Northern Plains and Upper Mississippi Valley and go on to produce hundreds of measured severe wind gusts and wind damage reports, of which over 60 were considered ���significant severe���. Over 75 hail reports and nearly three dozen tornado reports were also reported, with the majority of tornadoes occurring in SD and MN. For 2022, this will likely be remembered as one of the most severe convective events of the year, both locally, and across the greater region. A wind gust of 66 MPH was measured by a mesonet station located three miles east-northeast of Davenport. A gust of 61 MPH was measured by a mesonet stateion located four miles east-southeast of Davenport.", "ts_dict_index": [7866, 7867, 7868]}
+{"event_id": 974119, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2021-07-09 21:57:00", "end_date_time": "2021-07-09 21:57:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. Wind gusts were estimated to be near 65 MPH.", "ts_dict_index": [7854, 7855, 7856]}
+{"event_id": 1013553, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-04-29 17:33:00", "end_date_time": "2022-04-29 17:33:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A wind gust of 62 MPH was measured by a mesonet station located four miles west-northwest of Glenvil.", "ts_dict_index": [7827, 7828, 7829]}
+{"event_id": 1015412, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-04-29 18:13:00", "end_date_time": "2022-04-29 18:13:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A wind gust of 91 MPH was measured by a mesonet station located two miles south-southeast of Davenport.", "ts_dict_index": [7824, 7825, 7826]}
+{"event_id": 974130, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-07-09 22:20:00", "end_date_time": "2021-07-09 22:50:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. The peak measured wind gusts was 71 MPH, recorded at 11:37 PM CDT by a mesonet station located three miles east-southeast of Carleton. Other gusts included: 67 MPH, recorded at 11:45 PM CDT by a mesonet station located three miles east-southeast of Belvidere; 59 MPH, recorded at 11:41 PM CDT by a mesonet station located four miles northeast of Belvidere; 59 MPH, recorded at 11:21 PM CDT by a mesonet station located 2 miles south-southeast of Davenport. Emergency management reported power outages, tree and crop damage along and near this path, including a tree that fell onto a car in Alexandria. Corn was flattened in many spots, with at least a half-dozen pivots overturned. A power pole was snapped near the intersection of Highway 4 and Highway 5.", "ts_dict_index": [7839, 7840, 7841]}
+{"event_id": 974129, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-07-09 22:37:00", "end_date_time": "2021-07-09 22:37:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. Wind gusts were estimated to be near 70 MPH, with tree limbs down across town.", "ts_dict_index": [7860, 7861, 7862]}
+{"event_id": 974118, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2021-07-09 21:54:00", "end_date_time": "2021-07-09 21:54:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. A wind gust of 58 MPH was recorded by a mesonet station located 1 mile southwest of Roseland.", "ts_dict_index": [7857, 7858, 7859]}
+{"event_id": 1015429, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-04-29 18:38:00", "end_date_time": "2022-04-29 18:38:00", "narrative": "A substantial round of severe thunderstorms rolled through South Central Nebraska on this Friday afternoon-early evening, causing a plethora of wind damage, scattered pockets of large hail (some very large) and four confirmed, short-track tornadoes (one rated EF-0, three EF-Unknown). For being such a widespread event (the majority of the 24 counties experienced at least limited severe weather) it was fairly quick-evolving and quick-hitting, as all local storms occurred within a 4.5-hour span between 3:30-8 p.m. CDT. Convective mode was a potent, but messy mix consisting primarily of an eastward-charging quasi-linear convective system (QLCS), but also a few briefly-discrete supercells that flared up just ahead of the QLCS (and were subsequently overtaken by it), along with at least one supercell structure embedded within the southern reaches of the QLCS. Digging deeper into storm reports, and starting with the four tornadoes, the first two (both with no known damage) touched down briefly in southwestern Harlan County, spawned by the first (and most isolated) supercell of the day. A short time later, another brief tornado (also no damage reported) was spotted in south central Kearney County, associated with a supercell that initiated just ahead of the approaching QLCS. The fourth tornado, though only rated EF-0, was the most noteworthy one as it developed along the far southern fringes of the QLCS in the Ruskin-Deshler area, overturning several pivots and damaging an outbuilding along a nearly five mile path. However, by far the biggest story of the day was significant straight-line wind damage. Though sporadic pockets of damage occurred in western counties, by far the most concentrated swaths focused within the following counties: Adams, Nuckolls, Thayer and especially Clay/Fillmore. This was due to a combination of the QLCS peaking in intensity over this area, along with it containing the embedded supercell. The most notable corridor of destructive winds took aim on southeastern Clay, southwestern Fillmore and northern Thayer counties. To mention just a few storm reports from this zone: at least 250 irrigation pivots toppled; several grain bins and a few outbuildings destroyed; unofficial mesonet-measured wind gusts as high as 91 MPH near Davenport and 78 MPH near Shickley. Outside of this worst-hit area (and farther north/west): a sampling of thunderstorm wind issues included: estimated 75 MPH gusts that derailed approximately 15 train cars near Shelton, estimated winds of 65-70 MPH in the Minden and Hastings areas (downed trees in Minden and a small-but-sturdy storage shed blown from behind a home into a front yard in south Hastings); measured gusts of 64 MPH as far north as Ord and 61 MPH as far west as Bertrand. Although taking a back seat to damaging winds due to being more localized, several large hail reports came in from various counties, including some very large stones to at least tennis ball size. The majority of the largest hail occurred with the first supercell of the day in Furnas County, including up to baseball size south of Holbrook and tennis ball size in Beaver City/Hollinger. However, the outright-biggest stone of the event measured 4 inches in diameter, plunging earthward several miles southwest of Minden. On the less extreme side of things, ping pong ball to golf ball size hail fell in various locations including Kearney, Minden and Alma. ||Taking a closer look at event evolution/timing, the first supercell initiated over northern Furnas County around 3:30 p.m. CDT, forming on a classic surface triple point...slightly north-northwest of strong low pressure (992 millibars) centered over north central Kansas. For a short time this storm was the only show locally, drifting slowly southeastward and dropping large hail and brief tornadoes. However, by 4:30 p.m. CDT, a north-south oriented linear system was already into Dawson/Gosper counties, driven eastward by strong convergence along an accelerating cold front. Between 5-6 p.m. CDT a few supercells/discrete multicells briefly developed over Kearney/Buffalo counties (including the one that produced the very large hail/brief tornado in Kearney County), but these storms were soon ingested by the surging QLCS. Between 6-7 p.m. CDT this complex surged across the Highway 281 corridor while a new cluster of severe convection flared up just ahead its southern edge mainly over Webster/Clay/Nuckolls counties. Finally, between 7-8 p.m. CDT, the southern portion of the QLCS (with an embedded supercell) took center stage, wreaking havoc upon the Clay/Fillmore/Thayer counties area with damaging winds before exiting the local domain into southeast Nebraska. During this same time frame, the northern portion of the QLCS (near/north of Interstate 80) prevailed weaker in nature and yielded few storm reports, but did drop quarter size hail near Shelby before exiting the coverage area. Finishing with a closer look at the meteorological situation, overall this was a prime springtime severe thunderstorm setup. In the mid-upper levels, a strong, slightly negatively-tilted shortwave trough ejected out of the Rockies and across the heart of Nebraska/northern Kansas over the course of the afternoon-evening. At the surface, the primary low pressure center drifted slowly eastward across northern Kansas, with a fairly well-defined warm front taking shape along the NE/KS border ahead of it and a sharp cold front/dryline combination surging in behind it. Despite a somewhat marginal thermodynamic environment featuring surface temperatures only in the 70s (F) and dewpoints only upper 50s-low 60s, steep mid-level lapse rates prompted healthy instability with mixed-layer CAPE peaking as high as 1500-3000 J/kg mainly along/south of the I-80 corridor. Deep-layer shear was modestly-strong (as high as 40-50 knots) and storms entered an increasingly-volatile low-level shear environment as they worked east of Highway 281, with southern portions of the QLCS encountering significant 0-1 kilometer storm relative helicity (SRH) of 200-300 m2/s2 (corresponding to the area of greatest wind damage). From a forecast perspective this was a well-anticipated event, as SPC's Day 3 Outlook (issued on the 27th) already introduced an Enhanced Risk of severe weather (level 3 of 5) for far southeast portions of South Central Nebraska. Then, on the morning of the 29th, roughly the southeast quadrant of the area was upgraded to Moderate Risk (level 4 of 5). A wind gust of 66 MPH was measured by a mesonet station located three miles south of Ohiowa.", "ts_dict_index": [7806, 7807, 7808]}
+{"event_id": 1026873, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-05-12 17:35:00", "end_date_time": "2022-05-12 17:35:00", "narrative": "Major severe weather event unfolds across south central Nebraska during the afternoon and evening of May 12th, including wind gusts of 80 to 90 MPH. The most significant severe weather event of May 2022 occurred on a Thursday in which multiple rounds of thunderstorms wreaked havoc on essentially all of south central Nebraska at some point. The most intense severe weather, by far, was the first round. This activity actually developed over portions of west/southwest Kansas during the morning hours and moved northeast. Rapid intensification took place between 1PM and 2PM CDT as thunderstorms organized into a long line, and the first Severe Thunderstorm Warnings were issued for areas from Phillipsburg, KS to Lexington, NE. Initial storm reports ranged from quarter to ping pong ball size hail with the southern portion of the line, to widespread damaging wind gusts with the northern portion of the line across a large portion of Dawson County. Wind damage consisted of overturned pivots, uprooted trees, broken power poles, fence and roof damage, large tree limbs downed. Wind damage was widespread over central and western Dawson County where measured wind gusts of 60-70 MPH were common. Even an 82 MPH gust, which is considered ���significant severe���, was measured by a mesonet near Eddyville. Surface temperatures near 90 degrees and mixed layer CAPE values in excess of 3000 J/kg ahead of the line of thunderstorms, amidst 35kt to 50kt of southwesterly deep layer shear, allowed for continued intensification through the mid to late afternoon as the line raced northeast. Additional significant damaging wind impacts were felt across Sherman, Valley, and Greeley Counties. Valley County was another area especially hard hit. Here, several wind gusts in the 80-90 MPH range were reported, and damage was significant. Numerous trees were uprooted, pivots overturned, and outbuildings and grain bins destroyed. Another destructive aspect of this storm is that it also produced ping pong ball sized hail that was blown by the intense winds. This resulted in significant window and body damage to cars, as well as roof, siding, and window damage to homes. Additional significant wind damage was reported in and around Burwell (just barely outside this coverage area). The first round of thunderstorms exited north/northeast of the area around 3:30PM CDT, but the next round was ���hot on its heels���, and entered southern Nebraska around 4PM CDT, and quickly became severe. In fact, brief, but intense, circulations were noted on radar for a time just south and southeast of Hastings. This round affected mainly areas along and east of Highway 281. Since this region was spared from the first round, and a similar thermodynamic and kinematic environment was still in place, it���s no surprise that this round also intensified enough to produce ���significant severe��� wind gusts, most notably in a swath from Clay County northeast to Polk County. Several more 60-70 MPH wind gusts were reported in these areas, causing more overturned pivots, downed power lines, and damage to roofs, outbuildings, and grain bins. Also, intense wind gusts moved over Interstate 80 in Hamilton County, causing multiple overturned semis. This second round exited into eastern Nebraska and out of the Hastings CWA around 7PM CDT. The third and final round began to affect areas along and east Highway 183 between 7PM and 8PM CDT. The majority of this activity remained sub-severe as the greatest instability had been used up by the two previous rounds. However, a marginally severe wind gust of 59 MPH was measured at the Hastings airport shortly before 8PM. Thereafter, weakening ensued as the line became strung out and forward propagation slowed. Thunderstorms finally exited south central Nebraska between 11PM and midnight, ending a roughly 10 hour stretch of seemingly never ending severe weather!||Meteorologically speaking, this event was driven by a particularly volatile combination of intensifying shortwave ejecting from the central Rockies into the northern Plains, very unstable airmass (MUCAPE of 3000-4000 J/kg at it���s peak), and strong deep layer shear driven by 500 mb speed max of 60-70 kt. While this setup is not unheard of for mid-May, it���s certainly not very common, and for three distinct waves of thunderstorms to move through in a 10 hour period (two of which contained significant severe weather phenomena) is also not very common. From a regional perspective, the Hastings CWA was the developing grounds for a significant derecho that would propagate into the Northern Plains and Upper Mississippi Valley and go on to produce hundreds of measured severe wind gusts and wind damage reports, of which over 60 were considered ���significant severe���. Over 75 hail reports and nearly three dozen tornado reports were also reported, with the majority of tornadoes occurring in SD and MN. For 2022, this will likely be remembered as one of the most severe convective events of the year, both locally, and across the greater region. A wind gust of 58 MPH was measured by a mesonet station located three miles northwest of Geneva.", "ts_dict_index": [7872, 7873, 7874]}
+{"event_id": 1026833, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-05-12 15:47:00", "end_date_time": "2022-05-12 15:50:00", "narrative": "Major severe weather event unfolds across south central Nebraska during the afternoon and evening of May 12th, including wind gusts of 80 to 90 MPH. The most significant severe weather event of May 2022 occurred on a Thursday in which multiple rounds of thunderstorms wreaked havoc on essentially all of south central Nebraska at some point. The most intense severe weather, by far, was the first round. This activity actually developed over portions of west/southwest Kansas during the morning hours and moved northeast. Rapid intensification took place between 1PM and 2PM CDT as thunderstorms organized into a long line, and the first Severe Thunderstorm Warnings were issued for areas from Phillipsburg, KS to Lexington, NE. Initial storm reports ranged from quarter to ping pong ball size hail with the southern portion of the line, to widespread damaging wind gusts with the northern portion of the line across a large portion of Dawson County. Wind damage consisted of overturned pivots, uprooted trees, broken power poles, fence and roof damage, large tree limbs downed. Wind damage was widespread over central and western Dawson County where measured wind gusts of 60-70 MPH were common. Even an 82 MPH gust, which is considered ���significant severe���, was measured by a mesonet near Eddyville. Surface temperatures near 90 degrees and mixed layer CAPE values in excess of 3000 J/kg ahead of the line of thunderstorms, amidst 35kt to 50kt of southwesterly deep layer shear, allowed for continued intensification through the mid to late afternoon as the line raced northeast. Additional significant damaging wind impacts were felt across Sherman, Valley, and Greeley Counties. Valley County was another area especially hard hit. Here, several wind gusts in the 80-90 MPH range were reported, and damage was significant. Numerous trees were uprooted, pivots overturned, and outbuildings and grain bins destroyed. Another destructive aspect of this storm is that it also produced ping pong ball sized hail that was blown by the intense winds. This resulted in significant window and body damage to cars, as well as roof, siding, and window damage to homes. Additional significant wind damage was reported in and around Burwell (just barely outside this coverage area). The first round of thunderstorms exited north/northeast of the area around 3:30PM CDT, but the next round was ���hot on its heels���, and entered southern Nebraska around 4PM CDT, and quickly became severe. In fact, brief, but intense, circulations were noted on radar for a time just south and southeast of Hastings. This round affected mainly areas along and east of Highway 281. Since this region was spared from the first round, and a similar thermodynamic and kinematic environment was still in place, it���s no surprise that this round also intensified enough to produce ���significant severe��� wind gusts, most notably in a swath from Clay County northeast to Polk County. Several more 60-70 MPH wind gusts were reported in these areas, causing more overturned pivots, downed power lines, and damage to roofs, outbuildings, and grain bins. Also, intense wind gusts moved over Interstate 80 in Hamilton County, causing multiple overturned semis. This second round exited into eastern Nebraska and out of the Hastings CWA around 7PM CDT. The third and final round began to affect areas along and east Highway 183 between 7PM and 8PM CDT. The majority of this activity remained sub-severe as the greatest instability had been used up by the two previous rounds. However, a marginally severe wind gust of 59 MPH was measured at the Hastings airport shortly before 8PM. Thereafter, weakening ensued as the line became strung out and forward propagation slowed. Thunderstorms finally exited south central Nebraska between 11PM and midnight, ending a roughly 10 hour stretch of seemingly never ending severe weather!||Meteorologically speaking, this event was driven by a particularly volatile combination of intensifying shortwave ejecting from the central Rockies into the northern Plains, very unstable airmass (MUCAPE of 3000-4000 J/kg at it���s peak), and strong deep layer shear driven by 500 mb speed max of 60-70 kt. While this setup is not unheard of for mid-May, it���s certainly not very common, and for three distinct waves of thunderstorms to move through in a 10 hour period (two of which contained significant severe weather phenomena) is also not very common. From a regional perspective, the Hastings CWA was the developing grounds for a significant derecho that would propagate into the Northern Plains and Upper Mississippi Valley and go on to produce hundreds of measured severe wind gusts and wind damage reports, of which over 60 were considered ���significant severe���. Over 75 hail reports and nearly three dozen tornado reports were also reported, with the majority of tornadoes occurring in SD and MN. For 2022, this will likely be remembered as one of the most severe convective events of the year, both locally, and across the greater region. A wind gust of 66 MPH was measured by a mesonet station located three miles east-southeast of Fairfield. A gust of 59 MPH was measured by a mesonet station located four miles north-northwest of Edgar.", "ts_dict_index": [7878, 7879, 7880]}
+{"event_id": 1026844, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-05-12 15:50:00", "end_date_time": "2022-05-12 15:57:00", "narrative": "Major severe weather event unfolds across south central Nebraska during the afternoon and evening of May 12th, including wind gusts of 80 to 90 MPH. The most significant severe weather event of May 2022 occurred on a Thursday in which multiple rounds of thunderstorms wreaked havoc on essentially all of south central Nebraska at some point. The most intense severe weather, by far, was the first round. This activity actually developed over portions of west/southwest Kansas during the morning hours and moved northeast. Rapid intensification took place between 1PM and 2PM CDT as thunderstorms organized into a long line, and the first Severe Thunderstorm Warnings were issued for areas from Phillipsburg, KS to Lexington, NE. Initial storm reports ranged from quarter to ping pong ball size hail with the southern portion of the line, to widespread damaging wind gusts with the northern portion of the line across a large portion of Dawson County. Wind damage consisted of overturned pivots, uprooted trees, broken power poles, fence and roof damage, large tree limbs downed. Wind damage was widespread over central and western Dawson County where measured wind gusts of 60-70 MPH were common. Even an 82 MPH gust, which is considered ���significant severe���, was measured by a mesonet near Eddyville. Surface temperatures near 90 degrees and mixed layer CAPE values in excess of 3000 J/kg ahead of the line of thunderstorms, amidst 35kt to 50kt of southwesterly deep layer shear, allowed for continued intensification through the mid to late afternoon as the line raced northeast. Additional significant damaging wind impacts were felt across Sherman, Valley, and Greeley Counties. Valley County was another area especially hard hit. Here, several wind gusts in the 80-90 MPH range were reported, and damage was significant. Numerous trees were uprooted, pivots overturned, and outbuildings and grain bins destroyed. Another destructive aspect of this storm is that it also produced ping pong ball sized hail that was blown by the intense winds. This resulted in significant window and body damage to cars, as well as roof, siding, and window damage to homes. Additional significant wind damage was reported in and around Burwell (just barely outside this coverage area). The first round of thunderstorms exited north/northeast of the area around 3:30PM CDT, but the next round was ���hot on its heels���, and entered southern Nebraska around 4PM CDT, and quickly became severe. In fact, brief, but intense, circulations were noted on radar for a time just south and southeast of Hastings. This round affected mainly areas along and east of Highway 281. Since this region was spared from the first round, and a similar thermodynamic and kinematic environment was still in place, it���s no surprise that this round also intensified enough to produce ���significant severe��� wind gusts, most notably in a swath from Clay County northeast to Polk County. Several more 60-70 MPH wind gusts were reported in these areas, causing more overturned pivots, downed power lines, and damage to roofs, outbuildings, and grain bins. Also, intense wind gusts moved over Interstate 80 in Hamilton County, causing multiple overturned semis. This second round exited into eastern Nebraska and out of the Hastings CWA around 7PM CDT. The third and final round began to affect areas along and east Highway 183 between 7PM and 8PM CDT. The majority of this activity remained sub-severe as the greatest instability had been used up by the two previous rounds. However, a marginally severe wind gust of 59 MPH was measured at the Hastings airport shortly before 8PM. Thereafter, weakening ensued as the line became strung out and forward propagation slowed. Thunderstorms finally exited south central Nebraska between 11PM and midnight, ending a roughly 10 hour stretch of seemingly never ending severe weather!||Meteorologically speaking, this event was driven by a particularly volatile combination of intensifying shortwave ejecting from the central Rockies into the northern Plains, very unstable airmass (MUCAPE of 3000-4000 J/kg at it���s peak), and strong deep layer shear driven by 500 mb speed max of 60-70 kt. While this setup is not unheard of for mid-May, it���s certainly not very common, and for three distinct waves of thunderstorms to move through in a 10 hour period (two of which contained significant severe weather phenomena) is also not very common. From a regional perspective, the Hastings CWA was the developing grounds for a significant derecho that would propagate into the Northern Plains and Upper Mississippi Valley and go on to produce hundreds of measured severe wind gusts and wind damage reports, of which over 60 were considered ���significant severe���. Over 75 hail reports and nearly three dozen tornado reports were also reported, with the majority of tornadoes occurring in SD and MN. For 2022, this will likely be remembered as one of the most severe convective events of the year, both locally, and across the greater region. A wind gust of 74 MPH was measured by a mesonet station located two miles southeast of Harvard. A wind gust of 59 MPH was measured by a Nebraska Mesonet station located four miles southwest of Harvard. A NWS Cooperative Observer reported that a semi-truck was blown over on Highway 6 just west of the Highway 14 intersection north of Clay Center and a car was blown off of Highway 6 near Road T near Saronville.", "ts_dict_index": [7881, 7882, 7883]}
+{"event_id": 1026875, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-05-12 18:48:00", "end_date_time": "2022-05-12 18:48:00", "narrative": "Major severe weather event unfolds across south central Nebraska during the afternoon and evening of May 12th, including wind gusts of 80 to 90 MPH. The most significant severe weather event of May 2022 occurred on a Thursday in which multiple rounds of thunderstorms wreaked havoc on essentially all of south central Nebraska at some point. The most intense severe weather, by far, was the first round. This activity actually developed over portions of west/southwest Kansas during the morning hours and moved northeast. Rapid intensification took place between 1PM and 2PM CDT as thunderstorms organized into a long line, and the first Severe Thunderstorm Warnings were issued for areas from Phillipsburg, KS to Lexington, NE. Initial storm reports ranged from quarter to ping pong ball size hail with the southern portion of the line, to widespread damaging wind gusts with the northern portion of the line across a large portion of Dawson County. Wind damage consisted of overturned pivots, uprooted trees, broken power poles, fence and roof damage, large tree limbs downed. Wind damage was widespread over central and western Dawson County where measured wind gusts of 60-70 MPH were common. Even an 82 MPH gust, which is considered ���significant severe���, was measured by a mesonet near Eddyville. Surface temperatures near 90 degrees and mixed layer CAPE values in excess of 3000 J/kg ahead of the line of thunderstorms, amidst 35kt to 50kt of southwesterly deep layer shear, allowed for continued intensification through the mid to late afternoon as the line raced northeast. Additional significant damaging wind impacts were felt across Sherman, Valley, and Greeley Counties. Valley County was another area especially hard hit. Here, several wind gusts in the 80-90 MPH range were reported, and damage was significant. Numerous trees were uprooted, pivots overturned, and outbuildings and grain bins destroyed. Another destructive aspect of this storm is that it also produced ping pong ball sized hail that was blown by the intense winds. This resulted in significant window and body damage to cars, as well as roof, siding, and window damage to homes. Additional significant wind damage was reported in and around Burwell (just barely outside this coverage area). The first round of thunderstorms exited north/northeast of the area around 3:30PM CDT, but the next round was ���hot on its heels���, and entered southern Nebraska around 4PM CDT, and quickly became severe. In fact, brief, but intense, circulations were noted on radar for a time just south and southeast of Hastings. This round affected mainly areas along and east of Highway 281. Since this region was spared from the first round, and a similar thermodynamic and kinematic environment was still in place, it���s no surprise that this round also intensified enough to produce ���significant severe��� wind gusts, most notably in a swath from Clay County northeast to Polk County. Several more 60-70 MPH wind gusts were reported in these areas, causing more overturned pivots, downed power lines, and damage to roofs, outbuildings, and grain bins. Also, intense wind gusts moved over Interstate 80 in Hamilton County, causing multiple overturned semis. This second round exited into eastern Nebraska and out of the Hastings CWA around 7PM CDT. The third and final round began to affect areas along and east Highway 183 between 7PM and 8PM CDT. The majority of this activity remained sub-severe as the greatest instability had been used up by the two previous rounds. However, a marginally severe wind gust of 59 MPH was measured at the Hastings airport shortly before 8PM. Thereafter, weakening ensued as the line became strung out and forward propagation slowed. Thunderstorms finally exited south central Nebraska between 11PM and midnight, ending a roughly 10 hour stretch of seemingly never ending severe weather!||Meteorologically speaking, this event was driven by a particularly volatile combination of intensifying shortwave ejecting from the central Rockies into the northern Plains, very unstable airmass (MUCAPE of 3000-4000 J/kg at it���s peak), and strong deep layer shear driven by 500 mb speed max of 60-70 kt. While this setup is not unheard of for mid-May, it���s certainly not very common, and for three distinct waves of thunderstorms to move through in a 10 hour period (two of which contained significant severe weather phenomena) is also not very common. From a regional perspective, the Hastings CWA was the developing grounds for a significant derecho that would propagate into the Northern Plains and Upper Mississippi Valley and go on to produce hundreds of measured severe wind gusts and wind damage reports, of which over 60 were considered ���significant severe���. Over 75 hail reports and nearly three dozen tornado reports were also reported, with the majority of tornadoes occurring in SD and MN. For 2022, this will likely be remembered as one of the most severe convective events of the year, both locally, and across the greater region. A wind gust of 59 MPH was measured by the Hastings Airport ASOS.", "ts_dict_index": [7875, 7876, 7877]}
+{"event_id": 1026840, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-05-12 15:49:00", "end_date_time": "2022-05-12 15:49:00", "narrative": "Major severe weather event unfolds across south central Nebraska during the afternoon and evening of May 12th, including wind gusts of 80 to 90 MPH. The most significant severe weather event of May 2022 occurred on a Thursday in which multiple rounds of thunderstorms wreaked havoc on essentially all of south central Nebraska at some point. The most intense severe weather, by far, was the first round. This activity actually developed over portions of west/southwest Kansas during the morning hours and moved northeast. Rapid intensification took place between 1PM and 2PM CDT as thunderstorms organized into a long line, and the first Severe Thunderstorm Warnings were issued for areas from Phillipsburg, KS to Lexington, NE. Initial storm reports ranged from quarter to ping pong ball size hail with the southern portion of the line, to widespread damaging wind gusts with the northern portion of the line across a large portion of Dawson County. Wind damage consisted of overturned pivots, uprooted trees, broken power poles, fence and roof damage, large tree limbs downed. Wind damage was widespread over central and western Dawson County where measured wind gusts of 60-70 MPH were common. Even an 82 MPH gust, which is considered ���significant severe���, was measured by a mesonet near Eddyville. Surface temperatures near 90 degrees and mixed layer CAPE values in excess of 3000 J/kg ahead of the line of thunderstorms, amidst 35kt to 50kt of southwesterly deep layer shear, allowed for continued intensification through the mid to late afternoon as the line raced northeast. Additional significant damaging wind impacts were felt across Sherman, Valley, and Greeley Counties. Valley County was another area especially hard hit. Here, several wind gusts in the 80-90 MPH range were reported, and damage was significant. Numerous trees were uprooted, pivots overturned, and outbuildings and grain bins destroyed. Another destructive aspect of this storm is that it also produced ping pong ball sized hail that was blown by the intense winds. This resulted in significant window and body damage to cars, as well as roof, siding, and window damage to homes. Additional significant wind damage was reported in and around Burwell (just barely outside this coverage area). The first round of thunderstorms exited north/northeast of the area around 3:30PM CDT, but the next round was ���hot on its heels���, and entered southern Nebraska around 4PM CDT, and quickly became severe. In fact, brief, but intense, circulations were noted on radar for a time just south and southeast of Hastings. This round affected mainly areas along and east of Highway 281. Since this region was spared from the first round, and a similar thermodynamic and kinematic environment was still in place, it���s no surprise that this round also intensified enough to produce ���significant severe��� wind gusts, most notably in a swath from Clay County northeast to Polk County. Several more 60-70 MPH wind gusts were reported in these areas, causing more overturned pivots, downed power lines, and damage to roofs, outbuildings, and grain bins. Also, intense wind gusts moved over Interstate 80 in Hamilton County, causing multiple overturned semis. This second round exited into eastern Nebraska and out of the Hastings CWA around 7PM CDT. The third and final round began to affect areas along and east Highway 183 between 7PM and 8PM CDT. The majority of this activity remained sub-severe as the greatest instability had been used up by the two previous rounds. However, a marginally severe wind gust of 59 MPH was measured at the Hastings airport shortly before 8PM. Thereafter, weakening ensued as the line became strung out and forward propagation slowed. Thunderstorms finally exited south central Nebraska between 11PM and midnight, ending a roughly 10 hour stretch of seemingly never ending severe weather!||Meteorologically speaking, this event was driven by a particularly volatile combination of intensifying shortwave ejecting from the central Rockies into the northern Plains, very unstable airmass (MUCAPE of 3000-4000 J/kg at it���s peak), and strong deep layer shear driven by 500 mb speed max of 60-70 kt. While this setup is not unheard of for mid-May, it���s certainly not very common, and for three distinct waves of thunderstorms to move through in a 10 hour period (two of which contained significant severe weather phenomena) is also not very common. From a regional perspective, the Hastings CWA was the developing grounds for a significant derecho that would propagate into the Northern Plains and Upper Mississippi Valley and go on to produce hundreds of measured severe wind gusts and wind damage reports, of which over 60 were considered ���significant severe���. Over 75 hail reports and nearly three dozen tornado reports were also reported, with the majority of tornadoes occurring in SD and MN. For 2022, this will likely be remembered as one of the most severe convective events of the year, both locally, and across the greater region. A wind gust of 70 MPH was measured by a mesonet station located three miles west of Edgar.", "ts_dict_index": [7869, 7870, 7871]}
+{"event_id": 849564, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-08-07 02:38:00", "end_date_time": "2019-08-07 02:38:00", "narrative": "Although its main damage swath was only about 15 miles wide, the narrow-but-intense severe storm complex that raced from northwest-to-southeast through the heart of South Central Nebraska during the pre-dawn hours on this Wednesday was one of the most impactful events of the local convective season. Quite simply, this was a nasty wind storm, packing a punch with gusts ranging from around 60 to nearly 90 MPH along and several miles either side of a line stretching from Ord-Grand Island-Hastings-Hardy. For the city of Grand Island, this was likely the overall-worst wind storm in several years, as the airport ASOS clocked a peak gust of 87 MPH. Countless trees/large branches were blown down within the city, along with several power lines, and there was also some (mainly) minor structural damage. Grand Island Emergency Center logged nearly 300 storm related incidents, including traffic hazards, power outages, alarms and fire concerns from sparking electricity. The storm also caused an (indirect) traffic fatality in rural Hall County southeast of Cairo, when a man crashed his pickup into a large, downed tree arched across a paved county road. To the south in Hastings, damage was less-severe overall, as the ASOS peak gust on the west side of town was only 70 MPH. However, stronger winds likely impacted areas just east of the city, as large trees were uprooted at Central Community College and several rail cars were reportedly blown over at a repair facility near the Clay County line. Several smaller communities also reported notable wind damage, including: Cairo, Alda, Wood River, Doniphan, Glenvil, and Fairfield. West of Clay Center, fairly extensive damage occurred on the U.S. Meat Animal Research Center campus, including broken windows and roof damage to several buildings. In addition to the aforementioned peak wind gusts at Grand Island/Hastings airports, some of the more notable unofficial (mesonet) gusts included: 85 MPH near Fairfield, 80 MPH near Alda and Wood River, 79 MPH in Doniphan and 73 MPH near Nelson. Despite the multitude of damaging wind reports, hail reports were quite scarce, as the vast majority of stones were likely dime size or smaller. Rainfall-wise, a fairly widespread coverage of 2-3 soaked several northern counties including: Valley, Greeley, Sherman, Nance and Merrick. Although resultant flooding was not very extensive in most of the area, the Mira Creek in southern Valley County breached its banks for the second time in five days, again prompting minor flooding on the north side of North Loup that continued into the early morning of the 8th.||Breaking down the timing and meteorological background of this event, it's worth noting that these South Central Nebraska damaging winds were actually the finale to a much longer swath of severe weather that initiated in southern ND and north central SD during the afternoon/evening of the 6th. Between 1-2 a.m. CDT on the 7th, the leading edge of this narrow-but-potent mesoscale convective system (MCS) entered far northern portions of the local area into Valley/Greeley counties, signaling its arrival with a 59 MPH gust at Ord airport. However, the worst was yet to come, as during the next few hours the storm complex morphed into more of an outflow-dominant, high-precipitation supercell, slamming through the Grand Island/Hastings areas between 2:30-3:30 a.m. CDT before eventually exiting Nuckolls/Thayer counties into Kansas by 5 a.m. CDT. In the wake of the main show, a few weaker clusters of storms redeveloped over parts of the area into the daylight hours, but were of little significance. In the big picture of the mid-upper levels, this event occurred within a fairly classic summertime northwest-flow regime, as the Central Plains resided northeast of an expansive ridge centered over New Mexico. At the surface, South Central Nebraska was on the backside of a weak ridge axis centered near the Nebraska-Iowa border. This promoted light-but-steady, south-southeast breezes in advance of the approaching storm complex, with surface dewpoints averaging mid-upper 60s F. Although there were question marks about how far southward into Nebraska the potential severe weather threat would extend, the combination of seasonably-stout flow aloft (deep-layer wind shear of at least 40-60 knots) and sufficient instability (mixed-layer CAPE of 1000-2000 J/kg) was clearly supportive of an intense late-night storm. Also enhancing the severe weather environment was a modest, 30 knot  southwesterly low level jet (evident at 850 millibars) and its associated low-level warm air/moisture advection. A 67 MPH wind gust was measured by a mesonet station located 3 miles west of Edgar.", "ts_dict_index": [7902, 7903, 7904]}
+{"event_id": 1045509, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-07-16 20:49:00", "end_date_time": "2022-07-16 20:49:00", "narrative": "Several strong to severe thunderstorms, some that eventually merged into a compact mesoscale convective system (MCS), rumbled southeastward across various parts of South Central Nebraska mainly between 6:30-11:30 p.m. CDT on this Saturday evening, prompting assorted reports of large hail (up to baseball size) and damaging winds (estimated up to 80 MPH) and disrupting activities at a handful of local county fairs. The most prominent narrow swath of severe activity cut through the heart of the 24-county area, focusing within 10 miles either side of a line extending from Ord-Cairo-Hastings-Davenport as an initially isolated supercell merged with a separate cluster of severe storms to its west, forming the aforementioned MCS. During it's more supercellular phase near/north of the Highway 92 corridor (mainly 6:30-8:30 p.m. CDT), a combo of both damaging winds and large hail occurred, featuring measured gusts as high as 74 MPH at Ord airport and hail ranging from golf ball to baseball size particularly within western Howard and far northwestern Hall counties. In Howard County, a stripe of significant damage to crops and windows/siding was noted from around Farwell to west of Dannebrog. As this MCS reached areas near/south of Interstate 80 (primarily 9-11 p.m. CDT) the hail threat waned but damaging winds continued, evidenced by a measured 58 MPH gust at Hastings airport and unofficial mesonet-measured gusts of 67 MPH near Nelson and 62 MPH near Davenport. Within Clay County, tree branches were downed in several communities including Trumbull, Deweese, Fairfield and Edgar. Shortly before this storm complex exited the local area to the southeast between 11:00-11:30 p.m. CDT, wind intensity ramped down to slightly sub-severe levels within southern/eastern Thayer County. Although far from the only outdoor event interruption of the evening within South Central Nebraska, one of the more noteworthy ones associated with this MCS involved the Adams County Fairfest in Hastings, where an ongoing Nelly concert was cut short and an evacuation of the grounds was successfully initiated shortly before the storm struck. Although rain totals of 1-2 inches were common within the heart of the MCS track (overall highest inF Clay County), any flooding was of the very short term/nuisance variety. To the west of the aforementioned primary swath of severe weather, a few separate and smaller-scale areas of strong to severe storms impacted portions of primarily Furnas, Buffalo and Dawson counties mainly between 7-9 p.m. CDT. In Furnas County, a relatively small but intense supercell roamed northern and eastern parts of the county, with estimated 80 MPH winds destroying an outbuilding and grain bin at a farmstead between Holbrook and Arapahoe. Meanwhile, other semi-discrete convection within parts of Buffalo/Dawson counties yielded a few wind reports including a mesonet-measured 64 MPH gust near Kearney and a slightly sub-severe 54 MPH speed near Lexington. The eastern reaches of this activity eventually merged with the primary MCS as it charged across the I-80 corridor and into the Hastings area. ||Finishing with some details regarding the evolution and meteorology behind this event, the initial development of isolated to scattered thunderstorms during the mid-late afternoon hours occurred in separate areas slightly off to  the north and also west of South Central Nebraska, with this early activity gradually increasing in both coverage/intensity as it evolved into the local area. In the mid-upper levels, forcing was fairly weak, featuring only subtle shortwave energy working into the region in west-northwest flow, directed around the northeastern periphery of a large-scale ridge centered over the Four Corners region. At the surface, there were also no significant features of note locally, with most of South Central Nebraska simply reporting 5-15 MPH east-southeasterly breezes during the afternoon. However, the initial storm development off to the north and west of the area appeared to be tied to weak convergence along a pair of subtle boundaries. Despite the aforementioned weak forcing and also weak mid level lapse rates, the environment featured plentiful low level moisture/instability and seasonably-decent deep layer wind shear of 30-40 knots. Ahead of the incoming storms, late afternoon temperatures in the upper 80s-low 90s (F) and dewpoints in the upper 60s-mid 70s promoted mixed-layer CAPE 2000-3000 J/kg. Some tree branches were downed in Fairfield, with power outages also reported.", "ts_dict_index": [7920, 7921, 7922]}
+{"event_id": 845298, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-08-07 02:09:00", "end_date_time": "2019-08-07 02:09:00", "narrative": "Although its main damage swath was only about 15 miles wide, the narrow-but-intense severe storm complex that raced from northwest-to-southeast through the heart of South Central Nebraska during the pre-dawn hours on this Wednesday was one of the most impactful events of the local convective season. Quite simply, this was a nasty wind storm, packing a punch with gusts ranging from around 60 to nearly 90 MPH along and several miles either side of a line stretching from Ord-Grand Island-Hastings-Hardy. For the city of Grand Island, this was likely the overall-worst wind storm in several years, as the airport ASOS clocked a peak gust of 87 MPH. Countless trees/large branches were blown down within the city, along with several power lines, and there was also some (mainly) minor structural damage. Grand Island Emergency Center logged nearly 300 storm related incidents, including traffic hazards, power outages, alarms and fire concerns from sparking electricity. The storm also caused an (indirect) traffic fatality in rural Hall County southeast of Cairo, when a man crashed his pickup into a large, downed tree arched across a paved county road. To the south in Hastings, damage was less-severe overall, as the ASOS peak gust on the west side of town was only 70 MPH. However, stronger winds likely impacted areas just east of the city, as large trees were uprooted at Central Community College and several rail cars were reportedly blown over at a repair facility near the Clay County line. Several smaller communities also reported notable wind damage, including: Cairo, Alda, Wood River, Doniphan, Glenvil, and Fairfield. West of Clay Center, fairly extensive damage occurred on the U.S. Meat Animal Research Center campus, including broken windows and roof damage to several buildings. In addition to the aforementioned peak wind gusts at Grand Island/Hastings airports, some of the more notable unofficial (mesonet) gusts included: 85 MPH near Fairfield, 80 MPH near Alda and Wood River, 79 MPH in Doniphan and 73 MPH near Nelson. Despite the multitude of damaging wind reports, hail reports were quite scarce, as the vast majority of stones were likely dime size or smaller. Rainfall-wise, a fairly widespread coverage of 2-3 soaked several northern counties including: Valley, Greeley, Sherman, Nance and Merrick. Although resultant flooding was not very extensive in most of the area, the Mira Creek in southern Valley County breached its banks for the second time in five days, again prompting minor flooding on the north side of North Loup that continued into the early morning of the 8th.||Breaking down the timing and meteorological background of this event, it's worth noting that these South Central Nebraska damaging winds were actually the finale to a much longer swath of severe weather that initiated in southern ND and north central SD during the afternoon/evening of the 6th. Between 1-2 a.m. CDT on the 7th, the leading edge of this narrow-but-potent mesoscale convective system (MCS) entered far northern portions of the local area into Valley/Greeley counties, signaling its arrival with a 59 MPH gust at Ord airport. However, the worst was yet to come, as during the next few hours the storm complex morphed into more of an outflow-dominant, high-precipitation supercell, slamming through the Grand Island/Hastings areas between 2:30-3:30 a.m. CDT before eventually exiting Nuckolls/Thayer counties into Kansas by 5 a.m. CDT. In the wake of the main show, a few weaker clusters of storms redeveloped over parts of the area into the daylight hours, but were of little significance. In the big picture of the mid-upper levels, this event occurred within a fairly classic summertime northwest-flow regime, as the Central Plains resided northeast of an expansive ridge centered over New Mexico. At the surface, South Central Nebraska was on the backside of a weak ridge axis centered near the Nebraska-Iowa border. This promoted light-but-steady, south-southeast breezes in advance of the approaching storm complex, with surface dewpoints averaging mid-upper 60s F. Although there were question marks about how far southward into Nebraska the potential severe weather threat would extend, the combination of seasonably-stout flow aloft (deep-layer wind shear of at least 40-60 knots) and sufficient instability (mixed-layer CAPE of 1000-2000 J/kg) was clearly supportive of an intense late-night storm. Also enhancing the severe weather environment was a modest, 30 knot  southwesterly low level jet (evident at 850 millibars) and its associated low-level warm air/moisture advection. A 60 MPH wind gust was measured by a mesonet station located 3 miles northwest of Inland.", "ts_dict_index": [7914, 7915, 7916]}
+{"event_id": 1045512, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-07-16 21:01:00", "end_date_time": "2022-07-16 21:01:00", "narrative": "Several strong to severe thunderstorms, some that eventually merged into a compact mesoscale convective system (MCS), rumbled southeastward across various parts of South Central Nebraska mainly between 6:30-11:30 p.m. CDT on this Saturday evening, prompting assorted reports of large hail (up to baseball size) and damaging winds (estimated up to 80 MPH) and disrupting activities at a handful of local county fairs. The most prominent narrow swath of severe activity cut through the heart of the 24-county area, focusing within 10 miles either side of a line extending from Ord-Cairo-Hastings-Davenport as an initially isolated supercell merged with a separate cluster of severe storms to its west, forming the aforementioned MCS. During it's more supercellular phase near/north of the Highway 92 corridor (mainly 6:30-8:30 p.m. CDT), a combo of both damaging winds and large hail occurred, featuring measured gusts as high as 74 MPH at Ord airport and hail ranging from golf ball to baseball size particularly within western Howard and far northwestern Hall counties. In Howard County, a stripe of significant damage to crops and windows/siding was noted from around Farwell to west of Dannebrog. As this MCS reached areas near/south of Interstate 80 (primarily 9-11 p.m. CDT) the hail threat waned but damaging winds continued, evidenced by a measured 58 MPH gust at Hastings airport and unofficial mesonet-measured gusts of 67 MPH near Nelson and 62 MPH near Davenport. Within Clay County, tree branches were downed in several communities including Trumbull, Deweese, Fairfield and Edgar. Shortly before this storm complex exited the local area to the southeast between 11:00-11:30 p.m. CDT, wind intensity ramped down to slightly sub-severe levels within southern/eastern Thayer County. Although far from the only outdoor event interruption of the evening within South Central Nebraska, one of the more noteworthy ones associated with this MCS involved the Adams County Fairfest in Hastings, where an ongoing Nelly concert was cut short and an evacuation of the grounds was successfully initiated shortly before the storm struck. Although rain totals of 1-2 inches were common within the heart of the MCS track (overall highest inF Clay County), any flooding was of the very short term/nuisance variety. To the west of the aforementioned primary swath of severe weather, a few separate and smaller-scale areas of strong to severe storms impacted portions of primarily Furnas, Buffalo and Dawson counties mainly between 7-9 p.m. CDT. In Furnas County, a relatively small but intense supercell roamed northern and eastern parts of the county, with estimated 80 MPH winds destroying an outbuilding and grain bin at a farmstead between Holbrook and Arapahoe. Meanwhile, other semi-discrete convection within parts of Buffalo/Dawson counties yielded a few wind reports including a mesonet-measured 64 MPH gust near Kearney and a slightly sub-severe 54 MPH speed near Lexington. The eastern reaches of this activity eventually merged with the primary MCS as it charged across the I-80 corridor and into the Hastings area. ||Finishing with some details regarding the evolution and meteorology behind this event, the initial development of isolated to scattered thunderstorms during the mid-late afternoon hours occurred in separate areas slightly off to  the north and also west of South Central Nebraska, with this early activity gradually increasing in both coverage/intensity as it evolved into the local area. In the mid-upper levels, forcing was fairly weak, featuring only subtle shortwave energy working into the region in west-northwest flow, directed around the northeastern periphery of a large-scale ridge centered over the Four Corners region. At the surface, there were also no significant features of note locally, with most of South Central Nebraska simply reporting 5-15 MPH east-southeasterly breezes during the afternoon. However, the initial storm development off to the north and west of the area appeared to be tied to weak convergence along a pair of subtle boundaries. Despite the aforementioned weak forcing and also weak mid level lapse rates, the environment featured plentiful low level moisture/instability and seasonably-decent deep layer wind shear of 30-40 knots. Ahead of the incoming storms, late afternoon temperatures in the upper 80s-low 90s (F) and dewpoints in the upper 60s-mid 70s promoted mixed-layer CAPE 2000-3000 J/kg. Some tree branches were downed in Edgar, with power outages also reported.", "ts_dict_index": [7923, 7924, 7925]}
+{"event_id": 1026841, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-05-12 15:50:00", "end_date_time": "2022-05-12 15:50:00", "narrative": "Major severe weather event unfolds across south central Nebraska during the afternoon and evening of May 12th, including wind gusts of 80 to 90 MPH. The most significant severe weather event of May 2022 occurred on a Thursday in which multiple rounds of thunderstorms wreaked havoc on essentially all of south central Nebraska at some point. The most intense severe weather, by far, was the first round. This activity actually developed over portions of west/southwest Kansas during the morning hours and moved northeast. Rapid intensification took place between 1PM and 2PM CDT as thunderstorms organized into a long line, and the first Severe Thunderstorm Warnings were issued for areas from Phillipsburg, KS to Lexington, NE. Initial storm reports ranged from quarter to ping pong ball size hail with the southern portion of the line, to widespread damaging wind gusts with the northern portion of the line across a large portion of Dawson County. Wind damage consisted of overturned pivots, uprooted trees, broken power poles, fence and roof damage, large tree limbs downed. Wind damage was widespread over central and western Dawson County where measured wind gusts of 60-70 MPH were common. Even an 82 MPH gust, which is considered ���significant severe���, was measured by a mesonet near Eddyville. Surface temperatures near 90 degrees and mixed layer CAPE values in excess of 3000 J/kg ahead of the line of thunderstorms, amidst 35kt to 50kt of southwesterly deep layer shear, allowed for continued intensification through the mid to late afternoon as the line raced northeast. Additional significant damaging wind impacts were felt across Sherman, Valley, and Greeley Counties. Valley County was another area especially hard hit. Here, several wind gusts in the 80-90 MPH range were reported, and damage was significant. Numerous trees were uprooted, pivots overturned, and outbuildings and grain bins destroyed. Another destructive aspect of this storm is that it also produced ping pong ball sized hail that was blown by the intense winds. This resulted in significant window and body damage to cars, as well as roof, siding, and window damage to homes. Additional significant wind damage was reported in and around Burwell (just barely outside this coverage area). The first round of thunderstorms exited north/northeast of the area around 3:30PM CDT, but the next round was ���hot on its heels���, and entered southern Nebraska around 4PM CDT, and quickly became severe. In fact, brief, but intense, circulations were noted on radar for a time just south and southeast of Hastings. This round affected mainly areas along and east of Highway 281. Since this region was spared from the first round, and a similar thermodynamic and kinematic environment was still in place, it���s no surprise that this round also intensified enough to produce ���significant severe��� wind gusts, most notably in a swath from Clay County northeast to Polk County. Several more 60-70 MPH wind gusts were reported in these areas, causing more overturned pivots, downed power lines, and damage to roofs, outbuildings, and grain bins. Also, intense wind gusts moved over Interstate 80 in Hamilton County, causing multiple overturned semis. This second round exited into eastern Nebraska and out of the Hastings CWA around 7PM CDT. The third and final round began to affect areas along and east Highway 183 between 7PM and 8PM CDT. The majority of this activity remained sub-severe as the greatest instability had been used up by the two previous rounds. However, a marginally severe wind gust of 59 MPH was measured at the Hastings airport shortly before 8PM. Thereafter, weakening ensued as the line became strung out and forward propagation slowed. Thunderstorms finally exited south central Nebraska between 11PM and midnight, ending a roughly 10 hour stretch of seemingly never ending severe weather!||Meteorologically speaking, this event was driven by a particularly volatile combination of intensifying shortwave ejecting from the central Rockies into the northern Plains, very unstable airmass (MUCAPE of 3000-4000 J/kg at it���s peak), and strong deep layer shear driven by 500 mb speed max of 60-70 kt. While this setup is not unheard of for mid-May, it���s certainly not very common, and for three distinct waves of thunderstorms to move through in a 10 hour period (two of which contained significant severe weather phenomena) is also not very common. From a regional perspective, the Hastings CWA was the developing grounds for a significant derecho that would propagate into the Northern Plains and Upper Mississippi Valley and go on to produce hundreds of measured severe wind gusts and wind damage reports, of which over 60 were considered ���significant severe���. Over 75 hail reports and nearly three dozen tornado reports were also reported, with the majority of tornadoes occurring in SD and MN. For 2022, this will likely be remembered as one of the most severe convective events of the year, both locally, and across the greater region. Wind gusts estimated to be near 70 MPH resulted in damage across Clay Center. Emergency management reported widespread tree damage and power outages across town and much of Clay County. A couple metal buildings in town sustained damage, including one at the grain elevator. A few power poles were also damaged.", "ts_dict_index": [7887, 7888, 7889]}
+{"event_id": 845296, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-08-07 02:10:00", "end_date_time": "2019-08-07 02:10:00", "narrative": "Although its main damage swath was only about 15 miles wide, the narrow-but-intense severe storm complex that raced from northwest-to-southeast through the heart of South Central Nebraska during the pre-dawn hours on this Wednesday was one of the most impactful events of the local convective season. Quite simply, this was a nasty wind storm, packing a punch with gusts ranging from around 60 to nearly 90 MPH along and several miles either side of a line stretching from Ord-Grand Island-Hastings-Hardy. For the city of Grand Island, this was likely the overall-worst wind storm in several years, as the airport ASOS clocked a peak gust of 87 MPH. Countless trees/large branches were blown down within the city, along with several power lines, and there was also some (mainly) minor structural damage. Grand Island Emergency Center logged nearly 300 storm related incidents, including traffic hazards, power outages, alarms and fire concerns from sparking electricity. The storm also caused an (indirect) traffic fatality in rural Hall County southeast of Cairo, when a man crashed his pickup into a large, downed tree arched across a paved county road. To the south in Hastings, damage was less-severe overall, as the ASOS peak gust on the west side of town was only 70 MPH. However, stronger winds likely impacted areas just east of the city, as large trees were uprooted at Central Community College and several rail cars were reportedly blown over at a repair facility near the Clay County line. Several smaller communities also reported notable wind damage, including: Cairo, Alda, Wood River, Doniphan, Glenvil, and Fairfield. West of Clay Center, fairly extensive damage occurred on the U.S. Meat Animal Research Center campus, including broken windows and roof damage to several buildings. In addition to the aforementioned peak wind gusts at Grand Island/Hastings airports, some of the more notable unofficial (mesonet) gusts included: 85 MPH near Fairfield, 80 MPH near Alda and Wood River, 79 MPH in Doniphan and 73 MPH near Nelson. Despite the multitude of damaging wind reports, hail reports were quite scarce, as the vast majority of stones were likely dime size or smaller. Rainfall-wise, a fairly widespread coverage of 2-3 soaked several northern counties including: Valley, Greeley, Sherman, Nance and Merrick. Although resultant flooding was not very extensive in most of the area, the Mira Creek in southern Valley County breached its banks for the second time in five days, again prompting minor flooding on the north side of North Loup that continued into the early morning of the 8th.||Breaking down the timing and meteorological background of this event, it's worth noting that these South Central Nebraska damaging winds were actually the finale to a much longer swath of severe weather that initiated in southern ND and north central SD during the afternoon/evening of the 6th. Between 1-2 a.m. CDT on the 7th, the leading edge of this narrow-but-potent mesoscale convective system (MCS) entered far northern portions of the local area into Valley/Greeley counties, signaling its arrival with a 59 MPH gust at Ord airport. However, the worst was yet to come, as during the next few hours the storm complex morphed into more of an outflow-dominant, high-precipitation supercell, slamming through the Grand Island/Hastings areas between 2:30-3:30 a.m. CDT before eventually exiting Nuckolls/Thayer counties into Kansas by 5 a.m. CDT. In the wake of the main show, a few weaker clusters of storms redeveloped over parts of the area into the daylight hours, but were of little significance. In the big picture of the mid-upper levels, this event occurred within a fairly classic summertime northwest-flow regime, as the Central Plains resided northeast of an expansive ridge centered over New Mexico. At the surface, South Central Nebraska was on the backside of a weak ridge axis centered near the Nebraska-Iowa border. This promoted light-but-steady, south-southeast breezes in advance of the approaching storm complex, with surface dewpoints averaging mid-upper 60s F. Although there were question marks about how far southward into Nebraska the potential severe weather threat would extend, the combination of seasonably-stout flow aloft (deep-layer wind shear of at least 40-60 knots) and sufficient instability (mixed-layer CAPE of 1000-2000 J/kg) was clearly supportive of an intense late-night storm. Also enhancing the severe weather environment was a modest, 30 knot  southwesterly low level jet (evident at 850 millibars) and its associated low-level warm air/moisture advection. Wind gusts estimated to be near 80 MPH resulted in a trailer home being flipped onto its side. It was not properly strapped down.", "ts_dict_index": [7893, 7894, 7895]}
+{"event_id": 1026835, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-05-12 15:48:00", "end_date_time": "2022-05-12 16:00:00", "narrative": "Major severe weather event unfolds across south central Nebraska during the afternoon and evening of May 12th, including wind gusts of 80 to 90 MPH. The most significant severe weather event of May 2022 occurred on a Thursday in which multiple rounds of thunderstorms wreaked havoc on essentially all of south central Nebraska at some point. The most intense severe weather, by far, was the first round. This activity actually developed over portions of west/southwest Kansas during the morning hours and moved northeast. Rapid intensification took place between 1PM and 2PM CDT as thunderstorms organized into a long line, and the first Severe Thunderstorm Warnings were issued for areas from Phillipsburg, KS to Lexington, NE. Initial storm reports ranged from quarter to ping pong ball size hail with the southern portion of the line, to widespread damaging wind gusts with the northern portion of the line across a large portion of Dawson County. Wind damage consisted of overturned pivots, uprooted trees, broken power poles, fence and roof damage, large tree limbs downed. Wind damage was widespread over central and western Dawson County where measured wind gusts of 60-70 MPH were common. Even an 82 MPH gust, which is considered ���significant severe���, was measured by a mesonet near Eddyville. Surface temperatures near 90 degrees and mixed layer CAPE values in excess of 3000 J/kg ahead of the line of thunderstorms, amidst 35kt to 50kt of southwesterly deep layer shear, allowed for continued intensification through the mid to late afternoon as the line raced northeast. Additional significant damaging wind impacts were felt across Sherman, Valley, and Greeley Counties. Valley County was another area especially hard hit. Here, several wind gusts in the 80-90 MPH range were reported, and damage was significant. Numerous trees were uprooted, pivots overturned, and outbuildings and grain bins destroyed. Another destructive aspect of this storm is that it also produced ping pong ball sized hail that was blown by the intense winds. This resulted in significant window and body damage to cars, as well as roof, siding, and window damage to homes. Additional significant wind damage was reported in and around Burwell (just barely outside this coverage area). The first round of thunderstorms exited north/northeast of the area around 3:30PM CDT, but the next round was ���hot on its heels���, and entered southern Nebraska around 4PM CDT, and quickly became severe. In fact, brief, but intense, circulations were noted on radar for a time just south and southeast of Hastings. This round affected mainly areas along and east of Highway 281. Since this region was spared from the first round, and a similar thermodynamic and kinematic environment was still in place, it���s no surprise that this round also intensified enough to produce ���significant severe��� wind gusts, most notably in a swath from Clay County northeast to Polk County. Several more 60-70 MPH wind gusts were reported in these areas, causing more overturned pivots, downed power lines, and damage to roofs, outbuildings, and grain bins. Also, intense wind gusts moved over Interstate 80 in Hamilton County, causing multiple overturned semis. This second round exited into eastern Nebraska and out of the Hastings CWA around 7PM CDT. The third and final round began to affect areas along and east Highway 183 between 7PM and 8PM CDT. The majority of this activity remained sub-severe as the greatest instability had been used up by the two previous rounds. However, a marginally severe wind gust of 59 MPH was measured at the Hastings airport shortly before 8PM. Thereafter, weakening ensued as the line became strung out and forward propagation slowed. Thunderstorms finally exited south central Nebraska between 11PM and midnight, ending a roughly 10 hour stretch of seemingly never ending severe weather!||Meteorologically speaking, this event was driven by a particularly volatile combination of intensifying shortwave ejecting from the central Rockies into the northern Plains, very unstable airmass (MUCAPE of 3000-4000 J/kg at it���s peak), and strong deep layer shear driven by 500 mb speed max of 60-70 kt. While this setup is not unheard of for mid-May, it���s certainly not very common, and for three distinct waves of thunderstorms to move through in a 10 hour period (two of which contained significant severe weather phenomena) is also not very common. From a regional perspective, the Hastings CWA was the developing grounds for a significant derecho that would propagate into the Northern Plains and Upper Mississippi Valley and go on to produce hundreds of measured severe wind gusts and wind damage reports, of which over 60 were considered ���significant severe���. Over 75 hail reports and nearly three dozen tornado reports were also reported, with the majority of tornadoes occurring in SD and MN. For 2022, this will likely be remembered as one of the most severe convective events of the year, both locally, and across the greater region. A mesonet station located four miles northeast of Fairfield measured wind gusts of 64 MPH and 69 MPH. A wind gust of 60 MPH was measured by a mesonet station located four miles southeast of Clay Center. A NWS Cooperative Observer located six miles east-southeast of Clay Center estimated wind gusts to be near 70 MPH, and also reported near-zero visibility due to blowing dust.", "ts_dict_index": [7884, 7885, 7886]}
+{"event_id": 1045510, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-07-16 20:49:00", "end_date_time": "2022-07-16 20:49:00", "narrative": "Several strong to severe thunderstorms, some that eventually merged into a compact mesoscale convective system (MCS), rumbled southeastward across various parts of South Central Nebraska mainly between 6:30-11:30 p.m. CDT on this Saturday evening, prompting assorted reports of large hail (up to baseball size) and damaging winds (estimated up to 80 MPH) and disrupting activities at a handful of local county fairs. The most prominent narrow swath of severe activity cut through the heart of the 24-county area, focusing within 10 miles either side of a line extending from Ord-Cairo-Hastings-Davenport as an initially isolated supercell merged with a separate cluster of severe storms to its west, forming the aforementioned MCS. During it's more supercellular phase near/north of the Highway 92 corridor (mainly 6:30-8:30 p.m. CDT), a combo of both damaging winds and large hail occurred, featuring measured gusts as high as 74 MPH at Ord airport and hail ranging from golf ball to baseball size particularly within western Howard and far northwestern Hall counties. In Howard County, a stripe of significant damage to crops and windows/siding was noted from around Farwell to west of Dannebrog. As this MCS reached areas near/south of Interstate 80 (primarily 9-11 p.m. CDT) the hail threat waned but damaging winds continued, evidenced by a measured 58 MPH gust at Hastings airport and unofficial mesonet-measured gusts of 67 MPH near Nelson and 62 MPH near Davenport. Within Clay County, tree branches were downed in several communities including Trumbull, Deweese, Fairfield and Edgar. Shortly before this storm complex exited the local area to the southeast between 11:00-11:30 p.m. CDT, wind intensity ramped down to slightly sub-severe levels within southern/eastern Thayer County. Although far from the only outdoor event interruption of the evening within South Central Nebraska, one of the more noteworthy ones associated with this MCS involved the Adams County Fairfest in Hastings, where an ongoing Nelly concert was cut short and an evacuation of the grounds was successfully initiated shortly before the storm struck. Although rain totals of 1-2 inches were common within the heart of the MCS track (overall highest inF Clay County), any flooding was of the very short term/nuisance variety. To the west of the aforementioned primary swath of severe weather, a few separate and smaller-scale areas of strong to severe storms impacted portions of primarily Furnas, Buffalo and Dawson counties mainly between 7-9 p.m. CDT. In Furnas County, a relatively small but intense supercell roamed northern and eastern parts of the county, with estimated 80 MPH winds destroying an outbuilding and grain bin at a farmstead between Holbrook and Arapahoe. Meanwhile, other semi-discrete convection within parts of Buffalo/Dawson counties yielded a few wind reports including a mesonet-measured 64 MPH gust near Kearney and a slightly sub-severe 54 MPH speed near Lexington. The eastern reaches of this activity eventually merged with the primary MCS as it charged across the I-80 corridor and into the Hastings area. ||Finishing with some details regarding the evolution and meteorology behind this event, the initial development of isolated to scattered thunderstorms during the mid-late afternoon hours occurred in separate areas slightly off to  the north and also west of South Central Nebraska, with this early activity gradually increasing in both coverage/intensity as it evolved into the local area. In the mid-upper levels, forcing was fairly weak, featuring only subtle shortwave energy working into the region in west-northwest flow, directed around the northeastern periphery of a large-scale ridge centered over the Four Corners region. At the surface, there were also no significant features of note locally, with most of South Central Nebraska simply reporting 5-15 MPH east-southeasterly breezes during the afternoon. However, the initial storm development off to the north and west of the area appeared to be tied to weak convergence along a pair of subtle boundaries. Despite the aforementioned weak forcing and also weak mid level lapse rates, the environment featured plentiful low level moisture/instability and seasonably-decent deep layer wind shear of 30-40 knots. Ahead of the incoming storms, late afternoon temperatures in the upper 80s-low 90s (F) and dewpoints in the upper 60s-mid 70s promoted mixed-layer CAPE 2000-3000 J/kg. Some tree branches were downed in Deweese, with power outages also reported.", "ts_dict_index": [7917, 7918, 7919]}
+{"event_id": 1018103, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-04-23 03:09:00", "end_date_time": "2022-04-23 03:15:00", "narrative": "A strong mid-upper level trough axis made its way through the Rockies on Friday the 22nd, with a more organized circulation deepening Friday night into early Saturday morning the 23rd as it tracked into the central and northern High Plains. Through the rest of the day on the 23rd this system continued to deepen and become increasingly vertically-stacked, gradually sliding northeast into the central South Dakota/North Dakota border area by that evening. In response to this approaching system, surface low pressure intensified over northeastern Colorado into the southern border of Nebraska/Wyoming on the 22nd, bottoming out around 984 millibars by early evening. With South Central Nebraska sandwiched between this surface low and high pressure ridging southward through the entire eastern CONUS, the result was a tightening pressure gradient and intense southerly winds. Sustained southerly speeds of 35-45 MPH and gusts of 45-55 MPH were common across the area by midday on the 22nd. For western local counties, a few gusts had already crept a bit higher by mid-late afternoon, including 60 MPH at 3:30 p.m. CDT near Oxford in Harlan County. ||By mid-late afternoon on the 22nd, the main surface boundaries included the warm front (which had pushed north into southern South Dakota) and a dryline (which extended from South Dakota through west central Nebraska into western Kansas). This placed South Central Nebraska firmly in the warm sector, with well-above normal temperatures soaring into the mid 80s to mid 90s (F) and with dewpoints in far west-southwest locations near the dryline dropping into the 40s. This set the stage for critically-low relative humidity and fire weather conditions. Unfortunately, the fire danger threat was realized in a big-time way around 3:30 p.m. CDT when a wildfire ignited just outside the local area in far northwestern Norton County Kansas. Due to southerly winds gusting near 60 MPH, this fire quickly spread out of control and raced north-northwestward, primarily impacting areas along the Furnas/Red Willow County line. Firefighters were able to halt its forward progress by late that evening, but hot spots and flare ups continued through the overnight hours. Areas in and around Cambridge and Wilsonville were put on evacuation notices, with the town of Cambridge and surrounding areas eventually being evacuated. Fortunately, Cambridge itself was spared from the fire. This was the second significant wildfire to impact Furnas County in 15 days (the first being the Road 739 Fire that ignited on the 7th). In total, the Road 702 Fire burned approximately 44,000 acres, with the Furnas County portion in this South Central Nebraska coverage area accounting for around 15,000 acres (for more details regarding this fire please refer to the associated event narrative). ||In addition to the critical fire weather situation on the afternoon of the 22nd, a few scattered thunderstorms initiated along the surface dryline around 4 p.m. CDT. This initial cluster of storms developed in an environment with approximately 2000 j/kg mixed-layer CAPE but only around 30 knots of 0-6 kilometer shear. This activity moved out of the local area into north central Nebraska by early evening, but not before dropping hail up to the size of golf balls over Gothenburg around 5:30 p.m. CDT. Later into the mid-late evening hours, a more organized line of thunderstorms developed along the surface cold front over western Nebraska and Kansas as the main mid-upper level system pushed out of the Rockies into western Nebraska and South Dakota. This activity tracked east through South Central Nebraska mainly between 2-7 a.m. CDT on the 23rd. While most of these storms were sub-severe, increasing deep-layer shear and downdraft CAPE values near 1000 j/kg aided in a handful of storms producing severe gusts, including a peak gust of 65 MPH measured by a mesonet station located five miles north-northwest of Oxford. ||By around sunrise on the 23rd the surface low was located over south central South Dakota, with the initial cold front extending southward roughly along the Highway 81 corridor of South Central Nebraska, which prompted still-gusty winds to become southwesterly. A stronger, reinforcing cold front then made its way east across the area from mid-morning through the afternoon hours, ushering in a sharper switch to westerly winds and a cooler, drier air mass. Pressure rises and cold air advection in the wake of this frontal passage resulted in several hours of gusts near or exceeding 45-50 MPH, as well as a handful of gusts near 60 MPH. The highest measured gust through the afternoon and evening hours was 64 MPH at Central Nebraska Regional Airport in Grand Island. This wind switch also made a significant impact on the Road 702 Fire situation in Furnas County, causing the fire to reignite and burn out of control once again (this time spreading eastward). Fortunately, late that evening firefighters were again able to stop its progression. A wind gust of 59 MPH was measured by a mesonet station located two miles north of Hastings. Some tree damage was reported near the intersection of Showboat Road and Highway 74 near Pauline. A small tin outbuilding was damaged in this same vicinity.", "ts_dict_index": [7890, 7891, 7892]}
+{"event_id": 844686, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-08-07 01:55:00", "end_date_time": "2019-08-07 01:55:00", "narrative": "Although its main damage swath was only about 15 miles wide, the narrow-but-intense severe storm complex that raced from northwest-to-southeast through the heart of South Central Nebraska during the pre-dawn hours on this Wednesday was one of the most impactful events of the local convective season. Quite simply, this was a nasty wind storm, packing a punch with gusts ranging from around 60 to nearly 90 MPH along and several miles either side of a line stretching from Ord-Grand Island-Hastings-Hardy. For the city of Grand Island, this was likely the overall-worst wind storm in several years, as the airport ASOS clocked a peak gust of 87 MPH. Countless trees/large branches were blown down within the city, along with several power lines, and there was also some (mainly) minor structural damage. Grand Island Emergency Center logged nearly 300 storm related incidents, including traffic hazards, power outages, alarms and fire concerns from sparking electricity. The storm also caused an (indirect) traffic fatality in rural Hall County southeast of Cairo, when a man crashed his pickup into a large, downed tree arched across a paved county road. To the south in Hastings, damage was less-severe overall, as the ASOS peak gust on the west side of town was only 70 MPH. However, stronger winds likely impacted areas just east of the city, as large trees were uprooted at Central Community College and several rail cars were reportedly blown over at a repair facility near the Clay County line. Several smaller communities also reported notable wind damage, including: Cairo, Alda, Wood River, Doniphan, Glenvil, and Fairfield. West of Clay Center, fairly extensive damage occurred on the U.S. Meat Animal Research Center campus, including broken windows and roof damage to several buildings. In addition to the aforementioned peak wind gusts at Grand Island/Hastings airports, some of the more notable unofficial (mesonet) gusts included: 85 MPH near Fairfield, 80 MPH near Alda and Wood River, 79 MPH in Doniphan and 73 MPH near Nelson. Despite the multitude of damaging wind reports, hail reports were quite scarce, as the vast majority of stones were likely dime size or smaller. Rainfall-wise, a fairly widespread coverage of 2-3 soaked several northern counties including: Valley, Greeley, Sherman, Nance and Merrick. Although resultant flooding was not very extensive in most of the area, the Mira Creek in southern Valley County breached its banks for the second time in five days, again prompting minor flooding on the north side of North Loup that continued into the early morning of the 8th.||Breaking down the timing and meteorological background of this event, it's worth noting that these South Central Nebraska damaging winds were actually the finale to a much longer swath of severe weather that initiated in southern ND and north central SD during the afternoon/evening of the 6th. Between 1-2 a.m. CDT on the 7th, the leading edge of this narrow-but-potent mesoscale convective system (MCS) entered far northern portions of the local area into Valley/Greeley counties, signaling its arrival with a 59 MPH gust at Ord airport. However, the worst was yet to come, as during the next few hours the storm complex morphed into more of an outflow-dominant, high-precipitation supercell, slamming through the Grand Island/Hastings areas between 2:30-3:30 a.m. CDT before eventually exiting Nuckolls/Thayer counties into Kansas by 5 a.m. CDT. In the wake of the main show, a few weaker clusters of storms redeveloped over parts of the area into the daylight hours, but were of little significance. In the big picture of the mid-upper levels, this event occurred within a fairly classic summertime northwest-flow regime, as the Central Plains resided northeast of an expansive ridge centered over New Mexico. At the surface, South Central Nebraska was on the backside of a weak ridge axis centered near the Nebraska-Iowa border. This promoted light-but-steady, south-southeast breezes in advance of the approaching storm complex, with surface dewpoints averaging mid-upper 60s F. Although there were question marks about how far southward into Nebraska the potential severe weather threat would extend, the combination of seasonably-stout flow aloft (deep-layer wind shear of at least 40-60 knots) and sufficient instability (mixed-layer CAPE of 1000-2000 J/kg) was clearly supportive of an intense late-night storm. Also enhancing the severe weather environment was a modest, 30 knot  southwesterly low level jet (evident at 850 millibars) and its associated low-level warm air/moisture advection. Wind gusts estimated to be near 80 MPH resulted in a large tree being snapped just above the ground.", "ts_dict_index": [7911, 7912, 7913]}
+{"event_id": 844791, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-08-07 02:00:00", "end_date_time": "2019-08-07 02:10:00", "narrative": "Although its main damage swath was only about 15 miles wide, the narrow-but-intense severe storm complex that raced from northwest-to-southeast through the heart of South Central Nebraska during the pre-dawn hours on this Wednesday was one of the most impactful events of the local convective season. Quite simply, this was a nasty wind storm, packing a punch with gusts ranging from around 60 to nearly 90 MPH along and several miles either side of a line stretching from Ord-Grand Island-Hastings-Hardy. For the city of Grand Island, this was likely the overall-worst wind storm in several years, as the airport ASOS clocked a peak gust of 87 MPH. Countless trees/large branches were blown down within the city, along with several power lines, and there was also some (mainly) minor structural damage. Grand Island Emergency Center logged nearly 300 storm related incidents, including traffic hazards, power outages, alarms and fire concerns from sparking electricity. The storm also caused an (indirect) traffic fatality in rural Hall County southeast of Cairo, when a man crashed his pickup into a large, downed tree arched across a paved county road. To the south in Hastings, damage was less-severe overall, as the ASOS peak gust on the west side of town was only 70 MPH. However, stronger winds likely impacted areas just east of the city, as large trees were uprooted at Central Community College and several rail cars were reportedly blown over at a repair facility near the Clay County line. Several smaller communities also reported notable wind damage, including: Cairo, Alda, Wood River, Doniphan, Glenvil, and Fairfield. West of Clay Center, fairly extensive damage occurred on the U.S. Meat Animal Research Center campus, including broken windows and roof damage to several buildings. In addition to the aforementioned peak wind gusts at Grand Island/Hastings airports, some of the more notable unofficial (mesonet) gusts included: 85 MPH near Fairfield, 80 MPH near Alda and Wood River, 79 MPH in Doniphan and 73 MPH near Nelson. Despite the multitude of damaging wind reports, hail reports were quite scarce, as the vast majority of stones were likely dime size or smaller. Rainfall-wise, a fairly widespread coverage of 2-3 soaked several northern counties including: Valley, Greeley, Sherman, Nance and Merrick. Although resultant flooding was not very extensive in most of the area, the Mira Creek in southern Valley County breached its banks for the second time in five days, again prompting minor flooding on the north side of North Loup that continued into the early morning of the 8th.||Breaking down the timing and meteorological background of this event, it's worth noting that these South Central Nebraska damaging winds were actually the finale to a much longer swath of severe weather that initiated in southern ND and north central SD during the afternoon/evening of the 6th. Between 1-2 a.m. CDT on the 7th, the leading edge of this narrow-but-potent mesoscale convective system (MCS) entered far northern portions of the local area into Valley/Greeley counties, signaling its arrival with a 59 MPH gust at Ord airport. However, the worst was yet to come, as during the next few hours the storm complex morphed into more of an outflow-dominant, high-precipitation supercell, slamming through the Grand Island/Hastings areas between 2:30-3:30 a.m. CDT before eventually exiting Nuckolls/Thayer counties into Kansas by 5 a.m. CDT. In the wake of the main show, a few weaker clusters of storms redeveloped over parts of the area into the daylight hours, but were of little significance. In the big picture of the mid-upper levels, this event occurred within a fairly classic summertime northwest-flow regime, as the Central Plains resided northeast of an expansive ridge centered over New Mexico. At the surface, South Central Nebraska was on the backside of a weak ridge axis centered near the Nebraska-Iowa border. This promoted light-but-steady, south-southeast breezes in advance of the approaching storm complex, with surface dewpoints averaging mid-upper 60s F. Although there were question marks about how far southward into Nebraska the potential severe weather threat would extend, the combination of seasonably-stout flow aloft (deep-layer wind shear of at least 40-60 knots) and sufficient instability (mixed-layer CAPE of 1000-2000 J/kg) was clearly supportive of an intense late-night storm. Also enhancing the severe weather environment was a modest, 30 knot  southwesterly low level jet (evident at 850 millibars) and its associated low-level warm air/moisture advection. A 70 MPH wind gust was measured by the Hastings Airport ASOS at 3:10 AM CDT, and a 68 MPH wind gust was measured at the NWS Hastings office located 4 miles north of Hastings. These wind gusts resulted in reports of widespread tree damage across the Hastings area. Large trees were snapped and large limbs were downed. Foundation damage to a small outbuilding was also reported.", "ts_dict_index": [7908, 7909, 7910]}
+{"event_id": 845299, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-08-07 02:12:00", "end_date_time": "2019-08-07 02:12:00", "narrative": "Although its main damage swath was only about 15 miles wide, the narrow-but-intense severe storm complex that raced from northwest-to-southeast through the heart of South Central Nebraska during the pre-dawn hours on this Wednesday was one of the most impactful events of the local convective season. Quite simply, this was a nasty wind storm, packing a punch with gusts ranging from around 60 to nearly 90 MPH along and several miles either side of a line stretching from Ord-Grand Island-Hastings-Hardy. For the city of Grand Island, this was likely the overall-worst wind storm in several years, as the airport ASOS clocked a peak gust of 87 MPH. Countless trees/large branches were blown down within the city, along with several power lines, and there was also some (mainly) minor structural damage. Grand Island Emergency Center logged nearly 300 storm related incidents, including traffic hazards, power outages, alarms and fire concerns from sparking electricity. The storm also caused an (indirect) traffic fatality in rural Hall County southeast of Cairo, when a man crashed his pickup into a large, downed tree arched across a paved county road. To the south in Hastings, damage was less-severe overall, as the ASOS peak gust on the west side of town was only 70 MPH. However, stronger winds likely impacted areas just east of the city, as large trees were uprooted at Central Community College and several rail cars were reportedly blown over at a repair facility near the Clay County line. Several smaller communities also reported notable wind damage, including: Cairo, Alda, Wood River, Doniphan, Glenvil, and Fairfield. West of Clay Center, fairly extensive damage occurred on the U.S. Meat Animal Research Center campus, including broken windows and roof damage to several buildings. In addition to the aforementioned peak wind gusts at Grand Island/Hastings airports, some of the more notable unofficial (mesonet) gusts included: 85 MPH near Fairfield, 80 MPH near Alda and Wood River, 79 MPH in Doniphan and 73 MPH near Nelson. Despite the multitude of damaging wind reports, hail reports were quite scarce, as the vast majority of stones were likely dime size or smaller. Rainfall-wise, a fairly widespread coverage of 2-3 soaked several northern counties including: Valley, Greeley, Sherman, Nance and Merrick. Although resultant flooding was not very extensive in most of the area, the Mira Creek in southern Valley County breached its banks for the second time in five days, again prompting minor flooding on the north side of North Loup that continued into the early morning of the 8th.||Breaking down the timing and meteorological background of this event, it's worth noting that these South Central Nebraska damaging winds were actually the finale to a much longer swath of severe weather that initiated in southern ND and north central SD during the afternoon/evening of the 6th. Between 1-2 a.m. CDT on the 7th, the leading edge of this narrow-but-potent mesoscale convective system (MCS) entered far northern portions of the local area into Valley/Greeley counties, signaling its arrival with a 59 MPH gust at Ord airport. However, the worst was yet to come, as during the next few hours the storm complex morphed into more of an outflow-dominant, high-precipitation supercell, slamming through the Grand Island/Hastings areas between 2:30-3:30 a.m. CDT before eventually exiting Nuckolls/Thayer counties into Kansas by 5 a.m. CDT. In the wake of the main show, a few weaker clusters of storms redeveloped over parts of the area into the daylight hours, but were of little significance. In the big picture of the mid-upper levels, this event occurred within a fairly classic summertime northwest-flow regime, as the Central Plains resided northeast of an expansive ridge centered over New Mexico. At the surface, South Central Nebraska was on the backside of a weak ridge axis centered near the Nebraska-Iowa border. This promoted light-but-steady, south-southeast breezes in advance of the approaching storm complex, with surface dewpoints averaging mid-upper 60s F. Although there were question marks about how far southward into Nebraska the potential severe weather threat would extend, the combination of seasonably-stout flow aloft (deep-layer wind shear of at least 40-60 knots) and sufficient instability (mixed-layer CAPE of 1000-2000 J/kg) was clearly supportive of an intense late-night storm. Also enhancing the severe weather environment was a modest, 30 knot  southwesterly low level jet (evident at 850 millibars) and its associated low-level warm air/moisture advection. Wind gusts estimated to be at least 80 MPH resulted in 27 railroad cars being flipped on their sides off of the tracks.", "ts_dict_index": [7896, 7897, 7898]}
+{"event_id": 845301, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-08-07 02:10:00", "end_date_time": "2019-08-07 02:10:00", "narrative": "Although its main damage swath was only about 15 miles wide, the narrow-but-intense severe storm complex that raced from northwest-to-southeast through the heart of South Central Nebraska during the pre-dawn hours on this Wednesday was one of the most impactful events of the local convective season. Quite simply, this was a nasty wind storm, packing a punch with gusts ranging from around 60 to nearly 90 MPH along and several miles either side of a line stretching from Ord-Grand Island-Hastings-Hardy. For the city of Grand Island, this was likely the overall-worst wind storm in several years, as the airport ASOS clocked a peak gust of 87 MPH. Countless trees/large branches were blown down within the city, along with several power lines, and there was also some (mainly) minor structural damage. Grand Island Emergency Center logged nearly 300 storm related incidents, including traffic hazards, power outages, alarms and fire concerns from sparking electricity. The storm also caused an (indirect) traffic fatality in rural Hall County southeast of Cairo, when a man crashed his pickup into a large, downed tree arched across a paved county road. To the south in Hastings, damage was less-severe overall, as the ASOS peak gust on the west side of town was only 70 MPH. However, stronger winds likely impacted areas just east of the city, as large trees were uprooted at Central Community College and several rail cars were reportedly blown over at a repair facility near the Clay County line. Several smaller communities also reported notable wind damage, including: Cairo, Alda, Wood River, Doniphan, Glenvil, and Fairfield. West of Clay Center, fairly extensive damage occurred on the U.S. Meat Animal Research Center campus, including broken windows and roof damage to several buildings. In addition to the aforementioned peak wind gusts at Grand Island/Hastings airports, some of the more notable unofficial (mesonet) gusts included: 85 MPH near Fairfield, 80 MPH near Alda and Wood River, 79 MPH in Doniphan and 73 MPH near Nelson. Despite the multitude of damaging wind reports, hail reports were quite scarce, as the vast majority of stones were likely dime size or smaller. Rainfall-wise, a fairly widespread coverage of 2-3 soaked several northern counties including: Valley, Greeley, Sherman, Nance and Merrick. Although resultant flooding was not very extensive in most of the area, the Mira Creek in southern Valley County breached its banks for the second time in five days, again prompting minor flooding on the north side of North Loup that continued into the early morning of the 8th.||Breaking down the timing and meteorological background of this event, it's worth noting that these South Central Nebraska damaging winds were actually the finale to a much longer swath of severe weather that initiated in southern ND and north central SD during the afternoon/evening of the 6th. Between 1-2 a.m. CDT on the 7th, the leading edge of this narrow-but-potent mesoscale convective system (MCS) entered far northern portions of the local area into Valley/Greeley counties, signaling its arrival with a 59 MPH gust at Ord airport. However, the worst was yet to come, as during the next few hours the storm complex morphed into more of an outflow-dominant, high-precipitation supercell, slamming through the Grand Island/Hastings areas between 2:30-3:30 a.m. CDT before eventually exiting Nuckolls/Thayer counties into Kansas by 5 a.m. CDT. In the wake of the main show, a few weaker clusters of storms redeveloped over parts of the area into the daylight hours, but were of little significance. In the big picture of the mid-upper levels, this event occurred within a fairly classic summertime northwest-flow regime, as the Central Plains resided northeast of an expansive ridge centered over New Mexico. At the surface, South Central Nebraska was on the backside of a weak ridge axis centered near the Nebraska-Iowa border. This promoted light-but-steady, south-southeast breezes in advance of the approaching storm complex, with surface dewpoints averaging mid-upper 60s F. Although there were question marks about how far southward into Nebraska the potential severe weather threat would extend, the combination of seasonably-stout flow aloft (deep-layer wind shear of at least 40-60 knots) and sufficient instability (mixed-layer CAPE of 1000-2000 J/kg) was clearly supportive of an intense late-night storm. Also enhancing the severe weather environment was a modest, 30 knot  southwesterly low level jet (evident at 850 millibars) and its associated low-level warm air/moisture advection. A 65 MPH wind gust was measured by a mesonet station located 2 miles southwest of Roseland.", "ts_dict_index": [7899, 7900, 7901]}
+{"event_id": 1045506, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-07-16 20:37:00", "end_date_time": "2022-07-16 20:37:00", "narrative": "Several strong to severe thunderstorms, some that eventually merged into a compact mesoscale convective system (MCS), rumbled southeastward across various parts of South Central Nebraska mainly between 6:30-11:30 p.m. CDT on this Saturday evening, prompting assorted reports of large hail (up to baseball size) and damaging winds (estimated up to 80 MPH) and disrupting activities at a handful of local county fairs. The most prominent narrow swath of severe activity cut through the heart of the 24-county area, focusing within 10 miles either side of a line extending from Ord-Cairo-Hastings-Davenport as an initially isolated supercell merged with a separate cluster of severe storms to its west, forming the aforementioned MCS. During it's more supercellular phase near/north of the Highway 92 corridor (mainly 6:30-8:30 p.m. CDT), a combo of both damaging winds and large hail occurred, featuring measured gusts as high as 74 MPH at Ord airport and hail ranging from golf ball to baseball size particularly within western Howard and far northwestern Hall counties. In Howard County, a stripe of significant damage to crops and windows/siding was noted from around Farwell to west of Dannebrog. As this MCS reached areas near/south of Interstate 80 (primarily 9-11 p.m. CDT) the hail threat waned but damaging winds continued, evidenced by a measured 58 MPH gust at Hastings airport and unofficial mesonet-measured gusts of 67 MPH near Nelson and 62 MPH near Davenport. Within Clay County, tree branches were downed in several communities including Trumbull, Deweese, Fairfield and Edgar. Shortly before this storm complex exited the local area to the southeast between 11:00-11:30 p.m. CDT, wind intensity ramped down to slightly sub-severe levels within southern/eastern Thayer County. Although far from the only outdoor event interruption of the evening within South Central Nebraska, one of the more noteworthy ones associated with this MCS involved the Adams County Fairfest in Hastings, where an ongoing Nelly concert was cut short and an evacuation of the grounds was successfully initiated shortly before the storm struck. Although rain totals of 1-2 inches were common within the heart of the MCS track (overall highest inF Clay County), any flooding was of the very short term/nuisance variety. To the west of the aforementioned primary swath of severe weather, a few separate and smaller-scale areas of strong to severe storms impacted portions of primarily Furnas, Buffalo and Dawson counties mainly between 7-9 p.m. CDT. In Furnas County, a relatively small but intense supercell roamed northern and eastern parts of the county, with estimated 80 MPH winds destroying an outbuilding and grain bin at a farmstead between Holbrook and Arapahoe. Meanwhile, other semi-discrete convection within parts of Buffalo/Dawson counties yielded a few wind reports including a mesonet-measured 64 MPH gust near Kearney and a slightly sub-severe 54 MPH speed near Lexington. The eastern reaches of this activity eventually merged with the primary MCS as it charged across the I-80 corridor and into the Hastings area. ||Finishing with some details regarding the evolution and meteorology behind this event, the initial development of isolated to scattered thunderstorms during the mid-late afternoon hours occurred in separate areas slightly off to  the north and also west of South Central Nebraska, with this early activity gradually increasing in both coverage/intensity as it evolved into the local area. In the mid-upper levels, forcing was fairly weak, featuring only subtle shortwave energy working into the region in west-northwest flow, directed around the northeastern periphery of a large-scale ridge centered over the Four Corners region. At the surface, there were also no significant features of note locally, with most of South Central Nebraska simply reporting 5-15 MPH east-southeasterly breezes during the afternoon. However, the initial storm development off to the north and west of the area appeared to be tied to weak convergence along a pair of subtle boundaries. Despite the aforementioned weak forcing and also weak mid level lapse rates, the environment featured plentiful low level moisture/instability and seasonably-decent deep layer wind shear of 30-40 knots. Ahead of the incoming storms, late afternoon temperatures in the upper 80s-low 90s (F) and dewpoints in the upper 60s-mid 70s promoted mixed-layer CAPE 2000-3000 J/kg. Wind gusts were estimated to be near 65 MPH.", "ts_dict_index": [7929, 7930, 7931]}
+{"event_id": 974123, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2021-07-09 21:47:00", "end_date_time": "2021-07-09 21:56:00", "narrative": "Significant damaging wind event strikes south central Nebraska during the late evening hours of July 9, 2021. This event began well west and northwest of the Hastings County Warning Area (CWA), within the Nebraska Panhandle, during the late afternoon and early evening hours as a small cluster of thunderstorms. These thunderstorms became severe at various points during their eastward track across the Nebraska Sandhills through the evening, but it wasn���t until they reached the North Platte and Broken Bow areas around 9PM CDT that they became significantly organized and severe. This activity quickly moved into W and NW portions of the CWA between 9-10PM CDT, with the strongest thunderstorms and associated wind gusts focused across Dawson County. Wind gusts of 65 MPH to nearly 80 MPH were common across the county, which resulted in widespread tree damage and numerous power outages. Activity quickly grew upscale in terms of coverage and intensity as it shifted SE, and by 10 PM CDT, there was a solid line of thunderstorms from Nance County to Buffalo County to northern Gosper County that would prove to become a prolific damaging wind producer over the next couple of hours, including for the three largest cities in the Hastings CWA - Kearney, Grand Island, and Hastings. Wind gusts of 60-80 MPH were either reported or estimated in all of these areas. Not surprisingly, impacts were fairly significant, especially in terms of the overall scope of tree damage and power outages, including snapped power poles and healthy trees that were snapped off near the ground. Some of the trees fell onto homes and vehicles. In Kearney, a roof was partially torn off a movie theater, which also led to extensive water damage due to the torrential rain. Conditions became treacherous along Interstate 80 as the strong wind gusts on the leading edge of the thunderstorms led to overturned semi-trucks, other trailers, and campers, as well as very limited visibility due to blowing dust. As the line of thunderstorms moved east of Highway 281, some localized corridors of particularly intense winds, observed or estimated to be as high as 80-95 MPH, developed across portions of eastern Hall County, southern Hamilton County, and northern Clay County between 10:30-11:30 PM CDT. The most intense wind occurred in a swath from around Central Nebraska Regional Airport, where an 84 MPH gust was measured, southeast towards areas near and south of Aurora, to near Giltner. Damage in these areas included: significant tree and power line damage, snapped power poles, flattened crops, overturned pivots, damaged or destroyed grain bins and outbuildings, and two blown over semi-trucks on Interstate 80. Some tree limbs fell on cars and buildings, and some minor roof and window damage occurred to a few businesses. Perhaps the most impressive damage was downed high-voltage transmission lines approximately 4 miles south of Aurora where they cross Interstate 80. This led to traffic issues in the area for a time. Similar tree, power line, crop, irrigation pivot, and grain bin/outbuilding damage was reported in portions of Clay County. The line of thunderstorms weakened slightly as they shifted E and SE towards the Highway 81 corridor between 11PM and midnight, though gusts of 65-75 MPH were still reported in York, Fillmore, and Thayer Counties. Most notable damage (other than tree and power line damage) were half dozen overturned pivots, flattened corn, and a tree falling on a car. Severe thunderstorms finally exited south central Nebraska by 1AM on July 10. When all was said and done, a nearly continuous swath of relatively concentrated wind damage 30 to 50 miles wide occurred from near North Platte, NE to areas just E/NE of Hebron, NE. Gov. Ricketts declared disaster declaration for 14 total counties in Nebraska, including Clay, Fillmore, Hall, Hamilton and York counties in our CWA, and it was ultimately approved by President Biden. Preliminary assessment by FEMA estimated over 30 million dollars in damages.||Meteorologically speaking, this complex of thunderstorms was not unexpected, though intensity forecasts were ramped up just hours before the onset. SPC outlooks increased from a ���Slight��� risk in the morning, to an ���Enhanced��� risk for the western half of the CWA in the 3PM CDT update. The ���Enhanced��� risk was expanded to include all of south central Nebraska with the evening update. Strong wind shear (effective shear 50-60kt) was a consistent feature of the forecast, with the primary uncertainty being low level moisture quality and how much instability there would be for storms to work with as they moved off of the High Plains. Ultimately, low level moisture, in particular surface dew points, were much higher than modeled. For example, surface dew points were well into the mid 70s across a large portion of central and south central Nebraska, vs. modeled dew points in the 60s. This discrepancy was likely due to strong evapotranspiration from irrigation and mature crops, as well as weak low level mixing. As such, instability was very strong with MUCAPE of 5000-7000 J/kg, and this continued well into the overnight hours. Downdraft CAPE was also high at around 1000-1300 J/kg. Not surprisingly, the Derecho Composite parameter peaked between 4-6, which was significant. A wind gust of 63 MPH was recorded at 10:56 PM CDT by the Hastings Airport and a wind gust of 61 MPH was recorded at 10:47 PM CDT by the mesonet station located at the NWS Hastings office four miles north of Hastings. Emergency management reported tree damage in Hastings, including some limbs over roadways.", "ts_dict_index": [7863, 7864, 7865]}
+{"event_id": 1045505, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-07-16 20:26:00", "end_date_time": "2022-07-16 20:26:00", "narrative": "Several strong to severe thunderstorms, some that eventually merged into a compact mesoscale convective system (MCS), rumbled southeastward across various parts of South Central Nebraska mainly between 6:30-11:30 p.m. CDT on this Saturday evening, prompting assorted reports of large hail (up to baseball size) and damaging winds (estimated up to 80 MPH) and disrupting activities at a handful of local county fairs. The most prominent narrow swath of severe activity cut through the heart of the 24-county area, focusing within 10 miles either side of a line extending from Ord-Cairo-Hastings-Davenport as an initially isolated supercell merged with a separate cluster of severe storms to its west, forming the aforementioned MCS. During it's more supercellular phase near/north of the Highway 92 corridor (mainly 6:30-8:30 p.m. CDT), a combo of both damaging winds and large hail occurred, featuring measured gusts as high as 74 MPH at Ord airport and hail ranging from golf ball to baseball size particularly within western Howard and far northwestern Hall counties. In Howard County, a stripe of significant damage to crops and windows/siding was noted from around Farwell to west of Dannebrog. As this MCS reached areas near/south of Interstate 80 (primarily 9-11 p.m. CDT) the hail threat waned but damaging winds continued, evidenced by a measured 58 MPH gust at Hastings airport and unofficial mesonet-measured gusts of 67 MPH near Nelson and 62 MPH near Davenport. Within Clay County, tree branches were downed in several communities including Trumbull, Deweese, Fairfield and Edgar. Shortly before this storm complex exited the local area to the southeast between 11:00-11:30 p.m. CDT, wind intensity ramped down to slightly sub-severe levels within southern/eastern Thayer County. Although far from the only outdoor event interruption of the evening within South Central Nebraska, one of the more noteworthy ones associated with this MCS involved the Adams County Fairfest in Hastings, where an ongoing Nelly concert was cut short and an evacuation of the grounds was successfully initiated shortly before the storm struck. Although rain totals of 1-2 inches were common within the heart of the MCS track (overall highest inF Clay County), any flooding was of the very short term/nuisance variety. To the west of the aforementioned primary swath of severe weather, a few separate and smaller-scale areas of strong to severe storms impacted portions of primarily Furnas, Buffalo and Dawson counties mainly between 7-9 p.m. CDT. In Furnas County, a relatively small but intense supercell roamed northern and eastern parts of the county, with estimated 80 MPH winds destroying an outbuilding and grain bin at a farmstead between Holbrook and Arapahoe. Meanwhile, other semi-discrete convection within parts of Buffalo/Dawson counties yielded a few wind reports including a mesonet-measured 64 MPH gust near Kearney and a slightly sub-severe 54 MPH speed near Lexington. The eastern reaches of this activity eventually merged with the primary MCS as it charged across the I-80 corridor and into the Hastings area. ||Finishing with some details regarding the evolution and meteorology behind this event, the initial development of isolated to scattered thunderstorms during the mid-late afternoon hours occurred in separate areas slightly off to  the north and also west of South Central Nebraska, with this early activity gradually increasing in both coverage/intensity as it evolved into the local area. In the mid-upper levels, forcing was fairly weak, featuring only subtle shortwave energy working into the region in west-northwest flow, directed around the northeastern periphery of a large-scale ridge centered over the Four Corners region. At the surface, there were also no significant features of note locally, with most of South Central Nebraska simply reporting 5-15 MPH east-southeasterly breezes during the afternoon. However, the initial storm development off to the north and west of the area appeared to be tied to weak convergence along a pair of subtle boundaries. Despite the aforementioned weak forcing and also weak mid level lapse rates, the environment featured plentiful low level moisture/instability and seasonably-decent deep layer wind shear of 30-40 knots. Ahead of the incoming storms, late afternoon temperatures in the upper 80s-low 90s (F) and dewpoints in the upper 60s-mid 70s promoted mixed-layer CAPE 2000-3000 J/kg. Some tree branches were downed in Trumbull, with power outages also reported.", "ts_dict_index": [7932, 7933, 7934]}
+{"event_id": 1045518, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-07-16 21:39:00", "end_date_time": "2022-07-16 21:39:00", "narrative": "Several strong to severe thunderstorms, some that eventually merged into a compact mesoscale convective system (MCS), rumbled southeastward across various parts of South Central Nebraska mainly between 6:30-11:30 p.m. CDT on this Saturday evening, prompting assorted reports of large hail (up to baseball size) and damaging winds (estimated up to 80 MPH) and disrupting activities at a handful of local county fairs. The most prominent narrow swath of severe activity cut through the heart of the 24-county area, focusing within 10 miles either side of a line extending from Ord-Cairo-Hastings-Davenport as an initially isolated supercell merged with a separate cluster of severe storms to its west, forming the aforementioned MCS. During it's more supercellular phase near/north of the Highway 92 corridor (mainly 6:30-8:30 p.m. CDT), a combo of both damaging winds and large hail occurred, featuring measured gusts as high as 74 MPH at Ord airport and hail ranging from golf ball to baseball size particularly within western Howard and far northwestern Hall counties. In Howard County, a stripe of significant damage to crops and windows/siding was noted from around Farwell to west of Dannebrog. As this MCS reached areas near/south of Interstate 80 (primarily 9-11 p.m. CDT) the hail threat waned but damaging winds continued, evidenced by a measured 58 MPH gust at Hastings airport and unofficial mesonet-measured gusts of 67 MPH near Nelson and 62 MPH near Davenport. Within Clay County, tree branches were downed in several communities including Trumbull, Deweese, Fairfield and Edgar. Shortly before this storm complex exited the local area to the southeast between 11:00-11:30 p.m. CDT, wind intensity ramped down to slightly sub-severe levels within southern/eastern Thayer County. Although far from the only outdoor event interruption of the evening within South Central Nebraska, one of the more noteworthy ones associated with this MCS involved the Adams County Fairfest in Hastings, where an ongoing Nelly concert was cut short and an evacuation of the grounds was successfully initiated shortly before the storm struck. Although rain totals of 1-2 inches were common within the heart of the MCS track (overall highest inF Clay County), any flooding was of the very short term/nuisance variety. To the west of the aforementioned primary swath of severe weather, a few separate and smaller-scale areas of strong to severe storms impacted portions of primarily Furnas, Buffalo and Dawson counties mainly between 7-9 p.m. CDT. In Furnas County, a relatively small but intense supercell roamed northern and eastern parts of the county, with estimated 80 MPH winds destroying an outbuilding and grain bin at a farmstead between Holbrook and Arapahoe. Meanwhile, other semi-discrete convection within parts of Buffalo/Dawson counties yielded a few wind reports including a mesonet-measured 64 MPH gust near Kearney and a slightly sub-severe 54 MPH speed near Lexington. The eastern reaches of this activity eventually merged with the primary MCS as it charged across the I-80 corridor and into the Hastings area. ||Finishing with some details regarding the evolution and meteorology behind this event, the initial development of isolated to scattered thunderstorms during the mid-late afternoon hours occurred in separate areas slightly off to  the north and also west of South Central Nebraska, with this early activity gradually increasing in both coverage/intensity as it evolved into the local area. In the mid-upper levels, forcing was fairly weak, featuring only subtle shortwave energy working into the region in west-northwest flow, directed around the northeastern periphery of a large-scale ridge centered over the Four Corners region. At the surface, there were also no significant features of note locally, with most of South Central Nebraska simply reporting 5-15 MPH east-southeasterly breezes during the afternoon. However, the initial storm development off to the north and west of the area appeared to be tied to weak convergence along a pair of subtle boundaries. Despite the aforementioned weak forcing and also weak mid level lapse rates, the environment featured plentiful low level moisture/instability and seasonably-decent deep layer wind shear of 30-40 knots. Ahead of the incoming storms, late afternoon temperatures in the upper 80s-low 90s (F) and dewpoints in the upper 60s-mid 70s promoted mixed-layer CAPE 2000-3000 J/kg. A wind gust of 62 MPH was measured by a mesonet station located one mile south-southeast Davenport.", "ts_dict_index": [7935, 7936, 7937]}
+{"event_id": 837300, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2019-06-21 04:50:00", "end_date_time": "2019-06-21 04:50:00", "narrative": "The overall most significant, widespread damaging wind event of the 2019 convective season wrought havoc across much of South Central Nebraska between the late evening of Thursday the 20th and around sunrise on Friday the 21st. The culprits were two separate linear mesoscale convective systems (MCS), with the first one by far the most impactful. This first storm complex, which traversed the area between 10:30 p.m. and 3 a.m. CDT, produced a swath of damaging winds ranging anywhere from 60 up to around 90 MPH, particularly within a corridor centered roughly 15 miles either side of a line from Cambridge-Minden-Hastings-Sutton. Within this area, there were countless reports of damage, particularly to the likes of trees (many large trees uprooted), power poles/lines and irrigation pivots, but also to some structures (mainly rural outbuildings). A short list of some of the hardest-hit communities included: Arapahoe, Oxford, Kenesaw and Hastings, with Hastings likely enduring its most widespread tree damage in roughly five years. As just a few specific instances of damage and/or measured winds: a grain bin and outbuilding were destroyed near Holbrook with irrigation pipe blown up to one-half mile; an unofficial mesonet gusted to 95 MPH near Oxford; several farm outbuildings were damaged/destroyed near Phillips with sheet metal hanging in trees. Within the Tri Cities, Hastings clearly bore the brunt of wind issues, as Grand Island and Kearney only received a glancing blow of sub-severe gusts mainly in the 40-55 MPH range. However, some places outside of the main damage swath still weren't spared from storm impacts, including in Farwell, where a lightning-induced fire damaged a portion of the fire hall. This primary linear MCS exhibited impressive radar signatures including a bookend vortex and rear inflow notch, with the system as a whole taking on a notable S-shape on reflectivity. As the initial MCS began departing the local area into eastern Nebraska, a second round of storms got underway back to the west, in response to lift above the residual cold pool. Although not nearly as intense/organized as the earlier system, this convection congealed into a northeast-southwest oriented MCS as it entered southwestern counties such as Furnas/Gosper/Harlan between 3:30-4:30 a.m. CDT. For a while, this second system remained slightly sub-severe, with peak gusts only to around 50 MPH (including 53 MPH at Hastings airport). However, some intensification to marginally-severe levels occurred between 5:30-6:30 a.m. CDT in far southeast counties, evidenced by mesonet wind gusts of 67 MPH near Superior and 60 MPH at Davenport. The back edge of this second MCS departed the local area out of Thayer County by 7 a.m. CDT, finally ending the rocky night. ||Interestingly, severe-criteria hail was very limited during this event, taking a clear backseat to damaging winds. However, a few quarter size stones were reported in and near communities such as Cambridge and Nelson. The Cambridge area was likely the hardest-hit, as copious amounts of mainly small hail combined with winds to promote fairly extensive crop damage. Rainfall-wise, the majority of South Central Nebraska measured between 0.50-1.50, holding flooding issues at bay. However, there were limited corridors of 2-3+, particularly within parts of Furnas/Gosper/Phelps counties. Including more rain that fell on the morning of the 22nd, Thayer County actually dealt with some of the worst flooding issues in the ensuing few days, such as water over several rural roads and a bridge washout north of Chester. ||Looking at the meteorological setup, this was a fairly classic recipe for intense overnight convection in the Central Plains. In the mid-upper levels, seasonably-strong, west-southwesterly flow was in place, downstream from a large-scale trough centered over the Northern Rockies. At the surface, South Central Nebraska resided just north of a west-east oriented front stretched near the Kansas border. As a low-amplitude disturbance entered southern Nebraska during the evening, this forcing combined with a very unstable airmass and increasing moisture convergence within the exit region of a 30-40 knot southerly low level jet to spark the MCS activity. By late-night standards, it was a fairly volatile mesoscale environment, featuring 2000-4000 J/kg most-unstable CAPE and 30-40 knots of deep-layer wind shear. A wind gust of 60 MPH was measured by a mesonet station located in Davenport.", "ts_dict_index": [7944, 7945, 7946]}
+{"event_id": 1045504, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-07-16 20:24:00", "end_date_time": "2022-07-16 20:24:00", "narrative": "Several strong to severe thunderstorms, some that eventually merged into a compact mesoscale convective system (MCS), rumbled southeastward across various parts of South Central Nebraska mainly between 6:30-11:30 p.m. CDT on this Saturday evening, prompting assorted reports of large hail (up to baseball size) and damaging winds (estimated up to 80 MPH) and disrupting activities at a handful of local county fairs. The most prominent narrow swath of severe activity cut through the heart of the 24-county area, focusing within 10 miles either side of a line extending from Ord-Cairo-Hastings-Davenport as an initially isolated supercell merged with a separate cluster of severe storms to its west, forming the aforementioned MCS. During it's more supercellular phase near/north of the Highway 92 corridor (mainly 6:30-8:30 p.m. CDT), a combo of both damaging winds and large hail occurred, featuring measured gusts as high as 74 MPH at Ord airport and hail ranging from golf ball to baseball size particularly within western Howard and far northwestern Hall counties. In Howard County, a stripe of significant damage to crops and windows/siding was noted from around Farwell to west of Dannebrog. As this MCS reached areas near/south of Interstate 80 (primarily 9-11 p.m. CDT) the hail threat waned but damaging winds continued, evidenced by a measured 58 MPH gust at Hastings airport and unofficial mesonet-measured gusts of 67 MPH near Nelson and 62 MPH near Davenport. Within Clay County, tree branches were downed in several communities including Trumbull, Deweese, Fairfield and Edgar. Shortly before this storm complex exited the local area to the southeast between 11:00-11:30 p.m. CDT, wind intensity ramped down to slightly sub-severe levels within southern/eastern Thayer County. Although far from the only outdoor event interruption of the evening within South Central Nebraska, one of the more noteworthy ones associated with this MCS involved the Adams County Fairfest in Hastings, where an ongoing Nelly concert was cut short and an evacuation of the grounds was successfully initiated shortly before the storm struck. Although rain totals of 1-2 inches were common within the heart of the MCS track (overall highest inF Clay County), any flooding was of the very short term/nuisance variety. To the west of the aforementioned primary swath of severe weather, a few separate and smaller-scale areas of strong to severe storms impacted portions of primarily Furnas, Buffalo and Dawson counties mainly between 7-9 p.m. CDT. In Furnas County, a relatively small but intense supercell roamed northern and eastern parts of the county, with estimated 80 MPH winds destroying an outbuilding and grain bin at a farmstead between Holbrook and Arapahoe. Meanwhile, other semi-discrete convection within parts of Buffalo/Dawson counties yielded a few wind reports including a mesonet-measured 64 MPH gust near Kearney and a slightly sub-severe 54 MPH speed near Lexington. The eastern reaches of this activity eventually merged with the primary MCS as it charged across the I-80 corridor and into the Hastings area. ||Finishing with some details regarding the evolution and meteorology behind this event, the initial development of isolated to scattered thunderstorms during the mid-late afternoon hours occurred in separate areas slightly off to  the north and also west of South Central Nebraska, with this early activity gradually increasing in both coverage/intensity as it evolved into the local area. In the mid-upper levels, forcing was fairly weak, featuring only subtle shortwave energy working into the region in west-northwest flow, directed around the northeastern periphery of a large-scale ridge centered over the Four Corners region. At the surface, there were also no significant features of note locally, with most of South Central Nebraska simply reporting 5-15 MPH east-southeasterly breezes during the afternoon. However, the initial storm development off to the north and west of the area appeared to be tied to weak convergence along a pair of subtle boundaries. Despite the aforementioned weak forcing and also weak mid level lapse rates, the environment featured plentiful low level moisture/instability and seasonably-decent deep layer wind shear of 30-40 knots. Ahead of the incoming storms, late afternoon temperatures in the upper 80s-low 90s (F) and dewpoints in the upper 60s-mid 70s promoted mixed-layer CAPE 2000-3000 J/kg. A wind gust of 58 MPH was measured by the Hastings Airport ASOS.", "ts_dict_index": [7938, 7939, 7940]}
+{"event_id": 833548, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-06-21 00:09:00", "end_date_time": "2019-06-21 00:20:00", "narrative": "The overall most significant, widespread damaging wind event of the 2019 convective season wrought havoc across much of South Central Nebraska between the late evening of Thursday the 20th and around sunrise on Friday the 21st. The culprits were two separate linear mesoscale convective systems (MCS), with the first one by far the most impactful. This first storm complex, which traversed the area between 10:30 p.m. and 3 a.m. CDT, produced a swath of damaging winds ranging anywhere from 60 up to around 90 MPH, particularly within a corridor centered roughly 15 miles either side of a line from Cambridge-Minden-Hastings-Sutton. Within this area, there were countless reports of damage, particularly to the likes of trees (many large trees uprooted), power poles/lines and irrigation pivots, but also to some structures (mainly rural outbuildings). A short list of some of the hardest-hit communities included: Arapahoe, Oxford, Kenesaw and Hastings, with Hastings likely enduring its most widespread tree damage in roughly five years. As just a few specific instances of damage and/or measured winds: a grain bin and outbuilding were destroyed near Holbrook with irrigation pipe blown up to one-half mile; an unofficial mesonet gusted to 95 MPH near Oxford; several farm outbuildings were damaged/destroyed near Phillips with sheet metal hanging in trees. Within the Tri Cities, Hastings clearly bore the brunt of wind issues, as Grand Island and Kearney only received a glancing blow of sub-severe gusts mainly in the 40-55 MPH range. However, some places outside of the main damage swath still weren't spared from storm impacts, including in Farwell, where a lightning-induced fire damaged a portion of the fire hall. This primary linear MCS exhibited impressive radar signatures including a bookend vortex and rear inflow notch, with the system as a whole taking on a notable S-shape on reflectivity. As the initial MCS began departing the local area into eastern Nebraska, a second round of storms got underway back to the west, in response to lift above the residual cold pool. Although not nearly as intense/organized as the earlier system, this convection congealed into a northeast-southwest oriented MCS as it entered southwestern counties such as Furnas/Gosper/Harlan between 3:30-4:30 a.m. CDT. For a while, this second system remained slightly sub-severe, with peak gusts only to around 50 MPH (including 53 MPH at Hastings airport). However, some intensification to marginally-severe levels occurred between 5:30-6:30 a.m. CDT in far southeast counties, evidenced by mesonet wind gusts of 67 MPH near Superior and 60 MPH at Davenport. The back edge of this second MCS departed the local area out of Thayer County by 7 a.m. CDT, finally ending the rocky night. ||Interestingly, severe-criteria hail was very limited during this event, taking a clear backseat to damaging winds. However, a few quarter size stones were reported in and near communities such as Cambridge and Nelson. The Cambridge area was likely the hardest-hit, as copious amounts of mainly small hail combined with winds to promote fairly extensive crop damage. Rainfall-wise, the majority of South Central Nebraska measured between 0.50-1.50, holding flooding issues at bay. However, there were limited corridors of 2-3+, particularly within parts of Furnas/Gosper/Phelps counties. Including more rain that fell on the morning of the 22nd, Thayer County actually dealt with some of the worst flooding issues in the ensuing few days, such as water over several rural roads and a bridge washout north of Chester. ||Looking at the meteorological setup, this was a fairly classic recipe for intense overnight convection in the Central Plains. In the mid-upper levels, seasonably-strong, west-southwesterly flow was in place, downstream from a large-scale trough centered over the Northern Rockies. At the surface, South Central Nebraska resided just north of a west-east oriented front stretched near the Kansas border. As a low-amplitude disturbance entered southern Nebraska during the evening, this forcing combined with a very unstable airmass and increasing moisture convergence within the exit region of a 30-40 knot southerly low level jet to spark the MCS activity. By late-night standards, it was a fairly volatile mesoscale environment, featuring 2000-4000 J/kg most-unstable CAPE and 30-40 knots of deep-layer wind shear. Widespread wind gusts of 60 to 65 MPH were reported in and around Hastings, with a few higher measured gusts. A wind gust of 68 MPH was measured at 1:09 AM CDT by a mesonet station located 3 miles east-southeast of Juniata, and a gust of 67 MPH was measured at 1:18 AM CDT by a mesonet station located 4 miles east-southeast of Hastings. There were numerous reports of tree limbs, at least some larger than 6 inches in diameter, downed across the area. Some trees were uprooted, including southwest of Hastings at Southern Hills Golf Course. A power line was knocked down across 12th Street in Hastings.", "ts_dict_index": [7950, 7951, 7952]}
+{"event_id": 833546, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-06-21 00:05:00", "end_date_time": "2019-06-21 00:11:00", "narrative": "The overall most significant, widespread damaging wind event of the 2019 convective season wrought havoc across much of South Central Nebraska between the late evening of Thursday the 20th and around sunrise on Friday the 21st. The culprits were two separate linear mesoscale convective systems (MCS), with the first one by far the most impactful. This first storm complex, which traversed the area between 10:30 p.m. and 3 a.m. CDT, produced a swath of damaging winds ranging anywhere from 60 up to around 90 MPH, particularly within a corridor centered roughly 15 miles either side of a line from Cambridge-Minden-Hastings-Sutton. Within this area, there were countless reports of damage, particularly to the likes of trees (many large trees uprooted), power poles/lines and irrigation pivots, but also to some structures (mainly rural outbuildings). A short list of some of the hardest-hit communities included: Arapahoe, Oxford, Kenesaw and Hastings, with Hastings likely enduring its most widespread tree damage in roughly five years. As just a few specific instances of damage and/or measured winds: a grain bin and outbuilding were destroyed near Holbrook with irrigation pipe blown up to one-half mile; an unofficial mesonet gusted to 95 MPH near Oxford; several farm outbuildings were damaged/destroyed near Phillips with sheet metal hanging in trees. Within the Tri Cities, Hastings clearly bore the brunt of wind issues, as Grand Island and Kearney only received a glancing blow of sub-severe gusts mainly in the 40-55 MPH range. However, some places outside of the main damage swath still weren't spared from storm impacts, including in Farwell, where a lightning-induced fire damaged a portion of the fire hall. This primary linear MCS exhibited impressive radar signatures including a bookend vortex and rear inflow notch, with the system as a whole taking on a notable S-shape on reflectivity. As the initial MCS began departing the local area into eastern Nebraska, a second round of storms got underway back to the west, in response to lift above the residual cold pool. Although not nearly as intense/organized as the earlier system, this convection congealed into a northeast-southwest oriented MCS as it entered southwestern counties such as Furnas/Gosper/Harlan between 3:30-4:30 a.m. CDT. For a while, this second system remained slightly sub-severe, with peak gusts only to around 50 MPH (including 53 MPH at Hastings airport). However, some intensification to marginally-severe levels occurred between 5:30-6:30 a.m. CDT in far southeast counties, evidenced by mesonet wind gusts of 67 MPH near Superior and 60 MPH at Davenport. The back edge of this second MCS departed the local area out of Thayer County by 7 a.m. CDT, finally ending the rocky night. ||Interestingly, severe-criteria hail was very limited during this event, taking a clear backseat to damaging winds. However, a few quarter size stones were reported in and near communities such as Cambridge and Nelson. The Cambridge area was likely the hardest-hit, as copious amounts of mainly small hail combined with winds to promote fairly extensive crop damage. Rainfall-wise, the majority of South Central Nebraska measured between 0.50-1.50, holding flooding issues at bay. However, there were limited corridors of 2-3+, particularly within parts of Furnas/Gosper/Phelps counties. Including more rain that fell on the morning of the 22nd, Thayer County actually dealt with some of the worst flooding issues in the ensuing few days, such as water over several rural roads and a bridge washout north of Chester. ||Looking at the meteorological setup, this was a fairly classic recipe for intense overnight convection in the Central Plains. In the mid-upper levels, seasonably-strong, west-southwesterly flow was in place, downstream from a large-scale trough centered over the Northern Rockies. At the surface, South Central Nebraska resided just north of a west-east oriented front stretched near the Kansas border. As a low-amplitude disturbance entered southern Nebraska during the evening, this forcing combined with a very unstable airmass and increasing moisture convergence within the exit region of a 30-40 knot southerly low level jet to spark the MCS activity. By late-night standards, it was a fairly volatile mesoscale environment, featuring 2000-4000 J/kg most-unstable CAPE and 30-40 knots of deep-layer wind shear. Wind gusts estimated to be near 60 MPH resulted in some tree damage in the area. A 58 MPH wind gusts was measured at 1:11 AM CDT by a mesonet station located 3 miles southwest of Prosser.", "ts_dict_index": [7947, 7948, 7949]}
+{"event_id": 845295, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-08-07 02:15:00", "end_date_time": "2019-08-07 02:30:00", "narrative": "Although its main damage swath was only about 15 miles wide, the narrow-but-intense severe storm complex that raced from northwest-to-southeast through the heart of South Central Nebraska during the pre-dawn hours on this Wednesday was one of the most impactful events of the local convective season. Quite simply, this was a nasty wind storm, packing a punch with gusts ranging from around 60 to nearly 90 MPH along and several miles either side of a line stretching from Ord-Grand Island-Hastings-Hardy. For the city of Grand Island, this was likely the overall-worst wind storm in several years, as the airport ASOS clocked a peak gust of 87 MPH. Countless trees/large branches were blown down within the city, along with several power lines, and there was also some (mainly) minor structural damage. Grand Island Emergency Center logged nearly 300 storm related incidents, including traffic hazards, power outages, alarms and fire concerns from sparking electricity. The storm also caused an (indirect) traffic fatality in rural Hall County southeast of Cairo, when a man crashed his pickup into a large, downed tree arched across a paved county road. To the south in Hastings, damage was less-severe overall, as the ASOS peak gust on the west side of town was only 70 MPH. However, stronger winds likely impacted areas just east of the city, as large trees were uprooted at Central Community College and several rail cars were reportedly blown over at a repair facility near the Clay County line. Several smaller communities also reported notable wind damage, including: Cairo, Alda, Wood River, Doniphan, Glenvil, and Fairfield. West of Clay Center, fairly extensive damage occurred on the U.S. Meat Animal Research Center campus, including broken windows and roof damage to several buildings. In addition to the aforementioned peak wind gusts at Grand Island/Hastings airports, some of the more notable unofficial (mesonet) gusts included: 85 MPH near Fairfield, 80 MPH near Alda and Wood River, 79 MPH in Doniphan and 73 MPH near Nelson. Despite the multitude of damaging wind reports, hail reports were quite scarce, as the vast majority of stones were likely dime size or smaller. Rainfall-wise, a fairly widespread coverage of 2-3 soaked several northern counties including: Valley, Greeley, Sherman, Nance and Merrick. Although resultant flooding was not very extensive in most of the area, the Mira Creek in southern Valley County breached its banks for the second time in five days, again prompting minor flooding on the north side of North Loup that continued into the early morning of the 8th.||Breaking down the timing and meteorological background of this event, it's worth noting that these South Central Nebraska damaging winds were actually the finale to a much longer swath of severe weather that initiated in southern ND and north central SD during the afternoon/evening of the 6th. Between 1-2 a.m. CDT on the 7th, the leading edge of this narrow-but-potent mesoscale convective system (MCS) entered far northern portions of the local area into Valley/Greeley counties, signaling its arrival with a 59 MPH gust at Ord airport. However, the worst was yet to come, as during the next few hours the storm complex morphed into more of an outflow-dominant, high-precipitation supercell, slamming through the Grand Island/Hastings areas between 2:30-3:30 a.m. CDT before eventually exiting Nuckolls/Thayer counties into Kansas by 5 a.m. CDT. In the wake of the main show, a few weaker clusters of storms redeveloped over parts of the area into the daylight hours, but were of little significance. In the big picture of the mid-upper levels, this event occurred within a fairly classic summertime northwest-flow regime, as the Central Plains resided northeast of an expansive ridge centered over New Mexico. At the surface, South Central Nebraska was on the backside of a weak ridge axis centered near the Nebraska-Iowa border. This promoted light-but-steady, south-southeast breezes in advance of the approaching storm complex, with surface dewpoints averaging mid-upper 60s F. Although there were question marks about how far southward into Nebraska the potential severe weather threat would extend, the combination of seasonably-stout flow aloft (deep-layer wind shear of at least 40-60 knots) and sufficient instability (mixed-layer CAPE of 1000-2000 J/kg) was clearly supportive of an intense late-night storm. Also enhancing the severe weather environment was a modest, 30 knot  southwesterly low level jet (evident at 850 millibars) and its associated low-level warm air/moisture advection. Widespread wind gusts of 70 to 85 MPH occurred along this path. A 85 MPH wind gust was measured by a mesonet station located 2 miles west-northwest of Fairfield, and a 70 MPH wind gusts was measured by a mesonet station located 2 miles north-northeast of Deweese. Building damage was reported in the Glenvil and Fairfield areas, with the COOP building in Fairfield losing an entire wall. Numerous trees and power lines were down across the Glenvil, Fairfield and Deweese areas. Several area pivots were damaged, and a grain bin collapse occurred in Fairfield. There was considerable crop damage in the area, including at the U.S. Meat Animal Research Center located west of Clay Center, where several buildings were also damaged.", "ts_dict_index": [7905, 7906, 7907]}
+{"event_id": 902714, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-07-08 22:44:00", "end_date_time": "2020-07-08 22:44:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Wind gusts estimated to be 60 to 70 MPH resulted in tree damage across Trumbull, with a few limbs ending up on homes. Power lines were also downed. Doors to the highway department's building were damaged, trapping equipment inside.", "ts_dict_index": [7965, 7966, 7967]}
+{"event_id": 833557, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-06-21 00:26:00", "end_date_time": "2019-06-21 00:26:00", "narrative": "The overall most significant, widespread damaging wind event of the 2019 convective season wrought havoc across much of South Central Nebraska between the late evening of Thursday the 20th and around sunrise on Friday the 21st. The culprits were two separate linear mesoscale convective systems (MCS), with the first one by far the most impactful. This first storm complex, which traversed the area between 10:30 p.m. and 3 a.m. CDT, produced a swath of damaging winds ranging anywhere from 60 up to around 90 MPH, particularly within a corridor centered roughly 15 miles either side of a line from Cambridge-Minden-Hastings-Sutton. Within this area, there were countless reports of damage, particularly to the likes of trees (many large trees uprooted), power poles/lines and irrigation pivots, but also to some structures (mainly rural outbuildings). A short list of some of the hardest-hit communities included: Arapahoe, Oxford, Kenesaw and Hastings, with Hastings likely enduring its most widespread tree damage in roughly five years. As just a few specific instances of damage and/or measured winds: a grain bin and outbuilding were destroyed near Holbrook with irrigation pipe blown up to one-half mile; an unofficial mesonet gusted to 95 MPH near Oxford; several farm outbuildings were damaged/destroyed near Phillips with sheet metal hanging in trees. Within the Tri Cities, Hastings clearly bore the brunt of wind issues, as Grand Island and Kearney only received a glancing blow of sub-severe gusts mainly in the 40-55 MPH range. However, some places outside of the main damage swath still weren't spared from storm impacts, including in Farwell, where a lightning-induced fire damaged a portion of the fire hall. This primary linear MCS exhibited impressive radar signatures including a bookend vortex and rear inflow notch, with the system as a whole taking on a notable S-shape on reflectivity. As the initial MCS began departing the local area into eastern Nebraska, a second round of storms got underway back to the west, in response to lift above the residual cold pool. Although not nearly as intense/organized as the earlier system, this convection congealed into a northeast-southwest oriented MCS as it entered southwestern counties such as Furnas/Gosper/Harlan between 3:30-4:30 a.m. CDT. For a while, this second system remained slightly sub-severe, with peak gusts only to around 50 MPH (including 53 MPH at Hastings airport). However, some intensification to marginally-severe levels occurred between 5:30-6:30 a.m. CDT in far southeast counties, evidenced by mesonet wind gusts of 67 MPH near Superior and 60 MPH at Davenport. The back edge of this second MCS departed the local area out of Thayer County by 7 a.m. CDT, finally ending the rocky night. ||Interestingly, severe-criteria hail was very limited during this event, taking a clear backseat to damaging winds. However, a few quarter size stones were reported in and near communities such as Cambridge and Nelson. The Cambridge area was likely the hardest-hit, as copious amounts of mainly small hail combined with winds to promote fairly extensive crop damage. Rainfall-wise, the majority of South Central Nebraska measured between 0.50-1.50, holding flooding issues at bay. However, there were limited corridors of 2-3+, particularly within parts of Furnas/Gosper/Phelps counties. Including more rain that fell on the morning of the 22nd, Thayer County actually dealt with some of the worst flooding issues in the ensuing few days, such as water over several rural roads and a bridge washout north of Chester. ||Looking at the meteorological setup, this was a fairly classic recipe for intense overnight convection in the Central Plains. In the mid-upper levels, seasonably-strong, west-southwesterly flow was in place, downstream from a large-scale trough centered over the Northern Rockies. At the surface, South Central Nebraska resided just north of a west-east oriented front stretched near the Kansas border. As a low-amplitude disturbance entered southern Nebraska during the evening, this forcing combined with a very unstable airmass and increasing moisture convergence within the exit region of a 30-40 knot southerly low level jet to spark the MCS activity. By late-night standards, it was a fairly volatile mesoscale environment, featuring 2000-4000 J/kg most-unstable CAPE and 30-40 knots of deep-layer wind shear. A wind gust of 75 MPH was measured by a mesonet station located 3 miles northwest of Inland.", "ts_dict_index": [7953, 7954, 7955]}
+{"event_id": 907615, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-07-08 22:58:00", "end_date_time": "2020-07-08 23:00:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Wind gusts were estimated to be near 65 MPH. Tree damage was reported in Clay Center, including tree limbs landing on a few homes.", "ts_dict_index": [7974, 7975, 7976]}
+{"event_id": 833559, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-06-21 00:30:00", "end_date_time": "2019-06-21 00:35:00", "narrative": "The overall most significant, widespread damaging wind event of the 2019 convective season wrought havoc across much of South Central Nebraska between the late evening of Thursday the 20th and around sunrise on Friday the 21st. The culprits were two separate linear mesoscale convective systems (MCS), with the first one by far the most impactful. This first storm complex, which traversed the area between 10:30 p.m. and 3 a.m. CDT, produced a swath of damaging winds ranging anywhere from 60 up to around 90 MPH, particularly within a corridor centered roughly 15 miles either side of a line from Cambridge-Minden-Hastings-Sutton. Within this area, there were countless reports of damage, particularly to the likes of trees (many large trees uprooted), power poles/lines and irrigation pivots, but also to some structures (mainly rural outbuildings). A short list of some of the hardest-hit communities included: Arapahoe, Oxford, Kenesaw and Hastings, with Hastings likely enduring its most widespread tree damage in roughly five years. As just a few specific instances of damage and/or measured winds: a grain bin and outbuilding were destroyed near Holbrook with irrigation pipe blown up to one-half mile; an unofficial mesonet gusted to 95 MPH near Oxford; several farm outbuildings were damaged/destroyed near Phillips with sheet metal hanging in trees. Within the Tri Cities, Hastings clearly bore the brunt of wind issues, as Grand Island and Kearney only received a glancing blow of sub-severe gusts mainly in the 40-55 MPH range. However, some places outside of the main damage swath still weren't spared from storm impacts, including in Farwell, where a lightning-induced fire damaged a portion of the fire hall. This primary linear MCS exhibited impressive radar signatures including a bookend vortex and rear inflow notch, with the system as a whole taking on a notable S-shape on reflectivity. As the initial MCS began departing the local area into eastern Nebraska, a second round of storms got underway back to the west, in response to lift above the residual cold pool. Although not nearly as intense/organized as the earlier system, this convection congealed into a northeast-southwest oriented MCS as it entered southwestern counties such as Furnas/Gosper/Harlan between 3:30-4:30 a.m. CDT. For a while, this second system remained slightly sub-severe, with peak gusts only to around 50 MPH (including 53 MPH at Hastings airport). However, some intensification to marginally-severe levels occurred between 5:30-6:30 a.m. CDT in far southeast counties, evidenced by mesonet wind gusts of 67 MPH near Superior and 60 MPH at Davenport. The back edge of this second MCS departed the local area out of Thayer County by 7 a.m. CDT, finally ending the rocky night. ||Interestingly, severe-criteria hail was very limited during this event, taking a clear backseat to damaging winds. However, a few quarter size stones were reported in and near communities such as Cambridge and Nelson. The Cambridge area was likely the hardest-hit, as copious amounts of mainly small hail combined with winds to promote fairly extensive crop damage. Rainfall-wise, the majority of South Central Nebraska measured between 0.50-1.50, holding flooding issues at bay. However, there were limited corridors of 2-3+, particularly within parts of Furnas/Gosper/Phelps counties. Including more rain that fell on the morning of the 22nd, Thayer County actually dealt with some of the worst flooding issues in the ensuing few days, such as water over several rural roads and a bridge washout north of Chester. ||Looking at the meteorological setup, this was a fairly classic recipe for intense overnight convection in the Central Plains. In the mid-upper levels, seasonably-strong, west-southwesterly flow was in place, downstream from a large-scale trough centered over the Northern Rockies. At the surface, South Central Nebraska resided just north of a west-east oriented front stretched near the Kansas border. As a low-amplitude disturbance entered southern Nebraska during the evening, this forcing combined with a very unstable airmass and increasing moisture convergence within the exit region of a 30-40 knot southerly low level jet to spark the MCS activity. By late-night standards, it was a fairly volatile mesoscale environment, featuring 2000-4000 J/kg most-unstable CAPE and 30-40 knots of deep-layer wind shear. Wind gusts were estimated to be at least 65 MPH across the area. Numerous small tree limbs were downed. Isolated larger limbs were downed, up to 8 to 10 inches in diameter in Clay Center, with a limb closer to 15 inches in diameter in Harvard that fell onto a house.", "ts_dict_index": [7956, 7957, 7958]}
+{"event_id": 907626, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-07-08 23:03:00", "end_date_time": "2020-07-08 23:03:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. A wind gust of 66 MPH was recorded by a mesonet station in Harvard. Power outages were reported in town.", "ts_dict_index": [7959, 7960, 7961]}
+{"event_id": 907639, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2020-07-08 23:15:00", "end_date_time": "2020-07-08 23:18:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. A wind gust of 66 MPH was recorded by a mesonet station located 2 miles west of Shickley. Emergency management reported roof and door damage to an outbuilding in Shickley.", "ts_dict_index": [7971, 7972, 7973]}
+{"event_id": 907656, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-07-08 23:40:00", "end_date_time": "2020-07-08 23:40:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Wind gusts estimated to be near 60 MPH caused power outages in Gilead due to a downed power line.", "ts_dict_index": [7968, 7969, 7970]}
+{"event_id": 907641, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-07-08 23:17:00", "end_date_time": "2020-07-08 23:17:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. A wind gust of 63 MPH was recorded by a mesonet station located 1 mile south-southeast of Davenport.", "ts_dict_index": [7977, 7978, 7979]}
+{"event_id": 902711, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2020-07-08 22:42:00", "end_date_time": "2020-07-08 22:42:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. A wind gust of 65 MPH was recorded by a mesonet station located 1 mile west of Trumbull.", "ts_dict_index": [7962, 7963, 7964]}
+{"event_id": 1045508, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-07-16 20:46:00", "end_date_time": "2022-07-16 20:46:00", "narrative": "Several strong to severe thunderstorms, some that eventually merged into a compact mesoscale convective system (MCS), rumbled southeastward across various parts of South Central Nebraska mainly between 6:30-11:30 p.m. CDT on this Saturday evening, prompting assorted reports of large hail (up to baseball size) and damaging winds (estimated up to 80 MPH) and disrupting activities at a handful of local county fairs. The most prominent narrow swath of severe activity cut through the heart of the 24-county area, focusing within 10 miles either side of a line extending from Ord-Cairo-Hastings-Davenport as an initially isolated supercell merged with a separate cluster of severe storms to its west, forming the aforementioned MCS. During it's more supercellular phase near/north of the Highway 92 corridor (mainly 6:30-8:30 p.m. CDT), a combo of both damaging winds and large hail occurred, featuring measured gusts as high as 74 MPH at Ord airport and hail ranging from golf ball to baseball size particularly within western Howard and far northwestern Hall counties. In Howard County, a stripe of significant damage to crops and windows/siding was noted from around Farwell to west of Dannebrog. As this MCS reached areas near/south of Interstate 80 (primarily 9-11 p.m. CDT) the hail threat waned but damaging winds continued, evidenced by a measured 58 MPH gust at Hastings airport and unofficial mesonet-measured gusts of 67 MPH near Nelson and 62 MPH near Davenport. Within Clay County, tree branches were downed in several communities including Trumbull, Deweese, Fairfield and Edgar. Shortly before this storm complex exited the local area to the southeast between 11:00-11:30 p.m. CDT, wind intensity ramped down to slightly sub-severe levels within southern/eastern Thayer County. Although far from the only outdoor event interruption of the evening within South Central Nebraska, one of the more noteworthy ones associated with this MCS involved the Adams County Fairfest in Hastings, where an ongoing Nelly concert was cut short and an evacuation of the grounds was successfully initiated shortly before the storm struck. Although rain totals of 1-2 inches were common within the heart of the MCS track (overall highest inF Clay County), any flooding was of the very short term/nuisance variety. To the west of the aforementioned primary swath of severe weather, a few separate and smaller-scale areas of strong to severe storms impacted portions of primarily Furnas, Buffalo and Dawson counties mainly between 7-9 p.m. CDT. In Furnas County, a relatively small but intense supercell roamed northern and eastern parts of the county, with estimated 80 MPH winds destroying an outbuilding and grain bin at a farmstead between Holbrook and Arapahoe. Meanwhile, other semi-discrete convection within parts of Buffalo/Dawson counties yielded a few wind reports including a mesonet-measured 64 MPH gust near Kearney and a slightly sub-severe 54 MPH speed near Lexington. The eastern reaches of this activity eventually merged with the primary MCS as it charged across the I-80 corridor and into the Hastings area. ||Finishing with some details regarding the evolution and meteorology behind this event, the initial development of isolated to scattered thunderstorms during the mid-late afternoon hours occurred in separate areas slightly off to  the north and also west of South Central Nebraska, with this early activity gradually increasing in both coverage/intensity as it evolved into the local area. In the mid-upper levels, forcing was fairly weak, featuring only subtle shortwave energy working into the region in west-northwest flow, directed around the northeastern periphery of a large-scale ridge centered over the Four Corners region. At the surface, there were also no significant features of note locally, with most of South Central Nebraska simply reporting 5-15 MPH east-southeasterly breezes during the afternoon. However, the initial storm development off to the north and west of the area appeared to be tied to weak convergence along a pair of subtle boundaries. Despite the aforementioned weak forcing and also weak mid level lapse rates, the environment featured plentiful low level moisture/instability and seasonably-decent deep layer wind shear of 30-40 knots. Ahead of the incoming storms, late afternoon temperatures in the upper 80s-low 90s (F) and dewpoints in the upper 60s-mid 70s promoted mixed-layer CAPE 2000-3000 J/kg. A wind gust of 58 MPH was measured by a mesonet station located on the north side of Hastings. A CoCoRaHS observer in the same area reported that winds blew over trash cans, a BBQ grill, and downed small tree branches.", "ts_dict_index": [7926, 7927, 7928]}
+{"event_id": 907612, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-07-08 22:55:00", "end_date_time": "2020-07-08 22:55:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Wind gusts estimated to be near 60 MPH resulted in power outages in Deweese.", "ts_dict_index": [7989, 7990, 7991]}
+{"event_id": 907602, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-07-08 22:46:00", "end_date_time": "2020-07-08 22:51:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Peak wind gusts of 72 MPH and 66 MPH were measured by a mesonet station located 4 miles east of Pauline.", "ts_dict_index": [7998, 7999, 8000]}
+{"event_id": 907651, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-07-08 23:26:00", "end_date_time": "2020-07-08 23:26:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. A wind gust of 69 MPH was recorded by a mesonet station located 3 miles east-southeast of Carleton.", "ts_dict_index": [7986, 7987, 7988]}
+{"event_id": 907606, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2020-07-08 22:48:00", "end_date_time": "2020-07-08 22:48:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Tree limbs were downed in Hastings, blocking some roads.", "ts_dict_index": [7992, 7993, 7994]}
+{"event_id": 907652, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-07-08 23:27:00", "end_date_time": "2020-07-08 23:27:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Wind gusts estimated to be near 60 MPH downed small tree branches in Deshler.", "ts_dict_index": [7995, 7996, 7997]}
+{"event_id": 907650, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-07-08 23:24:00", "end_date_time": "2020-07-08 23:24:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. A wind gust of 75 MPH was recorded by a mesonet station located in Carleton.", "ts_dict_index": [7983, 7984, 7985]}
+{"event_id": 907643, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-07-08 23:23:00", "end_date_time": "2020-07-08 23:23:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Wind gusts estimated to be near 65 MPH resulted in tree damage in Hebron, with limbs up to 4 to 6 inches in diameter being downed.", "ts_dict_index": [7980, 7981, 7982]}
+{"event_id": 907653, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2020-07-08 23:29:00", "end_date_time": "2020-07-08 23:29:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. A wind gust of 59 MPH was recorded by a mesonet station located 3 miles south of Ohiowa.", "ts_dict_index": [8025, 8026, 8027]}
+{"event_id": 907636, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2020-07-08 23:14:00", "end_date_time": "2020-07-08 23:14:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. A wind gust of 61 MPH was recorded by a mesonet station located 4 miles north-northeast of Ong.", "ts_dict_index": [8010, 8011, 8012]}
+{"event_id": 907638, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-07-08 23:15:00", "end_date_time": "2020-07-08 23:15:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. A wind gust of 66 MPH was recorded by a mesonet station located 3 miles east-northeast of Edgar.", "ts_dict_index": [8019, 8020, 8021]}
+{"event_id": 907628, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-07-08 23:05:00", "end_date_time": "2020-07-08 23:07:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Wind gusts were estimated to be near 70 MPH by a Cooperative Observer and a trained spotter. Tree damage was reported, including small trees 8 to 10 inches in diameter being snapped.", "ts_dict_index": [8004, 8005, 8006]}
+{"event_id": 907623, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-07-08 23:03:00", "end_date_time": "2020-07-08 23:05:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Tree limbs were downed in Edgar, the largest was 1 foot in diameter.", "ts_dict_index": [8022, 8023, 8024]}
+{"event_id": 907625, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-07-08 23:03:00", "end_date_time": "2020-07-08 23:03:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Wind gusts estimated to be between 65 and 70 MPH caused damage to an irrigation pivot.", "ts_dict_index": [8016, 8017, 8018]}
+{"event_id": 913259, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-08-14 17:15:00", "end_date_time": "2020-08-14 17:15:00", "narrative": "Although it only impacted a small percentage of the 24-county South Central Nebraska area, the large and intense supercell storm that marched south-southwestward for over 90 miles through several eastern counties on this Friday afternoon/early evening was likely the local area's most noteworthy individual storm of the 2020 convective season. In addition to dropping three fairly brief EF-0 tornadoes in southeastern Hamilton and northeastern Clay counties, its main calling card was large hail, with several reports of golf ball to slightly larger than baseball size stones in Clay/Nuckolls counties, and smaller hail to around quarter size as far north as Osceola. Interestingly, damaging winds were not a major player, with no ground-truth gusts in excess of 50 MPH. Focusing on specific storm reports, and starting with the three EF-0 tornadoes, they all occurred between 5-6 p.m. CDT, touching down briefly along a roughly 15-mile long corridor from near Interstate 80 a few miles south of Hampton, down to the Saronville area. Per storm surveys, the first two tornadoes were each on the ground for roughly 2 miles. While the majority of minor damage was confined to crops and trees, a lean-to shed was destroyed and a pivot overturned. As for the hail, the largest reported was 3 diameter between Clay Center and Harvard, but towns including Sutton and Nelson endured stones to at least tennis ball size. Flooding was not much of an issue, as the storm was progressive enough to keep rainfall amounts largely under one inch. ||Breaking down the meteorological background and event timing, this was actually a fairly conditional severe weather setup for South Central Nebraska, with various pros and cons for/against robust activity. In the mid-upper levels, the local area resided a fair distance south of a vigorous shortwave trough swinging across the Dakotas towards northern MN, resulting in fairly limited forcing aloft. Also working against convection (especially widespread severe) was a plume of warm mid level temperatures, with 700 millibar values of 12-14C providing a healthy cap. On the other hand, low-level forcing was seasonably-strong, as a well-defined cold front slid southeastward into the area during the afternoon. Ahead of this boundary, a significantly-unstable airmass awaited, featuring temperatures in the upper 80s-low 90s F/dewpoints upper 60s-mid 70s F, yielding formidable mixed-layer CAPE around 4000 J/kg. This extreme instability, in the presence of sufficient deep-layer wind shear around 35 knots, clearly fostered a mesoscale environment capable of stout convection. As for what actually transpired, the main show was preceded by a broken line of non-severe, likely elevated storms that passed primarily through counties south of Interstate 80 and east of Highway 281 between 12:30-3:30 p.m. CDT. About the time this innocuous early afternoon activity was departing the local area to the southeast, a broken line of true, surface-based storms got going along the front in northeast Nebraska, with the southwestern-most cell building down into the far northeast corner of South Central Nebraska (eastern Nance/northeast Merrick/northern Polk counties) between 3-4 p.m. CDT. Within an hour thereafter, this tail end Charlie storm rapidly grew into a full-blown supercell over Polk/northern York counties, producing its first marginally-severe hail reports. During the following two hours (5-7 p.m. CDT), the storm anchored itself firmly to the surface front, with new updraft generation along its western edge promoting more of a southwestward propagation and causing it to grow larger in both intensity/size, becoming more of a supercell cluster. It was during this time that the brief tornadoes occurred along the storm's far western flank, likely driven by pronounced low-level vorticity stretching along the surface front. While the sporadic tornado touchdowns were brief, the storm continued to be a prolific hail-producer as it gradually exited the local area out of Nuckolls County into northern Kansas between 7-8 p.m. CDT, ending all South Central Nebraska convection for the night. Wind gusts were estimated to be near 60 MPH.", "ts_dict_index": [8028, 8029, 8030]}
+{"event_id": 907654, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-07-08 23:30:00", "end_date_time": "2020-07-08 23:30:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. A wind gust of 60 MPH was recorded by a mesonet station located 6 miles south-southeast of Davenport.", "ts_dict_index": [8001, 8002, 8003]}
+{"event_id": 898901, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2020-07-10 23:58:00", "end_date_time": "2020-07-11 00:05:00", "narrative": "Two rounds of severe weather affected portions of south central Nebraska and north central Kansas the evening of July 10th into the early morning hours of July 11th. For the first round, thunderstorms initially formed near the South Dakota and Nebraska border during the early afternoon hours, then shifted southeast into central Nebraska and eventually the northwest portions of the GID CWA during the late afternoon and early evening. Most of the severe reports were associated with an intense supercell on the southwestern flank of a line of thunderstorms. This supercell tracked from just south of Valentine to Broken Bow before it entered the local area in Buffalo and Sherman Counties around 5:30PM CDT. Multiple reports of 50-60mph wind gusts were received, along with 5 ft tall corn being blown over in northern Buffalo County. This thunderstorm continued southeast and impacted Kearney with 60-70mph winds, including a 61mph gust at the Kearney Airport. Additional severe wind reports, and even some quarter to half dollar size hail, occurred in Kearney County before the system weakened as it neared the state line during the late evening. These thunderstorms were supported by MLCAPE values of 2000-3000 J/kg, steep mid level lapse rates, and very strong effective shear of 50-60kt. ||The next round of thunderstorms brought high winds to central and northern portions of the area between 11PM CDT on the 10th, and 1AM CDT on the 11th. This round of severe weather actually stemmed from thunderstorms that developed well northwest of the area, across southeast Montana and northeast Wyoming, during the afternoon hours of July 10th. Weakening had been noted around midnight as the leading edge shifted into the northwest CWA, likely impacted by the remnant cool, drier outflow from the first wave resulting in decreasing surface based instability and increasing inhibition. However, a mesohigh quickly developed over north central Nebraska, which resulted in a rapidly increasing low level pressure gradient force and strong pressure rises. In fact, pressure rises on the order of 8-9mb/2 hr were noted at both Ord and Grand Island ASOSs. The pressure rises allowed strong wind to develop, despite an overall weakening trend within the convection itself. Multiple reports of 55-65mph wind gusts occurred with this second round of activity, impacting areas from Ord to Hastings, including Grand Island, east to the York area. The strong winds resulted in numerous downed tree branches and power lines. The pressure gradient and wind gusts gradually relaxed after 1AM, and any additional gusts remained sub severe.||The next round of thunderstorms brought high winds to central and northern portions of the area between 11PM CDT on the 10th, and 1AM CDT on the 11th. This round of severe weather actually stemmed from thunderstorms that developed well northwest of the area, across southeast Montana and northeast Wyoming, during the afternoon hours of July 10th. Weakening had been noted around midnight as the leading edge shifted into the northwest CWA, likely impacted by the remnant cool, drier outflow from the first wave. However, a mesohigh quickly developed over north central Nebraska, which resulted in a rapidly increasing low level pressure gradient force and strong pressure rises. In fact, rises on the order of 8-9mb/2 hr were noted at both Ord and Grand Island ASOSs. The pressure rises allowed strong wind to develop, despite an overall weakening trend within the convection itself. Multiple reports of 55-65mph wind gusts occurred with this second round of activity, impacting areas from Ord to Hastings, including Grand Island, east to the York area. The strong winds resulted in numerous downed tree branches and power lines. Wind gusts between 60 and 65 MPH affected locations in and around Hastings, with a 62 MPH gusts recorded by the Hastings Airport ASOS at 12:58 AM CDT. Emergency management reported numerous large tree branches downed across town. One power pole was broken, causing a tree fire in the Hastings College area. A power line was knocked down over 3rd Street on the west side of town.", "ts_dict_index": [8031, 8032, 8033]}
+{"event_id": 902708, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2020-07-08 22:40:00", "end_date_time": "2020-07-08 22:40:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Wind gusts were estimated to be near 60 MPH at the NWS Hastings office.", "ts_dict_index": [8013, 8014, 8015]}
+{"event_id": 839952, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-06-21 00:14:00", "end_date_time": "2019-06-21 00:14:00", "narrative": "The overall most significant, widespread damaging wind event of the 2019 convective season wrought havoc across much of South Central Nebraska between the late evening of Thursday the 20th and around sunrise on Friday the 21st. The culprits were two separate linear mesoscale convective systems (MCS), with the first one by far the most impactful. This first storm complex, which traversed the area between 10:30 p.m. and 3 a.m. CDT, produced a swath of damaging winds ranging anywhere from 60 up to around 90 MPH, particularly within a corridor centered roughly 15 miles either side of a line from Cambridge-Minden-Hastings-Sutton. Within this area, there were countless reports of damage, particularly to the likes of trees (many large trees uprooted), power poles/lines and irrigation pivots, but also to some structures (mainly rural outbuildings). A short list of some of the hardest-hit communities included: Arapahoe, Oxford, Kenesaw and Hastings, with Hastings likely enduring its most widespread tree damage in roughly five years. As just a few specific instances of damage and/or measured winds: a grain bin and outbuilding were destroyed near Holbrook with irrigation pipe blown up to one-half mile; an unofficial mesonet gusted to 95 MPH near Oxford; several farm outbuildings were damaged/destroyed near Phillips with sheet metal hanging in trees. Within the Tri Cities, Hastings clearly bore the brunt of wind issues, as Grand Island and Kearney only received a glancing blow of sub-severe gusts mainly in the 40-55 MPH range. However, some places outside of the main damage swath still weren't spared from storm impacts, including in Farwell, where a lightning-induced fire damaged a portion of the fire hall. This primary linear MCS exhibited impressive radar signatures including a bookend vortex and rear inflow notch, with the system as a whole taking on a notable S-shape on reflectivity. As the initial MCS began departing the local area into eastern Nebraska, a second round of storms got underway back to the west, in response to lift above the residual cold pool. Although not nearly as intense/organized as the earlier system, this convection congealed into a northeast-southwest oriented MCS as it entered southwestern counties such as Furnas/Gosper/Harlan between 3:30-4:30 a.m. CDT. For a while, this second system remained slightly sub-severe, with peak gusts only to around 50 MPH (including 53 MPH at Hastings airport). However, some intensification to marginally-severe levels occurred between 5:30-6:30 a.m. CDT in far southeast counties, evidenced by mesonet wind gusts of 67 MPH near Superior and 60 MPH at Davenport. The back edge of this second MCS departed the local area out of Thayer County by 7 a.m. CDT, finally ending the rocky night. ||Interestingly, severe-criteria hail was very limited during this event, taking a clear backseat to damaging winds. However, a few quarter size stones were reported in and near communities such as Cambridge and Nelson. The Cambridge area was likely the hardest-hit, as copious amounts of mainly small hail combined with winds to promote fairly extensive crop damage. Rainfall-wise, the majority of South Central Nebraska measured between 0.50-1.50, holding flooding issues at bay. However, there were limited corridors of 2-3+, particularly within parts of Furnas/Gosper/Phelps counties. Including more rain that fell on the morning of the 22nd, Thayer County actually dealt with some of the worst flooding issues in the ensuing few days, such as water over several rural roads and a bridge washout north of Chester. ||Looking at the meteorological setup, this was a fairly classic recipe for intense overnight convection in the Central Plains. In the mid-upper levels, seasonably-strong, west-southwesterly flow was in place, downstream from a large-scale trough centered over the Northern Rockies. At the surface, South Central Nebraska resided just north of a west-east oriented front stretched near the Kansas border. As a low-amplitude disturbance entered southern Nebraska during the evening, this forcing combined with a very unstable airmass and increasing moisture convergence within the exit region of a 30-40 knot southerly low level jet to spark the MCS activity. By late-night standards, it was a fairly volatile mesoscale environment, featuring 2000-4000 J/kg most-unstable CAPE and 30-40 knots of deep-layer wind shear. Wind gusts were estimated to be near 65 MPH.", "ts_dict_index": [7941, 7942, 7943]}
+{"event_id": 968160, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-06-22 20:20:00", "end_date_time": "2021-06-22 20:20:00", "narrative": "While the majority of South Central Nebraska enjoyed a seasonably-warm and tranquil Tuesday evening, it was a different story within a few far northeastern/east-central counties, where a pair of somewhat high-based supercells advanced south-southeastward, leaving behind swaths of mainly large hail but also more localized damaging winds. The first of these intense storms entered the local area into far eastern Nance County shortly after 7 p.m. CDT, striking Genoa and vicinity with a combination of estimated 70 MPH winds and nickel to quarter size hail. Around 8 p.m. CDT it reached central Polk County, pummeling the Osceola area with several minutes of hail up to 2 inches in diameter. An NeRAIN observer seven miles north of Osceola reported significantly stripped corn and that house flowers are now sticks. The supercell continued into eastern York County, still producing hail up to golf ball size in Thayer and ping pong balls east of McCool Junction. Around 9:30 p.m. CDT a weakening trend had commenced, but not before the storm brushed northeast Fillmore County on its way out of the local area and blew down a few tree branches near Exeter. Meanwhile, about 60 miles back to the northwest, another supercell somewhat-unexpectedly fired up over northern Nance County around 9 p.m. CDT. This storm was not as proficient of a large hail producer as its predecessor (largest reported was quarter size near Clarks and Hordville), but it packed more of a wind punch as its core started collapsing over the Hamilton-York County line between 10-10:30 p.m. CDT. Most notably, estimated 70 MPH gusts blew over a semi truck on Interstate 80 near the Hampton exit and also damaged a roof and broke power poles near Bradshaw. Shortly thereafter, this second supercell began dissipating, fading from radar over southeastern Fillmore County around 1130 p.m. CDT and bringing an end to all convection for the night. ||Forecast-wise, this was considered an all-or-nothing setup for South Central Nebraska in the early morning local forecast discussion, as some computer models correctly predicted the presence of supercells locally, while others insisted that all regional convection would focus at least slightly east-northeast of the area altogether. This uncertainty was understandable given various pros and cons at play. One of the biggest pros for robust supercell development was seasonably-strong deep layer wind shear of 40-50 knots, as the area resided under pronounced northwesterly flow within the interface between an expansive ridge over the southwestern states and a deep southeast Canada trough. As for cons, they were mainly highlighted by seasonably-unimpressive low level moisture and resultant instability. Although afternoon temperatures soared to around 90 (F) to the south of a west-east oriented warm front across northeast Nebraska, dewpoints along the front struggled to reach the low-60s during peak heating, yielding fairly modest mixed-layer CAPE no higher than 1000-1500 J/kg. Ultimately though, persistent low-level convergence along the intersection of the  aforementioned warm front and a subtle, northeast-southwest oriented trough proved sufficient to spark convective initiation as early as 4 p.m. CDT about 60 miles to the north of South Central Nebraska. This early convection drifted more eastward initially, but eventually dove more southward as it intensified, allowing the first supercell to infiltrate far northeastern local counties. For a while it appeared this would be South Central Nebraska's only severe storm of the evening, but the second one likely ignited as the onset of a southwesterly low level jet converged into the first storm's trailing outflow. Wind gusts estimated to be near 60 MPH resulted in some tree limbs of 2-4 inches in diameter blown down onto Highway 6.", "ts_dict_index": [8034, 8035, 8036]}
+{"event_id": 919288, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:30:00", "end_date_time": "2020-08-10 10:30:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Public report of a 77 mph peak wind gust from a Davis home weather station. Tree branches two to three inches in diameter broke and a 4 inch tree broke off at the ground.", "ts_dict_index": [8061, 8062, 8063]}
+{"event_id": 919006, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:13:00", "end_date_time": "2020-08-10 10:13:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. WHO TV relayed a report that part of the Buccaneers Arena roof was blown off.", "ts_dict_index": [8070, 8071, 8072]}
+{"event_id": 919008, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:14:00", "end_date_time": "2020-08-10 10:14:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. A trained spotter reported large tree branches down.", "ts_dict_index": [8064, 8065, 8066]}
+{"event_id": 919014, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:16:00", "end_date_time": "2020-08-10 10:16:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Public report of a fence blown down at 128th and Douglas.", "ts_dict_index": [8058, 8059, 8060]}
+{"event_id": 918990, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:12:00", "end_date_time": "2020-08-10 10:12:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. WOI TV relayed a report of trees down and damage to roofs.", "ts_dict_index": [8073, 8074, 8075]}
+{"event_id": 965364, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-07-30 03:07:00", "end_date_time": "2021-07-30 03:07:00", "narrative": "A strong low pressure system was present over the Great Lakes region to start the day on July 29th. From this extended a cold front to the southwest. As the low pressure continued eastward throughout the day, the cold front slowly shifted farther southward, before becoming elongated and slowing just north of the Ohio River. This kept much of Kentucky in the warm sector, with a strong push of warm/moist tropical air into the region. The front finally began to dip below the Ohio River as we headed into the overnight hours and transitioned to July 30th. SPC had us in a slight risk for severe thunderstorms, as showers and thunderstorms formed ahead of this frontal boundary. Many of these storms lead to heavy rainfall, and resulted in multiple instances of flash flooding. High winds were also a threat, as two severe thunderstorm warnings were issued, and numerous reports of wind damage were obtained. There was even enough low level rotation in one storm to constitute a tornado warning during the early morning hours on the 30th. Thankfully there were no reports from this.||Rainfall amounts from this event are summarized below:||...PRECIPITATION REPORTS...||Location                     Amount    Time/Date       Lat/Lon              |2 SSE Farmers           4.58 in   0700 AM 07/30   38.12N/83.53W        |1 SSE Stanton           4.22 in   0800 AM 07/30   37.83N/83.85W        |Koomer Ridge            4.20 in   1200 PM 07/30   37.78N/83.63W        |Peeled Oak                3.84 in   1200 PM 07/30   38.07N/83.80W        |0.8 NW Cannel City    3.63 in   1200 PM 07/30   37.80N/83.28W        |2 E Clay City              3.52 in   0700 AM 07/30   37.86N/83.90W        |2 NNW Loam              3.36 in   0800 AM 07/30   37.43N/84.14W        |Owingsville 4 S           3.23 in   1200 PM 07/30   38.09N/83.76W        |Waltersville                3.20 in   0700 AM 07/30   37.87N/83.93W        |Somerset 7 NNE         3.12 in   1200 PM 07/30   37.18N/84.56W        |1 WSW Clover Bottom 3.10 in   0800 AM 07/30   37.49N/84.17W        |1 NNW Owingsville      2.95 in   0800 AM 07/30   38.14N/83.76W        |Maytown                    2.92 in   1200 PM 07/30   37.85N/83.47W        |2 WNW Rockcastle Springs     2.76 in   0700 AM 07/30   37.02N/84.34W        |Wades Mill                 2.76 in   1200 PM 07/30   38.03N/84.02W        |1 S Paxton                 2.74 in   0700 AM 07/30   37.66N/83.41W        |1 S Paxton                 2.74 in   0700 AM 07/30   37.66N/83.41W        |2 NNE Mount Olive     2.72 in   0900 AM 07/30   37.63N/83.72W        |Buckner Branch         2.49 in   1200 PM 07/30   38.35N/83.40W        |Mt Sterling                2.45 in   1200 PM 07/30   38.03N/83.97W        |Peabody                   2.44 in   1200 PM 07/30   37.14N/83.58W        |Willailla                    2.35 in   0700 AM 07/30   37.30N/84.46W        |Whitley City 3 N       2.34 in   1200 PM 07/30   36.77N/84.48W        |1.2 W Jackson          2.28 in   1200 PM 07/30   37.55N/83.40W        |Judy                        2.24 in   0700 AM 07/30   38.13N/83.96W        |2.0 NE Monticello      2.22 in   1200 PM 07/30   36.87N/84.83W        |0.9 NW Wendover     2.20 in   1200 PM 07/30   37.14N/83.37W        |1.7 SE Ringos Mills   2.19 in   1200 PM 07/30   38.25N/83.59W        |1 ENE Gates             2.16 in   0709 AM 07/30   38.24N/83.34W        |McKee 5 S                2.10 in   1200 PM 07/30   37.36N/83.97W        |2 ESE Grassy Lick     2.09 in   0730 AM 07/30   38.07N/83.99W        |1.2 S Grassy Creek   2.01 in   1200 PM 07/30   37.85N/83.35W        |Cressy                     2.01 in   0800 AM 07/30   37.83N/84.04W  ||End of summary. A tree was blown down onto Public Road in the 5500 block near Bloss.", "ts_dict_index": [8040, 8041, 8042]}
+{"event_id": 901344, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-06-28 01:15:00", "end_date_time": "2020-06-28 01:15:00", "narrative": "This was an active late Saturday evening-early Sunday morning of thunderstorms across much of South Central Nebraska, featuring several reports of large hail and especially damaging winds mainly between midnight-3 a.m. CDT as two storm complexes rolled through and eventually merged. Focusing first on severe winds, most estimated or measured gusts were in the 50-70 MPH range and associated with primarily tree damage. However a few isolated structural damage reports were more suggestive of at least 75-80 MPH, including: 1) 10 power poles blown down and three grain bins destroyed (along with some overturned irrigation pivots) west of Aurora...2) grain bin damage and overturned pivots north of Minden. Hail was more limited overall, but stones reached golf ball size at Pauline and ping pong ball size in Davenport, while Hastings saw nickel to quarter size hail. Rainfall amounts varied considerably (most of South Central Nebraska had less than one-half inch), but a fairly narrow swath of at least 1.50-2.50 targeted parts of primarily Thayer/Nuckolls/Clay counties, with one unofficial report as high as 3.17 near Belvidere. Flooding was fairly minimal, although one rural road along the Fillmore/Thayer County line still had water running across it around sunrise. ||As for storm mode/evolution, this was a somewhat complex event. The first local convection of the night entered the Furnas County area out of northwest Kansas after 11 p.m. CDT, in the form of a compact linear mesoscale convective system (MCS) on a weakening trend. But then, between midnight-1 a.m. CDT, a broken band of intense, semi-discrete storms erupted out ahead of this MCS along a west-east axis centered from Phelps-Adams-Thayer counties (likely in response to the onset of a healthy low level jet). However, these initially semi-discrete storms (which accounted for all large hail reports) quickly consolidated/grew upscale into a new linear MCS that charged north-northeast across the Highway 6/Interstate 80 corridors between 1-2 a.m. CDT, gradually merging with the initial MCS racing up from the southwest in the process. During the ensuing hour, the two complexes completed a full merger; the northern end weakening as it reached far northeastern counties (such as Nance/Polk), while the southern end remained severe through Fillmore/Thayer counties before departing the local area into southeast Nebraska. This ended any severe threat for the night, although weaker storms and broader showers persisted until around sunrise in some spots. This was a ripe setup for severe nocturnal storms, especially with the exit region of a 30-40 knot southerly low level jet (evident at 850 millibars) aimed into the heart of South Central Nebraska after dark, and tapping into a large reservoir of most-unstable CAPE as high as 2000-3000 J/kg. In the mid-upper levels, flow over the region was not overly-strong, but contained various low-amplitude disturbances and was in the process of transitioning more southwesterly in response to a larger-scale trough setting up over the northwestern United States. There were no distinct surface features across the local area, but steady light southeast breezes prior to storm initiation maintained seasonably-high dewpoints in the mid-60s to low-70 F. Likely one of the main limiting factors against a more robust severe threat was only modest deep-layer wind shear around 30 knots. Wind gusts were estimated to be near 60 MPH, knocking down numerous tree branches up to 3 inches in diameter.", "ts_dict_index": [8052, 8053, 8054]}
+{"event_id": 965365, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-07-30 03:17:00", "end_date_time": "2021-07-30 03:17:00", "narrative": "A strong low pressure system was present over the Great Lakes region to start the day on July 29th. From this extended a cold front to the southwest. As the low pressure continued eastward throughout the day, the cold front slowly shifted farther southward, before becoming elongated and slowing just north of the Ohio River. This kept much of Kentucky in the warm sector, with a strong push of warm/moist tropical air into the region. The front finally began to dip below the Ohio River as we headed into the overnight hours and transitioned to July 30th. SPC had us in a slight risk for severe thunderstorms, as showers and thunderstorms formed ahead of this frontal boundary. Many of these storms lead to heavy rainfall, and resulted in multiple instances of flash flooding. High winds were also a threat, as two severe thunderstorm warnings were issued, and numerous reports of wind damage were obtained. There was even enough low level rotation in one storm to constitute a tornado warning during the early morning hours on the 30th. Thankfully there were no reports from this.||Rainfall amounts from this event are summarized below:||...PRECIPITATION REPORTS...||Location                     Amount    Time/Date       Lat/Lon              |2 SSE Farmers           4.58 in   0700 AM 07/30   38.12N/83.53W        |1 SSE Stanton           4.22 in   0800 AM 07/30   37.83N/83.85W        |Koomer Ridge            4.20 in   1200 PM 07/30   37.78N/83.63W        |Peeled Oak                3.84 in   1200 PM 07/30   38.07N/83.80W        |0.8 NW Cannel City    3.63 in   1200 PM 07/30   37.80N/83.28W        |2 E Clay City              3.52 in   0700 AM 07/30   37.86N/83.90W        |2 NNW Loam              3.36 in   0800 AM 07/30   37.43N/84.14W        |Owingsville 4 S           3.23 in   1200 PM 07/30   38.09N/83.76W        |Waltersville                3.20 in   0700 AM 07/30   37.87N/83.93W        |Somerset 7 NNE         3.12 in   1200 PM 07/30   37.18N/84.56W        |1 WSW Clover Bottom 3.10 in   0800 AM 07/30   37.49N/84.17W        |1 NNW Owingsville      2.95 in   0800 AM 07/30   38.14N/83.76W        |Maytown                    2.92 in   1200 PM 07/30   37.85N/83.47W        |2 WNW Rockcastle Springs     2.76 in   0700 AM 07/30   37.02N/84.34W        |Wades Mill                 2.76 in   1200 PM 07/30   38.03N/84.02W        |1 S Paxton                 2.74 in   0700 AM 07/30   37.66N/83.41W        |1 S Paxton                 2.74 in   0700 AM 07/30   37.66N/83.41W        |2 NNE Mount Olive     2.72 in   0900 AM 07/30   37.63N/83.72W        |Buckner Branch         2.49 in   1200 PM 07/30   38.35N/83.40W        |Mt Sterling                2.45 in   1200 PM 07/30   38.03N/83.97W        |Peabody                   2.44 in   1200 PM 07/30   37.14N/83.58W        |Willailla                    2.35 in   0700 AM 07/30   37.30N/84.46W        |Whitley City 3 N       2.34 in   1200 PM 07/30   36.77N/84.48W        |1.2 W Jackson          2.28 in   1200 PM 07/30   37.55N/83.40W        |Judy                        2.24 in   0700 AM 07/30   38.13N/83.96W        |2.0 NE Monticello      2.22 in   1200 PM 07/30   36.87N/84.83W        |0.9 NW Wendover     2.20 in   1200 PM 07/30   37.14N/83.37W        |1.7 SE Ringos Mills   2.19 in   1200 PM 07/30   38.25N/83.59W        |1 ENE Gates             2.16 in   0709 AM 07/30   38.24N/83.34W        |McKee 5 S                2.10 in   1200 PM 07/30   37.36N/83.97W        |2 ESE Grassy Lick     2.09 in   0730 AM 07/30   38.07N/83.99W        |1.2 S Grassy Creek   2.01 in   1200 PM 07/30   37.85N/83.35W        |Cressy                     2.01 in   0800 AM 07/30   37.83N/84.04W  ||End of summary. A tree was blown down onto Poplarville Road in the 2500 block near Mount Victory.", "ts_dict_index": [8037, 8038, 8039]}
+{"event_id": 919276, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:10:00", "end_date_time": "2020-08-10 10:10:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Mesonet station reported a 74 kts wind gust.", "ts_dict_index": [8079, 8080, 8081]}
+{"event_id": 918979, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:05:00", "end_date_time": "2020-08-10 10:05:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Public report via social media of roof damage to Buccaneer Arena at 72nd and Hickman Rd. Time estimated.", "ts_dict_index": [8085, 8086, 8087]}
+{"event_id": 849751, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-08-23 02:30:00", "end_date_time": "2019-08-23 02:50:00", "narrative": "As severe storm/flooding events go, some are definitely better-anticipated than others (forecast-wise). Unfortunately, what transpired on this Thursday evening the 22nd into early Friday morning the 23rd fell into the low-predictability category, as an apparent mesoscale convective vortex (MCV) sparked isolated-but-intense thunderstorms that not only dumped flooding rains on parts of Sherman/Buffalo/Howard/Hall/Adams counties, but also brought a damaging combination of winds and hail to parts of Hall/Adams counties. Going into more detail, and starting with the severe weather aspect, around 1:30 a.m. CDT a severe thunderstorm rapidly blossomed over southern Hall County. It started drifting slowly south-southeast, reaching Hastings around 3 a.m. CDT and eventually weakening/dissipating over southern Clay County between 4-5 a.m. CDT. Along the way, this storm produced winds measured as high as 76 MPH at Hastings airport, along  with copious amounts of hail up to half dollar size. In Hall County, at least one semi truck was blown over on Interstate 80. However, Hastings was the hardest hit local community, specifically the west side of town and adjacent rural areas, where the wind/hail combo shredded trees and gardens, damaged house siding and ravaged maturing crops. Some hail drifts in/near west Hastings were still visible well into the daytime hours (side note: this was at least the third time in 2019 that severe storms impacted Hastings). Flooding was certainly an issue within Hall/Adams counties as well, particularly in the Amick Acres neighborhood west of Doniphan where a CoCoRaHS observer measured 4.54 of rain. This prompted extensive flooding of basements and overflowed a series of small lakes (at least minor flooding would continue at Amick Acres for several more days). Flooding was less-severe in the Hastings area, but there was still short-term flooding of fields and rural roads (including the brief closure of Showboat Road just east of town). ||Although the weather impacts in Hall/Adams counties dominated the local news headlines, significant-but-localized flooding also occurred in more rural areas of southern Sherman, northeastern Buffalo and southeastern Howard counties earlier in the night. Focusing on the more significant event in Sherman/Buffalo counties, a slow-moving series of re-generating storms dumped 2-5+ inches of rain along a narrow corridor from south of Loup City to south of Ravenna, with the majority falling between 7 p.m. and midnight CDT. There were a few unofficial public reports of totals as high as 7-7.50, along with some ground-truth reports of flooding/flash flooding, including water running over portions of Highways 10 and 68. As mentioned at the top, the development and intensity of these evening and overnight storms was not well-anticipated in official forecasts, as numerical models failed to latch onto the apparent influence of a pesky, slow-moving MCV that drifted eastward into South Central Nebraska during the day on the 22nd and stuck around through the night. The larger scale mid-upper air pattern over Nebraska was not very notable, featuring only subtle/low amplitude disturbances ejecting eastward from a trough centered over the Northern Rockies. Adding to the surprising intensity of this convection, mesoscale analysis depicted only weak deep-layer wind shear of no more than 25-30 knots, along with only around 1000 J/kg most-unstable CAPE. Wind gusts estimated to be between 60 and 65 MPH lasted for approximately 20 minutes.", "ts_dict_index": [8046, 8047, 8048]}
+{"event_id": 919267, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:00:00", "end_date_time": "2020-08-10 10:00:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. A trained spotter reported 80 mph wind gusts with several large tree limbs down and tree trunks snapped. Roads were blocked.", "ts_dict_index": [8088, 8089, 8090]}
+{"event_id": 919282, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:15:00", "end_date_time": "2020-08-10 10:15:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. AWOS measurd a 68 knot wind gust.", "ts_dict_index": [8082, 8083, 8084]}
+{"event_id": 919233, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:26:00", "end_date_time": "2020-08-10 10:26:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Public report of mailboxes, trees, and limbs of undetermined size down.", "ts_dict_index": [8076, 8077, 8078]}
+{"event_id": 849748, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-08-23 01:59:00", "end_date_time": "2019-08-23 02:15:00", "narrative": "As severe storm/flooding events go, some are definitely better-anticipated than others (forecast-wise). Unfortunately, what transpired on this Thursday evening the 22nd into early Friday morning the 23rd fell into the low-predictability category, as an apparent mesoscale convective vortex (MCV) sparked isolated-but-intense thunderstorms that not only dumped flooding rains on parts of Sherman/Buffalo/Howard/Hall/Adams counties, but also brought a damaging combination of winds and hail to parts of Hall/Adams counties. Going into more detail, and starting with the severe weather aspect, around 1:30 a.m. CDT a severe thunderstorm rapidly blossomed over southern Hall County. It started drifting slowly south-southeast, reaching Hastings around 3 a.m. CDT and eventually weakening/dissipating over southern Clay County between 4-5 a.m. CDT. Along the way, this storm produced winds measured as high as 76 MPH at Hastings airport, along  with copious amounts of hail up to half dollar size. In Hall County, at least one semi truck was blown over on Interstate 80. However, Hastings was the hardest hit local community, specifically the west side of town and adjacent rural areas, where the wind/hail combo shredded trees and gardens, damaged house siding and ravaged maturing crops. Some hail drifts in/near west Hastings were still visible well into the daytime hours (side note: this was at least the third time in 2019 that severe storms impacted Hastings). Flooding was certainly an issue within Hall/Adams counties as well, particularly in the Amick Acres neighborhood west of Doniphan where a CoCoRaHS observer measured 4.54 of rain. This prompted extensive flooding of basements and overflowed a series of small lakes (at least minor flooding would continue at Amick Acres for several more days). Flooding was less-severe in the Hastings area, but there was still short-term flooding of fields and rural roads (including the brief closure of Showboat Road just east of town). ||Although the weather impacts in Hall/Adams counties dominated the local news headlines, significant-but-localized flooding also occurred in more rural areas of southern Sherman, northeastern Buffalo and southeastern Howard counties earlier in the night. Focusing on the more significant event in Sherman/Buffalo counties, a slow-moving series of re-generating storms dumped 2-5+ inches of rain along a narrow corridor from south of Loup City to south of Ravenna, with the majority falling between 7 p.m. and midnight CDT. There were a few unofficial public reports of totals as high as 7-7.50, along with some ground-truth reports of flooding/flash flooding, including water running over portions of Highways 10 and 68. As mentioned at the top, the development and intensity of these evening and overnight storms was not well-anticipated in official forecasts, as numerical models failed to latch onto the apparent influence of a pesky, slow-moving MCV that drifted eastward into South Central Nebraska during the day on the 22nd and stuck around through the night. The larger scale mid-upper air pattern over Nebraska was not very notable, featuring only subtle/low amplitude disturbances ejecting eastward from a trough centered over the Northern Rockies. Adding to the surprising intensity of this convection, mesoscale analysis depicted only weak deep-layer wind shear of no more than 25-30 knots, along with only around 1000 J/kg most-unstable CAPE. A 76 MPH wind gust was measured by the Hastings Airport ASOS at 2:59 AM CDT. Wind gusts were estimated to be near 70 to 75 MPH along this path. A light helicopter was blown over at the Hastings Airport. Quarter to half dollar size hail was also reported near the airport, which combined with intense winds to shred trees, crops and gardens, and damage house siding, in and near the west side of Hastings.", "ts_dict_index": [8049, 8050, 8051]}
+{"event_id": 901342, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-06-28 01:11:00", "end_date_time": "2020-06-28 01:11:00", "narrative": "This was an active late Saturday evening-early Sunday morning of thunderstorms across much of South Central Nebraska, featuring several reports of large hail and especially damaging winds mainly between midnight-3 a.m. CDT as two storm complexes rolled through and eventually merged. Focusing first on severe winds, most estimated or measured gusts were in the 50-70 MPH range and associated with primarily tree damage. However a few isolated structural damage reports were more suggestive of at least 75-80 MPH, including: 1) 10 power poles blown down and three grain bins destroyed (along with some overturned irrigation pivots) west of Aurora...2) grain bin damage and overturned pivots north of Minden. Hail was more limited overall, but stones reached golf ball size at Pauline and ping pong ball size in Davenport, while Hastings saw nickel to quarter size hail. Rainfall amounts varied considerably (most of South Central Nebraska had less than one-half inch), but a fairly narrow swath of at least 1.50-2.50 targeted parts of primarily Thayer/Nuckolls/Clay counties, with one unofficial report as high as 3.17 near Belvidere. Flooding was fairly minimal, although one rural road along the Fillmore/Thayer County line still had water running across it around sunrise. ||As for storm mode/evolution, this was a somewhat complex event. The first local convection of the night entered the Furnas County area out of northwest Kansas after 11 p.m. CDT, in the form of a compact linear mesoscale convective system (MCS) on a weakening trend. But then, between midnight-1 a.m. CDT, a broken band of intense, semi-discrete storms erupted out ahead of this MCS along a west-east axis centered from Phelps-Adams-Thayer counties (likely in response to the onset of a healthy low level jet). However, these initially semi-discrete storms (which accounted for all large hail reports) quickly consolidated/grew upscale into a new linear MCS that charged north-northeast across the Highway 6/Interstate 80 corridors between 1-2 a.m. CDT, gradually merging with the initial MCS racing up from the southwest in the process. During the ensuing hour, the two complexes completed a full merger; the northern end weakening as it reached far northeastern counties (such as Nance/Polk), while the southern end remained severe through Fillmore/Thayer counties before departing the local area into southeast Nebraska. This ended any severe threat for the night, although weaker storms and broader showers persisted until around sunrise in some spots. This was a ripe setup for severe nocturnal storms, especially with the exit region of a 30-40 knot southerly low level jet (evident at 850 millibars) aimed into the heart of South Central Nebraska after dark, and tapping into a large reservoir of most-unstable CAPE as high as 2000-3000 J/kg. In the mid-upper levels, flow over the region was not overly-strong, but contained various low-amplitude disturbances and was in the process of transitioning more southwesterly in response to a larger-scale trough setting up over the northwestern United States. There were no distinct surface features across the local area, but steady light southeast breezes prior to storm initiation maintained seasonably-high dewpoints in the mid-60s to low-70 F. Likely one of the main limiting factors against a more robust severe threat was only modest deep-layer wind shear around 30 knots. Wind gusts were estimated to be near 60 MPH. Some tin was blown into a tree.", "ts_dict_index": [8055, 8056, 8057]}
+{"event_id": 907632, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-07-08 23:07:00", "end_date_time": "2020-07-08 23:07:00", "narrative": "Extensive line of thunderstorms brought widespread severe wind to much of south central Nebraska and portions of north central Kansas on this date. This event will likely go down as the most widespread severe weather event of the spring and summer of 2020 for the Hastings County Warning Area (CWA). Thunderstorms developed along a cold front across north central Nebraska, and also within a zone of low level upslope flow over western Nebraska and northeast Colorado, during the early evening hours of July 8th. Both areas of development initially contained both line segments and embedded supercells, posing risks for all severe hazards, but quickly organized into two separate lines of convection, or quasi linear convective systems (QLCSs). By 9pm CDT, one line extended roughly west to east from Thedford, NE to O'Neill, NE and was moving southeast, while the other line extended roughly north to south from near Thedford, NE to just west of McCook, NE and was moving mainly east. Shortly thereafter, both lines began to merge together into one coherent line. Thunderstorms began to enter far northern and western portions of the CWA around 10pm CDT. By this time, thunderstorms already had a history of producing 60 to 75 mph wind gusts and a few instances of large hail just northwest and west of the CWA. The line of thunderstorms strengthened and organized further as they shifted southeast into the CWA between 10-11pm CDT. In fact, an impressive bow echo developed over Gosper and Furnas Counties during this time and raced eastward, affecting areas primarily between Interstate 80 in south central Nebraska and Highway 36 in north central Kansas. Severe wind gusts remained the primary threat. The QLCS had taken on an ���S��� shape by 11pm CDT, slanting southwest to northeast. The greatest concentration of severe wind reports occurred over central and eastern portions of the CWA, roughly from Grand Island and Hastings eastward to York and Hebron, between 11pm CDT on July 8th and 1am CDT on July 9th as forward speed increased dramatically. Several wind gusts were measured between 70-75mph in this area, including a peak wind gust of 75mph in Thayer County. Not surprisingly, widespread wind damage was reported, as well, especially to trees, power lines, and crops. Downed tree limbs (medium to large size) and snapped small trees were fairly common. Power outages were also common across many small towns during the overnight and into the early morning hours, though an exact estimation of peak power outages is unknown. A few buildings also sustained damage, such as blown in doors and roof damage from fallen trees and lost shingles. Finally, a brief EF-0 tornado was determined to have occurred in Merrick County, with peak winds estimated to be around 85mph. Damage was limited. The leading edge of the QLCS, and associated peak wind threat, shifted east and southeast of the CWA by 1AM CDT, though lingering stratiform rain as well as a northwest to southeast band of thunderstorms near the state line continued for a few more hours. The only severe hail reported with this event was along the southwest flank of the QLCS over Furnas County, where thunderstorms continued to regenerate. A few instances of quarter to golf ball size hail was reported.||Meteorologically speaking, this severe wind event was driven largely by a cold front interacting with a strongly unstable airmass due to steep mid level lapse rates, strong heating, and moist boundary layer. Initially cellular activity quickly grew upscale into line segments owing to the linear forcing along the cold front and generally outflow dominated activity, with peak DCAPE values in excess of 1500 J/kg. The primary shortwave trough responsible for the cold front remained well north of the area, near the Montana/Canadian border, but several weak perturbations moving west to east over the cold front likely aided in thunderstorm development as well. A distinct mesoscale convective vortex, modest deep layer shear of 30-35 knots, and an intensifying southerly low level jet up to 45 knots sustained the severe convection well past sunset. Finally, it's worth noting that an impressive surface pressure rise/fall couplet of at least 3mb/2hr accompanied the QLCS across the CWA between 05Z and 07Z. Wind gusts estimated to be near 60 MPH resulted in tree damage in Sutton.", "ts_dict_index": [8007, 8008, 8009]}
+{"event_id": 919268, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:01:00", "end_date_time": "2020-08-10 10:01:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Mesonet station reported a 60 knot wind gust.", "ts_dict_index": [8091, 8092, 8093]}
+{"event_id": 919236, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:39:00", "end_date_time": "2020-08-10 10:39:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Amateur radio report of multiple tree limbs down with the largest eight inches in diameter. Time estimated.", "ts_dict_index": [8094, 8095, 8096]}
+{"event_id": 919274, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:06:00", "end_date_time": "2020-08-10 10:06:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. NWS employee reported 70 mph wind gusts and lots of small branches down.", "ts_dict_index": [8067, 8068, 8069]}
+{"event_id": 922614, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-10-11 19:15:00", "end_date_time": "2020-10-11 19:15:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. A wind gust of 60 MPH was recorded by a mesonet station located 4 miles southwest of Harvard.", "ts_dict_index": [8130, 8131, 8132]}
+{"event_id": 918974, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:00:00", "end_date_time": "2020-08-10 10:00:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Trained spotter reported numerous trees and power lines down. Time estimated.", "ts_dict_index": [8100, 8101, 8102]}
+{"event_id": 919271, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:04:00", "end_date_time": "2020-08-10 10:04:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Des Moines Airport ASOS reported a wind gust of 65 knots.", "ts_dict_index": [8118, 8119, 8120]}
+{"event_id": 918985, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:10:00", "end_date_time": "2020-08-10 10:10:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. An NWS employee reported and uprooted tree in northwest Johnston. Time estimated.", "ts_dict_index": [8112, 8113, 8114]}
+{"event_id": 918981, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:05:00", "end_date_time": "2020-08-10 10:05:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Trained spotter reported twelve to eight inch diameter trees down.", "ts_dict_index": [8106, 8107, 8108]}
+{"event_id": 918986, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:10:00", "end_date_time": "2020-08-10 10:10:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. A trained spotter reported six inch and larger tree limbs down with power outages. Severe winds lasted 30 minutes.", "ts_dict_index": [8121, 8122, 8123]}
+{"event_id": 918983, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:10:00", "end_date_time": "2020-08-10 10:10:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. A trained spotter reported branches down.", "ts_dict_index": [8103, 8104, 8105]}
+{"event_id": 923027, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-10-11 19:52:00", "end_date_time": "2020-10-11 19:52:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. A wind gust of 59 MPH was measured by a mesonet station located 6 miles south-southeast of Davenport.", "ts_dict_index": [8124, 8125, 8126]}
+{"event_id": 919016, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 10:19:00", "end_date_time": "2020-08-10 10:19:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Trained spotter reported a large tree down.", "ts_dict_index": [8115, 8116, 8117]}
+{"event_id": 923022, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-10-11 19:47:00", "end_date_time": "2020-10-11 19:47:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. A wind gust of 71 MPH was measured by a mesonet station located 1 mile south-southeast of Davenport.", "ts_dict_index": [8127, 8128, 8129]}
+{"event_id": 914062, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-08-16 18:49:00", "end_date_time": "2020-08-16 18:49:00", "narrative": "On this late Sunday afternoon and evening, several scattered, strong to severe storms advanced southward across various portions of South Central Nebraska, prompting many accounts of large hail and a few damaging wind gusts. While most hail was in the quarter to golf ball size range, larger stones of 2-3 diameter fell in the Chapman and Marquette areas of Merrick/Hamilton counties. Ping pong to golf ball size hail occurred in or near the following communities/locations: Fullerton, Amherst, Orleans, Harlan County Lake, Naponee and Deweese. In the Tri Cities, only Grand Island saw severe weather, as two rounds of quarter to half dollar size hail moved through, one mainly affecting the north side of town (including the airport) around 6 p.m. CDT, and another about an hour later that clipped more of the city. As for thunderstorm winds, the vast majority of gusts captured by area sensors were non-severe (generally 40-50 MPH), but there were two reports estimated around 60 MPH, one near Hampton and another at Hebron, where a few large trees were downed and a store front sustained minor damage. Given fairly progressive storm motions, rainfall totals in most affected areas were less than 1 inch during the afternoon/evening. However, combined with localized heavy rain that fell during a separate round of early morning/non-severe activity, portions of mainly eastern Clay County registered over 3 for the day (including NWS coop observer total of 3.33 six miles east-southeast of Clay Center). As a result, the later-day storms prompted some isolated flash flooding, as School Creek overtopped the paved spur road south of Saronville. ||This event was characterized by truly scattered, hit-or-miss convection, as afternoon heating and subtle convergence along/ahead of a weak cold front sagging southward into the region prompted several strong to severe storms, mainly in the form of multicells/multicell clusters, but also a few brief supercells. Nearly every county in the 24-county area observed at least a touch of thunderstorm activity. That being said, the majority of ground-truth reports concentrated in two primary areas: 1) parts of Hall/Hamilton/Merrick counties...2) a swath from eastern Furnas to far southwestern Franklin counties. A few of the first severe storms of the event flared up over Furnas/Buffalo counties between 430-530 p.m. CDT, and the final severe storm of the evening was centered over the Nuckolls County area before weakening around 9 p.m. CDT. Thereafter, a smattering of strong storms lingered within counties south of Interstate 80 through around 10:30 pm. CDT before all convection ended for the night. In total, 19 Severe Thunderstorm Warnings were issued within South Central Nebraska over the course of over four hours. Digging deeper into the meteorological setup, it's worth noting that this event exceeded forecast expectations, especially in terms of the number of severe storms. This was due in part to greater-than-expected convective instability, as afternoon surface dewpoints soared into the upper 60s-low 70 F,  promoting significant mixed-layer CAPE of at least 3000-4000 J/kg. In tandem with deep layer wind shear around 35 knots, this CAPE/shear combo proved plenty sufficient for robust convection. In the mid-upper levels, a pronounced north-northwest flow regime resided over the Central Plains, within the interface between a stout western United States ridge and a broad eastern trough. Wind gusts estimated to be near 60 MPH downed two large trees and damaged one store front.", "ts_dict_index": [8043, 8044, 8045]}
+{"event_id": 923025, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2020-10-11 19:50:00", "end_date_time": "2020-10-11 19:50:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. Wind gusts were estimated to be near 60 MPH.", "ts_dict_index": [8142, 8143, 8144]}
+{"event_id": 923017, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-10-11 19:20:00", "end_date_time": "2020-10-11 19:21:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. Wind gusts estimated to be near 60 MPH resulted in blowing dust and corn stalks in the area, along with near zero visibility. One vehicle left the roadway due to the conditions. A power line was blown into a tree just northwest of town, causing a fire in the tree.", "ts_dict_index": [8139, 8140, 8141]}
+{"event_id": 923019, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-10-11 19:27:00", "end_date_time": "2020-10-11 19:30:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. Wind gusts estimated to be near 65 MPH resulted in tree damage in Sutton. A few downed branches were at least 6 inches in diameter.", "ts_dict_index": [8133, 8134, 8135]}
+{"event_id": 922609, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2020-10-11 19:09:00", "end_date_time": "2020-10-11 19:09:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. Wind gusts estimated to be near 60 MPH caused minor tree damage and downed power lines in Clay Center.", "ts_dict_index": [8136, 8137, 8138]}
+{"event_id": 919262, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 09:47:00", "end_date_time": "2020-08-10 09:47:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. A trained spotter reported 70 mph gusts at Mills Civic Parkway and Interstate 35.", "ts_dict_index": [8109, 8110, 8111]}
+{"event_id": 923030, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2020-10-11 20:03:00", "end_date_time": "2020-10-11 20:03:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. A wind gust of 58 MPH was measured by a mesonet station located 3 miles east of Strang.", "ts_dict_index": [8148, 8149, 8150]}
+{"event_id": 1099529, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2023-06-09 19:02:00", "end_date_time": "2023-06-09 19:02:00", "narrative": "Primarily between 2:30-9:30 p.m. CDT on this Friday afternoon and evening, scattered to numerous thunderstorms rumbled across much of South Central Nebraska, including a varied mix of isolated pulse/single cells, multicell clusters and small-scale line segments. Like the more spotty activity the day prior, the majority of this convection was non-severe, simply producing beneficial rainfall, gusty winds of no more than 40-50 MPH and isolated pockets of very small hail. However, a handful of storms became strong to marginally-severe. Ground-truth reports were quite limited, but included nickel size hail near Holbrook and a measured wind gust to 59 MPH near Shickley (unofficial mesonet). Based on radar data, marginally-severe storms might have also affected at least small portions of the following counties, but with no verification: Greeley, Howard, Nance and Gosper. Rainfall-wise, amounts across the 24-county area were highly variable, with most areas receiving no more than one-quarter to one-half inch, but ranging from hardly a drop in some spots, to several small pockets at least 1-2, particularly within portions of several counties along/north of Interstate 80. However, there were no reports of impactful flooding. ||Turning to the meteorological background and event evolution, this was another case of marginally-severe convection forming in a moderately-unstable, but weakly-sheared environment. In the mid-upper levels, wind fields remained unusually weak by early-June standards, thanks to South Central Nebraska residing under broad ridging stretched across the heart of the United States from north-northwest to south-southeast...well-removed from any larger-scale troughs centered over the northeastern and northwestern states. However, on the smaller-scale, a weak disturbance (possible MCV) drifted east into South Central Nebraska during the afternoon-evening, likely supporting more widespread convective coverage versus the day before. At the surface, there were no notable features in the pre-convective environment, only light south-southeasterly breezes and hints of a weak low pressure center over Nebraska. As temperatures climbed into the upper 80s-low 90s (F) by mid-afternoon, storms readily developed in a weakly-capped environment featuring moderate mixed-layer CAPE of of 1500-2500 J/kg, but seasonably-paltry deep-layer wind shear only around 20 knots at best. The majority of convection early in the event (mainly 2:30-5:30 p.m. CDT) was more discrete in nature and focused within northern/western portions of South Central Nebraska. Thereafter, activity trended a bit more upscale/linear over the next few hours as it progressed through mainly south central/southeast local counties, before departing southeastward into mainly northern Kansas by sunset. A wind gust of 59 MPH was measured by a mesonet station located three miles south-southwest of Shickley.", "ts_dict_index": [8178, 8179, 8180]}
+{"event_id": 923028, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2020-10-11 19:57:00", "end_date_time": "2020-10-11 19:57:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. A wind gust of 63 MPH was measured by a mesonet station located 4 miles north of Shickley.", "ts_dict_index": [8154, 8155, 8156]}
+{"event_id": 923033, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2020-10-11 19:35:00", "end_date_time": "2020-10-11 19:35:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. Wind gusts estimated to be near 65 MPH damaged some empty grain bins.", "ts_dict_index": [8145, 8146, 8147]}
+{"event_id": 849881, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-08-26 06:00:00", "end_date_time": "2019-08-26 06:00:00", "narrative": "A complex of strong to severe thunderstorms raced southeastward through mainly the northeast half of South Central Nebraska on this Monday morning, causing a few marginally-severe wind gusts, but mainly just dumping more unwelcomed rain, promoting new flooding issues and/or exacerbating ongoing flooding. The heart of this storm complex tracked along a 20-30 mile wide swath centered from roughly Arcadia-Grand Island-Geneva, entering the Valley/Sherman counties area around 5 a.m. CDT and exiting the Fillmore County area into southeast Nebraska around 8 a.m. CDT. Along the way, the Grand Island airport ASOS measured an official 59 MPH gust and on unofficial mesonet near Polk reported 60 MPH. Ground-truth wind damage reports were quite limited, but several tree branches were downed in McCool Junction. Certainly though, the biggest impact from this event was heavy rainfall/flooding, as most places within the aforementioned swath tallied early morning amounts of 1.00-2.50, with a few higher totals including 3.00 near Cotesfield and 2.69 west of Doniphan. As a result, at least minor flooding of several creeks and rural roads occurred or continued within several local counties, including along the West Fork Big Blue River between Hastings and McCool Junction. Among a few of the more newsworthy flooding impacts, Grand Island not only saw widespread short-term street flooding, but the State Fairgrounds were swamped with several inches of standing water for a few hours, disrupting Day 4 of the Nebraska State Fair. Also in Hall County, ongoing flooding issues at the Amick Acres neighborhood west of Doniphan were worsened, with flooding subsequently persisting for several more days. To put the Hall County hydrologic situation into some numerical perspective, a CoCoRaHS observer near Doniphan measured an incredible 11.91 between Aug. 21-26 and 16.76 for the entire month! At Grand Island airport, the official Aug. 21-26 total was only 5.34, but the monthly total of 11.94 shattered the previous August record of 8.73 in 1977 (normal August rainfall at Grand Island is 3.12). ||Breaking down the meteorological setup, it's worth noting that the primary storm cluster that traversed the local area between 5-8 a.m. CDT was not the only one of the morning, as it was preceded by a less-intense, non-severe batch of storms that roamed over many of the same areas 3-5 a.m. CDT. In the mid-upper levels, the pattern was seasonably-active, as South Central Nebraska resided under northwesterly flow, with shortwave disturbances tracking around the southern periphery of a large-scale trough centered over southern Canada. In the lower levels, convection was fed by warm air/moisture advection on the nose of a 30-35 knot low level jet. At the surface, a weak cold front gradually edged into the local area over the course of the morning. As the main storm complex pushed into South Central Nebraska, the mesoscale environment featured seasonably-strong deep-layer wind shear around 50 knots and 1000-2000 J/kg most-unstable CAPE. Wind gusts were estimated to be near 60 MPH and were accompanied by dime size hail.", "ts_dict_index": [8166, 8167, 8168]}
+{"event_id": 923024, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2020-10-11 19:48:00", "end_date_time": "2020-10-11 19:48:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. A wind gust of 67 MPH was measured by a mesonet station located 2 miles east-northeast of Fairmont.", "ts_dict_index": [8157, 8158, 8159]}
+{"event_id": 882473, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-04-12 19:00:00", "end_date_time": "2020-04-12 19:00:00", "narrative": "On the 8th as a cold front headed this way from Canada. It was a very warm afternoon, with high temperatures in the 80s to lower 90s. It was 92 degrees at Harrison (Boone County) and Russellville (Pope County), and 91 degrees at Mena (Polk County), and Mountain Home (Baxter County). Normal highs are in the upper 60s to mid 70s.||The heat and increasing moisture made the atmosphere extremely unstable. However, thunderstorms had some difficulty developing. Data acquired from a balloon launch by the National Weather Service at the North Little Rock Airport (Pulaski County) revealed warming aloft (an inversion) at 100 pm CDT. Readings went from 68 degrees at 2000 feet to 75 degrees at 2500 feet. This tended to cap the lower levels of the atmosphere, and prevented storms from taking off. For most of the afternoon, there were few clouds.||Capping was weakest in the northeast, and this is where isolated storms finally went haywire by 500 pm CDT. One storm in particular peaked the interest of radar operators and kept them busy for several hours. The storm unleashed baseball size hail at Strawberry (Lawrence County), and golf balls at Horseshoe Bend (Izard County), Lynn (Lawrence County), and Ravenden (Lawrence County).||The biggest event of month happened on the 12th (Easter) and 13th. There were more than 1,000 reports of wind damage and at least 130 tornadoes from Texas to the Carolinas. Sadly, there were three dozen casualties.||We had to deal with a line of nasty thunderstorms. The line had bowing segments, indicating that powerful winds were driving the storms forward and causing them to bulge outward. Severe Thunderstorm Warnings were first issued between 530 pm and 600 pm CDT, and continued for five hours until the storms moved east of the Mississippi River. The storms produced damaging wind gusts from 60 to more than 80 mph, and knocked out power to at least 150,000 utility customers.||There were numerous reports of trees and power lines downed, with trees blocking roads in some cases. Trees fell on residences, resulting in a death at White Hall (Jefferson County) and an injury at Glen Rose (Hot Spring County). Outbuildings and sheds were damaged or destroyed. A roof was blown off of a poultry farm on Highway 154 north of Danville (Yell County). A 68 mph gust was measured at Petit Jean State Park (Conway County).||Much of Arkansas received one to more than three inches of rain, with the heaviest amounts over central and southern sections of the state. Monticello (Drew County) had an estimated 3.73 inches of precipitation on the 12th, breaking a daily record that stood since 1877.||This was one of the more significant downpours of the month, and contributed to largely above average rainfall totals. Surpluses of liquid in April were more than an inch at Little Rock (Pulaski County), and Pine Bluff (Jefferson County). Trees were down and blocking Kanis Rd. in West Little Rock.", "ts_dict_index": [8175, 8176, 8177]}
+{"event_id": 996810, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-12-15 18:12:00", "end_date_time": "2021-12-15 18:12:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. Spotter reported wind gusts between 612 pm and 625 pm, estimated between 60 and 70 pm. Also reported large branches down, but exact size unknown.", "ts_dict_index": [8181, 8182, 8183]}
+{"event_id": 996814, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-12-15 18:23:00", "end_date_time": "2021-12-15 18:23:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. Public reported siding, shingle, and minor tree damage to townhomes. Report was relayed via broadcast media. Time estimated from radar.", "ts_dict_index": [8187, 8188, 8189]}
+{"event_id": 923023, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-10-11 19:48:00", "end_date_time": "2020-10-11 19:48:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. A wind gust of 67 MPH was measured by a mesonet station located 2 miles south-southeast of Davenport.", "ts_dict_index": [8160, 8161, 8162]}
+{"event_id": 923032, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-10-11 20:10:00", "end_date_time": "2020-10-11 20:11:00", "narrative": "A strong cold front brought intense non-thunderstorm and thunderstorm-related wind gusts to south central Nebraska on Sunday evening the 11th. This front entered western portions of the Hastings NWS county warning area (CWA) around 7pm CDT. The cold front already had a history of producing severe caliber, non-thunderstorm, straight line winds over western and central Nebraska, and this trend continued along and just behind the cold front as it marched through south central Nebraska. The strongest winds, initially, were focused roughly along an area from Furnas County northeast into Buffalo County, where measured and estimated wind gusts of 55-65 mph were fairly common. Damage reports from these areas were fairly typical for winds of this magnitude and mainly limited to tree and power line damage. By 7:30pm CDT, an area of showers and thunderstorms developed along and just behind the cold front over Kearney and Franklin Counties as the cold front continued to progress east. This activity reached roughly the Highway 281 corridor from Grand Island to Hastings around 8pm CDT. Wind gusts associated with the passage of the cold front had weakened slightly by this time, but were still quite strong around 50-55 mph, with mainly minor tree damage and power outages reported in the Tri Cities. After 8pm CDT, the area of thunderstorms began to expand northeast and connected up with existing thunderstorms that had already developed along the cold front over northeast and east central Nebraska, essentially filling in a gap that had existed in between the two thunderstorm clusters. Thunderstorm intensity increased just east of Hastings between 8pm CDT and 8:30pm CDT, such that the wind gusts produced by the thunderstorms exacerbated the already-high ambient synoptically driven non-thunderstorm wind gusts associated with the cold front. This resulted in the strongest wind gusts of the evening, generally 60 to 70mph, in a swath that covered portions of Clay, Fillmore, and Thayer Counties. Significant tree damage occurred in these areas, along with damage to a few empty grain bins. Another significant impact, albeit somewhat less obvious or common than typical tree/power line damage, was blowing dust and corn stalks (this event occurred during the harvest season) that led to reduced visibility and ultimately contributed to a four-vehicle accident along Highway 81 just north of Bruning. Another incidence of poor visibility caused a vehicle to leave the roadway in Clay County. ||The highest wind gust with this event was 71 mph, measured by a mesonet station in Thayer County. As mentioned above, the damaging wind events in the eastern half of the CWA were largely driven by convective winds that enhanced already-high ambient winds. Farther west, the severe wind was non-convective and driven by intense pressure rises behind the cold front on the order of 3-5 mb/2 hrs. Overall, this event was one of the more significant wind events of the season and was somewhat unique due to the narrow overlap, spatially and temporally, of both convective and non-convective damaging winds. Wind gusts estimated to be near 65 MPH caused downed tree branches in Bruning of at least 4 inches in diameter. An empty 500 gallen water tank was blown onto Main Street. There was a 4 vehicle accident on Highway 81 just north of Bruning due to poor visibility in blowing dust and corn stalks. Two of the vehicles were total losses.", "ts_dict_index": [8151, 8152, 8153]}
+{"event_id": 894474, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-06-03 22:01:00", "end_date_time": "2020-06-03 22:01:00", "narrative": "This Wednesday evening featured the first somewhat-widespread severe thunderstorm event of 2020 within South Central Nebraska, with several reports of damaging winds and large hail focused primarily near and northeast of a line from Loup City-Grand Island-Hebron. Overall, damaging winds were the bigger issue, highlighted by a measured gust of 79 MPH at the York airport shortly before 10 p.m. CDT. As these winds tore into town, they took down several large tree branches (a few entire trees), causing fairly widespread power outages and even partially-crushing an unoccupied car. About an hour before reaching York, measured winds of 70 MPH struck the Chapman area, flipping over irrigation pivots and taking down a light pole at a convenience store. Later in the evening, shortly before storms completely exited the local area, estimated 70 MPH winds took down a giant tree limb in Alexandria (3 ft. diameter/50 ft. long). Although the majority of wind damage focused within eastern counties, severe-criteria gusts were ongoing even as storms first entered the local area earlier in the evening, including 64 MPH at Ord airport. As for hail, the majority of limited reports were quarter size or smaller, although a few stones up to golf ball size were noted in North Loup.||Breaking down event timing and evolution, the scattered to numerous storms that eventually infiltrated South Central Nebraska first developed as separate storm clusters during the mid-late afternoon, one over northwest Nebraska and another in the NE/KS/CO border area. Between 7-9 p.m. CDT, both of these clusters entered northern and western portions of the local area. The southern one, which had been occasionally severe over southwest Nebraska, lost some steam as it moved east, yielding only slightly sub-severe wind gust reports in Furnas County. Meanwhile, the northern storm complex clearly established itself as dominant, charging southeastward as damaging winds peaked in intensity between 8:30-11:30 p.m. CDT. Shortly before midnight, the back edge of the now linear mesoscale convective system (MCS) exited southeast out of Thayer County, ending all storm activity for the night. Turning to the meteorological setup, this was not a strongly-forced event, with the main feature in the mid-upper levels consisting of a low-amplitude shortwave trough tracking east-southeast across Nebraska out of western SD over the course of the afternoon-evening. Surface features across South Central Nebraska ahead of the storms were fairly nondescript, dominated by weak high pressure and southerly-to-easterly breezes only around 10 MPH or less. However, fairly steep low-mid level lapse rates were in place, with damaging wind potential likely enhanced by fairly large surface dewpoint depressions heading into the evening (on the order of 25-30 degrees F). Evening mesoscale analysis over South Central Nebraska revealed 1000-2000 J/kg mixed-layer CAPE and around 35-40 knots of deep-layer wind shear. Wind gusts estimated to be near 65 MPH resulted in downed tree limbs in Deshler. Most branches were around 2 inches in diameter, the largest being approximately 1 foot in diameter and 25 feet long.", "ts_dict_index": [8172, 8173, 8174]}
+{"event_id": 829979, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2019-06-08 21:30:00", "end_date_time": "2019-06-08 21:36:00", "narrative": "Numerous thunderstorms rumbled across much of South Central Nebraska on the evening of Saturday the 8th into the early morning of Sunday the 9th. While most of this activity was sub-severe, producing only small hail and/or wind gusts up to around 50 MPH, a notable exception occurred in several southwestern counties where a briefly-supercellular storm produced a flurry of severe-criteria wind gusts primarily between 8-9 p.m. CDT. These severe winds of mainly 60-70 MPH concentrated within northern Furnas, southern Gosper, northwestern Harlan and southern Phelps counties, including an intense (albeit unofficial) gust of 86 MPH clocked by a personal weather station north-northwest of Oxford. While ground-truth damage reports were limited, they included: 1) a power pole blown onto Highway 6/34 in Arapahoe along with several large tree limbs down around town...2) various reports of mainly minor damage in/near Holdrege, including: damaged power poles, a large tree down at the cemetery, and part of an irrigation pivot blown onto a rural road a few miles west of town. As this storm of the day progressed into eastern Phelps County it weakened while transitioning to more of a multicell cluster mode. However, storm intensity occasionally flared up farther east, as evidenced by estimated 55-60 MPH winds in southeast Adams County. Lightning also made the news during the evening, as a bolt from a non-severe storm in Grand Island blew out a roughly 5-by-5 foot section from the roof of a retail store, sparking a small fire. Somewhat surprisingly, there was no verified severe-criteria hail during this event, with the largest reported stones only nickel size.||Timing-wise, the first severe storms of the day in close proximity to (but slightly west of) South Central Nebraska erupted along a well-defined cold front in west-central Nebraska during the mid-afternoon. A few hours later, the first strong storm to affect the local area entered western Dawson County between 6-7 p.m. CDT, followed a bit later by the main, outflow-dominant severe cell that rapidly intensified over Gosper/northern Furnas counties. As the night wore on a few larger-scale, predominantly sub-severe storm complexes traversed much of the 30-county area, with most places eventually rain-free by 4-5 a.m. CDT on the 9th. Meteorologically, this was a fairly strongly-forced event. In the mid-upper levels, west-southwesterly flow was present, slightly downstream from a seasonably-strong, large-scale trough traversing the Northern Rockies. At the surface, the aforementioned, northeast-southwest oriented cold front gradually made its way through South Central Nebraska during the evening and overnight hours. Ahead of this boundary, the mesoscale environment was clearly supportive of severe storms, with early-evening parameters featuring around 2000 J/kg mixed-layer CAPE and 30-40 knots of deep-layer wind shear. As a testament to the strength of the passing cold front, high temperatures across most of South Central Nebraska dropped from the mid-80s F on the 8th to only the upper-60s on the 9th. Estimated 55 to 60 mph wind gusts occurred. Winds were strong for about 5 to 7 minutes.", "ts_dict_index": [8163, 8164, 8165]}
+{"event_id": 894476, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-06-03 22:20:00", "end_date_time": "2020-06-03 22:20:00", "narrative": "This Wednesday evening featured the first somewhat-widespread severe thunderstorm event of 2020 within South Central Nebraska, with several reports of damaging winds and large hail focused primarily near and northeast of a line from Loup City-Grand Island-Hebron. Overall, damaging winds were the bigger issue, highlighted by a measured gust of 79 MPH at the York airport shortly before 10 p.m. CDT. As these winds tore into town, they took down several large tree branches (a few entire trees), causing fairly widespread power outages and even partially-crushing an unoccupied car. About an hour before reaching York, measured winds of 70 MPH struck the Chapman area, flipping over irrigation pivots and taking down a light pole at a convenience store. Later in the evening, shortly before storms completely exited the local area, estimated 70 MPH winds took down a giant tree limb in Alexandria (3 ft. diameter/50 ft. long). Although the majority of wind damage focused within eastern counties, severe-criteria gusts were ongoing even as storms first entered the local area earlier in the evening, including 64 MPH at Ord airport. As for hail, the majority of limited reports were quarter size or smaller, although a few stones up to golf ball size were noted in North Loup.||Breaking down event timing and evolution, the scattered to numerous storms that eventually infiltrated South Central Nebraska first developed as separate storm clusters during the mid-late afternoon, one over northwest Nebraska and another in the NE/KS/CO border area. Between 7-9 p.m. CDT, both of these clusters entered northern and western portions of the local area. The southern one, which had been occasionally severe over southwest Nebraska, lost some steam as it moved east, yielding only slightly sub-severe wind gust reports in Furnas County. Meanwhile, the northern storm complex clearly established itself as dominant, charging southeastward as damaging winds peaked in intensity between 8:30-11:30 p.m. CDT. Shortly before midnight, the back edge of the now linear mesoscale convective system (MCS) exited southeast out of Thayer County, ending all storm activity for the night. Turning to the meteorological setup, this was not a strongly-forced event, with the main feature in the mid-upper levels consisting of a low-amplitude shortwave trough tracking east-southeast across Nebraska out of western SD over the course of the afternoon-evening. Surface features across South Central Nebraska ahead of the storms were fairly nondescript, dominated by weak high pressure and southerly-to-easterly breezes only around 10 MPH or less. However, fairly steep low-mid level lapse rates were in place, with damaging wind potential likely enhanced by fairly large surface dewpoint depressions heading into the evening (on the order of 25-30 degrees F). Evening mesoscale analysis over South Central Nebraska revealed 1000-2000 J/kg mixed-layer CAPE and around 35-40 knots of deep-layer wind shear. Wind gusts were estimated to be near 70 MPH. Emergency management reported that a three foot diameter and 50 foot long tree limb and a 1.5 to 2 foot diameter tree limb were blown down and blocking Main Street in the community of Alexandria.", "ts_dict_index": [8169, 8170, 8171]}
+{"event_id": 918962, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2020-08-10 09:59:00", "end_date_time": "2020-08-10 09:59:00", "narrative": "Basic Summary: A cluster of storms in northeast Nebraska and southeast South Dakota developed into the destructive derecho that raced eastward across large portions of Iowa, northern Illinois, southern Wisconsin, northern Indiana, and southern Michigan during the morning and afternoon of August 10th. The strongest winds were experienced in central and east-central Iowa where 100+ mph winds were observed. Some of the strongest winds were in an area from roughly Marshalltown, IA eastward along the Highway 30 corridor to the Mississippi River, where estimated winds exceeded 120+ mph and approached 140 mph. A number of QLCS tornadoes were also experienced within the Highway 30 corridor. One of the most remarkable aspects of the derecho was the duration of severe winds, with many areas experiencing at least periodic, if not persistent, severe level (58+ mph) winds over a roughly 30 minute time frame. As the derecho moved eastward out of Iowa, it continued to expand, but weakened from its peak strength. Winds continued to exceed severe criteria (58+ mph) in Illinois, Wisconsin, Indiana, and Michigan and began to produce additional QLCS tornadoes across northern Illinois before fading out across northern Indiana and southern Michigan.||In the wake of the derecho, damage was substantial in many areas, rural and urban. Many agriculture fields, mainly corn, were flattened within the swaths of strongest winds. Initial estimates suggest at least 850,000 acres of partial or complete crop loss occurred from this event. Within urban and wooded areas extensive tree and structure damage was seen, including complete roof failure in a few instances. At its peak, total estimated customers without power exceeded 1.4 million across the affected states. In total, early estimates on losses (agriculture, infrastructure, private property) have exceeded $7.5 billion across the states affected. ||Environment: Broadly speaking, it was a ripe day for thunderstorms across the affected area with MUCAPE values often exceeding 3500-4000 J/kg by the mid morning hours concurrent with mid-upper level short wave support, and indications that any cold pool development would be strong (difference between cold pool and ambient air) and potentially long lived. For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Quad Cities, NWS Chicago, NWS Milwaukee, NWS Central Illinois, NWS Northern Indiana, or NWS Indianapolis.||Additional Details: Numerous injuries occurred during the derecho and in the aftermath during cleanup, including 4 direct and indirect deaths of which 3 occurred in Iowa (two in Poweshiek County and one in Linn County) and 1 in Indiana (Fort Wayne).||Disclaimer: The August 10, 2020 derecho resulted in widespread high-end damage across large portions of central and southern Iowa. Given the size and scope of the event and understanding that final damage and loss estimates (agriculture, infrastructure, and private property) will take months to complete, the NWS is not able to estimate the monetary impact at this time. Values may be added as more data becomes from various sources in future months. Public report of tree damage at 75th and Diamond in Urbandale.", "ts_dict_index": [8097, 8098, 8099]}
+{"event_id": 996817, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-12-15 18:28:00", "end_date_time": "2021-12-15 18:28:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. Broadcast media relayed public report of telephone pole damage at Wakonda Club Golf Course. Time estimated from radar.", "ts_dict_index": [8190, 8191, 8192]}
+{"event_id": 885188, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:50:00", "end_date_time": "2020-06-03 10:50:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large tree down near Yellow House Hotel near Douglasvile.  Time estimated from radar.", "ts_dict_index": [8262, 8263, 8264]}
+{"event_id": 885181, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:39:00", "end_date_time": "2020-06-03 10:39:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near Vinemont.  Time estimated from radar.", "ts_dict_index": [8229, 8230, 8231]}
+{"event_id": 885175, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:32:00", "end_date_time": "2020-06-03 10:32:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree down on wires on Mount Pleasant Road. Time estimated from radar.", "ts_dict_index": [8217, 8218, 8219]}
+{"event_id": 885592, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 17:15:00", "end_date_time": "2020-06-03 17:15:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree onto a house in Springmont.", "ts_dict_index": [8202, 8203, 8204]}
+{"event_id": 885178, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:35:00", "end_date_time": "2020-06-03 10:35:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Power pole fell onto a house near Reading, PA.  Time estimated from radar.", "ts_dict_index": [8247, 8248, 8249]}
+{"event_id": 885185, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:42:00", "end_date_time": "2020-06-03 10:42:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of trees and power lines down near Wyomissing.  Time estimate from radar.", "ts_dict_index": [8235, 8236, 8237]}
+{"event_id": 885180, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:38:00", "end_date_time": "2020-06-03 10:38:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires on State Highway 12 near Spring Valley Road.  Time estimated from radar.", "ts_dict_index": [8232, 8233, 8234]}
+{"event_id": 885492, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:15:00", "end_date_time": "2020-06-03 11:15:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple trees down near Delaware Valley University with the largest diameter around 1 foot.", "ts_dict_index": [8244, 8245, 8246]}
+{"event_id": 885183, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:40:00", "end_date_time": "2020-06-03 10:40:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree down onto a house on East Court Boulevard.  Time estimated from radar.", "ts_dict_index": [8250, 8251, 8252]}
+{"event_id": 885186, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:42:00", "end_date_time": "2020-06-03 10:42:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Widespread power outages with numerous reports of power lines and trees down near Muhlenberg Park.  Time estimated from radar.", "ts_dict_index": [8214, 8215, 8216]}
+{"event_id": 885179, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:38:00", "end_date_time": "2020-06-03 10:38:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires on State Highway 12 near the 11th Street interchange.  Time estimated from radar.", "ts_dict_index": [8238, 8239, 8240]}
+{"event_id": 885184, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:40:00", "end_date_time": "2020-06-03 10:40:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of trees and wires down at Spring Ridge Road and West Lawn Road.", "ts_dict_index": [8226, 8227, 8228]}
+{"event_id": 885182, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:40:00", "end_date_time": "2020-06-03 10:40:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large tree downed in Wyomissing.  Report via social media with video.  Time estimated from radar.", "ts_dict_index": [8223, 8224, 8225]}
+{"event_id": 885591, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 17:15:00", "end_date_time": "2020-06-03 17:15:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree damaged a property on Garfield Avenue in West Wyomissing. Time estimated from radar.", "ts_dict_index": [8193, 8194, 8195]}
+{"event_id": 885676, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:20:00", "end_date_time": "2020-06-03 18:20:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed trees on Leopard Road near Edgewood Avenue in Paoli. Time estimated from radar.", "ts_dict_index": [8199, 8200, 8201]}
+{"event_id": 885177, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:35:00", "end_date_time": "2020-06-03 10:35:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several tree limbs and power lines down in the Reading area. Estimated wind gusts up to 60 MPH.", "ts_dict_index": [8256, 8257, 8258]}
+{"event_id": 885593, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 17:15:00", "end_date_time": "2020-06-03 17:15:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed power lines near Texter Mountain Road in Wernersville. Time estimated from radar.", "ts_dict_index": [8208, 8209, 8210]}
+{"event_id": 885672, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:15:00", "end_date_time": "2020-06-03 18:15:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed wire on Paoli Pike near Rustic Lane in Malvern. Time estimated from radar.", "ts_dict_index": [8196, 8197, 8198]}
+{"event_id": 885494, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:15:00", "end_date_time": "2020-06-03 11:15:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on interstate 476 near the I-76 Interchange in West Conshohocken. Time estimated from radar.", "ts_dict_index": [8241, 8242, 8243]}
+{"event_id": 885495, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:15:00", "end_date_time": "2020-06-03 11:15:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires on Pennsylvania Avenue near Bridge Street in Oreland.  Time estimated from radar.", "ts_dict_index": [8253, 8254, 8255]}
+{"event_id": 885176, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:35:00", "end_date_time": "2020-06-03 10:35:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple trees and limbs snapped or downed in Fritztown.  Time estimated from radar.", "ts_dict_index": [8220, 8221, 8222]}
+{"event_id": 885170, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-06-03 10:51:00", "end_date_time": "2020-06-03 10:51:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near the intersection of Powder Valley Road and Palm Road.  Time estimated from radar.", "ts_dict_index": [8211, 8212, 8213]}
+{"event_id": 996813, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2021-12-15 18:20:00", "end_date_time": "2021-12-15 18:20:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. Emergency manager reported large tree down on a house in Clive. Time estimated from radar.", "ts_dict_index": [8184, 8185, 8186]}
+{"event_id": 885521, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:30:00", "end_date_time": "2020-06-03 11:30:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several large tree limbs snapped off near Bensalem, destroying a fence. Time estimated from radar.", "ts_dict_index": [8271, 8272, 8273]}
+{"event_id": 885639, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:13:00", "end_date_time": "2020-06-03 18:13:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree into a house on Hilltop Road in Paoli. Time estimated from radar.", "ts_dict_index": [8265, 8266, 8267]}
+{"event_id": 885633, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:11:00", "end_date_time": "2020-06-03 18:11:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on Hibernia Road near Lafayette Road in Coatsville. Time estimated from radar.", "ts_dict_index": [8268, 8269, 8270]}
+{"event_id": 885523, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:00:00", "end_date_time": "2020-06-03 11:00:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple tree branches covering the streest. Large branches between one and two inches thick. Estimated time based on radar.", "ts_dict_index": [8277, 8278, 8279]}
+{"event_id": 885219, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:00:00", "end_date_time": "2020-06-03 11:00:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees down in the Salford area.  Time estimated from radar.", "ts_dict_index": [8280, 8281, 8282]}
+{"event_id": 885206, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 10:56:00", "end_date_time": "2020-06-03 10:56:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near Trumbauersville.  Time estimated from radar.", "ts_dict_index": [8259, 8260, 8261]}
+{"event_id": 885596, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 17:20:00", "end_date_time": "2020-06-03 17:20:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree on wires on Woodward Drive in Reading. Time estimated from radar.", "ts_dict_index": [8292, 8293, 8294]}
+{"event_id": 885620, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:04:00", "end_date_time": "2020-06-03 18:04:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree and traffic light on Moores Avenue and Kelmar Avenue in Malvern. Time estimated from radar.", "ts_dict_index": [8307, 8308, 8309]}
+{"event_id": 885213, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:00:00", "end_date_time": "2020-06-03 11:00:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires in Sellersville. Time estimated from radar.", "ts_dict_index": [8304, 8305, 8306]}
+{"event_id": 885214, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 11:00:00", "end_date_time": "2020-06-03 11:00:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous trees down in Spring City.  Report via social media with photos. Time estimated from radar.", "ts_dict_index": [8298, 8299, 8300]}
+{"event_id": 885216, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 11:00:00", "end_date_time": "2020-06-03 11:00:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed limbs and power lines near Vincent. Time estimated from radar.", "ts_dict_index": [8295, 8296, 8297]}
+{"event_id": 885217, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:00:00", "end_date_time": "2020-06-03 11:00:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near Vernfield. Time estimated from radar.", "ts_dict_index": [8289, 8290, 8291]}
+{"event_id": 885630, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:10:00", "end_date_time": "2020-06-03 18:10:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on Kings Highway near Bailey Road near Downington.  Time estimated from radar.", "ts_dict_index": [8283, 8284, 8285]}
+{"event_id": 885627, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:09:00", "end_date_time": "2020-06-03 18:09:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree down on Lloyd Avenue in Malvern. Time estimated from radar.", "ts_dict_index": [8286, 8287, 8288]}
+{"event_id": 885622, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:07:00", "end_date_time": "2020-06-03 18:07:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree and wires on Monument Avenue in Malvern. Time estimated from radar.", "ts_dict_index": [8301, 8302, 8303]}
+{"event_id": 885678, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:20:00", "end_date_time": "2020-06-03 18:20:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree blocking Old Eagle School Road near Wayne. Time estimated from radar.", "ts_dict_index": [8205, 8206, 8207]}
+{"event_id": 885501, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:21:00", "end_date_time": "2020-06-03 11:21:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large trees down damaging fencing and other property at multiple residences in Davisville.  Time estimated from radar.", "ts_dict_index": [8343, 8344, 8345]}
+{"event_id": 885515, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:25:00", "end_date_time": "2020-06-03 11:25:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Trees and large limbs down in the Holland area. Time estimated from radar.", "ts_dict_index": [8316, 8317, 8318]}
+{"event_id": 885207, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 10:59:00", "end_date_time": "2020-06-03 10:59:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple large trees snapped in Spring City.", "ts_dict_index": [8331, 8332, 8333]}
+{"event_id": 885638, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:12:00", "end_date_time": "2020-06-03 18:12:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on Country Club Road near Beacon Hill Lane near Valley Forge. Time estimated from radar.", "ts_dict_index": [8337, 8338, 8339]}
+{"event_id": 885514, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:25:00", "end_date_time": "2020-06-03 11:25:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees uprooted near Churchville Park. Time estimated from radar.", "ts_dict_index": [8319, 8320, 8321]}
+{"event_id": 885512, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:25:00", "end_date_time": "2020-06-03 11:25:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple trees and power poles down on Bellevue Avenue. Report via social media with photos. County Emergency Management also reports widespread damage in Bensalem. Time estimated from radar.", "ts_dict_index": [8322, 8323, 8324]}
+{"event_id": 885204, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:55:00", "end_date_time": "2020-06-03 10:55:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of trees and power lines down near Plowville. Time estimated from radar.", "ts_dict_index": [8328, 8329, 8330]}
+{"event_id": 885210, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 10:52:00", "end_date_time": "2020-06-03 10:52:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on Schoolhouse Road near Kenilworth.  Time estimated from radar.", "ts_dict_index": [8325, 8326, 8327]}
+{"event_id": 885211, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 11:00:00", "end_date_time": "2020-06-03 11:00:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Trees and power lines down near Geigertown. Time estimated from radar.", "ts_dict_index": [8313, 8314, 8315]}
+{"event_id": 885203, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 10:53:00", "end_date_time": "2020-06-03 10:53:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near Geryville.  Time estimated from radar.", "ts_dict_index": [8340, 8341, 8342]}
+{"event_id": 885205, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 10:55:00", "end_date_time": "2020-06-03 10:55:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on Pughtown Road near Pughtown. Time estimated from radar.", "ts_dict_index": [8334, 8335, 8336]}
+{"event_id": 885520, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:26:00", "end_date_time": "2020-06-03 11:26:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large trees down in neighbors yard near Fort Washington PA. Time estimated from radar.", "ts_dict_index": [8274, 8275, 8276]}
+{"event_id": 885645, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:35:00", "end_date_time": "2020-06-03 10:35:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of tree and power line damage in the Reading area.", "ts_dict_index": [8355, 8356, 8357]}
+{"event_id": 885187, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:45:00", "end_date_time": "2020-06-03 10:45:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Building collapse caused by a tree falling into a house near Muhlenberg Park.", "ts_dict_index": [8358, 8359, 8360]}
+{"event_id": 885659, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:30:00", "end_date_time": "2020-06-03 11:30:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Bordentown NOS gauge.", "ts_dict_index": [8349, 8350, 8351]}
+{"event_id": 885189, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:50:00", "end_date_time": "2020-06-03 10:50:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of tree and power line damage near Wyomissing. Time estimated from radar.", "ts_dict_index": [8364, 8365, 8366]}
+{"event_id": 885509, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:25:00", "end_date_time": "2020-06-03 11:25:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several downed trees in the Bensalem area. Time estimated from radar.", "ts_dict_index": [8352, 8353, 8354]}
+{"event_id": 885202, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-06-03 10:53:00", "end_date_time": "2020-06-03 10:53:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near Dillingersvile. Time estimated from radar.", "ts_dict_index": [8346, 8347, 8348]}
+{"event_id": 885169, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-06-03 10:50:00", "end_date_time": "2020-06-03 10:50:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near the intersection of Palm Road and Kings Highway South.  Time estimated from radar.", "ts_dict_index": [8361, 8362, 8363]}
+{"event_id": 885212, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 11:00:00", "end_date_time": "2020-06-03 11:00:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree caused an accident on County Line Road near Boyertown.", "ts_dict_index": [8310, 8311, 8312]}
+{"event_id": 885197, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:40:00", "end_date_time": "2020-06-03 10:40:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree and wires on Cleveland Avenue in Springmont.", "ts_dict_index": [8370, 8371, 8372]}
+{"event_id": 885190, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:50:00", "end_date_time": "2020-06-03 10:50:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of trees and power lines down in Stoney Creek Mills. Time estimated from radar.", "ts_dict_index": [8367, 8368, 8369]}
+{"event_id": 885246, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:07:00", "end_date_time": "2020-06-03 11:07:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Portion of a roof blown off an apartment building in Fortuna. Time estimated from radar.", "ts_dict_index": [8427, 8428, 8429]}
+{"event_id": 885590, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 17:12:00", "end_date_time": "2020-06-03 17:12:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed power lines on Cleveland Avenue in West Lawn. Time estimated from radar.", "ts_dict_index": [8391, 8392, 8393]}
+{"event_id": 885244, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:06:00", "end_date_time": "2020-06-03 11:06:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees down near Mainland. Time estimated from radar.", "ts_dict_index": [8400, 8401, 8402]}
+{"event_id": 885487, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:12:00", "end_date_time": "2020-06-03 11:12:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Video via social media of transformers blowing during thunderstorm winds near Bridgeport. Time estimated from radar.", "ts_dict_index": [8412, 8413, 8414]}
+{"event_id": 885224, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:04:00", "end_date_time": "2020-06-03 11:04:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near Hatfield.  Time estimated from radar.", "ts_dict_index": [8424, 8425, 8426]}
+{"event_id": 885595, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 17:20:00", "end_date_time": "2020-06-03 17:20:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on wires near Octagon Avenue in West Wyomissing. Time estimated from radar.", "ts_dict_index": [8388, 8389, 8390]}
+{"event_id": 885505, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:23:00", "end_date_time": "2020-06-03 11:23:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A tree fell on the roof of a car killing one person near the intersection of Belmont Avenue and Rock Hill Road. Time estimated from radar.", "ts_dict_index": [8418, 8419, 8420]}
+{"event_id": 885242, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:05:00", "end_date_time": "2020-06-03 11:05:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large tree down in the 400 block of South Park Avenue in Trooper. Time estimated from radar.", "ts_dict_index": [8403, 8404, 8405]}
+{"event_id": 885597, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 17:22:00", "end_date_time": "2020-06-03 17:22:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. MPING report of trees down in Sinking Spring. Time estimated from radar.", "ts_dict_index": [8394, 8395, 8396]}
+{"event_id": 885225, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:04:00", "end_date_time": "2020-06-03 11:04:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple trees snapped near Skippack. Report via social media with photos. Time estimated from radar.", "ts_dict_index": [8397, 8398, 8399]}
+{"event_id": 885201, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 10:53:00", "end_date_time": "2020-06-03 10:53:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near the intersection of State Highway 23 and Coventryville Road. Time estimated from radar.", "ts_dict_index": [8385, 8386, 8387]}
+{"event_id": 885240, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 11:05:00", "end_date_time": "2020-06-03 11:05:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large tree down on a building at the Knollwood Apartments in Phoenixville. Photo shows considerable structural damage. Time estimated from radar.", "ts_dict_index": [8406, 8407, 8408]}
+{"event_id": 885486, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 11:12:00", "end_date_time": "2020-06-03 11:12:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree down on Saint Matthews Road near Birchrunville. Time estimated from radar.", "ts_dict_index": [8409, 8410, 8411]}
+{"event_id": 885200, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-06-03 10:51:00", "end_date_time": "2020-06-03 10:51:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near the intersection of Powder Valley Road and Palm Road near Hosensack. Time estimated from radar.", "ts_dict_index": [8382, 8383, 8384]}
+{"event_id": 885198, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-06-03 10:50:00", "end_date_time": "2020-06-03 10:50:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near the intersection of Palm Road and Kings Highway South near Hosensack.  Time estimated from radar.", "ts_dict_index": [8373, 8374, 8375]}
+{"event_id": 885199, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-06-03 10:50:00", "end_date_time": "2020-06-03 10:50:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of trees and power lines down near Alburtis.", "ts_dict_index": [8379, 8380, 8381]}
+{"event_id": 885221, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 11:02:00", "end_date_time": "2020-06-03 11:02:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed trees and power lines on Sycamore Road in Passmore. Time estimated from radar.", "ts_dict_index": [8376, 8377, 8378]}
+{"event_id": 885173, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:30:00", "end_date_time": "2020-06-03 10:30:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous reports of trees and wires down in North Heidelberg.  Time estimated from radar.", "ts_dict_index": [8433, 8434, 8435]}
+{"event_id": 885489, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:13:00", "end_date_time": "2020-06-03 11:13:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of trees and power lines down in the Warminster area. Time estimated from radar.", "ts_dict_index": [8439, 8440, 8441]}
+{"event_id": 885172, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:25:00", "end_date_time": "2020-06-03 10:25:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees downed on a property on River Road.  Report via social media with photos.  Time estimated from radar.", "ts_dict_index": [8430, 8431, 8432]}
+{"event_id": 885174, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 10:30:00", "end_date_time": "2020-06-03 10:30:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Trees down on wires on Christmas Village Road.  Time estimated from radar.", "ts_dict_index": [8436, 8437, 8438]}
+{"event_id": 885222, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:02:00", "end_date_time": "2020-06-03 11:02:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of trees and power lines down in the Collegeville area. Time estimated from radar.", "ts_dict_index": [8457, 8458, 8459]}
+{"event_id": 885491, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:13:00", "end_date_time": "2020-06-03 11:13:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees uprooted in Plymouth Valley.  Time estimated from radar.", "ts_dict_index": [8445, 8446, 8447]}
+{"event_id": 885490, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:13:00", "end_date_time": "2020-06-03 11:13:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several photos of uprooted trees in King of Prussia provided via social media. Time estimated from radar.", "ts_dict_index": [8442, 8443, 8444]}
+{"event_id": 885602, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 17:55:00", "end_date_time": "2020-06-03 17:55:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large tree down near the intersection of Fairview Road and Peters Lane in Glenmoore.", "ts_dict_index": [8454, 8455, 8456]}
+{"event_id": 885616, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:02:00", "end_date_time": "2020-06-03 18:03:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed wires on a vehicle on Coldstream Road in Kimberton. Time estimated from radar.", "ts_dict_index": [8448, 8449, 8450]}
+{"event_id": 885507, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:24:00", "end_date_time": "2020-06-03 11:24:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A tree fell on the roof of a car killing one person in Lower Merion along Medford Road.", "ts_dict_index": [8415, 8416, 8417]}
+{"event_id": 885615, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:00:00", "end_date_time": "2020-06-03 18:00:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree blocking Hillcrest Avenue near Forrest Avenue in Kimberton. Time estimated from radar.", "ts_dict_index": [8460, 8461, 8462]}
+{"event_id": 885599, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 17:33:00", "end_date_time": "2020-06-03 17:33:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed power lines on East Main Street and Chestnut Street in Kulptown. Time estimated from radar.", "ts_dict_index": [8466, 8467, 8468]}
+{"event_id": 885614, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:00:00", "end_date_time": "2020-06-03 18:00:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several large trees down near the intersection of Horseshoe Trail Road and Haverhill Road in Chester Springs.", "ts_dict_index": [8463, 8464, 8465]}
+{"event_id": 885488, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:12:00", "end_date_time": "2020-06-03 11:12:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree and wires down on West Main Street in Trooper.", "ts_dict_index": [8472, 8473, 8474]}
+{"event_id": 885245, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 11:07:00", "end_date_time": "2020-06-03 11:07:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous reports of power lines down in Valley Forge. Time estimated from radar.", "ts_dict_index": [8469, 8470, 8471]}
+{"event_id": 885679, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:21:00", "end_date_time": "2020-06-03 18:21:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree blocking Grubb Road near Treble Lane in Paoli. Time estimated from radar.", "ts_dict_index": [8451, 8452, 8453]}
+{"event_id": 885600, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-06-03 17:35:00", "end_date_time": "2020-06-03 17:35:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed trees and wires reported in Birdsboro. Time estimated from radar.", "ts_dict_index": [8508, 8509, 8510]}
+{"event_id": 885480, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:11:00", "end_date_time": "2020-06-03 11:11:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous reports of trees and power lines down in Warrington.  Time estimated from radar.", "ts_dict_index": [8505, 8506, 8507]}
+{"event_id": 885477, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-06-03 11:10:00", "end_date_time": "2020-06-03 11:10:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Trees and power lines down in numerous places across central Bucks County, including Chalfont. Time estimated from radar.", "ts_dict_index": [8484, 8485, 8486]}
+{"event_id": 1030987, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-05-15 15:14:00", "end_date_time": "2022-05-15 15:14:00", "narrative": "For much of the state, May 13th was the end of the heatwave as a cold front moved into the area and showers and thunderstorms developed. Thunderstorms were most widespread on the 15th with several reports of hail as large as golf balls and numerous wind damage reports. A wind gust of 58 mph was recorded at the Jacksonville/LR Air Force Base.||Some relief (cooler air) came on the 15th in the form of a cold front. At the same time, there were strong to severe storms ahead of the front.  Storms were sure to thrive given an enormous amount of energy in place. Models showed a line of storms traversing the region from northwest to southeast during the afternoon, and these were expected to unleash strong to damaging winds. Updrafts into some storms were likely to be powerful enough to suspend hailstones aloft, and allow them to grow. So, very large hail was possible. There were already a few hailstorms on the 14th, with lime size hail at Jasper (Newton County), and golf ball size hail at Harrison (Boone County). Tornadoes were much less likely because steering winds were generally weak (30 knots or less), and there was not much shear.||Between 1100 am and 1200 pm CST, a large cluster of storms arrived from Missouri. Ahead of the cluster, isolated to scattered storms erupted mainly north and west of Little Rock (Pulaski County). Golf ball size hail was reported at Boxley (Newton County) and the west side of Russellville (Pope County). There was half dollar size hail at London and just north of Russellville (both in Pope County), and quarter size stones at Chickalah (Yell County), Nimrod (Perry County), and Paris (Logan County).||As the afternoon progressed, the cluster of storms worked from northwest into central and southeast Arkansas. Numerous trees and power lines were downed, with some trees on houses. At least 50,000 power outages were noted at one point. At Russellville (Pope County), a tree fell on a vehicle, and two people had to be extricated and taken to the hospital. A tree also came down on a travel trailer close to Hazen (Prairie County). Fallen trees blocked Highway 7 near Fourche Junction (Perry County), Highway 46 at Sheridan (Grant County), and Highway 54 at Sulphur Springs (Jefferson County). Roads were blocked by trees at a campground northeast of Fifty Six (Stone County). A roof was blown off of a storage building west of Hot Springs (Garland County).||There was a 58 mph gust at the Little Rock Air Force Base (Pulaski County), a 56 mph gust at McCreanor (Lonoke County), a 55 mph gust at Little Rock National Airport (Pulaski County), and a 54 mph gust at the Stuttgart Airport in Fairmount (Prairie County). Social media showed a picture of a large tree, a foot in diameter, partially blown over, with a large limb knocked down. Additionally, the picture depicted a flag pole that was partially bent. The time is based on radar.", "ts_dict_index": [8520, 8521, 8522]}
+{"event_id": 885482, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 11:11:00", "end_date_time": "2020-06-03 11:11:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large tree down on Wall Street in Spring City. Time estimated from radar.", "ts_dict_index": [8511, 8512, 8513]}
+{"event_id": 885247, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:09:00", "end_date_time": "2020-06-03 11:09:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several large trees downed in Valley Forge National Historic Park. Multiple structures were damaged by the fallen trees. Time estimated from radar.", "ts_dict_index": [8499, 8500, 8501]}
+{"event_id": 885478, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 11:10:00", "end_date_time": "2020-06-03 11:10:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple large tree branches down and two trees snapped on golf course near Colonial Village.", "ts_dict_index": [8487, 8488, 8489]}
+{"event_id": 885479, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:10:00", "end_date_time": "2020-06-03 11:10:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree on wires at intersection of Routes 29 and 663 in Pennsburg. Time estimated from radar.", "ts_dict_index": [8490, 8491, 8492]}
+{"event_id": 831997, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2019-06-14 21:00:00", "end_date_time": "2019-06-14 21:00:00", "narrative": "For mainly southeastern portions of South Central Nebraska (mainly southeast of a York-Red Cloud line), this was an active Friday evening and early Saturday morning of thunderstorms. Things started out with a smattering of large hail reports before transitioning to mainly a heavy rain and relatively minor flash flooding event, particularly within western Nuckolls and far eastern Webster counties where rain totals of 2-4 inches were common, and highlighted by 4.72 per an unofficial mesonet west-southwest of Nelson. As for hail, the largest reported stones up to golf ball size occurred in McCool Junction and southeast of Sutton. Severe-criteria wind reports were quite limited, but a mesonet southwest of Nelson gusted to 64 MPH and a completely separate batch of storms farther west yielded a 63 MPH mesonet gust near Cambridge. The most impactful flooding report involved a multiple-hour closure of Highway 136 in far western Nuckolls County due to water over the road. In addition, runoff from heavy rain promoted minor flooding along the Republican River in southern Nuckolls County, with the automated gauge near Hardy cresting at 11.66 ft. during the very early morning hours of Sunday the 16th (flood stage 11.0 ft.).||Breaking down event evolution, severe storms initially got underway between 8-10 p.m. CDT as a cluster of semi-discrete cells erupted within Clay, Fillmore and southern York counties, yielding the majority of the evening's hail reports. Then between 10 p.m. and midnight CDT and slightly to the southwest of the initial storms, additional severe convection and flooding rains blossomed over Nuckolls and eastern Webster counties. After midnight, the most intense storms gradually weakened and/or slipped south of the state line into Kansas, although weaker activity lingered a few more hours before ending altogether. Completely separate from (and several counties to the west of) the severe convection in southeastern counties, a small cluster of storms entered Furnas County from the west shortly before midnight CDT, generating the aforementioned severe gust near Cambridge before quickly weakening. Turning to the meteorological setup, a broad quasi-zonal flow regime was present in the mid-upper levels, featuring passing low-amplitude disturbances. At the surface, the initial evening development seemed to concentrate along a subtle, west-east front, in a mesoscale environment featuring a relatively potent combination of 2000-3000 J/kg mixed-layer CAPE and around 30 knots of deep-layer wind shear. In addition, convection was aided by warm air/moisture advection along the northwestern fringes of a nocturnal low level jet primarily aligned from southern Kansas into Missouri. Estimated wind gusts of 50 to 60 MPH accompanied quarter to golf ball size hail.", "ts_dict_index": [8514, 8515, 8516]}
+{"event_id": 885484, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:11:00", "end_date_time": "2020-06-03 11:11:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous reports of trees and power lines down in Norristown. Time estimated from radar.", "ts_dict_index": [8496, 8497, 8498]}
+{"event_id": 885481, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 11:11:00", "end_date_time": "2020-06-03 11:11:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple trees down near the intersection of Spring Road and North Warren Avenue.  Time estimated from radar.", "ts_dict_index": [8478, 8479, 8480]}
+{"event_id": 885485, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 11:12:00", "end_date_time": "2020-06-03 11:12:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree down on Conestoga Road near Chester Springs.", "ts_dict_index": [8481, 8482, 8483]}
+{"event_id": 1030986, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-05-15 15:11:00", "end_date_time": "2022-05-15 15:11:00", "narrative": "For much of the state, May 13th was the end of the heatwave as a cold front moved into the area and showers and thunderstorms developed. Thunderstorms were most widespread on the 15th with several reports of hail as large as golf balls and numerous wind damage reports. A wind gust of 58 mph was recorded at the Jacksonville/LR Air Force Base.||Some relief (cooler air) came on the 15th in the form of a cold front. At the same time, there were strong to severe storms ahead of the front.  Storms were sure to thrive given an enormous amount of energy in place. Models showed a line of storms traversing the region from northwest to southeast during the afternoon, and these were expected to unleash strong to damaging winds. Updrafts into some storms were likely to be powerful enough to suspend hailstones aloft, and allow them to grow. So, very large hail was possible. There were already a few hailstorms on the 14th, with lime size hail at Jasper (Newton County), and golf ball size hail at Harrison (Boone County). Tornadoes were much less likely because steering winds were generally weak (30 knots or less), and there was not much shear.||Between 1100 am and 1200 pm CST, a large cluster of storms arrived from Missouri. Ahead of the cluster, isolated to scattered storms erupted mainly north and west of Little Rock (Pulaski County). Golf ball size hail was reported at Boxley (Newton County) and the west side of Russellville (Pope County). There was half dollar size hail at London and just north of Russellville (both in Pope County), and quarter size stones at Chickalah (Yell County), Nimrod (Perry County), and Paris (Logan County).||As the afternoon progressed, the cluster of storms worked from northwest into central and southeast Arkansas. Numerous trees and power lines were downed, with some trees on houses. At least 50,000 power outages were noted at one point. At Russellville (Pope County), a tree fell on a vehicle, and two people had to be extricated and taken to the hospital. A tree also came down on a travel trailer close to Hazen (Prairie County). Fallen trees blocked Highway 7 near Fourche Junction (Perry County), Highway 46 at Sheridan (Grant County), and Highway 54 at Sulphur Springs (Jefferson County). Roads were blocked by trees at a campground northeast of Fifty Six (Stone County). A roof was blown off of a storage building west of Hot Springs (Garland County).||There was a 58 mph gust at the Little Rock Air Force Base (Pulaski County), a 56 mph gust at McCreanor (Lonoke County), a 55 mph gust at Little Rock National Airport (Pulaski County), and a 54 mph gust at the Stuttgart Airport in Fairmount (Prairie County). A 50 KT peak wind gust (58 mph) was recorded at the Little Rock Air Force Base weather station.", "ts_dict_index": [8523, 8524, 8525]}
+{"event_id": 885171, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 10:53:00", "end_date_time": "2020-06-03 10:53:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near the intersection of State Highway 23 and Coventryville Road.  Time estimated from radar.", "ts_dict_index": [8493, 8494, 8495]}
+{"event_id": 885617, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-06-03 18:04:00", "end_date_time": "2020-06-03 18:04:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed wires on Conestoga Road near Lancaster Avenue in Malvern. Time estimated from radar.", "ts_dict_index": [8502, 8503, 8504]}
+{"event_id": 885500, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:20:00", "end_date_time": "2020-06-03 11:20:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A tree crased through the roof of a building at the Philmont Country Club in Lower Moreland Township killing one employee.", "ts_dict_index": [8421, 8422, 8423]}
+{"event_id": 1030984, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-05-15 15:10:00", "end_date_time": "2022-05-15 15:10:00", "narrative": "For much of the state, May 13th was the end of the heatwave as a cold front moved into the area and showers and thunderstorms developed. Thunderstorms were most widespread on the 15th with several reports of hail as large as golf balls and numerous wind damage reports. A wind gust of 58 mph was recorded at the Jacksonville/LR Air Force Base.||Some relief (cooler air) came on the 15th in the form of a cold front. At the same time, there were strong to severe storms ahead of the front.  Storms were sure to thrive given an enormous amount of energy in place. Models showed a line of storms traversing the region from northwest to southeast during the afternoon, and these were expected to unleash strong to damaging winds. Updrafts into some storms were likely to be powerful enough to suspend hailstones aloft, and allow them to grow. So, very large hail was possible. There were already a few hailstorms on the 14th, with lime size hail at Jasper (Newton County), and golf ball size hail at Harrison (Boone County). Tornadoes were much less likely because steering winds were generally weak (30 knots or less), and there was not much shear.||Between 1100 am and 1200 pm CST, a large cluster of storms arrived from Missouri. Ahead of the cluster, isolated to scattered storms erupted mainly north and west of Little Rock (Pulaski County). Golf ball size hail was reported at Boxley (Newton County) and the west side of Russellville (Pope County). There was half dollar size hail at London and just north of Russellville (both in Pope County), and quarter size stones at Chickalah (Yell County), Nimrod (Perry County), and Paris (Logan County).||As the afternoon progressed, the cluster of storms worked from northwest into central and southeast Arkansas. Numerous trees and power lines were downed, with some trees on houses. At least 50,000 power outages were noted at one point. At Russellville (Pope County), a tree fell on a vehicle, and two people had to be extricated and taken to the hospital. A tree also came down on a travel trailer close to Hazen (Prairie County). Fallen trees blocked Highway 7 near Fourche Junction (Perry County), Highway 46 at Sheridan (Grant County), and Highway 54 at Sulphur Springs (Jefferson County). Roads were blocked by trees at a campground northeast of Fifty Six (Stone County). A roof was blown off of a storage building west of Hot Springs (Garland County).||There was a 58 mph gust at the Little Rock Air Force Base (Pulaski County), a 56 mph gust at McCreanor (Lonoke County), a 55 mph gust at Little Rock National Airport (Pulaski County), and a 54 mph gust at the Stuttgart Airport in Fairmount (Prairie County). A tree fell on a power line on North Hills Blvd. just north of Crestwood.", "ts_dict_index": [8526, 8527, 8528]}
+{"event_id": 1030983, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-05-15 15:08:00", "end_date_time": "2022-05-15 15:08:00", "narrative": "For much of the state, May 13th was the end of the heatwave as a cold front moved into the area and showers and thunderstorms developed. Thunderstorms were most widespread on the 15th with several reports of hail as large as golf balls and numerous wind damage reports. A wind gust of 58 mph was recorded at the Jacksonville/LR Air Force Base.||Some relief (cooler air) came on the 15th in the form of a cold front. At the same time, there were strong to severe storms ahead of the front.  Storms were sure to thrive given an enormous amount of energy in place. Models showed a line of storms traversing the region from northwest to southeast during the afternoon, and these were expected to unleash strong to damaging winds. Updrafts into some storms were likely to be powerful enough to suspend hailstones aloft, and allow them to grow. So, very large hail was possible. There were already a few hailstorms on the 14th, with lime size hail at Jasper (Newton County), and golf ball size hail at Harrison (Boone County). Tornadoes were much less likely because steering winds were generally weak (30 knots or less), and there was not much shear.||Between 1100 am and 1200 pm CST, a large cluster of storms arrived from Missouri. Ahead of the cluster, isolated to scattered storms erupted mainly north and west of Little Rock (Pulaski County). Golf ball size hail was reported at Boxley (Newton County) and the west side of Russellville (Pope County). There was half dollar size hail at London and just north of Russellville (both in Pope County), and quarter size stones at Chickalah (Yell County), Nimrod (Perry County), and Paris (Logan County).||As the afternoon progressed, the cluster of storms worked from northwest into central and southeast Arkansas. Numerous trees and power lines were downed, with some trees on houses. At least 50,000 power outages were noted at one point. At Russellville (Pope County), a tree fell on a vehicle, and two people had to be extricated and taken to the hospital. A tree also came down on a travel trailer close to Hazen (Prairie County). Fallen trees blocked Highway 7 near Fourche Junction (Perry County), Highway 46 at Sheridan (Grant County), and Highway 54 at Sulphur Springs (Jefferson County). Roads were blocked by trees at a campground northeast of Fifty Six (Stone County). A roof was blown off of a storage building west of Hot Springs (Garland County).||There was a 58 mph gust at the Little Rock Air Force Base (Pulaski County), a 56 mph gust at McCreanor (Lonoke County), a 55 mph gust at Little Rock National Airport (Pulaski County), and a 54 mph gust at the Stuttgart Airport in Fairmount (Prairie County). A large tree was knocked down and partially blocking Jacksonville-Cato Rd. between Gibson and Gravel Ridge.", "ts_dict_index": [8529, 8530, 8531]}
+{"event_id": 964030, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-06-24 16:43:00", "end_date_time": "2021-06-24 16:43:00", "narrative": "For about three hours on this Thursday afternoon, the southeastern quadrant of South Central Nebraska saw a flare-up of eastward-tracking, strong-to-severe thunderstorms, yielding fairly localized swaths of large hail up to golf ball size and wind gusts estimated up to around 70 MPH. All hail reports were actually associated with the first severe storm of the day, an initially-isolated cell that rumbled along the borders between Adams/Hall and Clay/Hamilton counties mainly 4-5 p.m. CDT, dropping stones up to golf ball size in Hansen and Trumbull. During nearly that same time frame, a separate severe-warned storm (unverified) blossomed about 25 miles to the south, advancing from northern Webster into southern Clay County. By 5 p.m. CDT these two storms had merged into a small-scale complex over eastern Clay County, signaling a transition to more of a damaging wind threat as it marched across Fillmore County over the next hour. Along the way, tree damage was reported near Milligan and Exeter, and estimated 70 MPH gusts overturned irrigation pivots near Grafton. By 6:30 p.m. this convection departed Fillmore County to the east, ending this relatively brief/localized round of severe storms within South Central Nebraska.||As for the meteorological background, the local area resided under quasi-zonal flow in the mid-upper levels, well-downstream from an upper low just off the California coast that was ejecting various low-amplitude disturbances east-northeastward into the Central Plains. One of these upper waves arrived on scene into central Nebraska by mid-afternoon, likely sparking rapid convective initiation despite quite a bit of afternoon cloud cover and resultant questions about the degree of available instability. At the surface, these storms initiated slightly to the north-northwest (cool side) of a quasi-stationary front extending northeastward from a weak-but-evident low pressure center over central KS (around 1004 millibars at 21Z). Despite the aforementioned mostly cloudy skies over South Central Nebraska holding afternoon temperatures down in the upper 70-low 80s (F) most places, the combination of plentiful low-level moisture (dewpoints upper 60s/around 70), weak convergence along the surface frontal zone and favorable timing of the incoming mid-level wave proved sufficient for severe storm development. Mid-afternoon mesoscale parameters in the area of concern featured a decent combination of up to 2000 J/kg mixed-layer CAPE and 40 knots of deep-layer wind shear. Wind gusts estimated to be near 60 MPH resulted in tree damage in the area. Some limbs were down on Highway 6 between Roads 18 and 19.", "ts_dict_index": [8541, 8542, 8543]}
+{"event_id": 964027, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-06-24 16:12:00", "end_date_time": "2021-06-24 16:12:00", "narrative": "For about three hours on this Thursday afternoon, the southeastern quadrant of South Central Nebraska saw a flare-up of eastward-tracking, strong-to-severe thunderstorms, yielding fairly localized swaths of large hail up to golf ball size and wind gusts estimated up to around 70 MPH. All hail reports were actually associated with the first severe storm of the day, an initially-isolated cell that rumbled along the borders between Adams/Hall and Clay/Hamilton counties mainly 4-5 p.m. CDT, dropping stones up to golf ball size in Hansen and Trumbull. During nearly that same time frame, a separate severe-warned storm (unverified) blossomed about 25 miles to the south, advancing from northern Webster into southern Clay County. By 5 p.m. CDT these two storms had merged into a small-scale complex over eastern Clay County, signaling a transition to more of a damaging wind threat as it marched across Fillmore County over the next hour. Along the way, tree damage was reported near Milligan and Exeter, and estimated 70 MPH gusts overturned irrigation pivots near Grafton. By 6:30 p.m. this convection departed Fillmore County to the east, ending this relatively brief/localized round of severe storms within South Central Nebraska.||As for the meteorological background, the local area resided under quasi-zonal flow in the mid-upper levels, well-downstream from an upper low just off the California coast that was ejecting various low-amplitude disturbances east-northeastward into the Central Plains. One of these upper waves arrived on scene into central Nebraska by mid-afternoon, likely sparking rapid convective initiation despite quite a bit of afternoon cloud cover and resultant questions about the degree of available instability. At the surface, these storms initiated slightly to the north-northwest (cool side) of a quasi-stationary front extending northeastward from a weak-but-evident low pressure center over central KS (around 1004 millibars at 21Z). Despite the aforementioned mostly cloudy skies over South Central Nebraska holding afternoon temperatures down in the upper 70-low 80s (F) most places, the combination of plentiful low-level moisture (dewpoints upper 60s/around 70), weak convergence along the surface frontal zone and favorable timing of the incoming mid-level wave proved sufficient for severe storm development. Mid-afternoon mesoscale parameters in the area of concern featured a decent combination of up to 2000 J/kg mixed-layer CAPE and 40 knots of deep-layer wind shear. Wind gusts estimated to be near 70 MPH knocked three irrigation pivots over near Road H between Roads 5 and 6.", "ts_dict_index": [8547, 8548, 8549]}
+{"event_id": 964023, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-06-24 15:26:00", "end_date_time": "2021-06-24 15:26:00", "narrative": "For about three hours on this Thursday afternoon, the southeastern quadrant of South Central Nebraska saw a flare-up of eastward-tracking, strong-to-severe thunderstorms, yielding fairly localized swaths of large hail up to golf ball size and wind gusts estimated up to around 70 MPH. All hail reports were actually associated with the first severe storm of the day, an initially-isolated cell that rumbled along the borders between Adams/Hall and Clay/Hamilton counties mainly 4-5 p.m. CDT, dropping stones up to golf ball size in Hansen and Trumbull. During nearly that same time frame, a separate severe-warned storm (unverified) blossomed about 25 miles to the south, advancing from northern Webster into southern Clay County. By 5 p.m. CDT these two storms had merged into a small-scale complex over eastern Clay County, signaling a transition to more of a damaging wind threat as it marched across Fillmore County over the next hour. Along the way, tree damage was reported near Milligan and Exeter, and estimated 70 MPH gusts overturned irrigation pivots near Grafton. By 6:30 p.m. this convection departed Fillmore County to the east, ending this relatively brief/localized round of severe storms within South Central Nebraska.||As for the meteorological background, the local area resided under quasi-zonal flow in the mid-upper levels, well-downstream from an upper low just off the California coast that was ejecting various low-amplitude disturbances east-northeastward into the Central Plains. One of these upper waves arrived on scene into central Nebraska by mid-afternoon, likely sparking rapid convective initiation despite quite a bit of afternoon cloud cover and resultant questions about the degree of available instability. At the surface, these storms initiated slightly to the north-northwest (cool side) of a quasi-stationary front extending northeastward from a weak-but-evident low pressure center over central KS (around 1004 millibars at 21Z). Despite the aforementioned mostly cloudy skies over South Central Nebraska holding afternoon temperatures down in the upper 70-low 80s (F) most places, the combination of plentiful low-level moisture (dewpoints upper 60s/around 70), weak convergence along the surface frontal zone and favorable timing of the incoming mid-level wave proved sufficient for severe storm development. Mid-afternoon mesoscale parameters in the area of concern featured a decent combination of up to 2000 J/kg mixed-layer CAPE and 40 knots of deep-layer wind shear. Wind gusts estimated to be near 60 MPH resulted in minor tree damage in town.", "ts_dict_index": [8544, 8545, 8546]}
+{"event_id": 964029, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2021-06-24 16:40:00", "end_date_time": "2021-06-24 16:40:00", "narrative": "For about three hours on this Thursday afternoon, the southeastern quadrant of South Central Nebraska saw a flare-up of eastward-tracking, strong-to-severe thunderstorms, yielding fairly localized swaths of large hail up to golf ball size and wind gusts estimated up to around 70 MPH. All hail reports were actually associated with the first severe storm of the day, an initially-isolated cell that rumbled along the borders between Adams/Hall and Clay/Hamilton counties mainly 4-5 p.m. CDT, dropping stones up to golf ball size in Hansen and Trumbull. During nearly that same time frame, a separate severe-warned storm (unverified) blossomed about 25 miles to the south, advancing from northern Webster into southern Clay County. By 5 p.m. CDT these two storms had merged into a small-scale complex over eastern Clay County, signaling a transition to more of a damaging wind threat as it marched across Fillmore County over the next hour. Along the way, tree damage was reported near Milligan and Exeter, and estimated 70 MPH gusts overturned irrigation pivots near Grafton. By 6:30 p.m. this convection departed Fillmore County to the east, ending this relatively brief/localized round of severe storms within South Central Nebraska.||As for the meteorological background, the local area resided under quasi-zonal flow in the mid-upper levels, well-downstream from an upper low just off the California coast that was ejecting various low-amplitude disturbances east-northeastward into the Central Plains. One of these upper waves arrived on scene into central Nebraska by mid-afternoon, likely sparking rapid convective initiation despite quite a bit of afternoon cloud cover and resultant questions about the degree of available instability. At the surface, these storms initiated slightly to the north-northwest (cool side) of a quasi-stationary front extending northeastward from a weak-but-evident low pressure center over central KS (around 1004 millibars at 21Z). Despite the aforementioned mostly cloudy skies over South Central Nebraska holding afternoon temperatures down in the upper 70-low 80s (F) most places, the combination of plentiful low-level moisture (dewpoints upper 60s/around 70), weak convergence along the surface frontal zone and favorable timing of the incoming mid-level wave proved sufficient for severe storm development. Mid-afternoon mesoscale parameters in the area of concern featured a decent combination of up to 2000 J/kg mixed-layer CAPE and 40 knots of deep-layer wind shear. Wind gusts estimated to be near 60 MPH resulted in minor tree damage near Road P and Road 23.", "ts_dict_index": [8535, 8536, 8537]}
+{"event_id": 964026, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-06-24 16:00:00", "end_date_time": "2021-06-24 16:00:00", "narrative": "For about three hours on this Thursday afternoon, the southeastern quadrant of South Central Nebraska saw a flare-up of eastward-tracking, strong-to-severe thunderstorms, yielding fairly localized swaths of large hail up to golf ball size and wind gusts estimated up to around 70 MPH. All hail reports were actually associated with the first severe storm of the day, an initially-isolated cell that rumbled along the borders between Adams/Hall and Clay/Hamilton counties mainly 4-5 p.m. CDT, dropping stones up to golf ball size in Hansen and Trumbull. During nearly that same time frame, a separate severe-warned storm (unverified) blossomed about 25 miles to the south, advancing from northern Webster into southern Clay County. By 5 p.m. CDT these two storms had merged into a small-scale complex over eastern Clay County, signaling a transition to more of a damaging wind threat as it marched across Fillmore County over the next hour. Along the way, tree damage was reported near Milligan and Exeter, and estimated 70 MPH gusts overturned irrigation pivots near Grafton. By 6:30 p.m. this convection departed Fillmore County to the east, ending this relatively brief/localized round of severe storms within South Central Nebraska.||As for the meteorological background, the local area resided under quasi-zonal flow in the mid-upper levels, well-downstream from an upper low just off the California coast that was ejecting various low-amplitude disturbances east-northeastward into the Central Plains. One of these upper waves arrived on scene into central Nebraska by mid-afternoon, likely sparking rapid convective initiation despite quite a bit of afternoon cloud cover and resultant questions about the degree of available instability. At the surface, these storms initiated slightly to the north-northwest (cool side) of a quasi-stationary front extending northeastward from a weak-but-evident low pressure center over central KS (around 1004 millibars at 21Z). Despite the aforementioned mostly cloudy skies over South Central Nebraska holding afternoon temperatures down in the upper 70-low 80s (F) most places, the combination of plentiful low-level moisture (dewpoints upper 60s/around 70), weak convergence along the surface frontal zone and favorable timing of the incoming mid-level wave proved sufficient for severe storm development. Mid-afternoon mesoscale parameters in the area of concern featured a decent combination of up to 2000 J/kg mixed-layer CAPE and 40 knots of deep-layer wind shear. A wind gust of 58 MPH was measured by a mesonet station located 2 miles east of Edgar.", "ts_dict_index": [8538, 8539, 8540]}
+{"event_id": 1030980, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-05-15 15:08:00", "end_date_time": "2022-05-15 15:08:00", "narrative": "For much of the state, May 13th was the end of the heatwave as a cold front moved into the area and showers and thunderstorms developed. Thunderstorms were most widespread on the 15th with several reports of hail as large as golf balls and numerous wind damage reports. A wind gust of 58 mph was recorded at the Jacksonville/LR Air Force Base.||Some relief (cooler air) came on the 15th in the form of a cold front. At the same time, there were strong to severe storms ahead of the front.  Storms were sure to thrive given an enormous amount of energy in place. Models showed a line of storms traversing the region from northwest to southeast during the afternoon, and these were expected to unleash strong to damaging winds. Updrafts into some storms were likely to be powerful enough to suspend hailstones aloft, and allow them to grow. So, very large hail was possible. There were already a few hailstorms on the 14th, with lime size hail at Jasper (Newton County), and golf ball size hail at Harrison (Boone County). Tornadoes were much less likely because steering winds were generally weak (30 knots or less), and there was not much shear.||Between 1100 am and 1200 pm CST, a large cluster of storms arrived from Missouri. Ahead of the cluster, isolated to scattered storms erupted mainly north and west of Little Rock (Pulaski County). Golf ball size hail was reported at Boxley (Newton County) and the west side of Russellville (Pope County). There was half dollar size hail at London and just north of Russellville (both in Pope County), and quarter size stones at Chickalah (Yell County), Nimrod (Perry County), and Paris (Logan County).||As the afternoon progressed, the cluster of storms worked from northwest into central and southeast Arkansas. Numerous trees and power lines were downed, with some trees on houses. At least 50,000 power outages were noted at one point. At Russellville (Pope County), a tree fell on a vehicle, and two people had to be extricated and taken to the hospital. A tree also came down on a travel trailer close to Hazen (Prairie County). Fallen trees blocked Highway 7 near Fourche Junction (Perry County), Highway 46 at Sheridan (Grant County), and Highway 54 at Sulphur Springs (Jefferson County). Roads were blocked by trees at a campground northeast of Fifty Six (Stone County). A roof was blown off of a storage building west of Hot Springs (Garland County).||There was a 58 mph gust at the Little Rock Air Force Base (Pulaski County), a 56 mph gust at McCreanor (Lonoke County), a 55 mph gust at Little Rock National Airport (Pulaski County), and a 54 mph gust at the Stuttgart Airport in Fairmount (Prairie County). A social media picture showed a large tree over two feet in diameter blown over on |Cedar Creek Rd. in North Little Rock. Power lines were also knocked down in the area.", "ts_dict_index": [8532, 8533, 8534]}
+{"event_id": 1030990, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-05-15 15:26:00", "end_date_time": "2022-05-15 15:26:00", "narrative": "For much of the state, May 13th was the end of the heatwave as a cold front moved into the area and showers and thunderstorms developed. Thunderstorms were most widespread on the 15th with several reports of hail as large as golf balls and numerous wind damage reports. A wind gust of 58 mph was recorded at the Jacksonville/LR Air Force Base.||Some relief (cooler air) came on the 15th in the form of a cold front. At the same time, there were strong to severe storms ahead of the front.  Storms were sure to thrive given an enormous amount of energy in place. Models showed a line of storms traversing the region from northwest to southeast during the afternoon, and these were expected to unleash strong to damaging winds. Updrafts into some storms were likely to be powerful enough to suspend hailstones aloft, and allow them to grow. So, very large hail was possible. There were already a few hailstorms on the 14th, with lime size hail at Jasper (Newton County), and golf ball size hail at Harrison (Boone County). Tornadoes were much less likely because steering winds were generally weak (30 knots or less), and there was not much shear.||Between 1100 am and 1200 pm CST, a large cluster of storms arrived from Missouri. Ahead of the cluster, isolated to scattered storms erupted mainly north and west of Little Rock (Pulaski County). Golf ball size hail was reported at Boxley (Newton County) and the west side of Russellville (Pope County). There was half dollar size hail at London and just north of Russellville (both in Pope County), and quarter size stones at Chickalah (Yell County), Nimrod (Perry County), and Paris (Logan County).||As the afternoon progressed, the cluster of storms worked from northwest into central and southeast Arkansas. Numerous trees and power lines were downed, with some trees on houses. At least 50,000 power outages were noted at one point. At Russellville (Pope County), a tree fell on a vehicle, and two people had to be extricated and taken to the hospital. A tree also came down on a travel trailer close to Hazen (Prairie County). Fallen trees blocked Highway 7 near Fourche Junction (Perry County), Highway 46 at Sheridan (Grant County), and Highway 54 at Sulphur Springs (Jefferson County). Roads were blocked by trees at a campground northeast of Fifty Six (Stone County). A roof was blown off of a storage building west of Hot Springs (Garland County).||There was a 58 mph gust at the Little Rock Air Force Base (Pulaski County), a 56 mph gust at McCreanor (Lonoke County), a 55 mph gust at Little Rock National Airport (Pulaski County), and a 54 mph gust at the Stuttgart Airport in Fairmount (Prairie County). A social media picture showed a pontoon boat in the Ashley Downs Subdivision that had been blown away from it's original resting location into a drainage area behind the owner's house. The boat was upright on it's trailer and relatively undamaged.", "ts_dict_index": [8517, 8518, 8519]}
+{"event_id": 879891, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-12 19:23:00", "end_date_time": "2020-04-12 19:23:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. A 64 mph wind gust was measured at Barksdale Air Force Base (KBAD) in Bossier City.", "ts_dict_index": [8553, 8554, 8555]}
+{"event_id": 879889, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-12 19:12:00", "end_date_time": "2020-04-12 19:12:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. A NWS employee estimated 60-70 mph winds in the University Terrace subdivision in Southeast Shreveport. Numerous large limbs were snapped, and small trees along Youree Drive were uprooted. Power was also out in the area as well.", "ts_dict_index": [8565, 8566, 8567]}
+{"event_id": 877503, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-12 08:52:00", "end_date_time": "2020-04-12 08:52:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. A large tree fell onto a home in the Shady Grove neighborhood.", "ts_dict_index": [8568, 8569, 8570]}
+{"event_id": 965487, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2021-06-19 22:40:00", "end_date_time": "2021-06-19 22:40:00", "narrative": "Between 9 p.m. and 1 a.m. CDT on this Saturday evening into very early Sunday morning, the northern section of a fairly compact, but localized-intense mesoscale convective system (MCS) centered along the Nebraska-Kansas border took aim on mainly far southern portions of South Central Nebraska. Although available mesonets within the majority of affected counties clocked wind speeds no higher than 57 MPH, there was clearly a narrow swath of notably-higher winds that caused minor to moderate damage, particularly along the apex of a bowing segment that peaked in intensity within southern Franklin and Webster counties between 10-11 p.m. CDT. The most noteworthy damage reports originated from Franklin itself, where multiple trees were downed and some minor structural damage occurred. In the aftermath of the storm, the front page headline of the Franklin County Chronicle declared Chain Saws Hum on Father's Day. Just downstream in north central Webster County, a roof was ripped off of a motor home. After peaking in intensity within those counties, winds gradually weakened as the bowing segment pushed farther east-northeast, with the final, marginally-severe report of the night consisting of estimated 50-60 MPH winds in east-central Clay County. ||This MCS first organized and intensified to severe levels within northeast Colorado between 5-7 p.m. CDT, with its northern edge invading South Central Nebraska into Furnas/Harlan counties between 9-10 p.m. CDT and eventually departing the local area out of Fillmore/Thayer counties between 12-1 a.m. CDT. Turning to the meteorology behind this event, this was a fairly classic setup for High Plains MCS development. In the mid-upper levels, broad west-northwesterly flow prevailed over the region, with forcing aided by a low amplitude shortwave trough. At the surface, South Central Nebraska resided to the north of a west-east oriented quasi-stationary front draped through central Kansas. This placed the local area in an easterly wind regime and within the northern reaches of a low-level moisture/instability gradient. During the early evening, a rather unstable airmass occupied far southern local counties ahead of the approaching convective complex, with dewpoints well into the 60s (F) promoting mixed-layer CAPE of 2000-3000 J/kg. Although effective bulk shear was not overly-strong (only around 35 knots), the combination of a surging cold pool and the development of a 30-40 knot southerly low level jet aided MCS intensification. Thunderstorm wind gusts of 50 to 60 mph occurred near Road T and Road 311.", "ts_dict_index": [8550, 8551, 8552]}
+{"event_id": 877535, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-12 09:05:00", "end_date_time": "2020-04-12 09:05:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. A large tree was snapped and fell onto a home on Spring Branch Road near Lake Bistineau. A porch structure was also blown off of a residence on Spring Branch Road. Multiple other trees were blown down along Spring Ranch and Teague Roads.", "ts_dict_index": [8559, 8560, 8561]}
+{"event_id": 879893, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-12 19:37:00", "end_date_time": "2020-04-12 19:37:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. Trees were downed in the Tall Timbers subdivision.", "ts_dict_index": [8571, 8572, 8573]}
+{"event_id": 879898, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2020-04-12 18:55:00", "end_date_time": "2020-04-12 18:55:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. Two trees were uprooted along John Edwards Road. Quarter size hail also fell in this location as well.", "ts_dict_index": [8574, 8575, 8576]}
+{"event_id": 877552, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-04-12 09:19:00", "end_date_time": "2020-04-12 09:19:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. A tree was blown onto a home on North Main Street in Heflin. Another tree also fell through a home in Heflin.", "ts_dict_index": [8556, 8557, 8558]}
+{"event_id": 885483, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-06-03 11:11:00", "end_date_time": "2020-06-03 11:11:00", "narrative": "An area of thunderstorms, some of them severe, moved from northwest to southeast across southeastern Pennsylvania during the mid-morning hours on Wednesday, June 3rd.  Then a derecho, which developed just southeast of Lake Erie during the early morning hours, moved rapidly southeast across Pennsylvania before exiting off the New Jersey coast by early afternoon (130 PM). Damaging winds associated with this derecho were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread.  Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey.  Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows:  83 MPH at Reading Regional Airport (Berks County), 76 MPH in Pottstown (Montgomery County), 75 MPH in Malvern (Chester County), and 71 MPH in the Holmesburg section of Philadelphia.  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning, heavy rain, and a few instances of hail were also reported throughout the area.  ||Tragically, four deaths were reported in eastern Pennsylvania as a result of these severe wind gusts.  Three fatalities in Montgomery County were due directly to falling trees.  The fourth fatality in Delaware County was due to a house fire caused by an electrical malfunction from a fallen tree.  This is the highest number of fatalities from a derecho event in Pennsylvania since 1950.  ||Over 208,000 power outages were reported in southeastern Pennsylvania as a result |of fallen trees on power lines.  Some localities were without power for several days. Numerous road closures were also reported due to fallen trees.|A seven story 150 unit apartment building took severe roof damage in Lansdale Borough, Montgomery County. The Montgomery County Community Based COVID-19 Testing Site shut down at noon due to the storms. Personnel took shelter and reported minor property damage.||Because this derecho moved off the coast by 130 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day.  Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport.  The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree in wires near Exit 18 of Interstate 476 in Conshohocken. Time estimated from radar.", "ts_dict_index": [8475, 8476, 8477]}
+{"event_id": 978044, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2021-08-20 16:40:00", "end_date_time": "2021-08-20 16:50:00", "narrative": "Severe weather only clipped the far southeastern fringes of the 24-county South Central Nebraska area on this Friday afternoon, but it was an active few hours within especially Thayer County as an initially-isolated severe storm gradually grew upscale into more of a linear complex as it rumbled eastward across much of the county before departing the local area into southeast Nebraska. Although penny size hail was reported at Oak in Nuckolls County shortly after convective initiation, all severe-criteria reports emanated from Thayer County, highlighted by: hail up to ping pong ball size about halfway between Davenport and Deshler; estimated 65 MPH wind gusts along with pea to ping pong ball size hail in the Gilead area, including a social media report of a swath of corn and soybean crops at least 50 percent defoliated. ||This storm first developed/intensified over eastern Nuckolls County around 4 p.m. CDT,  along a well-defined late summer cold front gradually progressing across the region from west-to-east. During the next two hours, it first drifted northeast but then turned more east, primarily impacting northern and eastern section of Thayer County (and possibly extreme southern Fillmore County) along the way before fully departing the eastern fringes of the local area by 6:30 p.m. CDT. While the storm initially exhibited some supercell characteristics, including a brief wall cloud reported by emergency management, it gradually grew upscale/linear across the eastern half of Thayer County (the beginning stages of a larger-scale squall line that impacted parts of southeast Nebraska/northeast Kansas). In the mid-upper levels, forcing was seasonably-decent, with South Central Nebraska receiving a glancing blow from a potent, negatively-tilted shortwave trough swinging northeastward across the Dakotas during the afternoon-evening. However, the aforementioned surface cold front was the main synoptic feature in play, trailing southward through the far eastern portions of South Central Nebraska at mid-afternoon from a deepening 1000-millibar low pressure center over eastern ND. Along and just ahead of this front a very unstable airmass awaited, with the surface temperature/dewpoint in Hebron at 4 p.m. CDT registering 90/77 (F). Around this same time, mesoscale parameters featured 3000-4000 J/kg mixed-layer CAPE and 30-40 knots of deep-layer wind shear. Wind gusts were estimated to be at least 65 MPH along this path. A social media report stated the wind, combined with pea to approximately ping pong ball sized hail, resulted in corn and beans being defoliated by at least 50 percent near Gilead.", "ts_dict_index": [8583, 8584, 8585]}
+{"event_id": 877542, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-04-12 09:09:00", "end_date_time": "2020-04-12 09:09:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. Numerous trees were snapped by straight line winds along Plum Orchard Road.", "ts_dict_index": [8577, 8578, 8579]}
+{"event_id": 835571, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2019-07-10 04:25:00", "end_date_time": "2019-07-10 04:25:00", "narrative": "Isolated reports of severe winds and hail occurred after midnight on this Wednesday. During the evening hours of Tuesday, scattered thunderstorms were over southwest Nebraska. Around midnight CST, these storms began to intensify, and the easternmost storms began moving into south central Nebraska. One storm tracked across Furnas, Harlan, and Franklin counties, just north of Highway 136. This storm probably produced severe hail along much of its track but, due to the time of night, the only report received was quarter size hail in northwest Franklin county. Storms south of North Platte grew upscale into a short squall line that exhibited a bowing structure at times. This line of storms entered Gosper and Furnas counties around 130 AM CST. It continued moving southeast, affecting Harlan county as well, through 3 AM CST. Measured wind gusts of 69 MPH and 63 MPH were reported near and 6 miles east of Oxford, respectively. The northern portion of this line merged with the isolated severe storm over Franklin county. Meanwhile, a short east-west oriented line of storms erupted over Webster and Nuckolls counties around 230 AM CST. As this line blossomed, the squall line to the west quickly moved in and merged with it, with the squall line dominating the progression of the convection. The squall line continued moving east-southeast, affecting Thayer county as well through 430 AM CST. Hail up to 1.25 inches in diameter was reported in Ruskin, and winds were measured as high as 58 mph just south of Deshler. The duration of heavy rainfall was maximized over western Nuckolls county, where the east-west line developed, followed by the northern end of the squall line moving east from Webster county. This resulted in a swath of more than 2 inches of rain, with the highest amount 2.83 inches 8 miles northwest of Superior. In Ruskin, 2.48 inches was measured.||These storms occurred along and near a cold front that was associated with occluded low pressure over North Dakota. A fairly potent shortwave trough was over the Dakota's, embedded within the Westerlies which were located across the Northern United States. Just ahead of the thunderstorms, temperatures were in the lower to middle 70s, and dewpoints were in the lower 70s. Mid-level lapse rates were 6.5 to 7.0 deg C/km, resulting in MUCAPE between 2000 and 3000 J/kg. Effective deep layer shear was 35-40 kt. A 58 MPH wind gust was measured by a mesonet station located 3 miles south-southeast of Deshler.", "ts_dict_index": [8586, 8587, 8588]}
+{"event_id": 943099, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2021-04-04 18:22:00", "end_date_time": "2021-04-04 18:22:00", "narrative": "During the late afternoon and evening of Sunday the 4th, scattered, high-based showers and a few thunderstorms affected portions of South Central Nebraska. While the vast majority of this activity was sub-severe, several instances of gusty winds peaking mainly 50-56 MPH transpired under the primary convective cluster as it tracked east-northeast within a 20-30 mile wide corridor roughly centered along a line from Beaver City-Minden-Hastings/Grand Island-Central City. The one known exception to the prevailing sub-severe nature of these winds occurred at Hastings Municipal Airport, where the ASOS clocked a rogue gust of 63 MPH (there were no damage reports). Other slightly sub-severe gusts (all from unofficial mesonet sensors) included: 56 MPH at Hildreth and near Oxford, 55 MPH near Stamford, Odessa and Heartwell; and 54 MPH seven miles west of Macon. ||This was a classic early-spring setup for high-based convection with gusty winds. The 4th was the first truly unseasonably-warm day of the season as temperatures soared into the upper-80s to around 90 degrees (F). Meanwhile, low-level moisture was scant, with late afternoon/early evening dewpoints mainly mid-30s to low 40s F (yielding significant dewpoint depressions of 40-50 F) . In the mid-upper levels, broad and fairly weak zonal flow resided over the Central Plains. However, as a fairly subtle disturbance emerged off the High Plains late in the day, weak convergence near a surface low along western portions of the Nebraska/Kansas border helped ignite convection near the extreme southwestern fringes of South Central Nebraska as early as 3-4 p.m. CDT. Despite the notable dewpoint depressions, very steep low-mid level lapse rates in the hot, well-mixed environment yielded mixed-layer CAPE up to around 500 J/kg, but in the presence of only modest deep-layer wind shear around 25-30 knots. Despite the seemingly-unimpressive instability/shear environment, the very high-based convection (LCL heights around 3 km) had as much as 1000-1500 J/kg downdraft CAPE at its disposal...clearly sufficient for a number of strong (isolated marginally-severe) gusts. Timing-wise, the main cluster tracked through the Furnas/Gosper/Harlan counties area between 4-6 p.m. CDT, reached the Highway 281 corridor between Grand Island and Hastings by around 7 p.m. CDT, and finally started losing its punch in the eastern Merrick/Polk counties area between 8-9 p.m. CDT. ", "ts_dict_index": [8580, 8581, 8582]}
+{"event_id": 877425, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-12 17:42:00", "end_date_time": "2020-04-12 17:42:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. Multiple trees were downed near Tyler Pipe in the Swan community.", "ts_dict_index": [8640, 8641, 8642]}
+{"event_id": 875889, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-12 06:07:00", "end_date_time": "2020-04-12 06:07:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. An anemometer from a personal weather station measured a 63 mph wind gust at Emerald Bay on Lake Palestine.", "ts_dict_index": [8625, 8626, 8627]}
+{"event_id": 965432, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-29 18:35:00", "end_date_time": "2021-07-29 18:35:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. A large tree was uprooted.", "ts_dict_index": [8616, 8617, 8618]}
+{"event_id": 877391, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-12 17:28:00", "end_date_time": "2020-04-12 17:28:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. Trees were downed on FM 16 west near Hide-A-Way Lake.", "ts_dict_index": [8622, 8623, 8624]}
+{"event_id": 965430, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-29 18:19:00", "end_date_time": "2021-07-29 18:19:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. A tree was blown down, and large branches were blown down from other trees. Time estimated from radar.", "ts_dict_index": [8619, 8620, 8621]}
+{"event_id": 965418, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-29 16:30:00", "end_date_time": "2021-07-29 16:30:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. Trees or limbs blocked Fretz Valley Rd, Geigel Hill Rd, and Creamery Rd. Time estimated from radar.", "ts_dict_index": [8604, 8605, 8606]}
+{"event_id": 965417, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-29 16:50:00", "end_date_time": "2021-07-29 16:50:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. Widespread tree damage and minor damage to some structures was reported in Buckingham Twp.", "ts_dict_index": [8598, 8599, 8600]}
+{"event_id": 965431, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-29 18:30:00", "end_date_time": "2021-07-29 18:30:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. Metal bleachers were displaced, a fence and sign were blown down, and some shingles were blown off. Damage photos were consistent with straight line winds. Time estimated from radar.", "ts_dict_index": [8589, 8590, 8591]}
+{"event_id": 965427, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-29 18:10:00", "end_date_time": "2021-07-29 18:10:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. Trees and wires were downed along Neck Rd.", "ts_dict_index": [8595, 8596, 8597]}
+{"event_id": 965415, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-29 16:11:00", "end_date_time": "2021-07-29 16:11:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. Several trees were downed in Quakertown. This storm would go on to produce multiple tornadoes. Time estimated from radar.", "ts_dict_index": [8610, 8611, 8612]}
+{"event_id": 877398, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-12 17:40:00", "end_date_time": "2020-04-12 17:40:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. Trees were downed near I-20 between Highway 69 and Highway 14, near Lavender Road.", "ts_dict_index": [8628, 8629, 8630]}
+{"event_id": 877395, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-12 17:45:00", "end_date_time": "2020-04-12 17:45:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. Trees were downed near Winona.", "ts_dict_index": [8631, 8632, 8633]}
+{"event_id": 877456, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-04-12 08:10:00", "end_date_time": "2020-04-12 08:10:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. A tree was blown down on Woodley Road.", "ts_dict_index": [8646, 8647, 8648]}
+{"event_id": 1095246, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-04-01 02:46:00", "end_date_time": "2023-04-01 02:46:00", "narrative": "After an intense wind storm in early March, strong to damaging winds once again struck eastern Kentucky on April 1st. Another unseasonably intense low pressure system tracked from the Upper Midwest to across the Great Lakes, pulling a cold front across the area during the wee morning hours of April 1st. Storms along the front put down torrential downpours with pockets of strong gusty winds. This led to a few instances of poor drainage/small stream flooding as well as downed trees before sunrise. However, the more significant weather arrived mid to late morning as skies cleared and southwesterly winds increased sharply ahead of the storm system's secondary cold front. During the midday to mid afternoon hours, southwesterly wind gusts peaked between 30 and 50 mph in many of the valley locations, with gusts of 55 to 60 mph commonly being observed in the more open countryside and atop ridges. The strongest reported gust, 70 mph, was observed at a Kentucky Mesonet station atop Flatwoods (elevation 2,774 feet ASL) in Pike County.||The strong to damaging winds resulted in many trees being blown down onto power lines and snapped power poles. Power outages exceeded more than 50,000 customers across the Commonwealth. A vast majority of those outages were reported in eastern Kentucky and were most concentrated in the eastern Kentucky Coalfield. Kentucky Power, which covers much of southeast Kentucky took 3+ days to restore power in their service area. Repairs included replacing at least 79 power poles, 30 miles of power lines, 70 cross arms, and 44 transformers. The Big Sandy RECC also took at least two days to restore power to 3,171 of its approximately 12,500 customers. Aside from damage to power infrastructure, two individuals reportedly sustained injuries during the high wind event -- a branch struck a hiker near Natural Bridge and another tree fell on a fire truck in Letcher County. There were also numerous reports of downed trees and multiple instances of structural damage. The most notable building damage was reported in Floyd County where the Triple A Market in Martin lost its roof and an apartment building in Prestonsburg partially collapsed. A tree was reported down along KY-761, with a couple additional trees blown down in the vicinity.", "ts_dict_index": [8649, 8650, 8651]}
+{"event_id": 877422, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-12 18:12:00", "end_date_time": "2020-04-12 18:12:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. Trees and power lines were downed in the New London area from a damaging gust front.", "ts_dict_index": [8634, 8635, 8636]}
+{"event_id": 965413, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-07-29 15:08:00", "end_date_time": "2021-07-29 15:08:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. Trees and wires were downed. Time estimated by radar.", "ts_dict_index": [8613, 8614, 8615]}
+{"event_id": 965416, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-07-29 15:05:00", "end_date_time": "2021-07-29 15:05:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. Utility poles were reported down in the area.", "ts_dict_index": [8601, 8602, 8603]}
+{"event_id": 877443, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-04-12 08:17:00", "end_date_time": "2020-04-12 08:17:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. A tree was downed onto a power line on Strickland Springs Road South.", "ts_dict_index": [8643, 8644, 8645]}
+{"event_id": 965419, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-07-29 15:14:00", "end_date_time": "2021-07-29 15:14:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. Trees and wires were downed on Route 863, and the road was closed. Time estimated from radar.", "ts_dict_index": [8607, 8608, 8609]}
+{"event_id": 879888, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-12 19:10:00", "end_date_time": "2020-04-12 19:10:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. A 60 mph wind gust was estimated in the Deepwoods subdivision in South Shreveport.", "ts_dict_index": [8562, 8563, 8564]}
+{"event_id": 835595, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2019-07-05 02:24:00", "end_date_time": "2019-07-05 02:24:00", "narrative": "Hail up to the size of golf balls and damaging winds occurred on this Thursday night. Just after 9 PM CST, scattered, small thunderstorms began developing between Elwood and Minden. The storms increased in size and combined into an east-west oriented multi-cell line that was stationary across Gosper, Phelps, and Kearney counties. This line remained stationary through 1 AM CST Friday. However, between midnight and 1 AM, the MCS began to evolve. A storm over Kearney county began moving eastward and became dominant. As this storm moved into Adams county after 1 AM CST, new storms formed along the surging outflow boundary/cold pool from Red Cloud to Franklin to Alma. A transition to a comma-shaped echo configuration had occurred. This finally brought an end to the storms over Gosper, Phelps, and Kearney counties. The newly formed squall line increased in size between 2 and 430 AM CST, as it moved across the rest of south central Nebraska, south of Interstate 80. The initial east-west line of storms produced golf ball size hail several miles south of Elwood, and downburst winds knocked down power lines across highway 23 between Loomis and Holdrege. Outflow winds of 58 mph were also measured near Oxford. Later in the night, the squall line produced severe winds in a couple spots. A large tree limb was broken in Hastings, and winds were clocked at 60 mph in Harvard. There were not many rain gauge observations available where the heaviest rain fell, but the highest amount reported was 3.46 inches, 11 mi south of Elwood.||Throughout the day, a slow-moving cold front became stationary across northern Nebraska, from Scottsbluff to Sioux City, IA. These storms formed south of the front, where just prior to convection initiation, temperatures were in the upper 70s, and dewpoints were in the lower 70s. With the mid-level lapse rate around 7.5 C/km, MUCAPE was near 3000 J/kg. Effective deep layer shear was 25-30 kt. In the upper-levels, the flow was from the west-southwest across most of nation, with a weak (and weakening) trough over the northern Rockies. Wind speeds were weak over the central Plains with a low-amplitude ridge from near Denver to Omaha. A 60 MPH wind gust was measured by a mesonet station located in Harvard.", "ts_dict_index": [8661, 8662, 8663]}
+{"event_id": 916103, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-08-10 11:30:00", "end_date_time": "2020-08-10 12:50:00", "narrative": "A powerful line of severe thunderstorms produced a derecho which tracked across eastern Iowa and northwest Illinois on the afternoon of Monday, August 10th, resulting in widespread straight line wind damage. The cost of damage from this storm was extreme, reaching an estimated 7.5 billion dollars along the path of these storms from Iowa through Illinois.  Two brief tornadoes have been confirmed within the widespread swath of wind damage, one just north of the Eastern Iowa Airport in Linn County Iowa, and one just south of Freeport, Illinois. These tornadoes have been designated as EF-U, as there was no observable damage directly attributable to the tornadoes from which an EF-scale rating could be assigned. While an average of two derechos a year occur across the area, a derecho of this intensity is a roughly once-in-a-decade occurrence. Another unusual aspect of this derecho was the duration of the strong winds, with gusts over 60 mph for over an hour at some locations.||The most extreme winds, estimated at 110-140 mph, destroyed or damaged numerous outbuildings, barns, grain bins, homes, mobile homes, apartment buildings, trees, and power poles in parts of Benton, Linn, Jones, Cedar, and Clinton Counties. The Cedar Rapids area was particularly hard hit. One fatality occurred in Linn County, as a tree fell on a cyclist. Several homes, apartment complexes, and businesses sustained damage consistent with 130-140 mph winds. Radio transmission towers in Marion and Clinton, Iowa collapsed due to winds estimated around 130 mph. Wind gusts of 80-100 mph were common as the line of storms moved through the Quad Cities area and then through northwest Illinois. A small pocket of winds estimated at 100-110 mph impacted Princeton, IL in Bureau County, where a 150 foot communications tower collapsed and numerous power poles were snapped. In addition to the damage, numerous long-duration power outages occurred across the region. Damage to crops was considerable along the derecho path. Numerous semi trucks were also blown off roadways along the path of the derecho. Widespread straight-line winds that produced extensive damage were reported throughout Linn County, associated with a derecho. These winds lasted around an hour in total at any one location, even though the initial line of storms moved out quickly. Damaging straight-line winds continued and were associated with the rear inflow jet. Maximum wind speeds were estimated to be 80 to 100 MPH for much of the county, with areas in central Linn County that had wind speed estimates that were 120 MPH or higher. The highest estimated wind speed were in the Cedar Rapids area where extensive damage to an apartment complex occurred with damage indicating winds about 140 MPH. A radio transmission tower also collapsed with wind speed estimated at 130 MPH. These estimates were determined based off damage reports and photos submitted through social media as well as a damage survey. The peak thunderstorm wind gust measured at the Cedar Rapids airport ASOS before it lost power was 68 MPH. The duration of strong winds caused extensive damaged most if not all trees, crops, and structures in their path. Due to the widespread damage, long duration power outages occurred. One fatality occurred here when a 63 year old man riding a bicycle was struck and killed by a tree that was knocked down due to the winds. There were also numerous injuries reported in the Cedar Rapids area.", "ts_dict_index": [8670, 8671, 8672]}
+{"event_id": 817204, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-05-02 02:07:00", "end_date_time": "2019-05-02 02:07:00", "narrative": "A deep southerly flow increased across much of the Ark-La-Tex during the daytime hours of April 30th through May 1st, ahead of a slow moving upper level trough that drifted east into the Southern Plains from the Four Corners Region. A complex of showers and thunderstorms that developed over Western and Central Oklahoma during the evening of April 30th ahead of a stalled surface frontal boundary sent a cold pool southeast into portions of extreme Northeast Texas and Southwest Arkansas which eventually stalled out during the early morning hours on May 1st. Weak upper level disturbances in the southwest flow aloft ahead of the approaching trough triggered additional showers and thunderstorms across Northcentral Texas, which spread east northeast across East Texas, Southwest Arkansas, and North Louisiana during the evening hours of the 1st, and continued throughout the morning hours of the 2nd. The earlier stalled boundary over Northeast Texas and Southwest Arkansas helped to enhance the showers and thunderstorms, and coupled with the instability and deep moisture in place, some of the showers and thunderstorm became severe, producing large hail, damaging winds, and locally heavy rainfall. An isolated tornado even touched down across Eastern Shelby County Texas just prior to daybreak on the 2nd. Where the storms moved repeatedly over the same areas, flash flooding was observed with several roads flooded and closed across portions of East Texas. ||While the storms diminished shortly after daybreak on the 2nd, another complex of showers and thunderstorms developed during the late afternoon through the evening hours in Central and Southeast Texas ahead of another shortwave trough, with a portion of this complex migrating into Deep East Texas by mid-evening. Given the moderate instability in place across this area due to strong daytime heating, some of these storms also became severe, with damaging winds downing trees and destroying a chicken house in Northern Nacogdoches County before weakening by late evening. A tree was blown down on County Road 424 blocking the roadway just west of the intersection of FM 13.", "ts_dict_index": [8676, 8677, 8678]}
+{"event_id": 1012038, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2022-04-21 22:22:00", "end_date_time": "2022-04-21 22:31:00", "narrative": "Between 10 p.m. CDT on Thursday the 21st and 3:30 a.m. on Friday the 22nd, a cluster of slightly elevated strong-to-severe thunderstorms rumbled across parts of South Central Nebraska, primarily affecting counties along/north of Highway 6 and also areas mainly east of a line from Holdrege-Loup City. Severe-criteria reports were fairly limited but were highlighted by: estimated 65 MPH winds near Clay Center that snapped a 12-inch diameter cedar tree; mesonet-measured wind gusts of 65 MPH near Clarks and 63 MPH near Kearney; quarter size hail in Grand Island and Sutton. Most places received well under 1 inch of rain except for a fairly narrow, southwest-northeast oriented swath of 1.00-1.50 centered from just west of Grand Island up through much of Merrick/Nance counties. ||Breaking down timing and storm evolution, the initial convection fired up slightly south of the Highway 6 corridor between 10-11 p.m. CDT, taking the form of a broken west-east oriented line. Over the next few hours, this primarily multicell convective line drifted steadily northward across the I-80 corridor, although along the way an embedded supercell briefly took shape over Clay County. Between 1-3 a.m. CDT the broken, west-east line of storms gradually consolidated into more of a compact cluster centered over Merrick/Nance counties, with the back-edge of the last severe-warned core departing the local area into eastern Nebraska by 3:30 a.m. CDT. This nocturnal event was a classic case of slightly elevated storms blossoming within the leading/north edge of low-level moisture advection and convergence within the heart of a strengthening low-level jet (40-60 knots at 850 millibars). In the mid-upper levels, South Central Nebraska resided under broad southwesterly flow, well-downstream from a large-scale trough coming onshore into California. At the surface, this event focused slightly north of a warm front that gradually lifted from northern KS into central NE over the course of the night. Mesoscale parameters featured 1000-2000 J/kg most-unstable CAPE and 40-50 knots of deep-layer shear, promoting the organized multicell and brief/transient supercell storm mode. A wind gust of 62 MPH was measured by a mesonet station located four miles southeast of Clay Center. An NWS Cooperative Observer located six miles east-southeast of Clay Center noted wind gusts estimated to be between 55 and 65 MPH, damaging two cedar trees, one of which was 12 inches in diameter.", "ts_dict_index": [8667, 8668, 8669]}
+{"event_id": 1095255, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-04-01 02:52:00", "end_date_time": "2023-04-01 02:52:00", "narrative": "After an intense wind storm in early March, strong to damaging winds once again struck eastern Kentucky on April 1st. Another unseasonably intense low pressure system tracked from the Upper Midwest to across the Great Lakes, pulling a cold front across the area during the wee morning hours of April 1st. Storms along the front put down torrential downpours with pockets of strong gusty winds. This led to a few instances of poor drainage/small stream flooding as well as downed trees before sunrise. However, the more significant weather arrived mid to late morning as skies cleared and southwesterly winds increased sharply ahead of the storm system's secondary cold front. During the midday to mid afternoon hours, southwesterly wind gusts peaked between 30 and 50 mph in many of the valley locations, with gusts of 55 to 60 mph commonly being observed in the more open countryside and atop ridges. The strongest reported gust, 70 mph, was observed at a Kentucky Mesonet station atop Flatwoods (elevation 2,774 feet ASL) in Pike County.||The strong to damaging winds resulted in many trees being blown down onto power lines and snapped power poles. Power outages exceeded more than 50,000 customers across the Commonwealth. A vast majority of those outages were reported in eastern Kentucky and were most concentrated in the eastern Kentucky Coalfield. Kentucky Power, which covers much of southeast Kentucky took 3+ days to restore power in their service area. Repairs included replacing at least 79 power poles, 30 miles of power lines, 70 cross arms, and 44 transformers. The Big Sandy RECC also took at least two days to restore power to 3,171 of its approximately 12,500 customers. Aside from damage to power infrastructure, two individuals reportedly sustained injuries during the high wind event -- a branch struck a hiker near Natural Bridge and another tree fell on a fire truck in Letcher County. There were also numerous reports of downed trees and multiple instances of structural damage. The most notable building damage was reported in Floyd County where the Triple A Market in Martin lost its roof and an apartment building in Prestonsburg partially collapsed. A tree was blown down onto Slate Branch Road south of Somerset.", "ts_dict_index": [8652, 8653, 8654]}
+{"event_id": 907691, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2020-07-26 15:30:00", "end_date_time": "2020-07-26 15:30:00", "narrative": "Cold front brings slow moving thunderstorms and heavy rain to extreme southern portions of south central Nebraska during the late afternoon and evening of July 26. Thunderstorms developed between 3pm and 4pm CDT from southwest to northeast, generally along a line from Rooks County in north central Kansas, to Thayer County in south central Nebraska. Once thunderstorms developed, heavy rain quickly became the main concern, though a few non-severe wind gusts around 50 to 55 mph were reported across north central Kansas early on in the event, as well as an estimated wind gust near 60mph in Thayer County. The heavy rain threat was driven by several factors, including: weak mid and upper level winds which resulted in slow storm motion, training of thunderstorms over the same areas for several hours, and unusually high atmospheric moisture levels. In fact, precipitable water values were near 2��� on this evening, which is near 3 standard deviations above normal and in the upper 90th percentile of climatology. Heavy rain rates of 1-2��� per hour, or higher, were common under the strongest thunderstorm cores, especially between the hours of 4pm and 9pm CDT. Thunderstorms gradually decreased in intensity during the late evening as the persistent convection over the same areas and loss of daytime heating led to decreasing instability. The majority of the lingering light rain ended by midnight.||For south central Nebraska, the heavy rain was limited to primarily eastern Nuckolls County and all of Thayer County. Storm total rain amounts by the morning of July 27th of 3-4��� inches were common, with an isolated maximum of 4-5��� plus reported in the Hebron area. The highest reported rain amount was 5.50��� measured at the fire station in Hebron and relayed by emergency management. The primary impacts from the heavy rain were flooded roads across Thayer County. This included numerous county roads along with Highway 5 north of Deshler and Highway 81 (which is a major four lane highway) between Belvidere and the Nebraska/Kansas state line. The flooding on Highway 81 may have contributed to a semi tractor trailer to lose control and drive into a ditch. Wind gusts were estimated to be near 60 MPH.", "ts_dict_index": [8664, 8665, 8666]}
+{"event_id": 1095252, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-04-01 02:51:00", "end_date_time": "2023-04-01 02:51:00", "narrative": "After an intense wind storm in early March, strong to damaging winds once again struck eastern Kentucky on April 1st. Another unseasonably intense low pressure system tracked from the Upper Midwest to across the Great Lakes, pulling a cold front across the area during the wee morning hours of April 1st. Storms along the front put down torrential downpours with pockets of strong gusty winds. This led to a few instances of poor drainage/small stream flooding as well as downed trees before sunrise. However, the more significant weather arrived mid to late morning as skies cleared and southwesterly winds increased sharply ahead of the storm system's secondary cold front. During the midday to mid afternoon hours, southwesterly wind gusts peaked between 30 and 50 mph in many of the valley locations, with gusts of 55 to 60 mph commonly being observed in the more open countryside and atop ridges. The strongest reported gust, 70 mph, was observed at a Kentucky Mesonet station atop Flatwoods (elevation 2,774 feet ASL) in Pike County.||The strong to damaging winds resulted in many trees being blown down onto power lines and snapped power poles. Power outages exceeded more than 50,000 customers across the Commonwealth. A vast majority of those outages were reported in eastern Kentucky and were most concentrated in the eastern Kentucky Coalfield. Kentucky Power, which covers much of southeast Kentucky took 3+ days to restore power in their service area. Repairs included replacing at least 79 power poles, 30 miles of power lines, 70 cross arms, and 44 transformers. The Big Sandy RECC also took at least two days to restore power to 3,171 of its approximately 12,500 customers. Aside from damage to power infrastructure, two individuals reportedly sustained injuries during the high wind event -- a branch struck a hiker near Natural Bridge and another tree fell on a fire truck in Letcher County. There were also numerous reports of downed trees and multiple instances of structural damage. The most notable building damage was reported in Floyd County where the Triple A Market in Martin lost its roof and an apartment building in Prestonsburg partially collapsed. A powerline was blown down near the intersection of Winding Ridge Road and Oak Hill Road.", "ts_dict_index": [8655, 8656, 8657]}
+{"event_id": 818122, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2019-04-21 22:05:00", "end_date_time": "2019-04-21 22:05:00", "narrative": "Separate clusters of strong to severe thunderstorms affected portions of South Central Nebraska on this Sunday evening, mainly between 7-11 p.m. CDT. A southern area of storms was mainly a wind-producer, while a northern cluster primarily yielded hail. Focusing first on southern counties, a surge of strong-to-severe outflow winds crossed the state line out of northern Kansas mainly between 8:30-10:30 p.m. CDT, promoting a number of sub-severe gusts into at least the 40-56 MPH range within several counties mainly south of Interstate 80 and along and east of Highway 281. Only a few personal weather stations breached severe-criteria, including a 59 MPH gust near Nelson. In addition, a spotter estimated 60 MPH winds in central Webster County. These winds kicked up quite a bit of blowing dust, including in Hastings, where a 54 MPH gust occurred without any associated rainfall. Turning to the completely separate northern area of convection, a more isolated storm cluster blossomed over Buffalo County around 7 p.m. CDT. Over the next few hours, this activity drifted slowly northeast and occasionally dropped severe-criteria hail, including quarter size stones in or near Ravenna and Dannebrog, and up to ping pong ball size in St. Paul. This convection departed eastward out of Nance County (and thus out of the local area) around 11 p.m. CDT. ||Tracing the southern storm complex back to its roots, it actually originated in east-central Colorado during the early-to-mid afternoon before peaking in intensity over north central Kansas during the early evening. In the mid-upper levels, the main instigator for both areas of storms was a low-amplitude shortwave trough lifting east-northeast along the Nebraska-Kansas border. At the surface, convection was largely tied to a slow-moving cold front traversing the Central Plains from west-to-east.  Evening mesoscale convective parameters in South Central Nebraska featured around 1000 J/kg mixed-layer CAPE and 30-40 knots of effective deep-layer wind shear. A 58 MPH wind gust was measured by a mesonet station located 2 miles west of Shickley.", "ts_dict_index": [8685, 8686, 8687]}
+{"event_id": 866534, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-01-10 23:17:00", "end_date_time": "2020-01-10 23:17:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Several trees were blown down in Whitehouse.", "ts_dict_index": [8727, 8728, 8729]}
+{"event_id": 866533, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-01-10 22:45:00", "end_date_time": "2020-01-10 22:45:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Several trees were blown down in Lindale.", "ts_dict_index": [8721, 8722, 8723]}
+{"event_id": 809820, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-04-13 04:09:00", "end_date_time": "2019-04-13 04:09:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing several reports of damaging winds across portions of Northcentral Louisiana. These storms also produced locally heavy rainfall that led to instances of flash flooding, which resulted in two separate fatalities in Ouachita Parish. A 13 year old boy drowned in a drainage canal in the Bawcomville community during the heavy rains, and an 80 year old female drove past barricades on a closed road in Calhoun several hours after the heavy rains had ended, with her car becoming submerged in the flood waters. Unfortunately, she was unable to escape and drowned.  These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Several trees were uprooted, a tree was blown down on a home, a roof was blown off of a shop, and trees were downed across Highway 173 near Highway 1.", "ts_dict_index": [8745, 8746, 8747]}
+{"event_id": 854810, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2019-06-24 18:13:00", "end_date_time": "2019-06-24 18:30:00", "narrative": "Just 367 days after the last of the Great June Flood of 2018 had left its memorable mark on nearly all of the populated Rio Grande Valley, a confluence of atmospheric events came together during the late afternoon and evening of June 24th, 2019, to produce another memorable - and unfortunate - situation for parts of the Rio Grande Valley. This time, the impacted area was smaller and less populated but the results the same. For most of Willacy County's population, the western third of Cameron, and a corner of eastern Hidalgo, significant impacts were noted.  These included:||Over a foot of rain fell in about six hours, including a peak total of more than 15 inches near Santa Rosa (Cameron/Hidalgo line); hundreds of streets flooded, including 30 Texas-managed highways; 1,188 homes were considered destroyed or incurring major damage requiring significant repairs, with an additional 182 homes sustaining minor damage or mildly affected (as of July 10).  Individual Assistance (IA) costs were estimated at $27.6 million. Public Assistance (PA) costs were likely over $5 million, but totals were not available as of this writing. Total damage was likely to range from $50 to $100 million or more when all estimates have been received, and final estimated may not be known until late 2019.||More than 100 persons were evacuated to safe high ground from dozens of homes threatened by 2 or more feet of water in several locations in each county.  At least 45,000 private and public utility power customers were without power at the peak of the storm, and estimated 65 to 75 mph winds caused at least five poorly built mobile homes to be rolled or demolished in eastern Hidalgo County.  Lightning struck a wind turbine and set it ablaze in Willacy County, costing an estimated $5 million in damage.|New daily rainfall records were set at most available Rio Grande Valley climate recording locations. These totals ranged from 2.06 inches in Brownsville to 15.20 inches in Santa Rosa. A severe thunderstorm produced sporadic straight line wind damage|from Monte alto to portions of north Elsa during the evening of|June 24th. Storm motion was from northeast to southwest out of western Willacy County, and several large tree limbs were snapped, and a few trees were uprooted, on the east side of Monte Alto. Winds also caused a free standing metal tower to collapse in Monte Alto. As the storm moved southwestward, large swaths of sugar cane were|noticeably bent towards the ground. Farther west, two poorly |constructed mobile homes were completely destroyed and another was|rolled on its side in a colonia about 2 miles west of Monte Alto. Near Elsa, just off of  Monte Cristo Road, over a dozen wooden power poles were snapped across N. Mile Five and One-Half Road. Some metal sheet roofing was torn from a nearby home, and a storage shed had considerable damage to walls and roofing. Based on the construction quality of the buildings and the transmission tower, and the type of trees damaged, peak wind speeds were estimated at 65 to 75 mph.", "ts_dict_index": [8736, 8737, 8738]}
+{"event_id": 854814, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2019-06-24 17:00:00", "end_date_time": "2019-06-24 17:00:00", "narrative": "Just 367 days after the last of the Great June Flood of 2018 had left its memorable mark on nearly all of the populated Rio Grande Valley, a confluence of atmospheric events came together during the late afternoon and evening of June 24th, 2019, to produce another memorable - and unfortunate - situation for parts of the Rio Grande Valley. This time, the impacted area was smaller and less populated but the results the same. For most of Willacy County's population, the western third of Cameron, and a corner of eastern Hidalgo, significant impacts were noted.  These included:||Over a foot of rain fell in about six hours, including a peak total of more than 15 inches near Santa Rosa (Cameron/Hidalgo line); hundreds of streets flooded, including 30 Texas-managed highways; 1,188 homes were considered destroyed or incurring major damage requiring significant repairs, with an additional 182 homes sustaining minor damage or mildly affected (as of July 10).  Individual Assistance (IA) costs were estimated at $27.6 million. Public Assistance (PA) costs were likely over $5 million, but totals were not available as of this writing. Total damage was likely to range from $50 to $100 million or more when all estimates have been received, and final estimated may not be known until late 2019.||More than 100 persons were evacuated to safe high ground from dozens of homes threatened by 2 or more feet of water in several locations in each county.  At least 45,000 private and public utility power customers were without power at the peak of the storm, and estimated 65 to 75 mph winds caused at least five poorly built mobile homes to be rolled or demolished in eastern Hidalgo County.  Lightning struck a wind turbine and set it ablaze in Willacy County, costing an estimated $5 million in damage.|New daily rainfall records were set at most available Rio Grande Valley climate recording locations. These totals ranged from 2.06 inches in Brownsville to 15.20 inches in Santa Rosa. An off-duty NWS employee, along with local news media, reported a tractor trailer jack-knifed with the cab dangling on the side of Interstate 69C on the overpass above FM 490 just north of the South Texas International Airport.  It was not determined if the jack-knife was caused by wind, slick roads, or both, but wind gusts over 40 mph had begun as persistent outflows from a developing mesoscale convective system over eastern Hidalgo and western Willacy County.", "ts_dict_index": [8730, 8731, 8732]}
+{"event_id": 809833, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-04-13 10:10:00", "end_date_time": "2019-04-13 10:10:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing several reports of damaging winds across portions of Northcentral Louisiana. These storms also produced locally heavy rainfall that led to instances of flash flooding, which resulted in two separate fatalities in Ouachita Parish. A 13 year old boy drowned in a drainage canal in the Bawcomville community during the heavy rains, and an 80 year old female drove past barricades on a closed road in Calhoun several hours after the heavy rains had ended, with her car becoming submerged in the flood waters. Unfortunately, she was unable to escape and drowned.  These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. A tree was blown down on a home on Rose Court off of Kingston Road between Williamson Way and Flournoy Lucas Road.", "ts_dict_index": [8751, 8752, 8753]}
+{"event_id": 809835, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-04-13 10:10:00", "end_date_time": "2019-04-13 10:10:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing several reports of damaging winds across portions of Northcentral Louisiana. These storms also produced locally heavy rainfall that led to instances of flash flooding, which resulted in two separate fatalities in Ouachita Parish. A 13 year old boy drowned in a drainage canal in the Bawcomville community during the heavy rains, and an 80 year old female drove past barricades on a closed road in Calhoun several hours after the heavy rains had ended, with her car becoming submerged in the flood waters. Unfortunately, she was unable to escape and drowned.  These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Several trees were downed in the Southern Hills neighborhood in South Shreveport.", "ts_dict_index": [8748, 8749, 8750]}
+{"event_id": 854818, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2019-06-24 18:15:00", "end_date_time": "2019-06-24 18:35:00", "narrative": "Just 367 days after the last of the Great June Flood of 2018 had left its memorable mark on nearly all of the populated Rio Grande Valley, a confluence of atmospheric events came together during the late afternoon and evening of June 24th, 2019, to produce another memorable - and unfortunate - situation for parts of the Rio Grande Valley. This time, the impacted area was smaller and less populated but the results the same. For most of Willacy County's population, the western third of Cameron, and a corner of eastern Hidalgo, significant impacts were noted.  These included:||Over a foot of rain fell in about six hours, including a peak total of more than 15 inches near Santa Rosa (Cameron/Hidalgo line); hundreds of streets flooded, including 30 Texas-managed highways; 1,188 homes were considered destroyed or incurring major damage requiring significant repairs, with an additional 182 homes sustaining minor damage or mildly affected (as of July 10).  Individual Assistance (IA) costs were estimated at $27.6 million. Public Assistance (PA) costs were likely over $5 million, but totals were not available as of this writing. Total damage was likely to range from $50 to $100 million or more when all estimates have been received, and final estimated may not be known until late 2019.||More than 100 persons were evacuated to safe high ground from dozens of homes threatened by 2 or more feet of water in several locations in each county.  At least 45,000 private and public utility power customers were without power at the peak of the storm, and estimated 65 to 75 mph winds caused at least five poorly built mobile homes to be rolled or demolished in eastern Hidalgo County.  Lightning struck a wind turbine and set it ablaze in Willacy County, costing an estimated $5 million in damage.|New daily rainfall records were set at most available Rio Grande Valley climate recording locations. These totals ranged from 2.06 inches in Brownsville to 15.20 inches in Santa Rosa. A large tree was blown down on the road near the Edinburg/McAllen line 5 miles southwest of Edinburg. Large branches were also blown down nearby.  Peak wind gusts at McAllen/Miller International Airport reached 41 mph (36 knots) but reached 52 mph (45 knots) at South Texas International Airport (about 11 miles north of Edinburg) during the same time period.", "ts_dict_index": [8733, 8734, 8735]}
+{"event_id": 854815, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2019-06-24 18:30:00", "end_date_time": "2019-06-24 18:30:00", "narrative": "Just 367 days after the last of the Great June Flood of 2018 had left its memorable mark on nearly all of the populated Rio Grande Valley, a confluence of atmospheric events came together during the late afternoon and evening of June 24th, 2019, to produce another memorable - and unfortunate - situation for parts of the Rio Grande Valley. This time, the impacted area was smaller and less populated but the results the same. For most of Willacy County's population, the western third of Cameron, and a corner of eastern Hidalgo, significant impacts were noted.  These included:||Over a foot of rain fell in about six hours, including a peak total of more than 15 inches near Santa Rosa (Cameron/Hidalgo line); hundreds of streets flooded, including 30 Texas-managed highways; 1,188 homes were considered destroyed or incurring major damage requiring significant repairs, with an additional 182 homes sustaining minor damage or mildly affected (as of July 10).  Individual Assistance (IA) costs were estimated at $27.6 million. Public Assistance (PA) costs were likely over $5 million, but totals were not available as of this writing. Total damage was likely to range from $50 to $100 million or more when all estimates have been received, and final estimated may not be known until late 2019.||More than 100 persons were evacuated to safe high ground from dozens of homes threatened by 2 or more feet of water in several locations in each county.  At least 45,000 private and public utility power customers were without power at the peak of the storm, and estimated 65 to 75 mph winds caused at least five poorly built mobile homes to be rolled or demolished in eastern Hidalgo County.  Lightning struck a wind turbine and set it ablaze in Willacy County, costing an estimated $5 million in damage.|New daily rainfall records were set at most available Rio Grande Valley climate recording locations. These totals ranged from 2.06 inches in Brownsville to 15.20 inches in Santa Rosa. One tree was blown down along Cummings Road in Donna. Time estimated from radar and from nearby gust to 41 mph at McAllen/Miller Airport at 734 PM CDT.", "ts_dict_index": [8739, 8740, 8741]}
+{"event_id": 873408, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2020-01-10 23:59:00", "end_date_time": "2020-01-10 23:59:00", "narrative": "The month started off with a bang on the 10th. It felt like spring in Arkansas, with high temperatures in the 60s to lower 70s. As the day began, a powerful storm system was looming to the west in New Mexico. Moisture levels were on the rise ahead of the system. It was a perfect setup for severe weather and flash flooding.||By late afternoon and into the overnight hours/early on the 11th, a massive damaging wind episode unfolded. Wind gusts from 60 to 90 mph pounded parts of the state. Trees and/or power lines were downed at Yellville (Marion County), Henderson (Baxter County), Elizabeth (Fulton County), Melbourne (Izard County), Leslie (Searcy County), a few miles west of Arkadelphia (Clark County), Malvern (Hot Spring County), Judsonia (White County), Fordyce (Dallas County), Pine Bluff (Jefferson County), Cotton Plant (Woodruff County), Monticello (Drew County), St. Charles (Arkansas County), and Watson (Desha County). Some fallen trees landed on homes. Wind recording equipment measured a 74 mph gust at Fargo (Monroe County), and a 71 mph gust at the University of Arkansas at Monticello (Drew County).||There were also isolated tornadoes. At 740 pm CST on the 10th, a tornado (rated EF2) was spawned southwest of Midway (Logan County). The tornado cut close to a fourteen mile path before dissipating northeast of Scranton (Logan County).||Nine other mostly weak tornadoes (eight rated EF1/one rated EF2) were confirmed across the state through the wee hours of the 11th. Two of these tornadoes were in the Little Rock County Warning Area near Seaton (Lonoke County) and Jerome (Drew County). The former tornado blew in a grain bin and tossed a shed into nearby trees. The latter tornado mangled a silo. Trees were uprooted or snapped, and utility poles were taken out.||A few places reported sleet or snow on the back side of the system. A tree limb was blown down out of a tree.", "ts_dict_index": [8769, 8770, 8771]}
+{"event_id": 820528, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-14 13:16:00", "end_date_time": "2019-04-14 13:16:00", "narrative": "This event was characterized by a mid-level shortwave trough becoming negatively tilted as it entered the Tennessee Valley, initiating cyclogenesis in the Arklatex, with the resultant 992 hPa low pressure moving northeastward into the Ohio Valley. This setup a strong, meridional flow ahead of this feature. The 925 hPa low level jet of 44 kts was around 4 Standard Deviations above normal, and record for the date per the 12Z/14 TAE sounding. A pre-frontal trough pooled a narrow axis of moisture out ahead of the cold front, and served as a forcing mechanism for convection. Given Bulk Shear (0-6 km) around 60 knots and Surface Based CAPE around 1.2k J/kg, this was more than sufficient for organized, severe thunderstorms. The air mass just ahead of the pre-frontal trough was much drier and capped, initially limiting the development of more discrete cells ahead of the line. In fact, the 12Z/14 TAE sounding sampled a cap of over 5C just below 700 hPa! However as solar insolation and large scale ascent increased, this cap was broken around 15Z, and the QLCS intensified. The strong wind field and steep low-level lapse rates created an environment favorable for damaging wind gusts, particularly northwest of a line from the Apalachicola River to Tifton GA, where steeper mid-level lapse rates overlayed, leading to greater buoyancy. The tornado threat along the QLCS was dependent on storms becoming more favorably aligned with the Shear Vector (0-3 km), with otherwise sufficient CAPE (0-3 km) and low LCLs. Ahead of the QLCS, the low-level wind field was sheared in the 0-1 km layer, as evidenced on VAD Wind Profiles. As a result, the tornado threat increased with the more discrete cells after the cap broke. The aforementioned strong wind field and steep low-level lapse rates, combined with the isallobaric component of wind, lead to wind gusts around 40 mph well ahead of the QLCS. A total of 27 warnings were issued, including 15 SVRs, 6 TORs, and 6 SMWs. A tree was blown down onto a power line.", "ts_dict_index": [8742, 8743, 8744]}
+{"event_id": 866654, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-01-10 23:50:00", "end_date_time": "2020-01-10 23:50:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Trees were downed near the 9900 block of County Road 317 near the Minden community.", "ts_dict_index": [8697, 8698, 8699]}
+{"event_id": 866652, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-01-10 23:50:00", "end_date_time": "2020-01-10 23:50:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Trees were downed at the intersection of Highway 42 and Highway 323 near New London.", "ts_dict_index": [8700, 8701, 8702]}
+{"event_id": 858935, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-10-06 19:48:00", "end_date_time": "2019-10-06 19:48:00", "narrative": "The heaviest cloudbursts on the 4th were in Clark and Hot Spring Counties close to Interstate 30. Some flash flooding occurred, with high water near the Amtrak depot in Gurdon, and roads under water in Arkadelphia (both in Clark County). Radar estimated over a half foot of rain between Gurdon and Okolona (both in Clark County). A rain gauge at the latter location showed roughly five inches (via social media). Four to five inches of rain dumped in Arkadelphia (Clark County), with about an inch at Hot Springs (Garland County). It was the first time since mid-August that both sites received at least a half inch of precipitation in a day. ||The floodgates opened even more in the following days. A ridge of high pressure that persisted over Arkansas in September with dry/hot conditions finally broke down. That led to more cold fronts, chances of rain, and shots of cooler air.||One such front was on the doorstep to the northwest to begin the 6th. Ahead of the front, showers and thunderstorms were ongoing in northwest sections of the state. ||Heavy to excessive rain continued through much of the morning in areas toward the Missouri border. This kept temperatures in the 60s at Harrison (Boone County), and Mountain Home (Baxter County). Meanwhile, well ahead of the front where it was not raining, readings were in the 90s across the southern counties.||In the afternoon and evening, storms eventually worked to the south and east across the region. Along the way, there were several reports of severe weather. Golf ball size occurred near Atkins (Pope County), with quarter to half dollar size hail at Russellville (Pope County), Olmstead (Pulaski County), and around Hazen (Prairie County). A few miles east of Atkins (Pope County), a tree was blown onto the eastbound lanes of Interstate 40. A 56 mph gust was measured at the Stuttgart Airport in Fairmount (Prairie County). An estimated gust of 60 mph was reported at Olmstead.", "ts_dict_index": [8763, 8764, 8765]}
+{"event_id": 817205, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-05-02 02:15:00", "end_date_time": "2019-05-02 02:15:00", "narrative": "A deep southerly flow increased across much of the Ark-La-Tex during the daytime hours of April 30th through May 1st, ahead of a slow moving upper level trough that drifted east into the Southern Plains from the Four Corners Region. A complex of showers and thunderstorms that developed over Western and Central Oklahoma during the evening of April 30th ahead of a stalled surface frontal boundary sent a cold pool southeast into portions of extreme Northeast Texas and Southwest Arkansas which eventually stalled out during the early morning hours on May 1st. Weak upper level disturbances in the southwest flow aloft ahead of the approaching trough triggered additional showers and thunderstorms across Northcentral Texas, which spread east northeast across East Texas, Southwest Arkansas, and North Louisiana during the evening hours of the 1st, and continued throughout the morning hours of the 2nd. The earlier stalled boundary over Northeast Texas and Southwest Arkansas helped to enhance the showers and thunderstorms, and coupled with the instability and deep moisture in place, some of the showers and thunderstorm became severe, producing large hail, damaging winds, and locally heavy rainfall. An isolated tornado even touched down across Eastern Shelby County Texas just prior to daybreak on the 2nd. Where the storms moved repeatedly over the same areas, flash flooding was observed with several roads flooded and closed across portions of East Texas. ||While the storms diminished shortly after daybreak on the 2nd, another complex of showers and thunderstorms developed during the late afternoon through the evening hours in Central and Southeast Texas ahead of another shortwave trough, with a portion of this complex migrating into Deep East Texas by mid-evening. Given the moderate instability in place across this area due to strong daytime heating, some of these storms also became severe, with damaging winds downing trees and destroying a chicken house in Northern Nacogdoches County before weakening by late evening. Trees were blown down on County Road 126, as well as County Road 124.", "ts_dict_index": [8679, 8680, 8681]}
+{"event_id": 866538, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-01-10 23:40:00", "end_date_time": "2020-01-10 23:40:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Numerous trees and power lines were downed in the southern sections of Kilgore.", "ts_dict_index": [8718, 8719, 8720]}
+{"event_id": 809831, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2019-04-13 06:10:00", "end_date_time": "2019-04-13 06:10:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing several reports of damaging winds across portions of Northcentral Louisiana. These storms also produced locally heavy rainfall that led to instances of flash flooding, which resulted in two separate fatalities in Ouachita Parish. A 13 year old boy drowned in a drainage canal in the Bawcomville community during the heavy rains, and an 80 year old female drove past barricades on a closed road in Calhoun several hours after the heavy rains had ended, with her car becoming submerged in the flood waters. Unfortunately, she was unable to escape and drowned.  These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Trees were blown down on Pisgah Church Road.", "ts_dict_index": [8760, 8761, 8762]}
+{"event_id": 866657, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-01-10 23:55:00", "end_date_time": "2020-01-10 23:55:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Trees were downed on Farm to Market Road 840 southeast of Henderson.", "ts_dict_index": [8694, 8695, 8696]}
+{"event_id": 866658, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-01-11 00:07:00", "end_date_time": "2020-01-11 00:07:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Trees were downed at the intersection of Farm to Market Road 782 and Highway 149.", "ts_dict_index": [8691, 8692, 8693]}
+{"event_id": 866539, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-01-10 23:40:00", "end_date_time": "2020-01-10 23:40:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Damaging straight line winds estimated up to 100 mph partially ripped the roof off of a metal outbuilding and a nearby trailer was tipped over off of Texas 101 Spur and Woodlawn Street. Damage was found again along Meadowgreen Drive and Idylwood Drive just inside the Southern Gregg County side of Kilgore, where approximately 8 single family homes and 2 apartment buildings had partial roof damage. In addition, trees were snapped and uprooted in this area as well.", "ts_dict_index": [8715, 8716, 8717]}
+{"event_id": 809838, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2019-04-13 13:02:00", "end_date_time": "2019-04-13 13:02:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing several reports of damaging winds across portions of Northcentral Louisiana. These storms also produced locally heavy rainfall that led to instances of flash flooding, which resulted in two separate fatalities in Ouachita Parish. A 13 year old boy drowned in a drainage canal in the Bawcomville community during the heavy rains, and an 80 year old female drove past barricades on a closed road in Calhoun several hours after the heavy rains had ended, with her car becoming submerged in the flood waters. Unfortunately, she was unable to escape and drowned.  These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Trees and power lines were downed at the intersection of Dean Road and Highway 2.", "ts_dict_index": [8754, 8755, 8756]}
+{"event_id": 817231, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-05-02 04:32:00", "end_date_time": "2019-05-02 04:32:00", "narrative": "A deep southerly flow increased across much of the Ark-La-Tex during the daytime hours of April 30th through May 1st, ahead of a slow moving upper level trough that drifted east into the Southern Plains from the Four Corners Region. A complex of showers and thunderstorms that developed over Western and Central Oklahoma during the evening of April 30th ahead of a stalled surface frontal boundary sent a cold pool southeast into portions of extreme Northeast Texas and Southwest Arkansas which eventually stalled out during the early morning hours on May 1st. Weak upper level disturbances in the southwest flow aloft ahead of the approaching trough triggered additional showers and thunderstorms across Northcentral Texas, which spread east northeast across East Texas, Southwest Arkansas, and North Louisiana during the evening hours of the 1st, and continued throughout the morning hours of the 2nd. The earlier stalled boundary over Northeast Texas and Southwest Arkansas helped to enhance the showers and thunderstorms, and coupled with the instability and deep moisture in place, some of the showers and thunderstorm became severe, producing large hail, damaging winds, and locally heavy rainfall. An isolated tornado even touched down across Eastern Shelby County Texas just prior to daybreak on the 2nd. Where the storms moved repeatedly over the same areas, flash flooding was observed with several roads flooded and closed across portions of East Texas. ||While the storms diminished shortly after daybreak on the 2nd, another complex of showers and thunderstorms developed during the late afternoon through the evening hours in Central and Southeast Texas ahead of another shortwave trough, with a portion of this complex migrating into Deep East Texas by mid-evening. Given the moderate instability in place across this area due to strong daytime heating, some of these storms also became severe, with damaging winds downing trees and destroying a chicken house in Northern Nacogdoches County before weakening by late evening. A tree was blown down onto power lines at the intersection of FM 1798 and FM 840 in the Brachfield community.", "ts_dict_index": [8682, 8683, 8684]}
+{"event_id": 866669, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2020-01-11 00:40:00", "end_date_time": "2020-01-11 00:40:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Two small pine trees had their trunks snapped by straight line winds estimated near 70 mph.", "ts_dict_index": [8709, 8710, 8711]}
+{"event_id": 809839, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2019-04-13 13:02:00", "end_date_time": "2019-04-13 13:02:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing several reports of damaging winds across portions of Northcentral Louisiana. These storms also produced locally heavy rainfall that led to instances of flash flooding, which resulted in two separate fatalities in Ouachita Parish. A 13 year old boy drowned in a drainage canal in the Bawcomville community during the heavy rains, and an 80 year old female drove past barricades on a closed road in Calhoun several hours after the heavy rains had ended, with her car becoming submerged in the flood waters. Unfortunately, she was unable to escape and drowned.  These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Trees and power lines were blown down.", "ts_dict_index": [8757, 8758, 8759]}
+{"event_id": 866653, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-01-10 23:50:00", "end_date_time": "2020-01-10 23:50:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. A tree was blown down onto a house along Farm to Market Road 1798 near Highway 259.", "ts_dict_index": [8706, 8707, 8708]}
+{"event_id": 866664, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2020-01-11 00:19:00", "end_date_time": "2020-01-11 00:19:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Several softwood tree trunks were snapped along Farm to Market Road 959 by downburst winds estimated near 80 mph to the south of an EF-1 tornado just to the northwest.", "ts_dict_index": [8724, 8725, 8726]}
+{"event_id": 866660, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-01-11 00:05:00", "end_date_time": "2020-01-11 00:05:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Trees were downed near Hallsville.", "ts_dict_index": [8688, 8689, 8690]}
+{"event_id": 866650, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-01-10 23:53:00", "end_date_time": "2020-01-10 23:53:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Trees were blown down across Farm to Market Road 225 south of Henderson.", "ts_dict_index": [8703, 8704, 8705]}
+{"event_id": 866667, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-01-11 00:35:00", "end_date_time": "2020-01-11 00:35:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. Trees and power lines were downed in Karnack.", "ts_dict_index": [8712, 8713, 8714]}
+{"event_id": 1005484, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-01-01 15:30:00", "end_date_time": "2022-01-01 15:30:00", "narrative": "The second warmest December on record for Eastern Kentucky finished with a warm and moist air mass in place on New Year's Eve. A developing warm front slowly lifted northward out of the Tennessee Valley during the early morning hours on New Year's Day 2022 and stalled near the the Hal Rogers/Highway 80 corridor. The combination of strong lifting and near record atmospheric moisture levels for this time of year led to a line of training showers and thunderstorms, some with frequent lightning and intense downpours. The heaviest rainfall occurred from about 4 to 8 AM and led to many instances of flash flooding from Rockcastle County east northeast through Jackson, Owsley, Breathitt, Floyd, and Pike counties. By midday, locations affected by this activity had received 2 to 4 inches of rainfall. ||A temporary lull in the showers followed as the front shifted further to the north during the late morning and early afternoon. This allowed temperatures to surge into the 60s across the northeast Kentucky and into the lower to middle 70s closer the Kentucky/Tennessee border. ||Strong to severe thunderstorms developed in a high shear, low instability environment during the afternoon as a cold front swept from northwest to southeast across the area. While these storms mainly produced damaging wind gusts, one storm produced a brief spin-up tornado in far northwest Estill County. Impacts did not end with the passage of the cold front though; the excessive rainfall from earlier in the day quickly found its way into the mainstem rivers, sending multiple locations along the Kentucky and Red Rivers into flood stage. The most significant river flooding of the event ��� Moderate flood ��� was attained along the Kentucky River at Ravenna, the Red River at Clay City, and the South Fork Kentucky River at Booneville. A few other locations surpassed Minor flood stage. A tree was blown across powerlines along KY-635 West, about 6 miles out of Science Hill.", "ts_dict_index": [8766, 8767, 8768]}
+{"event_id": 952060, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2021-05-26 20:04:00", "end_date_time": "2021-05-26 20:04:00", "narrative": "Severe thunderstorms affected portions of south central Nebraska, south of Interstate 80, during the late evening hours of the 26th. Initial thunderstorm development for this event occurred well west of the area across NW Kansas and SW Nebraska during the late afternoon hours, in which several supercells developed in the vicinity of a low pressure, warm front, and dry line triple point. This is where the most severe weather, including tornadoes, occurred. Other, generally weaker, thunderstorms developed along a SW to NE line through Dawson County between 5-6PM CDT. Only marginally severe hail was reported there. The primary supercells approached far western portions of Furnas County between 7-8PM CDT, but by this time, they had weakened significantly and were no longer producing severe weather. The original Dawson County activity re-strengthened during the late evening hours, and ended up producing a narrow swath of damaging wind gusts from Phelps County eastward into Adams County. Wind gusts of 60-70 MPH were reported along with damage to an irrigation pivot. This activity weakened as it approached Hastings shortly after 9PM CDT. Additional thunderstorms developed between 9-10PM CDT in conjunction with an increasing low level jet. This activity focused across far southern Nebraska, but any severe weather remained further south across north central Kansas.||Overall, this event was less impactful than forecast. Much of south central Nebraska south of Interstate 80 and west of Highway 281 was included in a ���Moderate Risk��� in the SPC Day 1 Convective Outlook. A potent upper level disturbance provided strong deep layer shear, but combination of weaker instability (caused by convection earlier in the day) and slower upper disturbance led to the majority of severe convection to occur south and west of south central Nebraska. Outflow wind gusts estimated to be near 70 MPH damaged an irrigation pivot.", "ts_dict_index": [8772, 8773, 8774]}
+{"event_id": 866674, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-01-11 01:07:00", "end_date_time": "2020-01-11 01:07:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. A damage survey confirmed that a confined area of straight line winds caused scattered property and tree damage just south of Benton. A number of light poles and business signs were broken and bent as a result of the high winds. Benton Middle School received the greatest damage where the entire metal roof of one of its classroom wings was completely peeled back and removed.", "ts_dict_index": [8787, 8788, 8789]}
+{"event_id": 866676, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-01-11 01:10:00", "end_date_time": "2020-01-11 01:10:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Power lines were blown down onto the exit ramp of Interstate 49 at Kings Highway, some of which landed on a Shreveport police vehicle. However, the officer inside was not injured and was later rescued. Other debris was blown onto the southbound and northbound lanes of I-49 between Kings Highway and Interstate 20, prompting the closure of that section of the interstate.", "ts_dict_index": [8799, 8800, 8801]}
+{"event_id": 866675, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-01-11 01:10:00", "end_date_time": "2020-01-11 01:10:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Wind gusts were estimated to be near 60 mph in Southeast Shreveport.", "ts_dict_index": [8796, 8797, 8798]}
+{"event_id": 866671, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-01-11 00:44:00", "end_date_time": "2020-01-11 00:44:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. A damage survey confirmed that straight line winds estimated around 80 mph caused sporadic tree and branch damage along with some minor damage to homes in and near Oil City. One large tree was uprooted onto a home in Oil City, killing a 75 year old man inside.", "ts_dict_index": [8805, 8806, 8807]}
+{"event_id": 866672, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-01-11 00:44:00", "end_date_time": "2020-01-11 00:44:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Trees were blown down on Ferrylake Road in Oil City.", "ts_dict_index": [8802, 8803, 8804]}
+{"event_id": 867059, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2020-01-11 02:27:00", "end_date_time": "2020-01-11 02:27:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Numerous trees and power lines were downed blocking Highway 15 between Farmerville and Spearsville.", "ts_dict_index": [8784, 8785, 8786]}
+{"event_id": 818891, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-05-08 13:10:00", "end_date_time": "2019-05-08 13:10:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in several reports of tornadoes, with two separate tracks found across Northern Harrison and extreme Northeast Panola Counties, before the storms moved into North Louisiana by mid-afternoon. Locally heavy rainfall from the stronger storms within a short period of time also resulted in localized flash flooding across portions of Cass County, with flash flooding also reported across Eastern Harrison and Panola Counties during the early morning hours on May 9th as additional showers and thunderstorms redeveloped and moved repeatedly over the same areas. During the evening hours on the 9th, isolated severe thunderstorms developed over portions of Deep East Texas along old outflow boundaries from the storms earlier in the day. These storms produced large hail in extreme Southern Sabine County and Central Nacogdoches County before diminishing by midnight. Several trees were downed on Maple Street behind O'Reilly's Auto Parts on Highway 79.", "ts_dict_index": [8775, 8776, 8777]}
+{"event_id": 818884, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-05-08 13:05:00", "end_date_time": "2019-05-08 13:05:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in several reports of tornadoes, with two separate tracks found across Northern Harrison and extreme Northeast Panola Counties, before the storms moved into North Louisiana by mid-afternoon. Locally heavy rainfall from the stronger storms within a short period of time also resulted in localized flash flooding across portions of Cass County, with flash flooding also reported across Eastern Harrison and Panola Counties during the early morning hours on May 9th as additional showers and thunderstorms redeveloped and moved repeatedly over the same areas. During the evening hours on the 9th, isolated severe thunderstorms developed over portions of Deep East Texas along old outflow boundaries from the storms earlier in the day. These storms produced large hail in extreme Southern Sabine County and Central Nacogdoches County before diminishing by midnight. Several trees were blown down. A vehicle was blocked on a County Road southwest of the Lakeport community.", "ts_dict_index": [8781, 8782, 8783]}
+{"event_id": 818897, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-05-08 13:40:00", "end_date_time": "2019-05-08 13:40:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in several reports of tornadoes, with two separate tracks found across Northern Harrison and extreme Northeast Panola Counties, before the storms moved into North Louisiana by mid-afternoon. Locally heavy rainfall from the stronger storms within a short period of time also resulted in localized flash flooding across portions of Cass County, with flash flooding also reported across Eastern Harrison and Panola Counties during the early morning hours on May 9th as additional showers and thunderstorms redeveloped and moved repeatedly over the same areas. During the evening hours on the 9th, isolated severe thunderstorms developed over portions of Deep East Texas along old outflow boundaries from the storms earlier in the day. These storms produced large hail in extreme Southern Sabine County and Central Nacogdoches County before diminishing by midnight. Trees were downed on Meredith and Wingwood Street.", "ts_dict_index": [8778, 8779, 8780]}
+{"event_id": 867058, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2020-01-11 02:45:00", "end_date_time": "2020-01-11 02:45:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Trees and power lines were downed along Highway 33 near the Quigley community.", "ts_dict_index": [8808, 8809, 8810]}
+{"event_id": 866677, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-01-11 01:11:00", "end_date_time": "2020-01-11 01:11:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. The Shreveport Downtown Airport (KDTN) measured a wind gust of 59 mph.", "ts_dict_index": [8814, 8815, 8816]}
+{"event_id": 867057, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2020-01-11 02:30:00", "end_date_time": "2020-01-11 02:30:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Numerous trees and power lines were downed throughout Union Parish, prompting the closure of several roads including Highway 3121 north of Spearsville, and Highway 550 between Bridges Grocery and Highway 549.", "ts_dict_index": [8811, 8812, 8813]}
+{"event_id": 866683, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-01-11 01:25:00", "end_date_time": "2020-01-11 01:25:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Numerous trees were downed along Wilson Lane north of Haughton.", "ts_dict_index": [8820, 8821, 8822]}
+{"event_id": 867062, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2020-01-11 03:25:00", "end_date_time": "2020-01-11 03:25:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Trees were downed on Highway 2 near Pondee Road in the Crossroads community.", "ts_dict_index": [8793, 8794, 8795]}
+{"event_id": 867097, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-01-11 01:40:00", "end_date_time": "2020-01-11 01:40:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. A concrete baseball dugout at the Lakeside Jr/Sr. High School was destroyed with the roof being thrown into and damaging the new track field, while the other dugout was moved off its foundation. An awning at the school was also damaged as well.", "ts_dict_index": [8790, 8791, 8792]}
+{"event_id": 867060, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2020-01-11 02:45:00", "end_date_time": "2020-01-11 02:45:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Numerous trees and power lines were downed on Highway 33 between Farmerville and Marion.", "ts_dict_index": [8817, 8818, 8819]}
+{"event_id": 1084445, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:43:00", "end_date_time": "2023-04-28 23:50:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. The Fire Chief for Weslaco called and reported several business signs either damaged or blown down along Business 83. The largest sign blown down was an 8 foot tall Long John Silvers sign. An NWS Survey found there to be rust at the bottom of the sign, which kept wind estimates from being higher.", "ts_dict_index": [8859, 8860, 8861]}
+{"event_id": 1084468, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:55:00", "end_date_time": "2023-04-29 23:55:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. An NWS Storm Survey in southeastern Hidalgo County found metal roofs, large tree branches snapped, the top of a small palm tree snapped off and flung several yards, numerous power poles downed and a destroyed mobile home along Mile 3 Rd N between FM491 and Mile 2 E.", "ts_dict_index": [8853, 8854, 8855]}
+{"event_id": 1084443, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:30:00", "end_date_time": "2023-04-28 23:40:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. Member of the public shared an image of the roof blown off the Car Check Auto Service and Ultimate Dental Care building at the corner of N Cage Blvd and W Clark Ave. Timing estimated by radar.", "ts_dict_index": [8832, 8833, 8834]}
+{"event_id": 1084478, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:08:00", "end_date_time": "2023-04-28 23:20:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. A member of the public shared pictures of the Burger King in Palmview with its windows blown out around the play area. It's located at the intersection of Frontage Road and La Homa Road. Timing estimated from radar.", "ts_dict_index": [8838, 8839, 8840]}
+{"event_id": 1084440, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:22:00", "end_date_time": "2023-04-28 23:30:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. Weslaco Fire Marshal reported damage to four to five trees in his neighborhood in Mission.", "ts_dict_index": [8835, 8836, 8837]}
+{"event_id": 1084441, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:22:00", "end_date_time": "2023-04-28 23:30:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. Member of the public called in to report several trees that were uprooted along with several others that lost tree limbs. Timing based on their report and radar.", "ts_dict_index": [8841, 8842, 8843]}
+{"event_id": 1084261, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:55:00", "end_date_time": "2023-04-28 23:55:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. The ASOS station at the Mid Valley Airport (KTXW) recorded a wind gust of 50 knots at 12:55AM CDT.", "ts_dict_index": [8856, 8857, 8858]}
+{"event_id": 1084477, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:05:00", "end_date_time": "2023-04-28 23:15:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. A member of the public shared pictures with an NWS employee of significant damage to a mobile home trailer. The pictures show the mobile home destroyed with only one wall still standing. Timing estimated by radar.", "ts_dict_index": [8868, 8869, 8870]}
+{"event_id": 1084446, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:23:00", "end_date_time": "2023-04-28 23:30:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. Several citizens reported several large trees and traffic signs down along with stop signs pulled out of the ground along Highway 495 and Sugar Road. Timing estimated by radar.", "ts_dict_index": [8865, 8866, 8867]}
+{"event_id": 1084442, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:35:00", "end_date_time": "2023-04-28 23:35:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. An official NWS Survey found several sections of netting ripped at the Topgolf in Pharr. Timing estimated by radar.", "ts_dict_index": [8847, 8848, 8849]}
+{"event_id": 866678, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-01-11 01:07:00", "end_date_time": "2020-01-11 01:07:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Highway 3 between Burt Blvd to Highway 162 was temporarily closed due to debris in the roadway. The Sonic Restaurant sign on Burt Blvd was blown down.", "ts_dict_index": [8826, 8827, 8828]}
+{"event_id": 867061, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2020-01-11 03:00:00", "end_date_time": "2020-01-11 03:00:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Some shingles were blown off of a roof of a home just north of Natchez. One inch tree limbs were snapped as well. Report from mPING.", "ts_dict_index": [8823, 8824, 8825]}
+{"event_id": 1084257, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:20:00", "end_date_time": "2023-04-28 23:40:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. The ASOS station at McAllen-Miller International Airport observed winds equaling or exceeding 50 knots between 12:20AM CDT and 12:40AM CDT before briefly losing power shortly thereafter. The strongest wind gust of 64 knots was recorded at 12:34AM CDT. There was significant damage in and around the airport, including a Cessna that had been flipped and a Gulfstream aircraft that had been moved.  Damage at the airport is listed in a later report from the NWS Storm Survey.", "ts_dict_index": [8844, 8845, 8846]}
+{"event_id": 1084455, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:47:00", "end_date_time": "2023-04-28 23:50:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. An NWS Storm Survey found damage to a large, corrugated light steel fence that was blown down along S FM493 a few miles south of Donna. There were several other areas of damage between there and the intersection of Calle Santiago and Creager Road. That damage included a low masonry wall of about 4 feet in height blown over at intersection of Midway Road and W 34th St; and several buildings, including homes, with partial loss of the roof of vinyl/metal siding along S Texas Blvd on the west side of Progreso.", "ts_dict_index": [8850, 8851, 8852]}
+{"event_id": 1084453, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:32:00", "end_date_time": "2023-04-28 23:32:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. An NWS Storm Survey in and around the McAllen-Miller International Airport found a Cessna had been flipped onto its roof and a Gulfstream jet turned and pushed into the grass by strong thunderstorm winds. The McAllen-Miller International Airport ASOS (KMFE) officially recorded a wind gust of 74 mph before losing power. Wind estimates were closer to 74 knots, or 85 mph, due to the flipping of the Cessna. Additional damage was found downstream, or east, of the airport with large oak tree branches having been snapped and one oak tree snapped near its base at the McAllen Country Club. The roof of the Radisson Hotel McAllen Airport (0.5-1 mile east-southeast of the airport) was partially blown off and fell onto cars in the parking lot. The survey crew was told the roof was 3 years old with the building older than that. Decking was estimated to have been 55 feet above ground level and was fully exposed from the west. While winds are estimated to have been 74 knots, or 85 mph, it is possible higher winds were experienced at the roofline. Timing based on KMFE wind gusts before losing power.", "ts_dict_index": [8871, 8872, 8873]}
+{"event_id": 1084476, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:53:00", "end_date_time": "2023-04-28 23:55:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. A member of the public shared several pictures from the Progreso Port of Entry area showing damage to several grain silos and apparatus on the top of the silos. A few pictures in particular show a grain silo caved in. One limiting factor from going higher is the lack of damage to nearby mobile office structures in the foreground.", "ts_dict_index": [8874, 8875, 8876]}
+{"event_id": 1084433, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 22:59:00", "end_date_time": "2023-04-28 23:05:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. Member of the publics shows several mesquite trees down along Garza Avenue north of Military road. Time estimated by radar.", "ts_dict_index": [8883, 8884, 8885]}
+{"event_id": 1084452, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:29:00", "end_date_time": "2023-04-28 23:29:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. An NWS Storm Survey found more than 50 percent of shingles off on a two story building with full exposure to the west-northwest along S 29th St in McAllen. To the southeast of there, a tin roof and over a dozen trusses and rafters were taken off a lumber store and blown across the road. Additionally, the parapet roof over the Ross Department store was partially blown off. The roof was approximately 50 feet off the ground.", "ts_dict_index": [8880, 8881, 8882]}
+{"event_id": 1084434, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:02:00", "end_date_time": "2023-04-28 23:10:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. Video from the public shows the metal roof of a carport peeled back near the intersection of Mile 3 Road and Tom Gill Road. Time estimated by radar.", "ts_dict_index": [8886, 8887, 8888]}
+{"event_id": 1084436, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:14:00", "end_date_time": "2023-04-28 23:20:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. Broadcast media shared a picture of a few food trucks and trailers flipped over near the intersection of Bryan Road and Business 83 near Mission City Hall. Time estimated by radar.", "ts_dict_index": [8892, 8893, 8894]}
+{"event_id": 1084437, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:20:00", "end_date_time": "2023-04-28 23:30:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. Member of the public shared pictures of damage to several large oak trees, including several large branches about 8 to 12 inches in diameter, that had snapped. Timing estimated by radar.", "ts_dict_index": [8898, 8899, 8900]}
+{"event_id": 1084454, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:28:00", "end_date_time": "2023-04-28 23:30:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. An NWS Storm Survey found a McAllen Public Works truck impaled with 2x4s that were lofted into the front passengers side near the intersection of Nolana Ave W and N Bensten Road. The 2x4s was pulled from a weakly constructed wood scaffold nearby. Additional reports of semi-trucks turned over were reported by the broadcast media in the Walmart parking a few blocks east along Nolana Loop. Additional damage was found along N 23rd St with columns, which were rusted, of a gas station canopy bent near the base at the corner of N 23rd Street and Daffodil Ave. There was also minor metal damage to the roof of an abandoned car wash along N 23rd St across from McAllen High School.", "ts_dict_index": [8889, 8890, 8891]}
+{"event_id": 1084464, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:50:00", "end_date_time": "2023-04-29 23:50:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. An NWS Storm Survey found some metal roof damage to Dorothy Thompson Middle School in Progreso. Additional damage was found in and around the town of Progreso, including several large tree branches down and a large tree partially uprooted at the corner of Creager Road and S Mile 2 W on the southeast side of Progreso. There was also significant damage to the roof of a large metal warehouse just east of the intersection of Creager Road and S Mile 2 W.", "ts_dict_index": [8895, 8896, 8897]}
+{"event_id": 1087890, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-03 10:34:00", "end_date_time": "2023-03-03 10:34:00", "narrative": "A prolonged damaging gradient wind event combined with an intense squall line during the daylight hours of the 3rd to produce widespread wind damage and impacts to the region. Numerous power outages resulted from power poles being snapped and power lines being brought down.  All told, thousands were without power in north Alabama for at least for a couple of hours, and in some cases lasting into the next two to three days. Hundreds of reports of trees or limbs being knocked down were received, in many cases on homes, vehicles and other structures. Sadly, two people were killed outside their homes from fallen trees while picking up debris after the line of thunderstorms went through and additional high winds developed.  Other minor injuries were also reported including one utility worker who was working to restore power.||A powerful low pressure system intensified rapidly as it moved northeast from Texas through Arkansas, southeast Missouri into western Kentucky.  In doing so, very windy conditions developed across the Tennessee Valley ahead of an associated cold front and squall line. South winds increased to 35-45 mph, with gusts of 55-60 mph at times. An intense squall line moved in from Mississippi during the mid morning hours, sweeping east across the rest of the area through the midday hours. Peak wind gusts of 50-60 mph were reported frequently, with one gust up to 77 mph at Pryor Field in Decatur (Morgan County) and 69 mph at the Huntsville International Airport (Madison County). Also, at least two tornadoes were spawned by the line in Jackson County.  Behind the line of thunderstorms, the sky cleared out rapidly, but southwest winds intensified as well, with 35-45 mph sustained winds, gusting at 55-65 mph. The winds finally subsided quickly near sunset, but not after additional damage occurred. Recorded at the Northwest Alabama Regional Airport.", "ts_dict_index": [8901, 8902, 8903]}
+{"event_id": 1084451, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:30:00", "end_date_time": "2023-04-28 23:30:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. An NWS Storm Survey found extensive damage along W Business 83 in McAllen. A poorly constructed roof and cinderblock wall with no bond beam caused a portion of the roof to collapse; the wall was about 35 feet high and fully exposed. A decently constructed metal roof system was partially torn off along with a garage door partially caved in at the intersection of N 22nd St and Beech Ave.  The Linares Auto Center sign was also blown over at the corner of Business 83 and S 21st Street. The sign was mounted in concrete with some rust. It also fell on at least 3 cars in the parking lot. ||The strongest wind indicator was along S 20th St just south of Business 83 where wooden poles were bent or snapped along with several large tree limbs down.", "ts_dict_index": [8904, 8905, 8906]}
+{"event_id": 867096, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-01-11 01:20:00", "end_date_time": "2020-01-11 01:20:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. Major distribution power lines were downed across the roadways at the Port of Caddo-Bossier.", "ts_dict_index": [8829, 8830, 8831]}
+{"event_id": 1084450, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:25:00", "end_date_time": "2023-04-28 23:25:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. An NWS Storm Survey found roofing material still in plastic along with pull back of cinder block cladding near the intersection of S Bryan Road and W Frontage Road. A little ways east, a large billboard and pole fell onto vehicles. Pole was anchored into dirt, but sitting on high water from recent rains and uprooted. Lower wind speeds used based on poor anchoring and lack of surrounding damage.", "ts_dict_index": [8907, 8908, 8909]}
+{"event_id": 1084439, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 23:30:00", "end_date_time": "2023-04-28 23:30:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. The canopy over the gas pumps at the Exxon Gas station at the corner of Lark and N 23rd Street was blown over and pushed partially across the road. An official NWS Storm Survey team looked at the poles to the canopy and found that several of them had rust, which led to a slightly lower wind rating. Timing based on radar.", "ts_dict_index": [8862, 8863, 8864]}
+{"event_id": 1032883, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-06-24 23:48:00", "end_date_time": "2022-06-24 23:48:00", "narrative": "Mainly between 10:30 p.m. CDT on Friday the 24th and 2 a.m. CDT on Saturday the 25th, a small but potent complex of strong to severe thunderstorms tracked from southwestern into east-central portions of South Central Nebraska, prompting a few instances of marginally-severe wind gusts. The brunt of this complex affected areas between Interstate 80 and the Nebraska-Kansas state line, where numerous measured gusts of 45-55 MPH occurred. A few gusts reached or exceeded severe limits before activity abruptly weakened over northern York/southern Polk counties. The peak measured gust of 63 MPH occurred at two spots, near Holbrook in Furnas County and near Atlanta in Phelps County.||West-southwesterly flow prevailed in the upper levels, as broad high pressure was in place over southern and eastern portions of the CONUS. To the northwest, an area of low pressure was sliding east into central Canada, with a trough axis extending south into the Rockies and eventually the Plains. At the surface, the local area had east-southeasterly winds in place, with a trough axis extending through western Nebraska and Kansas between weak areas of low pressure.  With better forcing to the north and west and warm mid-level temperatures keeping things capped, the daytime and early-mid evening hours remained dry. Thunderstorms developed during the late afternoon hours along the surface trough axis over western Nebraska, eventually pushing east into South Central Nebraska after dark. Though the better upper level lift focused well to the north, an increasing low-level jet and warm air advection aided in sustaining this slightly elevated activity as it shifted east through portions of the local area. While mesoscale analysis showed most-unstable CAPE values exceeding 3000 J/kg, deep layer shear was rather weak, around 20-30 knots. A wind gust of 58 MPH was measured by the Hastings Airport ASOS.", "ts_dict_index": [8910, 8911, 8912]}
+{"event_id": 886897, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:18:00", "end_date_time": "2020-06-03 12:18:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 68 MPH gust reported by a HADS sensor in Beach Haven Heights.", "ts_dict_index": [8925, 8926, 8927]}
+{"event_id": 886793, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 19:37:00", "end_date_time": "2020-06-03 19:37:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed power lines reported in Beach Haven. Time estimated from radar.", "ts_dict_index": [8952, 8953, 8954]}
+{"event_id": 886794, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:29:00", "end_date_time": "2020-06-03 11:29:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Spotter measured a gust of 56 KTS in Delanco. Time estimated from radar.", "ts_dict_index": [8931, 8932, 8933]}
+{"event_id": 885755, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:27:00", "end_date_time": "2020-06-03 11:27:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple large trees down and at least one power pole snapped in Cinniminson. Report via social media with photos. Time estimated from radar.", "ts_dict_index": [8928, 8929, 8930]}
+{"event_id": 886595, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 12:05:00", "end_date_time": "2020-06-03 12:05:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed trees onto power lines and minor property damage reported on Turtle Creek Road near Wading River. Time estimated from radar.", "ts_dict_index": [8940, 8941, 8942]}
+{"event_id": 886768, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:41:00", "end_date_time": "2020-06-03 18:41:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed trees on the New Jersey Turnpike near Exit 3 near Haddon Leigh. Time estimated from radar.", "ts_dict_index": [8937, 8938, 8939]}
+{"event_id": 886269, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:45:00", "end_date_time": "2020-06-03 11:45:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed trees throughout the area south of Allentown, NJ. Spotter estimated winds at 60 MPH.", "ts_dict_index": [8955, 8956, 8957]}
+{"event_id": 886224, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:37:00", "end_date_time": "2020-06-03 11:37:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree snapped near the intersection of State Highway 70 and Medford Leas Road. Time estimated from radar.", "ts_dict_index": [8916, 8917, 8918]}
+{"event_id": 886797, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:30:00", "end_date_time": "2020-06-03 11:30:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 51 knot gust reported by a New Jersey Weathernet sensor in Pennsauken.", "ts_dict_index": [8922, 8923, 8924]}
+{"event_id": 886050, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:30:00", "end_date_time": "2020-06-03 11:30:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees down blocking roadways in Haddonfield. Time estimated from radar.", "ts_dict_index": [8949, 8950, 8951]}
+{"event_id": 886223, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:35:00", "end_date_time": "2020-06-03 11:35:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees and limbs down in Marlton and Voorhees. Time estimated from radar.", "ts_dict_index": [8946, 8947, 8948]}
+{"event_id": 886767, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:40:00", "end_date_time": "2020-06-03 18:40:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous trees and limbs down in the Somerdale area. Time estimated from radar.", "ts_dict_index": [8934, 8935, 8936]}
+{"event_id": 885756, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:27:00", "end_date_time": "2020-06-03 11:27:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed traffic light on State Highway 168 at Browning Road in Bellmawr.  Time estimated from radar.", "ts_dict_index": [8919, 8920, 8921]}
+{"event_id": 1084432, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-28 22:55:00", "end_date_time": "2023-04-28 23:05:00", "narrative": "Strong to severe thunderstorms ahead of a strong cold front raced along the Rio Grande from the evening of April 28th into the morning of April 29th. The initial phase of the storms produced large hail across Zapata and Starr Counties the evening of April 28th. The storms congealed into a squall line along the Rio Grande in southeastern Starr County and southwestern Hidalgo County just before midnight. This squall line went on to race across southern Hidalgo County, leaving a trail of destruction in its wake. ||An official NWS Storm Survey concluded the squall line produced several gusts between 75 to 85 mph at the surface, with higher gusts experienced at higher levels. Some of the damage included a plane being destroyed at McAllen-Miller International Airport; numerous poorly anchored roofs lifted off buildings; dozens, if not hundreds, of broken power poles; and dozens of damaged or destroyed billboards. ||The storms then went on to produce more damage across southeastern Hidalgo County and into eastern Cameron County early in the morning of April 29th. Another official NWS Storm Survey concluded winds of 70 to 80 mph were experienced here, which downed several trees and power poles, a few metal roofs lifted off and caused numerous power outages.||Total damage was unknown due to the large number of locations impacted. A state disaster declaration was given for Hidalgo County following the event, and dollar damages and recovery costs were expected to be more than $50 million.  Those numbers will be updated when available at a later date.||Times listed for individual wind events along the NWS Storm Survey were based on best estimates of when the strongest winds occurred; in general, strongest winds at or above severe limits (58 mph) likely lasted between 5 and 8 minutes either side of the listed time. Video shared by a member of the public shows several large trees down along El Pinto Road near Rosendo Benavides Elementary School. Time estimated by radar.", "ts_dict_index": [8877, 8878, 8879]}
+{"event_id": 886227, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:37:00", "end_date_time": "2020-06-03 11:37:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree and wires on U.S. Highway 130 southbound south of State Highway 156 near Bordentown.  Time estimated from radar.", "ts_dict_index": [8964, 8965, 8966]}
+{"event_id": 886267, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:43:00", "end_date_time": "2020-06-03 11:43:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of trees and power lines down in and near Pemberton. Time estimated from radar.", "ts_dict_index": [8961, 8962, 8963]}
+{"event_id": 886063, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:32:00", "end_date_time": "2020-06-03 11:32:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Photo shows a large tree downed on fence near Haddon Heights. Time estimated from radar.", "ts_dict_index": [8967, 8968, 8969]}
+{"event_id": 886772, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:46:00", "end_date_time": "2020-06-03 18:46:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Debris down on the railroad tracks along Atlantic Avenue in Somerdale.", "ts_dict_index": [8958, 8959, 8960]}
+{"event_id": 886836, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:14:00", "end_date_time": "2020-06-03 12:14:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Measured 72 MPH wind gust from Wxunderground knjlongb42 in Beach Haven Terrace.", "ts_dict_index": [8913, 8914, 8915]}
+{"event_id": 886599, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:05:00", "end_date_time": "2020-06-03 12:05:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous reports of trees and power lines down in Toms River. Time estimated from radar.", "ts_dict_index": [8976, 8977, 8978]}
+{"event_id": 886597, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:05:00", "end_date_time": "2020-06-03 12:05:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on Garden State Parkway southbound north of State Highway 72 in Stafford Township.  Time estimated from radar.", "ts_dict_index": [8988, 8989, 8990]}
+{"event_id": 886896, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:15:00", "end_date_time": "2020-06-03 12:15:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 63 MPH gust was reported by a member of the general public in Seaside Park.", "ts_dict_index": [8979, 8980, 8981]}
+{"event_id": 886272, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:48:00", "end_date_time": "2020-06-03 11:48:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Route 537 by Upper Elementary School near Jacobstown blocked by downed trees. Spotter estimated gusts in excess of 60 MPH. Time estimated from radar.", "ts_dict_index": [8973, 8974, 8975]}
+{"event_id": 886061, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:32:00", "end_date_time": "2020-06-03 11:32:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees snapped on Pioneer Boulevard off of Woodlane Road in Westampton.  Time estimated from radar.", "ts_dict_index": [8997, 8998, 8999]}
+{"event_id": 886796, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:30:00", "end_date_time": "2020-06-03 11:30:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 56 knot gust measured in Willingboro.  Large branches down.", "ts_dict_index": [8982, 8983, 8984]}
+{"event_id": 886270, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:46:00", "end_date_time": "2020-06-03 11:46:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree downed near the intersection of Powell Place Road and Eldorado Driver near Leisuretown.  Report via social media with photo. Time estimated from radar.", "ts_dict_index": [8991, 8992, 8993]}
+{"event_id": 886225, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:37:00", "end_date_time": "2020-06-03 11:37:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several large trees snapped in Lumberton. Report via social media with photo. Time estimated from radar.", "ts_dict_index": [8994, 8995, 8996]}
+{"event_id": 885761, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:29:00", "end_date_time": "2020-06-03 11:29:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on New Jersey Turnpikd north of State Highway 73 near Moorestown. Time estimated from radar.", "ts_dict_index": [8970, 8971, 8972]}
+{"event_id": 886770, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:45:00", "end_date_time": "2020-06-03 18:45:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several downed trees and limbs in the Haddon Heights area.", "ts_dict_index": [8985, 8986, 8987]}
+{"event_id": 886268, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:45:00", "end_date_time": "2020-06-03 11:45:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous trees down near Tabernacle. Time estimated from radar.", "ts_dict_index": [8943, 8944, 8945]}
+{"event_id": 886899, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:18:00", "end_date_time": "2020-06-03 12:18:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A gust of 68 MPH was reported by a Wxflow sensor in Beach Haven Heights.", "ts_dict_index": [9003, 9004, 9005]}
+{"event_id": 886895, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:15:00", "end_date_time": "2020-06-03 12:15:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 59 MPH wind gust was measured by a spotter in Surf City.", "ts_dict_index": [9012, 9013, 9014]}
+{"event_id": 886062, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:32:00", "end_date_time": "2020-06-03 11:32:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree uprooted and blocking most of Bridgeboro Road near Echo Avenue. Time estimated from radar.", "ts_dict_index": [9006, 9007, 9008]}
+{"event_id": 886271, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:48:00", "end_date_time": "2020-06-03 11:48:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of trees and power lines down near Country Lake Estates. Time estimated from radar.", "ts_dict_index": [9015, 9016, 9017]}
+{"event_id": 886226, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:37:00", "end_date_time": "2020-06-03 11:37:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on High Street in Mount Holly. Time estimated from radar.", "ts_dict_index": [9009, 9010, 9011]}
+{"event_id": 886773, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:47:00", "end_date_time": "2020-06-03 18:47:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large tree down with multipl parked cars underneath in Somerdale.", "ts_dict_index": [9000, 9001, 9002]}
+{"event_id": 886598, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:05:00", "end_date_time": "2020-06-03 12:05:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of power lines down in Barnegat Township. Time estimated from radar.", "ts_dict_index": [9021, 9022, 9023]}
+{"event_id": 886559, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:00:00", "end_date_time": "2020-06-03 12:00:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of downed trees and wires east of Lakehurst. Time estimated from radar.", "ts_dict_index": [9024, 9025, 9026]}
+{"event_id": 886819, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 11:58:00", "end_date_time": "2020-06-03 11:58:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 65 MPH wind gust reported by the AWOS unit at Joint Base Mcguire in Lakehurst.", "ts_dict_index": [9078, 9079, 9080]}
+{"event_id": 886795, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:30:00", "end_date_time": "2020-06-03 11:30:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 63 knot gust measured at Delran High School  Last reading before instrument failed. Time estimated from radar.", "ts_dict_index": [9018, 9019, 9020]}
+{"event_id": 886821, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:02:00", "end_date_time": "2020-06-03 12:02:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 58 MPH wind gust reported by the AWOS station at the Ocean County Airport.", "ts_dict_index": [9036, 9037, 9038]}
+{"event_id": 886554, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 11:58:00", "end_date_time": "2020-06-03 11:58:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A number of large trees downed or damaged in Lakehurst. Time estimated from radar.", "ts_dict_index": [9072, 9073, 9074]}
+{"event_id": 886842, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:15:00", "end_date_time": "2020-06-03 12:15:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 72 MPH wind gust reported by a New Jersey Weathernet sensor in Harvey Cedars (knjharve5).", "ts_dict_index": [9054, 9055, 9056]}
+{"event_id": 886553, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 11:54:00", "end_date_time": "2020-06-03 11:54:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of downed trees and power lines near Whiting. Time estimated from radar.", "ts_dict_index": [9084, 9085, 9086]}
+{"event_id": 886218, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:35:00", "end_date_time": "2020-06-03 11:35:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple trees down blocking roadways in Moorestown. Time estimated from radar.", "ts_dict_index": [9042, 9043, 9044]}
+{"event_id": 886060, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:32:00", "end_date_time": "2020-06-03 11:32:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Trees down in Delran with some on power lines and some blocking roads, including on Haines Mill Road. Time estimated from radar.", "ts_dict_index": [9027, 9028, 9029]}
+{"event_id": 886222, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:35:00", "end_date_time": "2020-06-03 11:35:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees onto power lines on Borton Landing Road between Creek Road and Hartford Road in Moorestown. Some power poles leaning over the road. Time estimated from radar.", "ts_dict_index": [9030, 9031, 9032]}
+{"event_id": 886261, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:40:00", "end_date_time": "2020-06-03 11:40:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Trees down near Mount Holly. Time estimated from radar.", "ts_dict_index": [9045, 9046, 9047]}
+{"event_id": 886555, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 11:58:00", "end_date_time": "2020-06-03 11:58:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous trees down near Lakehurst. Time estimated from radar.", "ts_dict_index": [9048, 9049, 9050]}
+{"event_id": 886615, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:40:00", "end_date_time": "2020-06-03 18:40:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree limbs and fencing at a residence in Blackwood. Time estimated from radar.", "ts_dict_index": [9057, 9058, 9059]}
+{"event_id": 886789, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 19:07:00", "end_date_time": "2020-06-03 19:07:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Debris down on the railroad tracks along Atlantic Avenue in Somerdale. Time estimated from radar.", "ts_dict_index": [9051, 9052, 9053]}
+{"event_id": 886232, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:39:00", "end_date_time": "2020-06-03 11:39:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed trees and power poles on U.S. Highway 206 south of Vincentown-Buddtown Road in Southampton Township.  Time estimated from radar.", "ts_dict_index": [9081, 9082, 9083]}
+{"event_id": 886263, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:40:00", "end_date_time": "2020-06-03 11:40:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large trees snapped near Cherry Hill.", "ts_dict_index": [9066, 9067, 9068]}
+{"event_id": 886057, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:31:00", "end_date_time": "2020-06-03 11:31:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed power lines on U.S. Highway 30 east of Graisbury Avenue.  Time estimated from radar.", "ts_dict_index": [9075, 9076, 9077]}
+{"event_id": 886054, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:31:00", "end_date_time": "2020-06-03 11:31:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on Interstate 295 southbound at Exit 43. Time estimated from radar.", "ts_dict_index": [9060, 9061, 9062]}
+{"event_id": 886219, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:35:00", "end_date_time": "2020-06-03 11:35:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed trees and power lines on Hainesport Road between State Highway 38 and Marne Highway in Hainesport. Time estimated from radar.", "ts_dict_index": [9063, 9064, 9065]}
+{"event_id": 886822, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:05:00", "end_date_time": "2020-06-03 12:05:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 67 MPH wind gust reported by the New Jersey Weathernet sensor in Berkeley Township.", "ts_dict_index": [9033, 9034, 9035]}
+{"event_id": 887364, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 15:40:00", "end_date_time": "2020-06-03 15:40:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 92 MPH wind gust was reported near Surf City on social media.", "ts_dict_index": [9096, 9097, 9098]}
+{"event_id": 887504, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:15:00", "end_date_time": "2020-06-03 12:15:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 78 MPH gust measured by a Weatherunderground mesonet site at Chadwick, Long Beach Island (knjlaval14).", "ts_dict_index": [9090, 9091, 9092]}
+{"event_id": 886231, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:39:00", "end_date_time": "2020-06-03 11:39:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Multiple trees down near the intersection of State Highway 70 and Old Red Lion Road near Medford Lakes. Time estimated by radar.", "ts_dict_index": [9105, 9106, 9107]}
+{"event_id": 886070, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:33:00", "end_date_time": "2020-06-03 11:33:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed power poles and wires on U.S. Highway 130 southbound near Neck Road.  Time estimated from radar.", "ts_dict_index": [9108, 9109, 9110]}
+{"event_id": 886779, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:58:00", "end_date_time": "2020-06-03 18:58:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree down in yard and dime-sized hail near Clementon.", "ts_dict_index": [9099, 9100, 9101]}
+{"event_id": 886234, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:39:00", "end_date_time": "2020-06-03 11:39:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on State Highway 68 near Monmouth Road in Wrightstown. Time estimated from radar.", "ts_dict_index": [9102, 9103, 9104]}
+{"event_id": 885739, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:19:00", "end_date_time": "2020-06-03 11:19:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Photo from social media shows a large tree split in half and downed onto a fence in Haddon Heights. Time estimated from radar.", "ts_dict_index": [9093, 9094, 9095]}
+{"event_id": 886052, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:31:00", "end_date_time": "2020-06-03 11:31:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree down on a car, also landing on a section of a home, near Moorestown.  No signficant damage apparent to home. Time estimated from radar.", "ts_dict_index": [9039, 9040, 9041]}
+{"event_id": 886826, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:12:00", "end_date_time": "2020-06-03 12:12:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 59 MPH wind gust reported by a WxFlow sensor near Ocean Beach Marina.", "ts_dict_index": [9129, 9130, 9131]}
+{"event_id": 886841, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:15:00", "end_date_time": "2020-06-03 12:15:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. An 89 MPH wind gusts reported by a mesonet station in Beach Haven (knjsurfc12).", "ts_dict_index": [9123, 9124, 9125]}
+{"event_id": 886823, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:08:00", "end_date_time": "2020-06-03 12:08:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 63 MPH wind gust reported by a WeatherFlow sensor in Seaside Heights.", "ts_dict_index": [9120, 9121, 9122]}
+{"event_id": 885751, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:25:00", "end_date_time": "2020-06-03 11:25:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on U.S. Highway 130 southbound south of Browning Road in Pennsauken. Time estimated from radar.", "ts_dict_index": [9135, 9136, 9137]}
+{"event_id": 887363, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:40:00", "end_date_time": "2020-06-03 11:40:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 60 MPH gust was reported in Lumberton by a trained spotter.", "ts_dict_index": [9126, 9127, 9128]}
+{"event_id": 886048, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:30:00", "end_date_time": "2020-06-03 11:30:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Solar panels damaged and blown off of Cold Spring Elementary School  Report via social medial, with photos. Time estimated from radar.", "ts_dict_index": [9111, 9112, 9113]}
+{"event_id": 885741, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:19:00", "end_date_time": "2020-06-03 11:19:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Extensive tree damage with several trees and large branches down in Gloucester Heights. Time estimated from radar.", "ts_dict_index": [9114, 9115, 9116]}
+{"event_id": 886056, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:31:00", "end_date_time": "2020-06-03 11:31:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree and wires on U.S. Highway 30 west of State Highway 41 near Barrington. |Time estimated from radar.", "ts_dict_index": [9138, 9139, 9140]}
+{"event_id": 886046, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:30:00", "end_date_time": "2020-06-03 11:30:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous trees down blocking roadways in Willingboro.  Time estimated from radar.", "ts_dict_index": [9132, 9133, 9134]}
+{"event_id": 886221, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:35:00", "end_date_time": "2020-06-03 11:35:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Trees down on Memorial Lane in Hainesport. Time estimated from radar.", "ts_dict_index": [9141, 9142, 9143]}
+{"event_id": 886611, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 13:00:00", "end_date_time": "2020-06-03 13:00:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree uprooted on Cuthbert Blvd in Haddon Township. Time estimated from radar.", "ts_dict_index": [9069, 9070, 9071]}
+{"event_id": 886558, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:00:00", "end_date_time": "2020-06-03 12:00:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees down near Beachwood. Time estimated from radar.", "ts_dict_index": [9147, 9148, 9149]}
+{"event_id": 886900, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:19:00", "end_date_time": "2020-06-03 12:19:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Measaured 93 MPH wind gust from Wxunderground knjlongb42.", "ts_dict_index": [9153, 9154, 9155]}
+{"event_id": 886799, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:35:00", "end_date_time": "2020-06-03 11:35:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A measured gust of 63 knots in Moorestown.  Time estimated from radar.", "ts_dict_index": [9159, 9160, 9161]}
+{"event_id": 886818, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:40:00", "end_date_time": "2020-06-03 11:40:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 60 MPH wind gust reported by a mesonet station on Wxunderground.", "ts_dict_index": [9156, 9157, 9158]}
+{"event_id": 886266, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:42:00", "end_date_time": "2020-06-03 11:42:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Trees uprooted near State Highway 70 and Huntington Drive near Leisuretown. Time estimated from radar.", "ts_dict_index": [9144, 9145, 9146]}
+{"event_id": 886274, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:40:00", "end_date_time": "2020-06-03 11:40:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. New Jersey Weather Net sensor site at Columbus reported a gust of 67 MPH.", "ts_dict_index": [9165, 9166, 9167]}
+{"event_id": 886614, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:38:00", "end_date_time": "2020-06-03 18:38:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of trees and power lines down in Blackwood. Time estimated from radar.", "ts_dict_index": [9150, 9151, 9152]}
+{"event_id": 886820, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:00:00", "end_date_time": "2020-06-03 12:00:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 58 MPH wind gust reported by a mesonet station in Jackson Township.", "ts_dict_index": [9087, 9088, 9089]}
+{"event_id": 886068, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:33:00", "end_date_time": "2020-06-03 11:33:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on the New Jersey Turnpike south of Exit 5. Time estimated from radar.", "ts_dict_index": [9177, 9178, 9179]}
+{"event_id": 886228, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:38:00", "end_date_time": "2020-06-03 11:38:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several power poles toppled on Eayrestown Road near Lumberton. Time estimated from radar.", "ts_dict_index": [9168, 9169, 9170]}
+{"event_id": 885762, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:29:00", "end_date_time": "2020-06-03 11:29:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees and power poles downed or snapped on Center Street between Virginia Avenue and Highland Avenue in Haddon Heights. Time estimated from radar.", "ts_dict_index": [9174, 9175, 9176]}
+{"event_id": 886064, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:32:00", "end_date_time": "2020-06-03 11:32:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Numerous trees snapped and uprooted with some onto houses in Westmont. Time estimated from radar.", "ts_dict_index": [9171, 9172, 9173]}
+{"event_id": 886217, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:35:00", "end_date_time": "2020-06-03 11:35:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree down on Larchmont Boulevard towards Union Mill.  Time estimated from radar.", "ts_dict_index": [9117, 9118, 9119]}
+{"event_id": 886602, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:10:00", "end_date_time": "2020-06-03 12:10:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several trees down near Mystic Island. Time estimated from radar.", "ts_dict_index": [9180, 9181, 9182]}
+{"event_id": 886551, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:51:00", "end_date_time": "2020-06-03 11:51:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large, healthy tree snapped, report via social media with a photo near Shamong. Time estimated from radar.", "ts_dict_index": [9186, 9187, 9188]}
+{"event_id": 886069, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:33:00", "end_date_time": "2020-06-03 11:33:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree near the Bridle Club on Ridgewood Way. Report via social media with photo. Time estimated from radar.", "ts_dict_index": [9192, 9193, 9194]}
+{"event_id": 886230, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:39:00", "end_date_time": "2020-06-03 11:39:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Tree down near a home in Tabernacle. No damage reported to house. Time estimated by radar.", "ts_dict_index": [9189, 9190, 9191]}
+{"event_id": 886047, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:30:00", "end_date_time": "2020-06-03 11:30:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several large trees and limbs down throughout the Beverly area.  Time estimated from radar.", "ts_dict_index": [9195, 9196, 9197]}
+{"event_id": 886220, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:35:00", "end_date_time": "2020-06-03 11:35:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Trees down on homes in Essex Place near Hainesport. Time estimated from radar.", "ts_dict_index": [9204, 9205, 9206]}
+{"event_id": 885749, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:25:00", "end_date_time": "2020-06-03 11:25:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on Interstate 76 Westbound ramp to Exit 1C in Gloucester Heights. Time estimated from radar.", "ts_dict_index": [9198, 9199, 9200]}
+{"event_id": 886055, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 11:31:00", "end_date_time": "2020-06-03 11:31:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on New Jersey Turnpike north of State Highway 168. Time estimated from radar.", "ts_dict_index": [9201, 9202, 9203]}
+{"event_id": 886775, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:53:00", "end_date_time": "2020-06-03 18:53:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Several reports of power lines down in the Chesilhurst area. Time estimated from radar.", "ts_dict_index": [9162, 9163, 9164]}
+{"event_id": 886901, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:20:00", "end_date_time": "2020-06-03 12:20:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A 92 MPH gust reported in Surf City.  Time updated based on when observation was taken.", "ts_dict_index": [9219, 9220, 9221]}
+{"event_id": 886839, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:14:00", "end_date_time": "2020-06-03 12:14:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. An 87 MPH wind gust from a WXFLOW sensor south of Mantoloking.", "ts_dict_index": [9216, 9217, 9218]}
+{"event_id": 886825, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:10:00", "end_date_time": "2020-06-03 12:10:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A wind gust of 65 MPH reported by a WxFlow sensor in Beach Haven Heights.", "ts_dict_index": [9213, 9214, 9215]}
+{"event_id": 886557, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:00:00", "end_date_time": "2020-06-03 12:00:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed tree on State Highway 72 east of Barnegat Road. Time estimated from radar.", "ts_dict_index": [9207, 9208, 9209]}
+{"event_id": 1064217, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-01-03 04:21:00", "end_date_time": "2023-01-03 04:21:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. The roof of a warehouse was damaged. Nearby trailers were also blown over.", "ts_dict_index": [9234, 9235, 9236]}
+{"event_id": 1064127, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-01-02 19:50:00", "end_date_time": "2023-01-02 19:50:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. A tree was blown down on Highway 527.", "ts_dict_index": [9240, 9241, 9242]}
+{"event_id": 886801, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-06-03 11:35:00", "end_date_time": "2020-06-03 11:35:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. A measured gust of 56 knots at a New Jersey Weathernet sensor in Moorestown.", "ts_dict_index": [9222, 9223, 9224]}
+{"event_id": 886612, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:35:00", "end_date_time": "2020-06-03 18:35:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Downed trees and power lines in the Magnolia area. Estimated gusts up to 70 MPH.", "ts_dict_index": [9210, 9211, 9212]}
+{"event_id": 1064218, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-01-03 04:25:00", "end_date_time": "2023-01-03 04:25:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. A few trees and power lines were downed in Elm Grove. A barn was also displaced.", "ts_dict_index": [9237, 9238, 9239]}
+{"event_id": 1099513, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-06-08 14:51:00", "end_date_time": "2023-06-08 14:51:00", "narrative": "Mainly between 2-7 p.m. CDT on this Thursday afternoon and early evening, isolated to scattered thunderstorms drifted slowly southward across South Central Nebraska, affecting various locations mainly along and west of a line from Ord-Grand Island-Hebron. Most storms were non-severe, producing only welcomed rain, breezy winds and perhaps very small hail. However, a few storms briefly became strong to severe. Most notably, a localized downburst produced measured 76 MPH winds near Davenport in Thayer County (unofficial mesonet), with these intense speeds substantiated by a ground-truth report of some flipped irrigation pivots in the area. Other storm reports included an unofficial mesonet gust of 58 MPH near Harvard and penny size hail on the west side of Grand Island. ||This event was a classic case of diurnally-driven, pulse thunderstorm activity, firing up during peak afternoon heating and fading away as sunset approached. In the mid-upper levels, wind fields were unusually-weak by early June standards, thanks to South Central Nebraska residing under broad ridging centered north-to-south over the heart of the Central Plains. As a result, this convection was almost sparked by a combination of diurnal instability and modest convergence along a weak surface front stretched across the heart of the local area from north-northwest to south-southeast. By early-mid afternoon, the combination of temperatures climbing into the low-90s (F) and dewpoints pooling into at least the low-60s near the boundary promoted mixed-layer CAPE of 1000-2000 J/kg. Although this was sufficient instability to initiate relatively spotty convection, including a few strong to very isolated severe storms, convective intensity was significantly held in check by unseasonably weak deep-layer wind shear of at most 20 knots. A wind gust of 58 MPH was measured by a mesonet station located two miles southeast of Harvard.", "ts_dict_index": [9231, 9232, 9233]}
+{"event_id": 1064112, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-01-02 18:24:00", "end_date_time": "2023-01-02 18:24:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. A tree was blown down on Alabama-Landing Road.", "ts_dict_index": [9246, 9247, 9248]}
+{"event_id": 1064135, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-01-02 20:27:00", "end_date_time": "2023-01-02 20:27:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. A power line was down on East 4th Street in Junction City.", "ts_dict_index": [9249, 9250, 9251]}
+{"event_id": 1099515, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2023-06-08 16:19:00", "end_date_time": "2023-06-08 16:25:00", "narrative": "Mainly between 2-7 p.m. CDT on this Thursday afternoon and early evening, isolated to scattered thunderstorms drifted slowly southward across South Central Nebraska, affecting various locations mainly along and west of a line from Ord-Grand Island-Hebron. Most storms were non-severe, producing only welcomed rain, breezy winds and perhaps very small hail. However, a few storms briefly became strong to severe. Most notably, a localized downburst produced measured 76 MPH winds near Davenport in Thayer County (unofficial mesonet), with these intense speeds substantiated by a ground-truth report of some flipped irrigation pivots in the area. Other storm reports included an unofficial mesonet gust of 58 MPH near Harvard and penny size hail on the west side of Grand Island. ||This event was a classic case of diurnally-driven, pulse thunderstorm activity, firing up during peak afternoon heating and fading away as sunset approached. In the mid-upper levels, wind fields were unusually-weak by early June standards, thanks to South Central Nebraska residing under broad ridging centered north-to-south over the heart of the Central Plains. As a result, this convection was almost sparked by a combination of diurnal instability and modest convergence along a weak surface front stretched across the heart of the local area from north-northwest to south-southeast. By early-mid afternoon, the combination of temperatures climbing into the low-90s (F) and dewpoints pooling into at least the low-60s near the boundary promoted mixed-layer CAPE of 1000-2000 J/kg. Although this was sufficient instability to initiate relatively spotty convection, including a few strong to very isolated severe storms, convective intensity was significantly held in check by unseasonably weak deep-layer wind shear of at most 20 knots. Wind gusts of 76 MPH were measured by two mesonet stations in this area. There was a public report of several blown over irrigation pivots.", "ts_dict_index": [9228, 9229, 9230]}
+{"event_id": 886603, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-06-03 12:15:00", "end_date_time": "2020-06-03 12:15:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Photo of a large tree down in a residential neighborhood in Little Egg Harbor Township. Time estimated from radar.", "ts_dict_index": [9183, 9184, 9185]}
+{"event_id": 1064129, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-01-02 19:50:00", "end_date_time": "2023-01-02 19:50:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. A pergola was lifted and relocated about 50 feet from its original location.", "ts_dict_index": [9255, 9256, 9257]}
+{"event_id": 1064126, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-01-02 19:40:00", "end_date_time": "2023-01-02 19:40:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. Trees were downed along Sligo Road.", "ts_dict_index": [9258, 9259, 9260]}
+{"event_id": 884900, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:42:00", "end_date_time": "2020-04-08 00:42:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Arnold Palmer Municipal Airport had two hangars completely destroyed and one other severely damaged by thunderstorm wind.  One plane was also completely destroyed, while another suffered heavy damage.", "ts_dict_index": [9267, 9268, 9269]}
+{"event_id": 1064128, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-01-02 19:50:00", "end_date_time": "2023-01-02 19:50:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. A tree was blown down onto a power line near the Eastwood community.", "ts_dict_index": [9252, 9253, 9254]}
+{"event_id": 884953, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:14:00", "end_date_time": "2020-04-08 00:14:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Numerous trees and wires were blown down in New Kensington.", "ts_dict_index": [9264, 9265, 9266]}
+{"event_id": 884860, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:14:00", "end_date_time": "2020-04-08 00:14:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A tree fell into a home along Crawford Run Road in Frazer Township.", "ts_dict_index": [9270, 9271, 9272]}
+{"event_id": 886776, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-06-03 18:55:00", "end_date_time": "2020-06-03 18:55:00", "narrative": "A derecho developed just southeast of Lake Erie during the early morning hours of June 3, 2020, then moved rapidly southeast across Pennsylvania before exiting the central New Jersey coast during the early afternoon hours, approximately 130 PM. Damaging winds in excess of 60 MPH were sporadic over western and central Pennsylvania, but as the thunderstorm complex moved into increasingly unstable air in the eastern part of the state just before noon, wind damage reports became more numerous and widespread. Most of these reports were confined within a 50-mile wide swath extending from Berks County eastward to the Philadelphia metro area, then further east to the Ocean County shoreline in New Jersey. Wind gust reports between 60 and 70 MPH were common within this swath, with some of the highest gusts as follows: 89 MPH in Beach Haven, 87 MPH in Brick (both in Ocean County), 76 MPH in Brielle (Monmouth County), and 67 MPH in Jacksonville (Burlington County).  In addition to these destructive wind gusts, frequent to continuous cloud to ground lightning and heavy downpours were also reported throughout the area.||Over 112,000 power outages were reported in southern New Jersey as a result |of fallen trees on power lines.  Some localities were without power for several days. ||Because this derecho moved off the coast by 200 PM, the warm afternoon sun was able to sufficiently destabilize the atmosphere for the formation of another round of severe thunderstorms over some of the same areas that experience them earlier in the day. Reported wind gusts associated with these thunderstorms generally ranged between 45 and 65 MPH, with a 65 MPH wind gust measured at the Philadelphia International Airport. The remaining thunderstorms then moved offshore by 1000 PM, which brought an end to the day's severe weather. Large tree snapped from its base in Westmont.", "ts_dict_index": [9225, 9226, 9227]}
+{"event_id": 884883, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:30:00", "end_date_time": "2020-04-08 00:30:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A tree was blown down onto Mars Hill Road.", "ts_dict_index": [9297, 9298, 9299]}
+{"event_id": 884890, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:36:00", "end_date_time": "2020-04-08 00:36:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A tree was downed onto a residence.", "ts_dict_index": [9312, 9313, 9314]}
+{"event_id": 884892, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:40:00", "end_date_time": "2020-04-08 00:40:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Numerous trees were reported to be downed in Elizabeth.  One playhouse was blown over 100 yards away.", "ts_dict_index": [9285, 9286, 9287]}
+{"event_id": 884886, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:33:00", "end_date_time": "2020-04-08 00:33:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Trees were blown down onto Willowbrook Road in Rostraver Township.", "ts_dict_index": [9288, 9289, 9290]}
+{"event_id": 884897, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:40:00", "end_date_time": "2020-04-08 00:40:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. At 701 Peer Street, a roof was blown off of a garage and the garage was displaced from its foundation.", "ts_dict_index": [9279, 9280, 9281]}
+{"event_id": 884938, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:06:00", "end_date_time": "2020-04-08 00:06:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A 65 knot wind gust was recorded at Pittsburgh International Airport.", "ts_dict_index": [9294, 9295, 9296]}
+{"event_id": 884841, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:10:00", "end_date_time": "2020-04-08 00:10:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Tree and roof damage was reported near Michael Road.", "ts_dict_index": [9303, 9304, 9305]}
+{"event_id": 884940, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:29:00", "end_date_time": "2020-04-08 00:29:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A wind gust of 53 knots was measured by the ASOS at Allegheny County Airport.", "ts_dict_index": [9306, 9307, 9308]}
+{"event_id": 884838, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:08:00", "end_date_time": "2020-04-08 00:08:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Multiple trees were reported to be snapped or uprooted in the Pine Grove area.  The time of occurrence was estimated based on radar data.", "ts_dict_index": [9300, 9301, 9302]}
+{"event_id": 884888, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:34:00", "end_date_time": "2020-04-08 00:34:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A tree was blown down onto a residence in West Newton.", "ts_dict_index": [9282, 9283, 9284]}
+{"event_id": 884842, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:12:00", "end_date_time": "2020-04-08 00:12:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A tree was reported to be blown down onto a residence near Center New Texas Road.", "ts_dict_index": [9309, 9310, 9311]}
+{"event_id": 884868, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:20:00", "end_date_time": "2020-04-08 00:20:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A large tree was blown down in a yard, and power lines were also downed around the area of the border between Mount Lebanon and Castle Shannon.", "ts_dict_index": [9276, 9277, 9278]}
+{"event_id": 884857, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:13:00", "end_date_time": "2020-04-08 00:13:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A roof was blown off of a church at 221 Ridge Avenue, with the resulting damage blocking the roadway.", "ts_dict_index": [9273, 9274, 9275]}
+{"event_id": 1064216, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-01-03 04:11:00", "end_date_time": "2023-01-03 04:11:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. A large tree was uprooted across the 500 block of College street, falling across multiple  power lines and a vehicle.", "ts_dict_index": [9243, 9244, 9245]}
+{"event_id": 884941, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:33:00", "end_date_time": "2020-04-08 00:33:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A 54 knot wind gust was measured by a citizen.", "ts_dict_index": [9315, 9316, 9317]}
+{"event_id": 884956, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:14:00", "end_date_time": "2020-04-08 00:14:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. The roof was blown off of St. Mary of Czestochowa in New Kensington.", "ts_dict_index": [9318, 9319, 9320]}
+{"event_id": 1064132, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2023-01-02 20:20:00", "end_date_time": "2023-01-02 20:20:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. A tree was blown down just southeast of Heflin near the Bienville Parish line.", "ts_dict_index": [9261, 9262, 9263]}
+{"event_id": 884939, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:20:00", "end_date_time": "2020-04-08 00:20:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A PennDOT sensor at exit 60 on I-79 north measured a wind gust of 60 knots.", "ts_dict_index": [9327, 9328, 9329]}
+{"event_id": 884875, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:25:00", "end_date_time": "2020-04-08 00:25:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Near Avonmore, many trees were blown down and uprooted, along with a few flagpoles. The time of occurrence was based on radar.", "ts_dict_index": [9345, 9346, 9347]}
+{"event_id": 884874, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:25:00", "end_date_time": "2020-04-08 00:25:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Across Bell Township, numerous trees and power lines were reported to be blown down.", "ts_dict_index": [9333, 9334, 9335]}
+{"event_id": 884962, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:15:00", "end_date_time": "2020-04-08 00:15:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A member of the public reported that several trees were blown down in their yard, one of which hit their house.", "ts_dict_index": [9342, 9343, 9344]}
+{"event_id": 884836, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:06:00", "end_date_time": "2020-04-08 00:06:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A tree was reported to be downed at the intersection of Coraopolis Road and Route 51.", "ts_dict_index": [9354, 9355, 9356]}
+{"event_id": 884972, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:18:00", "end_date_time": "2020-04-08 00:18:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Trees were reported to be blown down along County Route 780.  Time of occurrence was estimated based on radar data.", "ts_dict_index": [9339, 9340, 9341]}
+{"event_id": 884833, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:03:00", "end_date_time": "2020-04-08 00:03:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Multiple trees and power lines were reported to be blown down across the area of Sewickley.", "ts_dict_index": [9351, 9352, 9353]}
+{"event_id": 884844, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:13:00", "end_date_time": "2020-04-08 00:13:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Roof damage was reported to three homes near State Route 366, with several trees blown down around the area.", "ts_dict_index": [9321, 9322, 9323]}
+{"event_id": 884905, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:46:00", "end_date_time": "2020-04-08 00:46:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A tree was reported to be blown down on to a residence.", "ts_dict_index": [9324, 9325, 9326]}
+{"event_id": 884878, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:30:00", "end_date_time": "2020-04-08 00:30:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Downed trees and penny-sized hail were reported on Edgewood Lane.", "ts_dict_index": [9330, 9331, 9332]}
+{"event_id": 884829, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:00:00", "end_date_time": "2020-04-08 00:00:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Trees were heard to be falling in the woods adjacent to the National Weather Service office.  Continuous wind gusts to 70 MPH were observed for almost 10 minutes.", "ts_dict_index": [9336, 9337, 9338]}
+{"event_id": 884840, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:09:00", "end_date_time": "2020-04-08 00:09:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Trees were reported to be blown down and roof damage occurred near Crest Street.  A trampoline was also moved a distance.  Time of occurrence based on radar data.", "ts_dict_index": [9291, 9292, 9293]}
+{"event_id": 884958, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:15:00", "end_date_time": "2020-04-08 00:15:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A large trees was blown down on to a house in Crafton.", "ts_dict_index": [9375, 9376, 9377]}
+{"event_id": 884977, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:18:00", "end_date_time": "2020-04-08 00:18:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Multiple trees and power lines were reported to be down around Northmoreland Park.", "ts_dict_index": [9381, 9382, 9383]}
+{"event_id": 884880, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:30:00", "end_date_time": "2020-04-08 00:30:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Numerous trees were reported to be blown down along Vernon Road in Rostraver Township.", "ts_dict_index": [9360, 9361, 9362]}
+{"event_id": 884916, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:50:00", "end_date_time": "2020-04-08 00:50:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. At 1005 Chaintown Road, a garage collapsed and a telephone pole was snapped.", "ts_dict_index": [9378, 9379, 9380]}
+{"event_id": 884967, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:15:00", "end_date_time": "2020-04-08 00:15:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A roof was blown off of a building on Constitution Boulevard near CTS Services.", "ts_dict_index": [9363, 9364, 9365]}
+{"event_id": 884869, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:22:00", "end_date_time": "2020-04-08 00:22:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Numerous trees and power lines were blown down across Washington Township.", "ts_dict_index": [9384, 9385, 9386]}
+{"event_id": 884873, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:25:00", "end_date_time": "2020-04-08 00:25:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Parts of a brick storefront were brought down in Clairton.", "ts_dict_index": [9357, 9358, 9359]}
+{"event_id": 884970, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:16:00", "end_date_time": "2020-04-08 00:16:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. The tops of trees were snapped off in Penn Hills.  Time of occurrence was estimated using radar.", "ts_dict_index": [9372, 9373, 9374]}
+{"event_id": 884835, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:04:00", "end_date_time": "2020-04-08 00:04:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A large tree was reported to be uprooted near Duncan Avenue.  The time of occurrence was based on radar.", "ts_dict_index": [9366, 9367, 9368]}
+{"event_id": 884963, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:15:00", "end_date_time": "2020-04-08 00:15:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A member of the public reported widespread damage to trees, fences, awnings, and other structures near Tarentum.", "ts_dict_index": [9348, 9349, 9350]}
+{"event_id": 893303, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-07-05 19:40:00", "end_date_time": "2020-07-05 19:40:00", "narrative": "A weak shortwave trough drifted south into Southeast Oklahoma and Southwest Arkansas during the early morning hours of July 5th, with large scale forcing enhancing shower and thunderstorm development as they built south into more unstable air across East Texas, extreme Southwest Arkansas, and Northwest Louisiana. A southwesterly low level flow was enough to sustain these showers and thunderstorms as they shifted southeast, with some of these storms briefly severe producing damaging winds which downed trees and power lines across these areas. Given the very moist air mass in place, these storms were also prolific rainfall producers, with widespread rainfall amounts of 2-4 inches observed. In fact, some areas of Western Harrison County recorded 4-6+ inch amounts where thunderstorms repeatedly moved over this area between 300-700 am, with a CoCoRaHS observer about 6 miles north of Hallsville recording 6.43 inches of rainfall that morning, contributing to flash flooding in this area.||While these showers and thunderstorms weakened after daybreak on the 5th, additional scattered showers and thunderstorms developed throughout the day with diurnal heating as the trough became stationary of Northeast Texas, and a second shortwave trough drifting east from Northwest across North-central Texas, triggering a cluster of storms from the DFW Metroplex which tracked southeast into East-Central Texas as it continued to tap moderate instability through the afternoon and evening. Some of these storms became severe as they entered portions of Smith and Rusk Counties, with damaging winds downing trees and power lines over these areas. These storms eventually weakened during the late evening over extreme Eastern Texas as they entered an environment with reduced instability. Trees and power lines were blown down southeast of Winona.", "ts_dict_index": [9420, 9421, 9422]}
+{"event_id": 1015853, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-04-13 12:11:00", "end_date_time": "2022-04-13 12:11:00", "narrative": "A strong storm system brought multiple rounds of severe weather that led to fairly widespread rainfall and eventually river flooding. One round of severe weather occurred on Monday, April 11th. Large, individual thunderstorms known as supercells developed along the Arkansas River valley of western Arkansas. As these storms slowly drifted east, they produced four tornadoes across Sebastian, Franklin and Logan Counties and hail as large as 4.5 in diameter across Logan County. Later in the evening, storms began to develop across central Arkansas and move generally eastward. Two storms caused the most widespread severe weather across central into eastern Arkansas during the evening hours of the 11th. The main storm of interest developed across Perry and Faulkner Counties and moved east southeastward toward Lonoke County. As this storm intensified it produced a tornado as well as 3 hail near Cabot. The other main storm developed over portions of Garland County and moved east across Saline County. Before weakening, it produced a swath of hail as large as golf balls from Hot Springs Village to Bryant. ||Ahead of a cold front that moved across the state on the 13th, additional rain and thunderstorms developed and moved across the state. Fairly widespread rain, some of which was heavy and led to flash flooding, and thunderstorms shifted east across the area on the 13th. A swath of heavy rain in excess of 2-4 inches occurred from portions of southwest to east central Arkansas as well as across northwest sections of the state. Sadly, one person died after a tree fell on a mobile home in Cleveland County on April 13th. On the same day, flash flooding claimed the life of a 70 year old woman in Carroll County when she attempted to cross a flooded low water crossing. A tree was down near the intersection of McCain Blvd. and North Hills Blvd., blocking traffic.", "ts_dict_index": [9435, 9436, 9437]}
+{"event_id": 1015851, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-04-13 12:00:00", "end_date_time": "2022-04-13 12:00:00", "narrative": "A strong storm system brought multiple rounds of severe weather that led to fairly widespread rainfall and eventually river flooding. One round of severe weather occurred on Monday, April 11th. Large, individual thunderstorms known as supercells developed along the Arkansas River valley of western Arkansas. As these storms slowly drifted east, they produced four tornadoes across Sebastian, Franklin and Logan Counties and hail as large as 4.5 in diameter across Logan County. Later in the evening, storms began to develop across central Arkansas and move generally eastward. Two storms caused the most widespread severe weather across central into eastern Arkansas during the evening hours of the 11th. The main storm of interest developed across Perry and Faulkner Counties and moved east southeastward toward Lonoke County. As this storm intensified it produced a tornado as well as 3 hail near Cabot. The other main storm developed over portions of Garland County and moved east across Saline County. Before weakening, it produced a swath of hail as large as golf balls from Hot Springs Village to Bryant. ||Ahead of a cold front that moved across the state on the 13th, additional rain and thunderstorms developed and moved across the state. Fairly widespread rain, some of which was heavy and led to flash flooding, and thunderstorms shifted east across the area on the 13th. A swath of heavy rain in excess of 2-4 inches occurred from portions of southwest to east central Arkansas as well as across northwest sections of the state. Sadly, one person died after a tree fell on a mobile home in Cleveland County on April 13th. On the same day, flash flooding claimed the life of a 70 year old woman in Carroll County when she attempted to cross a flooded low water crossing. Trees and power lines were reported down in Park Hill and North Hills.", "ts_dict_index": [9438, 9439, 9440]}
+{"event_id": 1015735, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-04-11 19:20:00", "end_date_time": "2022-04-11 19:20:00", "narrative": "A strong storm system brought multiple rounds of severe weather that led to fairly widespread rainfall and eventually river flooding. One round of severe weather occurred on Monday, April 11th. Large, individual thunderstorms known as supercells developed along the Arkansas River valley of western Arkansas. As these storms slowly drifted east, they produced four tornadoes across Sebastian, Franklin and Logan Counties and hail as large as 4.5 in diameter across Logan County. Later in the evening, storms began to develop across central Arkansas and move generally eastward. Two storms caused the most widespread severe weather across central into eastern Arkansas during the evening hours of the 11th. The main storm of interest developed across Perry and Faulkner Counties and moved east southeastward toward Lonoke County. As this storm intensified it produced a tornado as well as 3 hail near Cabot. The other main storm developed over portions of Garland County and moved east across Saline County. Before weakening, it produced a swath of hail as large as golf balls from Hot Springs Village to Bryant. ||Ahead of a cold front that moved across the state on the 13th, additional rain and thunderstorms developed and moved across the state. Fairly widespread rain, some of which was heavy and led to flash flooding, and thunderstorms shifted east across the area on the 13th. A swath of heavy rain in excess of 2-4 inches occurred from portions of southwest to east central Arkansas as well as across northwest sections of the state. Sadly, one person died after a tree fell on a mobile home in Cleveland County on April 13th. On the same day, flash flooding claimed the life of a 70 year old woman in Carroll County when she attempted to cross a flooded low water crossing. A tree was downed near Batesville Pike and Watson Rd.", "ts_dict_index": [9432, 9433, 9434]}
+{"event_id": 1015858, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-04-13 12:30:00", "end_date_time": "2022-04-13 12:30:00", "narrative": "A strong storm system brought multiple rounds of severe weather that led to fairly widespread rainfall and eventually river flooding. One round of severe weather occurred on Monday, April 11th. Large, individual thunderstorms known as supercells developed along the Arkansas River valley of western Arkansas. As these storms slowly drifted east, they produced four tornadoes across Sebastian, Franklin and Logan Counties and hail as large as 4.5 in diameter across Logan County. Later in the evening, storms began to develop across central Arkansas and move generally eastward. Two storms caused the most widespread severe weather across central into eastern Arkansas during the evening hours of the 11th. The main storm of interest developed across Perry and Faulkner Counties and moved east southeastward toward Lonoke County. As this storm intensified it produced a tornado as well as 3 hail near Cabot. The other main storm developed over portions of Garland County and moved east across Saline County. Before weakening, it produced a swath of hail as large as golf balls from Hot Springs Village to Bryant. ||Ahead of a cold front that moved across the state on the 13th, additional rain and thunderstorms developed and moved across the state. Fairly widespread rain, some of which was heavy and led to flash flooding, and thunderstorms shifted east across the area on the 13th. A swath of heavy rain in excess of 2-4 inches occurred from portions of southwest to east central Arkansas as well as across northwest sections of the state. Sadly, one person died after a tree fell on a mobile home in Cleveland County on April 13th. On the same day, flash flooding claimed the life of a 70 year old woman in Carroll County when she attempted to cross a flooded low water crossing. Tree limbs were snapped and trees were uprooted on C Street in the Hillcrest part of Little Rock.", "ts_dict_index": [9429, 9430, 9431]}
+{"event_id": 893327, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-07-05 20:17:00", "end_date_time": "2020-07-05 20:17:00", "narrative": "A weak shortwave trough drifted south into Southeast Oklahoma and Southwest Arkansas during the early morning hours of July 5th, with large scale forcing enhancing shower and thunderstorm development as they built south into more unstable air across East Texas, extreme Southwest Arkansas, and Northwest Louisiana. A southwesterly low level flow was enough to sustain these showers and thunderstorms as they shifted southeast, with some of these storms briefly severe producing damaging winds which downed trees and power lines across these areas. Given the very moist air mass in place, these storms were also prolific rainfall producers, with widespread rainfall amounts of 2-4 inches observed. In fact, some areas of Western Harrison County recorded 4-6+ inch amounts where thunderstorms repeatedly moved over this area between 300-700 am, with a CoCoRaHS observer about 6 miles north of Hallsville recording 6.43 inches of rainfall that morning, contributing to flash flooding in this area.||While these showers and thunderstorms weakened after daybreak on the 5th, additional scattered showers and thunderstorms developed throughout the day with diurnal heating as the trough became stationary of Northeast Texas, and a second shortwave trough drifting east from Northwest across North-central Texas, triggering a cluster of storms from the DFW Metroplex which tracked southeast into East-Central Texas as it continued to tap moderate instability through the afternoon and evening. Some of these storms became severe as they entered portions of Smith and Rusk Counties, with damaging winds downing trees and power lines over these areas. These storms eventually weakened during the late evening over extreme Eastern Texas as they entered an environment with reduced instability. Trees and power lines were blown down on Highway 42 between Highway 323 and Highway 64.", "ts_dict_index": [9423, 9424, 9425]}
+{"event_id": 1061096, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 13:45:00", "end_date_time": "2022-10-15 13:45:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A Trained Spotter sent pictures of a couple of trees, with branches snapped, along with a large uprooted tree that fell onto an SUV causing some damage to the vehicle near the Love Truck Stop Station located just south of I-10 in Tolleson. TPHX terminal doppler radar measured over 70 mph in the area. No injuries were reported.", "ts_dict_index": [9399, 9400, 9401]}
+{"event_id": 1061341, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 18:55:00", "end_date_time": "2022-10-15 18:55:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. Power pole blown over due to thunderstorm winds in the area of Wintersburg Road and Latham Street near Tonopah. Winds were estimated at around 70 mph. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [9405, 9406, 9407]}
+{"event_id": 1061094, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 17:39:00", "end_date_time": "2022-10-15 17:39:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. Downed power poles, 18 approximately, affected 52 customers in an area between S Higley Road and S Mandarin Drive and between E San Tan Blvd and W San Dance Drive. Winds were estimated at around 70 mph based on radar data. No injuries were reported.", "ts_dict_index": [9417, 9418, 9419]}
+{"event_id": 1061146, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 18:05:00", "end_date_time": "2022-10-15 18:05:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. Downed power poles in Tonapah affecting 96 customers were reported in an area between 425th Drive to 411th Ave and between Glendale Avenue and I-10. Winds were estimated at around 70 mph. No injuries were reported.", "ts_dict_index": [9396, 9397, 9398]}
+{"event_id": 893296, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-07-05 02:50:00", "end_date_time": "2020-07-05 02:50:00", "narrative": "A weak shortwave trough drifted south into Southeast Oklahoma and Southwest Arkansas during the early morning hours of July 5th, with large scale forcing enhancing shower and thunderstorm development as they built south into more unstable air across East Texas, extreme Southwest Arkansas, and Northwest Louisiana. A southwesterly low level flow was enough to sustain these showers and thunderstorms as they shifted southeast, with some of these storms briefly severe producing damaging winds which downed trees and power lines across these areas. Given the very moist air mass in place, these storms were also prolific rainfall producers, with widespread rainfall amounts of 2-4 inches observed. In fact, some areas of Western Harrison County recorded 4-6+ inch amounts where thunderstorms repeatedly moved over this area between 300-700 am, with a CoCoRaHS observer about 6 miles north of Hallsville recording 6.43 inches of rainfall that morning, contributing to flash flooding in this area.||While these showers and thunderstorms weakened after daybreak on the 5th, additional scattered showers and thunderstorms developed throughout the day with diurnal heating as the trough became stationary of Northeast Texas, and a second shortwave trough drifting east from Northwest across North-central Texas, triggering a cluster of storms from the DFW Metroplex which tracked southeast into East-Central Texas as it continued to tap moderate instability through the afternoon and evening. Some of these storms became severe as they entered portions of Smith and Rusk Counties, with damaging winds downing trees and power lines over these areas. These storms eventually weakened during the late evening over extreme Eastern Texas as they entered an environment with reduced instability. Several trees were blown down near Hallsville.", "ts_dict_index": [9426, 9427, 9428]}
+{"event_id": 1061366, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 19:07:00", "end_date_time": "2022-10-15 19:07:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A trained spotter in Tonopah measured a 68 mph gust using a handheld anemometer. Spotter also reported pea-sized hail. There was wind damage to roof of nearby shed. 20-30 feet of roof beams and tin sheets were laying in the driveway as well as awning damage on a bus. No injuries were reported.", "ts_dict_index": [9390, 9391, 9392]}
+{"event_id": 1061145, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 17:40:00", "end_date_time": "2022-10-15 17:40:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. Downed powerlines affecting 252 customers were reported in an area between the Hassayampa River to Elliot Road to 355th Avenue to Wintersburg Road in Wintersburg. Winds were estimated at around 70 mph. No injuries were reported.", "ts_dict_index": [9393, 9394, 9395]}
+{"event_id": 1061148, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 19:03:00", "end_date_time": "2022-10-15 19:03:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. Severe wind damage occurred from a thunderstorm microburst in the Tonopah area from the second of two storms that passed through the area. Some of the damages included: two mobile homes destroyed; damage to some of the structures at the Belmont Dairy Farm (specifically a milking barn), which had some damage to some of the cow enclosures as well; 3 destroyed AC unit condensers; creosote bushes being fully defoliated in a field; and several large downed trees. Downed power poles affecting 121 customers were reported by the utility company in an area between 379th Avenue and 355th Avenue and between Missouri Avenue and I-10. There was also loss of livestock (unknown how many or type). Winds were estimated at around 80 mph. Timing estimated from radar.", "ts_dict_index": [9402, 9403, 9404]}
+{"event_id": 1061095, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 13:08:00", "end_date_time": "2022-10-15 13:08:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. A trained spotter recorded a 64mph wind gust with a handheld anemometer in the area of East Baseline Road and South Rural Road in Tempe. No damages or injuries were reported.", "ts_dict_index": [9408, 9409, 9410]}
+{"event_id": 1015857, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-04-13 12:58:00", "end_date_time": "2022-04-13 12:58:00", "narrative": "A strong storm system brought multiple rounds of severe weather that led to fairly widespread rainfall and eventually river flooding. One round of severe weather occurred on Monday, April 11th. Large, individual thunderstorms known as supercells developed along the Arkansas River valley of western Arkansas. As these storms slowly drifted east, they produced four tornadoes across Sebastian, Franklin and Logan Counties and hail as large as 4.5 in diameter across Logan County. Later in the evening, storms began to develop across central Arkansas and move generally eastward. Two storms caused the most widespread severe weather across central into eastern Arkansas during the evening hours of the 11th. The main storm of interest developed across Perry and Faulkner Counties and moved east southeastward toward Lonoke County. As this storm intensified it produced a tornado as well as 3 hail near Cabot. The other main storm developed over portions of Garland County and moved east across Saline County. Before weakening, it produced a swath of hail as large as golf balls from Hot Springs Village to Bryant. ||Ahead of a cold front that moved across the state on the 13th, additional rain and thunderstorms developed and moved across the state. Fairly widespread rain, some of which was heavy and led to flash flooding, and thunderstorms shifted east across the area on the 13th. A swath of heavy rain in excess of 2-4 inches occurred from portions of southwest to east central Arkansas as well as across northwest sections of the state. Sadly, one person died after a tree fell on a mobile home in Cleveland County on April 13th. On the same day, flash flooding claimed the life of a 70 year old woman in Carroll County when she attempted to cross a flooded low water crossing. Trees were down on Elm St. in the Hillcrest area of Little Rock.", "ts_dict_index": [9441, 9442, 9443]}
+{"event_id": 884837, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-04-08 00:06:00", "end_date_time": "2020-04-08 00:06:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. Numerous trees were reported to be blown down at Shannopin Country Club.", "ts_dict_index": [9369, 9370, 9371]}
+{"event_id": 880555, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-24 20:30:00", "end_date_time": "2020-04-24 20:30:00", "narrative": "A southerly return flow commenced throughout the day on April 24th, in wake of a cold frontal passage that had occurred a couple of days prior on the 22nd. However, low level moisture return was meager, but a sharply amplifying upper level trough over the Central Plains and Midwest region dug south into the Red River Valley of Southern Oklahoma and North Texas during the afternoon. Strong large scale forcing occurred ahead of this trough over Eastern and Southern Oklahoma into Northeast Texas, along and ahead of a reinforcing cold front that shifted southeast over these areas. Strong wind shear also developed ahead of the trough during the afternoon and evening, with very steep lapse rates noted beneath the trough over the Red River Valley into Northeast Texas. This contributed to the development of scattered severe thunderstorms during the afternoon over portions of Southern and Southeast Oklahoma and Northeast Texas, with several supercell thunderstorms developing and tracking southeast over these areas through the evening, and eventually into Northern Louisiana during the mid and late evening hours. Multiple cell mergers contributed to an extremely severe supercell with a large swath of destructive straight line winds in excess of 80-90 mph developing over Southern Morris and much of Cass Counties, which accelerated southeast into portions of Northwest Louisiana by mid-evening. This resulted in numerous reports of very large hail up to the size of softballs across much of Benton and North Bossier City, with this hailstorm spreading east southeast while gradually weakening through the late evening hours. Reports of isolated wind damage was also received before the storms weakened by midnight with the cold frontal passage. A large tree fell onto a mobile home off of Highway 1 just north of Oil City.", "ts_dict_index": [9450, 9451, 9452]}
+{"event_id": 914802, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 15:02:00", "end_date_time": "2020-08-10 15:02:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A 45 foot tall Pine tree was blown down in Chicago Heights.", "ts_dict_index": [9453, 9454, 9455]}
+{"event_id": 1015738, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-04-11 19:30:00", "end_date_time": "2022-04-11 19:30:00", "narrative": "A strong storm system brought multiple rounds of severe weather that led to fairly widespread rainfall and eventually river flooding. One round of severe weather occurred on Monday, April 11th. Large, individual thunderstorms known as supercells developed along the Arkansas River valley of western Arkansas. As these storms slowly drifted east, they produced four tornadoes across Sebastian, Franklin and Logan Counties and hail as large as 4.5 in diameter across Logan County. Later in the evening, storms began to develop across central Arkansas and move generally eastward. Two storms caused the most widespread severe weather across central into eastern Arkansas during the evening hours of the 11th. The main storm of interest developed across Perry and Faulkner Counties and moved east southeastward toward Lonoke County. As this storm intensified it produced a tornado as well as 3 hail near Cabot. The other main storm developed over portions of Garland County and moved east across Saline County. Before weakening, it produced a swath of hail as large as golf balls from Hot Springs Village to Bryant. ||Ahead of a cold front that moved across the state on the 13th, additional rain and thunderstorms developed and moved across the state. Fairly widespread rain, some of which was heavy and led to flash flooding, and thunderstorms shifted east across the area on the 13th. A swath of heavy rain in excess of 2-4 inches occurred from portions of southwest to east central Arkansas as well as across northwest sections of the state. Sadly, one person died after a tree fell on a mobile home in Cleveland County on April 13th. On the same day, flash flooding claimed the life of a 70 year old woman in Carroll County when she attempted to cross a flooded low water crossing. Several trees were blown down and windows were blown out.", "ts_dict_index": [9447, 9448, 9449]}
+{"event_id": 1015848, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-04-13 11:50:00", "end_date_time": "2022-04-13 11:50:00", "narrative": "A strong storm system brought multiple rounds of severe weather that led to fairly widespread rainfall and eventually river flooding. One round of severe weather occurred on Monday, April 11th. Large, individual thunderstorms known as supercells developed along the Arkansas River valley of western Arkansas. As these storms slowly drifted east, they produced four tornadoes across Sebastian, Franklin and Logan Counties and hail as large as 4.5 in diameter across Logan County. Later in the evening, storms began to develop across central Arkansas and move generally eastward. Two storms caused the most widespread severe weather across central into eastern Arkansas during the evening hours of the 11th. The main storm of interest developed across Perry and Faulkner Counties and moved east southeastward toward Lonoke County. As this storm intensified it produced a tornado as well as 3 hail near Cabot. The other main storm developed over portions of Garland County and moved east across Saline County. Before weakening, it produced a swath of hail as large as golf balls from Hot Springs Village to Bryant. ||Ahead of a cold front that moved across the state on the 13th, additional rain and thunderstorms developed and moved across the state. Fairly widespread rain, some of which was heavy and led to flash flooding, and thunderstorms shifted east across the area on the 13th. A swath of heavy rain in excess of 2-4 inches occurred from portions of southwest to east central Arkansas as well as across northwest sections of the state. Sadly, one person died after a tree fell on a mobile home in Cleveland County on April 13th. On the same day, flash flooding claimed the life of a 70 year old woman in Carroll County when she attempted to cross a flooded low water crossing. A report was received of trees down near the Little Rock Zoo.", "ts_dict_index": [9444, 9445, 9446]}
+{"event_id": 884907, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-04-08 00:48:00", "end_date_time": "2020-04-08 00:48:00", "narrative": "Broad ridging was in place across the Mississippi Valley on the morning of the 7th, with the Upper Ohio Valley region experiencing WNW flow aloft.  After morning showers and thunderstorms moved across the area due to a warm front, the upper level flow regime brought an elevated mixed layer (EML) into the region during the afternoon, capping convection during the afternoon and early evening hours. ||Convective clusters over Michigan during the evening congealed into a mesoscale convective system (MCS) and raced across Lake Erie, arriving in the NWS Pittsburgh forecast area shortly before midnight.  Steep mid-level lapse rates thanks to the EML allow for a few large hail reports initially.  However, the main impact of the system would be from wind.  Surface temperatures surged into the low to mid 60s ahead of the line on gusty southwest winds, resulting in surface CAPE of 1000 J/kg and a significant curving/lengthening of the hodograph. With the boundary layer no longer decoupled, strong ambient mid-level flow combined with highly efficient evaporational cooling in the convective downdrafts allowed substantial downdraft CAPE to be realized with surface wind gusts exceeding 70 mph observed and evident over a wide area given the volume of wind damage reports.  Embedded vortices in the quasi-linear convective system also led to five tornadoes in the EF0/EF1 range during this event across the region.||Numerous instances of tree and structural damage were observed, including damage to planes and hangars at Arnold Palmer Regional Airport.  Strong winds also tore off part of the roof of St. Mary of Czestochowa Church on Kenneth Avenue in New Kensington. Over 50,000 area electrical customers were without power in the wake of the storms, according to the Pittsburgh Post-Gazette. A tree was reported to be blown down on a residence along Wonderwood Lane.", "ts_dict_index": [9387, 9388, 9389]}
+{"event_id": 913106, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 15:08:00", "end_date_time": "2020-08-10 15:08:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Wind gusts were estimated to 60 mph in Thornton.", "ts_dict_index": [9477, 9478, 9479]}
+{"event_id": 918267, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:51:00", "end_date_time": "2020-08-10 14:53:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Trees, tree limbs and power lines were blown down in River Grove and Elmwood Park.  Several cars and houses were damaged by fallen trees.  Several roads were blocked by the fallen trees.", "ts_dict_index": [9462, 9463, 9464]}
+{"event_id": 914782, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:57:00", "end_date_time": "2020-08-10 14:57:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Three utility poles were leaning near Suak Trail and Governor's Highway.", "ts_dict_index": [9468, 9469, 9470]}
+{"event_id": 918112, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:57:00", "end_date_time": "2020-08-10 14:58:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. About 50 trees were knocked down or damaged along Logan Boulevard in the Logan Square neighborhood in Chicago.  Tree limbs and power lines were also blown down.", "ts_dict_index": [9480, 9481, 9482]}
+{"event_id": 918107, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:52:00", "end_date_time": "2020-08-10 14:52:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A garage collapsed near Roscoe Street and Nordica Avenue.", "ts_dict_index": [9459, 9460, 9461]}
+{"event_id": 915489, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 15:00:00", "end_date_time": "2020-08-10 15:10:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A corridor of significant straight line wind damage occurred from Harvey east to Calumet City.  Numerous trees were uprooted and snapped along this corridor.  Some roofs were damaged by falling trees; other roofs suffered minor shingle damage from the strong winds.  Some of the worst damage was in Harvey in an area between Sibley Boulevard to the north and 159th Street to the south.  Trees were snapped and uprooted and extensive damage occurred to utility poles and power lines, resulting in some portions of the power grid needing to be completely rebuilt.  Almost everyone in Harvey lost power.  An estimated 300 to 350 trees were blown down in Harvey.  Almost every road in Harvey was blocked by some amount of tree damage.  Significant tree damage was reported in forest preserve areas including in the Shabonna Woods Forest Preserve.  Damage was consistent with wind speeds up to 90 mph.||One day later, on August 11th, just after noon, a 59 year old man was walking in the 15000 block of Merrill Avenue in unincorporated Thornton Township near Calumet City.  He stepped on a downed power line that was live and collapsed in a grassy area where he died.", "ts_dict_index": [9465, 9466, 9467]}
+{"event_id": 914700, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:51:00", "end_date_time": "2020-08-10 14:52:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Tree damage occurred in Brookfield with the worst of the damage north of the railroad tracks.  A corridor of widespread damage occurred along Grant Avenue where large tree limbs were blocking streets and sidewalks.  A few larger tree limbs fell onto parked cars.  A tree was split down the middle near Cleveland Avenue with part of the tree landing on the roof of a brick bungalow.", "ts_dict_index": [9474, 9475, 9476]}
+{"event_id": 1061147, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-10-15 18:49:00", "end_date_time": "2022-10-15 18:49:00", "narrative": "A slow moving low pressure system brought several rounds of showers and thunderstorms across portions of south-central and southwestern Arizona throughout the day on the 15th. Strong southerly flow out ahead of the low pressure system brought in highly anomalous moisture content across the southern half of Arizona, with PWATs surging to 1.1-1.4, which are near record values for mid-October.  Along with the highly anomalous moisture values, moderate to high instability values were also present with MLCAPE rising to 1000-1500 J/KG. Bulk shear values between 25-35 kts were also present. The combination of the highly anomalous moisture content, instability, and shear along with the strong dynamic forcing to the east and north of the low pressure system was a recipe for these showers and thunderstorms to produce flash flooding as well as severe wind gusts and hail. The greatest flash flood impact occurred along portions of western Maricopa County in the area from Buckeye to Tonopah, The greatest damaging wind impact occurred in the Tonopah area, where two rounds of severe thunderstorms, one hour apart, impacted causing widespread power outages due to downed power poles, destroyed two mobile homes, damaged dairy farm structures, and resulted livestock losses. Severe hail was also reported with a storm that moved into the Mesa to Scottsdale area during the overnight period. ||As the area of low pressure moved eastward on the 16th, lingering moisture resulted in the development of more showers and thunderstorms, mainly concentrated across the higher terrain areas east of Phoenix. One isolated storm in particular developed on a open field near Sun Lakes, resulting in the development of a short-lived landspout during the mid-afternoon hours with no damages reported. Downed power poles in Wintersburg affecting 41 customers were reported Between Buchanan Street to Yuma Road and between Powers Butte Road to Johnson Road. Winds were estimated at around 70 mph. No injuries were reported.", "ts_dict_index": [9411, 9412, 9413]}
+{"event_id": 914801, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:55:00", "end_date_time": "2020-08-10 14:55:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A wind gust to 65 mph was measured in Burbank.", "ts_dict_index": [9483, 9484, 9485]}
+{"event_id": 918110, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 15:00:00", "end_date_time": "2020-08-10 15:00:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Roofing material was peeled off a roof just north of Waveland Avenue and just west of Lake Shore Drive with debris blown across Lake Shore Drive.", "ts_dict_index": [9495, 9496, 9497]}
+{"event_id": 915834, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:53:00", "end_date_time": "2020-08-10 14:53:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A tree was blown down blocking a road in Forest Park.", "ts_dict_index": [9498, 9499, 9500]}
+{"event_id": 918109, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:52:00", "end_date_time": "2020-08-10 14:53:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Numerous tree limbs were blown down in Oak Park.  More than a dozen streets were blocked by the fallen tree limbs.", "ts_dict_index": [9501, 9502, 9503]}
+{"event_id": 918263, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 15:02:00", "end_date_time": "2020-08-10 15:02:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Wind gusts to 80 mph were measured at the Montrose Harbor Light.", "ts_dict_index": [9513, 9514, 9515]}
+{"event_id": 914698, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:50:00", "end_date_time": "2020-08-10 14:50:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A narrow corridor of wind damage occurred along 23rd Street in North Riverside.  One large tree fell between two houses near 10th Avenue causing some damage to aluminum siding.  Another large tree near 2nd Avenue was completely uprooted, narrowly missing a house.", "ts_dict_index": [9492, 9493, 9494]}
+{"event_id": 918111, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 15:00:00", "end_date_time": "2020-08-10 15:00:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A tree was blown down blocking the exit from Lake Shore Drive to Wilson Drive.", "ts_dict_index": [9486, 9487, 9488]}
+{"event_id": 914820, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:48:00", "end_date_time": "2020-08-10 14:49:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Tree limbs and power lines were blown down in Westchester.  At least one tree was struck by lightning.", "ts_dict_index": [9504, 9505, 9506]}
+{"event_id": 913107, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:55:00", "end_date_time": "2020-08-10 14:55:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Tree damage was reported in Cicero.", "ts_dict_index": [9507, 9508, 9509]}
+{"event_id": 914783, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 15:00:00", "end_date_time": "2020-08-10 15:00:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A private weather station measured a wind gust to 72 mph on Fir Street.", "ts_dict_index": [9510, 9511, 9512]}
+{"event_id": 918813, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:58:00", "end_date_time": "2020-08-10 14:58:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A large tree was snapped blocking Eastwood Avenue.  Other large tree limbs were blown down nearby.", "ts_dict_index": [9456, 9457, 9458]}
+{"event_id": 917003, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:57:00", "end_date_time": "2020-08-10 14:58:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A corridor of significant wind damage occurred in Chicago, starting immediately east of Interstate 90/94 near Berteau and Kildare Avenues and continued northeast to near Montrose and Lawndale Avenues.  Significant tree damage occurred in this corridor with many trees snapped or uprooted.  Roof damage occurred to a few apartment buildings along Kedvale Avenue, just south of Cullom Avenue.  One building suffered damage to a brick wall.  Damage occurred to the top of a brick business at the southeast corner of Pulaski Road and Elston Avenue.  Vehicles were damaged by the falling bricks.  Several roofs sustained damage northeast of Elston Avenue, just south of Montrose Avenue and a window was blown out of a house.  Two utility poles were damaged near Avers Avenue.  Three buildings along Montrose Avenue suffered significant roof damage just east of Hamlin Avenue.  Two buildings had west and south facing windows blown out near Montrose Avenue and Lawndale Avenue.  The damage in this corridor indicates peak winds of 95 mph.", "ts_dict_index": [9519, 9520, 9521]}
+{"event_id": 919998, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:50:00", "end_date_time": "2020-08-10 15:05:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Widespread tree damage occurred across Chicago.  At least 11,000 trees were blown down.  Many more trees were damaged.  Dozens of vehicles were damaged by falling trees and tree limbs, some vehicles were crushed.  Numerous roads were blocked by the fallen trees.  Hundreds of power lines were blown down, some started small fires.", "ts_dict_index": [9528, 9529, 9530]}
+{"event_id": 912924, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:55:00", "end_date_time": "2020-08-10 14:55:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A wind gust to 72 mph was measured at Midway Airport.", "ts_dict_index": [9522, 9523, 9524]}
+{"event_id": 913268, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:39:00", "end_date_time": "2020-08-10 14:39:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Wind gusts were estimated between 60 mph and 70 mph in Schaumburg.", "ts_dict_index": [9525, 9526, 9527]}
+{"event_id": 915256, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 15:00:00", "end_date_time": "2020-08-10 15:01:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Trees, tree limbs and power lines were blown down in Park Forest.  Multiple vehicles were damaged by fallen trees.  Several homes had roof or siding damage.  Part of a brick wall collapsed off a house.  Widespread tree damage occurred in forest preserve areas near Park Forest.", "ts_dict_index": [9516, 9517, 9518]}
+{"event_id": 915894, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:55:00", "end_date_time": "2020-08-10 14:55:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Extensive damage occurred to several Maple trees near the First Baptist Church along 179th Street in Tinley Park.  Several shingles were blown off the roof of the church.  Some of the shingles were found more than two blocks away.", "ts_dict_index": [9531, 9532, 9533]}
+{"event_id": 914800, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:59:00", "end_date_time": "2020-08-10 15:01:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Sporadic straight line wind damage occurred across South Chicago Heights and continued east to State Street.", "ts_dict_index": [9471, 9472, 9473]}
+{"event_id": 914832, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:56:00", "end_date_time": "2020-08-10 14:56:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A large sign for an auto dealer was blown down from south to north onto a car parked on Irving Park Road.", "ts_dict_index": [9534, 9535, 9536]}
+{"event_id": 917004, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:57:00", "end_date_time": "2020-08-10 14:57:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A wind gust to 85 mph was measured.", "ts_dict_index": [9543, 9544, 9545]}
+{"event_id": 914821, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:50:00", "end_date_time": "2020-08-10 14:51:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Tree limbs and power lines were blown down in Orland Park.  A fence was damaged in the Catalina subdivision.", "ts_dict_index": [9552, 9553, 9554]}
+{"event_id": 915253, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:58:00", "end_date_time": "2020-08-10 14:59:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Tree limbs and power lines were blown down in Flossmoor.", "ts_dict_index": [9537, 9538, 9539]}
+{"event_id": 914823, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:52:00", "end_date_time": "2020-08-10 14:53:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Multiple trees were damaged in River Forest.  A couple of tree limbs fell onto vehicles.", "ts_dict_index": [9540, 9541, 9542]}
+{"event_id": 914359, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:50:00", "end_date_time": "2020-08-10 14:50:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A light pole was blown down along southbound River Road near Interstate 190.", "ts_dict_index": [9546, 9547, 9548]}
+{"event_id": 914728, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:57:00", "end_date_time": "2020-08-10 14:57:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A large tree was uprooted in Oak Lawn.", "ts_dict_index": [9549, 9550, 9551]}
+{"event_id": 913105, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:49:00", "end_date_time": "2020-08-10 14:49:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A wind gust was measured to 62 mph at Chicago O'Hare Airport.", "ts_dict_index": [9489, 9490, 9491]}
+{"event_id": 917372, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:51:00", "end_date_time": "2020-08-10 14:52:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Scattered tree limbs were blown down across Riverside.", "ts_dict_index": [9558, 9559, 9560]}
+{"event_id": 881112, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-29 23:51:00", "end_date_time": "2020-04-29 23:51:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Trees and power lines were downed just southwest of Lindale.", "ts_dict_index": [9576, 9577, 9578]}
+{"event_id": 914779, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:36:00", "end_date_time": "2020-08-10 14:36:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. A B-Class truck with a trailer was blown over at Irving Park Road and Schaumburg Road.", "ts_dict_index": [9561, 9562, 9563]}
+{"event_id": 881090, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-29 00:01:00", "end_date_time": "2020-04-29 00:01:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A 59 mph wind gust was measured at Tyler Pounds Field Airport.", "ts_dict_index": [9597, 9598, 9599]}
+{"event_id": 917005, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 14:59:00", "end_date_time": "2020-08-10 14:59:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Large tree limbs fell onto a small car near Catalpa Avenue and Spaulding Avenue, trapping the occupants in the car.  Firefighters had to cut the tree limbs away before the people could exit the car.  No injuries were reported.", "ts_dict_index": [9564, 9565, 9566]}
+{"event_id": 1032809, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2022-06-12 06:10:00", "end_date_time": "2022-06-12 06:10:00", "narrative": "Scattered strong to isolated severe thunderstorms rumbled across central and eastern portions of South Central Nebraska on this Sunday morning, prompting a few reports of hail up to ping pong ball size and wind gusts up to 65 MPH. Marginally-severe storms started off in Buffalo County, where hail reached nickel to quarter size. Farther southeast over portions of Fillmore and Thayer counties, both wind gusts and hail size increased. A swath with several wind gusts ranging from 45-55 MPH started in far southeast Clay County and continued along and just south of the Fillmore/Thayer County line. The peak measured wind gusts included 65 MPH three miles south of Ohiowa and 59 MPH just north of Alexandria. Hail up to the size of ping pong balls was reported in Carleton. The strongest storms cleared the coverage are to the east by around 8 AM CDT.||Fairly zonal mid-upper flow was in place across the Plains during the early morning. An embedded subtle mid-level shortwave disturbance made its way through the region, helping spark off elevated thunderstorm activity which moved into northwest portions the coverage area right around 4 AM CDT. Aided by increased low-mid level frontogenetical forcing and warm air advection, storms spread in coverage as they shifted southeast. The brunt of activity remained focused along and north of a line running roughly from Kearney-Hebron, which corresponded to areas where mid-level capping was a bit weaker (700mb temperatures less than 14C). Deep layer shear values were around 40 knots, while an axis of MUCAPE exceeding 2000 J/kg was in place across the area. As storms moved southeast, instability values increased, a trend reflected in their strength. A wind gust of 65 MPH was measured by a mesonet station located three miles south of Ohiowa.", "ts_dict_index": [9570, 9571, 9572]}
+{"event_id": 881115, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-29 00:45:00", "end_date_time": "2020-04-29 00:45:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A large tree was blown down across FM 2867 near the Pine Hill community.", "ts_dict_index": [9579, 9580, 9581]}
+{"event_id": 881108, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-29 00:29:00", "end_date_time": "2020-04-29 00:29:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Power lines were downed on Pinkston Drive in New London.", "ts_dict_index": [9585, 9586, 9587]}
+{"event_id": 881125, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-29 00:17:00", "end_date_time": "2020-04-29 00:17:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A pine tree was blown down across FM 3053 near County Road 1110.", "ts_dict_index": [9588, 9589, 9590]}
+{"event_id": 881124, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2020-04-29 00:25:00", "end_date_time": "2020-04-29 00:25:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A tree was blown down across Highway 79.", "ts_dict_index": [9594, 9595, 9596]}
+{"event_id": 881088, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-04-28 23:57:00", "end_date_time": "2020-04-28 23:57:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Trees were downed on FM 968 at Lancing Switch Road.", "ts_dict_index": [9582, 9583, 9584]}
+{"event_id": 881116, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-29 00:45:00", "end_date_time": "2020-04-29 00:45:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A tree fell on a home on FM 1798 east of Highway 259 near the Minden community.", "ts_dict_index": [9591, 9592, 9593]}
+{"event_id": 1032810, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2022-06-12 06:15:00", "end_date_time": "2022-06-12 06:15:00", "narrative": "Scattered strong to isolated severe thunderstorms rumbled across central and eastern portions of South Central Nebraska on this Sunday morning, prompting a few reports of hail up to ping pong ball size and wind gusts up to 65 MPH. Marginally-severe storms started off in Buffalo County, where hail reached nickel to quarter size. Farther southeast over portions of Fillmore and Thayer counties, both wind gusts and hail size increased. A swath with several wind gusts ranging from 45-55 MPH started in far southeast Clay County and continued along and just south of the Fillmore/Thayer County line. The peak measured wind gusts included 65 MPH three miles south of Ohiowa and 59 MPH just north of Alexandria. Hail up to the size of ping pong balls was reported in Carleton. The strongest storms cleared the coverage are to the east by around 8 AM CDT.||Fairly zonal mid-upper flow was in place across the Plains during the early morning. An embedded subtle mid-level shortwave disturbance made its way through the region, helping spark off elevated thunderstorm activity which moved into northwest portions the coverage area right around 4 AM CDT. Aided by increased low-mid level frontogenetical forcing and warm air advection, storms spread in coverage as they shifted southeast. The brunt of activity remained focused along and north of a line running roughly from Kearney-Hebron, which corresponded to areas where mid-level capping was a bit weaker (700mb temperatures less than 14C). Deep layer shear values were around 40 knots, while an axis of MUCAPE exceeding 2000 J/kg was in place across the area. As storms moved southeast, instability values increased, a trend reflected in their strength. A wind gust of 59 MPH was measured by a mesonet station located seven miles north of Alexandria.", "ts_dict_index": [9567, 9568, 9569]}
+{"event_id": 913269, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2020-08-10 15:02:00", "end_date_time": "2020-08-10 15:04:00", "narrative": "During the late morning through the afternoon of Monday August 10th, a line of intense thunderstorms known as a derecho brought widespread severe wind damage across Iowa, northern Illinois and northern Indiana.||In north central and northeast Illinois alone, the severe winds of 60 to 100 mph downed or damaged tens of thousands of trees, as well as caused severe damage to homes, businesses, and infrastructure.  There were 10 injuries reported in north central and northeast Illinois within the NWS Chicago/Romeoville County Warning Area (CWA).  Local officials estimated that nearly one million customers lost power across northern Illinois at the height of the derecho and some people were without power for several days.  Damage was estimated to be in the hundreds of millions of dollars in north central and northeast Illinois, with several billions of dollars in damages across the entire Corn Belt region including significant damage to crops and agriculture infrastructure.  While much of the damage was due to straight line winds, there were also 14 tornadoes documented in north central and northeast Illinois.||The combination of high moisture, explosive instability and very strong atmospheric wind flow for mid-summer had developed quickly over the Corn Belt region on the morning of August 10th.  This resulted in a progressive, well-organized complex of storms for hundreds of miles and at times traveling nearly 70 mph.  After bringing extensive damage from extreme wind speeds in Iowa that morning, the damage transitioned across northern Illinois from widespread wind damage to narrow, brief and intense swaths associated with compact circulations within the thunderstorm line, some of which were associated with tornadoes. Numerous trees were snapped and uprooted in Evanston.", "ts_dict_index": [9555, 9556, 9557]}
+{"event_id": 881107, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-29 00:26:00", "end_date_time": "2020-04-29 00:26:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A tree was blown down on Highway 135 just northeast of Overton.", "ts_dict_index": [9603, 9604, 9605]}
+{"event_id": 881104, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-29 00:23:00", "end_date_time": "2020-04-29 00:23:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A tree was blown down on FM 850 just east of Overton.", "ts_dict_index": [9612, 9613, 9614]}
+{"event_id": 881123, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2020-04-29 00:25:00", "end_date_time": "2020-04-29 00:25:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Trees were downed across Highway 315 just southwest of Carthage.", "ts_dict_index": [9600, 9601, 9602]}
+{"event_id": 881105, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2020-04-29 00:25:00", "end_date_time": "2020-04-29 00:25:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Trees were downed across FM 10 in Carthage.", "ts_dict_index": [9615, 9616, 9617]}
+{"event_id": 1080885, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-02 21:21:00", "end_date_time": "2023-03-02 21:21:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 1st and through March 2nd. Strong warm and moist air advection was ongoing in advance of the trough preceding the event. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. This environment produced an isolated strong thunderstorm that produced nickel size hail just south of Haworth on the 1st. A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing an isolated tornado in addition to large hail and damaging wind gusts Across McCurtain County Oklahoma. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threat of large hail also continued through the end of the event. An outdoor storage building was destroyed.", "ts_dict_index": [9630, 9631, 9632]}
+{"event_id": 881089, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-04-29 00:00:00", "end_date_time": "2020-04-29 00:00:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Trees were downed on FM 2625 west near 5 Notch Road.", "ts_dict_index": [9618, 9619, 9620]}
+{"event_id": 1124635, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-07-02 21:38:00", "end_date_time": "2023-07-02 21:38:00", "narrative": "Within a largely zonal flow regime, a midlevel shortwave trough progressed eastward from the mid MS Valley to the OH Valley by the overnight of July 2nd. Accompanying this trough, a belt of 40-50 kt midlevel flow overspread areas along and south of the OH River, across KY/TN through this evening.  Likewise, a weak surface cyclone in northern IL will moved eastward to OH during the evening and overnight, while a trailing cold front moved slowly southeastward.  The cold front stalled just west of Kentucky, and zone of ascent preceding the midlevel trough supported scattered to numerous thunderstorms through the night, with the attendant threats of damaging winds and large hail.||In the wake of weakening morning convection across KY, boundary-layer dewpoints in the low-mid 70s spread northeastward from the Mid-South as surface heating in cloud breaks boosted MLCAPE into the 2500-3500 J/kg range with minimal convective inhibition.  Thunderstorm development began by early-mid afternoon along and ahead of the front across KY/TN and vicinity, and storms subsequently spread east-northeastward through late evening/early night.  The increasing mid-upper flow over the warm sector resulted in sufficiently long and relatively straight hodographs for supercells and organized clusters capable of producing damaging winds and large hail.  An isolated tornado or two was not ruled out by SPC, primarily where storms interact with lingering convective outflow/locally backed near-surface winds.  ||Two lines of thunderstorms rolled through eastern Kentucky throughout the afternoon and evening, each one resulting in widespread wind damage. A tree was blown down on Malvin Hill Church Road near Hwy 192 near the communities of Ruth and Grade.", "ts_dict_index": [9636, 9637, 9638]}
+{"event_id": 1080881, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-02 21:10:00", "end_date_time": "2023-03-02 21:10:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 1st and through March 2nd. Strong warm and moist air advection was ongoing in advance of the trough preceding the event. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. This environment produced an isolated strong thunderstorm that produced nickel size hail just south of Haworth on the 1st. A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing an isolated tornado in addition to large hail and damaging wind gusts Across McCurtain County Oklahoma. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threat of large hail also continued through the end of the event. Tree reported down in the Pollard community southwest of Haworth.", "ts_dict_index": [9621, 9622, 9623]}
+{"event_id": 881086, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-04-28 23:50:00", "end_date_time": "2020-04-28 23:50:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Trees and power lines were downed on Runnels Road.", "ts_dict_index": [9609, 9610, 9611]}
+{"event_id": 1080884, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-02 21:20:00", "end_date_time": "2023-03-02 21:20:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 1st and through March 2nd. Strong warm and moist air advection was ongoing in advance of the trough preceding the event. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. This environment produced an isolated strong thunderstorm that produced nickel size hail just south of Haworth on the 1st. A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing an isolated tornado in addition to large hail and damaging wind gusts Across McCurtain County Oklahoma. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threat of large hail also continued through the end of the event. Trees reported down on power lines along Highway 3 just east of Broken Bow.", "ts_dict_index": [9633, 9634, 9635]}
+{"event_id": 881087, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-04-28 23:52:00", "end_date_time": "2020-04-28 23:52:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Trees were downed along I-20 west near Mile Marker 612.", "ts_dict_index": [9606, 9607, 9608]}
+{"event_id": 881110, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2020-04-29 00:40:00", "end_date_time": "2020-04-29 00:40:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Several trees were downed in Gary City.", "ts_dict_index": [9573, 9574, 9575]}
+{"event_id": 1112478, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-16 02:00:00", "end_date_time": "2023-06-16 02:00:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Numerous trees and power lines downed in and around Winona.", "ts_dict_index": [9660, 9661, 9662]}
+{"event_id": 1117223, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2023-07-29 06:12:00", "end_date_time": "2023-07-29 06:19:00", "narrative": "An upper level ridge was centered from the Four Corners Region to Arkansas. South central and central Nebraska were on the northern edge of this ridge. A weak upper trough extended over much of the Midwest. Temperatures were generally in the 70s during the early morning hours of July 29th across central and south central Nebraska. Dewpoint temperatures were generally in the mid 60s to lower 70s. Most unstable CAPE values were over 3,000 J/kg and the effective shear was around 40 knots. Surface winds were out of the north to northeast and winds at 500 millibars were out of the northwest. ||A complex of thunderstorms developed and strengthened over the Nebraska Sandhills during the early morning hours of July 29th and moved southeast. These storms began impacting the area just after 4:30 AM CDT in Valley County with wind gusts of 66 to 81 mph which caused tree damage. This complex of storms continued to move southeast across central and south central Nebraska and impacted Dawson, Phelps, Howard, Hall, Adams, Hamilton, Clay, and Fillmore Counties with severe wind gusts. These wind gusts ranged from 58 mph to 72 mph and resulted in tree and power pole damage. The final report of severe winds was at 7:30 AM CDT in Fillmore County. The most significant event was a brief tornado that had developed within the line/complex of storms in Clay County just before 7 AM CDT. The tornado moved from northwest to southeast across the town of Sutton. This tornado resulted in damage to trees, small outbuildings, homes, buildings, garages, a golf course, and a corn field. The tornado was rated as an EF-1 with winds up to 110 mph. A wind gust of 60 MPH was measured by a mesonet station located two miles north-northwest of Geneva and a wind gust of 58 MPH was measured by a mesonet station located five miles west of Geneva. Tree damage was reported in Geneva, and one power pole was damaged.", "ts_dict_index": [9645, 9646, 9647]}
+{"event_id": 1117220, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-07-29 06:05:00", "end_date_time": "2023-07-29 06:05:00", "narrative": "An upper level ridge was centered from the Four Corners Region to Arkansas. South central and central Nebraska were on the northern edge of this ridge. A weak upper trough extended over much of the Midwest. Temperatures were generally in the 70s during the early morning hours of July 29th across central and south central Nebraska. Dewpoint temperatures were generally in the mid 60s to lower 70s. Most unstable CAPE values were over 3,000 J/kg and the effective shear was around 40 knots. Surface winds were out of the north to northeast and winds at 500 millibars were out of the northwest. ||A complex of thunderstorms developed and strengthened over the Nebraska Sandhills during the early morning hours of July 29th and moved southeast. These storms began impacting the area just after 4:30 AM CDT in Valley County with wind gusts of 66 to 81 mph which caused tree damage. This complex of storms continued to move southeast across central and south central Nebraska and impacted Dawson, Phelps, Howard, Hall, Adams, Hamilton, Clay, and Fillmore Counties with severe wind gusts. These wind gusts ranged from 58 mph to 72 mph and resulted in tree and power pole damage. The final report of severe winds was at 7:30 AM CDT in Fillmore County. The most significant event was a brief tornado that had developed within the line/complex of storms in Clay County just before 7 AM CDT. The tornado moved from northwest to southeast across the town of Sutton. This tornado resulted in damage to trees, small outbuildings, homes, buildings, garages, a golf course, and a corn field. The tornado was rated as an EF-1 with winds up to 110 mph. Wind gusts estimated to be near 60 MPH downed a few tree branches of 3 to 4 inches in diameter.", "ts_dict_index": [9657, 9658, 9659]}
+{"event_id": 1117230, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "FILLMORE", "begin_date_time": "2023-07-29 06:30:00", "end_date_time": "2023-07-29 06:40:00", "narrative": "An upper level ridge was centered from the Four Corners Region to Arkansas. South central and central Nebraska were on the northern edge of this ridge. A weak upper trough extended over much of the Midwest. Temperatures were generally in the 70s during the early morning hours of July 29th across central and south central Nebraska. Dewpoint temperatures were generally in the mid 60s to lower 70s. Most unstable CAPE values were over 3,000 J/kg and the effective shear was around 40 knots. Surface winds were out of the north to northeast and winds at 500 millibars were out of the northwest. ||A complex of thunderstorms developed and strengthened over the Nebraska Sandhills during the early morning hours of July 29th and moved southeast. These storms began impacting the area just after 4:30 AM CDT in Valley County with wind gusts of 66 to 81 mph which caused tree damage. This complex of storms continued to move southeast across central and south central Nebraska and impacted Dawson, Phelps, Howard, Hall, Adams, Hamilton, Clay, and Fillmore Counties with severe wind gusts. These wind gusts ranged from 58 mph to 72 mph and resulted in tree and power pole damage. The final report of severe winds was at 7:30 AM CDT in Fillmore County. The most significant event was a brief tornado that had developed within the line/complex of storms in Clay County just before 7 AM CDT. The tornado moved from northwest to southeast across the town of Sutton. This tornado resulted in damage to trees, small outbuildings, homes, buildings, garages, a golf course, and a corn field. The tornado was rated as an EF-1 with winds up to 110 mph. Wind gusts were estimated to be near 70 MPH by emergency management in Milligan. A 66 MPH wind gust was measured by a mesonet station located four miles north-northwest of Ohiowa and a wind gust of 65 MPH was measured by a mesonet state located four miles west of Milligan.", "ts_dict_index": [9651, 9652, 9653]}
+{"event_id": 1117217, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-07-29 05:57:00", "end_date_time": "2023-07-29 05:57:00", "narrative": "An upper level ridge was centered from the Four Corners Region to Arkansas. South central and central Nebraska were on the northern edge of this ridge. A weak upper trough extended over much of the Midwest. Temperatures were generally in the 70s during the early morning hours of July 29th across central and south central Nebraska. Dewpoint temperatures were generally in the mid 60s to lower 70s. Most unstable CAPE values were over 3,000 J/kg and the effective shear was around 40 knots. Surface winds were out of the north to northeast and winds at 500 millibars were out of the northwest. ||A complex of thunderstorms developed and strengthened over the Nebraska Sandhills during the early morning hours of July 29th and moved southeast. These storms began impacting the area just after 4:30 AM CDT in Valley County with wind gusts of 66 to 81 mph which caused tree damage. This complex of storms continued to move southeast across central and south central Nebraska and impacted Dawson, Phelps, Howard, Hall, Adams, Hamilton, Clay, and Fillmore Counties with severe wind gusts. These wind gusts ranged from 58 mph to 72 mph and resulted in tree and power pole damage. The final report of severe winds was at 7:30 AM CDT in Fillmore County. The most significant event was a brief tornado that had developed within the line/complex of storms in Clay County just before 7 AM CDT. The tornado moved from northwest to southeast across the town of Sutton. This tornado resulted in damage to trees, small outbuildings, homes, buildings, garages, a golf course, and a corn field. The tornado was rated as an EF-1 with winds up to 110 mph. A wind gust of 62 MPH was measured by a mesonet station located one mile west-northwest of Sutton.", "ts_dict_index": [9648, 9649, 9650]}
+{"event_id": 1124636, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-07-02 21:52:00", "end_date_time": "2023-07-02 21:52:00", "narrative": "Within a largely zonal flow regime, a midlevel shortwave trough progressed eastward from the mid MS Valley to the OH Valley by the overnight of July 2nd. Accompanying this trough, a belt of 40-50 kt midlevel flow overspread areas along and south of the OH River, across KY/TN through this evening.  Likewise, a weak surface cyclone in northern IL will moved eastward to OH during the evening and overnight, while a trailing cold front moved slowly southeastward.  The cold front stalled just west of Kentucky, and zone of ascent preceding the midlevel trough supported scattered to numerous thunderstorms through the night, with the attendant threats of damaging winds and large hail.||In the wake of weakening morning convection across KY, boundary-layer dewpoints in the low-mid 70s spread northeastward from the Mid-South as surface heating in cloud breaks boosted MLCAPE into the 2500-3500 J/kg range with minimal convective inhibition.  Thunderstorm development began by early-mid afternoon along and ahead of the front across KY/TN and vicinity, and storms subsequently spread east-northeastward through late evening/early night.  The increasing mid-upper flow over the warm sector resulted in sufficiently long and relatively straight hodographs for supercells and organized clusters capable of producing damaging winds and large hail.  An isolated tornado or two was not ruled out by SPC, primarily where storms interact with lingering convective outflow/locally backed near-surface winds.  ||Two lines of thunderstorms rolled through eastern Kentucky throughout the afternoon and evening, each one resulting in widespread wind damage. A tree was blown down on Sandy Gap Road near the intersection with KY-80 between Somerset and London.", "ts_dict_index": [9639, 9640, 9641]}
+{"event_id": 1117216, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-07-29 05:30:00", "end_date_time": "2023-07-29 05:30:00", "narrative": "An upper level ridge was centered from the Four Corners Region to Arkansas. South central and central Nebraska were on the northern edge of this ridge. A weak upper trough extended over much of the Midwest. Temperatures were generally in the 70s during the early morning hours of July 29th across central and south central Nebraska. Dewpoint temperatures were generally in the mid 60s to lower 70s. Most unstable CAPE values were over 3,000 J/kg and the effective shear was around 40 knots. Surface winds were out of the north to northeast and winds at 500 millibars were out of the northwest. ||A complex of thunderstorms developed and strengthened over the Nebraska Sandhills during the early morning hours of July 29th and moved southeast. These storms began impacting the area just after 4:30 AM CDT in Valley County with wind gusts of 66 to 81 mph which caused tree damage. This complex of storms continued to move southeast across central and south central Nebraska and impacted Dawson, Phelps, Howard, Hall, Adams, Hamilton, Clay, and Fillmore Counties with severe wind gusts. These wind gusts ranged from 58 mph to 72 mph and resulted in tree and power pole damage. The final report of severe winds was at 7:30 AM CDT in Fillmore County. The most significant event was a brief tornado that had developed within the line/complex of storms in Clay County just before 7 AM CDT. The tornado moved from northwest to southeast across the town of Sutton. This tornado resulted in damage to trees, small outbuildings, homes, buildings, garages, a golf course, and a corn field. The tornado was rated as an EF-1 with winds up to 110 mph. Wind gusts were estimated to be near 60 MPH.", "ts_dict_index": [9654, 9655, 9656]}
+{"event_id": 1117215, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-07-29 05:20:00", "end_date_time": "2023-07-29 05:20:00", "narrative": "An upper level ridge was centered from the Four Corners Region to Arkansas. South central and central Nebraska were on the northern edge of this ridge. A weak upper trough extended over much of the Midwest. Temperatures were generally in the 70s during the early morning hours of July 29th across central and south central Nebraska. Dewpoint temperatures were generally in the mid 60s to lower 70s. Most unstable CAPE values were over 3,000 J/kg and the effective shear was around 40 knots. Surface winds were out of the north to northeast and winds at 500 millibars were out of the northwest. ||A complex of thunderstorms developed and strengthened over the Nebraska Sandhills during the early morning hours of July 29th and moved southeast. These storms began impacting the area just after 4:30 AM CDT in Valley County with wind gusts of 66 to 81 mph which caused tree damage. This complex of storms continued to move southeast across central and south central Nebraska and impacted Dawson, Phelps, Howard, Hall, Adams, Hamilton, Clay, and Fillmore Counties with severe wind gusts. These wind gusts ranged from 58 mph to 72 mph and resulted in tree and power pole damage. The final report of severe winds was at 7:30 AM CDT in Fillmore County. The most significant event was a brief tornado that had developed within the line/complex of storms in Clay County just before 7 AM CDT. The tornado moved from northwest to southeast across the town of Sutton. This tornado resulted in damage to trees, small outbuildings, homes, buildings, garages, a golf course, and a corn field. The tornado was rated as an EF-1 with winds up to 110 mph. Wind gusts were estimated to be near 60 MPH at the NWS Hastings office located four miles north of Hastings.", "ts_dict_index": [9642, 9643, 9644]}
+{"event_id": 1080883, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-02 21:16:00", "end_date_time": "2023-03-02 21:16:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 1st and through March 2nd. Strong warm and moist air advection was ongoing in advance of the trough preceding the event. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. This environment produced an isolated strong thunderstorm that produced nickel size hail just south of Haworth on the 1st. A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing an isolated tornado in addition to large hail and damaging wind gusts Across McCurtain County Oklahoma. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threat of large hail also continued through the end of the event. A tree fell on a house and caused damaged to a nearby fence.", "ts_dict_index": [9627, 9628, 9629]}
+{"event_id": 1112448, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-15 23:35:00", "end_date_time": "2023-06-15 23:35:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Trees downed near the intersection of Highway 271 and Landry Lane near the Starrville community.", "ts_dict_index": [9684, 9685, 9686]}
+{"event_id": 1112446, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-15 23:26:00", "end_date_time": "2023-06-15 23:26:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Trees downed at the intersection of Highway 271 and County Road 3110.", "ts_dict_index": [9687, 9688, 9689]}
+{"event_id": 825051, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-05-18 16:06:00", "end_date_time": "2019-05-18 16:06:00", "narrative": "While it heated up, it was not dry everywhere on the 15th. Before the ridge of high pressure could get here, a stationary front was in place across northeast sections of the state. Surrounding the front, scattered thunderstorms popped up during the afternoon. Some of the storms became strong to severe.||Mainly hail occurred with the strongest storms. The largest stones were about the size of a lime (two inches in diameter), and were reported just southwest of Salado (Independence County) at 711 pm CDT. Quarter to golf ball size hail was produced at  few miles west of Pocahontas (Randolph County), north of Huff, southwest of Batesville, and at Cushman (all in Independence County).||A few days later (on the 18th), a powerful storm system went from the southern Plains to the upper Midwest, with a cold front dragged into the region by the system. As the day began, storms were ongoing from Texas into Oklahoma. A line of storms eventually made it into western Arkansas by 200 pm CDT.||Just like on the 1st, part of the line bowed out (indicating the presence of strong to damaging winds) from Fort Smith (Sebastian County) to Clarksville (Johnson County). There was extensive tree damage, with trees on houses and blocking roads. Hardest hit areas inlcuded Paris and Scranton (both in Logan County). Gusts likely exceeded 90 mph.||Along the way, several photos showed a lot of dust kicked up by the wind. Gustnadoes or dust devils were also generated as the wind speed rapidly increased. There was a weak tornado (rated EF0) produced three miles west of Slovak (Prairie County). A couple of grain bins were dented or pushed in. The Cimarron Inn on Frontage Rd. sustained roof damage.", "ts_dict_index": [9672, 9673, 9674]}
+{"event_id": 825053, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-05-18 16:10:00", "end_date_time": "2019-05-18 16:10:00", "narrative": "While it heated up, it was not dry everywhere on the 15th. Before the ridge of high pressure could get here, a stationary front was in place across northeast sections of the state. Surrounding the front, scattered thunderstorms popped up during the afternoon. Some of the storms became strong to severe.||Mainly hail occurred with the strongest storms. The largest stones were about the size of a lime (two inches in diameter), and were reported just southwest of Salado (Independence County) at 711 pm CDT. Quarter to golf ball size hail was produced at  few miles west of Pocahontas (Randolph County), north of Huff, southwest of Batesville, and at Cushman (all in Independence County).||A few days later (on the 18th), a powerful storm system went from the southern Plains to the upper Midwest, with a cold front dragged into the region by the system. As the day began, storms were ongoing from Texas into Oklahoma. A line of storms eventually made it into western Arkansas by 200 pm CDT.||Just like on the 1st, part of the line bowed out (indicating the presence of strong to damaging winds) from Fort Smith (Sebastian County) to Clarksville (Johnson County). There was extensive tree damage, with trees on houses and blocking roads. Hardest hit areas inlcuded Paris and Scranton (both in Logan County). Gusts likely exceeded 90 mph.||Along the way, several photos showed a lot of dust kicked up by the wind. Gustnadoes or dust devils were also generated as the wind speed rapidly increased. There was a weak tornado (rated EF0) produced three miles west of Slovak (Prairie County). A couple of grain bins were dented or pushed in. A tree was down off of Hinkson Rd.", "ts_dict_index": [9669, 9670, 9671]}
+{"event_id": 825056, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-05-18 16:10:00", "end_date_time": "2019-05-18 16:10:00", "narrative": "While it heated up, it was not dry everywhere on the 15th. Before the ridge of high pressure could get here, a stationary front was in place across northeast sections of the state. Surrounding the front, scattered thunderstorms popped up during the afternoon. Some of the storms became strong to severe.||Mainly hail occurred with the strongest storms. The largest stones were about the size of a lime (two inches in diameter), and were reported just southwest of Salado (Independence County) at 711 pm CDT. Quarter to golf ball size hail was produced at  few miles west of Pocahontas (Randolph County), north of Huff, southwest of Batesville, and at Cushman (all in Independence County).||A few days later (on the 18th), a powerful storm system went from the southern Plains to the upper Midwest, with a cold front dragged into the region by the system. As the day began, storms were ongoing from Texas into Oklahoma. A line of storms eventually made it into western Arkansas by 200 pm CDT.||Just like on the 1st, part of the line bowed out (indicating the presence of strong to damaging winds) from Fort Smith (Sebastian County) to Clarksville (Johnson County). There was extensive tree damage, with trees on houses and blocking roads. Hardest hit areas inlcuded Paris and Scranton (both in Logan County). Gusts likely exceeded 90 mph.||Along the way, several photos showed a lot of dust kicked up by the wind. Gustnadoes or dust devils were also generated as the wind speed rapidly increased. There was a weak tornado (rated EF0) produced three miles west of Slovak (Prairie County). A couple of grain bins were dented or pushed in. A tree was blown down across Baseline Rd. All lanes were temporarily blocked.", "ts_dict_index": [9666, 9667, 9668]}
+{"event_id": 1112468, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2023-06-16 00:45:00", "end_date_time": "2023-06-16 00:45:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Reports of multiple trees downed across Panola County, with many trees blocking roads in the northern part of the county.", "ts_dict_index": [9675, 9676, 9677]}
+{"event_id": 1112443, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2023-06-16 00:35:00", "end_date_time": "2023-06-16 00:35:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. A 58 mph wind gust was recorded at the Texas Water Development Board Mesonet site south of De Berry.", "ts_dict_index": [9696, 9697, 9698]}
+{"event_id": 1112472, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2023-06-16 00:16:00", "end_date_time": "2023-06-16 00:16:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Several large trees downed across U.S. Highway 79 in the Panola area.", "ts_dict_index": [9681, 9682, 9683]}
+{"event_id": 1112470, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2023-06-16 00:15:00", "end_date_time": "2023-06-16 00:15:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Two structures damaged in the De Berry community.", "ts_dict_index": [9678, 9679, 9680]}
+{"event_id": 1112474, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-15 23:50:00", "end_date_time": "2023-06-15 23:50:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Numerous trees and utility poles downed in the Elderville area.", "ts_dict_index": [9690, 9691, 9692]}
+{"event_id": 1080882, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-02 21:15:00", "end_date_time": "2023-03-02 21:15:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 1st and through March 2nd. Strong warm and moist air advection was ongoing in advance of the trough preceding the event. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. This environment produced an isolated strong thunderstorm that produced nickel size hail just south of Haworth on the 1st. A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing an isolated tornado in addition to large hail and damaging wind gusts Across McCurtain County Oklahoma. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threat of large hail also continued through the end of the event. Large tree reported down on a home in Haworth on South Elm Street with no reports of injuries.", "ts_dict_index": [9624, 9625, 9626]}
+{"event_id": 1112430, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-15 23:45:00", "end_date_time": "2023-06-15 23:45:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Trees downed near the intersection of FM Road 3053 and County Road 1111.", "ts_dict_index": [9702, 9703, 9704]}
+{"event_id": 1112433, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-06-16 00:00:00", "end_date_time": "2023-06-16 00:00:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Widespread reports of trees downed along with widespread power outages in the city of Marshall.", "ts_dict_index": [9699, 9700, 9701]}
+{"event_id": 1112440, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-06-15 23:30:00", "end_date_time": "2023-06-15 23:30:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Trees downed near the intersection of FM Road 16 and County Road 32.", "ts_dict_index": [9663, 9664, 9665]}
+{"event_id": 1112850, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-06-16 00:29:00", "end_date_time": "2023-06-16 00:29:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. A 66 mph wind gust was recorded at the Shreveport Downtown Airport ASOS.", "ts_dict_index": [9714, 9715, 9716]}
+{"event_id": 1112844, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-06-16 00:45:00", "end_date_time": "2023-06-16 00:45:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Scattered reports of large tree limbs downed in and around the Legacy subdivision.", "ts_dict_index": [9711, 9712, 9713]}
+{"event_id": 1112801, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-06-16 02:30:00", "end_date_time": "2023-06-16 02:30:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Large tree downed across Highway 15 near Arthur McDaniel Road near Downsville.", "ts_dict_index": [9717, 9718, 9719]}
+{"event_id": 1112815, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-06-16 02:35:00", "end_date_time": "2023-06-16 02:35:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Numerous trees and power lines downed in the Point community area, with many trees across several roadways.", "ts_dict_index": [9720, 9721, 9722]}
+{"event_id": 1112814, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-06-16 02:25:00", "end_date_time": "2023-06-16 02:25:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Tree downed on Highway 151 near Fawn Drive close to Union and Ouachita Parish line.", "ts_dict_index": [9726, 9727, 9728]}
+{"event_id": 1112799, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-06-16 02:10:00", "end_date_time": "2023-06-16 02:10:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Tree downed on a vehicle on Highway 167 south of Bernice, trapping the driver but with no injuries reported.", "ts_dict_index": [9723, 9724, 9725]}
+{"event_id": 1112499, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-06-15 23:50:00", "end_date_time": "2023-06-15 23:50:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. NWS storm survey observed numerous snapped softwood trees indicative of 80 mph wind gusts, lying in southeasterly direction along Interstate 20 south of Marshall between State Highway 43 and U.S. Highway 59.", "ts_dict_index": [9705, 9706, 9707]}
+{"event_id": 1112489, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-06-15 23:52:00", "end_date_time": "2023-06-15 23:52:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Reports of widespread trees and power lines downed in Marshall and throughout Harrison County.", "ts_dict_index": [9693, 9694, 9695]}
+{"event_id": 1112819, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-16 00:45:00", "end_date_time": "2023-06-16 00:45:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Numerous trees downed in the Long Lake subdivision, including a couple of trees on a home on Chardonnay Circle.", "ts_dict_index": [9732, 9733, 9734]}
+{"event_id": 1112786, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-16 00:32:00", "end_date_time": "2023-06-16 00:32:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Numerous large pine trees were snapped on Ferry Creek Drive in the Ellerbe Wood subdivision in southeast Shreveport with widespread power outages reported.", "ts_dict_index": [9738, 9739, 9740]}
+{"event_id": 1112853, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-16 00:45:00", "end_date_time": "2023-06-16 00:45:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. An 80 mph wind gust was recorded at a Union Pacific Railroad Mesonet weather station along Highway 1 near the Port of Caddo-Bossier.", "ts_dict_index": [9735, 9736, 9737]}
+{"event_id": 1112813, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-16 00:35:00", "end_date_time": "2023-06-16 00:35:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Reports of numerous trees and power lines downed in the Southern Loop and Ellerbe Road areas, with one tree blocking the intersection of Ellerbe Road and Flournoy Lucas Road and another on Norris Ferry Road just north of Southern Loop.", "ts_dict_index": [9753, 9754, 9755]}
+{"event_id": 1112797, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-16 00:25:00", "end_date_time": "2023-06-16 00:25:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Several large limbs and a couple of trees downed in Blue Ridge Mobile Home Park on Buncombe Road in Shreveport with one street blocked.", "ts_dict_index": [9756, 9757, 9758]}
+{"event_id": 1112822, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-16 00:30:00", "end_date_time": "2023-06-16 00:30:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Reports of widespread downed trees throughout Shreveport and Caddo Parish.", "ts_dict_index": [9771, 9772, 9773]}
+{"event_id": 1112843, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-16 00:22:00", "end_date_time": "2023-06-16 00:22:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Tree downed onto a home in Blanchard, injuring an occupant of the home.", "ts_dict_index": [9729, 9730, 9731]}
+{"event_id": 1112848, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-16 00:26:00", "end_date_time": "2023-06-16 00:26:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. A 70 mph wind gust was recorded at the Shreveport Regional Airport ASOS.", "ts_dict_index": [9777, 9778, 9779]}
+{"event_id": 1112820, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-16 00:25:00", "end_date_time": "2023-06-16 00:25:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Reports of widespread downed trees and power lines in the Blanchard area.", "ts_dict_index": [9747, 9748, 9749]}
+{"event_id": 1112849, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-06-16 00:45:00", "end_date_time": "2023-06-16 00:45:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. A 67 mph wind gust was recorded by the Barksdale AFB ASOS in Bossier City.", "ts_dict_index": [9780, 9781, 9782]}
+{"event_id": 1112817, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-06-16 02:25:00", "end_date_time": "2023-06-16 02:25:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Numerous trees and power lines downed in the Downsville community area, with many trees across several roadways.", "ts_dict_index": [9750, 9751, 9752]}
+{"event_id": 1112794, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2023-06-16 01:05:00", "end_date_time": "2023-06-16 01:05:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Widespread downed trees in Doyline with a report of entrapment at a residence due to a tree on the home.", "ts_dict_index": [9759, 9760, 9761]}
+{"event_id": 1112788, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2023-06-16 01:10:00", "end_date_time": "2023-06-16 01:10:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Reports of widespread trees downed in Sibley.", "ts_dict_index": [9768, 9769, 9770]}
+{"event_id": 1112795, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2023-06-16 01:30:00", "end_date_time": "2023-06-16 01:30:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Several trees downed across the southern portions of Webster Parish, with multiple roads blocked.", "ts_dict_index": [9762, 9763, 9764]}
+{"event_id": 1112834, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-06-16 01:33:00", "end_date_time": "2023-06-16 01:33:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Multiple trees downed across Highway 6 near Robeline and the Sabine Parish line.", "ts_dict_index": [9774, 9775, 9776]}
+{"event_id": 1112833, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-06-16 01:20:00", "end_date_time": "2023-06-16 01:20:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Multiple trees were downed across Highway 9 north of Campti.", "ts_dict_index": [9741, 9742, 9743]}
+{"event_id": 1112431, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-15 23:50:00", "end_date_time": "2023-06-15 23:50:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Trees downed near the intersection of State Highway 42 and County Road 1115.", "ts_dict_index": [9708, 9709, 9710]}
+{"event_id": 964805, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2021-07-10 23:00:00", "end_date_time": "2021-07-10 23:00:00", "narrative": "Another cold front was set to push into Arkansas from the north by the 10th. Preceding the front, it was hot with high temperatures largely in the lower to mid 90s on the 8th. A few spots benefitted from isolated slow moving storms and prolonged downpours. During the early evening of the 8th, Conway (Faulkner County) got an impressive 2.88 inches of precipitation  On the 9th, Newport (Jackson County) got just shy of two inches of liquid, racking up 1.95 inches. Batesville (Independence County) received 2.06 inches of rain in 44 minutes, and recorded a 52 mph gust. There was also quarter size hail at Huff (Independence County).||Once the front arrived, storms tended to build to the west of Arkansas (from Oklahoma into Texas), and danced around the northern counties. There was less than a tenth of an inch of rain at Harrison (Boone County), and Mountain Home (Baxter County). A line of storms eventually formed toward central sections of the state as the evening progressed.||The line of storms was generally not severe, but some wind damage occurred toward 11 pm CST as trees were downed or snapped along and just south of Interstate 630 from west Little Rock (Pulaski County) toward the Arkansas State Fairgrounds. Trees were also toppled in parts of Lonoke County between 1100 am CST on the 9th and and 1200 am CST on the 10th.||Rain was the most widespread and heavy during this event in southwest Arkansas. In the twenty four hour period ending at 600 am CST on the 11th, Fordyce (Dallas County) got 1.90 inches of rain, with 1.72 inches at Waldron (Scott County), and 1.62 inches at Antoine (Pike County). A social media report showed pictures of several trees down off Kanis Rd. in the Twin Lakes area.", "ts_dict_index": [9783, 9784, 9785]}
+{"event_id": 1014820, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-12 20:47:00", "end_date_time": "2022-04-12 20:49:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. A band of damaging straight line winds estimated between 75-85 mph developed along the leading edge of a quasi-linear convective system (QLCS) across a portion of the Southern Hills neighborhood of South Shreveport, from the parent storm that would later spawn an EF-0 tornado over Southeast Shreveport and South Bossier City only 6-15 minutes later. Multiple large trees were snapped and uprooted in an area bounded by Bert Kouns Industrial loop to the south, Walker Road to the west, Highway 3132 to the north, and Kingston Road to the east. Trees fell on at least four homes in this area, with numerous large limbs snapped as well. A large portion of a metal roof was peeled off of the back of a used car company on Mackey Lane, with numerous shingles removed off of a business in the South Park Village. The front facade of another adjacent business in South Park Village was also blown into the parking lot. All of the snapped and uprooted trees throughout Southern Hills as well as the roof/facade damage in South Park Village were all blown/lying in a north-northeast direction, indicative of straight line winds.", "ts_dict_index": [9801, 9802, 9803]}
+{"event_id": 1015050, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-13 03:05:00", "end_date_time": "2022-04-13 03:05:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Roofs were damaged to mobile homes and other buildings in Bernice. Numerous trees were blown down as well.", "ts_dict_index": [9792, 9793, 9794]}
+{"event_id": 1015049, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-13 03:05:00", "end_date_time": "2022-04-13 03:05:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Multiple trees and power lines were downed on Highway 2 West from the Bernice Elementary School, forcing the closure of the roadway.", "ts_dict_index": [9789, 9790, 9791]}
+{"event_id": 1014850, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-12 22:28:00", "end_date_time": "2022-04-12 22:28:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. A tree fell onto a mobile home in the Truxno community.", "ts_dict_index": [9798, 9799, 9800]}
+{"event_id": 1015051, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-13 03:27:00", "end_date_time": "2022-04-13 03:27:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Multiple trees and power lines were downed on Pleasant Hill Road between Spearsville and Farmerville.", "ts_dict_index": [9786, 9787, 9788]}
+{"event_id": 1015048, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-13 03:05:00", "end_date_time": "2022-04-13 03:05:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. US 167 on the north side of Bernice was closed in both directions due to downed power lines lying across the road.", "ts_dict_index": [9804, 9805, 9806]}
+{"event_id": 1014841, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-04-12 21:18:00", "end_date_time": "2022-04-12 21:18:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Trees were blown down near the intersection of Old Highway 7 and Marathon Road just southeast of Cotton Valley.", "ts_dict_index": [9795, 9796, 9797]}
+{"event_id": 1112802, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-06-16 02:30:00", "end_date_time": "2023-06-16 02:30:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Tree downed on Scotts Hideaway Road near Lake D'Arbonne State Park.", "ts_dict_index": [9765, 9766, 9767]}
+{"event_id": 1014817, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-12 20:45:00", "end_date_time": "2022-04-12 20:45:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. A large tree was blown down onto a mobile home just north of Blanchard.", "ts_dict_index": [9807, 9808, 9809]}
+{"event_id": 1014819, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-12 20:48:00", "end_date_time": "2022-04-12 20:48:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. A portion of the roof of RJ's Restaurant was damaged. A sign from the restaurant was blown across Mansfield Road as well.", "ts_dict_index": [9816, 9817, 9818]}
+{"event_id": 1014837, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2022-04-12 20:58:00", "end_date_time": "2022-04-12 20:58:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Trees were downed at Bossier Elementary School.", "ts_dict_index": [9810, 9811, 9812]}
+{"event_id": 1015053, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-13 03:32:00", "end_date_time": "2022-04-13 03:32:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Numerous trees and power lines were downed several miles northwest of Farmerville.", "ts_dict_index": [9846, 9847, 9848]}
+{"event_id": 1014847, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-04-12 21:35:00", "end_date_time": "2022-04-12 21:35:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. A 66 mph wind gust was measured at the Minden Airport.", "ts_dict_index": [9828, 9829, 9830]}
+{"event_id": 1015054, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-13 03:40:00", "end_date_time": "2022-04-13 03:40:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Multiple trees were downed in the Truxno community.", "ts_dict_index": [9822, 9823, 9824]}
+{"event_id": 1015059, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2022-04-13 15:45:00", "end_date_time": "2022-04-13 15:45:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. A tree was downed on Highway 1227 northeast of Clarence.", "ts_dict_index": [9819, 9820, 9821]}
+{"event_id": 1014845, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-04-12 21:28:00", "end_date_time": "2022-04-12 21:28:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Several trees were blown down across the city of Minden, with some trees falling on vehicles.", "ts_dict_index": [9840, 9841, 9842]}
+{"event_id": 1014840, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-04-12 21:15:00", "end_date_time": "2022-04-12 21:15:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Several trees were blown down in and near Doyline.", "ts_dict_index": [9837, 9838, 9839]}
+{"event_id": 1014844, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-04-12 21:25:00", "end_date_time": "2022-04-12 21:25:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Multiple trees were blown down in and near Sibley.", "ts_dict_index": [9834, 9835, 9836]}
+{"event_id": 1014842, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-04-12 21:23:00", "end_date_time": "2022-04-12 21:23:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Trees were blown down on Martha Woods Road near Heflin.", "ts_dict_index": [9825, 9826, 9827]}
+{"event_id": 1015057, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2022-04-13 15:40:00", "end_date_time": "2022-04-13 15:40:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. A tree was blown down on Highway 480 east-southeast of Campti.", "ts_dict_index": [9843, 9844, 9845]}
+{"event_id": 1112789, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2023-06-16 01:05:00", "end_date_time": "2023-06-16 01:05:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. Numerous trees and power lines downed in Dixie Inn.", "ts_dict_index": [9744, 9745, 9746]}
+{"event_id": 1015047, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-13 03:05:00", "end_date_time": "2022-04-13 03:05:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Mobile homes were damaged in the Pisgah community.", "ts_dict_index": [9849, 9850, 9851]}
+{"event_id": 1014816, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-12 20:55:00", "end_date_time": "2022-04-12 20:55:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Numerous trees and power lines were downed throughout the city of Shreveport and the surrounding areas.", "ts_dict_index": [9813, 9814, 9815]}
+{"event_id": 1007730, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2022-03-31 18:44:00", "end_date_time": "2022-03-31 18:44:00", "narrative": "A warm front moved through the mid-Atlantic on the morning hours of March 31. This was associated with a strong area of low pressure moving through the Great Lakes, which had brought widespread severe weather to the Southeast US in prior days. Behind the warm front, widespread cloud cover and scattered showers lingered for most of the day over the eastern mid-Atlantic. Despite temperatures that still warmed to above average values, this greatly limited instability. However, more sunshine and subsequent instability developed further west over central Pennsylvania and northern Maryland. As a cold front approached by late afternoon, forcing for ascent increased, and strong wind fields were in place across the region in the warm sector of the Great Lakes low. Widespread convection developed over the interior mid-Atlantic, some of which became strong to severe. Convection generally favored a linear evolution with some embedded supercell structures. Because of the orientation of mid and upper level winds and the decreasing instability to the east, thunderstorms were very slow to move east and gradually lost intensity with time. In the local area, reports of severe weather were mostly isolated and confined to eastern Pennsylvania. However, a short-lived EF1 tornado did touch down over Bucks County, producing a 2 mile path of tree, utility, and some structural damage. Shower and thunderstorm activity continued through much of the night, slowly making its way to the coast, but was well below severe limits over New Jersey and Delmarva in the later hours of the night. A tree was reported down in Perry Twp near Zions Church Rd. Time estimated from radar.", "ts_dict_index": [9855, 9856, 9857]}
+{"event_id": 1007734, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2022-03-31 20:20:00", "end_date_time": "2022-03-31 20:20:00", "narrative": "A warm front moved through the mid-Atlantic on the morning hours of March 31. This was associated with a strong area of low pressure moving through the Great Lakes, which had brought widespread severe weather to the Southeast US in prior days. Behind the warm front, widespread cloud cover and scattered showers lingered for most of the day over the eastern mid-Atlantic. Despite temperatures that still warmed to above average values, this greatly limited instability. However, more sunshine and subsequent instability developed further west over central Pennsylvania and northern Maryland. As a cold front approached by late afternoon, forcing for ascent increased, and strong wind fields were in place across the region in the warm sector of the Great Lakes low. Widespread convection developed over the interior mid-Atlantic, some of which became strong to severe. Convection generally favored a linear evolution with some embedded supercell structures. Because of the orientation of mid and upper level winds and the decreasing instability to the east, thunderstorms were very slow to move east and gradually lost intensity with time. In the local area, reports of severe weather were mostly isolated and confined to eastern Pennsylvania. However, a short-lived EF1 tornado did touch down over Bucks County, producing a 2 mile path of tree, utility, and some structural damage. Shower and thunderstorm activity continued through much of the night, slowly making its way to the coast, but was well below severe limits over New Jersey and Delmarva in the later hours of the night. A tree was downed at Sycamore Rd and N Church St. Time estimated from radar.", "ts_dict_index": [9861, 9862, 9863]}
+{"event_id": 1142827, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-10-03 16:43:00", "end_date_time": "2023-10-03 16:45:00", "narrative": "A deep upper trough moved over the Central Plains. A shortwave moved over east central Colorado during the afternoon and CAPE values were highest just to the east of this feature. Low-level moisture was limited and instability was marginal across south central and central Nebraska but high enough for storms to produce severe updrafts.  Wind shear values were around 40 to 50 knots, and a cold front was moving toward the area. Low-level storm relative helicity was increasing which lead to a greater tornado threat. ||Thunderstorms developed during the afternoon ahead of the shortwave and became severe across portions of western Kansas and portions of southern Nebraska. These storms continued to develop and move eastward as the afternoon progressed. The storms began by producing nickel sized hail in Furnas County around 3 pm CDT. The hail got up to the size of golf balls in Dawson, Harlan, Phelps, and Adams Counties. A few of the storms produced tornadoes in Dawson and Sherman Counties. These tornadoes resulted in some damage and were rated EF-0. These storms eventually developed into a line as they moved across portions of Nebraska and Kansas. Aside from an estimated 70 mph wind causing some damage a farmstead near Marquette in Hamilton county, the strongest wind gust reported from the line of storms was 86 mph in Polk County. This wind gust along with other wind gusts resulted in wind damage across portions of south central and central Nebraska. The last severe report of the day was just before 7 pm CDT in Polk County with a wind gust near 60 mph. Wind gusts estimated to be near 70 MPH resulted in downed power lines in Glenvil and a flipped irrigation pivot located one mile south of Glenvil.", "ts_dict_index": [9870, 9871, 9872]}
+{"event_id": 1007733, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2022-03-31 20:15:00", "end_date_time": "2022-03-31 20:15:00", "narrative": "A warm front moved through the mid-Atlantic on the morning hours of March 31. This was associated with a strong area of low pressure moving through the Great Lakes, which had brought widespread severe weather to the Southeast US in prior days. Behind the warm front, widespread cloud cover and scattered showers lingered for most of the day over the eastern mid-Atlantic. Despite temperatures that still warmed to above average values, this greatly limited instability. However, more sunshine and subsequent instability developed further west over central Pennsylvania and northern Maryland. As a cold front approached by late afternoon, forcing for ascent increased, and strong wind fields were in place across the region in the warm sector of the Great Lakes low. Widespread convection developed over the interior mid-Atlantic, some of which became strong to severe. Convection generally favored a linear evolution with some embedded supercell structures. Because of the orientation of mid and upper level winds and the decreasing instability to the east, thunderstorms were very slow to move east and gradually lost intensity with time. In the local area, reports of severe weather were mostly isolated and confined to eastern Pennsylvania. However, a short-lived EF1 tornado did touch down over Bucks County, producing a 2 mile path of tree, utility, and some structural damage. Shower and thunderstorm activity continued through much of the night, slowly making its way to the coast, but was well below severe limits over New Jersey and Delmarva in the later hours of the night. A tree or limbs were downed on wires near Grace Rd at Coventryville Rd. Time estimated from radar.", "ts_dict_index": [9858, 9859, 9860]}
+{"event_id": 947264, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2021-05-04 11:11:00", "end_date_time": "2021-05-04 11:11:00", "narrative": "Very warm, moist, and humid air spread back north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma during the afternoon hours of May 3rd, along a strong southerly low level jet. This resulted in a moderately unstable air mass across the region, which lingered during the evening hours across Southeast Oklahoma, ahead of a upper trough that moved across the Southern Plains. This trough enhanced large scale forcing along the dryline across Central Oklahoma and North Texas, with scattered strong to severe thunderstorms developing over these areas, which shifted east northeast into the unstable air across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the late evening and early morning hours of the 14th. Numerous reports of damaging winds were received across these areas before the storms diminished during the early morning hours of the 4th.||These storms left behind a cold pool surface boundary across portions of East Texas, extreme Northwest Louisiana, and South-central Arkansas, which focused additional severe thunderstorm development from the late morning through the afternoon hours of the 4th, as large scale forcing again increased with the approaching upper trough atop the moderately unstable air mass along this mesoscale boundary. Additional reports of damaging winds were received across Deep East Texas, North Louisiana, and South-central Arkansas from these storms, before they spread southeast into Eastern and Southern Louisiana and Mississippi by mid and late afternoon. Numerous trees and power lines were downed across Natchitoches Parish.", "ts_dict_index": [9900, 9901, 9902]}
+{"event_id": 1007731, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2022-03-31 19:13:00", "end_date_time": "2022-03-31 19:13:00", "narrative": "A warm front moved through the mid-Atlantic on the morning hours of March 31. This was associated with a strong area of low pressure moving through the Great Lakes, which had brought widespread severe weather to the Southeast US in prior days. Behind the warm front, widespread cloud cover and scattered showers lingered for most of the day over the eastern mid-Atlantic. Despite temperatures that still warmed to above average values, this greatly limited instability. However, more sunshine and subsequent instability developed further west over central Pennsylvania and northern Maryland. As a cold front approached by late afternoon, forcing for ascent increased, and strong wind fields were in place across the region in the warm sector of the Great Lakes low. Widespread convection developed over the interior mid-Atlantic, some of which became strong to severe. Convection generally favored a linear evolution with some embedded supercell structures. Because of the orientation of mid and upper level winds and the decreasing instability to the east, thunderstorms were very slow to move east and gradually lost intensity with time. In the local area, reports of severe weather were mostly isolated and confined to eastern Pennsylvania. However, a short-lived EF1 tornado did touch down over Bucks County, producing a 2 mile path of tree, utility, and some structural damage. Shower and thunderstorm activity continued through much of the night, slowly making its way to the coast, but was well below severe limits over New Jersey and Delmarva in the later hours of the night. A tree was downed onto wires on Wertman Rd. Time estimated from radar.", "ts_dict_index": [9852, 9853, 9854]}
+{"event_id": 849792, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-20 04:30:00", "end_date_time": "2019-08-20 04:30:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. Public reported, via mPING, trees uprooted or snapped; roof blown off. Time estimated from radar.", "ts_dict_index": [9885, 9886, 9887]}
+{"event_id": 1141435, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-10-03 16:22:00", "end_date_time": "2023-10-03 16:22:00", "narrative": "A deep upper trough moved over the Central Plains. A shortwave moved over east central Colorado during the afternoon and CAPE values were highest just to the east of this feature. Low-level moisture was limited and instability was marginal across south central and central Nebraska but high enough for storms to produce severe updrafts.  Wind shear values were around 40 to 50 knots, and a cold front was moving toward the area. Low-level storm relative helicity was increasing which lead to a greater tornado threat. ||Thunderstorms developed during the afternoon ahead of the shortwave and became severe across portions of western Kansas and portions of southern Nebraska. These storms continued to develop and move eastward as the afternoon progressed. The storms began by producing nickel sized hail in Furnas County around 3 pm CDT. The hail got up to the size of golf balls in Dawson, Harlan, Phelps, and Adams Counties. A few of the storms produced tornadoes in Dawson and Sherman Counties. These tornadoes resulted in some damage and were rated EF-0. These storms eventually developed into a line as they moved across portions of Nebraska and Kansas. Aside from an estimated 70 mph wind causing some damage a farmstead near Marquette in Hamilton county, the strongest wind gust reported from the line of storms was 86 mph in Polk County. This wind gust along with other wind gusts resulted in wind damage across portions of south central and central Nebraska. The last severe report of the day was just before 7 pm CDT in Polk County with a wind gust near 60 mph. A wind gust of 76 MPH was measured by a mesonet station located five miles south-southeast of Roseland.", "ts_dict_index": [9873, 9874, 9875]}
+{"event_id": 1142833, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-10-03 17:00:00", "end_date_time": "2023-10-03 17:00:00", "narrative": "A deep upper trough moved over the Central Plains. A shortwave moved over east central Colorado during the afternoon and CAPE values were highest just to the east of this feature. Low-level moisture was limited and instability was marginal across south central and central Nebraska but high enough for storms to produce severe updrafts.  Wind shear values were around 40 to 50 knots, and a cold front was moving toward the area. Low-level storm relative helicity was increasing which lead to a greater tornado threat. ||Thunderstorms developed during the afternoon ahead of the shortwave and became severe across portions of western Kansas and portions of southern Nebraska. These storms continued to develop and move eastward as the afternoon progressed. The storms began by producing nickel sized hail in Furnas County around 3 pm CDT. The hail got up to the size of golf balls in Dawson, Harlan, Phelps, and Adams Counties. A few of the storms produced tornadoes in Dawson and Sherman Counties. These tornadoes resulted in some damage and were rated EF-0. These storms eventually developed into a line as they moved across portions of Nebraska and Kansas. Aside from an estimated 70 mph wind causing some damage a farmstead near Marquette in Hamilton county, the strongest wind gust reported from the line of storms was 86 mph in Polk County. This wind gust along with other wind gusts resulted in wind damage across portions of south central and central Nebraska. The last severe report of the day was just before 7 pm CDT in Polk County with a wind gust near 60 mph. Wind gusts were estimated to be near 60 MPH.", "ts_dict_index": [9864, 9865, 9866]}
+{"event_id": 815580, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2019-04-25 00:12:00", "end_date_time": "2019-04-25 00:12:00", "narrative": "A strong closed upper level low pressure system advanced east across Central Texas during the evening hours of April 24th, which helped to mix a warm front north into portions of Deep East Texas and Northcentral Louisiana. As a result, warm, moist, and unstable air began to build north along and south of the front, as steepening lapse rates aloft spread east along the axis of increasing large scale forcing ahead of the low. This resulted in an increase in scattered to numerous showers and thunderstorms near and south of the warm front from the late evening hours of the 24th through the early morning hours of the 25th across East Texas and North Louisiana. Coupled with the strong wind shear present across the expanding warm sector, several supercell thunderstorms developed, with one supercell spawning six separate tornadoes from San Augustine Texas northeast to Eastern Union Parish Louisiana, directly impacting the cities of San Augustine Texas and Ruston Louisiana along its 150+ mile track across the NWS Shreveport County Warning Area. In fact, this supercell spawned another tornado across Northwest Morehouse and Southern Ashley County Arkansas, to complete its nearly 180 mile track before dissipating. Other isolated supercells developed near and south of the warm front which spawned tornadoes across Northern Caddo Parish and Central La Salle Parish in Northern Louisiana, with other severe thunderstorms producing damaging winds across portions of Northcentral Louisiana as well, before the storms exited the region around daybreak on the 25th. Trees were downed along the 4300 block of Highway 485 north of Robeline.", "ts_dict_index": [9876, 9877, 9878]}
+{"event_id": 947270, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2021-05-04 11:44:00", "end_date_time": "2021-05-04 11:44:00", "narrative": "Very warm, moist, and humid air spread back north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma during the afternoon hours of May 3rd, along a strong southerly low level jet. This resulted in a moderately unstable air mass across the region, which lingered during the evening hours across Southeast Oklahoma, ahead of a upper trough that moved across the Southern Plains. This trough enhanced large scale forcing along the dryline across Central Oklahoma and North Texas, with scattered strong to severe thunderstorms developing over these areas, which shifted east northeast into the unstable air across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the late evening and early morning hours of the 14th. Numerous reports of damaging winds were received across these areas before the storms diminished during the early morning hours of the 4th.||These storms left behind a cold pool surface boundary across portions of East Texas, extreme Northwest Louisiana, and South-central Arkansas, which focused additional severe thunderstorm development from the late morning through the afternoon hours of the 4th, as large scale forcing again increased with the approaching upper trough atop the moderately unstable air mass along this mesoscale boundary. Additional reports of damaging winds were received across Deep East Texas, North Louisiana, and South-central Arkansas from these storms, before they spread southeast into Eastern and Southern Louisiana and Mississippi by mid and late afternoon. Trees were downed near Goldonna.", "ts_dict_index": [9891, 9892, 9893]}
+{"event_id": 849762, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-20 04:29:00", "end_date_time": "2019-08-20 04:29:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. NWS employee reported tree down over 61st street south of Merle Hay Mall. Time estimated from radar.", "ts_dict_index": [9888, 9889, 9890]}
+{"event_id": 849765, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-08-20 04:25:00", "end_date_time": "2019-08-20 04:25:00", "narrative": "Generally speaking, a bit of everything occurred during an overnight/early morning severe mesoscale convective system that rolled across Iowa. The predominant weather revolved around damaging winds and heavy rainfall, though a few instances of severe hail and low end tornadoes were experienced as well. Among the reports, numerous trees were downed, buildings damaged or destroyed from straight line winds or one of the weak tornadoes, and numerous instances of 2 to 4 plus inches of heavy rainfall. ||On the setup side of the coin, a lot of factors were in line for the event to potentially be a sustained nocturnal severe weather event. The previous day, the 19th, saw surface high pressure begin to exit the region eastward and allowing southerly return flow to work into eastern Nebraska and western Iowa. Tied in with mid to upper 70 dew points and steep mid-level lapse rates, a large area of 4000 plus J/kg CAPE values developed across eastern Nebraska and western Iowa and slowly built eastward. Additionally, effect bulk shear was consistently in the 40 to 50 kt range and low level shear roughly oriented to expected storm motion. As the evening progressed and the low level jet finally began to ramp up, boosting warm air advection and positive moisture flux, storms began to develop and eventually congeal. Organization, at least with regards to strong to severe criteria, was not immediate, waiting until around 5am local time to produce its first severe report. Severe reports then continued as the system moved southeast over the next 4 plus hours. Media reported several small and medium size tree branches down.", "ts_dict_index": [9882, 9883, 9884]}
+{"event_id": 947258, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2021-05-04 10:36:00", "end_date_time": "2021-05-04 10:36:00", "narrative": "Very warm, moist, and humid air spread back north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma during the afternoon hours of May 3rd, along a strong southerly low level jet. This resulted in a moderately unstable air mass across the region, which lingered during the evening hours across Southeast Oklahoma, ahead of a upper trough that moved across the Southern Plains. This trough enhanced large scale forcing along the dryline across Central Oklahoma and North Texas, with scattered strong to severe thunderstorms developing over these areas, which shifted east northeast into the unstable air across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the late evening and early morning hours of the 14th. Numerous reports of damaging winds were received across these areas before the storms diminished during the early morning hours of the 4th.||These storms left behind a cold pool surface boundary across portions of East Texas, extreme Northwest Louisiana, and South-central Arkansas, which focused additional severe thunderstorm development from the late morning through the afternoon hours of the 4th, as large scale forcing again increased with the approaching upper trough atop the moderately unstable air mass along this mesoscale boundary. Additional reports of damaging winds were received across Deep East Texas, North Louisiana, and South-central Arkansas from these storms, before they spread southeast into Eastern and Southern Louisiana and Mississippi by mid and late afternoon. A tree was blown down on Highway 80 East.", "ts_dict_index": [9903, 9904, 9905]}
+{"event_id": 947261, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2021-05-04 10:07:00", "end_date_time": "2021-05-04 10:07:00", "narrative": "Very warm, moist, and humid air spread back north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma during the afternoon hours of May 3rd, along a strong southerly low level jet. This resulted in a moderately unstable air mass across the region, which lingered during the evening hours across Southeast Oklahoma, ahead of a upper trough that moved across the Southern Plains. This trough enhanced large scale forcing along the dryline across Central Oklahoma and North Texas, with scattered strong to severe thunderstorms developing over these areas, which shifted east northeast into the unstable air across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the late evening and early morning hours of the 14th. Numerous reports of damaging winds were received across these areas before the storms diminished during the early morning hours of the 4th.||These storms left behind a cold pool surface boundary across portions of East Texas, extreme Northwest Louisiana, and South-central Arkansas, which focused additional severe thunderstorm development from the late morning through the afternoon hours of the 4th, as large scale forcing again increased with the approaching upper trough atop the moderately unstable air mass along this mesoscale boundary. Additional reports of damaging winds were received across Deep East Texas, North Louisiana, and South-central Arkansas from these storms, before they spread southeast into Eastern and Southern Louisiana and Mississippi by mid and late afternoon. A tree was blown down onto Highway 2 in Shongaloo.", "ts_dict_index": [9897, 9898, 9899]}
+{"event_id": 1142866, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-10-03 17:04:00", "end_date_time": "2023-10-03 17:10:00", "narrative": "A deep upper trough moved over the Central Plains. A shortwave moved over east central Colorado during the afternoon and CAPE values were highest just to the east of this feature. Low-level moisture was limited and instability was marginal across south central and central Nebraska but high enough for storms to produce severe updrafts.  Wind shear values were around 40 to 50 knots, and a cold front was moving toward the area. Low-level storm relative helicity was increasing which lead to a greater tornado threat. ||Thunderstorms developed during the afternoon ahead of the shortwave and became severe across portions of western Kansas and portions of southern Nebraska. These storms continued to develop and move eastward as the afternoon progressed. The storms began by producing nickel sized hail in Furnas County around 3 pm CDT. The hail got up to the size of golf balls in Dawson, Harlan, Phelps, and Adams Counties. A few of the storms produced tornadoes in Dawson and Sherman Counties. These tornadoes resulted in some damage and were rated EF-0. These storms eventually developed into a line as they moved across portions of Nebraska and Kansas. Aside from an estimated 70 mph wind causing some damage a farmstead near Marquette in Hamilton county, the strongest wind gust reported from the line of storms was 86 mph in Polk County. This wind gust along with other wind gusts resulted in wind damage across portions of south central and central Nebraska. The last severe report of the day was just before 7 pm CDT in Polk County with a wind gust near 60 mph. A wind gust of 62 MPH was measured by a mesonet station located four miles southwest of Hastings. Wind gusts were estimated to be near 60 MPH at the NWS Hastings office located four miles north of Hastings. Minor tree damage was reported in Hastings.", "ts_dict_index": [9867, 9868, 9869]}
+{"event_id": 1014846, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-04-12 21:29:00", "end_date_time": "2022-04-12 21:29:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. Multiple trees were blown down in and near Dubberly.", "ts_dict_index": [9831, 9832, 9833]}
+{"event_id": 947257, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-05-04 10:26:00", "end_date_time": "2021-05-04 10:26:00", "narrative": "Very warm, moist, and humid air spread back north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma during the afternoon hours of May 3rd, along a strong southerly low level jet. This resulted in a moderately unstable air mass across the region, which lingered during the evening hours across Southeast Oklahoma, ahead of a upper trough that moved across the Southern Plains. This trough enhanced large scale forcing along the dryline across Central Oklahoma and North Texas, with scattered strong to severe thunderstorms developing over these areas, which shifted east northeast into the unstable air across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the late evening and early morning hours of the 14th. Numerous reports of damaging winds were received across these areas before the storms diminished during the early morning hours of the 4th.||These storms left behind a cold pool surface boundary across portions of East Texas, extreme Northwest Louisiana, and South-central Arkansas, which focused additional severe thunderstorm development from the late morning through the afternoon hours of the 4th, as large scale forcing again increased with the approaching upper trough atop the moderately unstable air mass along this mesoscale boundary. Additional reports of damaging winds were received across Deep East Texas, North Louisiana, and South-central Arkansas from these storms, before they spread southeast into Eastern and Southern Louisiana and Mississippi by mid and late afternoon. Several trees were blown down across Southern Bossier Parish.", "ts_dict_index": [9906, 9907, 9908]}
+{"event_id": 947266, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2021-05-04 11:25:00", "end_date_time": "2021-05-04 11:25:00", "narrative": "Very warm, moist, and humid air spread back north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma during the afternoon hours of May 3rd, along a strong southerly low level jet. This resulted in a moderately unstable air mass across the region, which lingered during the evening hours across Southeast Oklahoma, ahead of a upper trough that moved across the Southern Plains. This trough enhanced large scale forcing along the dryline across Central Oklahoma and North Texas, with scattered strong to severe thunderstorms developing over these areas, which shifted east northeast into the unstable air across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the late evening and early morning hours of the 14th. Numerous reports of damaging winds were received across these areas before the storms diminished during the early morning hours of the 4th.||These storms left behind a cold pool surface boundary across portions of East Texas, extreme Northwest Louisiana, and South-central Arkansas, which focused additional severe thunderstorm development from the late morning through the afternoon hours of the 4th, as large scale forcing again increased with the approaching upper trough atop the moderately unstable air mass along this mesoscale boundary. Additional reports of damaging winds were received across Deep East Texas, North Louisiana, and South-central Arkansas from these storms, before they spread southeast into Eastern and Southern Louisiana and Mississippi by mid and late afternoon. Shingles were blown off the roof of a home in Farmerville.", "ts_dict_index": [9909, 9910, 9911]}
+{"event_id": 964699, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-07-10 16:54:00", "end_date_time": "2021-07-10 16:54:00", "narrative": "Several days of heavy to torrential rains and gusty winds were experienced across eastern Kentucky from July 9th through the 12th. A strong surface low pressure remained parked across Illinois to our WNW, with a frontal boundary expanding eastward and through Kentucky, sinking just south of the state to start the day on the 9th. During the day on the 9th and the 10th, the front began lifting northward through eastern Kentucky as a warm front, becoming the center for convective development, and also allowing for much deeper warm air and moisture advection into the region. As the front slowly continued just north of the state on the 11th and 12th, Kentucky found itself in the warm and unstable sector of the system, with showers and thunderstorms developing, peaking in coverage and intensity during the afternoon hours. ||Given the warm environment, storms were generally low centroid and moisture laden, exhibiting well above normal PWats, in the 2 to 2.5 inch range. Soundings also showed shallow inverted V signatures, indicative of steep low level lapse rates and the ability to easily mix down higher winds aloft. Pulsy scattered convection with heavy rain and high wind gusts were the main concerns. Locations where multiple storms moved over saw high water and some instances of flash flooding. Other locations experienced thunderstorm wind damage as stronger winds transferred to the surface, especially as the storms were beginning the dissipating phase. ||An 850 jet SW to NE, storms that NW to SE oriented were bowing. Multiple trees were blown down along Bauer Road.", "ts_dict_index": [9918, 9919, 9920]}
+{"event_id": 964698, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-07-10 16:52:00", "end_date_time": "2021-07-10 16:52:00", "narrative": "Several days of heavy to torrential rains and gusty winds were experienced across eastern Kentucky from July 9th through the 12th. A strong surface low pressure remained parked across Illinois to our WNW, with a frontal boundary expanding eastward and through Kentucky, sinking just south of the state to start the day on the 9th. During the day on the 9th and the 10th, the front began lifting northward through eastern Kentucky as a warm front, becoming the center for convective development, and also allowing for much deeper warm air and moisture advection into the region. As the front slowly continued just north of the state on the 11th and 12th, Kentucky found itself in the warm and unstable sector of the system, with showers and thunderstorms developing, peaking in coverage and intensity during the afternoon hours. ||Given the warm environment, storms were generally low centroid and moisture laden, exhibiting well above normal PWats, in the 2 to 2.5 inch range. Soundings also showed shallow inverted V signatures, indicative of steep low level lapse rates and the ability to easily mix down higher winds aloft. Pulsy scattered convection with heavy rain and high wind gusts were the main concerns. Locations where multiple storms moved over saw high water and some instances of flash flooding. Other locations experienced thunderstorm wind damage as stronger winds transferred to the surface, especially as the storms were beginning the dissipating phase. ||An 850 jet SW to NE, storms that NW to SE oriented were bowing. A tree was blown down along River Road near Sloans Valley.", "ts_dict_index": [9912, 9913, 9914]}
+{"event_id": 964700, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-07-10 16:54:00", "end_date_time": "2021-07-10 16:54:00", "narrative": "Several days of heavy to torrential rains and gusty winds were experienced across eastern Kentucky from July 9th through the 12th. A strong surface low pressure remained parked across Illinois to our WNW, with a frontal boundary expanding eastward and through Kentucky, sinking just south of the state to start the day on the 9th. During the day on the 9th and the 10th, the front began lifting northward through eastern Kentucky as a warm front, becoming the center for convective development, and also allowing for much deeper warm air and moisture advection into the region. As the front slowly continued just north of the state on the 11th and 12th, Kentucky found itself in the warm and unstable sector of the system, with showers and thunderstorms developing, peaking in coverage and intensity during the afternoon hours. ||Given the warm environment, storms were generally low centroid and moisture laden, exhibiting well above normal PWats, in the 2 to 2.5 inch range. Soundings also showed shallow inverted V signatures, indicative of steep low level lapse rates and the ability to easily mix down higher winds aloft. Pulsy scattered convection with heavy rain and high wind gusts were the main concerns. Locations where multiple storms moved over saw high water and some instances of flash flooding. Other locations experienced thunderstorm wind damage as stronger winds transferred to the surface, especially as the storms were beginning the dissipating phase. ||An 850 jet SW to NE, storms that NW to SE oriented were bowing. A tree was blown down along Blue John Road near Alpine.", "ts_dict_index": [9915, 9916, 9917]}
+{"event_id": 815583, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2019-04-25 01:05:00", "end_date_time": "2019-04-25 01:05:00", "narrative": "A strong closed upper level low pressure system advanced east across Central Texas during the evening hours of April 24th, which helped to mix a warm front north into portions of Deep East Texas and Northcentral Louisiana. As a result, warm, moist, and unstable air began to build north along and south of the front, as steepening lapse rates aloft spread east along the axis of increasing large scale forcing ahead of the low. This resulted in an increase in scattered to numerous showers and thunderstorms near and south of the warm front from the late evening hours of the 24th through the early morning hours of the 25th across East Texas and North Louisiana. Coupled with the strong wind shear present across the expanding warm sector, several supercell thunderstorms developed, with one supercell spawning six separate tornadoes from San Augustine Texas northeast to Eastern Union Parish Louisiana, directly impacting the cities of San Augustine Texas and Ruston Louisiana along its 150+ mile track across the NWS Shreveport County Warning Area. In fact, this supercell spawned another tornado across Northwest Morehouse and Southern Ashley County Arkansas, to complete its nearly 180 mile track before dissipating. Other isolated supercells developed near and south of the warm front which spawned tornadoes across Northern Caddo Parish and Central La Salle Parish in Northern Louisiana, with other severe thunderstorms producing damaging winds across portions of Northcentral Louisiana as well, before the storms exited the region around daybreak on the 25th. Numerous trees and power lines were downed in the Downsville area.", "ts_dict_index": [9879, 9880, 9881]}
+{"event_id": 854860, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-10-21 03:10:00", "end_date_time": "2019-10-21 03:10:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Several large trees were uprooted and many large branches were broken along County Road 2117.", "ts_dict_index": [9924, 9925, 9926]}
+{"event_id": 855078, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-10-21 03:00:00", "end_date_time": "2019-10-21 03:00:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Several trees were downed, with portions of the roof torn off of the Harry's Building Materials in Troup.", "ts_dict_index": [9927, 9928, 9929]}
+{"event_id": 855489, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 19:00:00", "end_date_time": "2019-10-20 19:00:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. A tree was blown down on County Road 305 just north of Carthage.", "ts_dict_index": [9933, 9934, 9935]}
+{"event_id": 855108, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 19:25:00", "end_date_time": "2019-10-20 19:25:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Tree down blocking County Road 124 near County Road 237.", "ts_dict_index": [9942, 9943, 9944]}
+{"event_id": 855120, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 18:45:00", "end_date_time": "2019-10-20 18:45:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. A tree was blown down across the intersection of County Road 202 and County Road 230.", "ts_dict_index": [9948, 9949, 9950]}
+{"event_id": 855091, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 18:35:00", "end_date_time": "2019-10-20 18:35:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Fourteen trees were downed near the intersection of County Road 188 and County Road 189.", "ts_dict_index": [9930, 9931, 9932]}
+{"event_id": 855118, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 18:25:00", "end_date_time": "2019-10-20 18:25:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Trees down covering both lanes of the road near the intersection of County Road 219 and County Road 959 in the Holland Quarters community.", "ts_dict_index": [9945, 9946, 9947]}
+{"event_id": 855093, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-21 03:55:00", "end_date_time": "2019-10-21 03:55:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. A tree fell on a home on County Road 4034 near Dixie Lake.", "ts_dict_index": [9939, 9940, 9941]}
+{"event_id": 1140295, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-10-12 15:38:00", "end_date_time": "2023-10-12 15:38:00", "narrative": "Southerly upper level winds moved across Nebraska and brought in a thick layer of low-level stratus clouds during the early morning hours. These clouds limited surface heating during the day; however, cooler air aloft moved over the area during midday. These conditions resulted in more instability. This instability combined with a low-pressure system, forcing from a strong 500 mb jet, and strong low-level wind shear. There was locally enhanced 0 ��� 1 km helicity near a surface low. There was an intersection of a surface warm front with a dryline and cold front near the center of the surface low. The cold front moved across the area during the overnight hours. These conditions resulted in severe weather during the afternoon hours. ||Thunderstorms were present across Nebraska during the early afternoon hours and moved northeastward. These storms began in south central Nebraska by producing a tornado in Phelps County at 1:05 PM CDT. This tornado was rated as an EF-0 and did some damage. These storms moved eastward and developed into line segments and went on to produce 5 more tornadoes. The additional tornadoes were in Dawson, Franklin, Kearney, Adams, and Hall Counties. The tornadoes in Franklin and Kearney Counties were rated EF-1 while the others were rated EF-0. These storms also produced hail and severe wind gusts. The biggest hail was half dollar size in Phelps County. There was a 63 mph wind gust in Adams County. The storms ended by producing nickel sized hail in Hamilton County at 5:05 PM CDT. A wind gust of 63 MPH was measured by a home weather station located in Hastings.", "ts_dict_index": [9921, 9922, 9923]}
+{"event_id": 947265, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2021-05-04 10:58:00", "end_date_time": "2021-05-04 10:58:00", "narrative": "Very warm, moist, and humid air spread back north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma during the afternoon hours of May 3rd, along a strong southerly low level jet. This resulted in a moderately unstable air mass across the region, which lingered during the evening hours across Southeast Oklahoma, ahead of a upper trough that moved across the Southern Plains. This trough enhanced large scale forcing along the dryline across Central Oklahoma and North Texas, with scattered strong to severe thunderstorms developing over these areas, which shifted east northeast into the unstable air across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the late evening and early morning hours of the 14th. Numerous reports of damaging winds were received across these areas before the storms diminished during the early morning hours of the 4th.||These storms left behind a cold pool surface boundary across portions of East Texas, extreme Northwest Louisiana, and South-central Arkansas, which focused additional severe thunderstorm development from the late morning through the afternoon hours of the 4th, as large scale forcing again increased with the approaching upper trough atop the moderately unstable air mass along this mesoscale boundary. Additional reports of damaging winds were received across Deep East Texas, North Louisiana, and South-central Arkansas from these storms, before they spread southeast into Eastern and Southern Louisiana and Mississippi by mid and late afternoon. Trees were downed near Flora and Provencal along Highway 120.", "ts_dict_index": [9894, 9895, 9896]}
+{"event_id": 855494, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 19:25:00", "end_date_time": "2019-10-20 19:25:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. A tree was blown down onto power lines on County Road 322.", "ts_dict_index": [9954, 9955, 9956]}
+{"event_id": 855493, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 19:25:00", "end_date_time": "2019-10-20 19:25:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. A tree was blown down onto power lines on Don Long Road.", "ts_dict_index": [9951, 9952, 9953]}
+{"event_id": 855490, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 19:20:00", "end_date_time": "2019-10-20 19:20:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. A tree was blown down onto power lines on County Road 328.", "ts_dict_index": [9936, 9937, 9938]}
+{"event_id": 1014537, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-04-12 19:04:00", "end_date_time": "2022-04-12 19:04:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. A tree was blown down near FM 2493 and 6th Street.", "ts_dict_index": [10014, 10015, 10016]}
+{"event_id": 1014536, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-04-12 19:08:00", "end_date_time": "2022-04-12 19:08:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. Windows were blown out at the Mother Frances Hospital near Downtown Tyler.", "ts_dict_index": [10002, 10003, 10004]}
+{"event_id": 1014532, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-04-12 19:00:00", "end_date_time": "2022-04-12 19:00:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. Trees were downed on Old Jacksonville Highway southwest of Tyler.", "ts_dict_index": [10011, 10012, 10013]}
+{"event_id": 1014534, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-04-12 07:03:00", "end_date_time": "2022-04-12 07:03:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. Damaging straight line winds affected much of the Azalea District south of Downtown Tyler, with a prolonged period of high winds impacting the area from a squall line of severe thunderstorms. Multiple hardwood trees were uprooted across the area, falling in a northeasterly direction with some tree trunks falling into buildings as well as one vehicle near West Philips Street. Hardwood tree uproots were the primary damage indicator, with winds estimated up to 100 mph.", "ts_dict_index": [10008, 10009, 10010]}
+{"event_id": 854859, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-10-21 02:43:00", "end_date_time": "2019-10-21 02:43:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. A roof was blown off of a house under construction on FM 344 near County Line Baptist Church between Teaselville and Bullard. In the vicinity of that location, a hay ring was moved, several trees were blown down, and large branches were broken.", "ts_dict_index": [9969, 9970, 9971]}
+{"event_id": 878151, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2020-02-05 19:06:00", "end_date_time": "2020-02-05 19:06:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down.", "ts_dict_index": [10026, 10027, 10028]}
+{"event_id": 855491, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 18:30:00", "end_date_time": "2019-10-20 18:30:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Trees were blown down onto County Road 107.", "ts_dict_index": [9963, 9964, 9965]}
+{"event_id": 854763, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-10-20 18:00:00", "end_date_time": "2019-10-20 18:00:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Multiple trees and power lines were blown down across FM 225.", "ts_dict_index": [9981, 9982, 9983]}
+{"event_id": 1014553, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-12 19:50:00", "end_date_time": "2022-04-12 19:50:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. A tree was blown down on Highway 301 just outside of the Henderson city limits.", "ts_dict_index": [9993, 9994, 9995]}
+{"event_id": 855492, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 18:31:00", "end_date_time": "2019-10-20 18:31:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Power lines were downed on County Road 104.", "ts_dict_index": [9966, 9967, 9968]}
+{"event_id": 854861, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-21 03:53:00", "end_date_time": "2019-10-21 03:53:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Trees were downed near Carthage.", "ts_dict_index": [9990, 9991, 9992]}
+{"event_id": 813764, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-04-13 12:05:00", "end_date_time": "2019-04-13 12:05:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing numerous reports of damaging winds with several tornadoes across portions of East Texas. These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Trees were downed across Highway 42 near the intersection of County Road 142D between the Laird Hill and Leveretts Chapel communities.", "ts_dict_index": [10023, 10024, 10025]}
+{"event_id": 1014547, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-12 19:34:00", "end_date_time": "2022-04-12 19:34:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. A tree was blown down onto Camp Street in Kilgore.", "ts_dict_index": [9999, 10000, 10001]}
+{"event_id": 854769, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 19:26:00", "end_date_time": "2019-10-20 19:26:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Power lines were downed and wrapped into trees in the Bethany community.", "ts_dict_index": [9987, 9988, 9989]}
+{"event_id": 855488, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 19:15:00", "end_date_time": "2019-10-20 19:15:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. A tree was blown down onto power lines on County Road 336 north of the DeBerry community.", "ts_dict_index": [9960, 9961, 9962]}
+{"event_id": 855487, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 19:23:00", "end_date_time": "2019-10-20 19:23:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Trees and power lines down on County Road 3332 in the Bethany community.", "ts_dict_index": [9957, 9958, 9959]}
+{"event_id": 854768, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 19:20:00", "end_date_time": "2019-10-20 19:20:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Trees and power lines were downed in the Panola community.", "ts_dict_index": [9972, 9973, 9974]}
+{"event_id": 854767, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 19:15:00", "end_date_time": "2019-10-20 19:15:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Multiple trees and power lines were downed in the De Berry community.", "ts_dict_index": [9975, 9976, 9977]}
+{"event_id": 854762, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-10-20 17:50:00", "end_date_time": "2019-10-20 17:50:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Tree tops were blown out southwest of Henderson.", "ts_dict_index": [9984, 9985, 9986]}
+{"event_id": 854766, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 18:57:00", "end_date_time": "2019-10-20 18:57:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. Trees were blown down blocking Highway 149 between Beckville and Carthage.", "ts_dict_index": [9978, 9979, 9980]}
+{"event_id": 811365, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-04-13 03:40:00", "end_date_time": "2019-04-13 03:40:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing numerous reports of damaging winds with several tornadoes across portions of East Texas. These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. A tree fell on a car on Highway 80 near FM 2199.", "ts_dict_index": [10020, 10021, 10022]}
+{"event_id": 1014567, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-12 20:14:00", "end_date_time": "2022-04-12 20:14:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. Multiple trees were downed South of Highway 84 west of Timpson.", "ts_dict_index": [10005, 10006, 10007]}
+{"event_id": 878139, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2020-02-05 18:04:00", "end_date_time": "2020-02-05 18:04:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked onto power lines.", "ts_dict_index": [10053, 10054, 10055]}
+{"event_id": 878154, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2020-02-05 17:41:00", "end_date_time": "2020-02-05 17:41:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down about one mile north-northwest of Sheffield.", "ts_dict_index": [10029, 10030, 10031]}
+{"event_id": 878185, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:54:00", "end_date_time": "2020-02-05 17:54:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down on Creekwood Circle in Florence.", "ts_dict_index": [10050, 10051, 10052]}
+{"event_id": 878159, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:48:00", "end_date_time": "2020-02-05 17:48:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down at Highway 157 at CR 9 in Underwood.", "ts_dict_index": [10038, 10039, 10040]}
+{"event_id": 878188, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:58:00", "end_date_time": "2020-02-05 17:58:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down at CR 159 near CR 136.", "ts_dict_index": [10062, 10063, 10064]}
+{"event_id": 878142, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 18:02:00", "end_date_time": "2020-02-05 18:02:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A large tree was down on Highway 101 north of CR 613.", "ts_dict_index": [10068, 10069, 10070]}
+{"event_id": 878184, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:45:00", "end_date_time": "2020-02-05 17:45:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. Trees were knocked down onto Highway 157 at CR 6 in Cloverdale.", "ts_dict_index": [10041, 10042, 10043]}
+{"event_id": 878134, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:45:00", "end_date_time": "2020-02-05 17:45:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked onto power lines across the CR 11 bridge north of CR 118.", "ts_dict_index": [10044, 10045, 10046]}
+{"event_id": 878162, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:52:00", "end_date_time": "2020-02-05 17:52:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree and power pole was knocked down with a power outage resulting.  This was at Chishom Road and Park Lane in Florence.", "ts_dict_index": [10032, 10033, 10034]}
+{"event_id": 878133, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:41:00", "end_date_time": "2020-02-05 17:41:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down in Oakland on CR 19, one-half mile north of CR 14. Time estimated by radar.", "ts_dict_index": [10047, 10048, 10049]}
+{"event_id": 878187, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:56:00", "end_date_time": "2020-02-05 17:56:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down on CR 31 at CR 171 in Center Star.", "ts_dict_index": [10077, 10078, 10079]}
+{"event_id": 878186, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 18:01:00", "end_date_time": "2020-02-05 18:01:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree and power lines were knocked down on CR 71 near CR 67 in Center Star.", "ts_dict_index": [10065, 10066, 10067]}
+{"event_id": 878140, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:57:00", "end_date_time": "2020-02-05 17:57:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. Power lines were also knocked down on Creekview Drive in Killen.", "ts_dict_index": [10074, 10075, 10076]}
+{"event_id": 878141, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 18:02:00", "end_date_time": "2020-02-05 18:02:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. Trees and power lines were knocked down between CR 414 and CR 67.", "ts_dict_index": [10071, 10072, 10073]}
+{"event_id": 878158, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:54:00", "end_date_time": "2020-02-05 17:54:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down on CR 25 in Green Hill.", "ts_dict_index": [10080, 10081, 10082]}
+{"event_id": 878138, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:58:00", "end_date_time": "2020-02-05 17:58:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. Trees were snapped and knocked down and a shed was damaged on CR 159. Report received via social media.", "ts_dict_index": [10059, 10060, 10061]}
+{"event_id": 1014562, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-12 20:02:00", "end_date_time": "2022-04-12 20:02:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. These storms eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas during the evening through the early morning hours of the 13th. Instances of large hail and damaging winds were reported from these storms, before they moved into North Louisiana during the early morning hours. The southern extent of this complex of storms eventually slowed as they became more parallel (west to east) to the extensive area of damaging winds, resulting in these storms developing/moving repeatedly over the same areas of Nacogdoches and Shelby Counties. Thus, instances of flash flooding were reported across these areas, as widespread rainfall amounts of three to in excess of five inches were observed. Additional showers and thunderstorms developed across East Texas during the mid-morning through the early afternoon hours of April 13th along a cold front, with some of these storms also becoming severe, downing trees across the area. These storms exited East Texas into Southwest Arkansas and North Louisiana during the early afternoon hours. A roof was blown off of a home in Mount Enterprise.", "ts_dict_index": [9996, 9997, 9998]}
+{"event_id": 878136, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2020-02-05 17:41:00", "end_date_time": "2020-02-05 17:41:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A power pole was knocked down.", "ts_dict_index": [10092, 10093, 10094]}
+{"event_id": 878137, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 18:01:00", "end_date_time": "2020-02-05 18:01:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. Trees were knocked down at the intersection of CR 478 and CR 71. Time estimated by radar.", "ts_dict_index": [10086, 10087, 10088]}
+{"event_id": 878183, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:54:00", "end_date_time": "2020-02-05 17:54:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down on CR 25 at CR 170.", "ts_dict_index": [10083, 10084, 10085]}
+{"event_id": 878135, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:48:00", "end_date_time": "2020-02-05 17:48:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A large tree was knocked down between Cloverdale and Petersville.  Report received via social media. Time estimated by radar.", "ts_dict_index": [10089, 10090, 10091]}
+{"event_id": 811368, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-04-13 03:50:00", "end_date_time": "2019-04-13 03:50:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing numerous reports of damaging winds with several tornadoes across portions of East Texas. These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. Numerous trees down on FM 1998, as well as Highway 80 near Scottsville. At least ten power poles were downed near Scottsville as well. Trees were also downed on the roadways near Karnack.", "ts_dict_index": [10017, 10018, 10019]}
+{"event_id": 878157, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2020-02-05 17:24:00", "end_date_time": "2020-02-05 17:24:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. Power lines were knocked down into the road.", "ts_dict_index": [10095, 10096, 10097]}
+{"event_id": 878147, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2020-02-05 18:51:00", "end_date_time": "2020-02-05 18:51:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. Trees were knocked down.", "ts_dict_index": [10098, 10099, 10100]}
+{"event_id": 878150, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2020-02-05 19:02:00", "end_date_time": "2020-02-05 19:02:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down.  Power flashes were observed nearby.", "ts_dict_index": [10101, 10102, 10103]}
+{"event_id": 976656, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-22 20:05:00", "end_date_time": "2021-07-22 20:05:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Social media photos and videos show several downed palo verde trees of varying sizes along Pinnacle Peak Road near 35th Avenue. Some of the palo verdes fell into the road. Timing estimated from radar. No injuries reported.", "ts_dict_index": [10107, 10108, 10109]}
+{"event_id": 976639, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-22 21:10:00", "end_date_time": "2021-07-22 21:10:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. A microburst caused significant damage in south Scottsdale with numerous downed trees of various sizes and with some falling on parked vehicles. At Scottsdale Road and Thomas Road one tree fell on top of two cars, damaging the frame and busting the window of one. Nearby at Thomas and 70th Street a carport at an apartment complex was destroyed with a portion of it collapsing on a parked SUV. Winds estimated around 60 mph based on damage reports in the affected area. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [10110, 10111, 10112]}
+{"event_id": 878161, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:48:00", "end_date_time": "2020-02-05 17:48:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down at CR 6 and C 16 in Central.", "ts_dict_index": [10035, 10036, 10037]}
+{"event_id": 881320, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2020-04-29 00:40:00", "end_date_time": "2020-04-29 00:40:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Several trees and power lines were downed.", "ts_dict_index": [10122, 10123, 10124]}
+{"event_id": 986969, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-22 16:00:00", "end_date_time": "2021-07-22 16:00:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Multiple RVs were damaged or displaced after strong to severe winds impacted the Sonoran Desert RV Park. 10 RVs were moved 5 to 6 feet and one was knocked over on its side. Additionally, one RV had windows broken and another had a cracked glass door. Winds estimated based on damage and timing based on radar. No injuries were reported.", "ts_dict_index": [10116, 10117, 10118]}
+{"event_id": 976648, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-22 21:25:00", "end_date_time": "2021-07-22 21:25:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. A microburst caused considerable damage from the McCormick Rach area and down to Scottsdale Road and McDonald Road with hundreds of downed trees and several downed power poles that caused a power outage to the area. The McCormick Ranch golf course had at least 220 large trees uprooted or snapped across the property. Several trees also fell on homes around the course. Course officials estimated the damage costs to the course at $600,000. At a shopping plaza on the southwest side of the course a palm tree fell onto a business, causing damage to the roof. Across Indian Bend Road to the south, McCormick-Stillman Railroad Park received extensive damage with several large trees, including pines, being uprooted or snapped across the park. Some of the toppled trees fell on park buildings and trains. At least 6 power poles were downed or snapped due to the winds with most of the poles along Scottsdale Road between Lincoln Drive and McDonald Drive. In this area 5 large trees were also uprooted with a couple of them being pine trees. Winds were estimated around 70-80 mph based on damage. Timing estimated from radar. There were no injuries.", "ts_dict_index": [10119, 10120, 10121]}
+{"event_id": 976655, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-22 20:15:00", "end_date_time": "2021-07-22 20:15:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. Photo of a large shallow-rooted tree that fell between two homes near 29th Avenue and Deer Valley Road and caused minor damage to both. Timing estimated from radar. No injuries reported.", "ts_dict_index": [10113, 10114, 10115]}
+{"event_id": 878160, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-05 17:53:00", "end_date_time": "2020-02-05 17:53:00", "narrative": "A strong influx of moisture, along with a potent upper level jet stream and incoming cold front brought multiple rounds of showers and thunderstorms, some heavy from the early morning of the 5th through the early morning of the 6th.  The first round yielded heavy rainfall in northwest Alabama through southern middle Tennessee during the early morning of the 5th.  A second round occurred with a line of thunderstorms during the late morning and midday hours.  Intense rainfall in a short period of time led to several instances of flash flooding of small creeks and streams.  Several roads were closed or barricaded as a result.||Then, a strong to severe line of thunderstorms developed in Mississippi during the afternoon of the 6th and rolled east through all of north Alabama and southern middle Tennessee during the evening hours. A supercell embedded along the line produced an EF-1 tornado in western Colbert County.  As the line progressed east, several reports of wind damage were received.  These storms also produced intense rainfall on top of already saturated grounds, producing flash flooding, followed by areal flooding that last through the entire day and into the nighttime hours of the 6th.  Once again, several roads became impassible and were closed or barricaded.||This was followed by another band of showers and thunderstorms that lifted northeast from west central and central Alabama through far northeast Alabama during the early morning hours of the 6th. A tree was knocked down on Lawrence Avenue in Florence.", "ts_dict_index": [10056, 10057, 10058]}
+{"event_id": 881311, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-29 00:01:00", "end_date_time": "2020-04-29 00:01:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A tree was blown down across Highway 3 on the north side of Bossier City.", "ts_dict_index": [10131, 10132, 10133]}
+{"event_id": 855060, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-10-20 20:19:00", "end_date_time": "2019-10-20 20:19:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. Trees and power lines were downed in both the Dogwood and Stockwell Place subdivisions in East Bossier City.", "ts_dict_index": [10152, 10153, 10154]}
+{"event_id": 881316, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-29 00:16:00", "end_date_time": "2020-04-29 00:16:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A picture was posted to social media of a large tree that was blown down at the intersection of Creswell Avenue and Jordan Street in Shreveport.", "ts_dict_index": [10128, 10129, 10130]}
+{"event_id": 881315, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-29 00:15:00", "end_date_time": "2020-04-29 00:15:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A tree was blown down on a home on Dudley Drive. Several other trees were downed across the city of Shreveport.", "ts_dict_index": [10125, 10126, 10127]}
+{"event_id": 855064, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-20 19:50:00", "end_date_time": "2019-10-20 19:50:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. Trees were downed on Shirley Francis Road between Audubon Meadow Drive and Al Bourland Drive.", "ts_dict_index": [10155, 10156, 10157]}
+{"event_id": 855063, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-20 19:41:00", "end_date_time": "2019-10-20 19:41:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. Trees were downed near the intersection of Buncombe Road and Cook Road.", "ts_dict_index": [10158, 10159, 10160]}
+{"event_id": 881319, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2020-04-29 00:26:00", "end_date_time": "2020-04-29 00:26:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. Several Trees were blown down north of Farmerville.", "ts_dict_index": [10137, 10138, 10139]}
+{"event_id": 881321, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2020-04-29 00:42:00", "end_date_time": "2020-04-29 00:42:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A vehicle waiting for the road to be cleared of fallen trees and power lines had another tree fall on it.", "ts_dict_index": [10149, 10150, 10151]}
+{"event_id": 881327, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2020-04-29 01:28:00", "end_date_time": "2020-04-29 01:28:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A tree was downed in Natchitoches.", "ts_dict_index": [10146, 10147, 10148]}
+{"event_id": 881314, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-04-29 00:13:00", "end_date_time": "2020-04-29 00:13:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A tree was blown down on a car along Highway 164 near Doyline.", "ts_dict_index": [10134, 10135, 10136]}
+{"event_id": 881310, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-04-28 23:45:00", "end_date_time": "2020-04-28 23:45:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A tree was blown down along Highway 371 in Sarepta.", "ts_dict_index": [10143, 10144, 10145]}
+{"event_id": 881313, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-04-29 00:10:00", "end_date_time": "2020-04-29 00:10:00", "narrative": "A weak shortwave trough shifted east across East Texas and North Louisiana during the morning hours of April 28th, where large scale forcing contributed to the development of showers and thunderstorms over East Texas and North Louisiana. Cold air aloft associated with this trough resulted in steep lapse rates such that isolated severe thunderstorms developed over portions of East Texas throughout the morning and afternoon, where instances of large hail were reported. These storms diminished during the late afternoon, but a deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. These storms exited Deep East Texas and the southern sections of Northcentral Louisiana into Southeast Texas and South Louisiana by 4 AM. A tree was blown down across Highway 518 east of Minden.", "ts_dict_index": [10140, 10141, 10142]}
+{"event_id": 855066, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-20 20:00:00", "end_date_time": "2019-10-20 20:00:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. Trees were downed on Lorraine Drive between Ridgeway Avenue and Hampton Lane.", "ts_dict_index": [10182, 10183, 10184]}
+{"event_id": 855058, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-20 19:52:00", "end_date_time": "2019-10-20 19:52:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. A tree fell onto a house in the Queensboro area of Shreveport.", "ts_dict_index": [10173, 10174, 10175]}
+{"event_id": 855065, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-20 19:49:00", "end_date_time": "2019-10-20 19:49:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. Trees were downed on Shirley Francis Road between Simpson Road and Oak Creek Trail.", "ts_dict_index": [10179, 10180, 10181]}
+{"event_id": 855061, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-10-20 20:20:00", "end_date_time": "2019-10-20 20:20:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. Trees were downed with damage to roofs in the Dogwood subdivision in East Bossier City.", "ts_dict_index": [10164, 10165, 10166]}
+{"event_id": 855062, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-20 19:52:00", "end_date_time": "2019-10-20 19:52:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. A couple of trees were downed along Hollywood Avenue near the entrance to the UPS and FedEx Shipping Center.", "ts_dict_index": [10161, 10162, 10163]}
+{"event_id": 855004, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-20 20:02:00", "end_date_time": "2019-10-20 20:02:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. A power line was blown down onto a home in the area of Montana Street and MLK Drive in North Shreveport, which sparked a fire in the attic. The resident was able to safely escape the home.", "ts_dict_index": [10167, 10168, 10169]}
+{"event_id": 855059, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-20 19:55:00", "end_date_time": "2019-10-20 19:55:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. A 63 mph wind gust was measured at the Shreveport Regional Airport.", "ts_dict_index": [10170, 10171, 10172]}
+{"event_id": 925448, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:23:00", "end_date_time": "2020-11-30 15:23:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Wires were downed near Ship Rd in Exton. Time estimated from radar.", "ts_dict_index": [10185, 10186, 10187]}
+{"event_id": 925453, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:28:00", "end_date_time": "2020-11-30 15:28:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree and wires were downed near Woodview Rd in Malvern. Time estimated from radar.", "ts_dict_index": [10191, 10192, 10193]}
+{"event_id": 925433, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 12:49:00", "end_date_time": "2020-11-30 12:49:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Several trees and limbs were downed near the intersection of Township Line Rd and Mowere Rd. Glass windows were broken. Time estimated from radar.", "ts_dict_index": [10188, 10189, 10190]}
+{"event_id": 925452, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:28:00", "end_date_time": "2020-11-30 15:28:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near Woodland Dr in Malvern. Time estimated from radar.", "ts_dict_index": [10194, 10195, 10196]}
+{"event_id": 976643, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-22 21:20:00", "end_date_time": "2021-07-22 21:20:00", "narrative": "Strong to severe thunderstorms developed in an unstable atmosphere in the afternoon of the 22nd. Storms initially developed over the high terrain of northern and eastern Arizona as well as near the Table Top mesa area south of Phoenix. High DCAPE promoted strong thunderstorm downbursts. The downbursts generated outflows that progressed into the greater Phoenix metro area and led to the development of additional scattered thunderstorm. The thunderstorms in the metro area produced damaging winds that led to numerous downed trees, downed power poles, and other property damage. The storms were also nearly stationary, under weak steering flow, and produced very heavy rainfall with rain rates around 1.5-2.0 inches per hour and briefly higher in the strongest storms. This led to considerable flash flooding around Phoenix with several road closure and significant flow in major washes. Even after the strongest storms in Phoenix subsided in the late evening of the 22nd, areas of moderate to heavy rain continued from northeast to southwest through the night and through mid-afternoon on the 23rd. The continued rain through the 23rd was aided by a strengthening diffluent flow regime between the monsoon high to the north and a retrograding upper low moving west through New Mexico. Additional significant flash flooding was observed on the 23rd, mostly in the foothills north of the Phoenix metro, with many road closures, flowing washes and creeks, and some water rescues. A microburst caused significant damage in Downtown Scottsdale with numerous toppled or snapped trees. Amongst the received reports, half a dozen trees were reportedly uprooted around Fashion Square outlet mall. At least a couple trees fell on vehicles. Two palm trees in front of the Galleria Corporate Center were snapped in half. A carport at the San Marin apartment complex was blown over and caused damage to the several cars parked underneath. A media report showed a restaraunt had a partial roof torn off while customers were inside. In all there were like many more unreported damages with unkown costs. Winds were estimated around 60-65 mph in the downtown area based on damage. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [10104, 10105, 10106]}
+{"event_id": 925460, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-30 12:52:00", "end_date_time": "2020-11-30 12:54:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A damaging wind event started in the area of College|Avenue at Joan Drive around 12:52 PM on November 30, 2020. Various|items of yard and patio furniture were tossed about, and a few trees|were downed or damaged. At least two houses sustained partial losses|of shingles and/or siding, and a couple of fences were destroyed.|About a mile to the northeast, an HVAC unit was blown across the roof|of the Perkiomen Valley Middle School East. A local fire chief reported|several trees uprooted on nearby Wartman Road. It is estimated the|damaging winds ended in this area near or before reaching Bridge Street,|or near Lodal Creek, as no additional damage was reported downstream of|Wartman Road. Radar data indicated a rear-inflow jet descending in the|area resulting in a narrow swath of wind damage, and some resident accounts suggested this may have been a tornado. Howeve, available evidence was not clear regarding a brief|tornado touchdown and therefore the damage is designated as straight-line|wind. We extend our thanks to the local residents who provided accounts|of damage for their assistance in this survey, which was conducted remotely.", "ts_dict_index": [10215, 10216, 10217]}
+{"event_id": 925432, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-30 15:46:00", "end_date_time": "2020-11-30 15:46:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near Maple Ave in Harleysville. Time estimated from radar.", "ts_dict_index": [10236, 10237, 10238]}
+{"event_id": 925463, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-30 15:44:00", "end_date_time": "2020-11-30 15:44:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near Tyson Rd in Skippack Twp. Time estimated from radar.", "ts_dict_index": [10233, 10234, 10235]}
+{"event_id": 925450, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:25:00", "end_date_time": "2020-11-30 15:25:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Wires were downed near Exton Square Parkway. Time estimated from radar.", "ts_dict_index": [10245, 10246, 10247]}
+{"event_id": 925436, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:19:00", "end_date_time": "2020-11-30 15:19:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree was downed on US-1 near PA-52. Time estimated from radar.", "ts_dict_index": [10218, 10219, 10220]}
+{"event_id": 925464, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-30 15:44:00", "end_date_time": "2020-11-30 15:44:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near Old Morris Rd in Lederach. Time estimated from radar.", "ts_dict_index": [10230, 10231, 10232]}
+{"event_id": 925437, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:19:00", "end_date_time": "2020-11-30 15:19:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A large tree was downed on Lucky Hill Rd. Time estimated from radar.", "ts_dict_index": [10212, 10213, 10214]}
+{"event_id": 925455, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:29:00", "end_date_time": "2020-11-30 15:29:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree and wires were downed near Hilltop Rd in Charlestown. Time estimated from radar.", "ts_dict_index": [10239, 10240, 10241]}
+{"event_id": 925451, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:26:00", "end_date_time": "2020-11-30 15:26:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree and wires were downed near Pickwick Ln in Malvern. Time estimated from radar.", "ts_dict_index": [10242, 10243, 10244]}
+{"event_id": 925456, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-30 15:32:00", "end_date_time": "2020-11-30 15:32:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near Clahor Ave. Time estimated from radar.", "ts_dict_index": [10200, 10201, 10202]}
+{"event_id": 925457, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:33:00", "end_date_time": "2020-11-30 15:33:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Wires were downed near the intersection of Waterloo Rd and Highland Ave. Time estimated from radar.", "ts_dict_index": [10203, 10204, 10205]}
+{"event_id": 925459, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:36:00", "end_date_time": "2020-11-30 15:36:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near Freemont St in Phoenixville. Time estimated from radar.", "ts_dict_index": [10209, 10210, 10211]}
+{"event_id": 925458, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:33:00", "end_date_time": "2020-11-30 15:33:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Several trees were downed on Dawson Dr. Time estimated from radar.", "ts_dict_index": [10206, 10207, 10208]}
+{"event_id": 925435, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:15:00", "end_date_time": "2020-11-30 15:15:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Wires were downed at the intersection of Skelp Level Rd and Spencer Dr. Time estimated from radar.", "ts_dict_index": [10224, 10225, 10226]}
+{"event_id": 925449, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:23:00", "end_date_time": "2020-11-30 15:23:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree was downed on Shetland Dr. Time estimated from radar.", "ts_dict_index": [10248, 10249, 10250]}
+{"event_id": 925466, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-11-30 15:47:00", "end_date_time": "2020-11-30 15:47:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree was downed into wires near Oak Ln in Upper Milford Twp. Time estimated from radar.", "ts_dict_index": [10221, 10222, 10223]}
+{"event_id": 855003, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-20 19:52:00", "end_date_time": "2019-10-20 19:52:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. Several large tree limbs were snapped in front of the National Weather Service Forecast Office in Shreveport. Other smaller limbs were downed over the grounds as well.", "ts_dict_index": [10176, 10177, 10178]}
+{"event_id": 925478, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-11-30 16:15:00", "end_date_time": "2020-11-30 16:15:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near Mechanicsville Rd. Time estimated from radar.", "ts_dict_index": [10251, 10252, 10253]}
+{"event_id": 925477, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-11-30 16:12:00", "end_date_time": "2020-11-30 16:12:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree and fence were knocked down on a property in Chalfont. Time estimated from radar.", "ts_dict_index": [10260, 10261, 10262]}
+{"event_id": 925447, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:23:00", "end_date_time": "2020-11-30 15:23:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree was downed near the intersection of Wilmington Pike and West Pleasant Grove Rd. Time estimated from radar.", "ts_dict_index": [10254, 10255, 10256]}
+{"event_id": 925446, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:22:00", "end_date_time": "2020-11-30 15:22:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Wires were downed near the intersection of Pocopson Rd and Chandler Rd. Time estimated from radar.", "ts_dict_index": [10257, 10258, 10259]}
+{"event_id": 925445, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:21:00", "end_date_time": "2020-11-30 15:21:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree and wires were downed on Ashbridge St. Time estimated from radar.", "ts_dict_index": [10266, 10267, 10268]}
+{"event_id": 925444, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:21:00", "end_date_time": "2020-11-30 15:21:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Wires were downed near the intersection of Fairville Rd and Cossart Dr. Time estimated from radar.", "ts_dict_index": [10269, 10270, 10271]}
+{"event_id": 925434, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:15:00", "end_date_time": "2020-11-30 15:15:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree and wires were downed near Marlborough Rd. Time estimated from radar.", "ts_dict_index": [10227, 10228, 10229]}
+{"event_id": 925472, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-11-30 15:53:00", "end_date_time": "2020-11-30 15:53:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree was downed in wires near Roudenbush Rd. Time estimated from radar.", "ts_dict_index": [10290, 10291, 10292]}
+{"event_id": 925473, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-11-30 15:55:00", "end_date_time": "2020-11-30 15:55:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near Blackburn Dr in Chalfont. Time estimated from radar.", "ts_dict_index": [10287, 10288, 10289]}
+{"event_id": 925439, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:19:00", "end_date_time": "2020-11-30 15:19:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near North Creek Rd and near East Bradford Twp. Time estimated from radar.", "ts_dict_index": [10296, 10297, 10298]}
+{"event_id": 925443, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:20:00", "end_date_time": "2020-11-30 15:20:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Wires were downed near Frame Ave and Mulberry Dr. Time estimated from radar.", "ts_dict_index": [10278, 10279, 10280]}
+{"event_id": 925474, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-30 15:59:00", "end_date_time": "2020-11-30 15:59:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A utility was downed on Limekiln Pike near Fairway Rd. Time estimated from radar.", "ts_dict_index": [10275, 10276, 10277]}
+{"event_id": 925440, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:19:00", "end_date_time": "2020-11-30 15:19:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near Lincoln Ave in Downingtown. Time estimated from radar.", "ts_dict_index": [10293, 10294, 10295]}
+{"event_id": 925442, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:20:00", "end_date_time": "2020-11-30 15:20:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree and wires were downed near Williamsburg Dr in Pocopson Twp. Time estimated from radar.", "ts_dict_index": [10284, 10285, 10286]}
+{"event_id": 925454, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-30 15:28:00", "end_date_time": "2020-11-30 15:28:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Multiple large trees were uprooted in Phoenixville. Time estimated from radar.", "ts_dict_index": [10281, 10282, 10283]}
+{"event_id": 1027560, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-05-26 15:26:00", "end_date_time": "2022-05-26 15:26:00", "narrative": "Thunderstorms broke out across east Kentucky May 26th thanks to a mature low pressure system moving into the Ohio Valley from the west. This system initially pulled a warm front through eastern Kentucky in the evening, and most of the severe convection was associated with the approach and passage of this warm front. A cold front was then dragged across the region overnight and into the morning. Instability was not overly impressive going into this event, around 1000-1500 J/kg of CAPE. However, storms that formed were able to take advantage of the roughly 40 kts of effective shear over the area and organize into more multicellular and linear structures. The limited CAPE profile meant a more limited hail threat, leaving strong to damaging wind gusts as the primary threat, though tornadoes were not able to be ruled out. Even though storm motions were fairly swift, given the abundant moisture associated with this system, there was also a threat for flash flooding if any training set up or an area was hit multiple times. Several warnings, including Severe Thunderstorm, Flash Flood, and Tornado, were issued that evening, mainly across our most western and southwestern counties. Multiple reports of damaging wind leading to downed trees were received across the same areas, along with a couple of reports of water flowing over roadways. There were some wind reports within the Tornado Warnings, but no tornadoes were confirmed in the JKL area. Tree damage, including uprooted or snapped trees, was reported at this location.", "ts_dict_index": [10302, 10303, 10304]}
+{"event_id": 1027562, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-05-26 15:32:00", "end_date_time": "2022-05-26 15:32:00", "narrative": "Thunderstorms broke out across east Kentucky May 26th thanks to a mature low pressure system moving into the Ohio Valley from the west. This system initially pulled a warm front through eastern Kentucky in the evening, and most of the severe convection was associated with the approach and passage of this warm front. A cold front was then dragged across the region overnight and into the morning. Instability was not overly impressive going into this event, around 1000-1500 J/kg of CAPE. However, storms that formed were able to take advantage of the roughly 40 kts of effective shear over the area and organize into more multicellular and linear structures. The limited CAPE profile meant a more limited hail threat, leaving strong to damaging wind gusts as the primary threat, though tornadoes were not able to be ruled out. Even though storm motions were fairly swift, given the abundant moisture associated with this system, there was also a threat for flash flooding if any training set up or an area was hit multiple times. Several warnings, including Severe Thunderstorm, Flash Flood, and Tornado, were issued that evening, mainly across our most western and southwestern counties. Multiple reports of damaging wind leading to downed trees were received across the same areas, along with a couple of reports of water flowing over roadways. There were some wind reports within the Tornado Warnings, but no tornadoes were confirmed in the JKL area. Trees were blown down onto powerlines on Etna Road.", "ts_dict_index": [10299, 10300, 10301]}
+{"event_id": 925467, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-30 15:47:00", "end_date_time": "2020-11-30 15:47:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree was downed on Swamp Creek Rd near the Price Rd intersection, closing the road. Time estimated from radar.", "ts_dict_index": [10197, 10198, 10199]}
+{"event_id": 940447, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-03-27 19:15:00", "end_date_time": "2021-03-27 19:15:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track across East Texas, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area through the early morning hours of the 28th. Power lines were downed just north of Oil City.", "ts_dict_index": [10314, 10315, 10316]}
+{"event_id": 1096317, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2023-05-07 21:20:00", "end_date_time": "2023-05-07 21:20:00", "narrative": "Middle to upper level winds were out of the west to southwest, and an upper level disturbance moved over the region from Colorado by the early evening hours. There was a weak surface low to the south with an inverted trough axis over portions of north central Kansas and south central Nebraska extending north of the low. This trough axis set up a frontal zone across Nebraska and Kansas. High based thunderstorms developed to the west of the area along a shortwave trough then moved eastward and encountered increased instability. Mixed layer CAPE was around 1000 to 2000 J/kg and deep layer wind shear was around 50 to 60 knots. There was a slight risk of severe storms from the Storm Prediction Center. ||Storms began developing to the west and northwest of the area during the afternoon hours. A cluster of storms moved in from the west and began impacting north central Kansas around 7 pm. This cluster of storms continued moving eastward during the evening hours and extended northward into portions of southern Nebraska. The cluster exited the area around 10:30 pm as it continued tracking eastward across Nebraska. There were several strong to severe wind gusts across north central Kansas and one report of golfball sized hail. One report of thunderstorm wind damage occurred in Mitchell County. The storms went on to produce a few severe wind gusts in Nuckolls and Thayer Counties in Nebraska as well as a wind damage report in Thayer County. Wind gusts estimated to be near 70 MPH resulted in an overturned irrigation pivot four miles east of Bruning.", "ts_dict_index": [10308, 10309, 10310]}
+{"event_id": 1096316, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2023-05-07 20:58:00", "end_date_time": "2023-05-07 20:58:00", "narrative": "Middle to upper level winds were out of the west to southwest, and an upper level disturbance moved over the region from Colorado by the early evening hours. There was a weak surface low to the south with an inverted trough axis over portions of north central Kansas and south central Nebraska extending north of the low. This trough axis set up a frontal zone across Nebraska and Kansas. High based thunderstorms developed to the west of the area along a shortwave trough then moved eastward and encountered increased instability. Mixed layer CAPE was around 1000 to 2000 J/kg and deep layer wind shear was around 50 to 60 knots. There was a slight risk of severe storms from the Storm Prediction Center. ||Storms began developing to the west and northwest of the area during the afternoon hours. A cluster of storms moved in from the west and began impacting north central Kansas around 7 pm. This cluster of storms continued moving eastward during the evening hours and extended northward into portions of southern Nebraska. The cluster exited the area around 10:30 pm as it continued tracking eastward across Nebraska. There were several strong to severe wind gusts across north central Kansas and one report of golfball sized hail. One report of thunderstorm wind damage occurred in Mitchell County. The storms went on to produce a few severe wind gusts in Nuckolls and Thayer Counties in Nebraska as well as a wind damage report in Thayer County. A wind gust of 60 MPH was measured by a mesonet station located three miles south-southeast of Gilead.", "ts_dict_index": [10305, 10306, 10307]}
+{"event_id": 1096315, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2023-05-07 20:45:00", "end_date_time": "2023-05-07 20:45:00", "narrative": "Middle to upper level winds were out of the west to southwest, and an upper level disturbance moved over the region from Colorado by the early evening hours. There was a weak surface low to the south with an inverted trough axis over portions of north central Kansas and south central Nebraska extending north of the low. This trough axis set up a frontal zone across Nebraska and Kansas. High based thunderstorms developed to the west of the area along a shortwave trough then moved eastward and encountered increased instability. Mixed layer CAPE was around 1000 to 2000 J/kg and deep layer wind shear was around 50 to 60 knots. There was a slight risk of severe storms from the Storm Prediction Center. ||Storms began developing to the west and northwest of the area during the afternoon hours. A cluster of storms moved in from the west and began impacting north central Kansas around 7 pm. This cluster of storms continued moving eastward during the evening hours and extended northward into portions of southern Nebraska. The cluster exited the area around 10:30 pm as it continued tracking eastward across Nebraska. There were several strong to severe wind gusts across north central Kansas and one report of golfball sized hail. One report of thunderstorm wind damage occurred in Mitchell County. The storms went on to produce a few severe wind gusts in Nuckolls and Thayer Counties in Nebraska as well as a wind damage report in Thayer County. A cattle trailer was overturned one mile east of the Thayer-Nuckolls County line on Highway 8. Wind gusts were estimated to be near 70 MPH, with measured gust of 72 MPH occurring approximately 4 miles to the northwest of this damage report.", "ts_dict_index": [10311, 10312, 10313]}
+{"event_id": 925476, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-11-30 16:10:00", "end_date_time": "2020-11-30 16:10:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. Trees and wires were downed near Church School Rd and Fell Rd in Doylestown. Time estimated from radar.", "ts_dict_index": [10263, 10264, 10265]}
+{"event_id": 940444, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-03-27 21:52:00", "end_date_time": "2021-03-27 21:52:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track across East Texas, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area through the early morning hours of the 28th. A large tree was blown down completely blocking Buncombe Road at Woolworth Road.", "ts_dict_index": [10317, 10318, 10319]}
+{"event_id": 940442, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-03-27 19:16:00", "end_date_time": "2021-03-27 19:16:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track across East Texas, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area through the early morning hours of the 28th. Trees were blown down on Belcher Oil City Road.", "ts_dict_index": [10320, 10321, 10322]}
+{"event_id": 842453, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-07-20 16:18:00", "end_date_time": "2019-07-20 16:18:00", "narrative": "The atmosphere was juiced so to speak ahead of a cold front sliding into the region. MUCAPE values very quickly approached and exceeded 4000 J/kg by mid-morning. With the cold front and previous storm outflows the impetus for new convection, discrete storms were not expected, with the prevailing storm type being the linear or quasi-linear convective system (QLCS) variety. Additional support for the QLCS mode was seen with, once again the cold frontal and outflow forcing, highly unstable atmosphere, and little to no convective inhibition.  Additional support for strong winds was seen with DCAPE values in excess of 1500 J/kg across much of the area  Once a system began to produce a decent cold pool, there would be little to prevent it from progressing. ||That was evident in Iowa as two distinct QLCSs moved through. First in the morning hours across northern Iowa, and second during the late morning through evening hours from central Iowa and on toward south central and southeast Iowa. In both cases, damaging winds widely prevailed. Across northern Iowa the gust front roared out ahead of the line of convection, continuing to produce severe wind reports in areas of no storms well to the south and east. In central and southeast Iowa, widespread reports of 60 to 70 mph winds and various tree damage (from large limbs to entire trees) were received along a path from roughly Perry, IA through Ottumwa, IA. Iowa DOT reported portable message boards blown over. Time estimated from radar.", "ts_dict_index": [10329, 10330, 10331]}
+{"event_id": 842452, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-07-20 16:15:00", "end_date_time": "2019-07-20 16:15:00", "narrative": "The atmosphere was juiced so to speak ahead of a cold front sliding into the region. MUCAPE values very quickly approached and exceeded 4000 J/kg by mid-morning. With the cold front and previous storm outflows the impetus for new convection, discrete storms were not expected, with the prevailing storm type being the linear or quasi-linear convective system (QLCS) variety. Additional support for the QLCS mode was seen with, once again the cold frontal and outflow forcing, highly unstable atmosphere, and little to no convective inhibition.  Additional support for strong winds was seen with DCAPE values in excess of 1500 J/kg across much of the area  Once a system began to produce a decent cold pool, there would be little to prevent it from progressing. ||That was evident in Iowa as two distinct QLCSs moved through. First in the morning hours across northern Iowa, and second during the late morning through evening hours from central Iowa and on toward south central and southeast Iowa. In both cases, damaging winds widely prevailed. Across northern Iowa the gust front roared out ahead of the line of convection, continuing to produce severe wind reports in areas of no storms well to the south and east. In central and southeast Iowa, widespread reports of 60 to 70 mph winds and various tree damage (from large limbs to entire trees) were received along a path from roughly Perry, IA through Ottumwa, IA. Public reported a resident shed tipped over. Time estimated from radar.", "ts_dict_index": [10332, 10333, 10334]}
+{"event_id": 842456, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-07-20 16:23:00", "end_date_time": "2019-07-20 16:23:00", "narrative": "The atmosphere was juiced so to speak ahead of a cold front sliding into the region. MUCAPE values very quickly approached and exceeded 4000 J/kg by mid-morning. With the cold front and previous storm outflows the impetus for new convection, discrete storms were not expected, with the prevailing storm type being the linear or quasi-linear convective system (QLCS) variety. Additional support for the QLCS mode was seen with, once again the cold frontal and outflow forcing, highly unstable atmosphere, and little to no convective inhibition.  Additional support for strong winds was seen with DCAPE values in excess of 1500 J/kg across much of the area  Once a system began to produce a decent cold pool, there would be little to prevent it from progressing. ||That was evident in Iowa as two distinct QLCSs moved through. First in the morning hours across northern Iowa, and second during the late morning through evening hours from central Iowa and on toward south central and southeast Iowa. In both cases, damaging winds widely prevailed. Across northern Iowa the gust front roared out ahead of the line of convection, continuing to produce severe wind reports in areas of no storms well to the south and east. In central and southeast Iowa, widespread reports of 60 to 70 mph winds and various tree damage (from large limbs to entire trees) were received along a path from roughly Perry, IA through Ottumwa, IA. Public reported a large 6 to 8 inch tree branch snapped. This is a delayed report and time estimated from radar.", "ts_dict_index": [10338, 10339, 10340]}
+{"event_id": 842472, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-07-20 18:00:00", "end_date_time": "2019-07-20 18:00:00", "narrative": "The atmosphere was juiced so to speak ahead of a cold front sliding into the region. MUCAPE values very quickly approached and exceeded 4000 J/kg by mid-morning. With the cold front and previous storm outflows the impetus for new convection, discrete storms were not expected, with the prevailing storm type being the linear or quasi-linear convective system (QLCS) variety. Additional support for the QLCS mode was seen with, once again the cold frontal and outflow forcing, highly unstable atmosphere, and little to no convective inhibition.  Additional support for strong winds was seen with DCAPE values in excess of 1500 J/kg across much of the area  Once a system began to produce a decent cold pool, there would be little to prevent it from progressing. ||That was evident in Iowa as two distinct QLCSs moved through. First in the morning hours across northern Iowa, and second during the late morning through evening hours from central Iowa and on toward south central and southeast Iowa. In both cases, damaging winds widely prevailed. Across northern Iowa the gust front roared out ahead of the line of convection, continuing to produce severe wind reports in areas of no storms well to the south and east. In central and southeast Iowa, widespread reports of 60 to 70 mph winds and various tree damage (from large limbs to entire trees) were received along a path from roughly Perry, IA through Ottumwa, IA. Amateur radio reported a large tree down, 20 to 30 feet tall and about 6 inches in diameter. Reported location at 142nd and Lakeview, in Clive.", "ts_dict_index": [10323, 10324, 10325]}
+{"event_id": 842451, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-07-20 16:15:00", "end_date_time": "2019-07-20 16:15:00", "narrative": "The atmosphere was juiced so to speak ahead of a cold front sliding into the region. MUCAPE values very quickly approached and exceeded 4000 J/kg by mid-morning. With the cold front and previous storm outflows the impetus for new convection, discrete storms were not expected, with the prevailing storm type being the linear or quasi-linear convective system (QLCS) variety. Additional support for the QLCS mode was seen with, once again the cold frontal and outflow forcing, highly unstable atmosphere, and little to no convective inhibition.  Additional support for strong winds was seen with DCAPE values in excess of 1500 J/kg across much of the area  Once a system began to produce a decent cold pool, there would be little to prevent it from progressing. ||That was evident in Iowa as two distinct QLCSs moved through. First in the morning hours across northern Iowa, and second during the late morning through evening hours from central Iowa and on toward south central and southeast Iowa. In both cases, damaging winds widely prevailed. Across northern Iowa the gust front roared out ahead of the line of convection, continuing to produce severe wind reports in areas of no storms well to the south and east. In central and southeast Iowa, widespread reports of 60 to 70 mph winds and various tree damage (from large limbs to entire trees) were received along a path from roughly Perry, IA through Ottumwa, IA. Polk County Emergency Management reported 4 inch tree branches down.", "ts_dict_index": [10341, 10342, 10343]}
+{"event_id": 842457, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-07-20 16:24:00", "end_date_time": "2019-07-20 16:24:00", "narrative": "The atmosphere was juiced so to speak ahead of a cold front sliding into the region. MUCAPE values very quickly approached and exceeded 4000 J/kg by mid-morning. With the cold front and previous storm outflows the impetus for new convection, discrete storms were not expected, with the prevailing storm type being the linear or quasi-linear convective system (QLCS) variety. Additional support for the QLCS mode was seen with, once again the cold frontal and outflow forcing, highly unstable atmosphere, and little to no convective inhibition.  Additional support for strong winds was seen with DCAPE values in excess of 1500 J/kg across much of the area  Once a system began to produce a decent cold pool, there would be little to prevent it from progressing. ||That was evident in Iowa as two distinct QLCSs moved through. First in the morning hours across northern Iowa, and second during the late morning through evening hours from central Iowa and on toward south central and southeast Iowa. In both cases, damaging winds widely prevailed. Across northern Iowa the gust front roared out ahead of the line of convection, continuing to produce severe wind reports in areas of no storms well to the south and east. In central and southeast Iowa, widespread reports of 60 to 70 mph winds and various tree damage (from large limbs to entire trees) were received along a path from roughly Perry, IA through Ottumwa, IA. Iowa DOT reported trees down at the Iowa DOT facility in Ankeny, including small 4 to 6 inch diameter trees snapped and blown down. This is a delayed report and time estimated from radar.", "ts_dict_index": [10335, 10336, 10337]}
+{"event_id": 925475, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-11-30 16:06:00", "end_date_time": "2020-11-30 16:06:00", "narrative": "A complex storm system affected the mid-Atlantic on November 30, 2020. Developing low pressure over the Southeast US began to interact and phase with a clipper system over the Great Lakes, leading to a steadily intensifying low tracking northward along the Appalachians. This would become the primary low pressure system, which moved into Pennsylvania by the afternoon of the 30th. Ahead of the low, a warm front pushed through the mid-Atlantic and brought a period of rain with embedded thunder during the morning and early afternoon. By later in the day, a cold front began to approach. While increasing mid-level dry air was an inhibiting factor, the development of some sunshine after the earlier rain helped some modest instability to develop as surface temperatures rose well above seasonal normal. Combined with strong forcing and very strong wind fields in the narrow warm sector of the intensifying and highly dynamic low, convection developed ahead of the cold front. The combination of these factors led to a spatially limited but considerably impactful severe weather event over portions of eastern Pennsylvania, New Jersey, the Eastern Shore of Maryland, and northern Delaware. A number of instances of damaging wind as well as a couple of tornadoes occurred in the region. This event was also noteworthy in that despite being a late season event, some of the stronger convective elements were comparable in depth to typical mid-summer convection. A tree and wires were downed near Sinkler Rd in Neshaminy. Time estimated from radar.", "ts_dict_index": [10272, 10273, 10274]}
+{"event_id": 1111970, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-07-04 19:50:00", "end_date_time": "2023-07-04 19:50:00", "narrative": "An upper level trough was over the northern Rocky Mountains and Northern Plains and was bringing a cold front south through Nebraska during the afternoon and evening hours of Independence Day. Temperatures heated up in advance of the front with dewpoints mostly in the 60s. A very moist and unstable atmosphere was present. CAPE values were generally near 4,000 J/kg ahead of the front, and 0 to 6 km wind shear values were around 35 knots. Mid-level lapse rates were generally 7 to 8 degrees C/km. ||Isolated showers and storms were moving across portions of south central Nebraska during the early to mid-afternoon hours. This activity did not produce any severe weather. The main storm activity developed late in the afternoon into the evening hours and was associated with the cold front moving through Nebraska. Storms began developing in central Nebraska in the late afternoon and early evening hours. Then storms developed in south central Nebraska and formed a line with the storms in the central part of the state. The storms in central Nebraska moved southeast during the evening hours while the storms in the south central part of the state remained fairly stationary. The storms produced large hail and wind gusts of 58 to 66 mph between 5:30 PM CDT and 9 PM CDT. The largest hail reported was up to 2.50 inches and was reported in Webster, Fillmore, and Thayer Counties. Emergency management estimated wind gusts near 60 MPH.", "ts_dict_index": [10347, 10348, 10349]}
+{"event_id": 1111955, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-07-04 18:41:00", "end_date_time": "2023-07-04 18:55:00", "narrative": "An upper level trough was over the northern Rocky Mountains and Northern Plains and was bringing a cold front south through Nebraska during the afternoon and evening hours of Independence Day. Temperatures heated up in advance of the front with dewpoints mostly in the 60s. A very moist and unstable atmosphere was present. CAPE values were generally near 4,000 J/kg ahead of the front, and 0 to 6 km wind shear values were around 35 knots. Mid-level lapse rates were generally 7 to 8 degrees C/km. ||Isolated showers and storms were moving across portions of south central Nebraska during the early to mid-afternoon hours. This activity did not produce any severe weather. The main storm activity developed late in the afternoon into the evening hours and was associated with the cold front moving through Nebraska. Storms began developing in central Nebraska in the late afternoon and early evening hours. Then storms developed in south central Nebraska and formed a line with the storms in the central part of the state. The storms in central Nebraska moved southeast during the evening hours while the storms in the south central part of the state remained fairly stationary. The storms produced large hail and wind gusts of 58 to 66 mph between 5:30 PM CDT and 9 PM CDT. The largest hail reported was up to 2.50 inches and was reported in Webster, Fillmore, and Thayer Counties. Peak wind gusts in the area included 66 MPH, measured by a mesonet station located three miles west of Edgar, and 59 MPH, measured by a mesonet station located two miles north of Edgar. Some minor tree damage was reported in Edgar. Emergency management estimated wind gusts near 60 mPH in Deweese.", "ts_dict_index": [10356, 10357, 10358]}
+{"event_id": 958270, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-07-01 00:18:00", "end_date_time": "2021-07-01 00:18:00", "narrative": "An upper level ridge was in place across eastern Kentucky and points eastward, but was weakening on June 30th heading into the evening  hours. This was allowing for decent return southerly flow and increased shower and thunderstorm potential. However, with little in the way of shear, most of the storms were poorly organized and pulsy in nature. The exception was a storm that moved through Pulaski County, and did result in some thunderstorm wind damage.||An upper level trough dropping southeast from the Great Lakes brought a modest increase in winds aloft overnight, along with lowering heights and upper level support for precipitation in the right entrance region of the upper level jet. The associated surface cold front also dropped south-southeast into the Ohio Valley, with a secondary stationary boundary setting up across the state just to our north and west during the day on the 1st. With low level flow increasing throughout the day ahead of these frontal systems, the stage was set for more scattered to widespread showers and thunderstorms to begin developing by dawn, continuing through the day, and resulting in locally heavy rainfall. The highest amounts were observed over east-central Kentucky, between Fayette and Powell County, where the Kentucky Mesonet reported 5.36 inches in Clark County, and the cooperative observer in Estill County reported 5.14 inches. A tree was reported down across Plato Van Hook Road near the community of Walnut  Grove, northeast of Somerset.", "ts_dict_index": [10344, 10345, 10346]}
+{"event_id": 1111960, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-07-04 18:56:00", "end_date_time": "2023-07-04 18:56:00", "narrative": "An upper level trough was over the northern Rocky Mountains and Northern Plains and was bringing a cold front south through Nebraska during the afternoon and evening hours of Independence Day. Temperatures heated up in advance of the front with dewpoints mostly in the 60s. A very moist and unstable atmosphere was present. CAPE values were generally near 4,000 J/kg ahead of the front, and 0 to 6 km wind shear values were around 35 knots. Mid-level lapse rates were generally 7 to 8 degrees C/km. ||Isolated showers and storms were moving across portions of south central Nebraska during the early to mid-afternoon hours. This activity did not produce any severe weather. The main storm activity developed late in the afternoon into the evening hours and was associated with the cold front moving through Nebraska. Storms began developing in central Nebraska in the late afternoon and early evening hours. Then storms developed in south central Nebraska and formed a line with the storms in the central part of the state. The storms in central Nebraska moved southeast during the evening hours while the storms in the south central part of the state remained fairly stationary. The storms produced large hail and wind gusts of 58 to 66 mph between 5:30 PM CDT and 9 PM CDT. The largest hail reported was up to 2.50 inches and was reported in Webster, Fillmore, and Thayer Counties. Minor tree damage was caused by wind gusts estimated around 60 MPH.", "ts_dict_index": [10359, 10360, 10361]}
+{"event_id": 1111966, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2023-07-04 19:45:00", "end_date_time": "2023-07-04 19:45:00", "narrative": "An upper level trough was over the northern Rocky Mountains and Northern Plains and was bringing a cold front south through Nebraska during the afternoon and evening hours of Independence Day. Temperatures heated up in advance of the front with dewpoints mostly in the 60s. A very moist and unstable atmosphere was present. CAPE values were generally near 4,000 J/kg ahead of the front, and 0 to 6 km wind shear values were around 35 knots. Mid-level lapse rates were generally 7 to 8 degrees C/km. ||Isolated showers and storms were moving across portions of south central Nebraska during the early to mid-afternoon hours. This activity did not produce any severe weather. The main storm activity developed late in the afternoon into the evening hours and was associated with the cold front moving through Nebraska. Storms began developing in central Nebraska in the late afternoon and early evening hours. Then storms developed in south central Nebraska and formed a line with the storms in the central part of the state. The storms in central Nebraska moved southeast during the evening hours while the storms in the south central part of the state remained fairly stationary. The storms produced large hail and wind gusts of 58 to 66 mph between 5:30 PM CDT and 9 PM CDT. The largest hail reported was up to 2.50 inches and was reported in Webster, Fillmore, and Thayer Counties. A wind gust of 61 MPH was measured by a mesonet station located seven miles southeast of Ohiowa.", "ts_dict_index": [10353, 10354, 10355]}
+{"event_id": 1111963, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2023-07-04 19:30:00", "end_date_time": "2023-07-04 19:30:00", "narrative": "An upper level trough was over the northern Rocky Mountains and Northern Plains and was bringing a cold front south through Nebraska during the afternoon and evening hours of Independence Day. Temperatures heated up in advance of the front with dewpoints mostly in the 60s. A very moist and unstable atmosphere was present. CAPE values were generally near 4,000 J/kg ahead of the front, and 0 to 6 km wind shear values were around 35 knots. Mid-level lapse rates were generally 7 to 8 degrees C/km. ||Isolated showers and storms were moving across portions of south central Nebraska during the early to mid-afternoon hours. This activity did not produce any severe weather. The main storm activity developed late in the afternoon into the evening hours and was associated with the cold front moving through Nebraska. Storms began developing in central Nebraska in the late afternoon and early evening hours. Then storms developed in south central Nebraska and formed a line with the storms in the central part of the state. The storms in central Nebraska moved southeast during the evening hours while the storms in the south central part of the state remained fairly stationary. The storms produced large hail and wind gusts of 58 to 66 mph between 5:30 PM CDT and 9 PM CDT. The largest hail reported was up to 2.50 inches and was reported in Webster, Fillmore, and Thayer Counties. A wind gust of 58 MPH was measured by a mesonet station located four miles northeast Belvidere.", "ts_dict_index": [10350, 10351, 10352]}
+{"event_id": 1087021, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-04-26 15:35:00", "end_date_time": "2023-04-26 15:35:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Numerous trees and power lines were downed in Troup.", "ts_dict_index": [10368, 10369, 10370]}
+{"event_id": 808276, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:07:00", "end_date_time": "2019-04-14 01:07:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down at 1206 CR 107.", "ts_dict_index": [10377, 10378, 10379]}
+{"event_id": 812546, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:25:00", "end_date_time": "2019-04-14 01:25:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree and power line was knocked down just south of 2500 CR 69.", "ts_dict_index": [10386, 10387, 10388]}
+{"event_id": 824992, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-05-28 16:35:00", "end_date_time": "2019-05-28 16:35:00", "narrative": "Mid-level westerly flow of 45-70kts streamed over the Great Lakes/Upper Ohio Valley. A shortwave trough embedded within this zonal flow entered the region and moved eastward throughout the day, helping to provide forcing for ascent and strengthening of deep layer shear.  Mid-level westerly flow of 45 to 70 knots also streamed over the Great Lakes and the Upper Ohio Valley. Large hail was supported by mean layer CAPE of 1500 to 3000 J/kg and effective bulk shear of 35 to 50kts. Additionally, strong synoptic winds and steepening low-level lapse rates increased the severe wind threat.||With high precipitable water values of around 1.5 inches, training storms were also able to produce localized flooding.||The hail from this event was so severe that windows in homes broke and cars were damaged. A local car dealership said that from the time of the incident to the end of September they were booked with car repairs due to hail damage. Roughly, the damage from hail for this event cost at least 12 million dollars.||The town of Zelienople, PA was hit hard with rain, as a total of 4 to 5 inches accumulated in just a few hours. As a result, the Connoquenessing Creek rose throughout the night and crested at just over 15.3 feet on Wednesday morning, May 29th.  Based on historical crests, this was the 4th highest crest on record; records go back to the early 1920s. A 911 call center reported a tree down near the intersection of Freeport Rd and Whistle Pig Lane.", "ts_dict_index": [10362, 10363, 10364]}
+{"event_id": 812552, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:41:00", "end_date_time": "2019-04-14 01:41:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down on CR 104 between CR 71 and CR 478.", "ts_dict_index": [10401, 10402, 10403]}
+{"event_id": 1087023, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-04-26 15:35:00", "end_date_time": "2023-04-26 15:35:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Trees and power lines were downed in the areas of County Road 2138, 2166, and 2169 just east of Troup.", "ts_dict_index": [10371, 10372, 10373]}
+{"event_id": 808275, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2019-04-14 00:28:00", "end_date_time": "2019-04-14 00:28:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. Numerous damage reported reported in the Springs Valley Community. This included power poles knocked down on Highway 20, Jackson Highway and Blake Drive.", "ts_dict_index": [10404, 10405, 10406]}
+{"event_id": 812553, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-13 23:49:00", "end_date_time": "2019-04-13 23:49:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down on Brooks Drive.", "ts_dict_index": [10395, 10396, 10397]}
+{"event_id": 812556, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 00:25:00", "end_date_time": "2019-04-14 00:25:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. Trees were knocked down on the road along North Shore Drive near CR 27.", "ts_dict_index": [10410, 10411, 10412]}
+{"event_id": 808274, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2019-04-13 23:32:00", "end_date_time": "2019-04-13 23:32:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. Several trees were knocked down on Mount Hester Road.", "ts_dict_index": [10383, 10384, 10385]}
+{"event_id": 808273, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2019-04-13 23:30:00", "end_date_time": "2019-04-13 23:30:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. Several trees were knocked down on Maude Road.", "ts_dict_index": [10380, 10381, 10382]}
+{"event_id": 812534, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:08:00", "end_date_time": "2019-04-14 01:08:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down at 1206 CR 107.  Other trees knocked down along other portions of CR 107.", "ts_dict_index": [10389, 10390, 10391]}
+{"event_id": 812555, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 02:05:00", "end_date_time": "2019-04-14 02:05:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down across the road on CR 92 just west of the the bridge.", "ts_dict_index": [10398, 10399, 10400]}
+{"event_id": 1087038, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2023-04-26 16:45:00", "end_date_time": "2023-04-26 16:45:00", "narrative": "A strong upper level trough shifted east across Northern New Mexico into West Texas during the daytime hours of April 26th, which enhanced surface low development along the dryline in West Texas. Meanwhile, a warm front extended east from this surface low across much of North Texas, bisecting East Texas generally along the Interstate 20 corridor into Northwest and North-central Louisiana. Showers and thunderstorms along and north of this warm front persisted through the day, given a series of upper level disturbances that ejected northeast ahead of the low atop the front, which kept the warmest temperatures and instability south of the front over Lower East Texas south of I-20 into West-central Louisiana. Large scale forcing increased during the afternoon south of the front and ahead of the eastward advancing dryline, with scattered to numerous showers and thunderstorms developing across the warm sector from the mid-afternoon through the evening hours. Some of these storms were severe, with damaging winds and large hail before exiting East Texas by midnight. In wake of these severe storms, a wake low pressure system developed near the I-20 corridor between Longview and Waskom, with multiple measured wind gusts between 40-50 mph across Gregg and Harrison Counties. These strong winds downed several trees across Harrison County before subsiding. Trees and power lines were downed southwest of Gary City around the area of FM 999 and County Roads 178, 179, and 180. Damage also extends south into Northern Shelby County.", "ts_dict_index": [10365, 10366, 10367]}
+{"event_id": 1064261, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-01-07 20:05:00", "end_date_time": "2023-01-07 20:05:00", "narrative": "An upper trough ejected east across the Central Plains on January 7th and into Iowa/Northern Missouri during the evening, inducing surface low development farther south over Southern Oklahoma which moved east into Central Arkansas by the evening. This system reinforced a cold front southeast across the Southern Plains during the afternoon, and into East Texas during the mid and late evening hours. Meanwhile, another shortwave trough rapidly traversed east from Northern Baja and merged with the southern extent of the upper trough axis over East Texas, increasing large scale forcing along and ahead of the front. Low level moisture return was already underway across East Texas and North Louisiana ahead of the front, and was sufficient enough for the development of scattered to numerous showers and thunderstorms across these areas during the evening and overnight hours. While shear ahead of the front was strong, instability was not particularly high across the area, but was adequate enough for the development of isolated strong to severe thunderstorms across portions of Lower East Texas, which moved east-southeast into Western Louisiana during the late evening hours. Damaging winds downed multiple trees southeast of Henderson in Rusk County, before these storms eventually produced more damaging winds and large hail in Sabine Parish Louisiana. Multiple trees were downed on FM 840 near the intersection of CR 355.", "ts_dict_index": [10374, 10375, 10376]}
+{"event_id": 842478, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-07-20 18:15:00", "end_date_time": "2019-07-20 18:15:00", "narrative": "The atmosphere was juiced so to speak ahead of a cold front sliding into the region. MUCAPE values very quickly approached and exceeded 4000 J/kg by mid-morning. With the cold front and previous storm outflows the impetus for new convection, discrete storms were not expected, with the prevailing storm type being the linear or quasi-linear convective system (QLCS) variety. Additional support for the QLCS mode was seen with, once again the cold frontal and outflow forcing, highly unstable atmosphere, and little to no convective inhibition.  Additional support for strong winds was seen with DCAPE values in excess of 1500 J/kg across much of the area  Once a system began to produce a decent cold pool, there would be little to prevent it from progressing. ||That was evident in Iowa as two distinct QLCSs moved through. First in the morning hours across northern Iowa, and second during the late morning through evening hours from central Iowa and on toward south central and southeast Iowa. In both cases, damaging winds widely prevailed. Across northern Iowa the gust front roared out ahead of the line of convection, continuing to produce severe wind reports in areas of no storms well to the south and east. In central and southeast Iowa, widespread reports of 60 to 70 mph winds and various tree damage (from large limbs to entire trees) were received along a path from roughly Perry, IA through Ottumwa, IA. Public reported a large tree branch, 6 to 8 inches in diameter, snapped. This is a delayed report. Time estimated from radar.", "ts_dict_index": [10326, 10327, 10328]}
+{"event_id": 812557, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 00:25:00", "end_date_time": "2019-04-14 00:25:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down onto CR 94 at Waters Edge Drive.", "ts_dict_index": [10434, 10435, 10436]}
+{"event_id": 812532, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-13 23:49:00", "end_date_time": "2019-04-13 23:49:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down at 1855 CR 31.", "ts_dict_index": [10413, 10414, 10415]}
+{"event_id": 808281, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2019-04-14 01:53:00", "end_date_time": "2019-04-14 01:53:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down on Jones Road near Highway 247.", "ts_dict_index": [10437, 10438, 10439]}
+{"event_id": 808277, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:25:00", "end_date_time": "2019-04-14 01:25:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. Two trees were knocked down on CR 227.", "ts_dict_index": [10425, 10426, 10427]}
+{"event_id": 812539, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:42:00", "end_date_time": "2019-04-14 01:42:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. Trees were knocked down on CR 8 in Zip City.", "ts_dict_index": [10416, 10417, 10418]}
+{"event_id": 812538, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:41:00", "end_date_time": "2019-04-14 01:41:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down onto the road at 8300 CR 71.", "ts_dict_index": [10419, 10420, 10421]}
+{"event_id": 808280, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:51:00", "end_date_time": "2019-04-14 01:51:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. Multiple trees were knocked down onto CR 8 at Parsonage Cemetery Road. Other trees were down on CR 52 blocking both lanes.", "ts_dict_index": [10431, 10432, 10433]}
+{"event_id": 812544, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 02:09:00", "end_date_time": "2019-04-14 02:09:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. Trees were knocked down on CR 67 south of Alabama Highway 64.", "ts_dict_index": [10422, 10423, 10424]}
+{"event_id": 812537, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:30:00", "end_date_time": "2019-04-14 01:30:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down at 416 CR 427.", "ts_dict_index": [10443, 10444, 10445]}
+{"event_id": 812542, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 02:05:00", "end_date_time": "2019-04-14 02:05:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down at 16751 Highway 72.", "ts_dict_index": [10428, 10429, 10430]}
+{"event_id": 812531, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 00:20:00", "end_date_time": "2019-04-14 00:20:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down at Huntsville Road near Huntsville Boulevard.", "ts_dict_index": [10440, 10441, 10442]}
+{"event_id": 855649, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-09-09 15:50:00", "end_date_time": "2019-09-09 15:50:00", "narrative": "A relatively cool, but juicy atmosphere existed across the area with southerly surface winds dominating and southwesterly mid and upper level flow. During the early morning hours of the 9th, scattered thunderstorms aided by the low level jet remained predominantly sub-severe with small hail. Through the morning and early afternoon hours, a surface warm front entered and moved across the state from southwest to northeast, all the while increasing MUCAPE values across the southeast half to two thirds of the state into the 2000-4000+ J/kg range. Additionally, moderate to steep low level lapse rates boosted DCAPE values into the 1000-1300 J/kg range, increasing the potential for strong downdrafts and resulting surface winds. Effective bulk shear was marginal through most of the event, yielding around 30 to 40kts. ||Resulting storms generally rolled through the state in waves from southwest to northeast, with at least periods of organization. The primary cluster of storms rolled through during the late afternoon, producing a fairly consistent trail severe thunderstorm winds and thunderstorm wind damage from southwest of Des Moines all the way through the Waterloo area. A second round of at least brief sever storms moved through overnight just southeast of the Des Moines metro, but was short lived unlike the cluster earlier in the day. Trained spotter reported telephone pole leaned over as well as a no passing sign leaned over. This is a delayed report and time estimated from radar.", "ts_dict_index": [10449, 10450, 10451]}
+{"event_id": 812541, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:44:00", "end_date_time": "2019-04-14 01:44:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down on CR 52 just before the county line.", "ts_dict_index": [10407, 10408, 10409]}
+{"event_id": 975495, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 18:50:00", "end_date_time": "2021-07-10 18:50:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. A SRP mesonet station at Horseshoe Dam measured an 83 mph wind gust.", "ts_dict_index": [10473, 10474, 10475]}
+{"event_id": 855666, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-09-09 18:50:00", "end_date_time": "2019-09-09 18:50:00", "narrative": "A relatively cool, but juicy atmosphere existed across the area with southerly surface winds dominating and southwesterly mid and upper level flow. During the early morning hours of the 9th, scattered thunderstorms aided by the low level jet remained predominantly sub-severe with small hail. Through the morning and early afternoon hours, a surface warm front entered and moved across the state from southwest to northeast, all the while increasing MUCAPE values across the southeast half to two thirds of the state into the 2000-4000+ J/kg range. Additionally, moderate to steep low level lapse rates boosted DCAPE values into the 1000-1300 J/kg range, increasing the potential for strong downdrafts and resulting surface winds. Effective bulk shear was marginal through most of the event, yielding around 30 to 40kts. ||Resulting storms generally rolled through the state in waves from southwest to northeast, with at least periods of organization. The primary cluster of storms rolled through during the late afternoon, producing a fairly consistent trail severe thunderstorm winds and thunderstorm wind damage from southwest of Des Moines all the way through the Waterloo area. A second round of at least brief sever storms moved through overnight just southeast of the Des Moines metro, but was short lived unlike the cluster earlier in the day. Public reported estimated 60 mph wind gusts.", "ts_dict_index": [10455, 10456, 10457]}
+{"event_id": 975692, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 20:01:00", "end_date_time": "2021-07-10 20:01:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Gilbert Police closed Riggs Road between Val Vista Drive and Adora Boulevard due to downed powerlines. Winds were estimated around 60 mph and timing was estimated from radar. No injuries were reported.", "ts_dict_index": [10476, 10477, 10478]}
+{"event_id": 975525, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 19:30:00", "end_date_time": "2021-07-10 19:30:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Mesonet station SRP20 at Bartlett Dam measured a 60 mph wind gust.", "ts_dict_index": [10464, 10465, 10466]}
+{"event_id": 855669, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-09-10 02:50:00", "end_date_time": "2019-09-10 02:50:00", "narrative": "A relatively cool, but juicy atmosphere existed across the area with southerly surface winds dominating and southwesterly mid and upper level flow. During the early morning hours of the 9th, scattered thunderstorms aided by the low level jet remained predominantly sub-severe with small hail. Through the morning and early afternoon hours, a surface warm front entered and moved across the state from southwest to northeast, all the while increasing MUCAPE values across the southeast half to two thirds of the state into the 2000-4000+ J/kg range. Additionally, moderate to steep low level lapse rates boosted DCAPE values into the 1000-1300 J/kg range, increasing the potential for strong downdrafts and resulting surface winds. Effective bulk shear was marginal through most of the event, yielding around 30 to 40kts. ||Resulting storms generally rolled through the state in waves from southwest to northeast, with at least periods of organization. The primary cluster of storms rolled through during the late afternoon, producing a fairly consistent trail severe thunderstorm winds and thunderstorm wind damage from southwest of Des Moines all the way through the Waterloo area. A second round of at least brief sever storms moved through overnight just southeast of the Des Moines metro, but was short lived unlike the cluster earlier in the day. Trained spotter reported trees down in the neighborhood, including winds over 60 mph.", "ts_dict_index": [10452, 10453, 10454]}
+{"event_id": 975547, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 21:14:00", "end_date_time": "2021-07-10 21:14:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Mesonet station MAMO at 2.2 miles SE of Mobile measured a 64 mph wind gust.", "ts_dict_index": [10458, 10459, 10460]}
+{"event_id": 975804, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-10 19:40:00", "end_date_time": "2021-07-10 19:40:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Numerous social media photos and reports of significant damage the the Skyline RV Resort, east of San Tan, due to strong thunderstorm winds. Photos show awning, roof, and side panel damage to a few mobile homes. The number of RVs and mobile homes damaged is unknown. An awning and a shed for one home were destroyed, along with a broken window, and a large portion of metal roof blew off from another. A few street signs were bent in half in the community. There was also a photo of a power pole in the area that snapped near the base of the pole and fell. Power was knocked out to many customers in the area. Winds were estimated around 60-65 mph. Timing estimated from radar. No injuries reported.", "ts_dict_index": [10467, 10468, 10469]}
+{"event_id": 975693, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-10 20:10:00", "end_date_time": "2021-07-10 20:10:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Multiple wooden power lines down due to strong thunderstorm winds on SR-587 near Nelson Road, leading to the closure of SR-587 between I-10 and Indian Route 68. Wind speeds estimated around 60 mph and timing estimated from radar. No injuries reported.", "ts_dict_index": [10470, 10471, 10472]}
+{"event_id": 812554, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2019-04-14 01:38:00", "end_date_time": "2019-04-14 01:38:00", "narrative": "During the evening of the 13th, isolated low-topped supercells develops in central moving into north Alabama north of an advancing warm front.  One of the storms produced large hail up to the size of tennis balls in Limestone County.||Later in the evening of the 13th and through the early morning hours of the 14th, multiple lines of thunderstorms developed in Mississippi ahead of a strong cold front and shifted slowly east into north Alabama. The individual line segments at times broke off into more super-cellular thunderstorms.  A couple of these produced tornadoes in Franklin and Colbert Counties.  Several other reports of thunderstorm wind damage were received.  In addition, gusty south-southeast winds developed ahead of the advancing line of thunderstorms.  Gusts over 40 mph were reported, and also knocked a few trees/limbs down in northwest Alabama.||Intense rainfall rates were observed with the thunderstorms at times, and in some cases a few areas received multiple periods of thunderstorms.  Rainfall amounts of 2-3 inches in just 1 to 2 hours was reported.  Rapid runoff from this rainfall resulted in flash flooding in a few locations of northwest Alabama.  In Franklin County, EMA reported a high water rescue and a road that was washed out near the town of Vina.  Other reports of flash flooding were reported by Colbert County EMA. A tree was knocked down onto a bridge on CR 33.", "ts_dict_index": [10392, 10393, 10394]}
+{"event_id": 975688, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 19:40:00", "end_date_time": "2021-07-10 19:40:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. A 15-20 foot long section of a concrete brick wall was blown over from strong winds near Carefree Highway and 7th Street in North Phoenix during a severe warned thunderstorm. Wind gusts were estimated around 55-65 mph. Timing estimated from radar. No injuries reported.", "ts_dict_index": [10479, 10480, 10481]}
+{"event_id": 975695, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 20:15:00", "end_date_time": "2021-07-10 20:15:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Video on social media shows the roof of a residential home was partially torn off due to strong thunderstorm winds near 43rd Avenue and Cactus Road. Winds estimated around 60 mph and timing estimated from radar. No injuries reported.", "ts_dict_index": [10482, 10483, 10484]}
+{"event_id": 855670, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-09-10 02:55:00", "end_date_time": "2019-09-10 02:55:00", "narrative": "A relatively cool, but juicy atmosphere existed across the area with southerly surface winds dominating and southwesterly mid and upper level flow. During the early morning hours of the 9th, scattered thunderstorms aided by the low level jet remained predominantly sub-severe with small hail. Through the morning and early afternoon hours, a surface warm front entered and moved across the state from southwest to northeast, all the while increasing MUCAPE values across the southeast half to two thirds of the state into the 2000-4000+ J/kg range. Additionally, moderate to steep low level lapse rates boosted DCAPE values into the 1000-1300 J/kg range, increasing the potential for strong downdrafts and resulting surface winds. Effective bulk shear was marginal through most of the event, yielding around 30 to 40kts. ||Resulting storms generally rolled through the state in waves from southwest to northeast, with at least periods of organization. The primary cluster of storms rolled through during the late afternoon, producing a fairly consistent trail severe thunderstorm winds and thunderstorm wind damage from southwest of Des Moines all the way through the Waterloo area. A second round of at least brief sever storms moved through overnight just southeast of the Des Moines metro, but was short lived unlike the cluster earlier in the day. Des Moines Public Safety reported a tree fell on a power line, causing power flashes in south Des Moines.", "ts_dict_index": [10446, 10447, 10448]}
+{"event_id": 871225, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-03-04 07:25:00", "end_date_time": "2020-03-04 07:25:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across East Texas during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Given the still saturated grounds in wake of much above normal rains that had fallen since mid-January, the locally heavy rainfall produced isolated reports of flash flooding as well, before rain rates diminished during the afternoon. Over 25 trees were blown down across Central and Southern Rusk County.", "ts_dict_index": [10527, 10528, 10529]}
+{"event_id": 871220, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-03-04 07:10:00", "end_date_time": "2020-03-04 07:10:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across East Texas during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Given the still saturated grounds in wake of much above normal rains that had fallen since mid-January, the locally heavy rainfall produced isolated reports of flash flooding as well, before rain rates diminished during the afternoon. A tree was downed on a home east of Lake Striker in the New Salem community.", "ts_dict_index": [10530, 10531, 10532]}
+{"event_id": 975546, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 22:03:00", "end_date_time": "2021-07-10 22:03:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. AWOS at Gila Bend Air Force Auxiliary Field (KGXF) measured a 61 mph wind gust.", "ts_dict_index": [10494, 10495, 10496]}
+{"event_id": 871215, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-03-04 07:05:00", "end_date_time": "2020-03-04 07:05:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across East Texas during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Given the still saturated grounds in wake of much above normal rains that had fallen since mid-January, the locally heavy rainfall produced isolated reports of flash flooding as well, before rain rates diminished during the afternoon. A small radio tower was blown down and scattered tree damage occurred east of Lake Striker and along FM 839.", "ts_dict_index": [10524, 10525, 10526]}
+{"event_id": 975694, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 20:10:00", "end_date_time": "2021-07-10 20:10:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Gilbert Police reported southbound lanes on Lindsay Road at Ray Road were blocked due to a downed power pole as a result of strong winds. Winds estimated around 60 mph and timing estimated from radar. No injuries reported.", "ts_dict_index": [10509, 10510, 10511]}
+{"event_id": 975498, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 18:55:00", "end_date_time": "2021-07-10 18:55:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Mesonet station SRP19 at 16.2 miles NE of Carefree measured a 68 mph wind gust.", "ts_dict_index": [10497, 10498, 10499]}
+{"event_id": 975529, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 20:00:00", "end_date_time": "2021-07-10 20:00:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Mesonet station SRP10 at 6.5 miles N of East Mesa measured a 67 mph wind gust.", "ts_dict_index": [10485, 10486, 10487]}
+{"event_id": 975511, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 20:00:00", "end_date_time": "2021-07-10 20:00:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. AWOS at Phoenix-Mesa Gateway airport (KIWA) measured a 60 mph wind gust.", "ts_dict_index": [10515, 10516, 10517]}
+{"event_id": 975690, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-10 19:47:00", "end_date_time": "2021-07-10 19:47:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Significant damage to a dog sanctuary near Phillips and Royce Roads in San Tan Valley due to estimated 55 to 65 mph wind gusts from a severe warned thunderstorm. A few couple hundred pound dog sheds were destroyed and one fell over and injured the paw of one of the dogs, named Chuckles, requiring surgery. Timing estimated from radar.", "ts_dict_index": [10521, 10522, 10523]}
+{"event_id": 975512, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 20:06:00", "end_date_time": "2021-07-10 20:06:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. AWOS at Mesa Falcon Field (KFFZ) measured a 63 mph wind gust.", "ts_dict_index": [10500, 10501, 10502]}
+{"event_id": 975689, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 20:00:00", "end_date_time": "2021-07-10 20:15:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Multiple photos and videos on social media and reports from broadcast media of at least 14 downed utility power poles along 35th Avenue between Dunlap Avenue and Cactus Road in Phoenix due to strong winds from a severe warned thunderstorm. The downed poles and lines also knocked over street signs and street lamps, disrupted traffic, and caused a power outage for the area that took more than a day to be restored. Additionally, several large trees were uprooted or snapped in and around Cortez Park at 35th Ave and Dunlap Ave and a metal carport reportedly blew more than a block away near 35th Ave and Peoria Ave. Wind gusts were estimated around 55-65 mph. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [10512, 10513, 10514]}
+{"event_id": 975696, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 20:15:00", "end_date_time": "2021-07-10 20:15:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Broadcast report from local media showed a carport ripped away from a residence near Sahuaro Drive and 37th Drive due to strong winds in a severe warned thunderstorm. The carport flew into an alley behind the residence, knocking over a cinderblock wall and shattering the window of a residence on the other side of the alley. Winds were estimated around 55-65 mph and timing was estimated from radar. No injuries reported.", "ts_dict_index": [10518, 10519, 10520]}
+{"event_id": 975802, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-10 20:40:00", "end_date_time": "2021-07-10 20:40:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. The top half of a 20 foot vertical antenna mast was toppled over in strong thunderstorm winds. Multiple downed trees were also reported across the town of Maricopa. Winds were estimated around 55-65 mph. Timing estimated from radar.", "ts_dict_index": [10491, 10492, 10493]}
+{"event_id": 975801, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-10 19:46:00", "end_date_time": "2021-07-10 19:46:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Nearly 40 trees were uprooted around the Johnson Ranch subdivision in San Tan Valley due to strong winds during a severe warned thunderstorm. Some trees reportedly fell on roofs, fences, and concrete walls with unknown degrees of damage. Minor roof damage was also reported. In a separate report, at an unspecified location in San Tan Valley, photos show strong winds peeled up a portion of a residential roof and a large section of a bedroom ceiling collapsed. Winds were estimated around 55-65 mph. Timing based on radar. No injuries reported.", "ts_dict_index": [10488, 10489, 10490]}
+{"event_id": 975545, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-10 19:45:00", "end_date_time": "2021-07-10 19:45:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Mesonet station SRP22 at 10.9 miles NW of Florence measured a 59 mph wind gust.", "ts_dict_index": [10461, 10462, 10463]}
+{"event_id": 871216, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-03-04 07:05:00", "end_date_time": "2020-03-04 07:05:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across East Texas during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Given the still saturated grounds in wake of much above normal rains that had fallen since mid-January, the locally heavy rainfall produced isolated reports of flash flooding as well, before rain rates diminished during the afternoon. Multiple trees were downed. A roof was removed from a pier and the pier was destroyed at the Lake Striker Resort.", "ts_dict_index": [10536, 10537, 10538]}
+{"event_id": 871223, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-03-04 07:20:00", "end_date_time": "2020-03-04 07:20:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across East Texas during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Given the still saturated grounds in wake of much above normal rains that had fallen since mid-January, the locally heavy rainfall produced isolated reports of flash flooding as well, before rain rates diminished during the afternoon. Trees were downed on Highway 42 near the intersection of County Road 468 in Southwest Rusk County.", "ts_dict_index": [10542, 10543, 10544]}
+{"event_id": 871211, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-03-04 06:57:00", "end_date_time": "2020-03-04 06:57:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across East Texas during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Given the still saturated grounds in wake of much above normal rains that had fallen since mid-January, the locally heavy rainfall produced isolated reports of flash flooding as well, before rain rates diminished during the afternoon. Trees were downed on FM 840 a couple of miles southeast of Henderson which forced the closure of the road.", "ts_dict_index": [10539, 10540, 10541]}
+{"event_id": 871224, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-03-04 07:30:00", "end_date_time": "2020-03-04 07:30:00", "narrative": "A weak and shallow cold front drifted south across much of East Texas into Central Louisiana during the early morning hours of March 4th, providing slightly cooler and more stable air at the surface in its wake across much of the Ark-La-Tex. However, large scale forcing began to increase across East Texas and North Louisiana well ahead of a closed upper level low pressure system that entered West Texas shortly after midnight on the 4th, as overrunning began to increase atop the shallow cool air dome. Very unstable air aloft in the form of steep lapse rates was present across Southeast Texas, Central and Southern Louisiana as these storms began to develop, with the more unstable air spreading northeast to near the I-20 corridor of East Texas and North Louisiana. Thus, scattered strong to severe elevated thunderstorms developed, producing numerous reports of large hail and isolated reports of damaging winds across East Texas during the early morning hours before the storms gradually weakened with the loss of instability by late morning through the afternoon. Given the still saturated grounds in wake of much above normal rains that had fallen since mid-January, the locally heavy rainfall produced isolated reports of flash flooding as well, before rain rates diminished during the afternoon. A tree was downed on Highway 84 near the intersection of County Road 3167 just west of Mount Enterprise.", "ts_dict_index": [10533, 10534, 10535]}
+{"event_id": 1052210, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-02 18:10:00", "end_date_time": "2022-09-02 18:10:00", "narrative": "Under a classic setup for storm motion from the Northern Arizona high terrain to Southern Arizona lower deserts, with the monsoon 500mb high positioned over Nevada and Utah, a few multicell storm clusters developed and progressed west-southwest through the lower deserts in the afternoon and evening hours of the 2nd. Increased east-northeast steering flow resulted in relatively high shear values for the monsoon (Sfc-6km shear around 25-30 kts) and very steep mid-level lapse rate (8-8.5 C/km) supported the organized multicellular storm mode with robust updrafts. Inversely, very high DCAPE values, up to 1500-1800 J/kg, supported very strong downbursts. Moisture levels were also above normal which, in combination with the strong updrafts, supported high rainfall rates (1.5-2 inches per hour average). There were a few multicell clusters that moved through Southern Arizona. One through the southeast parts of the greater Phoenix area, another that developed in Yavapai County before descending southwest along US-60 in Maricopa and La Paz Counties, and a third that developed off the Kofa Wilderness terrain south of Quartzsite before being caught by the cluster descending along US-60. Each cluster produced damaging winds, dense blowing dust, small to severe hail, and localized flash flooding. Multiple downed trees reported in the Villages of Queen Creek Subdivision. Wind speeds estimated around 60 mph. No injuries were reported.", "ts_dict_index": [10548, 10549, 10550]}
+{"event_id": 1056315, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-02 19:30:00", "end_date_time": "2022-09-02 19:30:00", "narrative": "Under a classic setup for storm motion from the Northern Arizona high terrain to Southern Arizona lower deserts, with the monsoon 500mb high positioned over Nevada and Utah, a few multicell storm clusters developed and progressed west-southwest through the lower deserts in the afternoon and evening hours of the 2nd. Increased east-northeast steering flow resulted in relatively high shear values for the monsoon (Sfc-6km shear around 25-30 kts) and very steep mid-level lapse rate (8-8.5 C/km) supported the organized multicellular storm mode with robust updrafts. Inversely, very high DCAPE values, up to 1500-1800 J/kg, supported very strong downbursts. Moisture levels were also above normal which, in combination with the strong updrafts, supported high rainfall rates (1.5-2 inches per hour average). There were a few multicell clusters that moved through Southern Arizona. One through the southeast parts of the greater Phoenix area, another that developed in Yavapai County before descending southwest along US-60 in Maricopa and La Paz Counties, and a third that developed off the Kofa Wilderness terrain south of Quartzsite before being caught by the cluster descending along US-60. Each cluster produced damaging winds, dense blowing dust, small to severe hail, and localized flash flooding. Social media pictures showed mobile home and metal shed destroyed in Rainbow Valley from damaging thunderstorm winds. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [10551, 10552, 10553]}
+{"event_id": 1056314, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-02 18:10:00", "end_date_time": "2022-09-02 18:10:00", "narrative": "Under a classic setup for storm motion from the Northern Arizona high terrain to Southern Arizona lower deserts, with the monsoon 500mb high positioned over Nevada and Utah, a few multicell storm clusters developed and progressed west-southwest through the lower deserts in the afternoon and evening hours of the 2nd. Increased east-northeast steering flow resulted in relatively high shear values for the monsoon (Sfc-6km shear around 25-30 kts) and very steep mid-level lapse rate (8-8.5 C/km) supported the organized multicellular storm mode with robust updrafts. Inversely, very high DCAPE values, up to 1500-1800 J/kg, supported very strong downbursts. Moisture levels were also above normal which, in combination with the strong updrafts, supported high rainfall rates (1.5-2 inches per hour average). There were a few multicell clusters that moved through Southern Arizona. One through the southeast parts of the greater Phoenix area, another that developed in Yavapai County before descending southwest along US-60 in Maricopa and La Paz Counties, and a third that developed off the Kofa Wilderness terrain south of Quartzsite before being caught by the cluster descending along US-60. Each cluster produced damaging winds, dense blowing dust, small to severe hail, and localized flash flooding. Report on social media of lost roof tiles from home and tree down near the area of South Meridian Road and East Pima Road. Winds were estimated at around 60 mph. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [10545, 10546, 10547]}
+{"event_id": 1057820, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-02 17:55:00", "end_date_time": "2022-09-02 17:55:00", "narrative": "Under a classic setup for storm motion from the Northern Arizona high terrain to Southern Arizona lower deserts, with the monsoon 500mb high positioned over Nevada and Utah, a few multicell storm clusters developed and progressed west-southwest through the lower deserts in the afternoon and evening hours of the 2nd. Increased east-northeast steering flow resulted in relatively high shear values for the monsoon (Sfc-6km shear around 25-30 kts) and very steep mid-level lapse rate (8-8.5 C/km) supported the organized multicellular storm mode with robust updrafts. Inversely, very high DCAPE values, up to 1500-1800 J/kg, supported very strong downbursts. Moisture levels were also above normal which, in combination with the strong updrafts, supported high rainfall rates (1.5-2 inches per hour average). There were a few multicell clusters that moved through Southern Arizona. One through the southeast parts of the greater Phoenix area, another that developed in Yavapai County before descending southwest along US-60 in Maricopa and La Paz Counties, and a third that developed off the Kofa Wilderness terrain south of Quartzsite before being caught by the cluster descending along US-60. Each cluster produced damaging winds, dense blowing dust, small to severe hail, and localized flash flooding. A photo on social media shows part of a destroyed metal carport lodged in the side of a home near the intersection of Gantzel Road and Ocotillo Road. Timing and wind speed estimated from radar. No injuries were reported.", "ts_dict_index": [10557, 10558, 10559]}
+{"event_id": 1052208, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-02 17:45:00", "end_date_time": "2022-09-02 17:45:00", "narrative": "Under a classic setup for storm motion from the Northern Arizona high terrain to Southern Arizona lower deserts, with the monsoon 500mb high positioned over Nevada and Utah, a few multicell storm clusters developed and progressed west-southwest through the lower deserts in the afternoon and evening hours of the 2nd. Increased east-northeast steering flow resulted in relatively high shear values for the monsoon (Sfc-6km shear around 25-30 kts) and very steep mid-level lapse rate (8-8.5 C/km) supported the organized multicellular storm mode with robust updrafts. Inversely, very high DCAPE values, up to 1500-1800 J/kg, supported very strong downbursts. Moisture levels were also above normal which, in combination with the strong updrafts, supported high rainfall rates (1.5-2 inches per hour average). There were a few multicell clusters that moved through Southern Arizona. One through the southeast parts of the greater Phoenix area, another that developed in Yavapai County before descending southwest along US-60 in Maricopa and La Paz Counties, and a third that developed off the Kofa Wilderness terrain south of Quartzsite before being caught by the cluster descending along US-60. Each cluster produced damaging winds, dense blowing dust, small to severe hail, and localized flash flooding. Several 6-8 inch diameter trees snapped off. Several other newer small trees uprooted. Minor roof damage to some homes under construction. In a nearby subdivision a large willow tree blown over and uprooted. No injuries were reported.", "ts_dict_index": [10560, 10561, 10562]}
+{"event_id": 975691, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-10 19:57:00", "end_date_time": "2021-07-10 19:57:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. Multiple large trees snapped or blown over in strong winds during a severe warned thunderstorm around the Superstition Springs Center near Power Road and Southern Avenue. Winds estimated around 55-60 mph. Timing estimated from radar. No injuries reported.", "ts_dict_index": [10503, 10504, 10505]}
+{"event_id": 1140008, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 21:10:00", "end_date_time": "2023-09-12 21:10:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Multiple large trees were snapped and/or uprooted in the area of North Power and East McKellips Roads in Mesa. Wind gusts were estimated at approximately 80 mph. No injuries were reported.", "ts_dict_index": [10572, 10573, 10574]}
+{"event_id": 1140013, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 20:40:00", "end_date_time": "2023-09-12 20:40:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Tree limb of approximately 6-8 inches in diameter was snapped from a large tree in the area of North Miller Road and East McDowell Road in Scottsdale. No injuries were reported.", "ts_dict_index": [10569, 10570, 10571]}
+{"event_id": 1140004, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 20:30:00", "end_date_time": "2023-09-12 20:30:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. A very large uprooted tree fell onto the roof of a home located along the area of North 40th Street and Indian School Road in Phoenix. Tree was estimated to be 90 feet tall with its root system at 13 feet in diameter. Winds were estimated at approximately 65-70 mph. No injuries were reported.", "ts_dict_index": [10575, 10576, 10577]}
+{"event_id": 1052209, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-02 17:55:00", "end_date_time": "2022-09-02 17:55:00", "narrative": "Under a classic setup for storm motion from the Northern Arizona high terrain to Southern Arizona lower deserts, with the monsoon 500mb high positioned over Nevada and Utah, a few multicell storm clusters developed and progressed west-southwest through the lower deserts in the afternoon and evening hours of the 2nd. Increased east-northeast steering flow resulted in relatively high shear values for the monsoon (Sfc-6km shear around 25-30 kts) and very steep mid-level lapse rate (8-8.5 C/km) supported the organized multicellular storm mode with robust updrafts. Inversely, very high DCAPE values, up to 1500-1800 J/kg, supported very strong downbursts. Moisture levels were also above normal which, in combination with the strong updrafts, supported high rainfall rates (1.5-2 inches per hour average). There were a few multicell clusters that moved through Southern Arizona. One through the southeast parts of the greater Phoenix area, another that developed in Yavapai County before descending southwest along US-60 in Maricopa and La Paz Counties, and a third that developed off the Kofa Wilderness terrain south of Quartzsite before being caught by the cluster descending along US-60. Each cluster produced damaging winds, dense blowing dust, small to severe hail, and localized flash flooding. A trained spotter estimated thunderstorm wind gusts around 60 mph and some minor tree damage. No injuries were reported.", "ts_dict_index": [10563, 10564, 10565]}
+{"event_id": 1140012, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 20:30:00", "end_date_time": "2023-09-12 20:30:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. A 60 foot pine tree was uprooted and toppled over a home causing damage to the patio roof. Wind gusts were estimated at between 65-70 mph. No injuries were reported.", "ts_dict_index": [10578, 10579, 10580]}
+{"event_id": 1140007, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 21:00:00", "end_date_time": "2023-09-12 21:00:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Numerous reports of considerable damage at Falcon Field Airport from a severe microburst. Around 25 airplanes, mostly Cessna small aircraft, were damaged or destroyed, with some flipped over. One aviation flight school lost one third of their fleet, but it is unknown how many aircraft that amounts to. A few pilots reported that even planes with proper tie-downs broke free, with wind eyelets snapping and chains breaking as the planes likely tried to become airborne. Numerous hangars suffered significant damage, with around 90 hangar doors damaged or destroyed. Two World War II era hangars were damaged, with one losing its roof. Another hangar had an entire side wall shorn off. There were several downed trees around the airport, as well as damages to some other airport infrastructure and property, like fencing. A news report nearly three months later stated repairs are still being done and the total damages at the airport is around $7.2 million. An ASOS at Falcon Field Airport did not measure peak wind gusts from this storm due to a loss of power at the airport. Thus, based on damages, winds were estimated around 90 mph. No injuries were reported.", "ts_dict_index": [10566, 10567, 10568]}
+{"event_id": 975513, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-10 20:35:00", "end_date_time": "2021-07-10 20:35:00", "narrative": "With upper level high pressure centered near Las Vegas, Nevada this promoted increased northeasterly flow through central and southern Arizona. 30-35 kts of 0-6 km bulk shear was analyzed over south-central Arizona under this regime and with 1000-1500 J/kg of MLCAPE, organized strong to severe thunderstorms developed over the Mogollon Rim in the afternoon and spread through the lower deserts of south-central Arizona through the evening hours. Two severe multi-cellular clusters progressed off the high terrain into the lower deserts of Pinal and Maricopa counties and eventually merged together in northwest Pinal county before continuing southwest. The severe storms produced widespread 40+ mph wind gusts with many areas of 60-70 mph gusts. There were numerous toppled trees, downed power lines, damaged roofs, and other infrastructure and property damage as a result of the severe winds. Over 35,000 customers across Phoenix also lost power. The severe winds also produced a dust storm out ahead of the storms with widespread dense blowing  dust pushing west through northern Pinal and southwest Maricopa counties. There was also an area of dense blowing dust reported in the North Phoenix foothills with the northern multi-cell cluster. This was the second day in a row with severe winds moving through some of the same areas. AWOS at Ak-Chin Regional Airport (KA39) measured a 60 mph wind gust.", "ts_dict_index": [10506, 10507, 10508]}
+{"event_id": 1140149, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 21:10:00", "end_date_time": "2023-09-12 21:10:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Large trees uprooted along with ceramic tiles on rooftops damaged in the Mountain Bridge Neighborhood located near East McKellips Road in Mesa. Wind gusts were estimated at approximately 80 mph. No injuries were reported.", "ts_dict_index": [10602, 10603, 10604]}
+{"event_id": 1140011, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 21:10:00", "end_date_time": "2023-09-12 21:10:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Large tree approximately 9-11 inches in diameter was uprooted in 8534 East Halifax Circle in Mesa. Wind gusts were estimated at around 60 mph. No injuries were reported.", "ts_dict_index": [10590, 10591, 10592]}
+{"event_id": 1140005, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 20:30:00", "end_date_time": "2023-09-12 20:30:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. More than 100 trees downed in the city of Scottsdale parks, including 60 in the area of Vista Del Camino and El Dorado Parks. Wind gusts were estimated at approximately 65-70 mph. No injuries were reported.", "ts_dict_index": [10587, 10588, 10589]}
+{"event_id": 1139885, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 19:45:00", "end_date_time": "2023-09-12 19:45:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Several large trees estimated to be up to 1 foot in diameter were uprooted in the area of West Indian School Road and North Litchfield Road in Goodyear. Wind gusts were estimated at approximately 60 mph. No injuries were reported.", "ts_dict_index": [10599, 10600, 10601]}
+{"event_id": 1140144, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 21:10:00", "end_date_time": "2023-09-12 21:10:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. A couple of mobile homes sustained severe roof damage in the area of East University Drive and Loop 202 in Mesa. Wind gusts were estimated at approximately 80 mph. No injuries were reported.", "ts_dict_index": [10581, 10582, 10583]}
+{"event_id": 1140014, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 21:10:00", "end_date_time": "2023-09-12 21:10:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Severe damage occurred at Zaharis Elementary School located at the intersection of East McKellips Road and North Ellsworth Road in Mesa. Significant water damage occurred with several ceiling tiles ripped off as well as downed trees and debris across the campus. School was forced to close down for approximately a week due to the heavy damage. Wind gusts were estimated at approximately 80 mph. No injuries were reported.", "ts_dict_index": [10596, 10597, 10598]}
+{"event_id": 1140009, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 21:10:00", "end_date_time": "2023-09-12 21:10:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. An AC unit was blown off the roof of a home located in the area of East Brown and North Power Roads in Mesa and landed on two brand new cars. The unit shattered the windshield of one car and dented the other car. Wind gusts were estimated at approximately 80 mph. No injuries were reported.", "ts_dict_index": [10593, 10594, 10595]}
+{"event_id": 1056282, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-02 17:41:00", "end_date_time": "2022-09-02 17:41:00", "narrative": "Under a classic setup for storm motion from the Northern Arizona high terrain to Southern Arizona lower deserts, with the monsoon 500mb high positioned over Nevada and Utah, a few multicell storm clusters developed and progressed west-southwest through the lower deserts in the afternoon and evening hours of the 2nd. Increased east-northeast steering flow resulted in relatively high shear values for the monsoon (Sfc-6km shear around 25-30 kts) and very steep mid-level lapse rate (8-8.5 C/km) supported the organized multicellular storm mode with robust updrafts. Inversely, very high DCAPE values, up to 1500-1800 J/kg, supported very strong downbursts. Moisture levels were also above normal which, in combination with the strong updrafts, supported high rainfall rates (1.5-2 inches per hour average). There were a few multicell clusters that moved through Southern Arizona. One through the southeast parts of the greater Phoenix area, another that developed in Yavapai County before descending southwest along US-60 in Maricopa and La Paz Counties, and a third that developed off the Kofa Wilderness terrain south of Quartzsite before being caught by the cluster descending along US-60. Each cluster produced damaging winds, dense blowing dust, small to severe hail, and localized flash flooding. Downed powerlines leaving 2005 people without power was reported in the area between Apache Junction, Gold Canyon, and Queen Valley. A spotter said there were several wooden poles snapped or toppled along US-60. Another spotter in the Gold Canyon area also shared pictures of an aluminum carport/awning that was torn from a home. Winds were estimated to be between 60-70 mph. No injuries were reported.", "ts_dict_index": [10554, 10555, 10556]}
+{"event_id": 1139892, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 20:30:00", "end_date_time": "2023-09-12 20:30:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Giant 60 year old pine was uprooted, taking out two block walls as well as a couple power lines in the area of North 66th Street and East Oak Street in Scottsdale. Wind gusts were estimated at 65-70 mph. No injuries were reported.", "ts_dict_index": [10611, 10612, 10613]}
+{"event_id": 1046954, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:30:00", "end_date_time": "2022-07-30 18:30:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Images showed a gas station canopy knocked over at 7th Street and Coral Gables Drive, falling onto a vehicle. Nearby, images showed an uprooted tree approximately 1 ft in diameter fallen over onto a fence, tearing part of the fence down. No injuries were reported.", "ts_dict_index": [10644, 10645, 10646]}
+{"event_id": 1140147, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 21:10:00", "end_date_time": "2023-09-12 21:10:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Video showed the roof from a home taken completely apart, flying approximately 100 feet away. Video also showed multiple large trees within the vicinity uprooted. The damage took place in a neighborhood complex located along North Recker Road just north of East McKellips Road in Mesa. Wind gusts were estimated at approximately 80 mph. No injuries were reported.", "ts_dict_index": [10617, 10618, 10619]}
+{"event_id": 1139884, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 15:10:00", "end_date_time": "2023-09-12 15:10:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Downed power poles near the area Maricopa Rd and Highway 347 just west of I-10. Traffic signals were out leading to significant traffic impacts. Wind gusts were estimated at approximately 60 mph. No injuries were reported.", "ts_dict_index": [10620, 10621, 10622]}
+{"event_id": 1139889, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 20:20:00", "end_date_time": "2023-09-12 20:20:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Power lines were snapped in the area of North 17th Street and East Oak Street in Phoenix. Wind gusts were estimated at approximately 65-70 mph. No injuries were reported.", "ts_dict_index": [10608, 10609, 10610]}
+{"event_id": 1046955, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:37:00", "end_date_time": "2022-07-30 18:37:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. ASOS at Phoenix-Deer Valley Municipal Airport.", "ts_dict_index": [10638, 10639, 10640]}
+{"event_id": 1046926, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:02:00", "end_date_time": "2022-07-30 18:02:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. An image showed a large tree that fell onto three parked vehicles at an apartment complex near 7th Avenue and Osborn Road. No injuries were reported.", "ts_dict_index": [10641, 10642, 10643]}
+{"event_id": 1140016, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-09-12 21:10:00", "end_date_time": "2023-09-12 21:10:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Downed powerlines were reported in the area of North Pinal Avenue and West Val Vista Boulevard in Casa Grande. Wind gusts were estimated at approximately 55-60 mph. No injuries were reported.", "ts_dict_index": [10626, 10627, 10628]}
+{"event_id": 1139883, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-09-12 14:15:00", "end_date_time": "2023-09-12 14:15:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Three downed power poles along West Miller Road about two miles west of Highway 347. Timing based on radar. Wind gusts were estimated at approximately 60 mph. No injuries were reported.", "ts_dict_index": [10605, 10606, 10607]}
+{"event_id": 1047143, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-07-30 16:50:00", "end_date_time": "2022-07-30 16:50:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Multiple toppled or snapped wooden power poles were reported along Rodeo Road west of SR 387. Additional downed power poles were reported along McCartney Road nearby. No injuries were reported.", "ts_dict_index": [10635, 10636, 10637]}
+{"event_id": 1140006, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 21:00:00", "end_date_time": "2023-09-12 21:00:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Multiple downed power poles and on top of houses in the area of Recker Road between East McDowell Road and East McKellips Road in Mesa. Multiple downed trees were also observed. Wind gusts were estimated at approximately 80 mph. No injuries were reported.", "ts_dict_index": [10614, 10615, 10616]}
+{"event_id": 1140015, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-09-12 21:10:00", "end_date_time": "2023-09-12 21:10:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Downed power lines resulting the closure of North Cox Road between West Randolph Road and West McCartney Road in Casa Grande were reported. Wind gusts were estimated at approximately 55-60 mph. No injuries were reported.", "ts_dict_index": [10623, 10624, 10625]}
+{"event_id": 1047141, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-07-30 16:40:00", "end_date_time": "2022-07-30 16:40:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Images showed significant roof damage to a couple of homes and a flipped trailer home just north of I-8 near Montgomery Road. No injuries were reported.", "ts_dict_index": [10632, 10633, 10634]}
+{"event_id": 1140010, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 21:00:00", "end_date_time": "2023-09-12 21:00:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Home weather station located at 2915 East Minton Road in Mesa recorded a peak wind gust of 81 mph.", "ts_dict_index": [10584, 10585, 10586]}
+{"event_id": 997739, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-12-11 06:40:00", "end_date_time": "2021-12-11 06:40:00", "narrative": "A very anomalous storm system produced winter weather across the Rockies, Upper Midwest, and Great Lakes region and severe weather across the mid-Mississippi and Ohio Valley regions. The combination of a warm and moist environment in place across the Ohio Valley region and a cold front that moved in from the west led to widespread thunderstorm development as the cold front pushed eastward through Missouri, Illinois and Kentucky. Additionally, a strong low level jet and low level wind shear contributed to strong thunderstorms developing that were favorable for tornadoes. ||As the storms moved across western and central Kentucky during the overnight hours, they produced a tornado outbreak of historic proportions. However, as they reached eastern Kentucky during the early morning hours on the 11th, they began to lose strength, continuing to push away from the area of best instability, highest low level winds, and with temperatures continuing to cool. Several tornado warnings were issued as the rotating and once tornadic storms moved across the Jackson CWA border, along with multiple severe thunderstorm warnings. Thankfully, no tornadoes impacted eastern Kentucky, though there were numerous reports of strong thunderstorm wind gusts and trees down across portions of the area. The Pulaski County Mesonet station in the community of Dabney reported a 56 mph gust.", "ts_dict_index": [10665, 10666, 10667]}
+{"event_id": 1046948, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:17:00", "end_date_time": "2022-07-30 18:17:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. An image showed a large tree fell onto and destroyed a metal carport, with an SUV parked underneath. No injuries were reported.", "ts_dict_index": [10659, 10660, 10661]}
+{"event_id": 997724, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-12-11 06:00:00", "end_date_time": "2021-12-11 06:00:00", "narrative": "A very anomalous storm system produced winter weather across the Rockies, Upper Midwest, and Great Lakes region and severe weather across the mid-Mississippi and Ohio Valley regions. The combination of a warm and moist environment in place across the Ohio Valley region and a cold front that moved in from the west led to widespread thunderstorm development as the cold front pushed eastward through Missouri, Illinois and Kentucky. Additionally, a strong low level jet and low level wind shear contributed to strong thunderstorms developing that were favorable for tornadoes. ||As the storms moved across western and central Kentucky during the overnight hours, they produced a tornado outbreak of historic proportions. However, as they reached eastern Kentucky during the early morning hours on the 11th, they began to lose strength, continuing to push away from the area of best instability, highest low level winds, and with temperatures continuing to cool. Several tornado warnings were issued as the rotating and once tornadic storms moved across the Jackson CWA border, along with multiple severe thunderstorm warnings. Thankfully, no tornadoes impacted eastern Kentucky, though there were numerous reports of strong thunderstorm wind gusts and trees down across portions of the area. A tree was downed and blocking Hwy-761 near the community of Nancy.", "ts_dict_index": [10671, 10672, 10673]}
+{"event_id": 1046953, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:20:00", "end_date_time": "2022-07-30 18:20:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. An image showed a metal carport roof blown onto a couple of parked cars. No injuries were reported.", "ts_dict_index": [10647, 10648, 10649]}
+{"event_id": 997726, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-12-11 06:05:00", "end_date_time": "2021-12-11 06:05:00", "narrative": "A very anomalous storm system produced winter weather across the Rockies, Upper Midwest, and Great Lakes region and severe weather across the mid-Mississippi and Ohio Valley regions. The combination of a warm and moist environment in place across the Ohio Valley region and a cold front that moved in from the west led to widespread thunderstorm development as the cold front pushed eastward through Missouri, Illinois and Kentucky. Additionally, a strong low level jet and low level wind shear contributed to strong thunderstorms developing that were favorable for tornadoes. ||As the storms moved across western and central Kentucky during the overnight hours, they produced a tornado outbreak of historic proportions. However, as they reached eastern Kentucky during the early morning hours on the 11th, they began to lose strength, continuing to push away from the area of best instability, highest low level winds, and with temperatures continuing to cool. Several tornado warnings were issued as the rotating and once tornadic storms moved across the Jackson CWA border, along with multiple severe thunderstorm warnings. Thankfully, no tornadoes impacted eastern Kentucky, though there were numerous reports of strong thunderstorm wind gusts and trees down across portions of the area. A tree was downed on power lines, both of which were laying across and blocking both lanes of Hwy-1674 just northeast of Somerset.", "ts_dict_index": [10674, 10675, 10676]}
+{"event_id": 1046940, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:03:00", "end_date_time": "2022-07-30 18:03:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Approximately 7-8 power poles were reported down along the Grand Canal, with many falling toward homes and crashing through cinder block walls. Another cinder block wall was knocked down after a metal shed blew out of the backyard of a home and into the canal. No injuries were reported.", "ts_dict_index": [10662, 10663, 10664]}
+{"event_id": 1046951, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 18:18:00", "end_date_time": "2022-07-30 18:18:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. Media live broadcast showed a snapped power pole near Cave Creek Road and Greenway Road. No injuries were reported.", "ts_dict_index": [10656, 10657, 10658]}
+{"event_id": 997734, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-12-11 06:07:00", "end_date_time": "2021-12-11 06:07:00", "narrative": "A very anomalous storm system produced winter weather across the Rockies, Upper Midwest, and Great Lakes region and severe weather across the mid-Mississippi and Ohio Valley regions. The combination of a warm and moist environment in place across the Ohio Valley region and a cold front that moved in from the west led to widespread thunderstorm development as the cold front pushed eastward through Missouri, Illinois and Kentucky. Additionally, a strong low level jet and low level wind shear contributed to strong thunderstorms developing that were favorable for tornadoes. ||As the storms moved across western and central Kentucky during the overnight hours, they produced a tornado outbreak of historic proportions. However, as they reached eastern Kentucky during the early morning hours on the 11th, they began to lose strength, continuing to push away from the area of best instability, highest low level winds, and with temperatures continuing to cool. Several tornado warnings were issued as the rotating and once tornadic storms moved across the Jackson CWA border, along with multiple severe thunderstorm warnings. Thankfully, no tornadoes impacted eastern Kentucky, though there were numerous reports of strong thunderstorm wind gusts and trees down across portions of the area. Power lines are downed in the community of Burnside at the intersection of Cliffside and Cumberland Drives.", "ts_dict_index": [10668, 10669, 10670]}
+{"event_id": 1047194, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-07-30 17:22:00", "end_date_time": "2022-07-30 17:22:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. A video showed a palm tree falling onto three vehicles at a car dealership resulting in damage to the vehicles. No injuries were reported.", "ts_dict_index": [10653, 10654, 10655]}
+{"event_id": 1047146, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-07-30 17:02:00", "end_date_time": "2022-07-30 17:02:00", "narrative": "Daytime heating combined with divergence aloft associated with an easterly wave near the Arizona/New Mexico border promoted thunderstorm initiation across southeast Arizona during the afternoon of the 30th. Outflow boundaries generated from these thunderstorms raced northwest toward south-central Arizona, resulting in a dust storm in Pinal County where multiple instances of dense blowing dust less than 1/4 mile were reported. New thunderstorm development occurred along these boundaries with some thunderstorms becoming severe. Numerous instances of damaging winds were reported across the Phoenix area and down into northwest Pinal County, which included multiple downed trees and power poles. A very moist environment, with PWATs in excess of 1.80 allowed for thunderstorms to become efficient heavy rainfall producers. Rainfall amounts upwards of around 1.50 within an hour were reported during the event. There were multiple reports of flash flooding across northern parts of the Phoenix area, leading to several water rescues and making some roads impassable. Flash flooding also led to water and mud entering some apartments in north Phoenix causing extensive water damage. Isolated flash flooding occurred across Pinal, Gila, and Yuma Counties. No injuries were reported with this event. An image showed a large branch of a tree snapped off and narrowly missed a home near Ocotillo Road and Meridian Road. A video taken in the area showed very strong winds estimated to be in excess of 60 mph. No injuries were reported.", "ts_dict_index": [10650, 10651, 10652]}
+{"event_id": 1057181, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-11-04 20:38:00", "end_date_time": "2022-11-04 20:38:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. Multiple trees were blown down along the length of Old Mooringsport Road just southeast of Mooringsport.", "ts_dict_index": [10680, 10681, 10682]}
+{"event_id": 1057189, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2022-11-04 21:43:00", "end_date_time": "2022-11-04 21:43:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. Multiple trees were blown down along Evangeline Drive. Two homes were damaged by high winds. One home was pushed off its blocks and another manufactured home had wall and roof damage. At least 2 metal carports were blown down the road into a heavily wooded area.", "ts_dict_index": [10677, 10678, 10679]}
+{"event_id": 1057256, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-11-04 22:38:00", "end_date_time": "2022-11-04 22:38:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. A tree was downed onto a power line just west of Spearsville.", "ts_dict_index": [10698, 10699, 10700]}
+{"event_id": 1057252, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-11-04 22:50:00", "end_date_time": "2022-11-04 22:50:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. Several trees were blown down on Patrick Church Road east of Bernice.", "ts_dict_index": [10686, 10687, 10688]}
+{"event_id": 1057254, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-11-04 22:40:00", "end_date_time": "2022-11-04 22:40:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. A tree was blown down just northeast of Spearsville.", "ts_dict_index": [10692, 10693, 10694]}
+{"event_id": 1057253, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-11-04 22:35:00", "end_date_time": "2022-11-04 22:35:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. A tree was blown down on Highway 167 and Price Road just north of the Lillie community.", "ts_dict_index": [10689, 10690, 10691]}
+{"event_id": 1057255, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-11-04 22:39:00", "end_date_time": "2022-11-04 22:39:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. Power lines were downed on Highway 3121 near Hunt Road.", "ts_dict_index": [10695, 10696, 10697]}
+{"event_id": 1057184, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-11-04 22:00:00", "end_date_time": "2022-11-04 22:00:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. Multiple trees and power lines were downed across scattered locations in Webster Parish.", "ts_dict_index": [10704, 10705, 10706]}
+{"event_id": 1057248, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2022-11-04 23:53:00", "end_date_time": "2022-11-04 23:53:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. Multiple trees were blown down across various locations in the northern portions of Natchitoches Parish.", "ts_dict_index": [10683, 10684, 10685]}
+{"event_id": 1140145, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-09-12 20:50:00", "end_date_time": "2023-09-12 20:50:00", "narrative": "The synoptic pattern was characterized by strong westerly flow aloft situated across most of the Desert Southwest with embedded shortwave energy providing the main source for rising motion. Above normal moisture was present with PWATs in excess of 1.5 across most of central and southwestern AZ. The available moisture in combination with the daytime heating led to the development of moderate instability  with MLCAPE in excess of 1000 J/KG. The strong westerly flow aloft led to strong vertical shear with 0-6 KM shear values ranging between 30-40 knots. All of these factors led to a very favorable environment for the development of strong to severe thunderstorms across portions of south-central AZ. Scattered thunderstorms started to develop by the early afternoon hours of the 12th with multiple rounds continuing into the evening hours. One severe thunderstorm in particular developed near the Buckeye area, became supercellular, and tracked generally eastward affecting areas such as Goodyear, Glendale, Phoenix, Scottsdale, Mesa and Apache Junction, causing extensive straight-line wind damage along its path. Additional thunderstorms developed just east of the Phoenix metro area during the overnight and early morning hours of the 13th, with the main impact being isolated flash flooding. Large tree uprooted in the area of Lindsay Road and East McKellips Road in Mesa. Wind gusts were estimated at 65-70 mph. No injuries were reported.", "ts_dict_index": [10629, 10630, 10631]}
+{"event_id": 829358, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-19 21:35:00", "end_date_time": "2019-06-19 21:35:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. Several large highway signs were blown over on I-49 North about 1.5 miles south of Highway 2. Several large limbs were downed in the area as well.", "ts_dict_index": [10758, 10759, 10760]}
+{"event_id": 828822, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-06-19 06:15:00", "end_date_time": "2019-06-19 06:15:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. Trees were downed, a mailbox was blown away, and shingles were ripped off the roofs of homes on Palmetto Drive in North Bossier City.", "ts_dict_index": [10746, 10747, 10748]}
+{"event_id": 828819, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-19 06:12:00", "end_date_time": "2019-06-19 06:12:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. Large tree limbs were downed on Old Mansfield Road and Mount Bethel Road.", "ts_dict_index": [10737, 10738, 10739]}
+{"event_id": 829362, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-19 21:25:00", "end_date_time": "2019-06-19 21:25:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. Several trees were blown down across Northern Caddo Parish.", "ts_dict_index": [10749, 10750, 10751]}
+{"event_id": 828810, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-19 05:50:00", "end_date_time": "2019-06-19 05:50:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. Trees and power lines were downed on Riviera Street between Crawford and Tacoma Blvd.", "ts_dict_index": [10752, 10753, 10754]}
+{"event_id": 828821, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-19 06:12:00", "end_date_time": "2019-06-19 06:12:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. A power line was downed on Southern Avenue and East 75th Street.", "ts_dict_index": [10743, 10744, 10745]}
+{"event_id": 828818, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-19 06:15:00", "end_date_time": "2019-06-19 06:15:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. A light pole was blown down near the intersection of Millicent Way and East Bert Kouns. Several large limbs were also downed in the University Terrace subdivision.", "ts_dict_index": [10734, 10735, 10736]}
+{"event_id": 828813, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-19 05:58:00", "end_date_time": "2019-06-19 05:58:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. Large tree limbs were downed on Dixie-Shreveport Road between Whitfield Circle and Sentell Road.", "ts_dict_index": [10755, 10756, 10757]}
+{"event_id": 838693, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-19 06:12:00", "end_date_time": "2019-06-19 06:12:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. A tree was downed on a power line on Boxwood Drive between Francais Drive and Crabapple Drive in the Southern Hills area of South Shreveport.", "ts_dict_index": [10761, 10762, 10763]}
+{"event_id": 829680, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-06-19 23:30:00", "end_date_time": "2019-06-19 23:30:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. These storms also spawned a brief, weak tornado over Harrison County just northwest of the Nesbitt community. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across East Texas. The storms produced damaging winds and large hail, with localized flash flooding in Northeast Wood County before finally weakening during the early morning hours of June 20th. Power lines were downed.", "ts_dict_index": [10716, 10717, 10718]}
+{"event_id": 828155, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-06-19 05:30:00", "end_date_time": "2019-06-19 05:30:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. These storms also spawned a brief, weak tornado over Harrison County just northwest of the Nesbitt community. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across East Texas. The storms produced damaging winds and large hail, with localized flash flooding in Northeast Wood County before finally weakening during the early morning hours of June 20th. A tree was blown down on Highway 43 about a mile and a half north of the Tatum city limits.", "ts_dict_index": [10713, 10714, 10715]}
+{"event_id": 828156, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-06-19 05:34:00", "end_date_time": "2019-06-19 05:34:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. These storms also spawned a brief, weak tornado over Harrison County just northwest of the Nesbitt community. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across East Texas. The storms produced damaging winds and large hail, with localized flash flooding in Northeast Wood County before finally weakening during the early morning hours of June 20th. A tree was blown down on County Road 241 just off of FM 124 near Beckville.", "ts_dict_index": [10722, 10723, 10724]}
+{"event_id": 828151, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-06-19 05:00:00", "end_date_time": "2019-06-19 05:00:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. These storms also spawned a brief, weak tornado over Harrison County just northwest of the Nesbitt community. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across East Texas. The storms produced damaging winds and large hail, with localized flash flooding in Northeast Wood County before finally weakening during the early morning hours of June 20th. A NWS Storm Survey confirmed straight line wind damage along Highway 154 and Haynes Road. Numerous trees fell into homes, with the majority of the damage focused along Highway 154. The most significant structural damage was found along Haynes Road west of Nesbitt. It was here where a barn and carport had their metal panels completely removed from their roofs with the metal wrapped around nearby trees.", "ts_dict_index": [10719, 10720, 10721]}
+{"event_id": 828154, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-06-19 05:27:00", "end_date_time": "2019-06-19 05:27:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. These storms also spawned a brief, weak tornado over Harrison County just northwest of the Nesbitt community. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across East Texas. The storms produced damaging winds and large hail, with localized flash flooding in Northeast Wood County before finally weakening during the early morning hours of June 20th. Several signs and a billboard were damaged by thunderstorm winds at the intersection of Highway 59 and Highway 80.", "ts_dict_index": [10728, 10729, 10730]}
+{"event_id": 828153, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-06-19 05:26:00", "end_date_time": "2019-06-19 05:26:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. These storms also spawned a brief, weak tornado over Harrison County just northwest of the Nesbitt community. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across East Texas. The storms produced damaging winds and large hail, with localized flash flooding in Northeast Wood County before finally weakening during the early morning hours of June 20th. A tree was blown down onto a home on East Rusk Street.", "ts_dict_index": [10731, 10732, 10733]}
+{"event_id": 829382, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-06-19 21:28:00", "end_date_time": "2019-06-19 21:28:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. These storms also spawned a brief, weak tornado over Harrison County just northwest of the Nesbitt community. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across East Texas. The storms produced damaging winds and large hail, with localized flash flooding in Northeast Wood County before finally weakening during the early morning hours of June 20th. Trees were downed in Karnack.", "ts_dict_index": [10710, 10711, 10712]}
+{"event_id": 1057185, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-11-04 22:06:00", "end_date_time": "2022-11-04 22:06:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. Trees were blown down across multiple locations in Southern Webster Parish, including the Heflin area.", "ts_dict_index": [10707, 10708, 10709]}
+{"event_id": 829361, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2019-06-19 22:11:00", "end_date_time": "2019-06-19 22:11:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. Several trees and power lines were downed near Sarepta.", "ts_dict_index": [10740, 10741, 10742]}
+{"event_id": 1057182, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-11-04 20:46:00", "end_date_time": "2022-11-04 20:46:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. Multiple trees were blown down along Belcher Oil City Road.", "ts_dict_index": [10701, 10702, 10703]}
+{"event_id": 829359, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-06-19 22:01:00", "end_date_time": "2019-06-19 22:01:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. A NWS Storm Survey confirmed 100 mph straight line wind damage from a pronounced bow echo line of severe thunderstorms across Northeast Bossier Parish. These damaging winds produced intermittent swaths of damage where both hardwood and softwood trees were snapped and uprooted. Extensive tree damage was observed on Highway 157, Bodcau Dam Road, Whittington Road, and Young Road before crossing over into extreme Western Webster Parish.", "ts_dict_index": [10770, 10771, 10772]}
+{"event_id": 961975, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-17 21:20:00", "end_date_time": "2021-07-17 21:20:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. A weak tornado was confirmed in Burlington County, NJ in association with a line of thunderstorms in the later evening. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. An mPing report of a tree or large limbs down.", "ts_dict_index": [10821, 10822, 10823]}
+{"event_id": 880062, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-22 17:06:00", "end_date_time": "2020-04-22 17:06:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Shingles were blown off of a home in East Shreveport. Small limbs were snapped off of trees. Report from mPING.", "ts_dict_index": [10788, 10789, 10790]}
+{"event_id": 961979, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-17 21:27:00", "end_date_time": "2021-07-17 21:27:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. A weak tornado was confirmed in Burlington County, NJ in association with a line of thunderstorms in the later evening. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Several trees were downed in Evesham Twp. Time estimated from radar.", "ts_dict_index": [10803, 10804, 10805]}
+{"event_id": 880058, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-22 16:42:00", "end_date_time": "2020-04-22 16:42:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Shingles were blown off of a home in North Bossier City. Tree limbs were snapped as well. Report from mPING.", "ts_dict_index": [10791, 10792, 10793]}
+{"event_id": 961978, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-17 21:32:00", "end_date_time": "2021-07-17 21:32:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. A weak tornado was confirmed in Burlington County, NJ in association with a line of thunderstorms in the later evening. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. A large tree was snapped and several large limbs were downed. Time estimated from radar.", "ts_dict_index": [10818, 10819, 10820]}
+{"event_id": 1061290, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-12-13 12:20:00", "end_date_time": "2022-12-13 12:20:00", "narrative": "A strong upper level low pressure system shifted northeast out of the Central Rockies across Eastern Colorado and Northwest Kansas during the day on December 13th, which allowed for surface low pressure to develop along an attendant cold front that extended south across Western Kansas into Western Oklahoma and Northwest Texas. Meanwhile, a tightening pressure gradient ahead of the front resulted in strong southerly low level winds across the Southern Plains and Lower Mississippi Valley, with an increase in warmer, more humid and unstable air spreading back north into East Texas and the Lower Mississippi Valley. Large scale forcing increased during the afternoon across East Texas ahead of the approaching upper trough, along a dry line that had mixed east ahead of the cold front. Thus, scattered showers and thunderstorms developed across much of East Texas, some of which became severe as they tapped the strongly sheared air mass in place and the better instability contributed from daytime heating. Several reports of damaging winds which downed trees were received across East Texas, and spawned an isolated tornado over Northern Panola and Southern Harrison Counties near the Elysian Fields community, before lifting prior to reaching Caddo Parish in Northwest Louisiana. Several trees were downed and mobile home covers were damaged along CR 317 just south of FM 16. Fences and telephone poles were also snapped.", "ts_dict_index": [10773, 10774, 10775]}
+{"event_id": 961977, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-17 21:14:00", "end_date_time": "2021-07-17 21:14:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. A weak tornado was confirmed in Burlington County, NJ in association with a line of thunderstorms in the later evening. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Numerous tree limbs were down with power outages reported in Edgewater Park. Time estimated from radar. Public report relayed by off duty NWS employee.", "ts_dict_index": [10800, 10801, 10802]}
+{"event_id": 1114466, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "CLAY", "begin_date_time": "2023-07-28 17:03:00", "end_date_time": "2023-07-28 17:03:00", "narrative": "An upper ridge was over most of the southern half of the country. A weak upper level disturbance was moving across northern Nebraska. A weak surface low pressure was across parts of south central Nebraska during the afternoon hours. Temperatures were in the mid 90s to triple digits, and dewpoints were in the upper 60s to lower 70s. Effective bulk shear values generally ranged from 30 to 45 knots, and most unstable CAPE was generally 4,000 to 6,000 J/kg. ||A storm developed and strengthened over south central Nebraska and produced 1.50 inch hail in Nuckolls County after 4 PM CDT. This storm went on to produce quarter and nickel size hail in the same county then moved south towards the Kansas border. The storm split as it was crossing the border with the northern storm remaining in Nebraska then weakening and the southern half of the storm moving into Kansas. Another storm moved into Hamilton County and produced hail up to two inches at 5:40 PM CDT. This storm moved into Clay County after 6 PM CDT and produced two inch hail along with 60 mph wind gusts. The storm continued to move south through Clay County and produced hail ranging in size from two to four inches. Finally, the storm crossed over into Fillmore County and produced golf ball sized hail at 7 PM CDT. Wind gusts estimated to be near 60 MPH were accompanied by hail up to two inches in diameter.", "ts_dict_index": [10827, 10828, 10829]}
+{"event_id": 961962, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-17 19:55:00", "end_date_time": "2021-07-17 19:55:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. A weak tornado was confirmed in Burlington County, NJ in association with a line of thunderstorms in the later evening. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Measured by cwop station ew8027.", "ts_dict_index": [10809, 10810, 10811]}
+{"event_id": 961980, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2021-07-17 21:02:00", "end_date_time": "2021-07-17 21:02:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. A weak tornado was confirmed in Burlington County, NJ in association with a line of thunderstorms in the later evening. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. A few trees were blown down in a Cherry Hill neighborhood.", "ts_dict_index": [10806, 10807, 10808]}
+{"event_id": 832448, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-06-23 17:08:00", "end_date_time": "2019-06-23 17:08:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. Trees were downed on Highway 162 east of Benton.", "ts_dict_index": [10836, 10837, 10838]}
+{"event_id": 961972, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-17 19:25:00", "end_date_time": "2021-07-17 19:25:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. A weak tornado was confirmed in Burlington County, NJ in association with a line of thunderstorms in the later evening. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Several trees were blown down. Time estimated from radar.", "ts_dict_index": [10824, 10825, 10826]}
+{"event_id": 961982, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-17 19:20:00", "end_date_time": "2021-07-17 19:20:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. A weak tornado was confirmed in Burlington County, NJ in association with a line of thunderstorms in the later evening. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Several large trees were downed. Time estimated from radar.", "ts_dict_index": [10812, 10813, 10814]}
+{"event_id": 832441, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-23 16:27:00", "end_date_time": "2019-06-23 16:27:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. A tree was blown down at the intersection of Highway 169 and South Lakeshore Drive.", "ts_dict_index": [10842, 10843, 10844]}
+{"event_id": 880063, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-04-22 17:20:00", "end_date_time": "2020-04-22 17:20:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. A few trees and a fence were blown over in the Town South subdivision.", "ts_dict_index": [10794, 10795, 10796]}
+{"event_id": 961976, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-17 21:10:00", "end_date_time": "2021-07-17 21:10:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. A weak tornado was confirmed in Burlington County, NJ in association with a line of thunderstorms in the later evening. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Several large limbs were blown down. Time estimated from radar.", "ts_dict_index": [10797, 10798, 10799]}
+{"event_id": 961981, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-17 21:20:00", "end_date_time": "2021-07-17 21:20:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. A weak tornado was confirmed in Burlington County, NJ in association with a line of thunderstorms in the later evening. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Several large tree limbs were downed in Burlington.", "ts_dict_index": [10815, 10816, 10817]}
+{"event_id": 880238, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-04-22 13:39:00", "end_date_time": "2020-04-22 13:39:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. A tree was blown down across Highway 42.", "ts_dict_index": [10776, 10777, 10778]}
+{"event_id": 880068, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-04-22 17:35:00", "end_date_time": "2020-04-22 17:35:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Trees were downed in Minden.", "ts_dict_index": [10785, 10786, 10787]}
+{"event_id": 884321, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2020-05-20 16:30:00", "end_date_time": "2020-05-20 16:30:00", "narrative": "A warm front lifting northeast into portions of East Texas and Westcentral Louisiana near or just east of the Sabine River during the morning hours of May 20th became stationary by midday, as a weak upper level disturbance rounded a closed upper low pressure system over the Tennessee Valley. Convergence and moisture pooling near this surface boundary and weak large scale forcing aloft contributed to areas of showers and thunderstorms developing from late morning through much of the afternoon near and just south of the front, as they continued to move southeast repeatedly over the same areas of Westcentral Louisiana. This environment resulted in efficient rainfall producers, with a narrow axis of 2-6 inch rains falling over Eastern Sabine, Southeast Desoto, and Western Natchitoches Parishes, with isolated higher amounts exceeding 11 inches along the Sabine/Natchitoches Parish line. Flash flooding was observed across these areas, before the rains diminished by late afternoon/early evening. In addition, some diurnal heating occurred within this area, contributing to moderate instability near the front as well, with isolated severe thunderstorms producing large hail over portions of Eastern Sabine and Western Natchitoches Parishes during the mid-afternoon hours. Power lines were downed along Highway 117.", "ts_dict_index": [10830, 10831, 10832]}
+{"event_id": 832453, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2019-06-23 17:27:00", "end_date_time": "2019-06-23 17:27:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. Trees were downed just north of Dixie Inn along Doc Steed Road.", "ts_dict_index": [10845, 10846, 10847]}
+{"event_id": 880067, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-04-22 17:30:00", "end_date_time": "2020-04-22 17:30:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. Trees were downed just east of Doyline.", "ts_dict_index": [10782, 10783, 10784]}
+{"event_id": 832450, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2019-06-23 17:37:00", "end_date_time": "2019-06-23 17:37:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. Trees were blown down at the intersection of Dorcheat Road and Highway 160.", "ts_dict_index": [10839, 10840, 10841]}
+{"event_id": 828823, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-06-19 06:15:00", "end_date_time": "2019-06-19 06:15:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. A tree was blown down on Norman Place in the Shady Grove subdivision of Bossier City.", "ts_dict_index": [10767, 10768, 10769]}
+{"event_id": 832439, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-23 16:24:00", "end_date_time": "2019-06-23 16:24:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. A telephone pole was blown down across Greenwood Road (Highway 79) at the corner of Rice Road.", "ts_dict_index": [10848, 10849, 10850]}
+{"event_id": 832445, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-06-23 16:55:00", "end_date_time": "2019-06-23 16:55:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. A tree was downed onto a power line near the intersection of Old Brownlee Road and Wemple Road.", "ts_dict_index": [10851, 10852, 10853]}
+{"event_id": 828157, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-06-19 05:50:00", "end_date_time": "2019-06-19 05:50:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. These storms also spawned a brief, weak tornado over Harrison County just northwest of the Nesbitt community. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across East Texas. The storms produced damaging winds and large hail, with localized flash flooding in Northeast Wood County before finally weakening during the early morning hours of June 20th. Power lines were downed near Carthage, with two transformers damaged. One transformer caught fire on Highway 79 north just beyond the Carthage city limits, with a second transformer smoking along County Road 301 across from the DCP Plant.", "ts_dict_index": [10725, 10726, 10727]}
+{"event_id": 832447, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-06-23 16:49:00", "end_date_time": "2019-06-23 16:49:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. Trees were downed in the East Bank District of Bossier City.", "ts_dict_index": [10854, 10855, 10856]}
+{"event_id": 832449, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2019-06-23 17:29:00", "end_date_time": "2019-06-23 17:29:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. Trees were blown down on Highway 371 near the Golf Course in the Cullen community.", "ts_dict_index": [10857, 10858, 10859]}
+{"event_id": 832444, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-23 16:42:00", "end_date_time": "2019-06-23 16:42:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. A power line was downed at the intersection of Corbitt Street and Fairfax Avenue.", "ts_dict_index": [10833, 10834, 10835]}
+{"event_id": 819403, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-05-08 14:54:00", "end_date_time": "2019-05-08 14:54:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. A tree was snapped and large limbs were downed on Hoover Drive just off of Line Avenue in Shreveport.", "ts_dict_index": [10878, 10879, 10880]}
+{"event_id": 832461, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-23 17:52:00", "end_date_time": "2019-06-23 17:52:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. A tree was blown down onto Mira Scotts Slough Road between Highway 71 and Gilliam Scotts Slough Road.", "ts_dict_index": [10863, 10864, 10865]}
+{"event_id": 832443, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-06-23 16:41:00", "end_date_time": "2019-06-23 16:41:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. A power line was downed on Missouri Avenue between Myrtle Street and Logan Street.", "ts_dict_index": [10866, 10867, 10868]}
+{"event_id": 819408, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2019-05-08 16:10:00", "end_date_time": "2019-05-08 16:10:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. Several trees were blown down on Crossroads Church Road northwest of Robeline. A portion of a metal roof was ripped off of a chicken house off of Allen-Marthaville Road.", "ts_dict_index": [10875, 10876, 10877]}
+{"event_id": 832463, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2019-06-24 00:16:00", "end_date_time": "2019-06-24 00:16:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destablized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of June 24th. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of North Louisiana. Pictures from social media revealed structural damage to the River of Life Church in Goldonna.", "ts_dict_index": [10872, 10873, 10874]}
+{"event_id": 819404, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-05-08 14:57:00", "end_date_time": "2019-05-08 14:57:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. Wind gusts to 60 mph were estimated in the University Terrace subdivision in Southeast Shreveport.", "ts_dict_index": [10884, 10885, 10886]}
+{"event_id": 819409, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2019-05-08 16:15:00", "end_date_time": "2019-05-08 16:15:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. Numerous trees were snapped or uprooted along Brandon Cotton Road and also along Highway 485.", "ts_dict_index": [10881, 10882, 10883]}
+{"event_id": 880254, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-04-22 16:18:00", "end_date_time": "2020-04-22 16:18:00", "narrative": "An upper level trough ejected east-northeast across the Oklahoma/Texas Panhandles during the morning of April 22nd, before shifting across much of Oklahoma during the afternoon. Meanwhile, a warm front over Central and Southeast Texas into Southern Louisiana lifted slowly north into portions of East Texas and Central Louisiana during the afternoon. Large scale forcing quickly increased ahead of this trough such that showers and thunderstorms developed near and north of the front during the day, where cold temperatures aloft ahead of the trough and north of the warm front contributed to steep lapse rates, resulting in slightly elevated showers and thunderstorms to develop over much of East Texas and North Louisiana. The storms over Deep East Texas and the southern sections of North Central Louisiana near the front which were rooted closer to the surface became severe, producing more in the way of damaging winds and large hail, with storms farther north across Northwest Louisiana more elevated, producing more sporadic wind damage and large hail. Locally heavy rainfall over relatively saturated grounds also resulted in instances of flash flooding as well. These storms eventually pushed out of the region during the evening hours, with the passage of a weak cold front. A tree was downed on Floyd Evans Road and Old Town Road north of Elysian Fields.", "ts_dict_index": [10779, 10780, 10781]}
+{"event_id": 1005786, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2022-01-17 01:20:00", "end_date_time": "2022-01-17 01:20:00", "narrative": "A strong storm affected the mid-Atlantic and much of the Eastern Seaboard from January 16-17, 2022. A strong negative tilt trough over the Southeast US spurred strong cyclogenesis near the Carolina coast late on January 16. This low would proceed to quickly deepen as it moved northward that evening and night. Upper level steering patterns caused the low to take an ���inside runner��� track which kept the low center inland of the coast. A very strong easterly low level jet developed in between the strengthening low and a departing high pressure center to the north. With the center of the low tracking west of the region and an influx of marine air courtesy of the low level jet, various precipitation types occurred during this event. An Arctic air mass had been in place in advance of this system, but due to the aforementioned factors, that air mass rapidly modified on the 16th. As precipitation arrived, temperatures remained cold enough for it to begin as snow in most areas away from the coast. However, a rapid transition from snow to mixed precipitation to rain occurred in most areas within hours. Frozen precipitation held on for longer across the interior, where some higher snowfall amounts occurred. The storm departed the region by early on January 17. A significant wind damage event occurred near and just north of Tuckerton NJ. Downed wires were reported on US-9 near Green St with all lanes closed. The most notable damage occurred a little further north, close to Freedom Fields County Park. Areal footage shot via a drone confirmed at least several dozen trees were snapped or uprooted in a wooden area. The pattern of damage was visually consistent with straight line wind damage. Time estimated from radar.", "ts_dict_index": [10890, 10891, 10892]}
+{"event_id": 810856, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-03-03 20:20:00", "end_date_time": "2019-03-03 20:20:00", "narrative": "This event featured all modes of severe weather in our forecast area, including 13 tornadoes, numerous reports of straight-line wind damage, and even large hail. The 13 tornadoes consisted of 1 EF3, 2 EF2s, 6 EF1s, and 4 EF0s. This is a very high number of tornadoes for our forecast area for a single event. This compares with 7 tornadoes in the 1/22/17 event, 8 tornadoes in the 1/2/17 event, and 10 tornadoes in the 3/1/07 event. This may have been the most tornadoes for a single event in our area since the Hurricane Ivan tornadoes back in 2004. The synoptic pattern was characterized by a fast-moving upper trough through relatively zonal flow. The forecast area was under the favorable right entrance region of the upper jet with lots of upper level divergence. An 850 mb jet near or in excess of 50 knots was also present, which is another typical ingredient for severe weather in this part of the country in the cool season. Cool season levels of shear (0-1 km shear > 30 knots and 0-6 km shear > 50 knots) were overlaid with moderate levels of instability (SBCAPE  1500 j/kg), as opposed to more typical winter SBCAPE < 500 j/kg. Without this strong low-level jet, the low-level shear values would have been weaker and we would have probably seen less tornadoes. Trees and power lines were blown down on Mahan Drive.", "ts_dict_index": [10896, 10897, 10898]}
+{"event_id": 813819, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-04-18 04:26:00", "end_date_time": "2019-04-18 04:26:00", "narrative": "A strong upper level trough shifted east into Western Texas and Oklahoma during the early morning hours of April 17th, entering Central Oklahoma and Texas during the afternoon. This trough allowed the dry line to mix east across Central Texas during the afternoon ahead of an associated cold front, while southerly winds increased across the Ark-La-Tex, returning warm, moist, and unstable air back north across much of the region. Large scale forcing increased across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana during the evening through the early morning hours on the 17th-18th, resulting in showers and thunderstorms becoming more numerous while spreading north northeast across the area. Steep mid level lapse rates and strong wind shear had spread east across the region ahead of the trough and associated cold front, such that scattered strong to severe thunderstorms developed, resulting in damaging winds which downed trees across portions of Shreveport, as well as in the Cloutierville community in Southern Natchitoches Parish. These storms weakened by mid-morning and diminished from west to east during the daytime hours on April 18th, as the cold front had pushed through the area returning cooler and drier air into the region. Numerous trees were blown down on East Ratcliff Street, some of which had fallen on at least a dozen homes and some vehicles near Querbes Park Golf Course. Other trees were downed on East Elmwood, and across a 4-5 block area near and west of Youree Drive.", "ts_dict_index": [10902, 10903, 10904]}
+{"event_id": 808467, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-03-02 07:25:00", "end_date_time": "2019-03-02 07:25:00", "narrative": "This event featured all modes of severe weather in our forecast area, including 13 tornadoes, numerous reports of straight-line wind damage, and even large hail. The 13 tornadoes consisted of 1 EF3, 2 EF2s, 6 EF1s, and 4 EF0s. This is a very high number of tornadoes for our forecast area for a single event. This compares with 7 tornadoes in the 1/22/17 event, 8 tornadoes in the 1/2/17 event, and 10 tornadoes in the 3/1/07 event. This may have been the most tornadoes for a single event in our area since the Hurricane Ivan tornadoes back in 2004. The synoptic pattern was characterized by a fast-moving upper trough through relatively zonal flow. The forecast area was under the favorable right entrance region of the upper jet with lots of upper level divergence. An 850 mb jet near or in excess of 50 knots was also present, which is another typical ingredient for severe weather in this part of the country in the cool season. Cool season levels of shear (0-1 km shear > 30 knots and 0-6 km shear > 50 knots) were overlaid with moderate levels of instability (SBCAPE  1500 j/kg), as opposed to more typical winter SBCAPE < 500 j/kg. Without this strong low-level jet, the low-level shear values would have been weaker and we would have probably seen less tornadoes. Debris covered Springhill Road for at least 2 miles south of the Tallahassee airport.  Twisted and broken trees were also reported.", "ts_dict_index": [10887, 10888, 10889]}
+{"event_id": 1008679, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-03-21 21:17:00", "end_date_time": "2022-03-21 21:17:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. A 61 mph wind gust was measured at Tyler Pounds Field Airport.", "ts_dict_index": [10905, 10906, 10907]}
+{"event_id": 983670, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 22:53:00", "end_date_time": "2021-08-16 22:53:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. The Phoenix Sky Harbor ASOS recorded a 69 mph gust.", "ts_dict_index": [10914, 10915, 10916]}
+{"event_id": 983858, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:15:00", "end_date_time": "2021-08-16 23:15:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. A weather station located at the Gila River Valley Lookout on South Mountain measured a 75.6 mph gust.", "ts_dict_index": [10908, 10909, 10910]}
+{"event_id": 983862, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:14:00", "end_date_time": "2021-08-16 23:14:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. A social media photo showed a large uprooted tree down on a carport at an apartment complex. No injuries or damaged cars were reported. Timing was estimated using radar.", "ts_dict_index": [10917, 10918, 10919]}
+{"event_id": 983863, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:14:00", "end_date_time": "2021-08-16 23:14:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Photos on social media showed a large tree approximately 40-50 feet tall snapped in half near 35th Avenue and Peoria Avenue. No injuries were reported.", "ts_dict_index": [10920, 10921, 10922]}
+{"event_id": 983861, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:08:00", "end_date_time": "2021-08-16 23:08:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Photos on social media showed a large uprooted tree along Alma School Road between Ray Road and Chandler Boulevard, causing damage to a block wall along with knocking down a light pole. No injuries were reported.", "ts_dict_index": [10923, 10924, 10925]}
+{"event_id": 983666, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-16 22:20:00", "end_date_time": "2021-08-16 22:20:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. A mature lemon tree along with multiple smaller trees with trunks approximately 8-10 inches in diameter were uprooted or broken. A saguaro was also pulled out of the ground. Timing was estimated using radar. No injuries were reported.", "ts_dict_index": [10911, 10912, 10913]}
+{"event_id": 1005787, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2022-01-17 01:21:00", "end_date_time": "2022-01-17 01:21:00", "narrative": "A strong storm affected the mid-Atlantic and much of the Eastern Seaboard from January 16-17, 2022. A strong negative tilt trough over the Southeast US spurred strong cyclogenesis near the Carolina coast late on January 16. This low would proceed to quickly deepen as it moved northward that evening and night. Upper level steering patterns caused the low to take an ���inside runner��� track which kept the low center inland of the coast. A very strong easterly low level jet developed in between the strengthening low and a departing high pressure center to the north. With the center of the low tracking west of the region and an influx of marine air courtesy of the low level jet, various precipitation types occurred during this event. An Arctic air mass had been in place in advance of this system, but due to the aforementioned factors, that air mass rapidly modified on the 16th. As precipitation arrived, temperatures remained cold enough for it to begin as snow in most areas away from the coast. However, a rapid transition from snow to mixed precipitation to rain occurred in most areas within hours. Frozen precipitation held on for longer across the interior, where some higher snowfall amounts occurred. The storm departed the region by early on January 17. ", "ts_dict_index": [10893, 10894, 10895]}
+{"event_id": 983678, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:10:00", "end_date_time": "2021-08-16 23:10:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. A photo on social media showed a large uprooted tree down on some power lines near 15th Avenue and Glendale Avenue. No injuries were reported.", "ts_dict_index": [10938, 10939, 10940]}
+{"event_id": 983668, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-16 22:45:00", "end_date_time": "2021-08-16 23:00:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. A large tree approximately 4 feet in diameter was uprooted near Oasis Lane and Hunt Highway. Additional large trees were reported down in a nearby subdivision. Reduced visibility was also reported due to blowing dust. Timing was estimated using radar. No injuries were reported.", "ts_dict_index": [10926, 10927, 10928]}
+{"event_id": 983686, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:04:00", "end_date_time": "2021-08-16 23:04:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Photos on social media showed downed power poles near 44th Street and Indian School Road. Additional photos showed a couple of snapped palm trees down in the same area causing severe damage to a vehicle as well as to the the gate of a driveway. No injuries were reported.", "ts_dict_index": [10956, 10957, 10958]}
+{"event_id": 983864, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 22:45:00", "end_date_time": "2021-08-16 22:45:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. A large uprooted tree was reported to have caused damage to a brick wall and a sprinkler system at a home near Cactus Road and 101st Street. No injuries were reported.", "ts_dict_index": [10965, 10966, 10967]}
+{"event_id": 1026036, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-06-23 14:25:00", "end_date_time": "2022-06-23 14:25:00", "narrative": "An upper-level low located over the Great Basin produced cooler than normal 500 mb temperature of between -9 and -10C and also some upper-level diffluence with a 50-60 kt jet at upper-levels. Moisture levels were also above normal with precipitable water values between 1.0-1.3 inches. The combination of all of these factors resulted in sufficient instability with MLCAPE values approaching 1000 J/KG while DCAPE values were approaching 1500 J/KG. Thunderstorms began to develop during the early to mid-afternoon hours across most of southern and central Arizona, with strong to locally damaging winds as well as dense blowing dust being the main hazards along with locally heavy rainfall. One of the damaged areas came just northwest of Stanfield, where there were multiple downed power poles as well as a rolled over RV. There were also visible photos from social media as well as from seasoned storm chasers of a couple of landspouts, one near damaged area just northwest of Stanfield and another over Buckeye. With respect to the landspout that developed just northwest of Stanfield, there was no confirmation that it was responsible for the damage observed, which most likely was due to downburst wind. No injuries were reported with these thunderstorms. Multiple reports from storm chasers and local media of multiple downed power poles, trees, flipped irrigation pivots, and a rolled RV along and just east of SR-347, northwest of Stanfield. The local utility company reported around 50 downed power poles across the area, most of which were blown toward the north. There was a confirmed landspout in the general area as well, however, there was no evidence that it was the cause of any of the damage. Therefore, the downburst winds are being treated as the official cause of the damages. Winds were estimated at around 70 mph after discussion with the utility company. No injuries were reported.", "ts_dict_index": [10932, 10933, 10934]}
+{"event_id": 983675, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:00:00", "end_date_time": "2021-08-16 23:00:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Photos on social media showed multiple trees uprooted along Cooper Road between Queen Creek Road and Ocotillo Road. No injuries were reported.", "ts_dict_index": [10962, 10963, 10964]}
+{"event_id": 983860, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 22:50:00", "end_date_time": "2021-08-16 23:00:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Helicopter footage from a local TV station showed a large uprooted tree down on a home near Scottsdale Road and Chaparral Road. Footage also showed another large tree down at a nearby apartment complex, resulting in damage to the pool area and to one of the apartment buildings. Approximately 1 mile to the northeast, a large tree 2 feet in diameter was reported to have snapped in half along 82nd Street across from Saguaro High School. No injuries were reported. Timing was estimated using radar.", "ts_dict_index": [10947, 10948, 10949]}
+{"event_id": 983676, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:04:00", "end_date_time": "2021-08-16 23:04:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Photos on social media showed a large tree down on power lines near Lower Buckeye Road between 67th Avenue and 75th Avenue. Timing of 60-65 mph winds was estimated using radar. No injuries were reported.", "ts_dict_index": [10971, 10972, 10973]}
+{"event_id": 983671, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 22:55:00", "end_date_time": "2021-08-16 22:55:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. A 68 mph gust was recorded by a trained weather spotter using a handheld anemometer near Baseline Road and Rural Road.", "ts_dict_index": [10941, 10942, 10943]}
+{"event_id": 983677, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:05:00", "end_date_time": "2021-08-16 23:05:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Videos on social media showed multiple trees down along Pecos Road between McQueen Road and Cooper Road in Chandler. Videos also showed a large tree in this area blocking a roadway requiring a large pickup truck to remove it. No injuries were reported.", "ts_dict_index": [10968, 10969, 10970]}
+{"event_id": 983734, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:59:00", "end_date_time": "2021-08-16 23:59:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. The Maricopa County Flood Control District Mobile AZ ALERT mesonet station recorded a 60 mph gust.", "ts_dict_index": [10974, 10975, 10976]}
+{"event_id": 983669, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-16 22:45:00", "end_date_time": "2021-08-16 23:00:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Multiple trees were reported down along Hunt Highway between Gary Road and Bella Vista Road. A fence was destroyed by a downed tree near Hunt Highway and Gantzel Road. No injuries were reported. Multiple trees were also reported to be uprooted along Charbray Drive between between Empire Boulevard and Skyline Drive. Timing was estimated using radar.", "ts_dict_index": [10929, 10930, 10931]}
+{"event_id": 983672, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-16 22:56:00", "end_date_time": "2021-08-16 22:56:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. A trained weather spotter recorded a 59 mph gust on a home weather station.", "ts_dict_index": [10977, 10978, 10979]}
+{"event_id": 983733, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:45:00", "end_date_time": "2021-08-16 23:45:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. Several downed trees were reported within neighborhoods surrounding Estrella Parkway and Yuma Road. The largest downed tree was approximately 40 feet tall. No injuries were reported.", "ts_dict_index": [10953, 10954, 10955]}
+{"event_id": 983681, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-16 23:16:00", "end_date_time": "2021-08-16 23:16:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. A downed power pole was reported near Ellsworth Road and Brown Road in Mesa. No injuries were reported.", "ts_dict_index": [10950, 10951, 10952]}
+{"event_id": 983683, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-16 23:16:00", "end_date_time": "2021-08-16 23:16:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. The Casa Grande Municipal Airport AWOS (KCGZ) recorded a 58 mph gust.", "ts_dict_index": [10935, 10936, 10937]}
+{"event_id": 983667, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-16 22:40:00", "end_date_time": "2021-08-16 22:40:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. The SRP Quail mesonet station recorded a 73 mph gust.", "ts_dict_index": [10944, 10945, 10946]}
+{"event_id": 983679, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-08-16 23:14:00", "end_date_time": "2021-08-16 23:14:00", "narrative": "A shortwave trough rotating through the region led to steepening lapse rates and increasingly unstable conditions across central Arizona on the 16th. With abundant moisture and high CAPE values in place, the environment was favorable for the development of strong to severe thunderstorms. Thunderstorms initially developed over the high terrain of eastern Arizona before racing toward the west/southwest into the lower deserts of south-central Arizona as a line of strong to severe thunderstorms. The main impacts associated with these thunderstorms occurred as they moved into the Phoenix metro, producing widespread damaging wind gusts. Multiple observations recorded wind gusts in excess of 60 mph with a few approaching 80 mph. Recently implemented damage threat categories for Severe Thunderstorm Warnings were put to the test with one destructive Severe Thunderstorm Warning being issued for 80 mph wind gusts for much of Phoenix. There were numerous reports of downed trees across the Valley as a result of the severe wind gusts. The strong winds also led to several reports of dense blowing dust in dust prone areas. Additionally, thunderstorms produced locally heavy rainfall that led to several instances of flash flooding. No injuries were reported. The SRP Randolph mesonet station near Coolidge recorded a 64 mph gust.", "ts_dict_index": [10959, 10960, 10961]}
+{"event_id": 813821, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2019-04-18 08:00:00", "end_date_time": "2019-04-18 08:00:00", "narrative": "A strong upper level trough shifted east into Western Texas and Oklahoma during the early morning hours of April 17th, entering Central Oklahoma and Texas during the afternoon. This trough allowed the dry line to mix east across Central Texas during the afternoon ahead of an associated cold front, while southerly winds increased across the Ark-La-Tex, returning warm, moist, and unstable air back north across much of the region. Large scale forcing increased across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana during the evening through the early morning hours on the 17th-18th, resulting in showers and thunderstorms becoming more numerous while spreading north northeast across the area. Steep mid level lapse rates and strong wind shear had spread east across the region ahead of the trough and associated cold front, such that scattered strong to severe thunderstorms developed, resulting in damaging winds which downed trees across portions of Shreveport, as well as in the Cloutierville community in Southern Natchitoches Parish. These storms weakened by mid-morning and diminished from west to east during the daytime hours on April 18th, as the cold front had pushed through the area returning cooler and drier air into the region. Trees were blown down on the south end of Highway 495 in the Cloutierville community.", "ts_dict_index": [10899, 10900, 10901]}
+{"event_id": 806407, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-03-25 02:13:00", "end_date_time": "2019-03-25 02:13:00", "narrative": "Warm and moist air began to return north across the Ark-La-Tex during the daytime hours on March 24th, ahead of an upper level shortwave trough that traversed east across Southern Oklahoma and North Texas. This resulted in scattered showers and thunderstorms developing during the evening over Southeast Oklahoma and portions of North Texas, where better instability developed earlier in the day in response to daytime heating. Despite the marginal instability near the surface, ample shear and forcing were noted aloft ahead of this approaching disturbance and associated cold front, where several supercell thunderstorms developed over these areas during the evening. Additional scattered severe thunderstorms spread east southeast into Northeast Texas and Southern McCurtain County Oklahoma during the late evening hours. Large hail reports were received across portions of these areas, before the storms organized into a cluster and surged southeast across portions of East Texas and Northwest Louisiana during the early morning hours on the 25th. Damaging winds became prevalent along this line of storms, although occasional reports of large hail were also received, before the storms weakened after 330 am once instability diminished even further. Small tree limbs were broken and some shingles were removed from the roof of a home in Shreveport. Report via mPING.", "ts_dict_index": [10989, 10990, 10991]}
+{"event_id": 1025662, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2022-05-05 13:30:00", "end_date_time": "2022-05-05 13:30:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms downed trees and power lines across portions of Northwest Louisiana before weakening by late afternoon, away from the stronger forcing along the cold front and closer to the upper low. Tree down on a home just southwest of Plain Dealing.", "ts_dict_index": [10998, 10999, 11000]}
+{"event_id": 1025664, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-05-05 15:12:00", "end_date_time": "2022-05-05 15:12:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms downed trees and power lines across portions of Northwest Louisiana before weakening by late afternoon, away from the stronger forcing along the cold front and closer to the upper low. Highway 169 just north of Blanchard Latex Road closed due to a fallen tree on power lines and across the roadway.", "ts_dict_index": [10995, 10996, 10997]}
+{"event_id": 1025659, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-05-05 12:47:00", "end_date_time": "2022-05-05 12:47:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms downed trees and power lines across portions of Northwest Louisiana before weakening by late afternoon, away from the stronger forcing along the cold front and closer to the upper low. Multiple trees down near Conley Lane east of Vivian.", "ts_dict_index": [10992, 10993, 10994]}
+{"event_id": 1145295, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-10-04 23:35:00", "end_date_time": "2023-10-04 23:35:00", "narrative": "A prolonged period of very heavy rainfall along with severe thunderstorms occurred on October 4th-5th across parts of Northeast Texas. Showers and thunderstorms with 1-3 inch per hour rainfall rates trained in the vicinity of a warm front, which was oriented across the Ark-La-Tex and in adjacent portions of Southeast Oklahoma and Northeast Louisiana. Deep convergence of moisture along the boundary resulted as the core of the low-level jet and associated moisture transport was directed due north from the Upper Texas coast. Other factors contributing to the heavy rainfall and severe storms included a sharp instability gradient with mean-layer CAPE values from 500-1500 J/kg, maximized precipitable water values from 2.0-2.2 inches and effective bulk shear of 25-30 knots. As a result, this area of Northeast Texas quickly became more favorable for increasing convective organization as multi-cell thunderstorms continued to train over the same areas from late morning throughout much of the afternoon and evening. Over time, flash flooding developed in areas impacted by 4-8 inch rainfall totals, most notably in and around the Texarkana metro area. Severe impacts from damaging wind gusts occurred farther south closer to the Interstate 20 corridor. Smith County Sheriff's Office reported power lines downed on the west side of Tyler.", "ts_dict_index": [10986, 10987, 10988]}
+{"event_id": 1145297, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-10-04 23:45:00", "end_date_time": "2023-10-04 23:45:00", "narrative": "A prolonged period of very heavy rainfall along with severe thunderstorms occurred on October 4th-5th across parts of Northeast Texas. Showers and thunderstorms with 1-3 inch per hour rainfall rates trained in the vicinity of a warm front, which was oriented across the Ark-La-Tex and in adjacent portions of Southeast Oklahoma and Northeast Louisiana. Deep convergence of moisture along the boundary resulted as the core of the low-level jet and associated moisture transport was directed due north from the Upper Texas coast. Other factors contributing to the heavy rainfall and severe storms included a sharp instability gradient with mean-layer CAPE values from 500-1500 J/kg, maximized precipitable water values from 2.0-2.2 inches and effective bulk shear of 25-30 knots. As a result, this area of Northeast Texas quickly became more favorable for increasing convective organization as multi-cell thunderstorms continued to train over the same areas from late morning throughout much of the afternoon and evening. Over time, flash flooding developed in areas impacted by 4-8 inch rainfall totals, most notably in and around the Texarkana metro area. Severe impacts from damaging wind gusts occurred farther south closer to the Interstate 20 corridor. Several trees downed in Tyler.", "ts_dict_index": [10983, 10984, 10985]}
+{"event_id": 1025661, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-05-05 13:27:00", "end_date_time": "2022-05-05 13:27:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms downed trees and power lines across portions of Northwest Louisiana before weakening by late afternoon, away from the stronger forcing along the cold front and closer to the upper low. Tree down in Springhill.", "ts_dict_index": [11001, 11002, 11003]}
+{"event_id": 1025660, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-05-05 13:26:00", "end_date_time": "2022-05-05 13:26:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms downed trees and power lines across portions of Northwest Louisiana before weakening by late afternoon, away from the stronger forcing along the cold front and closer to the upper low. Numerous trees and power lines down across several roads in Cotton Valley.", "ts_dict_index": [11004, 11005, 11006]}
+{"event_id": 1026035, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-06-23 13:55:00", "end_date_time": "2022-06-23 13:55:00", "narrative": "An upper-level low located over the Great Basin produced cooler than normal 500 mb temperature of between -9 and -10C and also some upper-level diffluence with a 50-60 kt jet at upper-levels. Moisture levels were also above normal with precipitable water values between 1.0-1.3 inches. The combination of all of these factors resulted in sufficient instability with MLCAPE values approaching 1000 J/KG while DCAPE values were approaching 1500 J/KG. Thunderstorms began to develop during the early to mid-afternoon hours across most of southern and central Arizona, with strong to locally damaging winds as well as dense blowing dust being the main hazards along with locally heavy rainfall. One of the damaged areas came just northwest of Stanfield, where there were multiple downed power poles as well as a rolled over RV. There were also visible photos from social media as well as from seasoned storm chasers of a couple of landspouts, one near damaged area just northwest of Stanfield and another over Buckeye. With respect to the landspout that developed just northwest of Stanfield, there was no confirmation that it was responsible for the damage observed, which most likely was due to downburst wind. No injuries were reported with these thunderstorms. Downed power pole. Winds were estimated at around 70 mph. No injuries were reported.", "ts_dict_index": [10980, 10981, 10982]}
+{"event_id": 832416, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-06-23 15:51:00", "end_date_time": "2019-06-23 15:51:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. Trees were blown down on a power line in front of a home on County Road 3032.", "ts_dict_index": [11037, 11038, 11039]}
+{"event_id": 1009536, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-03-22 01:35:00", "end_date_time": "2022-03-22 01:35:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable air north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into North Louisiana during the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas and North Louisiana, resulting in numerous reports of damaging winds. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. Several trees were downed in Minden. A tree was also downed on Highway 159 near Minden.", "ts_dict_index": [11052, 11053, 11054]}
+{"event_id": 832411, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-06-23 15:33:00", "end_date_time": "2019-06-23 15:33:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. Trees were downed at the intersection of Highway 79 and FM 1798.", "ts_dict_index": [11034, 11035, 11036]}
+{"event_id": 832421, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-06-23 16:24:00", "end_date_time": "2019-06-23 16:24:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. A tree was blown down blocking FM 1997 about 5 miles north of Loop 390.", "ts_dict_index": [11031, 11032, 11033]}
+{"event_id": 1009538, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-03-22 01:40:00", "end_date_time": "2022-03-22 01:40:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable air north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into North Louisiana during the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas and North Louisiana, resulting in numerous reports of damaging winds. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. A tree was blown down in Sibley. Another tree was downed on Lake Road near Diamond T Road south-southwest of Sibley.", "ts_dict_index": [11055, 11056, 11057]}
+{"event_id": 832434, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-06-23 15:33:00", "end_date_time": "2019-06-23 15:33:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. Trees were downed at the intersection of Highway 79, FM 1798, and Highway 42.", "ts_dict_index": [11025, 11026, 11027]}
+{"event_id": 832418, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-06-23 16:16:00", "end_date_time": "2019-06-23 16:16:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. Trees were blown down at the intersection of Highway 80 and FM 968 west of Marshall.", "ts_dict_index": [11019, 11020, 11021]}
+{"event_id": 1031879, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-05-05 12:30:00", "end_date_time": "2022-05-05 12:30:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms also produced a few isolated tornadoes across portions of Rusk and Western Panola Counties, with localized flash flooding observed across portions of Upshur and Panola Counties. Trees down on Highway 43 between Henderson and Tatum.", "ts_dict_index": [11010, 11011, 11012]}
+{"event_id": 832413, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-06-23 15:32:00", "end_date_time": "2019-06-23 15:32:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. Trees were downed at the intersection of FM 1798 and FM 840 in the Brachfield community.", "ts_dict_index": [11040, 11041, 11042]}
+{"event_id": 846612, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2019-09-21 19:40:00", "end_date_time": "2019-09-21 19:40:00", "narrative": "A severe thunderstorm produced low-end severe hail in Hebron early on this Monday evening, and produced winds strong enough to snap off a tree at its base. Around 5 PM CST, isolated thunderstorms began developed along a line from Hayes, KS to Hebron, NE to Sioux City, IA. Numerous other thunderstorms soon followed. Around 545 PM CST, a storm over Republic county Kansas crossed the state line into Thayer county. As this storm moved into Hebron, it produced hail up to the size of quarters, and snapped off a tree that was 2 ft in diameter. The health of the tree was unknown. No other damage was reported. Cell training from 6 to 8 PM CST, along with two other periods of heavy downpours, resulted in over 4 inches of rain in 12 hours in the town of Hubbell (6 PM to 6 AM).||These storms developed along a slow-moving cold front. At the upper-levels, a weak shortwave trough was moving through in moderately strong southwest flow. A longwave trough was over the West, with a subtropical high over Georgia. Just prior to the storm moving into Hebron, the temperature was in the middle 80s, with the dewpoint in the upper 60s. With a poor mid-level lapse rate, MLCAPE was only 1000 J/kg. Deep layer shear was about 30 kt. Tree damage was reported in Hubbell, including a 2 foot diameter tree of unknown health that was snapped at the base.", "ts_dict_index": [11049, 11050, 11051]}
+{"event_id": 832431, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-06-23 22:15:00", "end_date_time": "2019-06-23 22:15:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. Trees were downed blocking Highway 322 about 5-6 miles south of the Lakeport community.", "ts_dict_index": [11022, 11023, 11024]}
+{"event_id": 832415, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-06-23 15:50:00", "end_date_time": "2019-06-23 15:50:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. Trees were downed on FM 13 about 2 miles east of Price.", "ts_dict_index": [11043, 11044, 11045]}
+{"event_id": 832417, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-06-23 15:53:00", "end_date_time": "2019-06-23 15:53:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. A tree was blown down along Highway 80 near the Longview City limits.", "ts_dict_index": [11028, 11029, 11030]}
+{"event_id": 832423, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-06-23 16:26:00", "end_date_time": "2019-06-23 16:26:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. Power lines were downed along Highway 59 north in the Woodlawn community.", "ts_dict_index": [11046, 11047, 11048]}
+{"event_id": 881233, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-04-28 21:30:00", "end_date_time": "2020-04-28 21:30:00", "narrative": "A deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region during the afternoon and evening hours on April 28th, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Southeast Oklahoma into Northeast Texas, Southwest Arkansas, and North Louisiana just prior to midnight on the 29th. Wind gusts were estimated near 65 mph in Eagletown.", "ts_dict_index": [11058, 11059, 11060]}
+{"event_id": 1025663, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-05-05 14:55:00", "end_date_time": "2022-05-05 14:55:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms downed trees and power lines across portions of Northwest Louisiana before weakening by late afternoon, away from the stronger forcing along the cold front and closer to the upper low. Multiple trees and power lines down across Caddo Parish including the city of Shreveport.", "ts_dict_index": [11007, 11008, 11009]}
+{"event_id": 1085001, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-05 08:22:00", "end_date_time": "2023-04-05 08:22:00", "narrative": "An upper low pressure system over the Four Corners Region ejected northeast through the Southern Rockies into the Central Plains by the afternoon of April 5th, which reinforced a cold front southeast into East Texas, Southwest Arkansas, and North Louisiana before stalling out late in the day. Large scale ascent increased along and ahead of the front and the ejecting upper low, which had tapped into a warm and moderately unstable air mass that had pooled north from the Gulf of Mexico ahead of the front. This resulted in numerous shower and thunderstorm development during the morning around and after daybreak over Northeast Texas and Southwest Arkansas, which eventually moved into portions of extreme Northwest Louisiana by late morning/early afternoon. Some of these storms became severe, with damaging winds and large hail observed. While these storms eventually weakened by mid-afternoon, additional redevelopment occurred along the slowing front farther south of I-20 in East Texas and North Louisiana by late afternoon and early evening as they tapped stronger instability, with isolated severe thunderstorms producing large hail affecting portions of Western Caddo Parish before weakening. Part of a roof was removed off of a home just west of Ida.", "ts_dict_index": [11067, 11068, 11069]}
+{"event_id": 813807, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-04-18 02:02:00", "end_date_time": "2019-04-18 02:02:00", "narrative": "A strong upper level trough shifted east into Western Texas and Oklahoma during the early morning hours of April 17th, entering Central Oklahoma and Texas during the afternoon. This trough allowed the dry line to mix east across Central Texas during the afternoon ahead of an associated cold front, while southerly winds increased across the Ark-La-Tex, returning warm, moist, and unstable air back north across much of the region. Large scale forcing increased across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana during the evening through the early morning hours on the 17th-18th, resulting in showers and thunderstorms becoming more numerous while spreading north northeast across the area. Steep mid level lapse rates and strong wind shear had spread east across the region ahead of the trough and associated cold front, such that scattered strong to severe thunderstorms developed, resulting in damaging winds which downed trees across portions of East Texas along and south of Interstate 20. These storms weakened by daybreak and diminished from west to east on April 18th, as the cold front had pushed through the area returning cooler and drier air into the region. Trees were downed at various locations throughout Tyler and Smith County, including the intersection of West Grande Avenue and Old Noonday Road.", "ts_dict_index": [11088, 11089, 11090]}
+{"event_id": 1052642, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-08-08 12:49:00", "end_date_time": "2022-08-08 12:49:00", "narrative": "As August began, drought conditions were widespread in Arkansas, with dryness the most noticeable in northern and western sections of the state. Above normal temperatures were also common. On the 8th, a cold front approached from the north, and brought chances of rain and promised temporary relief from the heat.||Ahead of the front, thermometers showed readings in the 90s. During peak heating, thunderstorms popped up quickly in the northern half of the state. Some of the storms cranked out damaging winds. Trees were downed at Gravel Ridge and Macon (both in Pulaski County), with one tree on a fence. More trees were toppled in west Little Rock (Pulaski County). The trees fell on power lines and a home, and power outages lasted into the overnight hours for some residents. Tree damage was also noted in Hot Springs (Garland County), and several utility poles were snapped. This was the most severe weather reported during the month.||Locations with an inch or more of rainfall were few and far between. Bogg Springs (Polk County) received 2.02 inches of rain, 1.16 inches at Mena (Polk County), 1.07 inches at Hot Springs (Garland County), and 1.00 inch at Batesville (Independence County). A large tree was knocked down onto a home on West Stoney Pointe Court in West Little Rock.", "ts_dict_index": [11097, 11098, 11099]}
+{"event_id": 1052645, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-08-08 13:21:00", "end_date_time": "2022-08-08 13:21:00", "narrative": "As August began, drought conditions were widespread in Arkansas, with dryness the most noticeable in northern and western sections of the state. Above normal temperatures were also common. On the 8th, a cold front approached from the north, and brought chances of rain and promised temporary relief from the heat.||Ahead of the front, thermometers showed readings in the 90s. During peak heating, thunderstorms popped up quickly in the northern half of the state. Some of the storms cranked out damaging winds. Trees were downed at Gravel Ridge and Macon (both in Pulaski County), with one tree on a fence. More trees were toppled in west Little Rock (Pulaski County). The trees fell on power lines and a home, and power outages lasted into the overnight hours for some residents. Tree damage was also noted in Hot Springs (Garland County), and several utility poles were snapped. This was the most severe weather reported during the month.||Locations with an inch or more of rainfall were few and far between. Bogg Springs (Polk County) received 2.02 inches of rain, 1.16 inches at Mena (Polk County), 1.07 inches at Hot Springs (Garland County), and 1.00 inch at Batesville (Independence County). Multiple trees, tree limbs, and tops of trees were snapped in the Hatcher Rd. area near Sherwood.", "ts_dict_index": [11094, 11095, 11096]}
+{"event_id": 813814, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-04-18 02:41:00", "end_date_time": "2019-04-18 02:41:00", "narrative": "A strong upper level trough shifted east into Western Texas and Oklahoma during the early morning hours of April 17th, entering Central Oklahoma and Texas during the afternoon. This trough allowed the dry line to mix east across Central Texas during the afternoon ahead of an associated cold front, while southerly winds increased across the Ark-La-Tex, returning warm, moist, and unstable air back north across much of the region. Large scale forcing increased across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana during the evening through the early morning hours on the 17th-18th, resulting in showers and thunderstorms becoming more numerous while spreading north northeast across the area. Steep mid level lapse rates and strong wind shear had spread east across the region ahead of the trough and associated cold front, such that scattered strong to severe thunderstorms developed, resulting in damaging winds which downed trees across portions of East Texas along and south of Interstate 20. These storms weakened by daybreak and diminished from west to east on April 18th, as the cold front had pushed through the area returning cooler and drier air into the region. Trees and power lines were blown down in Henderson.", "ts_dict_index": [11079, 11080, 11081]}
+{"event_id": 813812, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-04-18 02:35:00", "end_date_time": "2019-04-18 02:35:00", "narrative": "A strong upper level trough shifted east into Western Texas and Oklahoma during the early morning hours of April 17th, entering Central Oklahoma and Texas during the afternoon. This trough allowed the dry line to mix east across Central Texas during the afternoon ahead of an associated cold front, while southerly winds increased across the Ark-La-Tex, returning warm, moist, and unstable air back north across much of the region. Large scale forcing increased across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana during the evening through the early morning hours on the 17th-18th, resulting in showers and thunderstorms becoming more numerous while spreading north northeast across the area. Steep mid level lapse rates and strong wind shear had spread east across the region ahead of the trough and associated cold front, such that scattered strong to severe thunderstorms developed, resulting in damaging winds which downed trees across portions of East Texas along and south of Interstate 20. These storms weakened by daybreak and diminished from west to east on April 18th, as the cold front had pushed through the area returning cooler and drier air into the region. Trees down on Highway 42 near FM 850 in New London.", "ts_dict_index": [11085, 11086, 11087]}
+{"event_id": 954105, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-06-08 09:55:00", "end_date_time": "2021-06-08 09:55:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, moving over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. ||Additional scattered severe thunderstorms developed later in the morning farther south across East Texas, which resulted in downed trees and even a few weak, short-lived tornadoes. These storms progressed into North Louisiana around midday, downing additional trees before exiting the region by mid-afternoon. A tree was blown down on FM 782.", "ts_dict_index": [11076, 11077, 11078]}
+{"event_id": 813811, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-04-18 02:24:00", "end_date_time": "2019-04-18 02:24:00", "narrative": "A strong upper level trough shifted east into Western Texas and Oklahoma during the early morning hours of April 17th, entering Central Oklahoma and Texas during the afternoon. This trough allowed the dry line to mix east across Central Texas during the afternoon ahead of an associated cold front, while southerly winds increased across the Ark-La-Tex, returning warm, moist, and unstable air back north across much of the region. Large scale forcing increased across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana during the evening through the early morning hours on the 17th-18th, resulting in showers and thunderstorms becoming more numerous while spreading north northeast across the area. Steep mid level lapse rates and strong wind shear had spread east across the region ahead of the trough and associated cold front, such that scattered strong to severe thunderstorms developed, resulting in damaging winds which downed trees across portions of East Texas along and south of Interstate 20. These storms weakened by daybreak and diminished from west to east on April 18th, as the cold front had pushed through the area returning cooler and drier air into the region. Trees were blown down and structural damage occurred at the Carlisle ISD in the community of Price.", "ts_dict_index": [11082, 11083, 11084]}
+{"event_id": 881224, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-04-28 20:51:00", "end_date_time": "2020-04-28 20:51:00", "narrative": "A deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region during the afternoon and evening hours on April 28th, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Southeast Oklahoma into Northeast Texas, Southwest Arkansas, and North Louisiana just prior to midnight on the 29th. Metal roofing was peeled off of a few chicken houses just off of Battiest Pickens Road just east of the Pickens community.", "ts_dict_index": [11064, 11065, 11066]}
+{"event_id": 813816, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-04-18 03:00:00", "end_date_time": "2019-04-18 03:00:00", "narrative": "A strong upper level trough shifted east into Western Texas and Oklahoma during the early morning hours of April 17th, entering Central Oklahoma and Texas during the afternoon. This trough allowed the dry line to mix east across Central Texas during the afternoon ahead of an associated cold front, while southerly winds increased across the Ark-La-Tex, returning warm, moist, and unstable air back north across much of the region. Large scale forcing increased across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana during the evening through the early morning hours on the 17th-18th, resulting in showers and thunderstorms becoming more numerous while spreading north northeast across the area. Steep mid level lapse rates and strong wind shear had spread east across the region ahead of the trough and associated cold front, such that scattered strong to severe thunderstorms developed, resulting in damaging winds which downed trees across portions of East Texas along and south of Interstate 20. These storms weakened by daybreak and diminished from west to east on April 18th, as the cold front had pushed through the area returning cooler and drier air into the region. A tree was blown onto a home and the steeple was blown off of the First United Methodist Church in Tatum.", "ts_dict_index": [11091, 11092, 11093]}
+{"event_id": 881221, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-04-28 20:59:00", "end_date_time": "2020-04-28 20:59:00", "narrative": "A deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region during the afternoon and evening hours on April 28th, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Southeast Oklahoma into Northeast Texas, Southwest Arkansas, and North Louisiana just prior to midnight on the 29th. Trees were downed on along Highway 259 at the Bethel Triangle. Trees were down on homes near Bethel.", "ts_dict_index": [11061, 11062, 11063]}
+{"event_id": 881222, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-04-28 21:04:00", "end_date_time": "2020-04-28 21:04:00", "narrative": "A deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region during the afternoon and evening hours on April 28th, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Southeast Oklahoma into Northeast Texas, Southwest Arkansas, and North Louisiana just prior to midnight on the 29th. Trees were downed along Highway 259 between Bethel and Smithville.", "ts_dict_index": [11073, 11074, 11075]}
+{"event_id": 881223, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-04-28 20:51:00", "end_date_time": "2020-04-28 20:51:00", "narrative": "A deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region during the afternoon and evening hours on April 28th, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Southeast Oklahoma into Northeast Texas, Southwest Arkansas, and North Louisiana just prior to midnight on the 29th. A large tree was uprooted along Battiest Pickens Road.", "ts_dict_index": [11070, 11071, 11072]}
+{"event_id": 887326, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-05-25 16:57:00", "end_date_time": "2020-05-25 16:57:00", "narrative": "A strong shortwave trough lifted north across East-central Texas during the daytime hours of May 25th, ahead of a digging upper level trough of low pressure over the Rockies into far West Texas. Meanwhile, a surface low pressure area developed over Southeast Texas during the morning, and slowly lifted north across East-central Texas during the afternoon and evening hours beneath this shortwave trough. Showers and thunderstorms increased throughout the day near the surface low center over East Texas, with showers and storms more scattered farther south, east, and north of the center as moderate instability developed in response to daytime heating. As a result, some of these storms became severe over portions of the region, with damaging winds which downed trees, as well as isolated instances of hail reported as well. The counterclockwise circulation around the northern and eastern periphery of the surface low contributed to adequate wind shear within some of these storms to contribute to a brief waterspout over Toledo Bend Reservoir in Western Sabine Parish Louisiana. These storms eventually diminished during the mid and late evening hours with the loss of heating and instability. A tree was blown down in the Spring Ridge community near 4 Forks Road and Springridge Drive.", "ts_dict_index": [11106, 11107, 11108]}
+{"event_id": 1052643, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-08-08 13:16:00", "end_date_time": "2022-08-08 13:16:00", "narrative": "As August began, drought conditions were widespread in Arkansas, with dryness the most noticeable in northern and western sections of the state. Above normal temperatures were also common. On the 8th, a cold front approached from the north, and brought chances of rain and promised temporary relief from the heat.||Ahead of the front, thermometers showed readings in the 90s. During peak heating, thunderstorms popped up quickly in the northern half of the state. Some of the storms cranked out damaging winds. Trees were downed at Gravel Ridge and Macon (both in Pulaski County), with one tree on a fence. More trees were toppled in west Little Rock (Pulaski County). The trees fell on power lines and a home, and power outages lasted into the overnight hours for some residents. Tree damage was also noted in Hot Springs (Garland County), and several utility poles were snapped. This was the most severe weather reported during the month.||Locations with an inch or more of rainfall were few and far between. Bogg Springs (Polk County) received 2.02 inches of rain, 1.16 inches at Mena (Polk County), 1.07 inches at Hot Springs (Garland County), and 1.00 inch at Batesville (Independence County). A large tree fell across a fence in Macon.", "ts_dict_index": [11103, 11104, 11105]}
+{"event_id": 806145, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-03-14 03:45:00", "end_date_time": "2019-03-14 03:45:00", "narrative": "A moist and unstable airmass was present during the afternoon and evening hours of March 13th across portions of Northcentral and Northeast Louisiana. A dryline moved rapidly eastward across Northern Louisiana during the day with showers and thunderstorms erupting along and ahead of this feature. Upper level forcing was present due to a vigorous upper level trough which moved into the Plains earlier in the day. Very strong winds were present in the lower and mid levels of the atmosphere across the Lower Mississippi Valley and a few storms that developed ahead of the dryline across Northeast Louisiana took on supercell characteristics. Damaging wind gusts were reported with one of these storms across Eastern Union Parish Louisiana with a report of trees downed east of Farmerville.||During the early morning hours of March 14th, a line of strong to severe thunderstorms developed along a cold front across Eastcentral Texas along the base of the upper level trough, and marched east into Northwest Louisiana after 330 am. These storms produced damaging winds which downed trees and power lines across portions of Caddo and Claiborne Parishes before weakening prior to daybreak. Several trees were blown down in the Spring Ridge community.", "ts_dict_index": [11112, 11113, 11114]}
+{"event_id": 806143, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2019-03-13 17:30:00", "end_date_time": "2019-03-13 17:30:00", "narrative": "A moist and unstable airmass was present during the afternoon and evening hours of March 13th across portions of Northcentral and Northeast Louisiana. A dryline moved rapidly eastward across Northern Louisiana during the day with showers and thunderstorms erupting along and ahead of this feature. Upper level forcing was present due to a vigorous upper level trough which moved into the Plains earlier in the day. Very strong winds were present in the lower and mid levels of the atmosphere across the Lower Mississippi Valley and a few storms that developed ahead of the dryline across Northeast Louisiana took on supercell characteristics. Damaging wind gusts were reported with one of these storms across Eastern Union Parish Louisiana with a report of trees downed east of Farmerville.||During the early morning hours of March 14th, a line of strong to severe thunderstorms developed along a cold front across Eastcentral Texas along the base of the upper level trough, and marched east into Northwest Louisiana after 330 am. These storms produced damaging winds which downed trees and power lines across portions of Caddo and Claiborne Parishes before weakening prior to daybreak. Trees were downed along Highway 2.", "ts_dict_index": [11115, 11116, 11117]}
+{"event_id": 1052641, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-08-08 12:47:00", "end_date_time": "2022-08-08 12:47:00", "narrative": "As August began, drought conditions were widespread in Arkansas, with dryness the most noticeable in northern and western sections of the state. Above normal temperatures were also common. On the 8th, a cold front approached from the north, and brought chances of rain and promised temporary relief from the heat.||Ahead of the front, thermometers showed readings in the 90s. During peak heating, thunderstorms popped up quickly in the northern half of the state. Some of the storms cranked out damaging winds. Trees were downed at Gravel Ridge and Macon (both in Pulaski County), with one tree on a fence. More trees were toppled in west Little Rock (Pulaski County). The trees fell on power lines and a home, and power outages lasted into the overnight hours for some residents. Tree damage was also noted in Hot Springs (Garland County), and several utility poles were snapped. This was the most severe weather reported during the month.||Locations with an inch or more of rainfall were few and far between. Bogg Springs (Polk County) received 2.02 inches of rain, 1.16 inches at Mena (Polk County), 1.07 inches at Hot Springs (Garland County), and 1.00 inch at Batesville (Independence County). A large tree was knocked over onto power lines along Napa Valley Dr. on the western side of Little Rock.", "ts_dict_index": [11100, 11101, 11102]}
+{"event_id": 832600, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-06-23 18:30:00", "end_date_time": "2019-06-23 18:30:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. The remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, some of which were severe given the moderate instability that had developed with afternoon heating and the deep moisture in place. Damaging winds downed several trees in and near Broken Bow, with these thunderstorms also producing very heavy rainfall which moved repeatedly over the same areas of Southern McCurtain County. This resulted in widespread flash flooding which flooded numerous roads across this area before the stronger storms gradually shifted southeast into East Texas, Southwest Arkansas, and Northern Louisiana during the late evening into the overnight/early morning hours of June 24th. Several trees were downed in and near Broken Bow.", "ts_dict_index": [11118, 11119, 11120]}
+{"event_id": 832598, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-06-23 17:57:00", "end_date_time": "2019-06-23 17:57:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. The remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, some of which were severe given the moderate instability that had developed with afternoon heating and the deep moisture in place. Damaging winds downed several trees in and near Broken Bow, with these thunderstorms also producing very heavy rainfall which moved repeatedly over the same areas of Southern McCurtain County. This resulted in widespread flash flooding which flooded numerous roads across this area before the stronger storms gradually shifted southeast into East Texas, Southwest Arkansas, and Northern Louisiana during the late evening into the overnight/early morning hours of June 24th. Trees were blown down near Lukfata Baptist Church just west of Broken Bow.", "ts_dict_index": [11121, 11122, 11123]}
+{"event_id": 832433, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-06-23 22:30:00", "end_date_time": "2019-06-23 22:30:00", "narrative": "With the departure of an upper level ridge that resulted in oppressive heat across the Ark-La-Tex area in the preceding days, the upper flow aloft became more southwest during the daytime hours on June 23rd, ahead of an upper level trough and associated cold front that shifted east southeast across Oklahoma and Arkansas. Scattered to numerous showers and thunderstorms developed by mid and late afternoon across portions of East Texas and North Louisiana ahead of this upper trough and associated cold front, where the air mass destabilized significantly given the hot and humid air mass in place. Some of these storms were severe, which downed trees and power lines during the mid and late afternoon hours. Meanwhile, the remnants of a mesoscale convective system (MCS) that moved across Southern Kansas and Northern Oklahoma earlier that morning helped to initiate another complex of showers and thunderstorms by early evening over Southeast Oklahoma and Southwest Arkansas, which intensified across portions of East Texas, Southwest Arkansas, and North Louisiana during the evening hours. Some of these storms were also severe, producing damaging winds which also downed more trees and power lines across portions of East Texas. A tree was downed blocking the intersection of County Road 4135 and Highway 323.", "ts_dict_index": [11016, 11017, 11018]}
+{"event_id": 972302, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2021-09-01 17:40:00", "end_date_time": "2021-09-01 17:40:00", "narrative": "The remnants of Hurricane Ida impacted the mid-Atlantic on September 1, 2021. As it moved northward, Ida began transitioning to a strong mid-latitude cyclone with pronounced frontal features, but with continued tropical moisture. On a regional level, the remnants of Ida became one of the most severe natural disasters in US history, due to a combination of several tornadoes, some of them strong, as well as catastrophic flooding over a large and densely populated area. The severe weather threat unfolded as the system's developing warm front lifted northward from the Delmarva region into Pennsylvania and New Jersey. South of the warm front, partial clearing and moderate to strong instability developed. Meanwhile, very strong shear and forcing, along with tropical moisture, were present within the warm sector. The result was widespread convection in the form of both supercell and quasi-linear thunderstorms. A number of storms became severe across the region, producing several tornadoes and other instances of wind damage. This continued an exceptionally active stretch of high end severe weather in the region, coming barely a month after the tornado outbreak of July 29. Multiple trees and wires were downed around Cherry Hill. Time estimated from radar.", "ts_dict_index": [11124, 11125, 11126]}
+{"event_id": 1031881, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2022-05-05 14:15:00", "end_date_time": "2022-05-05 14:15:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms also produced a few isolated tornadoes across portions of Rusk and Western Panola Counties, with localized flash flooding observed across portions of Upshur and Panola Counties. Trees reported down in DeBerry.", "ts_dict_index": [11013, 11014, 11015]}
+{"event_id": 972304, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2021-09-01 17:40:00", "end_date_time": "2021-09-01 17:40:00", "narrative": "The remnants of Hurricane Ida impacted the mid-Atlantic on September 1, 2021. As it moved northward, Ida began transitioning to a strong mid-latitude cyclone with pronounced frontal features, but with continued tropical moisture. On a regional level, the remnants of Ida became one of the most severe natural disasters in US history, due to a combination of several tornadoes, some of them strong, as well as catastrophic flooding over a large and densely populated area. The severe weather threat unfolded as the system's developing warm front lifted northward from the Delmarva region into Pennsylvania and New Jersey. South of the warm front, partial clearing and moderate to strong instability developed. Meanwhile, very strong shear and forcing, along with tropical moisture, were present within the warm sector. The result was widespread convection in the form of both supercell and quasi-linear thunderstorms. A number of storms became severe across the region, producing several tornadoes and other instances of wind damage. This continued an exceptionally active stretch of high end severe weather in the region, coming barely a month after the tornado outbreak of July 29. Several softwood trees and utility poles were snapped, and there was loss of siding on some homes along Cuthbert Rd, Lees Ln, and Heather Rd. Damage occurred downstream of an earlier tornado, but it was inconclusive as to whether this was tornado damage and is believed more likely to be straight line wind.", "ts_dict_index": [11127, 11128, 11129]}
+{"event_id": 1119938, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:15:00", "end_date_time": "2023-07-28 19:25:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Wind gust of 66 mph reported from personal weather station.", "ts_dict_index": [11154, 11155, 11156]}
+{"event_id": 1119934, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:15:00", "end_date_time": "2023-07-28 19:30:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Trained spotter reported a 72 mph wind gust.", "ts_dict_index": [11151, 11152, 11153]}
+{"event_id": 1119937, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:24:00", "end_date_time": "2023-07-28 19:35:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Report from mping regarding power poles and small tree limbs broken from the winds.", "ts_dict_index": [11157, 11158, 11159]}
+{"event_id": 1119932, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:16:00", "end_date_time": "2023-07-28 19:25:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. ASOS at Cedar Rapids Airport reported a 69 mph wind gust.", "ts_dict_index": [11163, 11164, 11165]}
+{"event_id": 1119952, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:22:00", "end_date_time": "2023-07-28 19:30:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Mesonet station measured a 65 mph wind gust.", "ts_dict_index": [11178, 11179, 11180]}
+{"event_id": 972303, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-09-01 18:06:00", "end_date_time": "2021-09-01 18:06:00", "narrative": "The remnants of Hurricane Ida impacted the mid-Atlantic on September 1, 2021. As it moved northward, Ida began transitioning to a strong mid-latitude cyclone with pronounced frontal features, but with continued tropical moisture. On a regional level, the remnants of Ida became one of the most severe natural disasters in US history, due to a combination of several tornadoes, some of them strong, as well as catastrophic flooding over a large and densely populated area. The severe weather threat unfolded as the system's developing warm front lifted northward from the Delmarva region into Pennsylvania and New Jersey. South of the warm front, partial clearing and moderate to strong instability developed. Meanwhile, very strong shear and forcing, along with tropical moisture, were present within the warm sector. The result was widespread convection in the form of both supercell and quasi-linear thunderstorms. A number of storms became severe across the region, producing several tornadoes and other instances of wind damage. This continued an exceptionally active stretch of high end severe weather in the region, coming barely a month after the tornado outbreak of July 29. Measured by nos gauge bdrn4.", "ts_dict_index": [11130, 11131, 11132]}
+{"event_id": 1119933, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:20:00", "end_date_time": "2023-07-28 19:30:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Thunderstorm wind damage to mobile homes.", "ts_dict_index": [11160, 11161, 11162]}
+{"event_id": 1031270, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-05-21 20:20:00", "end_date_time": "2022-05-21 20:20:00", "narrative": "Scattered strong to severe storms formed into a line across portions of northwestern and northern Arkansas along and ahead of an advancing cold front. The line made it into central sections of the state by early evening, and into the south during the overnight hours of the 21st.||Dry weather and above normal temperatures returned to the state for a few days before yet another storm system would impact the state on the 21st. Ahead of a strong cold front, there was a risk of severe weather stretching from the Texas/Mexico border northeastward to the Maine/Canada border. Thunderstorms initially developed across north/northwest Arkansas before forming into a line and marching east. While a brief, weak tornado occurred across Newton County, the most widespread damage occurred across portions of north central into northeast Arkansas. Numerous trees were blown down from Sharp County into portions of Lawrence and Randolph Counties. Additional storms developed later during the evening of May 21st across portions of western into central and southern Arkansas. Severe weather reports weren't widespread, but a second brief tornado developed near Royal in Garland County. A tree was blown down and blocking one lane of traffic on I-430.", "ts_dict_index": [11142, 11143, 11144]}
+{"event_id": 1119924, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 18:58:00", "end_date_time": "2023-07-28 19:10:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Report of 70 mph wind gust from thunderstorm.", "ts_dict_index": [11166, 11167, 11168]}
+{"event_id": 1119951, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:10:00", "end_date_time": "2023-07-28 19:20:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Mesonet reported a 75 mph wind gust along Interstate 380.", "ts_dict_index": [11175, 11176, 11177]}
+{"event_id": 1120948, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:09:00", "end_date_time": "2023-07-28 19:20:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Tree limbs blown down, with shingles blown off. Report from mping.", "ts_dict_index": [11172, 11173, 11174]}
+{"event_id": 1119942, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:20:00", "end_date_time": "2023-07-28 19:30:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Trained spotter reported a 90 mph wind gust.", "ts_dict_index": [11169, 11170, 11171]}
+{"event_id": 1031271, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2022-05-21 20:35:00", "end_date_time": "2022-05-21 20:35:00", "narrative": "Scattered strong to severe storms formed into a line across portions of northwestern and northern Arkansas along and ahead of an advancing cold front. The line made it into central sections of the state by early evening, and into the south during the overnight hours of the 21st.||Dry weather and above normal temperatures returned to the state for a few days before yet another storm system would impact the state on the 21st. Ahead of a strong cold front, there was a risk of severe weather stretching from the Texas/Mexico border northeastward to the Maine/Canada border. Thunderstorms initially developed across north/northwest Arkansas before forming into a line and marching east. While a brief, weak tornado occurred across Newton County, the most widespread damage occurred across portions of north central into northeast Arkansas. Numerous trees were blown down from Sharp County into portions of Lawrence and Randolph Counties. Additional storms developed later during the evening of May 21st across portions of western into central and southern Arkansas. Severe weather reports weren't widespread, but a second brief tornado developed near Royal in Garland County. Pictures were received of large trees that were blown over on Cedar Hill Rd., one of which was fallen on a house. The house did not appear to be significantly damaged. The time is based on radar data.", "ts_dict_index": [11139, 11140, 11141]}
+{"event_id": 948463, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2021-05-09 18:42:00", "end_date_time": "2021-05-09 18:42:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. Trees were downed near the intersection of Highways 117 and 118 in the Kisatchie community.", "ts_dict_index": [11145, 11146, 11147]}
+{"event_id": 911408, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-08-29 20:16:00", "end_date_time": "2020-08-29 20:16:00", "narrative": "Scattered showers and thunderstorms developed during the late afternoon through the evening hours of August 29th across Western Arkansas, near and just south of a weak surface front draped from Northeast Oklahoma into Western and Central Arkansas, and near an upper level disturbance shifting southeast through Arkansas. A very hot and humid air mass in place just ahead of the front fueled high amounts of instability, with these storms merging into a large mesoscale convective system (MCS) as they shifted south into extreme Southeast Oklahoma and much of Southwest Arkansas. Additional scattered strong to severe thunderstorms also developed over portions of Red River County Texas and McCurtain County Oklahoma, eventually merging into the MCS. As a result, much of this thunderstorm complex became severe, producing damaging winds which downed trees and power lines across McCurtain County Oklahoma and much of Southwest Arkansas during the late evening hours on the 29th through a portion of the early morning hours on the 30th. These storms gradually weakened overnight with diminished instability and as the primary upper level disturbance shifted east of the region. Large branches were downed north of Hochatown.", "ts_dict_index": [11133, 11134, 11135]}
+{"event_id": 911407, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-08-29 19:45:00", "end_date_time": "2020-08-29 19:45:00", "narrative": "Scattered showers and thunderstorms developed during the late afternoon through the evening hours of August 29th across Western Arkansas, near and just south of a weak surface front draped from Northeast Oklahoma into Western and Central Arkansas, and near an upper level disturbance shifting southeast through Arkansas. A very hot and humid air mass in place just ahead of the front fueled high amounts of instability, with these storms merging into a large mesoscale convective system (MCS) as they shifted south into extreme Southeast Oklahoma and much of Southwest Arkansas. Additional scattered strong to severe thunderstorms also developed over portions of Red River County Texas and McCurtain County Oklahoma, eventually merging into the MCS. As a result, much of this thunderstorm complex became severe, producing damaging winds which downed trees and power lines across McCurtain County Oklahoma and much of Southwest Arkansas during the late evening hours on the 29th through a portion of the early morning hours on the 30th. These storms gradually weakened overnight with diminished instability and as the primary upper level disturbance shifted east of the region. Large branches were downed in Idabel.", "ts_dict_index": [11136, 11137, 11138]}
+{"event_id": 948464, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2021-05-09 19:06:00", "end_date_time": "2021-05-09 19:06:00", "narrative": "Warm, humid, and unstable conditions were in place across the Four State Region on May 9th, ahead of a cold front and attendant shortwave trough that traversed the Southern Plains during the afternoon. Large scale forcing ahead of the trough increased during the afternoon, with scattered showers and thunderstorms developing near and ahead of the front across Southwest Arkansas, North Louisiana, and East Texas. Moderate instability and adequate wind shear contributed to the development of strong to severe thunderstorms across the region, which produced damaging winds and large hail. One specific cluster of strong to severe thunderstorms affected portions of Deep East Texas and West-central Louisiana, and continued to redevelop over the same areas, producing a wide swath of heavy rainfall with rainfall amounts of three to in excess of seven inches falling over Southern Cherokee, Nacogdoches, Angelina, San Augustine, and Sabine Counties, as well as Central and Southern Sabine Parish. This resulted in widespread flash flooding over these areas, which persisted into the early morning hours of the 10th before the storms shifted south of the area by daybreak. A tree and power line were downed in the Marco community.", "ts_dict_index": [11148, 11149, 11150]}
+{"event_id": 806144, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-03-14 03:00:00", "end_date_time": "2019-03-14 03:00:00", "narrative": "A moist and unstable airmass was present during the afternoon and evening hours of March 13th across portions of Northcentral and Northeast Louisiana. A dryline moved rapidly eastward across Northern Louisiana during the day with showers and thunderstorms erupting along and ahead of this feature. Upper level forcing was present due to a vigorous upper level trough which moved into the Plains earlier in the day. Very strong winds were present in the lower and mid levels of the atmosphere across the Lower Mississippi Valley and a few storms that developed ahead of the dryline across Northeast Louisiana took on supercell characteristics. Damaging wind gusts were reported with one of these storms across Eastern Union Parish Louisiana with a report of trees downed east of Farmerville.||During the early morning hours of March 14th, a line of strong to severe thunderstorms developed along a cold front across Eastcentral Texas along the base of the upper level trough, and marched east into Northwest Louisiana after 330 am. These storms produced damaging winds which downed trees and power lines across portions of Caddo and Claiborne Parishes before weakening prior to daybreak. A large tree was blown down on Old Mooringsport Road near Mooringsport.", "ts_dict_index": [11109, 11110, 11111]}
+{"event_id": 1119928, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:04:00", "end_date_time": "2023-07-28 19:15:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Trained spotter reported a 65 mph wind gust with the thunderstorm.", "ts_dict_index": [11193, 11194, 11195]}
+{"event_id": 1119940, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:10:00", "end_date_time": "2023-07-28 19:20:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. RWIS reported a 58 mph wind gust.", "ts_dict_index": [11187, 11188, 11189]}
+{"event_id": 1119929, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:02:00", "end_date_time": "2023-07-28 19:15:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Trained spotter reported an 82 mph wind gust with the thunderstorm.", "ts_dict_index": [11190, 11191, 11192]}
+{"event_id": 1119930, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:10:00", "end_date_time": "2023-07-28 19:20:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Tree limbs down and power is out, due to 80 mph wind gusts.", "ts_dict_index": [11199, 11200, 11201]}
+{"event_id": 1119953, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:18:00", "end_date_time": "2023-07-28 19:30:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Large tree limb was snapped.", "ts_dict_index": [11181, 11182, 11183]}
+{"event_id": 961953, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-17 19:08:00", "end_date_time": "2021-07-17 19:08:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Several power outages were reported. Large branches were blown down and siding was also blown off a house. The spotter estimated winds above 60 mph. Time estimated from radar.", "ts_dict_index": [11208, 11209, 11210]}
+{"event_id": 1119931, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:11:00", "end_date_time": "2023-07-28 19:20:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Trained spotter reporting 90 mph wind gusts for at least 6 minutes, with zero visibility.", "ts_dict_index": [11202, 11203, 11204]}
+{"event_id": 961952, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-17 19:15:00", "end_date_time": "2021-07-17 19:15:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. A tree was reported down.", "ts_dict_index": [11211, 11212, 11213]}
+{"event_id": 961945, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-17 12:08:00", "end_date_time": "2021-07-17 12:08:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Several large trees and numerous branches were downed with power outages.", "ts_dict_index": [11214, 11215, 11216]}
+{"event_id": 961958, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-17 18:05:00", "end_date_time": "2021-07-17 18:05:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Several trees were blown down near the intersection of Fleecy Dale Rd and River Rd.", "ts_dict_index": [11205, 11206, 11207]}
+{"event_id": 961951, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-17 18:00:00", "end_date_time": "2021-07-17 18:00:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Several reports of downed trees and power outages in the area. Time estimated from radar.", "ts_dict_index": [11226, 11227, 11228]}
+{"event_id": 961955, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-17 20:29:00", "end_date_time": "2021-07-17 20:29:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Downed tree limbs blocked Kaolin Rd at Limestone Rd. Time estimated from radar and dispatch report.", "ts_dict_index": [11223, 11224, 11225]}
+{"event_id": 961954, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-17 20:32:00", "end_date_time": "2021-07-17 20:32:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. A downed tree blocked the road on Round Hill Rd at Kaoli Rd. Time estimated from radar and dispatch report.", "ts_dict_index": [11229, 11230, 11231]}
+{"event_id": 843627, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-08-30 18:05:00", "end_date_time": "2019-08-30 18:05:00", "narrative": "The remnants of a complex of showers and thunderstorms that diminished during the morning hours of August 30th over Southern Oklahoma and Western Arkansas sent a large outflow boundary south into Northern and Eastern Texas during the late morning through the afternoon. Strong heating and instability ahead of this boundary resulted in additional scattered shower and thunderstorm development over much of North Texas and the DFW Metroplex, with another complex of showers and thunderstorms over this area building east into portions of East Texas during the late afternoon and evening hours before gradually weakening. Convective boundaries from this complex of storms, as well as the early morning storms interacted with the strong heating and instability that had developed over East Texas, such that isolated to scattered showers and thunderstorms developed during the mid-afternoon through the evening hours. One thunderstorm became severe over portions of Gregg and Harrison Counties, which downed a couple of trees and snapped large branches near Hallsville and Scottsville. These storms weakened by mid-evening with the loss of heating and instability. A tree was blown down inside the Scottsville city limits.", "ts_dict_index": [11232, 11233, 11234]}
+{"event_id": 843625, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-08-30 17:20:00", "end_date_time": "2019-08-30 17:20:00", "narrative": "The remnants of a complex of showers and thunderstorms that diminished during the morning hours of August 30th over Southern Oklahoma and Western Arkansas sent a large outflow boundary south into Northern and Eastern Texas during the late morning through the afternoon. Strong heating and instability ahead of this boundary resulted in additional scattered shower and thunderstorm development over much of North Texas and the DFW Metroplex, with another complex of showers and thunderstorms over this area building east into portions of East Texas during the late afternoon and evening hours before gradually weakening. Convective boundaries from this complex of storms, as well as the early morning storms interacted with the strong heating and instability that had developed over East Texas, such that isolated to scattered showers and thunderstorms developed during the mid-afternoon through the evening hours. One thunderstorm became severe over portions of Gregg and Harrison Counties, which downed a couple of trees and snapped large branches near Hallsville and Scottsville. These storms weakened by mid-evening with the loss of heating and instability. A tree was blown down on Quail Lane.", "ts_dict_index": [11235, 11236, 11237]}
+{"event_id": 961946, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-07-17 14:10:00", "end_date_time": "2021-07-17 14:10:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. A large tree was snapped. Time estimated from radar.", "ts_dict_index": [11217, 11218, 11219]}
+{"event_id": 961948, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-07-17 14:10:00", "end_date_time": "2021-07-17 14:10:00", "narrative": "A warm and very humid air mass was in place over the mid-Atlantic on July 17. A warm front which had sagged south into the region on the night of the 16th pushed back to the north on the morning of the 17th. Meanwhile, a cold front slowly approached by evening, with a pre-frontal surface trough ahead of it. The presence of multiple synoptic and mesoscale boundaries led to a highly complex convective evolution. Several areas and multiple rounds of convection affected the eastern mid-Atlantic over about a 12 hour period from early afternoon on the 17th to a little after midnight on the 18th. With shear falling in the weak to moderate range, convection mainly took the form of multi-cellular and linear clusters, though some semi-discrete supercellular structures were noted at times. A number of storms became severe with damaging wind. Areas of heavy rain and flash flooding also occurred due to the widespread and at times slow moving nature of the convection. Eventually, by later in the night, the approach of the cold front and significant overturning of the atmosphere from the day's convection caused remaining activity to weaken and shift offshore. Some siding was blown off a home. Time estimated from radar.", "ts_dict_index": [11220, 11221, 11222]}
+{"event_id": 843626, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-08-30 17:30:00", "end_date_time": "2019-08-30 17:30:00", "narrative": "The remnants of a complex of showers and thunderstorms that diminished during the morning hours of August 30th over Southern Oklahoma and Western Arkansas sent a large outflow boundary south into Northern and Eastern Texas during the late morning through the afternoon. Strong heating and instability ahead of this boundary resulted in additional scattered shower and thunderstorm development over much of North Texas and the DFW Metroplex, with another complex of showers and thunderstorms over this area building east into portions of East Texas during the late afternoon and evening hours before gradually weakening. Convective boundaries from this complex of storms, as well as the early morning storms interacted with the strong heating and instability that had developed over East Texas, such that isolated to scattered showers and thunderstorms developed during the mid-afternoon through the evening hours. One thunderstorm became severe over portions of Gregg and Harrison Counties, which downed a couple of trees and snapped large branches near Hallsville and Scottsville. These storms weakened by mid-evening with the loss of heating and instability. A retired NWS employee and current CoCoRaHS observer reported large tree branches that were broken in his yard, with patio furniture blown over.", "ts_dict_index": [11238, 11239, 11240]}
+{"event_id": 1119927, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:05:00", "end_date_time": "2023-07-28 19:15:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Trained spotter reported a 90 mph wind gust along the leading edge of the thunderstorm.", "ts_dict_index": [11196, 11197, 11198]}
+{"event_id": 1027151, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-05-21 21:38:00", "end_date_time": "2022-05-21 21:38:00", "narrative": "A weak upper level trough moved into much of Arkansas, Northeast and Central Texas, and North Louisiana during the afternoon and evening hours of May 21st, which helped to reinforce a weak cold front southeast into the region during the evening and overnight hours. The air mass ahead of the front was very unstable, with steep lapse rates present along the trough once large scale forcing was adequate enough to initiate shower and thunderstorm development. As a result, showers and thunderstorms quickly developed during the early to mid evening hours along and just ahead of the front, with many of these storms becoming severe across East Texas, Southwest Arkansas, and Northwest Louisiana. Damaging winds and isolated instances of large hail accompanied these storms as they moved across East Texas during the mid and late evening.  A second complex of severe thunderstorms developed over Central Texas near Waco, which quickly moved east into East Texas south of I-20. Damaging winds were widespread with the convective complex moving across Central and East Texas, before the winds weakened prior to reaching Western Louisiana by midnight on the 22nd. Trees downed along Broadway Avenue in Tyler and near the UT Tyler campus.", "ts_dict_index": [11244, 11245, 11246]}
+{"event_id": 1027149, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-05-21 21:37:00", "end_date_time": "2022-05-21 21:37:00", "narrative": "A weak upper level trough moved into much of Arkansas, Northeast and Central Texas, and North Louisiana during the afternoon and evening hours of May 21st, which helped to reinforce a weak cold front southeast into the region during the evening and overnight hours. The air mass ahead of the front was very unstable, with steep lapse rates present along the trough once large scale forcing was adequate enough to initiate shower and thunderstorm development. As a result, showers and thunderstorms quickly developed during the early to mid evening hours along and just ahead of the front, with many of these storms becoming severe across East Texas, Southwest Arkansas, and Northwest Louisiana. Damaging winds and isolated instances of large hail accompanied these storms as they moved across East Texas during the mid and late evening.  A second complex of severe thunderstorms developed over Central Texas near Waco, which quickly moved east into East Texas south of I-20. Damaging winds were widespread with the convective complex moving across Central and East Texas, before the winds weakened prior to reaching Western Louisiana by midnight on the 22nd. Trees and power lines reported down.", "ts_dict_index": [11241, 11242, 11243]}
+{"event_id": 820547, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 06:58:00", "end_date_time": "2019-04-19 06:58:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down onto a home near Woodville Highway.  An 8 year old girl was killed and a 12 year old boy was injured.", "ts_dict_index": [11274, 11275, 11276]}
+{"event_id": 820548, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 06:59:00", "end_date_time": "2019-04-19 06:59:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down on Bronough Street north of Tennessee Street.", "ts_dict_index": [11277, 11278, 11279]}
+{"event_id": 820569, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:30:00", "end_date_time": "2019-04-19 08:30:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down at Disston Street.", "ts_dict_index": [11280, 11281, 11282]}
+{"event_id": 1027147, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-05-21 21:14:00", "end_date_time": "2022-05-21 21:14:00", "narrative": "A weak upper level trough moved into much of Arkansas, Northeast and Central Texas, and North Louisiana during the afternoon and evening hours of May 21st, which helped to reinforce a weak cold front southeast into the region during the evening and overnight hours. The air mass ahead of the front was very unstable, with steep lapse rates present along the trough once large scale forcing was adequate enough to initiate shower and thunderstorm development. As a result, showers and thunderstorms quickly developed during the early to mid evening hours along and just ahead of the front, with many of these storms becoming severe across East Texas, Southwest Arkansas, and Northwest Louisiana. Damaging winds and isolated instances of large hail accompanied these storms as they moved across East Texas during the mid and late evening.  A second complex of severe thunderstorms developed over Central Texas near Waco, which quickly moved east into East Texas south of I-20. Damaging winds were widespread with the convective complex moving across Central and East Texas, before the winds weakened prior to reaching Western Louisiana by midnight on the 22nd. Several trees snapped in Bullard.", "ts_dict_index": [11256, 11257, 11258]}
+{"event_id": 1027150, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-05-21 21:37:00", "end_date_time": "2022-05-21 21:37:00", "narrative": "A weak upper level trough moved into much of Arkansas, Northeast and Central Texas, and North Louisiana during the afternoon and evening hours of May 21st, which helped to reinforce a weak cold front southeast into the region during the evening and overnight hours. The air mass ahead of the front was very unstable, with steep lapse rates present along the trough once large scale forcing was adequate enough to initiate shower and thunderstorm development. As a result, showers and thunderstorms quickly developed during the early to mid evening hours along and just ahead of the front, with many of these storms becoming severe across East Texas, Southwest Arkansas, and Northwest Louisiana. Damaging winds and isolated instances of large hail accompanied these storms as they moved across East Texas during the mid and late evening.  A second complex of severe thunderstorms developed over Central Texas near Waco, which quickly moved east into East Texas south of I-20. Damaging winds were widespread with the convective complex moving across Central and East Texas, before the winds weakened prior to reaching Western Louisiana by midnight on the 22nd. Vehicle collided with a downed tree at the intersection of Highway 42 and County Road 468 with one minor injury reported.", "ts_dict_index": [11250, 11251, 11252]}
+{"event_id": 851261, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-10-06 17:09:00", "end_date_time": "2019-10-06 17:09:00", "narrative": "A strong upper level trough of low pressure over the Central Plains shifted east into the Mississippi Valley during the afternoon and evening hours on October 6th, which reinforced a strong cold front southeast across Oklahoma and Western Arkansas. This resulted in upper level ridging to gradually begin to retreat east and weaken over the Southeastern U.S., but not until afternoon temperatures again climbed back well above normal into the lower 90s across Southeast Oklahoma and Southwest Arkansas. Increasing gulf moisture was ushered north ahead of the front with the southerly winds, which allowed for a moderately unstable air mass to develop ahead of the approaching front. Large scale forcing along the front and ahead of the approaching upper trough resulted in scattered to numerous showers and thunderstorms developing over Southeast Oklahoma and Western Arkansas, some of which became severe over McCurtain County Oklahoma. These storms produced large hail and damaging winds during the late afternoon and early evening hours before weakening during the mid and late evening with the loss of heating and reduced instability. Three large trees were blown down in the Mount Herman community. Large branches were snapped in the area as well.", "ts_dict_index": [11271, 11272, 11273]}
+{"event_id": 823538, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2019-05-19 01:15:00", "end_date_time": "2019-05-19 01:15:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas, and spread across much of North Louisiana during the evening and overnight hours on the 18th-19th. An isolated tornado also touched down in extreme Southern Natchitoches Parish during the early morning hours of May 19th. These storms began to move repeatedly over the same areas during the early morning hours of the 19th, with instances of flash flooding reported as well. These storms eventually diminished just prior to daybreak on the 19th. Numerous trees were downed along Highway 1 south of Cloutierville. Widespread power outages were reported.", "ts_dict_index": [11262, 11263, 11264]}
+{"event_id": 1027153, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2022-05-21 22:40:00", "end_date_time": "2022-05-21 22:40:00", "narrative": "A weak upper level trough moved into much of Arkansas, Northeast and Central Texas, and North Louisiana during the afternoon and evening hours of May 21st, which helped to reinforce a weak cold front southeast into the region during the evening and overnight hours. The air mass ahead of the front was very unstable, with steep lapse rates present along the trough once large scale forcing was adequate enough to initiate shower and thunderstorm development. As a result, showers and thunderstorms quickly developed during the early to mid evening hours along and just ahead of the front, with many of these storms becoming severe across East Texas, Southwest Arkansas, and Northwest Louisiana. Damaging winds and isolated instances of large hail accompanied these storms as they moved across East Texas during the mid and late evening.  A second complex of severe thunderstorms developed over Central Texas near Waco, which quickly moved east into East Texas south of I-20. Damaging winds were widespread with the convective complex moving across Central and East Texas, before the winds weakened prior to reaching Western Louisiana by midnight on the 22nd. Trees reported down in the Shadowood Estates.", "ts_dict_index": [11253, 11254, 11255]}
+{"event_id": 851262, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-10-06 18:16:00", "end_date_time": "2019-10-06 18:16:00", "narrative": "A strong upper level trough of low pressure over the Central Plains shifted east into the Mississippi Valley during the afternoon and evening hours on October 6th, which reinforced a strong cold front southeast across Oklahoma and Western Arkansas. This resulted in upper level ridging to gradually begin to retreat east and weaken over the Southeastern U.S., but not until afternoon temperatures again climbed back well above normal into the lower 90s across Southeast Oklahoma and Southwest Arkansas. Increasing gulf moisture was ushered north ahead of the front with the southerly winds, which allowed for a moderately unstable air mass to develop ahead of the approaching front. Large scale forcing along the front and ahead of the approaching upper trough resulted in scattered to numerous showers and thunderstorms developing over Southeast Oklahoma and Western Arkansas, some of which became severe over McCurtain County Oklahoma. These storms produced large hail and damaging winds during the late afternoon and early evening hours before weakening during the mid and late evening with the loss of heating and reduced instability. A tree was blown down on Red Arrow Road just east of Broken Bow.", "ts_dict_index": [11268, 11269, 11270]}
+{"event_id": 820570, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:30:00", "end_date_time": "2019-04-19 08:30:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down onto Brewer Street.", "ts_dict_index": [11283, 11284, 11285]}
+{"event_id": 1120947, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-07-28 19:07:00", "end_date_time": "2023-07-28 19:20:00", "narrative": "Very hot and humid air in place across eastern Iowa, northwest Illinois, and far northeast Missouri interacted with a southward moving frontal boundary and disturbance aloft, setting the stage for development and organization of severe thunderstorms across the region. Storms initially formed from north central Iowa and southern Wisconsin along the frontal boundary, which slowly worked south into the hot, humid air in place across the region. As storms arrived across east central Iowa, they began producing winds around 70 MPH across the Hwy 20 corridor. Another storm to the south further intensified, and began producing winds of 80+ MPH as it tracked along the Hwy 30 corridor. This impacted the northern suburbs of Cedar Rapids into Clinton. These storms continued to produce wind gusts around 60-70 MPH as they progressed into northwest Illinois. One brief EF-0 tornado began in Clinton, Iowa, then moved across the Mississippi River before dissipating near Fulton, Illinois. Damage near Andrew, Iowa in Jackson County was determined to be straight-line winds. Storms additionally produced large hail around the Dubuque metro, with quarter size hail reported. Report from mping regarding tree limbs down, power poles damaged, and shingles blown off of a roof.", "ts_dict_index": [11184, 11185, 11186]}
+{"event_id": 820566, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:16:00", "end_date_time": "2019-04-19 08:16:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down at Oaks Edge Road.", "ts_dict_index": [11286, 11287, 11288]}
+{"event_id": 820554, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 07:15:00", "end_date_time": "2019-04-19 07:15:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down on Capitola Road at Benjamin Chaires Road.", "ts_dict_index": [11301, 11302, 11303]}
+{"event_id": 820546, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 06:55:00", "end_date_time": "2019-04-19 06:55:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down on Tram Road near St Joe Road.", "ts_dict_index": [11298, 11299, 11300]}
+{"event_id": 820559, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:00:00", "end_date_time": "2019-04-19 08:00:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. The public reported trees uprooted or snapped via mping.", "ts_dict_index": [11319, 11320, 11321]}
+{"event_id": 820552, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 07:14:00", "end_date_time": "2019-04-19 07:14:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down onto a home near Woodville Highway.", "ts_dict_index": [11292, 11293, 11294]}
+{"event_id": 820565, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:14:00", "end_date_time": "2019-04-19 08:14:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down on Ox Bow Road near Ox Bottom Road.", "ts_dict_index": [11316, 11317, 11318]}
+{"event_id": 820557, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 07:54:00", "end_date_time": "2019-04-19 07:54:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down onto power lines near Roberts Ave and Paul Dirac Dr.", "ts_dict_index": [11310, 11311, 11312]}
+{"event_id": 820571, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:30:00", "end_date_time": "2019-04-19 08:30:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down at Shamrock East at Ardara Dr.", "ts_dict_index": [11304, 11305, 11306]}
+{"event_id": 820564, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:10:00", "end_date_time": "2019-04-19 08:10:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. Several trees were blown down in the Golden Eagle area.", "ts_dict_index": [11295, 11296, 11297]}
+{"event_id": 820573, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:35:00", "end_date_time": "2019-04-19 08:35:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down on Walden Road at Atascadera Lane.", "ts_dict_index": [11325, 11326, 11327]}
+{"event_id": 820563, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:10:00", "end_date_time": "2019-04-19 08:10:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down at the intersection of Bannerman Road and Bull Headley Road.", "ts_dict_index": [11313, 11314, 11315]}
+{"event_id": 820567, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:20:00", "end_date_time": "2019-04-19 08:20:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down at I-10 at Mile Marker 201 eastbound.", "ts_dict_index": [11289, 11290, 11291]}
+{"event_id": 820560, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:00:00", "end_date_time": "2019-04-19 08:00:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down on Stone Road near Lakeshore Drive.", "ts_dict_index": [11322, 11323, 11324]}
+{"event_id": 823524, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-05-18 19:10:00", "end_date_time": "2019-05-18 19:10:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas, and spread across much of North Louisiana during the evening and overnight hours on the 18th-19th. An isolated tornado also touched down in extreme Southern Natchitoches Parish during the early morning hours of May 19th. These storms began to move repeatedly over the same areas during the early morning hours of the 19th, with instances of flash flooding reported as well. These storms eventually diminished just prior to daybreak on the 19th. A large oak tree was blown down across Highway 71 in Belcher.", "ts_dict_index": [11259, 11260, 11261]}
+{"event_id": 1010146, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-05 01:48:00", "end_date_time": "2022-04-05 01:48:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. Shingles were blown off of multiple homes on Hoyte Drive.", "ts_dict_index": [11334, 11335, 11336]}
+{"event_id": 820562, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:02:00", "end_date_time": "2019-04-19 08:02:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. A tree was blown down on the side of an apartment building near Gadsden and Carolina Street.", "ts_dict_index": [11328, 11329, 11330]}
+{"event_id": 1010201, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-05 03:02:00", "end_date_time": "2022-04-05 03:02:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. Damaging straight line winds affected much of the Rocky Branch community, with a swath of 80-85 mph winds sweeping across this area from a line of severe thunderstorms. Multiple trees were snapped or uprooted in an easterly direction, especially along Acree Road, east to Highway 143, along Wendy Lane, and Charles Dean Road. The most significant structural damage occurred when two large line trees were uprooted onto a home on Acree Road, another tree was uprooted onto a truck and mobile home also on Acree Road, and a large hardwood tree crushed a wooden barn along Wendy Lane.", "ts_dict_index": [11343, 11344, 11345]}
+{"event_id": 982054, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:55:00", "end_date_time": "2021-08-13 22:55:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. A 40 foot tree fell through a 5 foot cinderblock wall and onto a chicken coop at a home near University Drive and 96th Street. There were no chickens in the coop at the time and no injuries were reported. Winds were estimated around 55 to 65 mph. Timing estimated from radar.", "ts_dict_index": [11346, 11347, 11348]}
+{"event_id": 862172, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2019-12-16 12:57:00", "end_date_time": "2019-12-16 12:57:00", "narrative": "From the mid-morning through the mid-afternoon hours on December 16th, 2019, a strong cold front progressed from west to east across the Four State region, ahead of a strong upper level trough which progressed east across the Southern Plains. Just ahead of the front, several severe thunderstorms formed in the unstable and highly-sheared air mass in place over Deep East Texas, Central Louisiana, and the Ark-La-Miss. The most potent storm produced a long-track EF-1 tornado that initially touched down in central Bossier Parish and tracked over 26 miles, before lifting in far west-central Claiborne Parish. Along most of its track, the tornado passed over rural areas and most of the damage was limited to trees. However, in east-central Webster Parish, the tornado either severely damaged or destroyed several residences, but fortunately, there were no reported casualties. A few other storms produced relatively minor wind damage in Northern Louisiana, limited to downed trees and power lines. This local event was on the northwestern edge of a large regional tornado outbreak affecting Louisiana, Mississippi, and Alabama. A power pole and power lines were downed in Robeline.", "ts_dict_index": [11331, 11332, 11333]}
+{"event_id": 981719, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 21:43:00", "end_date_time": "2021-08-13 21:43:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Numerous tree branches of varying sizes blown down. Wind gusts estimated 50 to 60 mph. No injuries reported.", "ts_dict_index": [11337, 11338, 11339]}
+{"event_id": 982020, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:52:00", "end_date_time": "2021-08-13 22:52:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Public report, confirmed by police, that a road was blocked by downed power lines at 83rd Avenue and Broadway Road. Winds estimated around 55-65 mph and timing estimated from radar. No injuries reported.", "ts_dict_index": [11340, 11341, 11342]}
+{"event_id": 1010153, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-05 01:50:00", "end_date_time": "2022-04-05 01:50:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. A tree was blown down near Dixie Meadow and Dixie Garden Road.", "ts_dict_index": [11352, 11353, 11354]}
+{"event_id": 1010144, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-05 01:37:00", "end_date_time": "2022-04-05 01:37:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. A tree was blown down at Greenwood Baptist Church Road and Greenwood Springridge Road.", "ts_dict_index": [11349, 11350, 11351]}
+{"event_id": 820561, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2019-04-19 08:00:00", "end_date_time": "2019-04-19 08:00:00", "narrative": "This event was characterized by a mid-level shortwave becoming negatively tilted in the Tennessee Valley and attendant surface low pressure. The strong wind field associated with this system included another anomalously strong low-level jet, with 925 hPa winds sampled on the 12Z/19 TAE Sounding around 40 knots! This advected warm, moist, and unstable air northward, ahead of a pre-frontal trough which served as a focusing mechanism for convection. Instability was initially lacking Thursday Night, but increased on Friday, with Mixed Layer CAPE ranging from 1-1.5k J/kg. Furthermore, the 12Z/19 TAE Sounding revealed Surface Based CAPE of nearly 2.4k J/kg, which is a record for the date per SPC Sounding Climatology! The instability and Bulk Shear (0-6 km) over 50 knots overcame the poorer mid-level lapse rates, and the QLCS intensified as it moved east of the Flint and Apalachicola Rivers on Friday. Despite Shear (0-1 km) around 35 knots on the 12Z/19 TAE Sounding, the hodograph revealed a more unidirectional wind within this layer, however there may have been slightly more veering based on the nearby observations from TLH. ", "ts_dict_index": [11307, 11308, 11309]}
+{"event_id": 1010148, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-05 01:48:00", "end_date_time": "2022-04-05 01:48:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. Shingles were blown off of multiple homes on Mackey Lane.", "ts_dict_index": [11358, 11359, 11360]}
+{"event_id": 1010150, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-05 01:48:00", "end_date_time": "2022-04-05 01:48:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. Power lines were downed near East Stoner and Viking Drive and near River Parkway Drive in East Shreveport.", "ts_dict_index": [11355, 11356, 11357]}
+{"event_id": 1010155, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-05 01:47:00", "end_date_time": "2022-04-05 01:47:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. A large tree was blown down on Robinson Place.", "ts_dict_index": [11382, 11383, 11384]}
+{"event_id": 1010186, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-05 03:08:00", "end_date_time": "2022-04-05 03:08:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. About 75-100 trees, mostly tall/skinny pines, were uprooted (with some snaps) in the D'Arbonne National Wildlife Refuge. All of these trees were lying in an east-northeasterly direction, indicative of straight line winds. Pictures were submitted by a forest ranger from the refuge.", "ts_dict_index": [11373, 11374, 11375]}
+{"event_id": 1010182, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-05 02:38:00", "end_date_time": "2022-04-05 02:38:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. Trees down on Highway 550 and Village Creek Road east of Bernice. Numerous trees were downed elsewhere across Union Parish including Highway 33 north at the Union Parish Elementary School, Highway 33 south at Hicks Frazier Road, Highway 15 south at Holmesville Road, Highway 15 south at Bobbie Cox Road, Highway 3121 in the Lockhart community, and Highway 143 at Albert Smith Road.", "ts_dict_index": [11379, 11380, 11381]}
+{"event_id": 1010183, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-05 02:54:00", "end_date_time": "2022-04-05 02:54:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. Damaging straight line winds affected areas along and just south of Ruggs Bluff Road just southeast of Lake D'Arbonne, where a large portion of a metal roof was blown off of a metal barn and thrown across the roadway. Numerous trees were snapped and uprooted farther east along Ruggs Bluff Road, with the greatest concentration of damage occurring where three pine trees were uprooted and fell onto a home. Numerous other hardwood and softwood trees were snapped and uprooted in an easterly direction nearby, with the winds rated here estimated near 95 mph. The wind damage became more sporadic farther east-southeast along Ruggs Bluff Road, especially as it crossed Francis Creek.", "ts_dict_index": [11376, 11377, 11378]}
+{"event_id": 982143, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 20:44:00", "end_date_time": "2021-08-13 20:44:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Mesonet station MAHL at Horseshoe Lake measured a 63 mph wind gust.", "ts_dict_index": [11388, 11389, 11390]}
+{"event_id": 982112, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:20:00", "end_date_time": "2021-08-13 22:20:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. A photo on social media shows a metal patio awning blew down in strong winds near 19th Avenue and Bell Road. Winds estimated around 50 to 55 mph and timing based on radar. No injuries were reported.", "ts_dict_index": [11391, 11392, 11393]}
+{"event_id": 1010161, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-04-05 02:05:00", "end_date_time": "2022-04-05 02:05:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. A tree was blown down across Highway 79 just north of Grider Road northeast of Minden. A motorist was killed when the vehicle he was driving struck this fallen tree.", "ts_dict_index": [11367, 11368, 11369]}
+{"event_id": 982024, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:55:00", "end_date_time": "2021-08-13 22:55:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. The SRP32 mesonet station near 43rd Avenue and Lower Buckeye Road measured a 61 mph wind gust. A microburst signature was observed on radar in this area. The Phoenix terminal doppler weather radar TPHX, near 51st Avenue and Lower Buckeye Road, took a direct hit and stopped transmitting after its 1039MST scan. There were no damages to TPHX reported and it was restored by 1000MST  on the 14th.", "ts_dict_index": [11370, 11371, 11372]}
+{"event_id": 982119, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:50:00", "end_date_time": "2021-08-13 22:50:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Large shallow-rooted tree uprooted and fell into the street near Miller Road and Southern Avenue. Wind speeds estimated between 45 to 55 mph. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [11385, 11386, 11387]}
+{"event_id": 981720, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 21:55:00", "end_date_time": "2021-08-13 21:55:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. A home weather station measured a 60 mph wind gust.", "ts_dict_index": [11361, 11362, 11363]}
+{"event_id": 1027152, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-05-21 22:04:00", "end_date_time": "2022-05-21 22:04:00", "narrative": "A weak upper level trough moved into much of Arkansas, Northeast and Central Texas, and North Louisiana during the afternoon and evening hours of May 21st, which helped to reinforce a weak cold front southeast into the region during the evening and overnight hours. The air mass ahead of the front was very unstable, with steep lapse rates present along the trough once large scale forcing was adequate enough to initiate shower and thunderstorm development. As a result, showers and thunderstorms quickly developed during the early to mid evening hours along and just ahead of the front, with many of these storms becoming severe across East Texas, Southwest Arkansas, and Northwest Louisiana. Damaging winds and isolated instances of large hail accompanied these storms as they moved across East Texas during the mid and late evening.  A second complex of severe thunderstorms developed over Central Texas near Waco, which quickly moved east into East Texas south of I-20. Damaging winds were widespread with the convective complex moving across Central and East Texas, before the winds weakened prior to reaching Western Louisiana by midnight on the 22nd. Tree downed and blocking FM Road 2011 near County Road 2124D near Lake Cherokee.", "ts_dict_index": [11247, 11248, 11249]}
+{"event_id": 1010156, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2022-04-05 01:56:00", "end_date_time": "2022-04-05 01:56:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited the region to the east prior to sunrise on the 5th. A 59 mph wind gust was measured at Barksdale Air Force Base (KBAD).", "ts_dict_index": [11406, 11407, 11408]}
+{"event_id": 849574, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-08-08 16:37:00", "end_date_time": "2019-08-08 16:37:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. The county emergency manager reported that trees were blown down on Brokers Lane.", "ts_dict_index": [11415, 11416, 11417]}
+{"event_id": 849575, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-08-08 16:37:00", "end_date_time": "2019-08-08 16:37:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. County 911 officials reported that trees were blown down on Mickanin Road.", "ts_dict_index": [11424, 11425, 11426]}
+{"event_id": 849570, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-08-08 16:26:00", "end_date_time": "2019-08-08 16:26:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. A social media user reported that a tree and power lines were down at the intersection of Oliver Way and Lincoln Way.", "ts_dict_index": [11430, 11431, 11432]}
+{"event_id": 849576, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-08-08 16:40:00", "end_date_time": "2019-08-08 16:40:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. A tree was blown down on Brownstown Road, according to the county emergency manager.", "ts_dict_index": [11412, 11413, 11414]}
+{"event_id": 849572, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-08-08 16:30:00", "end_date_time": "2019-08-08 16:30:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. The county emergency manager reported that poles and wires were blown down on Ridge Road.", "ts_dict_index": [11433, 11434, 11435]}
+{"event_id": 853681, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-08-08 16:37:00", "end_date_time": "2019-08-08 16:37:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. The county emergency manager reported that trees were blown down on Mickanin Road.", "ts_dict_index": [11418, 11419, 11420]}
+{"event_id": 849577, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-08-08 16:41:00", "end_date_time": "2019-08-08 16:41:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. A member of the public reported that trees and limbs were blown down to the south and southeast of town.", "ts_dict_index": [11427, 11428, 11429]}
+{"event_id": 982097, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 23:01:00", "end_date_time": "2021-08-13 23:01:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Video shows a large tree snapped near the base and fell on a home near University Drive and Lindsey Road causing damage. The extent of the damage was not reported. Winds were estimated around 50 to 60 mph based on radar. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [11394, 11395, 11396]}
+{"event_id": 1010206, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-04-04 22:19:00", "end_date_time": "2022-04-04 22:19:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas and Southeast Oklahoma during the late evening hours of the 4th. Given the extent of elevated instability and the strong southerly low level jet in place across Southeast Oklahoma, these storms became severe as they spread east across McCurtain County, resulting in multiple reports of hail as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited Southeast Oklahoma by midnight that night. Large limbs were downed just north of the Tom community.", "ts_dict_index": [11409, 11410, 11411]}
+{"event_id": 982091, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:55:00", "end_date_time": "2021-08-13 22:55:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Photos from APS utility company on social media show several downed or snapped wooden and metal power poles along 27th Avenue just north of Durango Street. A microburst signature was evident on radar in this area. Winds were estimated around 60-65 mph based on a 61 mph measured gust a few blocks away. No injuries were reported.", "ts_dict_index": [11400, 11401, 11402]}
+{"event_id": 982067, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:57:00", "end_date_time": "2021-08-13 22:57:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. A strong downburst knocked over or broke 20 to 30 trees and a few saguaro cacti along Brown Road and Ellsworth Road. Winds estimated around 55-65 mph and timing based on radar. No injuries reported.", "ts_dict_index": [11403, 11404, 11405]}
+{"event_id": 981721, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:23:00", "end_date_time": "2021-08-13 22:23:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Multiple large trees were blown over due to strong winds at Latitude Apartment Complex near 19th Avenue and Thunderbird Road. One tree fell on a second story unit, causing unknown damage. Another couple fell on portions of carports that caused the carports to collapse and damage an unknown number of cars that were parked underneath. A separate carport also experienced damage. Winds were estimated up to 55 to 65 mph based on radar and timing was based on radar as well. No injuries were reported.", "ts_dict_index": [11364, 11365, 11366]}
+{"event_id": 1087927, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 22:01:00", "end_date_time": "2023-03-24 22:01:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A 66 mph wind gust was recorded at the Northwest Alabama Regional Airport (KMSL).", "ts_dict_index": [11454, 11455, 11456]}
+{"event_id": 849489, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-08-08 16:20:00", "end_date_time": "2019-08-08 16:20:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. A trained spotter reported that a tree was downed on Main Street.", "ts_dict_index": [11442, 11443, 11444]}
+{"event_id": 849488, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-08-08 16:10:00", "end_date_time": "2019-08-08 16:10:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. A trained spotter reported that trees were blown down on Baldwin and McMichael Roads.", "ts_dict_index": [11439, 11440, 11441]}
+{"event_id": 1090819, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 22:07:00", "end_date_time": "2023-03-24 22:07:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. Fence and siding damage of a gymnasium was reported at Rogers High School.", "ts_dict_index": [11472, 11473, 11474]}
+{"event_id": 1088499, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 21:52:00", "end_date_time": "2023-03-24 22:12:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A bow echo from an embedded supercell within a line of thunderstorms intensified and produced a long-lived and at times wide swath of wind damage as it entered the Shoals, including Florence and Killen, to the east central part of Lauderdale County north of Elgin. Widespread wind damage occurred in south, southeast and eastern Florence to Killen, becoming more sporadic further east. Wind speeds of 60-65 mph occurred in much of this area, with a few gusts of 80-90 mph in a few locations. One of the hardest hit locations was between Killen and Florence where the entire roof was taken off of antique mall, a sign was blown out at a church, and roofing was taken off of a fire station. Trees, power poles and power lines were taken down in numerous locations, stormwater and gas lines were damaged, and debris and utility restoration costs were extensive. Schools buses were damaged, parks were damaged with extensive cleanup.  A significant number of residences experienced damage due to falling trees. Damage, cleanup and repair costs are in the millions of dollars.", "ts_dict_index": [11463, 11464, 11465]}
+{"event_id": 1087910, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 22:06:00", "end_date_time": "2023-03-24 22:06:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. Several trees were knocked down across roads in the Aqua Vista neighborhood.", "ts_dict_index": [11460, 11461, 11462]}
+{"event_id": 1088490, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 21:57:00", "end_date_time": "2023-03-24 21:57:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. Trees were knocked down onto Kendall Drive.", "ts_dict_index": [11466, 11467, 11468]}
+{"event_id": 1090818, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 21:57:00", "end_date_time": "2023-03-24 21:57:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. Roof damage was reported at Wilson High School.", "ts_dict_index": [11469, 11470, 11471]}
+{"event_id": 849484, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-08-08 04:03:00", "end_date_time": "2019-08-08 04:03:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. Large branches were blown down according to a National Weather Service employee.", "ts_dict_index": [11436, 11437, 11438]}
+{"event_id": 956314, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-06-21 15:27:00", "end_date_time": "2021-06-21 15:27:00", "narrative": "A very warm air mass with rich low-level moisture and fairly dry mid-levels was in place over eastern Kentucky. With little in the way of capping, showers and storms quickly blossomed toward midday, especially near the I-64 corridor where an outflow, the lone remnants of an upstream storm cluster, likely provided the trigger. While the initial cells were rather disorganized, slowly increasing westerly winds in the mid-levels, ahead of a strong cold front, provided sufficient shear for the storms to loosely organize into lines, some of which took on a bowing structure. The bowing segments which produced the strongest gusts were oriented more north-to-south, perpendicular to the strengthening mid-level winds. The focus for the storms gradually shifted southeast through the afternoon, ahead of conglomerating thunderstorm outflows. Numerous reports of downed trees and branches were received, along with isolated instances of damage to homes and other structures. Wind gusts between 40 and 57 mph were recorded by several local weather stations, but the strongest winds appear to have missed those locations. The Pulaski County dispatch reported that multiple trees had fallen along Ohio Street due to strong thunderstorm wind gusts.", "ts_dict_index": [11448, 11449, 11450]}
+{"event_id": 956301, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-06-21 15:27:00", "end_date_time": "2021-06-21 15:27:00", "narrative": "A very warm air mass with rich low-level moisture and fairly dry mid-levels was in place over eastern Kentucky. With little in the way of capping, showers and storms quickly blossomed toward midday, especially near the I-64 corridor where an outflow, the lone remnants of an upstream storm cluster, likely provided the trigger. While the initial cells were rather disorganized, slowly increasing westerly winds in the mid-levels, ahead of a strong cold front, provided sufficient shear for the storms to loosely organize into lines, some of which took on a bowing structure. The bowing segments which produced the strongest gusts were oriented more north-to-south, perpendicular to the strengthening mid-level winds. The focus for the storms gradually shifted southeast through the afternoon, ahead of conglomerating thunderstorm outflows. Numerous reports of downed trees and branches were received, along with isolated instances of damage to homes and other structures. Wind gusts between 40 and 57 mph were recorded by several local weather stations, but the strongest winds appear to have missed those locations. The Pulaski County dispatch reported that strong thunderstorm wind gusts had knocked down multiple trees along Jasper Street, with one tree falling onto powerlines near the intersection with Mount Vernon Street.", "ts_dict_index": [11451, 11452, 11453]}
+{"event_id": 956311, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2021-06-21 15:27:00", "end_date_time": "2021-06-21 15:27:00", "narrative": "A very warm air mass with rich low-level moisture and fairly dry mid-levels was in place over eastern Kentucky. With little in the way of capping, showers and storms quickly blossomed toward midday, especially near the I-64 corridor where an outflow, the lone remnants of an upstream storm cluster, likely provided the trigger. While the initial cells were rather disorganized, slowly increasing westerly winds in the mid-levels, ahead of a strong cold front, provided sufficient shear for the storms to loosely organize into lines, some of which took on a bowing structure. The bowing segments which produced the strongest gusts were oriented more north-to-south, perpendicular to the strengthening mid-level winds. The focus for the storms gradually shifted southeast through the afternoon, ahead of conglomerating thunderstorm outflows. Numerous reports of downed trees and branches were received, along with isolated instances of damage to homes and other structures. Wind gusts between 40 and 57 mph were recorded by several local weather stations, but the strongest winds appear to have missed those locations. The Pulaski County dispatch reported multiple trees knocked down by strong thunderstorm wind gusts at the intersection of Hope Way and Railroad Street.", "ts_dict_index": [11445, 11446, 11447]}
+{"event_id": 849571, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-08-08 16:30:00", "end_date_time": "2019-08-08 16:30:00", "narrative": "Several ingredients were in place for scattered severe thunderstorms on August 8th.  An upper shortwave trough embedded in northwest flow crossed the Great Lakes during the day.  Moist west-southwest flow maintained dewpoints in the mid 60s, which in concert with daytime heating, fueled instability.  Strengthening mid-level wind contributed to sufficient levels of shear, allowing an organized line of thunderstorms to cross the region in advance of a cold front.  Steep low-level lapse rates promoted a damaging wind threat, but low-level shear was insufficient for a tornado threat.  The Storm Prediction Center place the region under a slight risk of severe weather for the day.||Thunderstorms began to form in earnest in southeast Ohio around 4 PM, creating wind damage in Columbiana and Noble Counties, along with a large hail report.  The storms formed an organized line and swept across southwest Pennsylvania and northern West Virginia through the late afternoon and early evening.  Wind damage was mainly confined to Allegheny and Westmoreland Counties, with numerous reports of tree and power line damage. The county emergency manager reported trees down on Kalamazoo Road and Highberger Road.", "ts_dict_index": [11421, 11422, 11423]}
+{"event_id": 1087867, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:45:00", "end_date_time": "2023-03-24 21:45:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at 310 South Blackwell Road. Time estimated by radar.", "ts_dict_index": [11475, 11476, 11477]}
+{"event_id": 1087872, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:47:00", "end_date_time": "2023-03-24 21:47:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at 2206 Ashe Blvd. Time estimated by radar.", "ts_dict_index": [11487, 11488, 11489]}
+{"event_id": 1088280, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:38:00", "end_date_time": "2023-03-24 22:05:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A bow echo from an embedded supercell within a line of thunderstorms intensified and produced a long-lived and at times wide swath of wind damage as it entered the Shoals, including Tuscumbia, Sheffield and Muscle Shoals, to the northeast part of the county before crossing the Tennessee River.  Wind speeds were measured over 60 mph at multiple locations, and gusts may have reached up to 80-90 mph when a brick wall of a two story building collapsed and a large part of roofing was taken off another portion of the building. Trees, power poles and power lines were taken down in numerous locations. According to utilities in Sheffield, Tuscumbia and Muscle Shoals, over 60 power poles were knocked down or snapped and over 25 transformers were knocked out resulting in widespread power outages. Numerous trees were knocked down. Extensive debris had to be cleaned up off area roads and streets. At least two vehicles were damaged or destroyed by falling trees or other debris.  Numerous residences experienced minor to significant damage due to falling trees, or roof damage due to the high winds, and resultant flooding inside homes.  At least one home was struct by lightning sparking a damaging fire. Damage and repair costs for public, business and residential exceeded $10 Million.", "ts_dict_index": [11484, 11485, 11486]}
+{"event_id": 1087875, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 21:52:00", "end_date_time": "2023-03-24 21:52:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. The roof was torn off of the El Politos restaurant. Multiple trees and power lines were also knocked down along Chisholm Road.", "ts_dict_index": [11493, 11494, 11495]}
+{"event_id": 1087880, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 22:45:00", "end_date_time": "2023-03-24 22:45:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A 67 mph wind gust was measured northwest of Rogersville.", "ts_dict_index": [11490, 11491, 11492]}
+{"event_id": 1088423, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:44:00", "end_date_time": "2023-03-24 21:44:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down onto a concrete railing at the Henson Creek bridge on Wagon Mountain Road.", "ts_dict_index": [11478, 11479, 11480]}
+{"event_id": 982489, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-13 22:23:00", "end_date_time": "2021-08-13 22:23:00", "narrative": "A classic bow echo developed along the Mogollon Rim in central Arizona around 1900MST on the 13th and merged with thunderstorm clusters that developed in south-central Arizona around 2030MST to form one southwestward-moving MCS that progressed all the way to the town of Yuma in far southwest Arizona by 0230MST on the 14th. The MCS produced widespread strong winds with localized damaging winds from individual microbursts across the region. The strong winds also generated dense blowing dust in southwest Arizona. In addition to the wind, storms were producing average rain rates of 1 to 2 inches per hour with briefly higher rates in the strongest cells. This led to flash flooding in multiple areas. The town of Gila Bend suffered catastrophic flash flooding after 2 to 4 inches of rain fell over a large portion of the basin containing Sand Tank and Bender Washes, which flow into Gila Bend. A breach of the canal in town due to erosion added to the flash flooding. Significant flow through the washes impacted numerous homes and businesses and there were 2 fatalities. A state of emergency was declared for this event. Roof partially torn off in strong winds near Interstate-17 and Thunderbird Road. Winds estimated around 55 to 65 mph. Timing based on radar. No injuries reported.", "ts_dict_index": [11397, 11398, 11399]}
+{"event_id": 1087876, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 21:54:00", "end_date_time": "2023-03-24 21:54:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down onto an automobile in the Seven Points area. Person inside vehicle.", "ts_dict_index": [11502, 11503, 11504]}
+{"event_id": 1088486, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 22:00:00", "end_date_time": "2023-03-24 22:00:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A power line was knocked down.", "ts_dict_index": [11505, 11506, 11507]}
+{"event_id": 1087877, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:55:00", "end_date_time": "2023-03-24 21:55:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A 63 mph wind gust was measured at the HCN/CRN station MSXA1 on the TVA reservation.", "ts_dict_index": [11499, 11500, 11501]}
+{"event_id": 1087859, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:18:00", "end_date_time": "2023-03-24 21:18:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at 1465 Maud Road. Time estimated by radar.", "ts_dict_index": [11514, 11515, 11516]}
+{"event_id": 1087878, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:59:00", "end_date_time": "2023-03-24 21:59:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at the intersection of River Road and County Line Road.", "ts_dict_index": [11496, 11497, 11498]}
+{"event_id": 1087866, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:45:00", "end_date_time": "2023-03-24 21:45:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at 1085 Tennessee Avenue. Time estimated by radar.", "ts_dict_index": [11508, 11509, 11510]}
+{"event_id": 1087862, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:40:00", "end_date_time": "2023-03-24 21:40:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at the intersection of Willingham Loop and Sweetgum Lane. Time estimated by radar.", "ts_dict_index": [11511, 11512, 11513]}
+{"event_id": 1088488, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 22:03:00", "end_date_time": "2023-03-24 22:06:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A narrow swath of very high winds knocked down trees, power lines, uplifted roofing at multiple residences, and destroyed a well constructed outbuilding/detached garage.", "ts_dict_index": [11457, 11458, 11459]}
+{"event_id": 1087865, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:45:00", "end_date_time": "2023-03-24 21:45:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down on Spring Court. Time estimated by radar.", "ts_dict_index": [11517, 11518, 11519]}
+{"event_id": 1088420, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 22:02:00", "end_date_time": "2023-03-24 22:02:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. Shingles were blown off of a house which caused some water to enter the residence.", "ts_dict_index": [11526, 11527, 11528]}
+{"event_id": 1088519, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 22:06:00", "end_date_time": "2023-03-24 22:06:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. Trees were knocked down onto the eastbound lanes of Highway 72 in front of Brooks High School.", "ts_dict_index": [11535, 11536, 11537]}
+{"event_id": 1087869, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:45:00", "end_date_time": "2023-03-24 21:45:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at 1309 Annapolis Avenue. Time estimated by radar.", "ts_dict_index": [11538, 11539, 11540]}
+{"event_id": 1088518, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 22:07:00", "end_date_time": "2023-03-24 22:07:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at 1000 Fawn Lane. Time estimated by radar.", "ts_dict_index": [11532, 11533, 11534]}
+{"event_id": 1088496, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 21:38:00", "end_date_time": "2023-03-24 21:38:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down onto a house at 1225 CR 139. Time estimated by radar.", "ts_dict_index": [11520, 11521, 11522]}
+{"event_id": 1088497, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 21:59:00", "end_date_time": "2023-03-24 21:59:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down onto CR 94. Time estimated by radar.", "ts_dict_index": [11523, 11524, 11525]}
+{"event_id": 1087874, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:52:00", "end_date_time": "2023-03-24 21:52:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at 682 Pinegrove Drive. Time estimated by radar.", "ts_dict_index": [11481, 11482, 11483]}
+{"event_id": 1087873, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:47:00", "end_date_time": "2023-03-24 21:47:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at the intersection of McGee Street and Tressie Street. Time estimated by radar.", "ts_dict_index": [11550, 11551, 11552]}
+{"event_id": 1087863, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:44:00", "end_date_time": "2023-03-24 21:44:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at the intersection of Oak Hill Avenue and Edgewood Drive. Time estimated by radar.", "ts_dict_index": [11553, 11554, 11555]}
+{"event_id": 1087871, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:47:00", "end_date_time": "2023-03-24 21:47:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down on Ashe Blvd. near the railroad bridge. Time estimated by radar.", "ts_dict_index": [11541, 11542, 11543]}
+{"event_id": 1087860, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:38:00", "end_date_time": "2023-03-24 21:38:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at 2265 Old Memphis Pike. Time estimated by radar.", "ts_dict_index": [11556, 11557, 11558]}
+{"event_id": 1087868, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:45:00", "end_date_time": "2023-03-24 21:45:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at the intersection of St. Louis Avenue and West 6th Street. Time estimated by radar.", "ts_dict_index": [11544, 11545, 11546]}
+{"event_id": 1010118, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-04-05 00:37:00", "end_date_time": "2022-04-05 00:37:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited East Texas shortly after 1 am on the 5th. A downburst affected much of the southern and eastern sections of the city of Whitehouse, resulting in numerous trees being snapped and uprooted along its path. The majority of the more significant damage occurred in an east-southeasterly direction, which began in the Willows subdivision just west of Willingham Road, where several small Bradford pear trees were snapped, and small areas of shingles were ripped from the roofs of a couple of homes with winds estimated in the range of 70-75 mph. The winds from this downburst intensified as it crossed Willingham Road, affecting several streets along and to the west of Highway 110. Here, numerous hardwood trees and large limbs were snapped and uprooted, with winds consistent of 90-95 mph. Trees fell on at least 4 homes in this area. The maximum winds near 100 mph from this downburst were estimated as it impacted the Whitehouse Mobile Home and RV Park, where multiple large trees were snapped and uprooted. Unfortunately, one fatality occurred here as a large pine tree fell onto an RV on Barbara Drive, killing a 71 year-old male sleeping inside. Additional large hardwood trees were downed along and to the north of Hagan Road, Railroad Avenue, before weakening as it entered the Waterton subdivision on East Main Street. It should be noted that wind damage was noted across much of Smith County and East Texas from these severe thunderstorms.", "ts_dict_index": [11568, 11569, 11570]}
+{"event_id": 1010129, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-05 01:06:00", "end_date_time": "2022-04-05 01:06:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited East Texas shortly after 1 am on the 5th. A large tree was blown down and small limb debris fell onto County Road 407 near the Lakeview RV Park.", "ts_dict_index": [11565, 11566, 11567]}
+{"event_id": 1010140, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-05 01:10:00", "end_date_time": "2022-04-05 01:10:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited East Texas shortly after 1 am on the 5th. A roof was blown off of a building in Downtown Henderson.", "ts_dict_index": [11571, 11572, 11573]}
+{"event_id": 1010130, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-05 01:10:00", "end_date_time": "2022-04-05 01:10:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited East Texas shortly after 1 am on the 5th. A roof and an awning was damaged on a building on Richardson Drive in Henderson.", "ts_dict_index": [11559, 11560, 11561]}
+{"event_id": 1010128, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-05 01:05:00", "end_date_time": "2022-04-05 01:05:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited East Texas shortly after 1 am on the 5th. A storage building was blown to the side of the roadway on Highway 64 near the intersection of Highway 42 in the Turnertown community.", "ts_dict_index": [11574, 11575, 11576]}
+{"event_id": 1010141, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-05 01:15:00", "end_date_time": "2022-04-05 01:15:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited East Texas shortly after 1 am on the 5th. Small trees were downed and debris was thrown across FM 225 south of Henderson.", "ts_dict_index": [11562, 11563, 11564]}
+{"event_id": 1088460, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2023-03-24 21:52:00", "end_date_time": "2023-03-24 22:12:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A bow echo from an embedded supercell within a line of thunderstorms intensified and produced destructive winds in a narrow swath of north and northeast Florence.|Wind speeds of 60-65 mph occurred in much of this area, with a few gusts of 80-90 mph in a few locations. Trees, power poles and power lines were taken down in multiple locations. Trees were knocked down onto multiple homes and vehicles. The Seven Points district and areas just north and northeast of the University of North Alabama campus were hit particular hard. Along this long swath, a significant number of trees, power lines and power pols were knocked down. Many residences experience minor to severe damage from trees falling onto their homes or vehicles.", "ts_dict_index": [11529, 11530, 11531]}
+{"event_id": 959075, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-01 15:59:00", "end_date_time": "2021-07-01 15:59:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Several reports of downed power lines near Fairless Hills. Time estimated from radar.", "ts_dict_index": [11598, 11599, 11600]}
+{"event_id": 959062, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-01 16:39:00", "end_date_time": "2021-07-01 16:39:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Wires were downed on Locust Trail in Browns Mills. Time estimated from radar.", "ts_dict_index": [11619, 11620, 11621]}
+{"event_id": 959077, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-01 15:53:00", "end_date_time": "2021-07-01 15:53:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. There were numerous reports of downed tree limbs and wires in Levittown. Radar indicated some rotation with this storm, prompting a Tornado Warning. However, damage was consistent with straight line winds. Time estimated from radar.", "ts_dict_index": [11601, 11602, 11603]}
+{"event_id": 867082, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-12-28 22:48:00", "end_date_time": "2019-12-28 22:48:00", "narrative": "A system dragged a cold front toward Arkansas on the 28th. The front sparked a line of showers and isolated thunderstorms. While temperatures remained mild (in the 60s to lower 70s), the atmosphere was not overly unstable. It made it difficult for thunderstorms to develop, and there was very little lightning.||Looking aloft, winds were sustained at 50 to 60 mph between 5000 and 10000 feet. These higher speeds combined with acceleration in heavy downpours were driven toward the ground in spots. This resulted in some wind damage.||At Haskell (Saline County), trees were downed and minor roof damage occurred. A dugout was also destroyed at a local high school. A large pine tree fell on a mobile home in the Landmark area about ten miles south of Little Rock (Pulaski County). A woman was injured and was taken to a hospital. Just northeast of Williford (Sharp County), a barn was heavily damaged. A house near Guy (Faulkner County) lost much of its roof. More trees were toppled around Ozone (Johnson County), Solgohachia (Conway County), Quitman (Cleburne County), and east of Malvern (Hot Spring County). The time was updated based on the NWS storm survey. A large tree was blown down on top of a mobile home, causing substantial damage and one injury.", "ts_dict_index": [11586, 11587, 11588]}
+{"event_id": 959080, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-01 14:51:00", "end_date_time": "2021-07-01 14:51:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Several reports of downed tree limbs and wires near Valley Forge and Phoenixville. Time estimated from radar.", "ts_dict_index": [11613, 11614, 11615]}
+{"event_id": 959074, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-01 15:50:00", "end_date_time": "2021-07-01 15:50:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. A tree was downed on US-1. Time estimated from radar.", "ts_dict_index": [11610, 11611, 11612]}
+{"event_id": 959065, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-01 14:13:00", "end_date_time": "2021-07-01 14:13:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. A tree was downed on Lammey Rd. Time estimated from radar.", "ts_dict_index": [11604, 11605, 11606]}
+{"event_id": 959066, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-01 14:21:00", "end_date_time": "2021-07-01 14:21:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. A tree was downed on Fisherville Rd. Time estimated from radar.", "ts_dict_index": [11607, 11608, 11609]}
+{"event_id": 959071, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-01 14:23:00", "end_date_time": "2021-07-01 14:23:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. An mPing report of tree limbs or power lines down near Route 100. Time estimated from radar.", "ts_dict_index": [11616, 11617, 11618]}
+{"event_id": 959067, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-01 14:27:00", "end_date_time": "2021-07-01 14:27:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. A tree was downed on Beaver Run Rd. Time estimated from radar.", "ts_dict_index": [11622, 11623, 11624]}
+{"event_id": 959064, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-01 14:31:00", "end_date_time": "2021-07-01 14:31:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Wires were downed near Horseshoe Trail. Time estimated from radar.", "ts_dict_index": [11592, 11593, 11594]}
+{"event_id": 1010124, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-05 01:00:00", "end_date_time": "2022-04-05 01:00:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited East Texas shortly after 1 am on the 5th. Power lines were downed in and near the New London community.", "ts_dict_index": [11580, 11581, 11582]}
+{"event_id": 1010122, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2022-04-05 00:50:00", "end_date_time": "2022-04-05 00:50:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited East Texas shortly after 1 am on the 5th. A tree was blown down at the intersection of FM 449 and FM 450.", "ts_dict_index": [11577, 11578, 11579]}
+{"event_id": 959063, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-07-01 14:21:00", "end_date_time": "2021-07-01 14:21:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Wires were downed near Elm Rd. Time estimated from radar.", "ts_dict_index": [11589, 11590, 11591]}
+{"event_id": 1087870, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2023-03-24 21:47:00", "end_date_time": "2023-03-24 21:47:00", "narrative": "A severe line of thunderstorms rolled through north Alabama during the late evening hours of the 24th into the early morning hours of the 25th, producing 7 tornadoes. An embedded supercell thunderstorm with a history of tornadoes in Mississippi moved east-northeast across northwest Alabama, yielding another two tornadoes in Lauderdale County in Florence and near Anderson. Associated with this line, multiple narrow swaths of intense damaging winds of 60 to 90 mph occurred across the Shoals metro area, including Sheffield, Tuscumbia, Muscle Shoals and Florence.  The winds caused widespread power outages, damaged numerous structures, and toppled or snapped numerous trees, power poles and power lines. A few trees and power poles were dropped onto residences and vehicles, either destroying or heavily damaging them. Roof damages were reported at many locations as well. All told, an estimated #### million in damages occurred, the majority in northwest Alabama in Colbert and Lauderdale Counties.  As the line continued east, additional tornadoes were spawned in Lawrence, Morgan, Jackson and DeKalb Counties. A tree was knocked down at 3306 Northeast 13th Avenue. Time estimated by radar.", "ts_dict_index": [11547, 11548, 11549]}
+{"event_id": 959085, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-01 15:00:00", "end_date_time": "2021-07-01 15:00:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Trees and wires were downed on Marshall Bridge Rd in Kennett Square. Time estimated from radar.", "ts_dict_index": [11628, 11629, 11630]}
+{"event_id": 959083, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-01 14:26:00", "end_date_time": "2021-07-01 14:26:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Trees and wires were downed near Valley Station Rd in Coatesville. Time estimated from radar.", "ts_dict_index": [11625, 11626, 11627]}
+{"event_id": 959084, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-01 14:47:00", "end_date_time": "2021-07-01 14:47:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Wires were downed near Paradise Valley Nature area in Downingtown. Time estimated from radar.", "ts_dict_index": [11631, 11632, 11633]}
+{"event_id": 959053, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-01 16:19:00", "end_date_time": "2021-07-01 16:19:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Wires were downed on Grand Ave. Time estimated from radar.", "ts_dict_index": [11595, 11596, 11597]}
+{"event_id": 959056, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-07-01 17:20:00", "end_date_time": "2021-07-01 17:20:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Several reports of downed wires in Brick Twp and the Leisure Village area. Time estimated from radar.", "ts_dict_index": [11634, 11635, 11636]}
+{"event_id": 879680, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-04-13 15:33:00", "end_date_time": "2020-04-13 15:33:00", "narrative": "A highly anomalous weather system affected much of the eastern United States on April 13. From the night of April 12 through the day on April 13, strengthening low pressure tracked in an almost due northerly direction from the Ohio Valley, through the Great Lakes, and into Canada. A record strong low level jet developed ahead of it along the East Coast. In the mid-Atlantic, a warm front moved through the region during the morning of the 13th, bringing showery weather. During and after the warm frontal passage, mixing with the low level jet brought destructive wind gusts to the surface, especially near the coast where gusts were enhanced by a well-defined gravity wave.||During the afternoon hours, a strong cold front approached, providing strong forcing to an environment of strong to extreme wind shear. Instability was limited due to a lack of clearing following the morning warm frontal passage. However, enough heating occurred by mid-afternoon that a line of strong to severe thunderstorms did manage to develop, producing a number of damaging wind reports as it moved towards the coast. Wires were downed on US-9 with all lanes closed and detoured.", "ts_dict_index": [11682, 11683, 11684]}
+{"event_id": 959081, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-01 15:19:00", "end_date_time": "2021-07-01 15:19:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Trees and wires were downed near Turk Rd in Doylestown. Time estimated from radar.", "ts_dict_index": [11643, 11644, 11645]}
+{"event_id": 959070, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-01 15:12:00", "end_date_time": "2021-07-01 15:12:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Tree limbs were downed on Joshua Rd near Cedar Grove Rd. Time estimated from radar.", "ts_dict_index": [11646, 11647, 11648]}
+{"event_id": 959082, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-01 14:59:00", "end_date_time": "2021-07-01 14:59:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. Trees and wires were downed near Garfield Park in Lansdale. Time estimated from radar.", "ts_dict_index": [11640, 11641, 11642]}
+{"event_id": 854869, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-10-21 00:55:00", "end_date_time": "2019-10-21 00:55:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. While an isolated severe thunderstorm developed over portions of East Texas during the evening, which moved into Northwest Louisiana before diminishing, additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Southeast Oklahoma and Northeast Texas, which later pushed into Southwest Arkansas and North Louisiana ahead of this trough and associated strong cold front. These storms produced several reports of damaging winds which downed trees and power lines across portions of McCurtain County Oklahoma, before diminishing shortly after daybreak with the departure of this system. Trees and power lines were downed in Broken Bow.", "ts_dict_index": [11649, 11650, 11651]}
+{"event_id": 854868, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-10-21 00:51:00", "end_date_time": "2019-10-21 00:51:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. While an isolated severe thunderstorm developed over portions of East Texas during the evening, which moved into Northwest Louisiana before diminishing, additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Southeast Oklahoma and Northeast Texas, which later pushed into Southwest Arkansas and North Louisiana ahead of this trough and associated strong cold front. These storms produced several reports of damaging winds which downed trees and power lines across portions of McCurtain County Oklahoma, before diminishing shortly after daybreak with the departure of this system. Trees and power lines were downed in Idabel.", "ts_dict_index": [11652, 11653, 11654]}
+{"event_id": 854866, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-10-20 22:02:00", "end_date_time": "2019-10-20 22:02:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. While an isolated severe thunderstorm developed over portions of East Texas during the evening, which moved into Northwest Louisiana before diminishing, additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Southeast Oklahoma and Northeast Texas, which later pushed into Southwest Arkansas and North Louisiana ahead of this trough and associated strong cold front. These storms produced several reports of damaging winds which downed trees and power lines across portions of McCurtain County Oklahoma, before diminishing shortly after daybreak with the departure of this system. Power lines were downed in Downtown Valliant.", "ts_dict_index": [11655, 11656, 11657]}
+{"event_id": 1095369, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-05-16 14:28:00", "end_date_time": "2023-05-16 14:28:00", "narrative": "The most widespread severe thunderstorm activity in many months broke out across eastern Kentucky on Tuesday, May 16th. A warm front lifted to near the Mountain Parkway during the morning hours, ushering in a muggy airmass for those locations to the south of the Parkway. Sun shining on this juicy air mass helped build up moderate amounts of instability south of the warm front as temperatures warmed into the upper 70s to mid 80s there. Meanwhile, persistent cloud cover and a weak northeasterly breeze north of the front kept temperatures cooler and conditions much more stable. A wave of low pressure rode along the stalled warm front during this afternoon, triggering supercell storms in the area between the warm front and the Hal Rogers Parkway/KY-80 corridor. These storms dropped severe to significant-sized hail. One of the supercells also produced a brief tornado in Magoffin County southwest of Salyersville. Further south, weaker shear led to less organized storm structures, but even there the storms still generated strong outflows leading to bowing storm lines and damaging wind gusts. County dispatch reported power line blown down on Bourne Avenue close to the intersection of Murphy Avenue.", "ts_dict_index": [11670, 11671, 11672]}
+{"event_id": 1095385, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-05-16 14:45:00", "end_date_time": "2023-05-16 14:45:00", "narrative": "The most widespread severe thunderstorm activity in many months broke out across eastern Kentucky on Tuesday, May 16th. A warm front lifted to near the Mountain Parkway during the morning hours, ushering in a muggy airmass for those locations to the south of the Parkway. Sun shining on this juicy air mass helped build up moderate amounts of instability south of the warm front as temperatures warmed into the upper 70s to mid 80s there. Meanwhile, persistent cloud cover and a weak northeasterly breeze north of the front kept temperatures cooler and conditions much more stable. A wave of low pressure rode along the stalled warm front during this afternoon, triggering supercell storms in the area between the warm front and the Hal Rogers Parkway/KY-80 corridor. These storms dropped severe to significant-sized hail. One of the supercells also produced a brief tornado in Magoffin County southwest of Salyersville. Further south, weaker shear led to less organized storm structures, but even there the storms still generated strong outflows leading to bowing storm lines and damaging wind gusts. County dispatch reported tree blown down around the 2000 block of Old Whitney Road.", "ts_dict_index": [11667, 11668, 11669]}
+{"event_id": 854867, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-10-21 00:25:00", "end_date_time": "2019-10-21 00:25:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. While an isolated severe thunderstorm developed over portions of East Texas during the evening, which moved into Northwest Louisiana before diminishing, additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Southeast Oklahoma and Northeast Texas, which later pushed into Southwest Arkansas and North Louisiana ahead of this trough and associated strong cold front. These storms produced several reports of damaging winds which downed trees and power lines across portions of McCurtain County Oklahoma, before diminishing shortly after daybreak with the departure of this system. Several large trees fell onto a mobile home west of Valliant on Sandpiper Road near the Choctaw County line. One fatality occurred at the scene when a 48 year old female was killed by a fallen tree. One injury was also reported to a male resident in the home.", "ts_dict_index": [11658, 11659, 11660]}
+{"event_id": 1095366, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-05-16 14:25:00", "end_date_time": "2023-05-16 14:25:00", "narrative": "The most widespread severe thunderstorm activity in many months broke out across eastern Kentucky on Tuesday, May 16th. A warm front lifted to near the Mountain Parkway during the morning hours, ushering in a muggy airmass for those locations to the south of the Parkway. Sun shining on this juicy air mass helped build up moderate amounts of instability south of the warm front as temperatures warmed into the upper 70s to mid 80s there. Meanwhile, persistent cloud cover and a weak northeasterly breeze north of the front kept temperatures cooler and conditions much more stable. A wave of low pressure rode along the stalled warm front during this afternoon, triggering supercell storms in the area between the warm front and the Hal Rogers Parkway/KY-80 corridor. These storms dropped severe to significant-sized hail. One of the supercells also produced a brief tornado in Magoffin County southwest of Salyersville. Further south, weaker shear led to less organized storm structures, but even there the storms still generated strong outflows leading to bowing storm lines and damaging wind gusts. County dispatch reported tree blown down off of Nelson Valley Road near the intersection of Jeffries Drive.", "ts_dict_index": [11676, 11677, 11678]}
+{"event_id": 1126053, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-08 06:10:00", "end_date_time": "2023-08-08 06:10:00", "narrative": "The combination of an outflow boundary as well as gravity waves in the mid to upper levels originating from a decaying thunderstorm complex that developed across northern Sonora, Mexico the evening prior resulted in elevated thunderstorm development across portions of the Phoenix metro area during the early morning hours of the 8th. Precipitable water values near 1.7 inches and elevated instability with MLCAPE of a couple of hundreds of J/KG were sufficient for some of these thunderstorms to become strong. One thunderstorm complex in particular developed and affected the Chandler to Gilbert areas, resulting in tree damage with estimated wind gusts of between 55-60 mph based on radar data. ||Later during the day, during the afternoon and early evening hours, thunderstorms developed and affected portions of southeast Arizona. Outflows from these storms resulted in additional development further north into northwestern Pinal County, including Arizona City, where some isolated wind damage was reported. The environment was characterized by moderate instability with MLCAPE of 1000-1500 J/KG. Video as well as pictures showed several trees were damaged along the general between North Cooper Road and South Gilbert Road in Gilbert. Some trees had tree limbs broken while other trees were uprooted. Wind gusts were estimated between 55-60 mph based on radar estimates. No injuries were reported.", "ts_dict_index": [11661, 11662, 11663]}
+{"event_id": 1126063, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-08-08 17:50:00", "end_date_time": "2023-08-08 17:50:00", "narrative": "The combination of an outflow boundary as well as gravity waves in the mid to upper levels originating from a decaying thunderstorm complex that developed across northern Sonora, Mexico the evening prior resulted in elevated thunderstorm development across portions of the Phoenix metro area during the early morning hours of the 8th. Precipitable water values near 1.7 inches and elevated instability with MLCAPE of a couple of hundreds of J/KG were sufficient for some of these thunderstorms to become strong. One thunderstorm complex in particular developed and affected the Chandler to Gilbert areas, resulting in tree damage with estimated wind gusts of between 55-60 mph based on radar data. ||Later during the day, during the afternoon and early evening hours, thunderstorms developed and affected portions of southeast Arizona. Outflows from these storms resulted in additional development further north into northwestern Pinal County, including Arizona City, where some isolated wind damage was reported. The environment was characterized by moderate instability with MLCAPE of 1000-1500 J/KG. A parked semi-truck was blown over in the area of West Monaco Boulevard and South Saxon Road in Arizona City. Given that the truck was parked, it was likely that it was empty and thus was more likely to be blown over by sub-severe winds, which were estimated to be at around 50 mph. No injuries were reported.", "ts_dict_index": [11664, 11665, 11666]}
+{"event_id": 1095365, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-05-16 14:25:00", "end_date_time": "2023-05-16 14:25:00", "narrative": "The most widespread severe thunderstorm activity in many months broke out across eastern Kentucky on Tuesday, May 16th. A warm front lifted to near the Mountain Parkway during the morning hours, ushering in a muggy airmass for those locations to the south of the Parkway. Sun shining on this juicy air mass helped build up moderate amounts of instability south of the warm front as temperatures warmed into the upper 70s to mid 80s there. Meanwhile, persistent cloud cover and a weak northeasterly breeze north of the front kept temperatures cooler and conditions much more stable. A wave of low pressure rode along the stalled warm front during this afternoon, triggering supercell storms in the area between the warm front and the Hal Rogers Parkway/KY-80 corridor. These storms dropped severe to significant-sized hail. One of the supercells also produced a brief tornado in Magoffin County southwest of Salyersville. Further south, weaker shear led to less organized storm structures, but even there the storms still generated strong outflows leading to bowing storm lines and damaging wind gusts. A member of the public reported a tree blown down along KY-80 near Somerset.", "ts_dict_index": [11673, 11674, 11675]}
+{"event_id": 1010126, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-04-05 01:05:00", "end_date_time": "2022-04-05 01:05:00", "narrative": "Warm, moist, and unstable air spread north across North and East Texas, North Louisiana, and extreme Southern Arkansas during the evening through the early morning hours of April 4th-5th, behind a warm front that lifted north through these areas. Meanwhile, an upper trough dug through Western Texas and into the Southern Plains during the afternoon and evening hours of the 4th, enhancing large scale forcing along and ahead of a dry line that developed and spread east across North-central Texas. This resulted in shower and thunderstorm development which rapidly intensified over this area, which spread east into East Texas during the late evening through the early morning hours of the 4th-5th. Given the extent of instability and the strong southerly low level jet in place, these storms became severe as they spread east across East Texas and North Louisiana, resulting in numerous reports of damaging winds as these storms organized into a quasi-linear convective system (QLCS) which quickly spread across the region through the pre-dawn hours. These storms exited East Texas shortly after 1 am on the 5th. A large tree was blown down on Highway 259 between Henderson and Kilgore.", "ts_dict_index": [11583, 11584, 11585]}
+{"event_id": 1086989, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-03-03 00:20:00", "end_date_time": "2023-03-03 00:20:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Large pine tree downed on Highway 527 south of Sligo Road.", "ts_dict_index": [11697, 11698, 11699]}
+{"event_id": 1086993, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-03-02 23:22:00", "end_date_time": "2023-03-02 23:22:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Tree downed on Roy Road near Blanchard.", "ts_dict_index": [11691, 11692, 11693]}
+{"event_id": 1088031, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-03-02 22:27:00", "end_date_time": "2023-03-02 22:27:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Numerous trees downed across parts of Harrison County.", "ts_dict_index": [11700, 11701, 11702]}
+{"event_id": 1087635, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-03-02 22:36:00", "end_date_time": "2023-03-02 22:36:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Several trees downed near FM Road 1798 and County Road 2174 near Laneville.", "ts_dict_index": [11694, 11695, 11696]}
+{"event_id": 1153314, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-12-22 18:00:00", "end_date_time": "2023-12-22 18:00:00", "narrative": "A potent upper-level low pressure system situated across southern California transported a plume of deep subtropical moisture across the Desert Southwest, with PWAT values peaking as high as 1-1.2 across portions of southern Arizona. PWATs this high in late December is near the 99th percentile of climatology. The anonymously high moisture content in combination with the strong dynamics associated with the low pressure system itself resulted in the development of widespread rainfall activity across most of central and southern Arizona. Widespread rainfall amounts of between 0.5-2 with locally higher amounts were observed, resulting in areas of localized flooding. Embedded within the widespread rainfall activity were a couple of linear segments of strong thunderstorms that materialized mainly across portions of southwestern Arizona between Yuma through western Maricopa Counties due to some instability with MLCAPE values between 100-500 J/KG. Localized damaging winds were observed with a linear segment that moved from west to east from eastern Yuma through southwestern Maricopa Counties. The Oatman RAWS station measured a 66 mph wind gust.", "ts_dict_index": [11685, 11686, 11687]}
+{"event_id": 959069, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-01 15:30:00", "end_date_time": "2021-07-01 15:30:00", "narrative": "After a significant heatwave, a cold front approached the mid-Atlantic on July 1, 2021. A potent mid-level trough was also digging southward through southern Ontario and into the Great Lakes region, and a strong upper level jet streak was present downstream the trough axis, over the interior mid-Atlantic and northern New England. This strong upper level forcing combined with the approaching front and a lingering warm, moist air mass ahead of it caused widespread thunderstorm development on July 1. Storms occurred almost exclusively south of Interstate 78, in the environment of best instability. A number of storms became severe, taking the form of mainly linear and multi-cellular clusters but with some embedded supercellular characteristics. Straight line wind damage was the primary hazard, with a number of reports of downed trees and power outages due to winds. With the cold front remaining to the west, some storm activity continued into the overnight, but storm coverage and intensity gradually waned with the loss of daytime heating and the overturning of the atmosphere from earlier storms. A tree and wires were downed near the intersection of Washington Ln and Pepper Rd. Time estimated from radar.", "ts_dict_index": [11637, 11638, 11639]}
+{"event_id": 1086986, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-03-02 23:35:00", "end_date_time": "2023-03-02 23:35:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Tree downed in back yard of a house along Camelback Drive.", "ts_dict_index": [11706, 11707, 11708]}
+{"event_id": 1087982, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-03-02 21:20:00", "end_date_time": "2023-03-02 21:20:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Numerous trees and power lines downed across parts of Smith County.", "ts_dict_index": [11721, 11722, 11723]}
+{"event_id": 1086991, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-03-03 01:18:00", "end_date_time": "2023-03-03 01:18:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Tree downed on a house trapping the occupant who was reported to be uninjured.", "ts_dict_index": [11718, 11719, 11720]}
+{"event_id": 1086990, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2023-03-03 00:42:00", "end_date_time": "2023-03-03 00:42:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Tree downed near the Heflin community.", "ts_dict_index": [11712, 11713, 11714]}
+{"event_id": 931631, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:25:00", "end_date_time": "2021-01-25 13:25:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm pushed east and across the western portion of the greater Phoenix area during early afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front generated some gusty and damaging outflow winds. At 1325MST a public social media post showed a large Palo Verde tree approximately one foot in diameter that was blown down and crashed through a concrete wall and onto a house. Another social media post showed the roof of a gazebo ripped off and a concrete block wall blown over. Winds were estimated to be at least 55 mph in strength. The damage occurred about 3 miles north of Goodyear, or just southeast of the intersection of Highway 303 and Indian School Road. An outdoor COVID-19 vaccination site in Goodyear also reported some minor damage. There were no reports of any injuries.", "ts_dict_index": [11727, 11728, 11729]}
+{"event_id": 931678, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:45:00", "end_date_time": "2021-01-25 13:45:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved through the central portion of the greater Phoenix area during the afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front caused some gusty and damaging outflow wind in the community of Glendale. According to a report from the general public, at 1345MST gusty winds estimated as high as 60 mph downed a large tree which damaged a carport when it fell. The downed tree was located about 4 miles northeast of Glendale and near the intersection of 35th Avenue and Thunderbird Road.", "ts_dict_index": [11733, 11734, 11735]}
+{"event_id": 931633, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:36:00", "end_date_time": "2021-01-25 13:36:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved east across the western portion of the greater Phoenix area during the early afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front generated some gusty and damaging outflow winds that affected areas around Sun City. According to reports from local broadcast media, at 1336MST gusty winds estimated up to 60 mph ripped the roof off a home and also ripped off roof singles from a few other homes in Sun City; the winds also downed a couple of Palo Verde trees and blew down some fencing. The damage occurred about 1 mile northeast of Youngtown, and along 107th Avenue just to the south of Alabama Avenue. An outdoor COVID-19 vaccination site near Sun City also experienced some minor damage from the strong winds that moved through the area. There were no reports of injuries due to the damaging winds.", "ts_dict_index": [11730, 11731, 11732]}
+{"event_id": 1087641, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-03-02 22:30:00", "end_date_time": "2023-03-02 22:30:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Numerous trees downed, shingles removed and one brick support blown away in Marshall.", "ts_dict_index": [11709, 11710, 11711]}
+{"event_id": 931628, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:55:00", "end_date_time": "2021-01-25 14:00:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved through the central portions of the greater Phoenix area during the early afternoon hours on January 25th. A line of severe thunderstorms developed as the front moved through and they generated gusty and damaging outflow winds. According to a report from the public, at 1355MST gusty winds estimated at 65 mph knocked down two large trees into an apartment complex at 15th Avenue and Camelback Road, just to the east of Interstate 17, causing major structural damage to the apartment and minor damage to a car. At roughly the same time and a few miles to the east, local broadcast media reported that similarly strong outflow winds caused a palm tree to snap at its base and the tree fell onto an apartment complex located near 12th Street and Highland Avenue. The falling palm tree crashed through a second story unit with the single resident and his dog present at the time. Fortunately there were no reports of injuries at either location due to the falling trees. An COVID-19 vaccination site located at the State Fairgrounds sustained minor damage as the strong winds moved through the area.", "ts_dict_index": [11724, 11725, 11726]}
+{"event_id": 1088035, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-03-02 17:30:00", "end_date_time": "2023-03-02 17:30:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Large tree downed on FM Road 1997 between Marshall and Jefferson.", "ts_dict_index": [11715, 11716, 11717]}
+{"event_id": 931641, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:53:00", "end_date_time": "2021-01-25 13:53:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved through the northern and central portions of the greater Phoenix area, including communities of Peoria and Deer Valley, during afternoon hours on January 25th. A line of severe thunderstorms developed as the front moved through and they generated gusty and damaging outflow winds. According to a report from the general public, at 1353MST gusty winds estimated to be as high as 65 mph downed a number of trees near the intersection of 15th Avenue and Rose Garden Lane, about 9 miles east of Peoria. This was just northeast of the intersection of Loop 101 and Interstate 17. The Twitter follower also reported that there was a lot of debris in the area due to the strong winds. There were no reports of any injuries due to the damaging wind and falling trees.", "ts_dict_index": [11736, 11737, 11738]}
+{"event_id": 1095361, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-05-16 14:24:00", "end_date_time": "2023-05-16 14:24:00", "narrative": "The most widespread severe thunderstorm activity in many months broke out across eastern Kentucky on Tuesday, May 16th. A warm front lifted to near the Mountain Parkway during the morning hours, ushering in a muggy airmass for those locations to the south of the Parkway. Sun shining on this juicy air mass helped build up moderate amounts of instability south of the warm front as temperatures warmed into the upper 70s to mid 80s there. Meanwhile, persistent cloud cover and a weak northeasterly breeze north of the front kept temperatures cooler and conditions much more stable. A wave of low pressure rode along the stalled warm front during this afternoon, triggering supercell storms in the area between the warm front and the Hal Rogers Parkway/KY-80 corridor. These storms dropped severe to significant-sized hail. One of the supercells also produced a brief tornado in Magoffin County southwest of Salyersville. Further south, weaker shear led to less organized storm structures, but even there the storms still generated strong outflows leading to bowing storm lines and damaging wind gusts. County dispatch reported tree blown down onto a power line off of KY-1247 near the intersection of Raleigh Road.", "ts_dict_index": [11679, 11680, 11681]}
+{"event_id": 932312, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:40:00", "end_date_time": "2021-01-25 13:40:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved through the western portions of the greater Phoenix area, including the community of Glendale, during the afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front generated some gusty and damaging outflow winds. At around 1340MST, reports show that strong winds estimated around 60 mph caused damage to six vehicles, numerous trees, and campus buildings at Glendale Community College. A power line also sustained damage along Olive Ave. No injuries were reported.", "ts_dict_index": [11748, 11749, 11750]}
+{"event_id": 932306, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:49:00", "end_date_time": "2021-01-25 13:49:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm pushed east and across the western portion of the greater Phoenix area during early afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front generated some gusty and damaging outflow winds. A wind gust of 56 mph was measured at the Glendale Municipal Airport. Less than 2 miles to the east of the airport, an outdoor COVID-19 vaccination site at State Farm Stadium saw minor damages to the tents and overall setup, which led to delays. No injuries were reported.", "ts_dict_index": [11745, 11746, 11747]}
+{"event_id": 931640, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:50:00", "end_date_time": "2021-01-25 13:50:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved through central portions of the greater Phoenix area during the afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front generated some gusty and damaging outflow winds that affected the community of Paradise Valley. According a a report from a trained spotter located about 2 miles northwest of Paradise Valley, strong winds downed a 50 foot tall tree that was 2 feet in diameter. The tree was downed near the intersection of Doubletree Ranch Road and Tatum Boulevard. No damage or injuries occurred as a result of the falling tree.", "ts_dict_index": [11742, 11743, 11744]}
+{"event_id": 932238, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:29:00", "end_date_time": "2021-01-25 13:29:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm pushed east and across the western portion of the greater Phoenix area during early afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front generated some gusty and damaging outflow winds. In Litchfield Park, multiple public social media photos and videos showed substantial tree damage at the Wigwam Golf Course. Numerous large tree branches were snapped and trees were uprooted due to outflow winds estimated around 70 mph. A golf event was taking place at the time, but fortunately there were no reports of injuries. Just across the street to the west of the golf course, an NWS COOP observer reported their 50 year old Aleppo pine tree was blown down by the strong winds and the tree damaged a corner of the observer's house. They reported an 8 inch diameter tree and a 30 foot long block wall were also knocked down. A social media post shared by local media showed an awning with metal supports was destroyed at a playground next to the same COOP observer. Timing estimated by radar.", "ts_dict_index": [11739, 11740, 11741]}
+{"event_id": 1086992, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-03-03 01:59:00", "end_date_time": "2023-03-03 01:59:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. A tree was downed and blocking one lane on Highway 2 near Dean Road.", "ts_dict_index": [11688, 11689, 11690]}
+{"event_id": 915027, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-08-24 17:57:00", "end_date_time": "2020-08-24 17:57:00", "narrative": "A hot and humid airmass was in place, providing enough energy for scattered thunderstorms to develop across the region. The hardest hit area was in the town of Whitehall, New York which saw repeated rounds of heavy rain and thunderstorms during the afternoon and early evening hours of August 24th. An impressive 4 to 6 inches of rain fell across the far northeast portions of Washington County, resulting in 8 flooded roadways, 21 flooded structures, 1 water rescue, several cars partially submerged and the Whitehall Junior-Senior High School being significantly damaged by the flood waters. The school superintendent estimated that it would cost 16 million dollars to repair the damages from the flood waters. Overall, 40 homes and 13 businesses or non-profit organizations sustained damage totaling 1.5 million dollars. There was also about 1,200 power outages as a result of the storms in Washington County. A Physical Disaster Declaration was declared for Washington County as a result of the storms. There was also one isolated report of trees down in Albany county from a separate storm. Trees were downed onto wires along North Mountain Street as well as a tree downed on McCotter Street. Time was estimated by radar.", "ts_dict_index": [11775, 11776, 11777]}
+{"event_id": 915024, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-08-24 16:05:00", "end_date_time": "2020-08-24 16:05:00", "narrative": "A hot and humid airmass was in place, providing enough energy for scattered thunderstorms to develop across the region. The hardest hit area was in the town of Whitehall, New York which saw repeated rounds of heavy rain and thunderstorms during the afternoon and early evening hours of August 24th. An impressive 4 to 6 inches of rain fell across the far northeast portions of Washington County, resulting in 8 flooded roadways, 21 flooded structures, 1 water rescue, several cars partially submerged and the Whitehall Junior-Senior High School being significantly damaged by the flood waters. The school superintendent estimated that it would cost 16 million dollars to repair the damages from the flood waters. Overall, 40 homes and 13 businesses or non-profit organizations sustained damage totaling 1.5 million dollars. There was also about 1,200 power outages as a result of the storms in Washington County. A Physical Disaster Declaration was declared for Washington County as a result of the storms. There was also one isolated report of trees down in Albany county from a separate storm. Trees were downed on North and South Williams Streets and County Route 12. A tree was downed onto a vehicle along South Williams Street. Time was estimated by radar.", "ts_dict_index": [11772, 11773, 11774]}
+{"event_id": 915023, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-08-24 16:03:00", "end_date_time": "2020-08-24 16:03:00", "narrative": "A hot and humid airmass was in place, providing enough energy for scattered thunderstorms to develop across the region. The hardest hit area was in the town of Whitehall, New York which saw repeated rounds of heavy rain and thunderstorms during the afternoon and early evening hours of August 24th. An impressive 4 to 6 inches of rain fell across the far northeast portions of Washington County, resulting in 8 flooded roadways, 21 flooded structures, 1 water rescue, several cars partially submerged and the Whitehall Junior-Senior High School being significantly damaged by the flood waters. The school superintendent estimated that it would cost 16 million dollars to repair the damages from the flood waters. Overall, 40 homes and 13 businesses or non-profit organizations sustained damage totaling 1.5 million dollars. There was also about 1,200 power outages as a result of the storms in Washington County. A Physical Disaster Declaration was declared for Washington County as a result of the storms. There was also one isolated report of trees down in Albany county from a separate storm. Numerous snapped and downed trees near Skenesborough Drive in Whitehall. A house nearby also had roof damage.", "ts_dict_index": [11778, 11779, 11780]}
+{"event_id": 931679, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:50:00", "end_date_time": "2021-01-25 14:00:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm pushed across the north central portion of the greater Phoenix area during the afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the frontal passage generated some damaging outflow winds affecting northern portions of the town of Glendale. According to a report from the general public, at 1350MST strong winds estimated to be nearly 70 mph in strength blew down a large steel power pole and power lines near 3040 West Morrow Drive, about 7 miles northeast of Glendale. About 10 minutes later, local broadcast media reported that 9 power poles were blown down near the intersection of 35th Avenue and Union Hills Drive. Both incidents of downed poles took place just west of Interstate 17 and between the Loop 101 and Bell Road. No injuries were reported.", "ts_dict_index": [11757, 11758, 11759]}
+{"event_id": 931681, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:40:00", "end_date_time": "2021-01-25 13:41:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved through the north central portion of the greater Phoenix area during the afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front generated some gusty and damaging outflow winds that affected northern portions of the town of Glendale. According to the trained weather spotter, at about 1340MST gusty winds estimated to be upwards of 65 mph damaged the roof of a home, and managed to blow a wind turbine off of the roof. The damage occurred about 6 miles northeast of Glendale, just southwest of the intersection of Bell Road and Interstate 17. There were no injuries reported.", "ts_dict_index": [11769, 11770, 11771]}
+{"event_id": 931530, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:45:00", "end_date_time": "2021-01-25 13:45:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved through the southeast portion of the greater Phoenix area during the early afternoon on January 25th. A line of strong to severe thunderstorms associated with the front produced strong wind gusts estimated to be in excess of 60 mph at times. According to a trained weather spotter located 5 miles southwest of Mesa, the strong winds blew a rooftop air conditioner off of the roof at about 1345MST. Additionally, roof shingles were stripped off of rooftops in the area as the winds blew through the area. The damage occurred southeast of the intersection of Baseline and Cooper roads. There were no reports of injury due to the damaging winds.", "ts_dict_index": [11751, 11752, 11753]}
+{"event_id": 931682, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 14:00:00", "end_date_time": "2021-01-25 14:00:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved through the north central portion of the greater Phoenix area during the afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front generated some gusty and damaging outflow winds. According to a Twitter follower located about 8 miles northeast of the town of Glendale, at 1400MST gusty winds estimated at 60 mph blew down a large tree near the intersection of 19th Avenue and Union Hills Drive. This is just northeast of the Bell Road and Interstate 17 intersection. No injuries were reported.", "ts_dict_index": [11766, 11767, 11768]}
+{"event_id": 931635, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:55:00", "end_date_time": "2021-01-25 14:00:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved across the central portion of the greater Phoenix area during the early afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the frontal passage developed some gusty and damaging outflow winds. At 1355MST a trained spotter located 5 miles northeast of Phoenix reported roof damage, as winds estimated as high as 60 mph blew the roof off of a shed. The damage occurred just south of Lookout Mountain Park. Just a few minutes later and not far to the west, broadcast media reported that power poles were down, and some of them were of the metal variety. The outflow winds here were estimated to be as high as 70 mph. The downed poles were near the intersection of 7th Street and Thunderbird Road. There were no reports of injury due to the damaging winds.", "ts_dict_index": [11763, 11764, 11765]}
+{"event_id": 931637, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 14:00:00", "end_date_time": "2021-01-25 14:02:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved across central and eastern portions of the greater Phoenix area during the afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front produced some gusty and damaging outflow winds that affected portions of Paradise Valley. According to a report from the public, at about 1400MST gusty winds estimated as high as 60 mph blew down some large trees along Eastwood Road in McCormick Ranch, just to the east of Scottsdale Road and east of the Camelback Golf Club. No injuries were reported.", "ts_dict_index": [11754, 11755, 11756]}
+{"event_id": 931630, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-01-25 13:40:00", "end_date_time": "2021-01-25 13:40:00", "narrative": "A strong winter storm and its associated cold front rolled through the central Arizona deserts on January 25th, leading to widespread wind damage across much of the greater Phoenix metropolitan area. A line of strong to severe thunderstorms associated with the front generated wind gusts in excess of 60 mph in some locations and the gusty severe winds downed numerous trees, caused damage to roofs and fencing, and in southwest Mesa managed to blow a rooftop air conditioner off of the roof. More than 30,000 utility customers across the Valley lost power at the height of the storm as numerous power poles were snapped or blown over. Several Phoenix area outdoor COVID-19 vaccination sites saw some minor damage to the tents and overall setup from the strong winds, which led to some delays. Rain cooled air associated with the strong storms lowered afternoon temperatures at Phoenix Sky Harbor airport from around 50 degrees to 36 degrees in 25 minutes. Many areas saw pea-sized hail as the storms moved through the Valley. There were no reports of injuries associated with the damaging winds. A cold front associated with a strong winter storm moved through the central and western portions of the greater Phoenix area during the early afternoon hours on January 25th. A line of strong to severe thunderstorms associated with the front generated some gusty and damaging outflow winds. According to a report from the public (a Facebook follower), at 1340MST gusty winds estimated at nearly 60 mph ripped off roofing shingles from a home located at 83rd Avenue and Camelback Road, about 6 miles southwest of Glendale. No injuries were reported.", "ts_dict_index": [11760, 11761, 11762]}
+{"event_id": 915026, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-08-24 17:55:00", "end_date_time": "2020-08-24 17:55:00", "narrative": "A hot and humid airmass was in place, providing enough energy for scattered thunderstorms to develop across the region. The hardest hit area was in the town of Whitehall, New York which saw repeated rounds of heavy rain and thunderstorms during the afternoon and early evening hours of August 24th. An impressive 4 to 6 inches of rain fell across the far northeast portions of Washington County, resulting in 8 flooded roadways, 21 flooded structures, 1 water rescue, several cars partially submerged and the Whitehall Junior-Senior High School being significantly damaged by the flood waters. The school superintendent estimated that it would cost 16 million dollars to repair the damages from the flood waters. Overall, 40 homes and 13 businesses or non-profit organizations sustained damage totaling 1.5 million dollars. There was also about 1,200 power outages as a result of the storms in Washington County. A Physical Disaster Declaration was declared for Washington County as a result of the storms. There was also one isolated report of trees down in Albany county from a separate storm. Trees were downed onto wires on Gilmore Street and Potter Terrace. Time was estimated by radar.", "ts_dict_index": [11796, 11797, 11798]}
+{"event_id": 915025, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-08-24 17:05:00", "end_date_time": "2020-08-24 17:05:00", "narrative": "A hot and humid airmass was in place, providing enough energy for scattered thunderstorms to develop across the region. The hardest hit area was in the town of Whitehall, New York which saw repeated rounds of heavy rain and thunderstorms during the afternoon and early evening hours of August 24th. An impressive 4 to 6 inches of rain fell across the far northeast portions of Washington County, resulting in 8 flooded roadways, 21 flooded structures, 1 water rescue, several cars partially submerged and the Whitehall Junior-Senior High School being significantly damaged by the flood waters. The school superintendent estimated that it would cost 16 million dollars to repair the damages from the flood waters. Overall, 40 homes and 13 businesses or non-profit organizations sustained damage totaling 1.5 million dollars. There was also about 1,200 power outages as a result of the storms in Washington County. A Physical Disaster Declaration was declared for Washington County as a result of the storms. There was also one isolated report of trees down in Albany county from a separate storm. A tree was downed on Route 4 and Route 21. Time was estimated by radar.", "ts_dict_index": [11787, 11788, 11789]}
+{"event_id": 915019, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-08-24 15:45:00", "end_date_time": "2020-08-24 15:45:00", "narrative": "A hot and humid airmass was in place, providing enough energy for scattered thunderstorms to develop across the region. The hardest hit area was in the town of Whitehall, New York which saw repeated rounds of heavy rain and thunderstorms during the afternoon and early evening hours of August 24th. An impressive 4 to 6 inches of rain fell across the far northeast portions of Washington County, resulting in 8 flooded roadways, 21 flooded structures, 1 water rescue, several cars partially submerged and the Whitehall Junior-Senior High School being significantly damaged by the flood waters. The school superintendent estimated that it would cost 16 million dollars to repair the damages from the flood waters. Overall, 40 homes and 13 businesses or non-profit organizations sustained damage totaling 1.5 million dollars. There was also about 1,200 power outages as a result of the storms in Washington County. A Physical Disaster Declaration was declared for Washington County as a result of the storms. There was also one isolated report of trees down in Albany county from a separate storm. A tree was downed onto wires along County Route 7 and Blue Goose Road. Time was estimated by radar.", "ts_dict_index": [11781, 11782, 11783]}
+{"event_id": 915021, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-08-24 16:00:00", "end_date_time": "2020-08-24 16:00:00", "narrative": "A hot and humid airmass was in place, providing enough energy for scattered thunderstorms to develop across the region. The hardest hit area was in the town of Whitehall, New York which saw repeated rounds of heavy rain and thunderstorms during the afternoon and early evening hours of August 24th. An impressive 4 to 6 inches of rain fell across the far northeast portions of Washington County, resulting in 8 flooded roadways, 21 flooded structures, 1 water rescue, several cars partially submerged and the Whitehall Junior-Senior High School being significantly damaged by the flood waters. The school superintendent estimated that it would cost 16 million dollars to repair the damages from the flood waters. Overall, 40 homes and 13 businesses or non-profit organizations sustained damage totaling 1.5 million dollars. There was also about 1,200 power outages as a result of the storms in Washington County. A Physical Disaster Declaration was declared for Washington County as a result of the storms. There was also one isolated report of trees down in Albany county from a separate storm. Trees were downed on Skenesborough Drive in the front of Skeneborough EMS Building.", "ts_dict_index": [11790, 11791, 11792]}
+{"event_id": 915022, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-08-24 16:02:00", "end_date_time": "2020-08-24 16:02:00", "narrative": "A hot and humid airmass was in place, providing enough energy for scattered thunderstorms to develop across the region. The hardest hit area was in the town of Whitehall, New York which saw repeated rounds of heavy rain and thunderstorms during the afternoon and early evening hours of August 24th. An impressive 4 to 6 inches of rain fell across the far northeast portions of Washington County, resulting in 8 flooded roadways, 21 flooded structures, 1 water rescue, several cars partially submerged and the Whitehall Junior-Senior High School being significantly damaged by the flood waters. The school superintendent estimated that it would cost 16 million dollars to repair the damages from the flood waters. Overall, 40 homes and 13 businesses or non-profit organizations sustained damage totaling 1.5 million dollars. There was also about 1,200 power outages as a result of the storms in Washington County. A Physical Disaster Declaration was declared for Washington County as a result of the storms. There was also one isolated report of trees down in Albany county from a separate storm. Trees were downed on wires along Route 12/Upper Turnpike Road. Time was estimated by radar.", "ts_dict_index": [11793, 11794, 11795]}
+{"event_id": 883783, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-05-08 04:46:00", "end_date_time": "2020-05-08 04:46:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. In addition, strong surface winds with gusts up to 50 mph ahead of the complex of showers and thunderstorms also downed several trees given the wet antecedent soil moisture conditions in place from above normal rainfall observed since the start of the year. These storms exited North Louisiana shortly after daybreak on the 8th. Trees were blown down onto Highway 160 near the Claiborne Parish line.", "ts_dict_index": [11805, 11806, 11807]}
+{"event_id": 883781, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-05-08 04:28:00", "end_date_time": "2020-05-08 04:28:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. In addition, strong surface winds with gusts up to 50 mph ahead of the complex of showers and thunderstorms also downed several trees given the wet antecedent soil moisture conditions in place from above normal rainfall observed since the start of the year. These storms exited North Louisiana shortly after daybreak on the 8th. Trees down on and near Highway 157 in Springhill. Trees were also blown down onto several homes in town.", "ts_dict_index": [11808, 11809, 11810]}
+{"event_id": 883789, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-05-08 05:04:00", "end_date_time": "2020-05-08 05:04:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. In addition, strong surface winds with gusts up to 50 mph ahead of the complex of showers and thunderstorms also downed several trees given the wet antecedent soil moisture conditions in place from above normal rainfall observed since the start of the year. These storms exited North Louisiana shortly after daybreak on the 8th. Trees were downed onto Interstate 20 west near Exit 52 (Highway 532), forcing the closure of the interstate.", "ts_dict_index": [11799, 11800, 11801]}
+{"event_id": 883782, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-05-08 04:30:00", "end_date_time": "2020-05-08 04:30:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. In addition, strong surface winds with gusts up to 50 mph ahead of the complex of showers and thunderstorms also downed several trees given the wet antecedent soil moisture conditions in place from above normal rainfall observed since the start of the year. These storms exited North Louisiana shortly after daybreak on the 8th. Numerous trees and power lines down in the Springhill and Evergreen areas.", "ts_dict_index": [11802, 11803, 11804]}
+{"event_id": 1087643, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-03-02 22:26:00", "end_date_time": "2023-03-02 22:26:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing several tornadoes in addition to large hail and damaging wind gusts. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threats of large hail and isolated tornadoes continued through the end of the event. Damage survey concluded that damage on the southeast side of Marshall was consistent with that of straight-line winds near 95 mph with several trees uprooted and/or snapped. Concentrated tree damage was observed in the Bel Air community.", "ts_dict_index": [11703, 11704, 11705]}
+{"event_id": 1047246, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-07-14 07:30:00", "end_date_time": "2022-07-14 07:30:00", "narrative": "A strong and persistent upper-level ridge across the Four Corners Region retrograded slightly westward, allowing an upper-level trough to shift southward from the Plains and Ozarks. The trough helped to drive a weak frontal boundary in the region where ample instability was in place as daytime maximum temperatures averaged between 100-105 degrees on July 13th. Convection began to form by mid to late afternoon with several thunderstorms quickly becoming severe in the very unstable conditions. The high-based thunderstorms presented a primary damaging wind threat, which resulted in numerous damage reports through the afternoon and evening hours on the 13th. Some of the severe thunderstorms also produced hail of various sizes, including a few reports of large hail. These storms continued through the early morning hours of the 14th before diminishing. Additional isolated severe thunderstorms developed during the afternoon of the 14th over Eastern Smith County, producing damaging winds that tore a portion of the roof off of the Chapel Hill High School cafeteria. Widespread downed trees, power lines, and power poles reported throughout the city of Tyler.", "ts_dict_index": [11838, 11839, 11840]}
+{"event_id": 906864, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 16:57:00", "end_date_time": "2020-07-11 16:57:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. Several large tree branches blown down.", "ts_dict_index": [11868, 11869, 11870]}
+{"event_id": 906895, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 16:50:00", "end_date_time": "2020-07-11 16:50:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. A spotter estimated high winds.", "ts_dict_index": [11859, 11860, 11861]}
+{"event_id": 1047248, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-07-14 19:35:00", "end_date_time": "2022-07-14 19:35:00", "narrative": "A strong and persistent upper-level ridge across the Four Corners Region retrograded slightly westward, allowing an upper-level trough to shift southward from the Plains and Ozarks. The trough helped to drive a weak frontal boundary in the region where ample instability was in place as daytime maximum temperatures averaged between 100-105 degrees on July 13th. Convection began to form by mid to late afternoon with several thunderstorms quickly becoming severe in the very unstable conditions. The high-based thunderstorms presented a primary damaging wind threat, which resulted in numerous damage reports through the afternoon and evening hours on the 13th. Some of the severe thunderstorms also produced hail of various sizes, including a few reports of large hail. These storms continued through the early morning hours of the 14th before diminishing. Additional isolated severe thunderstorms developed during the afternoon of the 14th over Eastern Smith County, producing damaging winds that tore a portion of the roof off of the Chapel Hill High School cafeteria. A portion of the roof was blown off of the Chapel Hill High School cafeteria.", "ts_dict_index": [11835, 11836, 11837]}
+{"event_id": 883785, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-05-08 05:00:00", "end_date_time": "2020-05-08 05:00:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. In addition, strong surface winds with gusts up to 50 mph ahead of the complex of showers and thunderstorms also downed several trees given the wet antecedent soil moisture conditions in place from above normal rainfall observed since the start of the year. These storms exited North Louisiana shortly after daybreak on the 8th. A picture was posted to social media of large limbs that were downed in the Shady Grove neighborhood in Bossier City.", "ts_dict_index": [11820, 11821, 11822]}
+{"event_id": 843631, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-09-09 16:05:00", "end_date_time": "2019-09-09 16:05:00", "narrative": "An area of high pressure in the upper levels of the atmosphere was anchored over the Southeast United States during the afternoon of September 9th, which resulted in a deep southerly flow off of the Gulf of Mexico across North Louisiana and East Texas. This enhanced the seabreeze, with scattered showers and thunderstorms spreading north throughout the day into portions of East Texas and North Louisiana. Strong daytime heating, with temperatures climbing into the upper 90s, coupled with a moist and unstable air mass, resulted in isolated pulse severe thunderstorms to develop across portions of North Louisiana and East Texas during the mid and late afternoon hours. These thunderstorms produced brief downbursts that led to sporadic wind damage to trees across portions of Desoto, Bossier, Caldwell, and Ouachita Parishes. A thunderstorm also produced a cloud to ground lightning strike at the Wade Correctional Facility north of Homer, which injured 10 inmates outside, one critically. These storms diminished by late evening with the loss of heating and instability. A tree was blown down onto power lines in the Shady Grove neighborhood of Bossier City just south of Barksdale Air Force Base.", "ts_dict_index": [11826, 11827, 11828]}
+{"event_id": 905061, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-06-10 17:47:00", "end_date_time": "2020-06-10 17:47:00", "narrative": "Warm, moist advection during the morning and early afternoon hours of the 10th led to humid and very warm conditions.  Mean-layer CAPE of around 2000 J/kg, highest over eastern Ohio, illustrated the very unstable conditions.  A few discrete thunderstorm cells were able to form over southwest PA initially, with a few hail and wind damage reports.  However, the bulk of the severe weather was the result of the passage of a negatively-tilted upper trough and a strong cold front, which crossed during the late afternoon and evening hours. Bulk shear of 40 to 50 knots and the cold front allowed for the development of a quasi-linear convective system, resulting in widespread reports of wind damage.  Gusts of 70-80 MPH were estimated in some cases, leading to numerous reports of damage to trees and power lines, as well as mostly minor structural damage to roofing and shingles. Mesovortices in the QLCS also led to the development and confirmation of three tornadoes in the NWS Pittsburgh forecast area. The strongest was in Beaver County PA, with EF1 damage observed. It was reported that multiple trees were uprooted.", "ts_dict_index": [11850, 11851, 11852]}
+{"event_id": 883784, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-05-08 04:50:00", "end_date_time": "2020-05-08 04:50:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. In addition, strong surface winds with gusts up to 50 mph ahead of the complex of showers and thunderstorms also downed several trees given the wet antecedent soil moisture conditions in place from above normal rainfall observed since the start of the year. These storms exited North Louisiana shortly after daybreak on the 8th. Trees and power lines were downed on Wesley Avenue in the North Highland area of Shreveport.", "ts_dict_index": [11811, 11812, 11813]}
+{"event_id": 1047245, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-07-14 07:22:00", "end_date_time": "2022-07-14 07:22:00", "narrative": "A strong and persistent upper-level ridge across the Four Corners Region retrograded slightly westward, allowing an upper-level trough to shift southward from the Plains and Ozarks. The trough helped to drive a weak frontal boundary in the region where ample instability was in place as daytime maximum temperatures averaged between 100-105 degrees on July 13th. Convection began to form by mid to late afternoon with several thunderstorms quickly becoming severe in the very unstable conditions. The high-based thunderstorms presented a primary damaging wind threat, which resulted in numerous damage reports through the afternoon and evening hours on the 13th. Some of the severe thunderstorms also produced hail of various sizes, including a few reports of large hail. These storms continued through the early morning hours of the 14th before diminishing. Additional isolated severe thunderstorms developed during the afternoon of the 14th over Eastern Smith County, producing damaging winds that tore a portion of the roof off of the Chapel Hill High School cafeteria. Numerous trees were downed in the East Lake Woods Subdivision along the eastern shore of Lake Tyler East and a large tree also fell through a mobile home nearby along Highway 64, injuring a female and baby in the home.", "ts_dict_index": [11829, 11830, 11831]}
+{"event_id": 843630, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-09-09 16:12:00", "end_date_time": "2019-09-09 16:12:00", "narrative": "An area of high pressure in the upper levels of the atmosphere was anchored over the Southeast United States during the afternoon of September 9th, which resulted in a deep southerly flow off of the Gulf of Mexico across North Louisiana and East Texas. This enhanced the seabreeze, with scattered showers and thunderstorms spreading north throughout the day into portions of East Texas and North Louisiana. Strong daytime heating, with temperatures climbing into the upper 90s, coupled with a moist and unstable air mass, resulted in isolated pulse severe thunderstorms to develop across portions of North Louisiana and East Texas during the mid and late afternoon hours. These thunderstorms produced brief downbursts that led to sporadic wind damage to trees across portions of Desoto, Bossier, Caldwell, and Ouachita Parishes. A thunderstorm also produced a cloud to ground lightning strike at the Wade Correctional Facility north of Homer, which injured 10 inmates outside, one critically. These storms diminished by late evening with the loss of heating and instability. A tree was downed and a power pole was bent in a neighborhood near the north gate of Barksdale Air Force Base.", "ts_dict_index": [11823, 11824, 11825]}
+{"event_id": 906855, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 09:20:00", "end_date_time": "2020-07-11 09:20:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. Two large metal grain bins downed by thunderstorm winds and blown across a field. A cattle and hay shed was also destroyed.", "ts_dict_index": [11865, 11866, 11867]}
+{"event_id": 905075, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-06-10 21:04:00", "end_date_time": "2020-06-10 21:04:00", "narrative": "Warm, moist advection during the morning and early afternoon hours of the 10th led to humid and very warm conditions.  Mean-layer CAPE of around 2000 J/kg, highest over eastern Ohio, illustrated the very unstable conditions.  A few discrete thunderstorm cells were able to form over southwest PA initially, with a few hail and wind damage reports.  However, the bulk of the severe weather was the result of the passage of a negatively-tilted upper trough and a strong cold front, which crossed during the late afternoon and evening hours. Bulk shear of 40 to 50 knots and the cold front allowed for the development of a quasi-linear convective system, resulting in widespread reports of wind damage.  Gusts of 70-80 MPH were estimated in some cases, leading to numerous reports of damage to trees and power lines, as well as mostly minor structural damage to roofing and shingles. Mesovortices in the QLCS also led to the development and confirmation of three tornadoes in the NWS Pittsburgh forecast area. The strongest was in Beaver County PA, with EF1 damage observed. Several instances of downed trees and power lines were reported.", "ts_dict_index": [11844, 11845, 11846]}
+{"event_id": 905063, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-06-10 17:49:00", "end_date_time": "2020-06-10 17:49:00", "narrative": "Warm, moist advection during the morning and early afternoon hours of the 10th led to humid and very warm conditions.  Mean-layer CAPE of around 2000 J/kg, highest over eastern Ohio, illustrated the very unstable conditions.  A few discrete thunderstorm cells were able to form over southwest PA initially, with a few hail and wind damage reports.  However, the bulk of the severe weather was the result of the passage of a negatively-tilted upper trough and a strong cold front, which crossed during the late afternoon and evening hours. Bulk shear of 40 to 50 knots and the cold front allowed for the development of a quasi-linear convective system, resulting in widespread reports of wind damage.  Gusts of 70-80 MPH were estimated in some cases, leading to numerous reports of damage to trees and power lines, as well as mostly minor structural damage to roofing and shingles. Mesovortices in the QLCS also led to the development and confirmation of three tornadoes in the NWS Pittsburgh forecast area. The strongest was in Beaver County PA, with EF1 damage observed. Numerous trees were blown down in the area around Osceola Drive.", "ts_dict_index": [11841, 11842, 11843]}
+{"event_id": 905062, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-06-10 17:48:00", "end_date_time": "2020-06-10 17:48:00", "narrative": "Warm, moist advection during the morning and early afternoon hours of the 10th led to humid and very warm conditions.  Mean-layer CAPE of around 2000 J/kg, highest over eastern Ohio, illustrated the very unstable conditions.  A few discrete thunderstorm cells were able to form over southwest PA initially, with a few hail and wind damage reports.  However, the bulk of the severe weather was the result of the passage of a negatively-tilted upper trough and a strong cold front, which crossed during the late afternoon and evening hours. Bulk shear of 40 to 50 knots and the cold front allowed for the development of a quasi-linear convective system, resulting in widespread reports of wind damage.  Gusts of 70-80 MPH were estimated in some cases, leading to numerous reports of damage to trees and power lines, as well as mostly minor structural damage to roofing and shingles. Mesovortices in the QLCS also led to the development and confirmation of three tornadoes in the NWS Pittsburgh forecast area. The strongest was in Beaver County PA, with EF1 damage observed. Several trees were reported to be blown down on Butler's Golf Course.", "ts_dict_index": [11853, 11854, 11855]}
+{"event_id": 906857, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 09:34:00", "end_date_time": "2020-07-11 09:34:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. A large tree branch blown down along with crop damage.", "ts_dict_index": [11856, 11857, 11858]}
+{"event_id": 906869, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 17:04:00", "end_date_time": "2020-07-11 17:04:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. A tree was blown over.", "ts_dict_index": [11862, 11863, 11864]}
+{"event_id": 883787, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-05-08 05:00:00", "end_date_time": "2020-05-08 05:00:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. In addition, strong surface winds with gusts up to 50 mph ahead of the complex of showers and thunderstorms also downed several trees given the wet antecedent soil moisture conditions in place from above normal rainfall observed since the start of the year. These storms exited North Louisiana shortly after daybreak on the 8th. Multiple trees were downed in the city of Minden.", "ts_dict_index": [11817, 11818, 11819]}
+{"event_id": 883788, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-05-08 05:01:00", "end_date_time": "2020-05-08 05:01:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. In addition, strong surface winds with gusts up to 50 mph ahead of the complex of showers and thunderstorms also downed several trees given the wet antecedent soil moisture conditions in place from above normal rainfall observed since the start of the year. These storms exited North Louisiana shortly after daybreak on the 8th. Trees were blown down onto Highway 79 northeast of Minden.", "ts_dict_index": [11814, 11815, 11816]}
+{"event_id": 915020, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-08-24 15:50:00", "end_date_time": "2020-08-24 15:50:00", "narrative": "A hot and humid airmass was in place, providing enough energy for scattered thunderstorms to develop across the region. The hardest hit area was in the town of Whitehall, New York which saw repeated rounds of heavy rain and thunderstorms during the afternoon and early evening hours of August 24th. An impressive 4 to 6 inches of rain fell across the far northeast portions of Washington County, resulting in 8 flooded roadways, 21 flooded structures, 1 water rescue, several cars partially submerged and the Whitehall Junior-Senior High School being significantly damaged by the flood waters. The school superintendent estimated that it would cost 16 million dollars to repair the damages from the flood waters. Overall, 40 homes and 13 businesses or non-profit organizations sustained damage totaling 1.5 million dollars. There was also about 1,200 power outages as a result of the storms in Washington County. A Physical Disaster Declaration was declared for Washington County as a result of the storms. There was also one isolated report of trees down in Albany county from a separate storm. Trees were downed on several roads, including Bellamy, North, West, Saunders and Kirtland Streets and on Railroad Avenue. Tree was downed onto a vehicle on Kirtland. Time was estimated by radar.", "ts_dict_index": [11784, 11785, 11786]}
+{"event_id": 906856, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 09:25:00", "end_date_time": "2020-07-11 09:25:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. A tree was blown down onto a house.", "ts_dict_index": [11871, 11872, 11873]}
+{"event_id": 906871, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 17:11:00", "end_date_time": "2020-07-11 17:11:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. A four inch diameter tree branch blown down.", "ts_dict_index": [11880, 11881, 11882]}
+{"event_id": 906867, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 17:00:00", "end_date_time": "2020-07-11 17:00:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. A large tree was blown down, falling through a garage.", "ts_dict_index": [11874, 11875, 11876]}
+{"event_id": 1047247, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2022-07-14 07:39:00", "end_date_time": "2022-07-14 07:39:00", "narrative": "A strong and persistent upper-level ridge across the Four Corners Region retrograded slightly westward, allowing an upper-level trough to shift southward from the Plains and Ozarks. The trough helped to drive a weak frontal boundary in the region where ample instability was in place as daytime maximum temperatures averaged between 100-105 degrees on July 13th. Convection began to form by mid to late afternoon with several thunderstorms quickly becoming severe in the very unstable conditions. The high-based thunderstorms presented a primary damaging wind threat, which resulted in numerous damage reports through the afternoon and evening hours on the 13th. Some of the severe thunderstorms also produced hail of various sizes, including a few reports of large hail. These storms continued through the early morning hours of the 14th before diminishing. Additional isolated severe thunderstorms developed during the afternoon of the 14th over Eastern Smith County, producing damaging winds that tore a portion of the roof off of the Chapel Hill High School cafeteria. Tree limbs down and power reported out east of Whitehouse.", "ts_dict_index": [11832, 11833, 11834]}
+{"event_id": 987078, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-11-11 01:23:00", "end_date_time": "2021-11-11 01:23:00", "narrative": "A longwave trough dug into the Southern Plains from the Central and Southern Rockies during the evening through the early morning hours of November 10th-11th, which reinforced a cold front southeast into these areas. A strong low level jet ahead of the front and attendant trough allowed for moisture to deepen across much of Texas and Oklahoma, with increased large scale forcing contributing to the development of numerous showers and thunderstorms over these areas during the evening of the 10th, which organized into a squall line as it pushed east of the I-35 corridor into the Four State Region. These storms weakened as they entered the area, but re-intensified over portions of extreme Eastern Texas and Northwest Louisiana during the early morning hours of the 11th, producing several reports of wind damage which downed trees and power lines. This squall line also produced two brief tornadoes over Southern Harrison County Texas and another two brief tornadoes over Northwest Louisiana, before weakening as they moved east into North-Central Louisiana. A fence was blown down and siding to an outbuilding was damaged on Grover Place Drive in the Grover Place subdivision.", "ts_dict_index": [11904, 11905, 11906]}
+{"event_id": 906896, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 16:54:00", "end_date_time": "2020-07-11 16:54:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. A citizen reported estimated high winds.", "ts_dict_index": [11889, 11890, 11891]}
+{"event_id": 987081, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-11-11 01:35:00", "end_date_time": "2021-11-11 01:35:00", "narrative": "A longwave trough dug into the Southern Plains from the Central and Southern Rockies during the evening through the early morning hours of November 10th-11th, which reinforced a cold front southeast into these areas. A strong low level jet ahead of the front and attendant trough allowed for moisture to deepen across much of Texas and Oklahoma, with increased large scale forcing contributing to the development of numerous showers and thunderstorms over these areas during the evening of the 10th, which organized into a squall line as it pushed east of the I-35 corridor into the Four State Region. These storms weakened as they entered the area, but re-intensified over portions of extreme Eastern Texas and Northwest Louisiana during the early morning hours of the 11th, producing several reports of wind damage which downed trees and power lines. This squall line also produced two brief tornadoes over Southern Harrison County Texas and another two brief tornadoes over Northwest Louisiana, before weakening as they moved east into North-Central Louisiana. A large tree was blown down across Highway 527 near Sunset Villa Drive.", "ts_dict_index": [11910, 11911, 11912]}
+{"event_id": 987074, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-11-11 01:14:00", "end_date_time": "2021-11-11 01:14:00", "narrative": "A longwave trough dug into the Southern Plains from the Central and Southern Rockies during the evening through the early morning hours of November 10th-11th, which reinforced a cold front southeast into these areas. A strong low level jet ahead of the front and attendant trough allowed for moisture to deepen across much of Texas and Oklahoma, with increased large scale forcing contributing to the development of numerous showers and thunderstorms over these areas during the evening of the 10th, which organized into a squall line as it pushed east of the I-35 corridor into the Four State Region. These storms weakened as they entered the area, but re-intensified over portions of extreme Eastern Texas and Northwest Louisiana during the early morning hours of the 11th, producing several reports of wind damage which downed trees and power lines. This squall line also produced two brief tornadoes over Southern Harrison County Texas and another two brief tornadoes over Northwest Louisiana, before weakening as they moved east into North-Central Louisiana. Large tree limbs were downed near the intersection of Dean Road and Bert Kouns Industrial Loop.", "ts_dict_index": [11895, 11896, 11897]}
+{"event_id": 987075, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-11-11 01:15:00", "end_date_time": "2021-11-11 01:15:00", "narrative": "A longwave trough dug into the Southern Plains from the Central and Southern Rockies during the evening through the early morning hours of November 10th-11th, which reinforced a cold front southeast into these areas. A strong low level jet ahead of the front and attendant trough allowed for moisture to deepen across much of Texas and Oklahoma, with increased large scale forcing contributing to the development of numerous showers and thunderstorms over these areas during the evening of the 10th, which organized into a squall line as it pushed east of the I-35 corridor into the Four State Region. These storms weakened as they entered the area, but re-intensified over portions of extreme Eastern Texas and Northwest Louisiana during the early morning hours of the 11th, producing several reports of wind damage which downed trees and power lines. This squall line also produced two brief tornadoes over Southern Harrison County Texas and another two brief tornadoes over Northwest Louisiana, before weakening as they moved east into North-Central Louisiana. A large tree was downed onto Walker Road blocking the southbound lanes just south of Bert Kouns Industrial Loop.", "ts_dict_index": [11901, 11902, 11903]}
+{"event_id": 987076, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-11-11 01:23:00", "end_date_time": "2021-11-11 01:23:00", "narrative": "A longwave trough dug into the Southern Plains from the Central and Southern Rockies during the evening through the early morning hours of November 10th-11th, which reinforced a cold front southeast into these areas. A strong low level jet ahead of the front and attendant trough allowed for moisture to deepen across much of Texas and Oklahoma, with increased large scale forcing contributing to the development of numerous showers and thunderstorms over these areas during the evening of the 10th, which organized into a squall line as it pushed east of the I-35 corridor into the Four State Region. These storms weakened as they entered the area, but re-intensified over portions of extreme Eastern Texas and Northwest Louisiana during the early morning hours of the 11th, producing several reports of wind damage which downed trees and power lines. This squall line also produced two brief tornadoes over Southern Harrison County Texas and another two brief tornadoes over Northwest Louisiana, before weakening as they moved east into North-Central Louisiana. Large tree limbs were downed in the Pepper Tree subdivision in Southeast Shreveport.", "ts_dict_index": [11907, 11908, 11909]}
+{"event_id": 906859, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 09:35:00", "end_date_time": "2020-07-11 09:35:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. A large tree branch was reported blown down on Prairie Chapel Road, north of Wittier.", "ts_dict_index": [11892, 11893, 11894]}
+{"event_id": 987071, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-11-11 01:05:00", "end_date_time": "2021-11-11 01:05:00", "narrative": "A longwave trough dug into the Southern Plains from the Central and Southern Rockies during the evening through the early morning hours of November 10th-11th, which reinforced a cold front southeast into these areas. A strong low level jet ahead of the front and attendant trough allowed for moisture to deepen across much of Texas and Oklahoma, with increased large scale forcing contributing to the development of numerous showers and thunderstorms over these areas during the evening of the 10th, which organized into a squall line as it pushed east of the I-35 corridor into the Four State Region. These storms weakened as they entered the area, but re-intensified over portions of extreme Eastern Texas and Northwest Louisiana during the early morning hours of the 11th, producing several reports of wind damage which downed trees and power lines. This squall line also produced two brief tornadoes over Southern Harrison County Texas and another two brief tornadoes over Northwest Louisiana, before weakening as they moved east into North-Central Louisiana. Trees were blown down at the 6500 block of North Lakeshore Drive.", "ts_dict_index": [11898, 11899, 11900]}
+{"event_id": 906862, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 16:30:00", "end_date_time": "2020-07-11 16:30:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. Several large trees were split or downed, and large limbs snapped.", "ts_dict_index": [11883, 11884, 11885]}
+{"event_id": 906865, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 16:57:00", "end_date_time": "2020-07-11 16:57:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. A metal shed was blown across 29th Ave in Marion.", "ts_dict_index": [11886, 11887, 11888]}
+{"event_id": 905070, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-06-10 20:50:00", "end_date_time": "2020-06-10 20:50:00", "narrative": "Warm, moist advection during the morning and early afternoon hours of the 10th led to humid and very warm conditions.  Mean-layer CAPE of around 2000 J/kg, highest over eastern Ohio, illustrated the very unstable conditions.  A few discrete thunderstorm cells were able to form over southwest PA initially, with a few hail and wind damage reports.  However, the bulk of the severe weather was the result of the passage of a negatively-tilted upper trough and a strong cold front, which crossed during the late afternoon and evening hours. Bulk shear of 40 to 50 knots and the cold front allowed for the development of a quasi-linear convective system, resulting in widespread reports of wind damage.  Gusts of 70-80 MPH were estimated in some cases, leading to numerous reports of damage to trees and power lines, as well as mostly minor structural damage to roofing and shingles. Mesovortices in the QLCS also led to the development and confirmation of three tornadoes in the NWS Pittsburgh forecast area. The strongest was in Beaver County PA, with EF1 damage observed. Five large trees were uprooted.", "ts_dict_index": [11847, 11848, 11849]}
+{"event_id": 987073, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-11-11 01:03:00", "end_date_time": "2021-11-11 01:03:00", "narrative": "A longwave trough dug into the Southern Plains from the Central and Southern Rockies during the evening through the early morning hours of November 10th-11th, which reinforced a cold front southeast into these areas. A strong low level jet ahead of the front and attendant trough allowed for moisture to deepen across much of Texas and Oklahoma, with increased large scale forcing contributing to the development of numerous showers and thunderstorms over these areas during the evening of the 10th, which organized into a squall line as it pushed east of the I-35 corridor into the Four State Region. These storms weakened as they entered the area, but re-intensified over portions of extreme Eastern Texas and Northwest Louisiana during the early morning hours of the 11th, producing several reports of wind damage which downed trees and power lines. This squall line also produced two brief tornadoes over Southern Harrison County Texas and another two brief tornadoes over Northwest Louisiana, before weakening as they moved east into North-Central Louisiana. Trees were blown down near the Beavers Nest subdivision along Highway 169 between Buncombe Road and Providence Road.", "ts_dict_index": [11919, 11920, 11921]}
+{"event_id": 987072, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-11-11 01:00:00", "end_date_time": "2021-11-11 01:00:00", "narrative": "A longwave trough dug into the Southern Plains from the Central and Southern Rockies during the evening through the early morning hours of November 10th-11th, which reinforced a cold front southeast into these areas. A strong low level jet ahead of the front and attendant trough allowed for moisture to deepen across much of Texas and Oklahoma, with increased large scale forcing contributing to the development of numerous showers and thunderstorms over these areas during the evening of the 10th, which organized into a squall line as it pushed east of the I-35 corridor into the Four State Region. These storms weakened as they entered the area, but re-intensified over portions of extreme Eastern Texas and Northwest Louisiana during the early morning hours of the 11th, producing several reports of wind damage which downed trees and power lines. This squall line also produced two brief tornadoes over Southern Harrison County Texas and another two brief tornadoes over Northwest Louisiana, before weakening as they moved east into North-Central Louisiana. A large tree was blown down across Highway 157 near the intersection of Redland Road.", "ts_dict_index": [11916, 11917, 11918]}
+{"event_id": 906868, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-11 17:00:00", "end_date_time": "2020-07-11 17:00:00", "narrative": "Severe thunderstorms developed across eastern Iowa and northwest Illinois Saturday, July 11, producing widespread wind damage and very large hail. The first line of storms came through during the morning, producing damaging wind gusts and reports of quarter to ping pong ball size hail from Independence to Tipton Iowa. A wind gust of 65 MPH was measured just west of Independence. The second round of thunderstorms developed as a result of an upper level disturbance interacting with an atmosphere characterized by extremely high instability with modest vertical wind shear. Activity initially formed in north central Iowa, producing golf ball to two inch hail from Fort Dodge to Waterloo Iowa. Eventually, storms made their way towards the Cedar Rapids/Iowa City metro areas, producing widespread wind damage and hail up to baseball size. These storms continued through the Quad Cities metro east towards Princeton, Sterling, and Hennepin Illinois, producing additional reports of wind damage and winds of 70 to 90 mph. Numerous power outages were also reported. A two foot diameter tree was blown down.", "ts_dict_index": [11877, 11878, 11879]}
+{"event_id": 927912, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-11-25 02:01:00", "end_date_time": "2020-11-25 02:01:00", "narrative": "A vigorous upper level shortwave trough shifting northeast across Oklahoma into the Ozarks during the evening through the early morning hours of November 24th-25th, drove a surface frontal system through the Southern Plains. Large scale forcing ahead of the trough and cold front produced a line of strong thunderstorms that moved east through the Four State Region during the evening and overnight hours. Strong instability and forcing resulted in these storms exploding vigorously to the west over North Texas early in the evening, producing some severe wind gusts even as the storms moved into portions of East-central Texas. These storms gradually weakened as they pushed through the remainder of East Texas, but strengthened as they moved into Northwest Louisiana (including Shreveport) after 2 am, where 60 mph winds were measured and downed trees and power lines across portions of Caddo, Bossier, Webster, and Bienville Parishes. These storms weakened further just before daybreak on the 25th as they moved across Northcentral Louisiana. A 60 mph wind gust was measured at the Shreveport Regional Airport.", "ts_dict_index": [11943, 11944, 11945]}
+{"event_id": 927922, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-11-25 02:06:00", "end_date_time": "2020-11-25 02:06:00", "narrative": "A vigorous upper level shortwave trough shifting northeast across Oklahoma into the Ozarks during the evening through the early morning hours of November 24th-25th, drove a surface frontal system through the Southern Plains. Large scale forcing ahead of the trough and cold front produced a line of strong thunderstorms that moved east through the Four State Region during the evening and overnight hours. Strong instability and forcing resulted in these storms exploding vigorously to the west over North Texas early in the evening, producing some severe wind gusts even as the storms moved into portions of East-central Texas. These storms gradually weakened as they pushed through the remainder of East Texas, but strengthened as they moved into Northwest Louisiana (including Shreveport) after 2 am, where 60 mph winds were measured and downed trees and power lines across portions of Caddo, Bossier, Webster, and Bienville Parishes. These storms weakened further just before daybreak on the 25th as they moved across Northcentral Louisiana. A tree was blown down on West 84th Street near David Street.", "ts_dict_index": [11955, 11956, 11957]}
+{"event_id": 887338, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-05-26 20:03:00", "end_date_time": "2020-05-26 20:03:00", "narrative": "A slow moving upper low pressure system over Southern Oklahoma and Northeast Texas drifted east along the Red River Valley during the afternoon and evening hours of May 26th. This system contributed to a decayed complex of showers and thunderstorms that moved through portions of East Texas and North Louisiana during the morning hours, thus stabilizing the air mass through much of the day. However, diurnal heating did contribute to the development of some instability during the late afternoon through the evening hours from Southeast Texas north into portions of East Texas and Northwest Louisiana, as another spoke of upper level energy rotated north-northeast around the center of the upper level low pressure area. This resulted in scattered shower and thunderstorm development by late afternoon through much of the evening hours, with some of these storms becoming severe, resulting in several reports of large hail and isolated damaging winds. These storms persisted into the early morning hours of May 27th, but weakened given the loss of instability. Numerous trees and power lines were downed in Benton.", "ts_dict_index": [11922, 11923, 11924]}
+{"event_id": 927913, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2020-11-25 02:15:00", "end_date_time": "2020-11-25 02:15:00", "narrative": "A vigorous upper level shortwave trough shifting northeast across Oklahoma into the Ozarks during the evening through the early morning hours of November 24th-25th, drove a surface frontal system through the Southern Plains. Large scale forcing ahead of the trough and cold front produced a line of strong thunderstorms that moved east through the Four State Region during the evening and overnight hours. Strong instability and forcing resulted in these storms exploding vigorously to the west over North Texas early in the evening, producing some severe wind gusts even as the storms moved into portions of East-central Texas. These storms gradually weakened as they pushed through the remainder of East Texas, but strengthened as they moved into Northwest Louisiana (including Shreveport) after 2 am, where 60 mph winds were measured and downed trees and power lines across portions of Caddo, Bossier, Webster, and Bienville Parishes. These storms weakened further just before daybreak on the 25th as they moved across Northcentral Louisiana. A 60 mph wind gust was estimated on Ferry Creek Drive in the Ellerbe Road Estates in Southeast Shreveport. Report from a retired NWS employee.", "ts_dict_index": [11946, 11947, 11948]}
+{"event_id": 927908, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-11-25 00:10:00", "end_date_time": "2020-11-25 00:10:00", "narrative": "A vigorous upper level shortwave trough shifting northeast across Oklahoma into the Ozarks during the evening through the early morning hours of November 24th-25th, drove a surface frontal system through the Southern Plains. Large scale forcing ahead of the trough and cold front produced a line of strong thunderstorms that moved east through the Four State Region during the evening and overnight hours. Strong instability and forcing resulted in these storms exploding vigorously to the west over North Texas early in the evening, producing some severe wind gusts even as the storms moved into portions of East-central Texas, where trees were blown down in Red River, Smith, Cherokee, and Panola Counties. A brief EF-1 tornado was also spawned from these storms in Southern Panola County. These storms gradually weakened as they pushed through the remainder of East Texas into Southwest Arkansas and North Louisiana,  although gusty winds of 40 to 50 mph persisted with the line of thunderstorms before weakening further just before daybreak on the 25th. Trees were blown down on Barber Road.", "ts_dict_index": [11925, 11926, 11927]}
+{"event_id": 927916, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-11-25 02:33:00", "end_date_time": "2020-11-25 02:33:00", "narrative": "A vigorous upper level shortwave trough shifting northeast across Oklahoma into the Ozarks during the evening through the early morning hours of November 24th-25th, drove a surface frontal system through the Southern Plains. Large scale forcing ahead of the trough and cold front produced a line of strong thunderstorms that moved east through the Four State Region during the evening and overnight hours. Strong instability and forcing resulted in these storms exploding vigorously to the west over North Texas early in the evening, producing some severe wind gusts even as the storms moved into portions of East-central Texas. These storms gradually weakened as they pushed through the remainder of East Texas, but strengthened as they moved into Northwest Louisiana (including Shreveport) after 2 am, where 60 mph winds were measured and downed trees and power lines across portions of Caddo, Bossier, Webster, and Bienville Parishes. These storms weakened further just before daybreak on the 25th as they moved across Northcentral Louisiana. A tree was blown down blocking Johnson Road at Camp Bistineau Road near the north side of Lake Bistineau.", "ts_dict_index": [11949, 11950, 11951]}
+{"event_id": 927910, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2020-11-25 01:32:00", "end_date_time": "2020-11-25 01:32:00", "narrative": "A vigorous upper level shortwave trough shifting northeast across Oklahoma into the Ozarks during the evening through the early morning hours of November 24th-25th, drove a surface frontal system through the Southern Plains. Large scale forcing ahead of the trough and cold front produced a line of strong thunderstorms that moved east through the Four State Region during the evening and overnight hours. Strong instability and forcing resulted in these storms exploding vigorously to the west over North Texas early in the evening, producing some severe wind gusts even as the storms moved into portions of East-central Texas, where trees were blown down in Red River, Smith, Cherokee, and Panola Counties. A brief EF-1 tornado was also spawned from these storms in Southern Panola County. These storms gradually weakened as they pushed through the remainder of East Texas into Southwest Arkansas and North Louisiana,  although gusty winds of 40 to 50 mph persisted with the line of thunderstorms before weakening further just before daybreak on the 25th. Large trees were blown down on County Road 193 at Lake Murvaul. Report from a Red Cross official.", "ts_dict_index": [11928, 11929, 11930]}
+{"event_id": 1132125, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 20:34:00", "end_date_time": "2023-08-31 20:34:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Downed powerlines were reported along the area of South 20th street to South 32nd Street and East Elwood street to East Roeser Road in Phoenix. Wind gusts were estimated to be up to 65 mph. No injuries were reported.", "ts_dict_index": [11961, 11962, 11963]}
+{"event_id": 927920, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2020-11-25 02:30:00", "end_date_time": "2020-11-25 02:30:00", "narrative": "A vigorous upper level shortwave trough shifting northeast across Oklahoma into the Ozarks during the evening through the early morning hours of November 24th-25th, drove a surface frontal system through the Southern Plains. Large scale forcing ahead of the trough and cold front produced a line of strong thunderstorms that moved east through the Four State Region during the evening and overnight hours. Strong instability and forcing resulted in these storms exploding vigorously to the west over North Texas early in the evening, producing some severe wind gusts even as the storms moved into portions of East-central Texas. These storms gradually weakened as they pushed through the remainder of East Texas, but strengthened as they moved into Northwest Louisiana (including Shreveport) after 2 am, where 60 mph winds were measured and downed trees and power lines across portions of Caddo, Bossier, Webster, and Bienville Parishes. These storms weakened further just before daybreak on the 25th as they moved across Northcentral Louisiana. An estimated 60 mph wind gust was reported just east of Doyline.", "ts_dict_index": [11952, 11953, 11954]}
+{"event_id": 822527, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-27 06:03:00", "end_date_time": "2019-05-27 06:03:00", "narrative": "A pair of convective complexes, rolled through the state within a roughly 24 to 36 hour period. The first of which was linear in nature and started its life back in central and western Kansas during the evening of the 26th and made its way towards Iowa with the help of SW 500mb flow and a potent 850 mb low level jet. The second system originated across south central and western Nebraska and propagated eastward as a mesoscale convective systems along a relatively sharp MUCAPE gradient.  ||Generally speaking in both cases MUCAPE values were around 500-1500 J/kg, effective bulk shear around 30 to 50 kts, and aided by the low level jet (especially on the morning of the 27th).  Given the progressive nature of the storms, heavy rainfall and flooding was generally not seen, but a few locations were able to see around 2 inches of rainfall over the roughly 24 hour period between the main rounds of storms. The main results of the storms were multiple severe wind gust and wind damage reports, though a couple severe hail reports were also received. Public reported several 3 plus inch tree branches broken across the Beaverdale neighborhood. Over 2000 residents without power. This is a delayed report.", "ts_dict_index": [11931, 11932, 11933]}
+{"event_id": 1119137, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-08-08 23:08:00", "end_date_time": "2023-08-08 23:08:00", "narrative": "A complex of thunderstorm produced a swath of strong to severe wind gusts roughly along and south of Interstate 80 during the late evening hours of August 8th. Widespread thunderstorms developed north to south along the High Plains of western Nebraska and northeast Colorado during the late afternoon hours, then gradually spread eastward at around 30 to 40 MPH during the evening. The complex actually weakened to below severe levels as it moved through the North Platte area around sunset. However, activity reintensified as it moved into the Lexington and Kearney areas with the help of higher instability and an increasing low level jet. Activity was also aided by a potent mesoscale convective vortex, or MCV. Severe thunderstorm warnings continued east-southeast into the Hastings area by around midnight, then weakened shortly thereafter. While a couple wind gusts in the 70s were reported between Elm Creek and Kearney, the vast majority of the observed wind gusts were in the 55-60 MPH range, and reported damage was minimal and/or minor. A wind gust of 60 MPH was measured by a mesonet station located two miles north-northeast of Hastings.", "ts_dict_index": [11937, 11938, 11939]}
+{"event_id": 822526, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-27 05:54:00", "end_date_time": "2019-05-27 05:54:00", "narrative": "A pair of convective complexes, rolled through the state within a roughly 24 to 36 hour period. The first of which was linear in nature and started its life back in central and western Kansas during the evening of the 26th and made its way towards Iowa with the help of SW 500mb flow and a potent 850 mb low level jet. The second system originated across south central and western Nebraska and propagated eastward as a mesoscale convective systems along a relatively sharp MUCAPE gradient.  ||Generally speaking in both cases MUCAPE values were around 500-1500 J/kg, effective bulk shear around 30 to 50 kts, and aided by the low level jet (especially on the morning of the 27th).  Given the progressive nature of the storms, heavy rainfall and flooding was generally not seen, but a few locations were able to see around 2 inches of rainfall over the roughly 24 hour period between the main rounds of storms. The main results of the storms were multiple severe wind gust and wind damage reports, though a couple severe hail reports were also received. NWS employee reported heavy patio furniture blown over/across yard. This is a delayed report.", "ts_dict_index": [11934, 11935, 11936]}
+{"event_id": 994043, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2022-01-09 05:31:00", "end_date_time": "2022-01-09 05:31:00", "narrative": "A strong upper level low pressure system tracked east across the Red River Valley of Southern Oklahoma and North Texas during the afternoon of January 8th, before shifting across Northeast Texas into Southwest Arkansas during the early morning hours of the 9th. Ahead of this low, strong southerly low level winds rapidly transported low level moisture back north across the region, with large scale forcing and elevated instability ahead of the low contributing to areas of showers and embedded thunderstorms over East Texas, North Louisiana, and Southwest Arkansas.  Meanwhile, a warm front had spread north into portions of Deep East Texas and Central Louisiana during the late evening and early morning hours, with increasing instability and low level wind shear fueling the development of strong to severe thunderstorms over these areas. These storms produced damaging winds which downed trees and power lines, and also spawned two tornadoes in Southern Sabine Parish before gradually weakening as they shifted northeast away from the front. A power pole was snapped and power lines were blown down over a road in the Red Dirt community.", "ts_dict_index": [11940, 11941, 11942]}
+{"event_id": 987068, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-11-11 00:57:00", "end_date_time": "2021-11-11 00:57:00", "narrative": "A longwave trough dug into the Southern Plains from the Central and Southern Rockies during the evening through the early morning hours of November 10th-11th, which reinforced a cold front southeast into these areas. A strong low level jet ahead of the front and attendant trough allowed for moisture to deepen across much of Texas and Oklahoma, with increased large scale forcing contributing to the development of numerous showers and thunderstorms over these areas during the evening of the 10th, which organized into a squall line as it pushed east of the I-35 corridor into the Four State Region. These storms weakened as they entered the area, but re-intensified over portions of extreme Eastern Texas and Northwest Louisiana during the early morning hours of the 11th, producing several reports of wind damage which downed trees and power lines. This squall line also produced two brief tornadoes over Southern Harrison County Texas and another two brief tornadoes over Northwest Louisiana, before weakening as they moved east into North-Central Louisiana. Trees and large tree limbs were downed along Highway 169 near Lowry Road.", "ts_dict_index": [11913, 11914, 11915]}
+{"event_id": 1131792, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 20:45:00", "end_date_time": "2023-08-31 20:45:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 59 mph wind gust was measured at a mesonet station located in the area of North Highland Drive and East Lamar Road in Paradise Valley.", "ts_dict_index": [11976, 11977, 11978]}
+{"event_id": 1132526, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:30:00", "end_date_time": "2023-08-31 21:30:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A damaged mobile home awning laid on the road of North 103 Avenue between West Olive Avenue and West Northern Avenue in Glendale. Timing estimated from radar. Wind gusts were estimated at around 60 mph. No injuries were reported.", "ts_dict_index": [11964, 11965, 11966]}
+{"event_id": 1131806, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:55:00", "end_date_time": "2023-08-31 21:55:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 58 mph wind gust was measured at Luke Air Force Base.", "ts_dict_index": [11973, 11974, 11975]}
+{"event_id": 1132144, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:42:00", "end_date_time": "2023-08-31 21:42:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Downed powerlines were reported along the area of Yuma Road to Broadway Road and 231st Avenue to Airport Road in Buckeye. Wind gusts were estimated at around 60 mph. No injuries were reported.", "ts_dict_index": [11967, 11968, 11969]}
+{"event_id": 1132530, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:15:00", "end_date_time": "2023-08-31 21:15:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Massive 2-4 foot diameter tree fell across a few cars in the area of North 75th Avenue and West Indian School Road in Glendale. Wind gusts were estimated at around 60 mph. No injuries were reported.", "ts_dict_index": [11970, 11971, 11972]}
+{"event_id": 1095480, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 15:52:00", "end_date_time": "2023-06-03 15:52:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Power lines downed on Walker Road between Green Terrace Road and Bert Kouns Industrial Loop.", "ts_dict_index": [12048, 12049, 12050]}
+{"event_id": 1131793, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 20:48:00", "end_date_time": "2023-08-31 20:48:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A couple of mesquite trees, estimated at 8-10 diameter, were blown over in the area of E Jefferson Street between 10th and 11th street in downtown Phoenix. Wind gusts were estimated to be up to 65 mph. No injuries were reported.", "ts_dict_index": [11982, 11983, 11984]}
+{"event_id": 1131803, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:53:00", "end_date_time": "2023-08-31 21:53:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 62 mph wind gust was measured at Phoenix Deer Valley Airport.", "ts_dict_index": [11991, 11992, 11993]}
+{"event_id": 1132534, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-08-31 20:15:00", "end_date_time": "2023-08-31 20:15:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Photos showing several large uprooted trees in the city of Maricopa. Wind gusts were estimated of up to 60 mph. No injuries were reported.", "ts_dict_index": [12003, 12004, 12005]}
+{"event_id": 1100163, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-05-11 09:13:00", "end_date_time": "2023-05-11 09:13:00", "narrative": "An upper level low pressure system slowly ejected northeast across the piney woods of East Texas during the evening through the morning hours of May 10th-11th. A southerly low level jet present ahead of the low spilled copious amounts of low level moisture north into East Texas and Western Louisiana, with strong large scale forcing ahead of the low enhancing numerous shower and thunderstorm development which moved repeatedly over these areas throughout much of the overnight into the early morning hours. Widespread rainfall amounts of 2-4+ inches fell across much of North Louisiana during the morning through the early afternoon hours on the 11th, resulting in instances of flash flooding across this area. Given the strong low level wind shear out ahead of the low, as well as increased instability especially with the onset of daytime heating, severe thunderstorms containing damaging winds, while also spawning a few isolated tornadoes, were observed throughout the morning as well before eventually diminishing during the afternoon. A tree was downed near Creston.", "ts_dict_index": [12045, 12046, 12047]}
+{"event_id": 1132533, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:15:00", "end_date_time": "2023-08-31 21:15:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Photos of large tree branches blocking road in the Glenarm Farms Neighborhood in Avondale. Wind gusts were estimated of up to 60 mph. No injuries were reported.", "ts_dict_index": [12009, 12010, 12011]}
+{"event_id": 1132127, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:00:00", "end_date_time": "2023-08-31 21:00:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Downed powerlines were reported along the area of South Priest Drive to South Hardy Drive and West 1st Street to West University Drive in Tempe. Wind gusts were estimated to be up to 65 mph. No injuries were reported.", "ts_dict_index": [12033, 12034, 12035]}
+{"event_id": 1131800, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:15:00", "end_date_time": "2023-08-31 21:15:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 65 mph wind gust was measured at a mesonet station located at the Phoenix International Raceway in Avondale.", "ts_dict_index": [11979, 11980, 11981]}
+{"event_id": 1131802, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:35:00", "end_date_time": "2023-08-31 21:35:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A large downed 20 year old Mesquite Tree was reported at North Crooked Stick Road in Anthem. The downed tree was blocking the road and sitting on a car. Wind gusts were estimated at around 60 mph. No injuries were reported.", "ts_dict_index": [12039, 12040, 12041]}
+{"event_id": 1131805, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:25:00", "end_date_time": "2023-08-31 21:25:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 58 mph wind gust was measured at a mesonet station located in the area of North 107th Avenue just south of Interstate 10.", "ts_dict_index": [12015, 12016, 12017]}
+{"event_id": 1131779, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-08-31 20:10:00", "end_date_time": "2023-08-31 20:10:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A wind gust of 64 mph was measured at the Ak-Chin Regional Airport.", "ts_dict_index": [11985, 11986, 11987]}
+{"event_id": 1131797, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 20:54:00", "end_date_time": "2023-08-31 20:54:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 73 mph wind gust was measured at Phoenix Sky Harbor Airport.", "ts_dict_index": [12030, 12031, 12032]}
+{"event_id": 1131778, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-08-31 19:50:00", "end_date_time": "2023-08-31 19:50:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 58 mph wind gust was measured at a mesonet station located just northwest of Casa Grande.", "ts_dict_index": [11994, 11995, 11996]}
+{"event_id": 1131798, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:05:00", "end_date_time": "2023-08-31 21:05:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 59 mph wind gust was measured at a mesonet station located along the area of South 43rd Avenue and West Lower Buckeye Road in Phoenix.", "ts_dict_index": [12021, 12022, 12023]}
+{"event_id": 1131804, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:25:00", "end_date_time": "2023-08-31 21:25:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 58 mph wind gust was measured at a mesonet station located along West Britton Avenue in Glendale.", "ts_dict_index": [12027, 12028, 12029]}
+{"event_id": 1132130, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:09:00", "end_date_time": "2023-08-31 21:09:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Downed powerlines were reported along the area of McKinley St to Pima St and 31st Ave to 23rd Ave in Phoenix. Wind gusts were estimated to be up to 65 mph. No injuries were reported.", "ts_dict_index": [12042, 12043, 12044]}
+{"event_id": 1131782, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-08-31 20:02:00", "end_date_time": "2023-08-31 20:02:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 74 mph wind gust was measured along the area of Sunland Gin Road and Kramer Lane in Arizona City.", "ts_dict_index": [11997, 11998, 11999]}
+{"event_id": 1132532, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:00:00", "end_date_time": "2023-08-31 21:00:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A large uprooted tree in the area of South 35th Avenue and West Vineyard Road in Phoenix. Wind gusts were estimated of up to 65 mph. No injuries were reported.", "ts_dict_index": [12024, 12025, 12026]}
+{"event_id": 1132536, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:00:00", "end_date_time": "2023-08-31 21:00:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Large uprooted tree in the area of North Central Avenue and East Northern Avenue in Phoenix. Wind gusts were estimated of up to 60 mph. No injuries were reported.", "ts_dict_index": [12006, 12007, 12008]}
+{"event_id": 1131801, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:30:00", "end_date_time": "2023-08-31 21:30:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 58 mph wind gust was measured at a mesonet station located in the area of South Avondale Boulevard and West Coldwater Springs Boulevard in Avondale.", "ts_dict_index": [11988, 11989, 11990]}
+{"event_id": 1132531, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:00:00", "end_date_time": "2023-08-31 21:00:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A palm tree fell and landed on top of a car in the area of South 40th street and East Van Buren Street. Wind gusts were estimated of up to 70 mph. No injuries were reported.", "ts_dict_index": [12012, 12013, 12014]}
+{"event_id": 1131794, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 20:48:00", "end_date_time": "2023-08-31 20:48:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 65 mph wind gust was measured from a mesonet station located along the area of South 16th street and East Roeser Road in Phoenix.", "ts_dict_index": [12000, 12001, 12002]}
+{"event_id": 1132132, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:16:00", "end_date_time": "2023-08-31 21:16:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Downed powerlines were reported along the area of Auto Drive to Western Avenue and Litchfield Road to 5th Street in Goodyear. Wind gusts were estimated at around 60 mph. No injuries were reported.", "ts_dict_index": [11958, 11959, 11960]}
+{"event_id": 1103904, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 15:54:00", "end_date_time": "2023-06-03 15:54:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. A 58 mph wind gust was measured at the Shreveport Regional Airport.", "ts_dict_index": [12051, 12052, 12053]}
+{"event_id": 1095479, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 15:50:00", "end_date_time": "2023-06-03 15:50:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Power lines downed near Avalon Drive and Mackey Lane in southwest Shreveport.", "ts_dict_index": [12066, 12067, 12068]}
+{"event_id": 1095482, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 15:42:00", "end_date_time": "2023-06-03 15:42:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Tree downed on Waterwood Drive and Bea Lane in Greenwood.", "ts_dict_index": [12057, 12058, 12059]}
+{"event_id": 1095483, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 16:00:00", "end_date_time": "2023-06-03 16:00:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Power lines downed in the vicinity of Fairfield Avenue, Ockley Drive, and Avery Street in Shreveport.", "ts_dict_index": [12060, 12061, 12062]}
+{"event_id": 1095478, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 15:29:00", "end_date_time": "2023-06-03 15:29:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Several trees and power lines downed in vicinity of the Calumet refinery in Shreveport.", "ts_dict_index": [12063, 12064, 12065]}
+{"event_id": 1132126, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-08-31 21:09:00", "end_date_time": "2023-08-31 21:09:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. Downed powerlines were reported along the area of North 59th Avenue to North 51st Avenue and West Bethany Home Road to West Missouri Avenue in Glendale. Wind gusts were estimated to be at approximately 60 mph. No injuries were reported.", "ts_dict_index": [12036, 12037, 12038]}
+{"event_id": 1095484, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 16:10:00", "end_date_time": "2023-06-03 16:10:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Power lines downed in the vicinity of Georgia Street and Dee Street in Shreveport.", "ts_dict_index": [12075, 12076, 12077]}
+{"event_id": 1017057, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2022-05-23 22:25:00", "end_date_time": "2022-05-23 22:30:00", "narrative": "A strong 500mb shortwave aided in the development of two thunderstorm complexes that impacted Deep South Texas and the Rio Grande Valley on May 23rd and 24th. The first complex began shortly after 6 PM in Zapata County and inched southeastward across the region before becoming nearly stationary in Cameron and Willacy Counties around 2 AM on the morning of the 24th. This lead to numerous reports of flooding and several reports of damaging wind, especially in central Hidalgo County, where the worst of the damage was reported.||The second complex developed in northern Mexico and entered Zapata County around 4 AM on the morning of May 24th, which helped to spark several showers and storms ahead of it in Starr County. This is when there were several reports of hail. Also, additional flooding occurred in southern Hidalgo and Cameron Counties. By the time all was said and done, much of the Rio Grande Valley had picked up between 2 to 6 inches of rain, with locally higher 5 to 9 inches in parts of Zapata and Starr Counties. The metal roof of the Segovia State Prison Unit was peeled back. A large metal shipping container next to the Lopez State Prison Unit was rolled several times due to the wind. Several trees with large branches were broken. A large tree was uprooted in front of the Lopez State Prison Unit.", "ts_dict_index": [12102, 12103, 12104]}
+{"event_id": 1095487, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 16:11:00", "end_date_time": "2023-06-03 16:11:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Power lines downed in the vicinity of Fairfield Avenue and E. 76th Street in Shreveport.", "ts_dict_index": [12069, 12070, 12071]}
+{"event_id": 1017059, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2022-05-23 22:00:00", "end_date_time": "2022-05-23 22:00:00", "narrative": "A strong 500mb shortwave aided in the development of two thunderstorm complexes that impacted Deep South Texas and the Rio Grande Valley on May 23rd and 24th. The first complex began shortly after 6 PM in Zapata County and inched southeastward across the region before becoming nearly stationary in Cameron and Willacy Counties around 2 AM on the morning of the 24th. This lead to numerous reports of flooding and several reports of damaging wind, especially in central Hidalgo County, where the worst of the damage was reported.||The second complex developed in northern Mexico and entered Zapata County around 4 AM on the morning of May 24th, which helped to spark several showers and storms ahead of it in Starr County. This is when there were several reports of hail. Also, additional flooding occurred in southern Hidalgo and Cameron Counties. By the time all was said and done, much of the Rio Grande Valley had picked up between 2 to 6 inches of rain, with locally higher 5 to 9 inches in parts of Zapata and Starr Counties. Additional pictures of tree damage was shared by the public near the intersection of Interstate 69C and Davis Road in Hidalgo County.", "ts_dict_index": [12096, 12097, 12098]}
+{"event_id": 1095485, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 16:05:00", "end_date_time": "2023-06-03 16:05:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Power lines downed in the vicinity of Wilkinson Street and Gilbert Drive in Shreveport.", "ts_dict_index": [12078, 12079, 12080]}
+{"event_id": 1017058, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2022-05-23 22:00:00", "end_date_time": "2022-05-23 22:00:00", "narrative": "A strong 500mb shortwave aided in the development of two thunderstorm complexes that impacted Deep South Texas and the Rio Grande Valley on May 23rd and 24th. The first complex began shortly after 6 PM in Zapata County and inched southeastward across the region before becoming nearly stationary in Cameron and Willacy Counties around 2 AM on the morning of the 24th. This lead to numerous reports of flooding and several reports of damaging wind, especially in central Hidalgo County, where the worst of the damage was reported.||The second complex developed in northern Mexico and entered Zapata County around 4 AM on the morning of May 24th, which helped to spark several showers and storms ahead of it in Starr County. This is when there were several reports of hail. Also, additional flooding occurred in southern Hidalgo and Cameron Counties. By the time all was said and done, much of the Rio Grande Valley had picked up between 2 to 6 inches of rain, with locally higher 5 to 9 inches in parts of Zapata and Starr Counties. Power lines and crop damage (light to severe) were reported by the COOP observer in McCook. He also reported pea to nickel sized hail as the storms rolled through.", "ts_dict_index": [12099, 12100, 12101]}
+{"event_id": 1095481, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 16:20:00", "end_date_time": "2023-06-03 16:20:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Tree downed across Gayle Red Bluff Road and Ellerbe Road in far southeast Caddo Parish.", "ts_dict_index": [12072, 12073, 12074]}
+{"event_id": 828824, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-06-19 16:31:00", "end_date_time": "2019-06-19 16:31:00", "narrative": "A complex of severe thunderstorms that tracked across portions of East Texas and Northwest Louisiana during the early morning hours of July 19th left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across portions of McCurtain County Oklahoma. These storms produced damaging winds which downed trees near Wright City and along the McCurtain County Oklahoma/Little River County Arkansas line, and produced large hail that fell in Idabel and near Broken Bow before moving into portions of Northeast Texas and Southwest Arkansas late in the afternoon. A brief, isolated tornado also touched down in the Haworth community. Several trees were blown down on Old State Highway 98 near Wright City.", "ts_dict_index": [12081, 12082, 12083]}
+{"event_id": 828829, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-06-19 17:33:00", "end_date_time": "2019-06-19 17:33:00", "narrative": "A complex of severe thunderstorms that tracked across portions of East Texas and Northwest Louisiana during the early morning hours of July 19th left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across portions of McCurtain County Oklahoma. These storms produced damaging winds which downed trees near Wright City and along the McCurtain County Oklahoma/Little River County Arkansas line, and produced large hail that fell in Idabel and near Broken Bow before moving into portions of Northeast Texas and Southwest Arkansas late in the afternoon. A brief, isolated tornado also touched down in the Haworth community. The same supercell thunderstorm that spawned the brief EF-1 tornado in the community of Haworth developed a potent rear flank downdraft, which produced a large swath of 65-85 mph winds along D2213 Road and adjacent roads just east of the America community in far Southeastern McCurtain County and just into Little River County in far Southwest Arkansas. Hundreds of hardwood and softwood trees were snapped or uprooted, with the overwhelming majority of the trees laid over in a southeasterly direction. The breadth of the severe winds was at least 5 miles wide ending just inside the Arkansas state line.", "ts_dict_index": [12084, 12085, 12086]}
+{"event_id": 1117949, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-08-02 02:27:00", "end_date_time": "2023-08-02 02:27:00", "narrative": "A large complex of thunderstorms brought scattered severe wind gusts to portions of south central Nebraska during the early morning hours of August 2nd. A large thunderstorm complex developed during the late evening hours of August 1st over the High Plains, then rolled east into south central Nebraska between 1-2 AM CDT. This complex was strong, but largely sub-severe as it moved along the Highway 6 corridor from Arapahoe to Holdrege with wind gusts of 40-50 MPH. The leading edge of the complex intensified briefly as it moved into the Hastings area around 3 AM. A few severe wind gusts around 60-65 MPH were reported via mesonet stations, but the strongest wind gust was 75 MPH reported at the Hastings Airport ASOS. However, it appears winds this strong were isolated and/or brief as any damage was limited and not indicative of gusts that strong. Downed small tree limbs and sporadic power outages were the main impacts. The complex weakened significantly as it moved east and northeast of the Tri-Cities between 4-5 AM CDT. A wind gust of 62 MPH was measured by a mesonet station located four miles southwest of Hastings.", "ts_dict_index": [12093, 12094, 12095]}
+{"event_id": 1117952, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-08-02 02:34:00", "end_date_time": "2023-08-02 02:34:00", "narrative": "A large complex of thunderstorms brought scattered severe wind gusts to portions of south central Nebraska during the early morning hours of August 2nd. A large thunderstorm complex developed during the late evening hours of August 1st over the High Plains, then rolled east into south central Nebraska between 1-2 AM CDT. This complex was strong, but largely sub-severe as it moved along the Highway 6 corridor from Arapahoe to Holdrege with wind gusts of 40-50 MPH. The leading edge of the complex intensified briefly as it moved into the Hastings area around 3 AM. A few severe wind gusts around 60-65 MPH were reported via mesonet stations, but the strongest wind gust was 75 MPH reported at the Hastings Airport ASOS. However, it appears winds this strong were isolated and/or brief as any damage was limited and not indicative of gusts that strong. Downed small tree limbs and sporadic power outages were the main impacts. The complex weakened significantly as it moved east and northeast of the Tri-Cities between 4-5 AM CDT. A wind gust of 75 MPH was measured by the Hastings Airport ASOS.", "ts_dict_index": [12087, 12088, 12089]}
+{"event_id": 1117950, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2023-08-02 02:28:00", "end_date_time": "2023-08-02 02:28:00", "narrative": "A large complex of thunderstorms brought scattered severe wind gusts to portions of south central Nebraska during the early morning hours of August 2nd. A large thunderstorm complex developed during the late evening hours of August 1st over the High Plains, then rolled east into south central Nebraska between 1-2 AM CDT. This complex was strong, but largely sub-severe as it moved along the Highway 6 corridor from Arapahoe to Holdrege with wind gusts of 40-50 MPH. The leading edge of the complex intensified briefly as it moved into the Hastings area around 3 AM. A few severe wind gusts around 60-65 MPH were reported via mesonet stations, but the strongest wind gust was 75 MPH reported at the Hastings Airport ASOS. However, it appears winds this strong were isolated and/or brief as any damage was limited and not indicative of gusts that strong. Downed small tree limbs and sporadic power outages were the main impacts. The complex weakened significantly as it moved east and northeast of the Tri-Cities between 4-5 AM CDT. A wind gust of 61 MPH was measured by a mesonet station located two miles north of Hastings.", "ts_dict_index": [12090, 12091, 12092]}
+{"event_id": 1017056, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2022-05-23 22:05:00", "end_date_time": "2022-05-23 22:15:00", "narrative": "A strong 500mb shortwave aided in the development of two thunderstorm complexes that impacted Deep South Texas and the Rio Grande Valley on May 23rd and 24th. The first complex began shortly after 6 PM in Zapata County and inched southeastward across the region before becoming nearly stationary in Cameron and Willacy Counties around 2 AM on the morning of the 24th. This lead to numerous reports of flooding and several reports of damaging wind, especially in central Hidalgo County, where the worst of the damage was reported.||The second complex developed in northern Mexico and entered Zapata County around 4 AM on the morning of May 24th, which helped to spark several showers and storms ahead of it in Starr County. This is when there were several reports of hail. Also, additional flooding occurred in southern Hidalgo and Cameron Counties. By the time all was said and done, much of the Rio Grande Valley had picked up between 2 to 6 inches of rain, with locally higher 5 to 9 inches in parts of Zapata and Starr Counties. A manufactured home resting on cinder blocks was blown off of the cinder blocks. The metal roof of another manufactured home was completely lifted up and torn off. Another manufactured home was flipped over on its side. Large branches of several trees were broken. Fencing was knocked down next to manufactured home blown off the cinder blocks.  Several other homes in the neighborhood, known locally as a colonia, had minor roof and siding damage.  Two persons were injured at one of the homes, one whose hand was injured by corrugated siding that had blown between two sections of the structure.", "ts_dict_index": [12105, 12106, 12107]}
+{"event_id": 1012856, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2022-03-30 18:38:00", "end_date_time": "2022-03-30 18:38:00", "narrative": "A powerful low pressure system moved northeast from the central Plains into the Great Lakes, bringing a strong cold front through the Mississippi and Tennessee Valleys. Very windy conditions developed during the morning and extended into the early evening hours of the 30th, producing sustained speeds of 25-35 mph and gusts of 45 to 55 mph. These winds knocked down numerous tree limbs and trees, some power lines and some power poles This resulted in power outages in portions of northern Alabama.  Significant roof damage also occurred.||A squall line which originated during the early morning of the 30th over Arkansas reached northwest Alabama around 5-7 PM, and tracked east across the remainder of north Alabama during the evening hours.  The line of thunderstorms also produced sporadic wind damage, the most severe being in western and central Lauderdale County, where a narrow swath of damage included homes being destroyed and a church experiencing heavy damage. Several trees were snapped or toppled in the path. Trees and powerlines were reported down near the Colbert Ferry Boat Ramp.", "ts_dict_index": [12132, 12133, 12134]}
+{"event_id": 949138, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-05-11 14:30:00", "end_date_time": "2021-05-11 14:30:00", "narrative": "A shallow cold front which moved through the Four State Region on May 9th lifted back north as a warm front into portions of Lower East Texas south of Interstate 20 during the afternoon of the 11th, with warm, humid, and unstable air spilling back north into this area ahead of an upper trough that shifted east into the Central and Southern Plains. This trough and associated large scale forcing contributed to a large area of elevated showers and thunderstorms that developed over West Texas during the morning, and spread east into East Texas during the mid and late afternoon. These storms became more surface based as they moved into the warm sector of Lower East Texas, and quickly became severe, producing damaging winds and large hail. However, the storms quickly weakened by late afternoon as they moved back into a more stable air mass near and east of the Sabine River into North Louisiana, but continued to produce widespread moderate to heavy rainfall before exiting the area during the early and mid evening hours. Trees were downed on Highway 135 north of Overton.", "ts_dict_index": [12111, 12112, 12113]}
+{"event_id": 949141, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-05-11 14:45:00", "end_date_time": "2021-05-11 14:45:00", "narrative": "A shallow cold front which moved through the Four State Region on May 9th lifted back north as a warm front into portions of Lower East Texas south of Interstate 20 during the afternoon of the 11th, with warm, humid, and unstable air spilling back north into this area ahead of an upper trough that shifted east into the Central and Southern Plains. This trough and associated large scale forcing contributed to a large area of elevated showers and thunderstorms that developed over West Texas during the morning, and spread east into East Texas during the mid and late afternoon. These storms became more surface based as they moved into the warm sector of Lower East Texas, and quickly became severe, producing damaging winds and large hail. However, the storms quickly weakened by late afternoon as they moved back into a more stable air mass near and east of the Sabine River into North Louisiana, but continued to produce widespread moderate to heavy rainfall before exiting the area during the early and mid evening hours. A very large tree was blown down on County Road 102 about one-half mile west of Highway 259.", "ts_dict_index": [12108, 12109, 12110]}
+{"event_id": 823316, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-05-18 18:10:00", "end_date_time": "2019-05-18 18:10:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas. An isolated tornado also touched down just southeast of Tyler with one supercell thunderstorm. These storms began to move repeatedly over the same areas during the evening, with instances of flash flooding reported as well. These storms eventually spread into portions of North Louisiana during the early morning hours of the 19th. Several trees were snapped off near Tatum.", "ts_dict_index": [12114, 12115, 12116]}
+{"event_id": 1089187, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-03-16 21:05:00", "end_date_time": "2023-03-16 21:05:00", "narrative": "A long-lived cluster of supercell thunderstorms advanced across northeast Texas into northwest Louisiana on the evening of March 16th just ahead of an accelerating band of thunderstorms along a cold front. As the evening progressed, the cold front gradually overtook the ongoing supercell cluster with the primary threat of hail transitioning to damaging winds within the expanding QLCS. Initially within the far eastern edge of the warm sector, supercell thunderstorms over Sabine County/Parish in Deep East Texas and far western Louisiana produced large hail. The QLCS continued to evolve along the cold front, with an embedded long-lived supercell over Rusk County Texas later in the evening. The environment favored a continuation of the severe threat downstream, with the greatest threat expected along the QLCS segment and with the embedded supercell. As that portion of the line moved southeastward, the threat for damaging winds persisted with a few additional reports of damage in East Texas and Northwest Louisiana. Tree downed along County Road 311 and County Road 317 south of Henderson.", "ts_dict_index": [12123, 12124, 12125]}
+{"event_id": 823320, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-05-18 19:40:00", "end_date_time": "2019-05-18 19:40:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas. An isolated tornado also touched down just southeast of Tyler with one supercell thunderstorm. These storms began to move repeatedly over the same areas during the evening, with instances of flash flooding reported as well. These storms eventually spread into portions of North Louisiana during the early morning hours of the 19th. Numerous trees were downed blocking multiple roads in the Laneville community.", "ts_dict_index": [12117, 12118, 12119]}
+{"event_id": 1089170, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-03-16 23:10:00", "end_date_time": "2023-03-16 23:10:00", "narrative": "A long-lived cluster of supercell thunderstorms advanced across northeast Texas into northwest Louisiana on the evening of March 16th just ahead of an accelerating band of thunderstorms along a cold front. As the evening progressed, the cold front gradually overtook the ongoing supercell cluster with the primary threat of hail transitioning to damaging winds within the expanding QLCS. Initially within the far eastern edge of the warm sector, supercell thunderstorms over Sabine County/Parish in Deep East Texas and far western Louisiana produced large hail. The QLCS continued to evolve along the cold front, with an embedded long-lived supercell over Rusk County Texas later in the evening. The environment favored a continuation of the severe threat downstream, with the greatest threat expected along the QLCS segment and with the embedded supercell. As that portion of the line moved southeastward, the threat for damaging winds persisted with a few additional reports of damage in East Texas and Northwest Louisiana. Tree damage reported along State Highway 1226 with road blocked near Goldonna.", "ts_dict_index": [12126, 12127, 12128]}
+{"event_id": 823562, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-05-18 18:20:00", "end_date_time": "2019-05-18 18:20:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas. An isolated tornado also touched down just southeast of Tyler with one supercell thunderstorm. These storms began to move repeatedly over the same areas during the evening, with instances of flash flooding reported as well. These storms eventually spread into portions of North Louisiana during the early morning hours of the 19th. A NWS Storm Survey confirmed that damaging straight line winds uprooted approximately five trees along Interstate 20 between exits 610 and 614 and again at the Granger Hall Cemetery along Highway 43 just southwest of Marshall. Large limbs were also snapped off, with all of the damage oriented in a northeast direction.", "ts_dict_index": [12120, 12121, 12122]}
+{"event_id": 1095489, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-03 16:10:00", "end_date_time": "2023-06-03 16:10:00", "narrative": "Thunderstorms began to develop during the afternoon of June 3rd across parts of East and Northeast Texas, extending eastward into portions of Northwest Louisiana. Strong daytime heating and dew points in the middle 60s to lower 70s allowed for modest air mass destabilization, with as much as 1500-2000 J/kg of instability from East Texas into much of neighboring Northwest Louisiana. Deep layer flow was weak, resulting in slow moving storms and very little shear in the background environment. Given this regime, storms generally posed a brief severe risk and remained very pulse in nature, with an increasing threat of flash flooding throughout the afternoon. Numerous local storm reports were documented of large hail, damaging winds, and flash flooding. Unfortunately, one flash flood related fatality was reported when a male driver tried to drive through floodwaters on Hearne Avenue in Shreveport. The truck he was driving in quickly took on water, and while his passenger was able to escape, the driver drowned in the high water. Large tree uprooted in the vicinity of Stratford Avenue and Broadmoor Boulevard near Querbes golf course in Shreveport.", "ts_dict_index": [12054, 12055, 12056]}
+{"event_id": 1012845, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2022-03-30 18:37:00", "end_date_time": "2022-03-30 18:37:00", "narrative": "A powerful low pressure system moved northeast from the central Plains into the Great Lakes, bringing a strong cold front through the Mississippi and Tennessee Valleys. Very windy conditions developed during the morning and extended into the early evening hours of the 30th, producing sustained speeds of 25-35 mph and gusts of 45 to 55 mph. These winds knocked down numerous tree limbs and trees, some power lines and some power poles This resulted in power outages in portions of northern Alabama.  Significant roof damage also occurred.||A squall line which originated during the early morning of the 30th over Arkansas reached northwest Alabama around 5-7 PM, and tracked east across the remainder of north Alabama during the evening hours.  The line of thunderstorms also produced sporadic wind damage, the most severe being in western and central Lauderdale County, where a narrow swath of damage included homes being destroyed and a church experiencing heavy damage. Several trees were snapped or toppled in the path. A tree was reported down at 6220 North Pike Road.", "ts_dict_index": [12138, 12139, 12140]}
+{"event_id": 1012840, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2022-03-30 19:25:00", "end_date_time": "2022-03-30 19:28:00", "narrative": "A powerful low pressure system moved northeast from the central Plains into the Great Lakes, bringing a strong cold front through the Mississippi and Tennessee Valleys. Very windy conditions developed during the morning and extended into the early evening hours of the 30th, producing sustained speeds of 25-35 mph and gusts of 45 to 55 mph. These winds knocked down numerous tree limbs and trees, some power lines and some power poles This resulted in power outages in portions of northern Alabama.  Significant roof damage also occurred.||A squall line which originated during the early morning of the 30th over Arkansas reached northwest Alabama around 5-7 PM, and tracked east across the remainder of north Alabama during the evening hours.  The line of thunderstorms also produced sporadic wind damage, the most severe being in western and central Lauderdale County, where a narrow swath of damage included homes being destroyed and a church experiencing heavy damage. Several trees were snapped or toppled in the path. A tree was reported down on Milk Springs Road.", "ts_dict_index": [12135, 12136, 12137]}
+{"event_id": 1012849, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2022-03-30 18:38:00", "end_date_time": "2022-03-30 18:38:00", "narrative": "A powerful low pressure system moved northeast from the central Plains into the Great Lakes, bringing a strong cold front through the Mississippi and Tennessee Valleys. Very windy conditions developed during the morning and extended into the early evening hours of the 30th, producing sustained speeds of 25-35 mph and gusts of 45 to 55 mph. These winds knocked down numerous tree limbs and trees, some power lines and some power poles This resulted in power outages in portions of northern Alabama.  Significant roof damage also occurred.||A squall line which originated during the early morning of the 30th over Arkansas reached northwest Alabama around 5-7 PM, and tracked east across the remainder of north Alabama during the evening hours.  The line of thunderstorms also produced sporadic wind damage, the most severe being in western and central Lauderdale County, where a narrow swath of damage included homes being destroyed and a church experiencing heavy damage. Several trees were snapped or toppled in the path. Trees and powerlines were blown down along North Pike Road.", "ts_dict_index": [12141, 12142, 12143]}
+{"event_id": 1013195, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2022-03-30 18:46:00", "end_date_time": "2022-03-30 18:58:00", "narrative": "A powerful low pressure system moved northeast from the central Plains into the Great Lakes, bringing a strong cold front through the Mississippi and Tennessee Valleys. Very windy conditions developed during the morning and extended into the early evening hours of the 30th, producing sustained speeds of 25-35 mph and gusts of 45 to 55 mph. These winds knocked down numerous tree limbs and trees, some power lines and some power poles This resulted in power outages in portions of northern Alabama.  Significant roof damage also occurred.||A squall line which originated during the early morning of the 30th over Arkansas reached northwest Alabama around 5-7 PM, and tracked east across the remainder of north Alabama during the evening hours.  The line of thunderstorms also produced sporadic wind damage, the most severe being in western and central Lauderdale County, where a narrow swath of damage included homes being destroyed and a church experiencing heavy damage. Several trees were snapped or toppled in the path. A narrow swath of winds between 64 and 93 mph affect locations just southwest of the intersection of CR 106 and Highway 20 (east of the Natchez Trace Parkway) and moved northeast before weakening near the Cloverdale community.  Some of the most severe damage occurred near the beginning of the its path, where the roof of Cornerstone  Church of Christ received significant damage, two power poles were snapped near its base, and trees were uprooted.  Several very large trees were uprooted along CR 81 as it moved further northeast.  Significant roof damage occurred along CR 200 just southwest of the intersection of Lindsey Drive to a commercial structure.  Additional uprooted trees and roof/awning damage occurred to homes near Lindsey Drive and Lynne Drive.  A huge 3 to 4 foot in diameter pine tree was snapped at its base near Lynn Drive.  These intense winds continued to move northeast, crossing CR 154 and  uprooting several large softwood trees just west of the intersection of CR 291.  As the severe storm continued northeast, winds collapsed the door of  a small barn and broke off large branches from trees as it crossed CR 8. The swath of damage continue to near the intersection of Cloverdale road and Cooper Drive, where several more trees were uprooted.", "ts_dict_index": [12144, 12145, 12146]}
+{"event_id": 1012857, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2022-03-30 19:58:00", "end_date_time": "2022-03-30 19:58:00", "narrative": "A powerful low pressure system moved northeast from the central Plains into the Great Lakes, bringing a strong cold front through the Mississippi and Tennessee Valleys. Very windy conditions developed during the morning and extended into the early evening hours of the 30th, producing sustained speeds of 25-35 mph and gusts of 45 to 55 mph. These winds knocked down numerous tree limbs and trees, some power lines and some power poles This resulted in power outages in portions of northern Alabama.  Significant roof damage also occurred.||A squall line which originated during the early morning of the 30th over Arkansas reached northwest Alabama around 5-7 PM, and tracked east across the remainder of north Alabama during the evening hours.  The line of thunderstorms also produced sporadic wind damage, the most severe being in western and central Lauderdale County, where a narrow swath of damage included homes being destroyed and a church experiencing heavy damage. Several trees were snapped or toppled in the path. A tree was reported down at the intersection of Wheeler View Drive and River Road.", "ts_dict_index": [12147, 12148, 12149]}
+{"event_id": 1131791, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-08-31 20:19:00", "end_date_time": "2023-08-31 20:19:00", "narrative": "The overall pattern featured an upper-level low pressure situated along the west coast and the subtropical high pressure centered over New Mexico. This overall pattern configuration resulted in southerly flow across Arizona, which helped transport moisture into the region. Thus, the environment became conducive for thunderstorm activity as PWATs rose to 1.3-1.5 and MLCAPE values ranged between 1000-2000 J/kg across most of central and southern AZ. DCAPE values were very high, on the order of 2000 J/kg, which resulted in a very favorable setup for strong to severe winds. Thunderstorms first developed over southeast Arizona and then, with the southerly flow, were steered into south-central AZ. There were widespread reports of dense blowing dust with visibilities reduced to 1/4 mile or less as well as wind damage as winds were in excess of 60 mph. In addition, a training thunderstorm over northern Maricopa County, in the Anthem area, resulted in 2-4 of rain according to doppler radar estimates and led to significant flash flooding. A 60 mph wind gust was measured at a mesonet station located along State Route 230 just west of Maricopa.", "ts_dict_index": [12018, 12019, 12020]}
+{"event_id": 972196, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:56:00", "end_date_time": "2021-07-07 14:56:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Near Fall Run Park, trees were reported to be uprooted.", "ts_dict_index": [12174, 12175, 12176]}
+{"event_id": 972191, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-07-07 14:49:00", "end_date_time": "2021-07-07 14:49:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Snapped trees were reported via social media images on Puckety Church Road.", "ts_dict_index": [12177, 12178, 12179]}
+{"event_id": 903224, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-09 14:20:00", "end_date_time": "2020-07-09 14:20:00", "narrative": "Storms that developed in the early afternoon took advantage of the very high instability and had no trouble becoming strong, and even severe, in a short amount of time. Storms initially formed along and north of the Highway 30 corridor in eastern Iowa, produced widespread damage to crops in Buchanan and Delaware counties, and eventually went on to produce a wind gust near 60 mph at the Dubuque Regional Airport. Storms across this area eventually merged and slowed down, leading to localized rainfall amounts of 4-5 inches. This very heavy rainfall produced flash flooding in the Dubuque metro, with law enforcement reporting several road closures along Highway 20.|Storms continued to form along a line to the south through the mid afternoon, and reached the Mississippi River around 6-7 PM. Several reports of wind damage to trees were received from McDonough county to the Quad Cities metro area. A few reports of funnel clouds were also received from the Kirkwood, IL area, but no tornado was ever observed. Recorded by rwis system.", "ts_dict_index": [12162, 12163, 12164]}
+{"event_id": 972950, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-07-07 19:53:00", "end_date_time": "2021-07-07 19:53:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Multiple reports of downed trees were received from around the New Florence area.", "ts_dict_index": [12189, 12190, 12191]}
+{"event_id": 903199, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2020-07-09 14:49:00", "end_date_time": "2020-07-09 14:49:00", "narrative": "Storms that developed in the early afternoon took advantage of the very high instability and had no trouble becoming strong, and even severe, in a short amount of time. Storms initially formed along and north of the Highway 30 corridor in eastern Iowa, produced widespread damage to crops in Buchanan and Delaware counties, and eventually went on to produce a wind gust near 60 mph at the Dubuque Regional Airport. Storms across this area eventually merged and slowed down, leading to localized rainfall amounts of 4-5 inches. This very heavy rainfall produced flash flooding in the Dubuque metro, with law enforcement reporting several road closures along Highway 20.|Storms continued to form along a line to the south through the mid afternoon, and reached the Mississippi River around 6-7 PM. Several reports of wind damage to trees were received from McDonough county to the Quad Cities metro area. A few reports of funnel clouds were also received from the Kirkwood, IL area, but no tornado was ever observed. Video sent through social media showing a tree falling in a yard and over a road.", "ts_dict_index": [12159, 12160, 12161]}
+{"event_id": 972194, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:54:00", "end_date_time": "2021-07-07 14:54:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Trees were blown down on to a vehicle in Shaler.", "ts_dict_index": [12180, 12181, 12182]}
+{"event_id": 972192, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:54:00", "end_date_time": "2021-07-07 14:54:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Trees were reported to be blown down in Natrona Heights.", "ts_dict_index": [12186, 12187, 12188]}
+{"event_id": 825075, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-15 16:34:00", "end_date_time": "2019-06-15 16:34:00", "narrative": "Increasingly humid conditions, a weak low pressure system, and an impinging northern weak cold front combined to create an environment ripe for strong to severe storms across northern and central Iowa, with much of the severe activity through central Iowa. ||The resulting environment from the aforementioned ingredients included SBCAPE values in the 2000-3000+ J/kg range, marginal effective bulk shear around 30 kts, 400-600 J/kg CAPE in the hail growth region, and at least a few hours with steep low level lapse rates around or greater than 8 deg C/km. All in all while the environment did not lend much support to long lived strong to severe storms, it was more than enough for brief periods of severe storms as many pulsed up and down prior to congealing into multi-cellular clusters and eventually an mesoscale convective system by the evening. Most reports revolved around severe and damaging winds, with a few instances of hail, heavy rainfall, and a land-spout reported north of Whitten in Hardin county. Des Moines International Airport ASOS recorded a 70 mph wind gust.", "ts_dict_index": [12171, 12172, 12173]}
+{"event_id": 825076, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-15 16:35:00", "end_date_time": "2019-06-15 16:35:00", "narrative": "Increasingly humid conditions, a weak low pressure system, and an impinging northern weak cold front combined to create an environment ripe for strong to severe storms across northern and central Iowa, with much of the severe activity through central Iowa. ||The resulting environment from the aforementioned ingredients included SBCAPE values in the 2000-3000+ J/kg range, marginal effective bulk shear around 30 kts, 400-600 J/kg CAPE in the hail growth region, and at least a few hours with steep low level lapse rates around or greater than 8 deg C/km. All in all while the environment did not lend much support to long lived strong to severe storms, it was more than enough for brief periods of severe storms as many pulsed up and down prior to congealing into multi-cellular clusters and eventually an mesoscale convective system by the evening. Most reports revolved around severe and damaging winds, with a few instances of hail, heavy rainfall, and a land-spout reported north of Whitten in Hardin county. Public relayed images of tree branches and power lines down. Time estimated from radar.", "ts_dict_index": [12150, 12151, 12152]}
+{"event_id": 832937, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-07-10 16:45:00", "end_date_time": "2019-07-10 16:45:00", "narrative": "A weak upper trough shifted east across the High Plains/Upper Midwest during July 10th, with the tail end of this trough pushing southeast into Eastern Oklahoma and Northern Arkansas. This upper trough helped nudge a weak cool front south across Central and Eastern Oklahoma into Central Arkansas on the 10th, with compressional warming ahead of the front allowing for temperatures to climb into the middle 90s across Southeast Oklahoma and Southwest Arkansas. With a moist air mass already in place, moderate to high amounts of instability developed ahead of the front, with large scale forcing adequate enough near the weak front/upper trough to result in a band of strong to severe thunderstorms developing by mid and late afternoon across Southeast Oklahoma and Western Arkansas, which shifted south into McCurtain County Oklahoma and much of Southwest Arkansas. These storms produced damaging winds, which downed large tree limbs near Hochatown before slowly weakening as they entered extreme Northeast Texas. Large tree limbs were downed near Hochatown.", "ts_dict_index": [12165, 12166, 12167]}
+{"event_id": 825073, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-15 16:33:00", "end_date_time": "2019-06-15 16:33:00", "narrative": "Increasingly humid conditions, a weak low pressure system, and an impinging northern weak cold front combined to create an environment ripe for strong to severe storms across northern and central Iowa, with much of the severe activity through central Iowa. ||The resulting environment from the aforementioned ingredients included SBCAPE values in the 2000-3000+ J/kg range, marginal effective bulk shear around 30 kts, 400-600 J/kg CAPE in the hail growth region, and at least a few hours with steep low level lapse rates around or greater than 8 deg C/km. All in all while the environment did not lend much support to long lived strong to severe storms, it was more than enough for brief periods of severe storms as many pulsed up and down prior to congealing into multi-cellular clusters and eventually an mesoscale convective system by the evening. Most reports revolved around severe and damaging winds, with a few instances of hail, heavy rainfall, and a land-spout reported north of Whitten in Hardin county. WOI TV relayed viewer photo of a large tree snapped near SW 18th St and Army Post Rd in Des Moines.", "ts_dict_index": [12153, 12154, 12155]}
+{"event_id": 825078, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-15 16:35:00", "end_date_time": "2019-06-15 16:35:00", "narrative": "Increasingly humid conditions, a weak low pressure system, and an impinging northern weak cold front combined to create an environment ripe for strong to severe storms across northern and central Iowa, with much of the severe activity through central Iowa. ||The resulting environment from the aforementioned ingredients included SBCAPE values in the 2000-3000+ J/kg range, marginal effective bulk shear around 30 kts, 400-600 J/kg CAPE in the hail growth region, and at least a few hours with steep low level lapse rates around or greater than 8 deg C/km. All in all while the environment did not lend much support to long lived strong to severe storms, it was more than enough for brief periods of severe storms as many pulsed up and down prior to congealing into multi-cellular clusters and eventually an mesoscale convective system by the evening. Most reports revolved around severe and damaging winds, with a few instances of hail, heavy rainfall, and a land-spout reported north of Whitten in Hardin county. Public reported a couple large tree limbs down with one estimated around a foot in diameter falling and damaging a chain link fence on Wade St. Another 5 inch diameter tree branch was down on Mason Ave from the storm. Time estimated from radar.", "ts_dict_index": [12156, 12157, 12158]}
+{"event_id": 1089169, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-03-16 23:10:00", "end_date_time": "2023-03-16 23:10:00", "narrative": "A long-lived cluster of supercell thunderstorms advanced across northeast Texas into northwest Louisiana on the evening of March 16th just ahead of an accelerating band of thunderstorms along a cold front. As the evening progressed, the cold front gradually overtook the ongoing supercell cluster with the primary threat of hail transitioning to damaging winds within the expanding QLCS. Initially within the far eastern edge of the warm sector, supercell thunderstorms over Sabine County/Parish in Deep East Texas and far western Louisiana produced large hail. The QLCS continued to evolve along the cold front, with an embedded long-lived supercell over Rusk County Texas later in the evening. The environment favored a continuation of the severe threat downstream, with the greatest threat expected along the QLCS segment and with the embedded supercell. As that portion of the line moved southeastward, the threat for damaging winds persisted with a few additional reports of damage in East Texas and Northwest Louisiana. Tree downed on Dab Brown Road.", "ts_dict_index": [12129, 12130, 12131]}
+{"event_id": 972149, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:16:00", "end_date_time": "2021-07-07 14:16:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Trees were reported to be blown down in Swissvale.", "ts_dict_index": [12204, 12205, 12206]}
+{"event_id": 972116, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 15:10:00", "end_date_time": "2021-07-07 15:10:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Trees were reported to be blown down on McKean Road.", "ts_dict_index": [12213, 12214, 12215]}
+{"event_id": 972148, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:15:00", "end_date_time": "2021-07-07 14:15:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Widespread wind damage was reported in Edgewood Boro, resulting in the declaration of a local state of emergency.", "ts_dict_index": [12195, 12196, 12197]}
+{"event_id": 972151, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:25:00", "end_date_time": "2021-07-07 14:25:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. In Renton Junction, there was a report of numerous trees being blown down, resulting in power outages.", "ts_dict_index": [12192, 12193, 12194]}
+{"event_id": 972147, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:15:00", "end_date_time": "2021-07-07 14:15:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Trees were reported to be blown down in Regent Square.", "ts_dict_index": [12201, 12202, 12203]}
+{"event_id": 972159, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:35:00", "end_date_time": "2021-07-07 14:35:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. A large tree was blown down along West Swissvale Avenue.", "ts_dict_index": [12207, 12208, 12209]}
+{"event_id": 972157, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:35:00", "end_date_time": "2021-07-07 14:35:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. In the neighborhood of Friendship, shingles were blown off of a structure and tree limbs were downed.", "ts_dict_index": [12198, 12199, 12200]}
+{"event_id": 972132, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:10:00", "end_date_time": "2021-07-07 14:10:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Trees were reported to be blown down, causing power outages.", "ts_dict_index": [12210, 12211, 12212]}
+{"event_id": 972949, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-07-07 19:24:00", "end_date_time": "2021-07-07 19:24:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Trees were blown down in Greensburg.", "ts_dict_index": [12183, 12184, 12185]}
+{"event_id": 902576, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-06 18:11:00", "end_date_time": "2020-07-06 18:11:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Trees and wires were downed near Furnace Rd in New Morgan. Time estimated from radar.", "ts_dict_index": [12237, 12238, 12239]}
+{"event_id": 902390, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-07-06 13:23:00", "end_date_time": "2020-07-06 13:23:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree fell on wires on Creek Rd at NJ-38 in Hainsesport. Time estimated from radar.", "ts_dict_index": [12240, 12241, 12242]}
+{"event_id": 902568, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-06 16:58:00", "end_date_time": "2020-07-06 16:58:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was down on Englesville Rd at S Washington St. Time estimated from radar.", "ts_dict_index": [12246, 12247, 12248]}
+{"event_id": 902514, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-06 17:25:00", "end_date_time": "2020-07-06 17:25:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed at north 10th St and Bern St in Reading. Time estimated from radar.", "ts_dict_index": [12255, 12256, 12257]}
+{"event_id": 1057083, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-10-25 00:30:00", "end_date_time": "2022-10-25 00:30:00", "narrative": "A potent upper level low pressure system over New Mexico shifted east across Western and North Texas south of the Red River during the afternoon and evening hours of October 24th, which allowed for a dry line to mix east across Texas. A cold front extended east of this upper low over Eastern Oklahoma and Northeast Texas, with the dry line eventually overtaking the front but provided strong forcing for a linear line of showers and thunderstorms to develop during the evening and overnight hours as they entered East Texas. Although instability was limited given cooler conditions during the latter evening hours, strong shear resulted in a well-organized line of strong to severe thunderstorms along these surface features, producing damaging winds which downed trees across portions of East Texas. These storms weakened further upon entering Western Louisiana during the early morning hours on the 25th, but still produced isolated pockets of wind damage across Central Caddo and Western Claiborne Parishes. A tree was blown down on Irving Bluff Road.", "ts_dict_index": [12234, 12235, 12236]}
+{"event_id": 902513, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 16:55:00", "end_date_time": "2020-07-06 16:55:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Trees and wires were downed at the Gilbertsville Golf Course. Time estimated from radar.", "ts_dict_index": [12243, 12244, 12245]}
+{"event_id": 902541, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 14:30:00", "end_date_time": "2020-07-06 14:30:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed on wires on Pawlings Rd. Time estimated from radar.", "ts_dict_index": [12249, 12250, 12251]}
+{"event_id": 972188, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 14:49:00", "end_date_time": "2021-07-07 14:49:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Trees were reported to be blown down in Harrison Township.", "ts_dict_index": [12219, 12220, 12221]}
+{"event_id": 1085469, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-04-15 20:13:00", "end_date_time": "2023-04-15 20:13:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. A tree was blown down at the corner of Five Oaks Road and Highway 550.", "ts_dict_index": [12228, 12229, 12230]}
+{"event_id": 972323, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-07 16:40:00", "end_date_time": "2021-07-07 16:40:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Trees and power lines were blown down in Millvale.", "ts_dict_index": [12222, 12223, 12224]}
+{"event_id": 1085464, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-04-15 18:55:00", "end_date_time": "2023-04-15 18:55:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. Trees were downed on Highway 84 east of Clarence.", "ts_dict_index": [12231, 12232, 12233]}
+{"event_id": 1085463, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-04-15 18:35:00", "end_date_time": "2023-04-15 18:35:00", "narrative": "A longwave trough exited the Intermountain West into the Central and Southern Plains on April 15th, which reinforced a cold front southeast into Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the afternoon. Hot and humid air spread north across the region from the Gulf of Mexico ahead of the front with the northward advance of a warm front, with temperatures climbing into the upper 80s and lower 90s areawide. These abnormally hot and humid conditions resulted in moderate to very unstable conditions ahead of the front, as large scale ascent increased ahead of the ejecting trough along and just ahead of the approaching cold front. As a result, scattered to numerous strong to severe thunderstorms developed during the afternoon and evening hours across Northeast Texas, Southwest Arkansas, and North Louisiana, and produced multiple instances of damaging winds, large hail, and even an isolated tornado over Western Bienville Parish before exiting the area during the mid-evening hours. A few trees and power lines were blown down between Black Lake and Campti.", "ts_dict_index": [12225, 12226, 12227]}
+{"event_id": 825074, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-15 16:33:00", "end_date_time": "2019-06-15 16:33:00", "narrative": "Increasingly humid conditions, a weak low pressure system, and an impinging northern weak cold front combined to create an environment ripe for strong to severe storms across northern and central Iowa, with much of the severe activity through central Iowa. ||The resulting environment from the aforementioned ingredients included SBCAPE values in the 2000-3000+ J/kg range, marginal effective bulk shear around 30 kts, 400-600 J/kg CAPE in the hail growth region, and at least a few hours with steep low level lapse rates around or greater than 8 deg C/km. All in all while the environment did not lend much support to long lived strong to severe storms, it was more than enough for brief periods of severe storms as many pulsed up and down prior to congealing into multi-cellular clusters and eventually an mesoscale convective system by the evening. Most reports revolved around severe and damaging winds, with a few instances of hail, heavy rainfall, and a land-spout reported north of Whitten in Hardin county. Trained spotter estimated 60 to 70 mph wind gusts near Blank Park Zoo.", "ts_dict_index": [12168, 12169, 12170]}
+{"event_id": 902366, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-07-06 13:15:00", "end_date_time": "2020-07-06 13:15:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Downed wires closed NJ-73 in both directions between Brick Rd and Maple Ave. All lanes were closed and detoured. Time estimated from radar.", "ts_dict_index": [12258, 12259, 12260]}
+{"event_id": 902364, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-07-06 13:14:00", "end_date_time": "2020-07-06 13:14:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Tree limbs and wires were downed near Branch St in Medford. Time estimated from radar.", "ts_dict_index": [12264, 12265, 12266]}
+{"event_id": 902354, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-07-06 12:47:00", "end_date_time": "2020-07-06 12:47:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Wires were downed near Green St in Mount Holly. Time estimated from radar.", "ts_dict_index": [12261, 12262, 12263]}
+{"event_id": 972187, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-07-07 14:49:00", "end_date_time": "2021-07-07 14:49:00", "narrative": "A nearly stationary front remained to the north of the region on July 7th. An upper trough dug across the Great Lakes during the daytime hours as well. While better upper-level forcing remained to the north, return flow increased between this trough and the tropical system Elsa to the southeast. An abundant amount of moisture and warm air was thus funneled into our region.  Deep-layer shear was weak, but enough instability and dry air aloft was present to promote many instances of damaging wind gusts.  Damage to trees and power poles was fairly widespread, and there were a few instances of structural damage as well.  Planes were overturned by wind at Butler Airport, and Edgewood Borough declared a local state of emergency due to thunderstorm wind damage. ||Multiple rounds of thunderstorms also lead to flash flooding concerns in the urbanized areas of Allegheny County. Several instances of stuck vehicles were reported, and several homes were evacuated for a time in Bridgeville due to creek flooding. Trees and power poles were reported to be blown down.", "ts_dict_index": [12216, 12217, 12218]}
+{"event_id": 902533, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-07-06 13:42:00", "end_date_time": "2020-07-06 13:42:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Several trees and wires were downed in Warwick Twp. Time estimated from radar.", "ts_dict_index": [12282, 12283, 12284]}
+{"event_id": 902537, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-07-06 14:00:00", "end_date_time": "2020-07-06 14:00:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A power pole was snapped with wires downed on Scott Rd at Keller's Church Rd. Report via social media. Time estimated from radar.", "ts_dict_index": [12297, 12298, 12299]}
+{"event_id": 902555, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-06 16:00:00", "end_date_time": "2020-07-06 16:00:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed on Phoenixville Pike near King Rd in Exton. Time estimated from radar.", "ts_dict_index": [12285, 12286, 12287]}
+{"event_id": 902391, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-07-06 13:32:00", "end_date_time": "2020-07-06 13:32:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Trees and wires were downed in Lindenwold. Time estimated from radar.", "ts_dict_index": [12276, 12277, 12278]}
+{"event_id": 902530, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 13:28:00", "end_date_time": "2020-07-06 13:28:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Power lines were downed on Landis Mill Rd near Level Rd in Collegeville. Time estimated from radar.", "ts_dict_index": [12267, 12268, 12269]}
+{"event_id": 902542, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-06 14:37:00", "end_date_time": "2020-07-06 14:37:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Several reports of trees and wires down in the Valley Forge area, including near Oakwood Ln, Valley Park Rd, Jug Hollow Rd, and Davis Rd. Time estimated from radar.", "ts_dict_index": [12288, 12289, 12290]}
+{"event_id": 902546, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 15:06:00", "end_date_time": "2020-07-06 15:06:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed near Richard's Rd and Stephen's Dr, blocking Richard's Rd near Valley Forge. Time estimated from radar.", "ts_dict_index": [12300, 12301, 12302]}
+{"event_id": 902511, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-06 16:27:00", "end_date_time": "2020-07-06 16:27:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Trees and wires were downed near the intersection of Meetinghouse Rd and Creek Rd north of Chadds Ford. Time estimated from radar.", "ts_dict_index": [12291, 12292, 12293]}
+{"event_id": 902561, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-06 16:07:00", "end_date_time": "2020-07-06 16:07:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Tree limbs and wires were downed near Matthew's Ln in Alburtis. Time estimated from radar.", "ts_dict_index": [12279, 12280, 12281]}
+{"event_id": 902557, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-06 16:01:00", "end_date_time": "2020-07-06 16:01:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Tree limbs and wires were downed near Molasses Barrel Rd in Emerald. Time estimated from radar.", "ts_dict_index": [12270, 12271, 12272]}
+{"event_id": 902560, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-06 16:05:00", "end_date_time": "2020-07-06 16:05:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Trees were downed southeast of Mertztown. Time estimated from radar.", "ts_dict_index": [12252, 12253, 12254]}
+{"event_id": 902567, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-06 16:52:00", "end_date_time": "2020-07-06 16:52:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed on Manatawny Rd. Time estimated from radar.", "ts_dict_index": [12303, 12304, 12305]}
+{"event_id": 902575, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-06 17:34:00", "end_date_time": "2020-07-06 17:34:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Trees and wires were downed near Tulpehocken Rd in Reading. Time estimated from radar.", "ts_dict_index": [12309, 12310, 12311]}
+{"event_id": 902549, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-06 15:24:00", "end_date_time": "2020-07-06 15:24:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed near the intersection of Sproul Rd and Three Tun Rd in East Whiteland Twp. Time estimated from radar.", "ts_dict_index": [12306, 12307, 12308]}
+{"event_id": 902539, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-06 14:29:00", "end_date_time": "2020-07-06 14:29:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Several reports of trees and wires down in Spring City, Royersford, Phoenixville, and Upper Providence Twp. Time estimated from radar.", "ts_dict_index": [12294, 12295, 12296]}
+{"event_id": 902525, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 12:50:00", "end_date_time": "2020-07-06 12:50:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was snapped. Report via social media with a photo. Time estimated from radar.", "ts_dict_index": [12321, 12322, 12323]}
+{"event_id": 902357, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-07-06 13:00:00", "end_date_time": "2020-07-06 13:00:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Wires were downed near Monmouth Rd in Springfield Twp. Time estimated from radar.", "ts_dict_index": [12339, 12340, 12341]}
+{"event_id": 902572, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-06 17:10:00", "end_date_time": "2020-07-06 17:10:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed along PA-61 near Hamburg. Time estimated from radar.", "ts_dict_index": [12312, 12313, 12314]}
+{"event_id": 902526, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 13:05:00", "end_date_time": "2020-07-06 13:05:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed onto a vehicle on Walnut Farm Rd in Lower Gwynedd Twp. Time estimated from radar.", "ts_dict_index": [12318, 12319, 12320]}
+{"event_id": 902515, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-06 17:41:00", "end_date_time": "2020-07-06 17:41:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree fell into wires near Wernersville. Time estimated from radar.", "ts_dict_index": [12348, 12349, 12350]}
+{"event_id": 902356, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-07-06 12:55:00", "end_date_time": "2020-07-06 12:55:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Tree limbs and wires were downed near Columbia Blvd in Cherry Hill. Time estimated from radar.", "ts_dict_index": [12333, 12334, 12335]}
+{"event_id": 902527, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-07-06 13:08:00", "end_date_time": "2020-07-06 13:08:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Wires were downed on County Line Rd in Feasterville. Time estimated from radar.", "ts_dict_index": [12360, 12361, 12362]}
+{"event_id": 902570, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-06 17:02:00", "end_date_time": "2020-07-06 17:02:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed on Eagle Point Rd at Long Ln. Time estimated from radar.", "ts_dict_index": [12315, 12316, 12317]}
+{"event_id": 902360, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-07-06 13:06:00", "end_date_time": "2020-07-06 13:06:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree and wires were downed near Locust Ave in Haddon Twp. Time estimated from radar.", "ts_dict_index": [12330, 12331, 12332]}
+{"event_id": 902358, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-07-06 13:06:00", "end_date_time": "2020-07-06 13:06:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Several reports of trees and wires down in the Springdale, Society Hill, and Ellisburg areas. Time estimated from radar.", "ts_dict_index": [12336, 12337, 12338]}
+{"event_id": 902566, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-06 16:40:00", "end_date_time": "2020-07-06 16:40:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed on Ellicott Rd in Avondale. Time estimated from radar.", "ts_dict_index": [12342, 12343, 12344]}
+{"event_id": 902528, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 13:10:00", "end_date_time": "2020-07-06 13:10:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed onto wires on Washington Ln at Old York Rd in Jenkintown. Time estimated from radar.", "ts_dict_index": [12369, 12370, 12371]}
+{"event_id": 902521, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 12:18:00", "end_date_time": "2020-07-06 12:18:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed on Green Valley Rd near Thornberry Rd in Wyncote. Time estimated from radar.", "ts_dict_index": [12351, 12352, 12353]}
+{"event_id": 902367, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-07-06 13:20:00", "end_date_time": "2020-07-06 13:20:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Multiple trees and wires were downed on NJ-73 in Marlton. Report via social media. Time estimated from radar.", "ts_dict_index": [12363, 12364, 12365]}
+{"event_id": 902573, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-06 17:26:00", "end_date_time": "2020-07-06 17:26:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Power lines were downed near Kevin Court in West Lawn. Time estimated from radar.", "ts_dict_index": [12372, 12373, 12374]}
+{"event_id": 902564, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-06 16:32:00", "end_date_time": "2020-07-06 16:32:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Multiple reports of trees down into wires on US-1. Time estimated from radar.", "ts_dict_index": [12324, 12325, 12326]}
+{"event_id": 902545, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-06 14:58:00", "end_date_time": "2020-07-06 14:58:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed on Cool Valley Rd near Shadow Oak Dr in Devault. Time estimated from radar.", "ts_dict_index": [12375, 12376, 12377]}
+{"event_id": 902547, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-06 15:07:00", "end_date_time": "2020-07-06 15:07:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Tree limbs and wires were downed near Red Maple Acres in Ancient Oaks. Time estimated from radar.", "ts_dict_index": [12357, 12358, 12359]}
+{"event_id": 902563, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-06 16:15:00", "end_date_time": "2020-07-06 16:15:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Trees and wires were downed north of New Tripoli. Time estimated from radar.", "ts_dict_index": [12327, 12328, 12329]}
+{"event_id": 902565, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-06 16:32:00", "end_date_time": "2020-07-06 16:32:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Trees and wires were downed near the intersection of Mountain Rd and Chester Rd. Time estimated from radar.", "ts_dict_index": [12345, 12346, 12347]}
+{"event_id": 902562, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-06 16:10:00", "end_date_time": "2020-07-06 16:10:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Multiple reports of downed trees and wires were received on Mountain Rd. Time estimated from radar.", "ts_dict_index": [12273, 12274, 12275]}
+{"event_id": 902369, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-07-06 13:45:00", "end_date_time": "2020-07-06 13:45:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Measured by NJweathernet site NJ66.", "ts_dict_index": [12381, 12382, 12383]}
+{"event_id": 902519, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-07-06 12:15:00", "end_date_time": "2020-07-06 12:15:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Wires were downed on Mill St. Time estimated from radar.", "ts_dict_index": [12378, 12379, 12380]}
+{"event_id": 902551, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-06 15:29:00", "end_date_time": "2020-07-06 15:29:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed into wires on Valley Park Rd at Pothouse Rd. Time estimated from radar.", "ts_dict_index": [12384, 12385, 12386]}
+{"event_id": 902362, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-07-06 13:08:00", "end_date_time": "2020-07-06 13:08:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Several reports of downed tree limbs and wires in the Evesboro and Marlton areas. Time estimated from radar.", "ts_dict_index": [12366, 12367, 12368]}
+{"event_id": 902353, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-07-06 11:51:00", "end_date_time": "2020-07-06 11:51:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Wires downed near Riverside Twp High School. Time estimated from radar.", "ts_dict_index": [12390, 12391, 12392]}
+{"event_id": 851259, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-03 17:17:00", "end_date_time": "2019-10-03 17:17:00", "narrative": "A large upper level ridge of high pressure extended from the Carolinas/Tennessee Valley across much of the Southeast U.S. during October 3rd, maintaining record heat over these areas and even west into much of the North Louisiana, Southwest Arkansas, and East Texas. Meanwhile, a weak upper low and associated inverted trough over the Western Gulf drifted west to the Texas coast into West Central Louisiana and East Texas during the afternoon, around the western periphery of the upper level ridge. A plume of very moist air spread west across much of North Louisiana and into portions of East Texas during the day on the 3rd, and coupled with strong heating, resulted in moderate instability that enabled scattered strong to severe thunderstorms to develop and spread west across Western Louisiana and portions of East Texas during the afternoon and evening. Some of these storms produced damaging winds which downed trees across portions of Webster and Caddo Parishes before diminishing by late evening. A large tree was blown onto power lines near the intersection of McCutchen Avenue and Lucille Street. A nearby power pole was snapped. Numerous large branches were snapped along McCutchen Avenue. Other power lines were downed throughout Shreveport.", "ts_dict_index": [12414, 12415, 12416]}
+{"event_id": 902534, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 13:43:00", "end_date_time": "2020-07-06 13:43:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed on Eagleville Rd near Pinetown Rd in Oaks. Time estimated from radar.", "ts_dict_index": [12396, 12397, 12398]}
+{"event_id": 902536, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 13:45:00", "end_date_time": "2020-07-06 13:45:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed on Hillside Ave near Coleman St in Norristown. Time estimated from radar.", "ts_dict_index": [12387, 12388, 12389]}
+{"event_id": 902524, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 12:29:00", "end_date_time": "2020-07-06 12:29:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree was downed on Bobarn Dr near Hagys Ford Rd in Gladwyne. Time estimated from radar.", "ts_dict_index": [12402, 12403, 12404]}
+{"event_id": 851257, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-03 17:17:00", "end_date_time": "2019-10-03 17:17:00", "narrative": "A large upper level ridge of high pressure extended from the Carolinas/Tennessee Valley across much of the Southeast U.S. during October 3rd, maintaining record heat over these areas and even west into much of the North Louisiana, Southwest Arkansas, and East Texas. Meanwhile, a weak upper low and associated inverted trough over the Western Gulf drifted west to the Texas coast into West Central Louisiana and East Texas during the afternoon, around the western periphery of the upper level ridge. A plume of very moist air spread west across much of North Louisiana and into portions of East Texas during the day on the 3rd, and coupled with strong heating, resulted in moderate instability that enabled scattered strong to severe thunderstorms to develop and spread west across Western Louisiana and portions of East Texas during the afternoon and evening. Some of these storms produced damaging winds which downed trees across portions of Webster and Caddo Parishes before diminishing by late evening. A large tree was snapped in front of the Mary Goula Baptist Church on Mansfield Rd. near Highway 3132.", "ts_dict_index": [12411, 12412, 12413]}
+{"event_id": 902355, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-07-06 12:53:00", "end_date_time": "2020-07-06 12:53:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. A tree and wires were downed near Ashley Ln in Lumberton. Time estimated from radar.", "ts_dict_index": [12393, 12394, 12395]}
+{"event_id": 902523, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-06 12:26:00", "end_date_time": "2020-07-06 12:26:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Wires were downed near the intersection of Bowman Ave and Linden Ln. Time estimated from radar.", "ts_dict_index": [12399, 12400, 12401]}
+{"event_id": 851256, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2019-10-03 15:50:00", "end_date_time": "2019-10-03 15:50:00", "narrative": "A large upper level ridge of high pressure extended from the Carolinas/Tennessee Valley across much of the Southeast U.S. during October 3rd, maintaining record heat over these areas and even west into much of the North Louisiana, Southwest Arkansas, and East Texas. Meanwhile, a weak upper low and associated inverted trough over the Western Gulf drifted west to the Texas coast into West Central Louisiana and East Texas during the afternoon, around the western periphery of the upper level ridge. A plume of very moist air spread west across much of North Louisiana and into portions of East Texas during the day on the 3rd, and coupled with strong heating, resulted in moderate instability that enabled scattered strong to severe thunderstorms to develop and spread west across Western Louisiana and portions of East Texas during the afternoon and evening. Some of these storms produced damaging winds which downed trees across portions of Webster and Caddo Parishes before diminishing by late evening. A tree was blown down on Penal Farm Road just south of Minden.", "ts_dict_index": [12408, 12409, 12410]}
+{"event_id": 946944, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-04-23 23:55:00", "end_date_time": "2021-04-23 23:55:00", "narrative": "Warm, moist, and unstable air began to return north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma on April 23rd, in response to a strong southerly low level jet which advanced a warm front north into these areas ahead of an approaching upper trough which ejected into the Southern Plains from the Southwestern U.S. Increasing wind shear and steep mid level lapse rates ahead of this trough contributed to increased large scale forcing such that a cluster of strong to severe thunderstorms developed over Southern Oklahoma and North Texas during the evening of the 23rd, with the resultant cold pool from these storms enhancing a line of strong to severe thunderstorms within a more unstable air mass across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the early morning hours of the 24th. Numerous trees were downed across McCurtain County Oklahoma, with trees falling on homes near Broken Bow, south of Idabel, and also near Wright City. Trees were downed onto homes in Wright City.", "ts_dict_index": [12420, 12421, 12422]}
+{"event_id": 946945, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-04-24 00:06:00", "end_date_time": "2021-04-24 00:06:00", "narrative": "Warm, moist, and unstable air began to return north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma on April 23rd, in response to a strong southerly low level jet which advanced a warm front north into these areas ahead of an approaching upper trough which ejected into the Southern Plains from the Southwestern U.S. Increasing wind shear and steep mid level lapse rates ahead of this trough contributed to increased large scale forcing such that a cluster of strong to severe thunderstorms developed over Southern Oklahoma and North Texas during the evening of the 23rd, with the resultant cold pool from these storms enhancing a line of strong to severe thunderstorms within a more unstable air mass across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the early morning hours of the 24th. Numerous trees were downed across McCurtain County Oklahoma, with trees falling on homes near Broken Bow, south of Idabel, and also near Wright City. A wind gust of 58 mph was measured at the Idabel AWOS.", "ts_dict_index": [12417, 12418, 12419]}
+{"event_id": 902363, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-07-06 13:11:00", "end_date_time": "2020-07-06 13:11:00", "narrative": "A slow moving backdoor cold front drifted southwest through the mid-Atlantic region on July 6. Meanwhile, a shortwave vorticity impulse, one of several in a series, moved across the region during the day. A very hot and humid air mass was present ahead of the backdoor cold front, leading to the development of strong to extreme instability over the region. The approaching upper level disturbance allowed for the development of moderate wind shear over the region. Combined with the front, it also acted as a trigger mechanism for convection. Severe thunderstorms developed by early afternoon over eastern PA and southern and central New Jersey. These storms produced strong outflow boundaries which served to initiate additional severe convection. The result was a ring of fire in which outflow steadily propagated outward in all directions. This caused severe weather to spread radially outward from its origin near Philadelphia to much of New Jersey, other portions of eastern Pennsylvania, and Delmarva. Reports of tree limbs and wires downed near Georgia Trail in Medford. Time estimated from radar.", "ts_dict_index": [12354, 12355, 12356]}
+{"event_id": 1044282, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "ADAMS", "begin_date_time": "2022-08-06 21:38:00", "end_date_time": "2022-08-06 21:38:00", "narrative": "A cold front moved into the NWS Hastings coverage area during the daytime hours of August 6th, and was located roughly southwest to northeast across central portions of the area by late afternoon. Very hot, humid, and unstable conditions existed ahead of the cold front, with heat indices of 100 to 105 degrees common. By early evening, a few thunderstorms developed south-southwest of Holdrege and slowly drifted northeast. As the cold front approached this activity, initial spotty thunderstorms increased in coverage and grew upscale into a small cluster. The hot, deeply mixed airmass from the daytime hours, and high cloud bases, were conducive to isolated strong wind gusts. The only wind report with this activity came from emergency management of an overturned pivot near Holstein in Adams County. This was estimated to have occurred during the late evening hours. Non-severe thunderstorms continued into the early morning hours of the 7th, mainly south of Interstate 80 and east of Highway 183. Emergency management reported irrigation pivots flipped and a damaged grain bin near Holstein.", "ts_dict_index": [12426, 12427, 12428]}
+{"event_id": 946943, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-04-24 00:06:00", "end_date_time": "2021-04-24 00:06:00", "narrative": "Warm, moist, and unstable air began to return north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma on April 23rd, in response to a strong southerly low level jet which advanced a warm front north into these areas ahead of an approaching upper trough which ejected into the Southern Plains from the Southwestern U.S. Increasing wind shear and steep mid level lapse rates ahead of this trough contributed to increased large scale forcing such that a cluster of strong to severe thunderstorms developed over Southern Oklahoma and North Texas during the evening of the 23rd, with the resultant cold pool from these storms enhancing a line of strong to severe thunderstorms within a more unstable air mass across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the early morning hours of the 24th. Numerous trees were downed across McCurtain County Oklahoma, with trees falling on homes near Broken Bow, south of Idabel, and also near Wright City. Numerous trees were blown down across McCurtain County. Trees were downed onto homes near Idabel and Broken Bow.", "ts_dict_index": [12423, 12424, 12425]}
+{"event_id": 851255, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2019-10-03 15:49:00", "end_date_time": "2019-10-03 15:49:00", "narrative": "A large upper level ridge of high pressure extended from the Carolinas/Tennessee Valley across much of the Southeast U.S. during October 3rd, maintaining record heat over these areas and even west into much of the North Louisiana, Southwest Arkansas, and East Texas. Meanwhile, a weak upper low and associated inverted trough over the Western Gulf drifted west to the Texas coast into West Central Louisiana and East Texas during the afternoon, around the western periphery of the upper level ridge. A plume of very moist air spread west across much of North Louisiana and into portions of East Texas during the day on the 3rd, and coupled with strong heating, resulted in moderate instability that enabled scattered strong to severe thunderstorms to develop and spread west across Western Louisiana and portions of East Texas during the afternoon and evening. Some of these storms produced damaging winds which downed trees across portions of Webster and Caddo Parishes before diminishing by late evening. Numerous trees and large limbs were downed, street signs were blown over on Highway 531, and power poles were leaning throughout the city of Minden. The entire city was without power at one point.", "ts_dict_index": [12405, 12406, 12407]}
+{"event_id": 959182, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-06 19:39:00", "end_date_time": "2021-07-06 19:39:00", "narrative": "Hot and humid conditions existed over the mid-Atlantic on July 6, with a cold front well northwest over the Great Lakes and southern Canada. As temperatures rose into the 90s with dew points in the upper 60s and low 70s, strong instability built over the region. A pre-frontal trough and a fast moving upper level disturbance provided some lift, which helped convection develop by mid afternoon. Convection was initially concentrated over northern Pennsylvania and New York, near the better forcing, but propagated southeastward with time. Shear was weak to moderate but sufficient to allow some storm organization into multi-cellular and linear segments. A number of storms became severe, producing damaging winds and some hail. As storms moved southeast, outflow boundaries moving even further south helped ignite additional convection, some severe, which continued into the early overnight hours. The early overnight convection was also noted to be especially prolific with regard to lightning. An mPing report of large tree limbs or power lines down.", "ts_dict_index": [12468, 12469, 12470]}
+{"event_id": 1063690, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2022-11-27 15:16:00", "end_date_time": "2022-11-27 15:16:00", "narrative": "A strong, occluding surface low crossed the Great Lakes on November 27th. After morning rain, instability in the form of around 500 J/kg of mean-layer CAPE was able to develop in the Middle Ohio Valley and advect northeast into northern West Virginia and southwest Pennsylvania.  A strongly sheared environment was also present. Strong low-level flow helped to support a damaging-wind threat, while cold temperatures aloft and favorable deep-layer shear also supported large hail, which is unusual for late November.  In fact, severe conditions were locally quite signficant, with one report of an 87 MPH gust in a mesovortex, as well as hail reaching two inches in diameter.  Many reports of downed trees and power lines were received, with some generally minor structural damage as well.  In Perry Township, estimates were that up to 400 vehicles were damaged by hail, with an estimated 1.2 million dollars worth of damage. A similar amount of car damage also likely occurred in Westmoreland County. Multiple trees and wires were reported to be down in the area.", "ts_dict_index": [12441, 12442, 12443]}
+{"event_id": 959149, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-06 17:06:00", "end_date_time": "2021-07-06 17:06:00", "narrative": "Hot and humid conditions existed over the mid-Atlantic on July 6, with a cold front well northwest over the Great Lakes and southern Canada. As temperatures rose into the 90s with dew points in the upper 60s and low 70s, strong instability built over the region. A pre-frontal trough and a fast moving upper level disturbance provided some lift, which helped convection develop by mid afternoon. Convection was initially concentrated over northern Pennsylvania and New York, near the better forcing, but propagated southeastward with time. Shear was weak to moderate but sufficient to allow some storm organization into multi-cellular and linear segments. A number of storms became severe, producing damaging winds and some hail. As storms moved southeast, outflow boundaries moving even further south helped ignite additional convection, some severe, which continued into the early overnight hours. The early overnight convection was also noted to be especially prolific with regard to lightning. A large tree was downed at the Jeffersonville Golf Course. Time estimated from radar.", "ts_dict_index": [12459, 12460, 12461]}
+{"event_id": 1063698, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2022-11-27 15:15:00", "end_date_time": "2022-11-27 15:15:00", "narrative": "A strong, occluding surface low crossed the Great Lakes on November 27th. After morning rain, instability in the form of around 500 J/kg of mean-layer CAPE was able to develop in the Middle Ohio Valley and advect northeast into northern West Virginia and southwest Pennsylvania.  A strongly sheared environment was also present. Strong low-level flow helped to support a damaging-wind threat, while cold temperatures aloft and favorable deep-layer shear also supported large hail, which is unusual for late November.  In fact, severe conditions were locally quite signficant, with one report of an 87 MPH gust in a mesovortex, as well as hail reaching two inches in diameter.  Many reports of downed trees and power lines were received, with some generally minor structural damage as well.  In Perry Township, estimates were that up to 400 vehicles were damaged by hail, with an estimated 1.2 million dollars worth of damage. A similar amount of car damage also likely occurred in Westmoreland County. This peak wind gust was measured with an anemometer, and was coincident with the passage of a mesovortex. The wind carried shelters tens of feet, created minor structural damage, and uprooted some softwood trees.", "ts_dict_index": [12444, 12445, 12446]}
+{"event_id": 913753, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-09-28 01:55:00", "end_date_time": "2020-09-28 01:55:00", "narrative": "A strong upper level trough shifted southeast across the Southern Plains and into East Texas and Southwest Arkansas during the evening hours of September 27th, which reinforced the first fall cold front of the season southeast into the Ark-La-Tex from the late evening hours through the morning hours of September 28th. A strong southerly low level flow ahead of the front resulted in a rapid increase in low level moisture north across East Texas, Southeast Oklahoma, Southwest Arkansas, and Northwest Louisiana ahead of the front, while strong large scale forcing increased near this boundary within an unstable air mass. As a result, a cluster of strong thunderstorms developed near and just ahead of the front, and spread southeast into Northern Louisiana during the early morning hours of the 28th. An isolated severe thunderstorm developed near Haughton just ahead of the front, which downed trees onto homes. These storms weakened as they continued to shift southeast across North Louisiana. Two mobile homes were damaged by falling trees on Rodgers Lane in Haughton. No injuries were reported.", "ts_dict_index": [12450, 12451, 12452]}
+{"event_id": 1063695, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2022-11-27 15:21:00", "end_date_time": "2022-11-27 15:21:00", "narrative": "A strong, occluding surface low crossed the Great Lakes on November 27th. After morning rain, instability in the form of around 500 J/kg of mean-layer CAPE was able to develop in the Middle Ohio Valley and advect northeast into northern West Virginia and southwest Pennsylvania.  A strongly sheared environment was also present. Strong low-level flow helped to support a damaging-wind threat, while cold temperatures aloft and favorable deep-layer shear also supported large hail, which is unusual for late November.  In fact, severe conditions were locally quite signficant, with one report of an 87 MPH gust in a mesovortex, as well as hail reaching two inches in diameter.  Many reports of downed trees and power lines were received, with some generally minor structural damage as well.  In Perry Township, estimates were that up to 400 vehicles were damaged by hail, with an estimated 1.2 million dollars worth of damage. A similar amount of car damage also likely occurred in Westmoreland County. Multiple trees were uprooted in the area.", "ts_dict_index": [12429, 12430, 12431]}
+{"event_id": 959158, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-06 19:56:00", "end_date_time": "2021-07-06 19:56:00", "narrative": "Hot and humid conditions existed over the mid-Atlantic on July 6, with a cold front well northwest over the Great Lakes and southern Canada. As temperatures rose into the 90s with dew points in the upper 60s and low 70s, strong instability built over the region. A pre-frontal trough and a fast moving upper level disturbance provided some lift, which helped convection develop by mid afternoon. Convection was initially concentrated over northern Pennsylvania and New York, near the better forcing, but propagated southeastward with time. Shear was weak to moderate but sufficient to allow some storm organization into multi-cellular and linear segments. A number of storms became severe, producing damaging winds and some hail. As storms moved southeast, outflow boundaries moving even further south helped ignite additional convection, some severe, which continued into the early overnight hours. The early overnight convection was also noted to be especially prolific with regard to lightning. A large tree fell and other branches and limbs were downed in the area from a likely downburst. Time estimated from radar.", "ts_dict_index": [12462, 12463, 12464]}
+{"event_id": 959147, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-06 16:30:00", "end_date_time": "2021-07-06 16:30:00", "narrative": "Hot and humid conditions existed over the mid-Atlantic on July 6, with a cold front well northwest over the Great Lakes and southern Canada. As temperatures rose into the 90s with dew points in the upper 60s and low 70s, strong instability built over the region. A pre-frontal trough and a fast moving upper level disturbance provided some lift, which helped convection develop by mid afternoon. Convection was initially concentrated over northern Pennsylvania and New York, near the better forcing, but propagated southeastward with time. Shear was weak to moderate but sufficient to allow some storm organization into multi-cellular and linear segments. A number of storms became severe, producing damaging winds and some hail. As storms moved southeast, outflow boundaries moving even further south helped ignite additional convection, some severe, which continued into the early overnight hours. The early overnight convection was also noted to be especially prolific with regard to lightning. Large tree limbs were downed on Jefferson Ave. Time estimated from radar.", "ts_dict_index": [12465, 12466, 12467]}
+{"event_id": 959160, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-06 19:56:00", "end_date_time": "2021-07-06 19:56:00", "narrative": "Hot and humid conditions existed over the mid-Atlantic on July 6, with a cold front well northwest over the Great Lakes and southern Canada. As temperatures rose into the 90s with dew points in the upper 60s and low 70s, strong instability built over the region. A pre-frontal trough and a fast moving upper level disturbance provided some lift, which helped convection develop by mid afternoon. Convection was initially concentrated over northern Pennsylvania and New York, near the better forcing, but propagated southeastward with time. Shear was weak to moderate but sufficient to allow some storm organization into multi-cellular and linear segments. A number of storms became severe, producing damaging winds and some hail. As storms moved southeast, outflow boundaries moving even further south helped ignite additional convection, some severe, which continued into the early overnight hours. The early overnight convection was also noted to be especially prolific with regard to lightning. Multiple large trees were downed on Uhlerstown Hill Rd near Tinicum Twp. Time estimated from radar.", "ts_dict_index": [12456, 12457, 12458]}
+{"event_id": 1063689, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2022-11-27 14:52:00", "end_date_time": "2022-11-27 14:52:00", "narrative": "A strong, occluding surface low crossed the Great Lakes on November 27th. After morning rain, instability in the form of around 500 J/kg of mean-layer CAPE was able to develop in the Middle Ohio Valley and advect northeast into northern West Virginia and southwest Pennsylvania.  A strongly sheared environment was also present. Strong low-level flow helped to support a damaging-wind threat, while cold temperatures aloft and favorable deep-layer shear also supported large hail, which is unusual for late November.  In fact, severe conditions were locally quite signficant, with one report of an 87 MPH gust in a mesovortex, as well as hail reaching two inches in diameter.  Many reports of downed trees and power lines were received, with some generally minor structural damage as well.  In Perry Township, estimates were that up to 400 vehicles were damaged by hail, with an estimated 1.2 million dollars worth of damage. A similar amount of car damage also likely occurred in Westmoreland County. Multiple trees were reported down in the area.", "ts_dict_index": [12435, 12436, 12437]}
+{"event_id": 1063691, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2022-11-27 15:19:00", "end_date_time": "2022-11-27 15:19:00", "narrative": "A strong, occluding surface low crossed the Great Lakes on November 27th. After morning rain, instability in the form of around 500 J/kg of mean-layer CAPE was able to develop in the Middle Ohio Valley and advect northeast into northern West Virginia and southwest Pennsylvania.  A strongly sheared environment was also present. Strong low-level flow helped to support a damaging-wind threat, while cold temperatures aloft and favorable deep-layer shear also supported large hail, which is unusual for late November.  In fact, severe conditions were locally quite signficant, with one report of an 87 MPH gust in a mesovortex, as well as hail reaching two inches in diameter.  Many reports of downed trees and power lines were received, with some generally minor structural damage as well.  In Perry Township, estimates were that up to 400 vehicles were damaged by hail, with an estimated 1.2 million dollars worth of damage. A similar amount of car damage also likely occurred in Westmoreland County. Multiple trees were reported to be down in Fairfield Township, with a few trees downed on houses.", "ts_dict_index": [12438, 12439, 12440]}
+{"event_id": 959146, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-06 16:41:00", "end_date_time": "2021-07-06 16:41:00", "narrative": "Hot and humid conditions existed over the mid-Atlantic on July 6, with a cold front well northwest over the Great Lakes and southern Canada. As temperatures rose into the 90s with dew points in the upper 60s and low 70s, strong instability built over the region. A pre-frontal trough and a fast moving upper level disturbance provided some lift, which helped convection develop by mid afternoon. Convection was initially concentrated over northern Pennsylvania and New York, near the better forcing, but propagated southeastward with time. Shear was weak to moderate but sufficient to allow some storm organization into multi-cellular and linear segments. A number of storms became severe, producing damaging winds and some hail. As storms moved southeast, outflow boundaries moving even further south helped ignite additional convection, some severe, which continued into the early overnight hours. The early overnight convection was also noted to be especially prolific with regard to lightning. A tree brought down a transformer and wires. Time estimated from radar.", "ts_dict_index": [12453, 12454, 12455]}
+{"event_id": 1063693, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2022-11-27 15:20:00", "end_date_time": "2022-11-27 15:20:00", "narrative": "A strong, occluding surface low crossed the Great Lakes on November 27th. After morning rain, instability in the form of around 500 J/kg of mean-layer CAPE was able to develop in the Middle Ohio Valley and advect northeast into northern West Virginia and southwest Pennsylvania.  A strongly sheared environment was also present. Strong low-level flow helped to support a damaging-wind threat, while cold temperatures aloft and favorable deep-layer shear also supported large hail, which is unusual for late November.  In fact, severe conditions were locally quite signficant, with one report of an 87 MPH gust in a mesovortex, as well as hail reaching two inches in diameter.  Many reports of downed trees and power lines were received, with some generally minor structural damage as well.  In Perry Township, estimates were that up to 400 vehicles were damaged by hail, with an estimated 1.2 million dollars worth of damage. A similar amount of car damage also likely occurred in Westmoreland County. Trees were reported to be blown down along Route 30.", "ts_dict_index": [12432, 12433, 12434]}
+{"event_id": 1113461, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:51:00", "end_date_time": "2023-06-11 15:51:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. Trees were blown down and blocking the roadway at Oak Hill Baptist Church in Somerset, making the road impassable.", "ts_dict_index": [12471, 12472, 12473]}
+{"event_id": 1113474, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:35:00", "end_date_time": "2023-06-11 15:35:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. Trees were reported down along the Cumberland Parkway at mile marker 78 (Nancy Exit), blocking both of the eastbound lanes. The first responders that were called out also reported having golf ball sized hail en route to the location.", "ts_dict_index": [12474, 12475, 12476]}
+{"event_id": 1113460, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:51:00", "end_date_time": "2023-06-11 15:51:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. A powerline was down in the yard of a residence at the 1700 block of Patterson Branch Road, southwest of Somerset. The pole was also reported to have possibly been broken.", "ts_dict_index": [12480, 12481, 12482]}
+{"event_id": 1113453, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 16:40:00", "end_date_time": "2023-06-11 16:40:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. A tree was blown down and blocking the roadway at 3000 block of Simpson Drive in Somerset.", "ts_dict_index": [12489, 12490, 12491]}
+{"event_id": 1113468, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 16:04:00", "end_date_time": "2023-06-11 16:04:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. A powerline was reported down across Elliott Drive in Somerset, near Loveless Lane.", "ts_dict_index": [12492, 12493, 12494]}
+{"event_id": 1113435, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:35:00", "end_date_time": "2023-06-11 15:35:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. Trees were reported down for about a mile along Highway 1664 near the intersection with Pierce Road (Sputter Branch Road), just west of Nancy. Many of the trees were partially rotten or small, and survey conducted by emergency management concluded the damage was from straightline winds.", "ts_dict_index": [12483, 12484, 12485]}
+{"event_id": 1113864, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 16:05:00", "end_date_time": "2023-06-11 16:05:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. A tree was reported to have been blown down onto a residence somewhere in the Somerset vicinity.", "ts_dict_index": [12477, 12478, 12479]}
+{"event_id": 1113459, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:35:00", "end_date_time": "2023-06-11 15:35:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. A tree was downed and completely blocking Hudson Road (Calhoun Road) near the intersection of Burnetta Road, northwest of the community of Nancy.", "ts_dict_index": [12486, 12487, 12488]}
+{"event_id": 1113473, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:38:00", "end_date_time": "2023-06-11 15:38:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. Trees were blocking the entire roadway on Hwy-196, just past the Faubush Fire Department, near the community of Nancy.", "ts_dict_index": [12501, 12502, 12503]}
+{"event_id": 1113464, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:19:00", "end_date_time": "2023-06-11 15:19:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. A tree was reportedly fallen and leaning on a power line at the 200 block of Lanetown Road (W. Frye Road) in the community of Nancy.", "ts_dict_index": [12495, 12496, 12497]}
+{"event_id": 1113472, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:40:00", "end_date_time": "2023-06-11 15:40:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. A powerline was downed from winds at the 300 block of Pierce Road, near the community of Nancy.", "ts_dict_index": [12504, 12505, 12506]}
+{"event_id": 1113462, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:51:00", "end_date_time": "2023-06-11 15:51:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. Large branches were reported in the roadway on Grand Central Blvd, near the intersection with Grand Circle, southwest of Somerset.", "ts_dict_index": [12507, 12508, 12509]}
+{"event_id": 1113457, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:43:00", "end_date_time": "2023-06-11 15:43:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. What appears to be cable lines are laying across the road at the 2300 block of Slate Branch Road, just northwest of Burnside.", "ts_dict_index": [12513, 12514, 12515]}
+{"event_id": 1113433, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:34:00", "end_date_time": "2023-06-11 15:34:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. Trees were reported blown down across the road, resulting in downed powerlines at the 2100 block of Faubush Road near the community of Faubush.", "ts_dict_index": [12510, 12511, 12512]}
+{"event_id": 913752, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-09-28 01:53:00", "end_date_time": "2020-09-28 01:53:00", "narrative": "A strong upper level trough shifted southeast across the Southern Plains and into East Texas and Southwest Arkansas during the evening hours of September 27th, which reinforced the first fall cold front of the season southeast into the Ark-La-Tex from the late evening hours through the morning hours of September 28th. A strong southerly low level flow ahead of the front resulted in a rapid increase in low level moisture north across East Texas, Southeast Oklahoma, Southwest Arkansas, and Northwest Louisiana ahead of the front, while strong large scale forcing increased near this boundary within an unstable air mass. As a result, a cluster of strong thunderstorms developed near and just ahead of the front, and spread southeast into Northern Louisiana during the early morning hours of the 28th. An isolated severe thunderstorm developed near Haughton just ahead of the front, which downed trees onto homes. These storms weakened as they continued to shift southeast across North Louisiana. A tree fell onto a mobile home on Foster Road in Haughton. No injuries were reported.", "ts_dict_index": [12447, 12448, 12449]}
+{"event_id": 879571, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-04-09 13:29:00", "end_date_time": "2020-04-09 13:29:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. ", "ts_dict_index": [12519, 12520, 12521]}
+{"event_id": 879570, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-04-09 13:25:00", "end_date_time": "2020-04-09 13:25:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. NJWeathernet site.", "ts_dict_index": [12522, 12523, 12524]}
+{"event_id": 879593, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-04-09 12:18:00", "end_date_time": "2020-04-09 12:18:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Two large trees uprooted in Richboro. Time estimated from radar.", "ts_dict_index": [12531, 12532, 12533]}
+{"event_id": 879590, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-04-09 12:00:00", "end_date_time": "2020-04-09 12:00:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A tree was downed on a house in Lower Providence Twp.", "ts_dict_index": [12528, 12529, 12530]}
+{"event_id": 879650, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-04-09 12:18:00", "end_date_time": "2020-04-09 12:18:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A large tree was uprooted. Time estimated from radar.", "ts_dict_index": [12534, 12535, 12536]}
+{"event_id": 879659, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-04-09 22:50:00", "end_date_time": "2020-04-09 22:50:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Several reports of downed trees and power lines in the West Grove and Landenberg areas. Time estimated from radar.", "ts_dict_index": [12525, 12526, 12527]}
+{"event_id": 1113418, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:54:00", "end_date_time": "2023-06-11 15:54:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. A tree was reported down on a house along Patterson Branch Road. The extent of the damage is unknown.", "ts_dict_index": [12498, 12499, 12500]}
+{"event_id": 879569, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-04-09 13:10:00", "end_date_time": "2020-04-09 13:10:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Miller Air Park.", "ts_dict_index": [12543, 12544, 12545]}
+{"event_id": 879592, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-04-09 12:15:00", "end_date_time": "2020-04-09 12:15:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. An outdoor shed was significantly damaged. Time estimated from radar.", "ts_dict_index": [12552, 12553, 12554]}
+{"event_id": 879921, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-19 11:56:00", "end_date_time": "2020-04-19 11:56:00", "narrative": "A warm front lifted north into Deep East Texas and the southern sections of North Central Louisiana by afternoon on April 19th, ahead of a vigorous upper level trough that ejected east from New Mexico across Texas. Large scale forcing increased by afternoon ahead of the trough as it approached the expanding warm sector, characteristic of moderate instability and strong wind shear. Areas of showers and thunderstorms developed and became widespread near and north of the warm front, and limited the northward progress of the front, but severe thunderstorms still developed within the warm sector across Deep East Texas and Northcentral Louisiana, resulting in areas of damaging winds across these areas. An isolated elevated severe thunderstorm also developed over portions of Lamar County Texas, which moved into Red River County and produced quarter size hail near Clarksville. These storms eventually weakened during the mid evening hours with the passage of the trough through the area. Trees were blown down on County Road 452.", "ts_dict_index": [12558, 12559, 12560]}
+{"event_id": 879535, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-04-09 12:35:00", "end_date_time": "2020-04-09 12:35:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A downed tree blocked the right lane of the westbound New Jersey Turnpike. Time estimated from radar.", "ts_dict_index": [12540, 12541, 12542]}
+{"event_id": 879591, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-04-09 12:05:00", "end_date_time": "2020-04-09 12:05:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A video posted to social media from downtown Reading showed numerous trees uprooted and downed, as well as numerous downed power lines. Time estimated from radar.", "ts_dict_index": [12555, 12556, 12557]}
+{"event_id": 879658, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-04-09 22:40:00", "end_date_time": "2020-04-09 22:40:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A tree was downed on PA-472. Time estimated from radar.", "ts_dict_index": [12546, 12547, 12548]}
+{"event_id": 879657, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-04-09 22:35:00", "end_date_time": "2020-04-09 22:35:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Wires were downed near the intersection of Mount Pleasant Rd and Grant St. Time estimated from radar.", "ts_dict_index": [12549, 12550, 12551]}
+{"event_id": 879660, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-04-09 22:52:00", "end_date_time": "2020-04-09 22:52:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Wires were downed near the intersection of Chesterville Rd and Penn Green Rd. Time estimated from radar.", "ts_dict_index": [12561, 12562, 12563]}
+{"event_id": 879563, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-04-09 12:35:00", "end_date_time": "2020-04-09 12:35:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. NJ Weathernet site.", "ts_dict_index": [12567, 12568, 12569]}
+{"event_id": 879661, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-04-09 22:52:00", "end_date_time": "2020-04-09 22:52:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A tree was downed on Laurel Heights Rd. Time estimated from radar.", "ts_dict_index": [12564, 12565, 12566]}
+{"event_id": 1113451, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-06-11 15:34:00", "end_date_time": "2023-06-11 15:34:00", "narrative": "A warm front was parked across western Kentucky during the early morning hours on Sunday June 11th. This slowly transitioned eastward through the first part of the day as an area of low pressure tracked along the Ohio River. By late afternoon and evening, the warm front was through eastern Kentucky, putting us in a more unstable pattern, especially with a quickly approaching cold front and a low pressure system so close by. Multiple Severe Thunderstorm and Tornado Warnings were issued between 4pm and 9pm across eastern Kentucky, with widespread reports of damaging winds and large hail from some of the storms that developed. The strongest storm impacted Pulaski county, resulting in baseball size hail between Nancy and Somerset, and widespread straight-line winds in the communities of Faubush and Nancy. Activity finally settled down as we headed into the overnight an lost the best instability, though the cold front didn't move through until the wee hours of the morning on the 12th. A tree fell onto a garage at the 2400 block of Faubush Road near the community of Nancy.", "ts_dict_index": [12516, 12517, 12518]}
+{"event_id": 879547, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-04-09 12:46:00", "end_date_time": "2020-04-09 12:46:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Several large tree limbs were downed with some minor property damage at a residence. Time estimated from radar.", "ts_dict_index": [12576, 12577, 12578]}
+{"event_id": 879583, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-04-09 11:24:00", "end_date_time": "2020-04-09 11:24:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Photos of several large trees down in the area. Time estimated from radar.", "ts_dict_index": [12582, 12583, 12584]}
+{"event_id": 879924, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2020-04-19 11:37:00", "end_date_time": "2020-04-19 11:37:00", "narrative": "A warm front lifted north into Deep East Texas and the southern sections of North Central Louisiana by afternoon on April 19th, ahead of a vigorous upper level trough that ejected east from New Mexico across Texas. Large scale forcing increased by afternoon ahead of the trough as it approached the expanding warm sector, characteristic of moderate instability and strong wind shear. Areas of showers and thunderstorms developed and became widespread near and north of the warm front, and limited the northward progress of the front, but severe thunderstorms still developed within the warm sector across Deep East Texas and Northcentral Louisiana, resulting in areas of damaging winds across these areas. An isolated elevated severe thunderstorm also developed over portions of Lamar County Texas, which moved into Red River County and produced quarter size hail near Clarksville. These storms eventually weakened during the mid evening hours with the passage of the trough through the area. Trees were blown down on Highway 455.", "ts_dict_index": [12579, 12580, 12581]}
+{"event_id": 879543, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-04-09 12:42:00", "end_date_time": "2020-04-09 12:42:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A tree was downed on I-295 north of Exit 43. Lane restrictions were required. Time estimated from radar.", "ts_dict_index": [12591, 12592, 12593]}
+{"event_id": 879587, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-04-09 11:48:00", "end_date_time": "2020-04-09 11:48:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Trees and wires downed in the area. Pea size hail also reported.", "ts_dict_index": [12588, 12589, 12590]}
+{"event_id": 879653, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-04-09 12:13:00", "end_date_time": "2020-04-09 12:13:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A tree was uprooted and blocked a roadway. Power lines were also downed. Time estimated from radar.", "ts_dict_index": [12570, 12571, 12572]}
+{"event_id": 879588, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-04-09 11:50:00", "end_date_time": "2020-04-09 11:50:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A tree was downed near Township Line Rd and Nutt Rd.", "ts_dict_index": [12585, 12586, 12587]}
+{"event_id": 1052140, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-01 20:36:00", "end_date_time": "2022-09-01 20:36:00", "narrative": "Under a classic setup for storm motion from the Mogollon Rim to the Valley (Rim-to-Valley), with the monsoon 500mb high positioned over Nevada, a multicell storm cluster descended out of the White Mountains, through Gila County, and into the lower deserts of Maricopa and Pinal Counties in the early overnight hours of the 1st. Moisture levels were near average for the time of year, but steep mid level lapse rates over the high terrain (7-8 C/km) and modest shear (Sfc-6km around 20-25 kts) was sufficient to support the development of an organized multicell storm cluster. The environment was also supportive of strong downbursts, with DCAPE up around 1000-1500 J/kg. A single ordinary storm also developed in the Queen Creek/San Tan Valley area a couple hours before the multicell cluster moved into the lower deserts, and produced a damaging downburst. Strong winds leading to a dust storm was eventually generated by the multicell cluster once it moved into Maricopa and Pinal Counties. Two large trees (20-24 inch diameter trunks) were uprooted and each fell through concrete block walls and onto a couple homes in the Johnson Ranch community. The extent of the damage to the homes was unknown. There were also several street signs reportedly ripped from their posts or were twisted/mangled. Winds were estimated around 55-60 mph and timing was based on radar. No injuries were reported.", "ts_dict_index": [12594, 12595, 12596]}
+{"event_id": 1052139, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-01 20:35:00", "end_date_time": "2022-09-01 20:35:00", "narrative": "Under a classic setup for storm motion from the Mogollon Rim to the Valley (Rim-to-Valley), with the monsoon 500mb high positioned over Nevada, a multicell storm cluster descended out of the White Mountains, through Gila County, and into the lower deserts of Maricopa and Pinal Counties in the early overnight hours of the 1st. Moisture levels were near average for the time of year, but steep mid level lapse rates over the high terrain (7-8 C/km) and modest shear (Sfc-6km around 20-25 kts) was sufficient to support the development of an organized multicell storm cluster. The environment was also supportive of strong downbursts, with DCAPE up around 1000-1500 J/kg. A single ordinary storm also developed in the Queen Creek/San Tan Valley area a couple hours before the multicell cluster moved into the lower deserts, and produced a damaging downburst. Strong winds leading to a dust storm was eventually generated by the multicell cluster once it moved into Maricopa and Pinal Counties. Approximately 5-6 trees, at 20 to 30 feet tall, were toppled on Johnson Ranch Boulevard. Wind speeds estimated around 55-60 mph and timing estimated from radar. No injuries were reported.", "ts_dict_index": [12600, 12601, 12602]}
+{"event_id": 879536, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-04-09 12:35:00", "end_date_time": "2020-04-09 12:35:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A section of a roof was peeled off with reports of large branches scattered about in the city.", "ts_dict_index": [12537, 12538, 12539]}
+{"event_id": 879586, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-04-09 11:42:00", "end_date_time": "2020-04-09 11:42:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A utility pole was snapped in half in Boyertown. Time estimated from radar.", "ts_dict_index": [12624, 12625, 12626]}
+{"event_id": 804369, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-03-09 11:09:00", "end_date_time": "2019-03-09 11:09:00", "narrative": "A large upper level trough moved out of the Intermountain West and into the Southern Plains during the early morning hours of March 9th, taking on a negative tilt as it lifted east northeast across much of Central and Eastern Texas into Northern Louisiana and Southwest Arkansas. The trough allowed for a dry line to mix east across Central and Eastern Oklahoma, as well as Central Texas, into a region of moderate instability produced by a surge of very warm and moist air north from the Gulf of Mexico. As large scale forcing increased during the morning hours of the 9th, showers and thunderstorms, some of which were severe, developed and spread east northeast across Southeast Oklahoma, Southwest Arkansas, portions of Northeast Texas, and North Louisiana.  Damaging winds downed trees across portions of Northwest Louisiana, with NWS storm surveys confirming three tornado touchdowns across Northern Caddo, Bossier, and Webster Parishes before the storms weakened by early afternoon. A pine tree was uprooted, and several large branches were snapped off.", "ts_dict_index": [12633, 12634, 12635]}
+{"event_id": 879589, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-04-09 11:54:00", "end_date_time": "2020-04-09 11:54:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Several reports of downed trees and wires in the area. Time estimated from radar.", "ts_dict_index": [12603, 12604, 12605]}
+{"event_id": 879545, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-04-09 12:45:00", "end_date_time": "2020-04-09 12:45:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Power lines were downed on Coral Ave in Mount Laurel.", "ts_dict_index": [12621, 12622, 12623]}
+{"event_id": 879541, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-04-09 12:39:00", "end_date_time": "2020-04-09 12:39:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. A tree was downed on I-295 south of Exit 34. Lane restrictions were required. Time estimated from radar.", "ts_dict_index": [12606, 12607, 12608]}
+{"event_id": 1113741, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-26 06:12:00", "end_date_time": "2023-06-26 06:12:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Several large oak trees snapped and power lines downed.", "ts_dict_index": [12636, 12637, 12638]}
+{"event_id": 879539, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-04-09 12:37:00", "end_date_time": "2020-04-09 12:37:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Photo received of hardwood tree down.", "ts_dict_index": [12615, 12616, 12617]}
+{"event_id": 879540, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-04-09 12:37:00", "end_date_time": "2020-04-09 12:37:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Fencing was blown over with several large tree limbs down at a residence. Time estimated from radar.", "ts_dict_index": [12618, 12619, 12620]}
+{"event_id": 879542, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-04-09 12:40:00", "end_date_time": "2020-04-09 12:40:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Downed trees caused at least one road closure in the area. Time estimated from radar.", "ts_dict_index": [12609, 12610, 12611]}
+{"event_id": 1113750, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-06-26 07:07:00", "end_date_time": "2023-06-26 07:07:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Report of power lines downed.", "ts_dict_index": [12630, 12631, 12632]}
+{"event_id": 1113748, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-06-26 06:57:00", "end_date_time": "2023-06-26 06:57:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Tree downed and blocking Highway 9.", "ts_dict_index": [12627, 12628, 12629]}
+{"event_id": 879562, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-04-09 12:35:00", "end_date_time": "2020-04-09 12:35:00", "narrative": "A warm front moved through the mid-Atlantic on the morning of April 9. During the late morning and early afternoon, the mid-Atlantic was in a narrow warm sector with a cold front quickly approaching from the west as low pressure tracked through the Great Lakes and then began to redevelop over southern New England. Ahead of the front, a strongly forced and highly sheared environment existed. Heating and moisture were limited in the small warm sector region, but sufficient instability developed to support convective development, and a broken line of showers and thunderstorms moved across the region, causing a considerable amount of wind damage.||That evening, additional severe weather occurred as several post-frontal squalls developed. One of these squalls developed into a low-topped thunderstorm. Steep lapse rates and strong wind profiles allowed this storm to also produce wind damage over southeastern Pennsylvania, northeast Maryland, northern Delaware, and southern New Jersey. Winds estimated at 50 to 60 mph were reported in Gloucester City. Tree damage was also observed in the area.", "ts_dict_index": [12573, 12574, 12575]}
+{"event_id": 1113742, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-26 06:15:00", "end_date_time": "2023-06-26 06:15:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Trees and power lines downed with damage to a home, leading to a rescue operation.", "ts_dict_index": [12639, 12640, 12641]}
+{"event_id": 1113753, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-06-26 06:00:00", "end_date_time": "2023-06-26 06:00:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Trees downed and utility poles snapped near 7th Street in Benton.", "ts_dict_index": [12645, 12646, 12647]}
+{"event_id": 834613, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-06-28 20:15:00", "end_date_time": "2019-06-28 20:15:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. A social media user reported that trees were blown down, and also shared a picture of their trampoline, which had been thrown across the yard.", "ts_dict_index": [12675, 12676, 12677]}
+{"event_id": 1113749, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-26 06:30:00", "end_date_time": "2023-06-26 06:30:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Tree snapped in front of a home on Barron Road in Keithville.", "ts_dict_index": [12642, 12643, 12644]}
+{"event_id": 1113744, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-06-26 06:10:00", "end_date_time": "2023-06-26 06:10:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Large limbs were snapped south of Benton. Report via mPING.", "ts_dict_index": [12651, 12652, 12653]}
+{"event_id": 1102780, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-05-07 16:00:00", "end_date_time": "2023-05-07 16:10:00", "narrative": "Several rounds of severe thunderstorms impacted the area on Sunday May 7, 2023.  Two areas of storms were present during the mid to late afternoon, one entering the Cedar Rapids and Iowa City metros and another around the Burlington and Fort Madison metros. The first was the most severe, producing hail up to baseball size in Koszta, Iowa and widespread wind damage, especially around West Liberty, Iowa. This storm, and storms to the west, eventually merged into a cluster of severe thunderstorms, producing large hail and destructive winds around 70-75 mph all the way to Mount Pleasant, Iowa and Macomb, Illinois. The latter produced sporadic reports of quarter to half dollar sized hail, along with a brief landspout tornado east of Yorktown, IL.  There was also severe blowing dust which was especially bad near I-55 in north central Illinois. Even more thunderstorms developed overnight across the area, and mainly produced torrential rain and isolated large hail reports. Estimated 66 mph wind gust at Eastern Iowa Airport ASOS.", "ts_dict_index": [12669, 12670, 12671]}
+{"event_id": 834611, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-06-28 19:35:00", "end_date_time": "2019-06-28 19:35:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. Power lines were blown down at the intersection of Route 136 and Wooster Street, according to county 911 dispatchers.", "ts_dict_index": [12672, 12673, 12674]}
+{"event_id": 1113745, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2023-06-26 06:10:00", "end_date_time": "2023-06-26 06:10:00", "narrative": "An upper ridge of high pressure remained anchored over Central Mexico into west central Texas and Western Oklahoma on June 25th-26th. However, a weak surface front remained stationary from portions of Southeast Oklahoma into Western and Southwest Arkansas, as a shortwave trough rounding the top of the ridge axis shifted southeast along the stalled front. Ample surface and elevated instability and adequate moisture remained near this front, with large scale forcing associated with the trough enhancing scattered severe thunderstorm development across portions of McCurtain County Oklahoma into portions of extreme Northeast Texas, Southwest Arkansas, and much of Northwest Louisiana during the early morning hours of June 26th. Instances of large hail were reported initially, before transitioning to damaging winds as the storms accelerated into extreme Northeast Texas, Southwest Arkansas, and Northwest Louisiana. These storms then weakened as they exited the region by mid-morning. Tress and power lines downed in Minden.", "ts_dict_index": [12648, 12649, 12650]}
+{"event_id": 850054, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 18:45:00", "end_date_time": "2019-09-23 18:45:00", "narrative": "Copious amounts of tropical moisture interacted with a strong upper level low pressure system to produce scattered to numerous showers and thunderstorms across the greater Phoenix metropolitan area during the afternoon and evening hours on September 23rd. Although many of the thunderstorms generated heavy rain which led to flash flooding, a number of the stronger storms also produced large hail due to cooler temperatures in the upper atmosphere. Many places such as Scottsdale and central Phoenix reported hail ranging from one quarter of an inch to one inch or greater in diameter. Fortunately there were few if any reports of damage due to the larger hail. Some of the storms also generated gusty and damaging outflow winds in excess of 50 mph. At 1410MST the public reported multiple large trees downed near Fountain Hills and at 1845MST broadcast media reported that very strong winds uprooted a tree and sent it into a kitchen window about 2 miles east of Paradise Valley. Scattered to numerous showers and thunderstorms developed across the greater Phoenix area, affecting communities such as Paradise Valley and Scottsdale. In addition to very heavy rain, some of the stronger storms generated gusty and damaging outflow winds. According to a report from local broadcast media, at 1845MST winds estimated to be at least 60 mph in strength uprooted a tree about 2 miles east of Paradise Valley. The tree had an estimated diameter of 6 inches, and was thrown into a kitchen window by the strong gusts. The damage occurred near the Indian Bend Wash, just north of the intersection of Hayden Road and McDonald Drive. There were no reports of injuries.", "ts_dict_index": [12663, 12664, 12665]}
+{"event_id": 956924, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-01-25 13:20:00", "end_date_time": "2021-01-25 13:20:00", "narrative": "A pair of winter storm systems moved across Arizona January 24 through 26. The first brought moderate snow accumulations to several mountain ranges above 6000 feet on January 24. Mt. Lemmon Highway was closed at the base as a result. Thunderstorms produced hail and gusty winds at lower elevations. The second storm brought widespread heavy snow to southeast Arizona above 3500 feet, and even brought slushy  snow accumulations and slippery road conditions to parts of the greater Tucson Metro area. The bulk of the snow fell from the evening of January 25 through the morning of January 26, and was accompanied at times by wind gusts of 35 to 45 mph.  Snow accumulations of 3 to 6 inches occurred between 3500 and 5000 feet with 6 to 12 inches from 5000 to 7000 feet and 12 to 20 inches above 7000 feet. The additional snow forced the closure of Mt. Lemmon Highway near Tucson to continue, and also triggered closures of Highway 191 north of Hannagan Meadow and Route 80 near Bisbee. Thunderstorm winds caused minor roof damage to a home in North Komelik.  Rain caused further damage inside the home.", "ts_dict_index": [12654, 12655, 12656]}
+{"event_id": 850056, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2019-09-23 14:38:00", "end_date_time": "2019-09-23 14:38:00", "narrative": "Copious amounts of tropical moisture interacted with a strong upper level low pressure system to produce scattered to numerous showers and thunderstorms across the greater Phoenix metropolitan area during the afternoon and evening hours on September 23rd. Although many of the thunderstorms generated heavy rain which led to flash flooding, a number of the stronger storms also produced large hail due to cooler temperatures in the upper atmosphere. Many places such as Scottsdale and central Phoenix reported hail ranging from one quarter of an inch to one inch or greater in diameter. Fortunately there were few if any reports of damage due to the larger hail. Some of the storms also generated gusty and damaging outflow winds in excess of 50 mph. At 1410MST the public reported multiple large trees downed near Fountain Hills and at 1845MST broadcast media reported that very strong winds uprooted a tree and sent it into a kitchen window about 2 miles east of Paradise Valley. Scattered to numerous showers and thunderstorms developed across eastern portions of the greater Phoenix during the morning and afternoon hours on September 23rd. In addition to locally heavy rain which led to flash flooding, some of the storms produced gusty and damaging outflow winds which impacted the community of Apache Junction. According to a report from the public, at 1438MST gusty winds estimated to be upwards of 55 mph blew shingles off the roof of a home located about one mile east of Apache Junction. The damage occurred north of Broadway Road and near the Apache Trail.", "ts_dict_index": [12660, 12661, 12662]}
+{"event_id": 850787, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 06:45:00", "end_date_time": "2019-09-23 06:45:00", "narrative": "Copious amounts of tropical moisture interacted with a strong upper level low pressure system to produce scattered to numerous showers and thunderstorms across the greater Phoenix metropolitan area during the afternoon and evening hours on September 23rd. Although many of the thunderstorms generated heavy rain which led to flash flooding, a number of the stronger storms also produced large hail due to cooler temperatures in the upper atmosphere. Many places such as Scottsdale and central Phoenix reported hail ranging from one quarter of an inch to one inch or greater in diameter. Fortunately there were few if any reports of damage due to the larger hail. Some of the storms also generated gusty and damaging outflow winds in excess of 50 mph. At 1410MST the public reported multiple large trees downed near Fountain Hills and at 1845MST broadcast media reported that very strong winds uprooted a tree and sent it into a kitchen window about 2 miles east of Paradise Valley. Scattered to numerous thunderstorms developed across the central and northern portions of the greater Phoenix area during the afternoon hours on September 23rd. Although most of the storms generated very heavy rain, leading to multiple flash flood events, a few of the storms did produce gusty and damaging outflow winds. One such storm impacted the north Scottsdale area. According to a report from local broadcast media, gusty winds estimated to be as high as 60 mph uprooted a large tree about 3.5 miles north of Scottsdale. The uprooted tree was near the Indian Bend Wash, just to the west of Hayden Road.", "ts_dict_index": [12666, 12667, 12668]}
+{"event_id": 1052138, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-01 20:34:00", "end_date_time": "2022-09-01 20:34:00", "narrative": "Under a classic setup for storm motion from the Mogollon Rim to the Valley (Rim-to-Valley), with the monsoon 500mb high positioned over Nevada, a multicell storm cluster descended out of the White Mountains, through Gila County, and into the lower deserts of Maricopa and Pinal Counties in the early overnight hours of the 1st. Moisture levels were near average for the time of year, but steep mid level lapse rates over the high terrain (7-8 C/km) and modest shear (Sfc-6km around 20-25 kts) was sufficient to support the development of an organized multicell storm cluster. The environment was also supportive of strong downbursts, with DCAPE up around 1000-1500 J/kg. A single ordinary storm also developed in the Queen Creek/San Tan Valley area a couple hours before the multicell cluster moved into the lower deserts, and produced a damaging downburst. Strong winds leading to a dust storm was eventually generated by the multicell cluster once it moved into Maricopa and Pinal Counties. A bus barn at Poston Butte High School had two 3X70 foot pieces of sheet metal roofing peeled off in a downburst. A stack of wooden pallets was reportedly tossed 150 feet and there was at least minor damage to other equipment and supplies. A light pole, rusted near the base, also toppled over at the high school. Wind speeds estimated around 55-60 mph and timing based on radar. No injuries were reported.", "ts_dict_index": [12597, 12598, 12599]}
+{"event_id": 834604, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-06-28 18:25:00", "end_date_time": "2019-06-28 18:25:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. The county DOT office reported single trees down on Talley Cavey Road and Wildwood Road.  Time of occurrence was estimated from radar.", "ts_dict_index": [12681, 12682, 12683]}
+{"event_id": 834610, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-06-28 19:28:00", "end_date_time": "2019-06-28 19:28:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. A social media user reported that trees were blown down just west of Crafton.", "ts_dict_index": [12678, 12679, 12680]}
+{"event_id": 834624, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-06-29 16:21:00", "end_date_time": "2019-06-29 16:21:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. A trained spotter reported that several trees were blown down in Bell Acres.", "ts_dict_index": [12684, 12685, 12686]}
+{"event_id": 946628, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-04-09 21:55:00", "end_date_time": "2021-04-09 21:55:00", "narrative": "A strong upper trough dove southeast across the Northern and Central Plains on April 9th, reinforcing a cold front southeast into the Southern Plains. The approach of this storm system enhanced a southerly low level jet, which allowed for the return of a warm front north across East Texas, North Louisiana, Southern Arkansas, and extreme Southeast Oklahoma resulting in very warm, humid, and unstable air in advance of the front. The combination of this increasing instability, wind shear, and strong forcing ahead of the cold front and associated upper level storm system resulted in a prolonged period of severe thunderstorms across much of the region, with these storms affecting McCurtain County Oklahoma along the cold front during the late evening hours. Damaging winds were measured at 70 mph from the Idabel Mesonet station, with golfball size hail falling in the Harris community, before exiting the county to the southeast just prior to midnight with the passage of the cold front. The Idabel Mesonet station measured a 70 mph thunderstorm wind gust.", "ts_dict_index": [12612, 12613, 12614]}
+{"event_id": 939687, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2021-02-28 15:32:00", "end_date_time": "2021-02-28 15:32:00", "narrative": "Heavy rain brought flash flooding to parts of Arkansas on February the 28th. By the 28th, thermometers were in the mid to upper 70s across the central and southern counties. It was 76 degrees at Little Rock (Pulaski County) and Monticello (Drew County). It certainly felt like spring, and thunderstorms were back in the forecast.||Storms were sparked by a new cold front that penetrated into northwest Arkansas by lunchtime on the 28th, and approached the Louisiana border toward evening. Along the way, downpours were widespread, and there was at least a concern for severe weather (damaging winds, large hail, and maybe a tornado or two).||In the end, this was mainly a heavy rain event. Roads were flooded in Malvern (Hot Spring County), Pine Bluff (Jefferson County), and Sheridan (Grant County). Severe storms were few, with trees blown down at Greenbrier (Faulkner County) and Olmstead (Pulaski County), and nickel size hail just west of Wooster (Faulkner County). A large tree was blown down near Highway 89. The time was estimated and based on radar data.", "ts_dict_index": [12708, 12709, 12710]}
+{"event_id": 834623, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-06-29 16:20:00", "end_date_time": "2019-06-29 16:20:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. A social media user reported that several trees were blown down in Walter Panek Park.", "ts_dict_index": [12687, 12688, 12689]}
+{"event_id": 832959, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2019-07-10 19:50:00", "end_date_time": "2019-07-10 19:50:00", "narrative": "A weak upper trough shifted east across the High Plains/Upper Midwest during July 10th, with the tail end of this trough pushing southeast into Eastern Oklahoma and Northern Arkansas. This upper trough helped nudge a weak cool front south across Central and Eastern Oklahoma into Central Arkansas on the 10th, with compressional warming ahead of the front allowing for temperatures to climb into the middle 90s across Southeast Oklahoma, Southwest Arkansas, and East Texas. With a moist air mass already in place, moderate to high amounts of instability developed ahead of the front, with large scale forcing adequate enough near the weak front/upper trough to result in a band of strong to severe thunderstorms developing by mid and late afternoon across Southeast Oklahoma and Western Arkansas, which shifted south into East Texas during the evening. These storms produced damaging winds, which downed trees at various locations across East Texas before diminishing late. A tree was blown down onto a home in the Deer Run subdivision of Chapel Hill.", "ts_dict_index": [12702, 12703, 12704]}
+{"event_id": 834622, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-06-29 16:20:00", "end_date_time": "2019-06-29 16:20:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. Trees were blown down in Leetsdale, according to county 911 dispatchers.", "ts_dict_index": [12690, 12691, 12692]}
+{"event_id": 834625, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2019-06-29 16:25:00", "end_date_time": "2019-06-29 16:25:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. A county 911 dispatcher reported that a tree was down and partially blocking State Route 65.", "ts_dict_index": [12693, 12694, 12695]}
+{"event_id": 832958, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-07-10 19:45:00", "end_date_time": "2019-07-10 19:45:00", "narrative": "A weak upper trough shifted east across the High Plains/Upper Midwest during July 10th, with the tail end of this trough pushing southeast into Eastern Oklahoma and Northern Arkansas. This upper trough helped nudge a weak cool front south across Central and Eastern Oklahoma into Central Arkansas on the 10th, with compressional warming ahead of the front allowing for temperatures to climb into the middle 90s across Southeast Oklahoma, Southwest Arkansas, and East Texas. With a moist air mass already in place, moderate to high amounts of instability developed ahead of the front, with large scale forcing adequate enough near the weak front/upper trough to result in a band of strong to severe thunderstorms developing by mid and late afternoon across Southeast Oklahoma and Western Arkansas, which shifted south into East Texas during the evening. These storms produced damaging winds, which downed trees at various locations across East Texas before diminishing late. A tree was downed at the intersection of Highway 259 and County Road 236 (Brown Road) between Henderson and Kilgore.", "ts_dict_index": [12705, 12706, 12707]}
+{"event_id": 1104150, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-10 12:30:00", "end_date_time": "2023-06-10 12:30:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. Numerous trees downed in the Tatum area.", "ts_dict_index": [12714, 12715, 12716]}
+{"event_id": 1104148, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-10 12:30:00", "end_date_time": "2023-06-10 12:30:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. Numerous trees downed in the Lake Cherokee area off of Farm to Market Road 1716.", "ts_dict_index": [12711, 12712, 12713]}
+{"event_id": 832960, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-07-10 20:15:00", "end_date_time": "2019-07-10 20:15:00", "narrative": "A weak upper trough shifted east across the High Plains/Upper Midwest during July 10th, with the tail end of this trough pushing southeast into Eastern Oklahoma and Northern Arkansas. This upper trough helped nudge a weak cool front south across Central and Eastern Oklahoma into Central Arkansas on the 10th, with compressional warming ahead of the front allowing for temperatures to climb into the middle 90s across Southeast Oklahoma, Southwest Arkansas, and East Texas. With a moist air mass already in place, moderate to high amounts of instability developed ahead of the front, with large scale forcing adequate enough near the weak front/upper trough to result in a band of strong to severe thunderstorms developing by mid and late afternoon across Southeast Oklahoma and Western Arkansas, which shifted south into East Texas during the evening. These storms produced damaging winds, which downed trees at various locations across East Texas before diminishing late. A tree was blown down across FM 1798 in front of the Laneville ISD campus.", "ts_dict_index": [12699, 12700, 12701]}
+{"event_id": 1103906, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-10 09:35:00", "end_date_time": "2023-06-10 09:35:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. A tree downed on Highway 3 near the Tom community.", "ts_dict_index": [12717, 12718, 12719]}
+{"event_id": 850055, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-09-23 14:10:00", "end_date_time": "2019-09-23 14:10:00", "narrative": "Copious amounts of tropical moisture interacted with a strong upper level low pressure system to produce scattered to numerous showers and thunderstorms across the greater Phoenix metropolitan area during the afternoon and evening hours on September 23rd. Although many of the thunderstorms generated heavy rain which led to flash flooding, a number of the stronger storms also produced large hail due to cooler temperatures in the upper atmosphere. Many places such as Scottsdale and central Phoenix reported hail ranging from one quarter of an inch to one inch or greater in diameter. Fortunately there were few if any reports of damage due to the larger hail. Some of the storms also generated gusty and damaging outflow winds in excess of 50 mph. At 1410MST the public reported multiple large trees downed near Fountain Hills and at 1845MST broadcast media reported that very strong winds uprooted a tree and sent it into a kitchen window about 2 miles east of Paradise Valley. Scattered to numerous showers and thunderstorms developed across the greater Phoenix area during the afternoon hours on September 23rd; in additions to very heavy rain some of the stronger storms generated gusty and damaging outflow winds that impacted communities such as Fountain Hills and Scottsdale. According to a report from the public, at 1410MST gusty winds estimated to be as high as 60 mph knocked down multiple trees about 5 miles southwest of Fountain Hills. The downed trees were located just to the northeast of Shea Boulevard and Frank Lloyd Wright Boulevard. No injuries occurred from the falling trees.", "ts_dict_index": [12657, 12658, 12659]}
+{"event_id": 1104309, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-10 11:45:00", "end_date_time": "2023-06-10 11:45:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. Trees downed near Rodessa.", "ts_dict_index": [12729, 12730, 12731]}
+{"event_id": 1110568, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-06-14 12:30:00", "end_date_time": "2023-06-14 12:30:00", "narrative": "Supercell thunderstorms developed toward midday across the middle Red River Valley along and south of a stalled frontal boundary. These thunderstorms progressed east southeast with upper 80s temperatures on the warm side of the boundary with dew points exceeding 75 degrees. Mid-level lapse rates of 7-8 C/km overspread this very moist low-level air mass over a rather broad west-to-east corridor, supporting extreme instability upwards of 4500 J/kg well downstream of the upscale-growing convection. Coinciding this corridor of extreme buoyancy was very strong effective bulk shear near 65 kts along with hodographs that were modestly curved at the low levels and elongated above 3 km AGL. Numerous local storm reports were documented of large hail and damaging wind gusts across parts of North Louisiana throughout the event. Unfortunately, a 73 year old male was killed in a fire ignited after lightning struck his home near Shongaloo in Northern Webster Parish. Numerous trees downed throughout Bossier Parish.", "ts_dict_index": [12744, 12745, 12746]}
+{"event_id": 1110569, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-06-14 12:30:00", "end_date_time": "2023-06-14 12:30:00", "narrative": "Supercell thunderstorms developed toward midday across the middle Red River Valley along and south of a stalled frontal boundary. These thunderstorms progressed east southeast with upper 80s temperatures on the warm side of the boundary with dew points exceeding 75 degrees. Mid-level lapse rates of 7-8 C/km overspread this very moist low-level air mass over a rather broad west-to-east corridor, supporting extreme instability upwards of 4500 J/kg well downstream of the upscale-growing convection. Coinciding this corridor of extreme buoyancy was very strong effective bulk shear near 65 kts along with hodographs that were modestly curved at the low levels and elongated above 3 km AGL. Numerous local storm reports were documented of large hail and damaging wind gusts across parts of North Louisiana throughout the event. Unfortunately, a 73 year old male was killed in a fire ignited after lightning struck his home near Shongaloo in Northern Webster Parish. Tree downed on top of a mobile home on Wise Road north of Plain Dealing.", "ts_dict_index": [12741, 12742, 12743]}
+{"event_id": 1110567, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-06-14 12:28:00", "end_date_time": "2023-06-14 12:28:00", "narrative": "Supercell thunderstorms developed toward midday across the middle Red River Valley along and south of a stalled frontal boundary. These thunderstorms progressed east southeast with upper 80s temperatures on the warm side of the boundary with dew points exceeding 75 degrees. Mid-level lapse rates of 7-8 C/km overspread this very moist low-level air mass over a rather broad west-to-east corridor, supporting extreme instability upwards of 4500 J/kg well downstream of the upscale-growing convection. Coinciding this corridor of extreme buoyancy was very strong effective bulk shear near 65 kts along with hodographs that were modestly curved at the low levels and elongated above 3 km AGL. Numerous local storm reports were documented of large hail and damaging wind gusts across parts of North Louisiana throughout the event. Unfortunately, a 73 year old male was killed in a fire ignited after lightning struck his home near Shongaloo in Northern Webster Parish. Trees and power lines downed north of Highway 2 along with damage to a mobile home.", "ts_dict_index": [12750, 12751, 12752]}
+{"event_id": 1104156, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-10 12:30:00", "end_date_time": "2023-06-10 12:30:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. Trees downed across Rusk County and one tree downed on a power line near County Road 2164.", "ts_dict_index": [12720, 12721, 12722]}
+{"event_id": 994076, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2021-12-10 20:24:00", "end_date_time": "2021-12-10 20:24:00", "narrative": "A powerful storm system developed and moved across the central Plains into the Mid-Mississippi Valley on Friday into Friday night. This storm complex brought a cold front through the state. Ahead of the cold front, in the open warm sector, near record warm temperatures, upper 70s/lower 80s, and elevated dew points, mid 60s to 70, were observed across Arkansas. This provided a warm and unstable environment and with favorable clockwise turning of winds with height, strong storms were expected to develop. Showers and thunderstorms did develop over portions of central Arkansas and trekked northeast into the evening. Storms organized over the aforementioned area, which went on to produce multiple tornadoes across northeast parts of Arkansas. This tornado activity continued into extreme northeast Arkansas, Missouri Bootheel, northwestern Tennessee, and Kentucky. Strong damaging winds and marginally severe hail also accompanied the storms over the state. A 64 mph wind gust was measured at Little Rock AFB.", "ts_dict_index": [12753, 12754, 12755]}
+{"event_id": 1104152, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2023-06-10 12:52:00", "end_date_time": "2023-06-10 12:52:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. Trees and power lines downed throughout Panola County.", "ts_dict_index": [12738, 12739, 12740]}
+{"event_id": 1104151, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-06-10 12:10:00", "end_date_time": "2023-06-10 12:10:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. Trees downed throughout Harrison County.", "ts_dict_index": [12735, 12736, 12737]}
+{"event_id": 1110566, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2023-06-14 12:50:00", "end_date_time": "2023-06-14 12:50:00", "narrative": "Supercell thunderstorms developed toward midday across the middle Red River Valley along and south of a stalled frontal boundary. These thunderstorms progressed east southeast with upper 80s temperatures on the warm side of the boundary with dew points exceeding 75 degrees. Mid-level lapse rates of 7-8 C/km overspread this very moist low-level air mass over a rather broad west-to-east corridor, supporting extreme instability upwards of 4500 J/kg well downstream of the upscale-growing convection. Coinciding this corridor of extreme buoyancy was very strong effective bulk shear near 65 kts along with hodographs that were modestly curved at the low levels and elongated above 3 km AGL. Numerous local storm reports were documented of large hail and damaging wind gusts across parts of North Louisiana throughout the event. Unfortunately, a 73 year old male was killed in a fire ignited after lightning struck his home near Shongaloo in Northern Webster Parish. Multiple trees downed along Highway 371 in Cotton Valley.", "ts_dict_index": [12747, 12748, 12749]}
+{"event_id": 1104428, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-06-10 14:40:00", "end_date_time": "2023-06-10 14:40:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. Several trees downed throughout Natchitoches Parish.", "ts_dict_index": [12732, 12733, 12734]}
+{"event_id": 1104377, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-06-10 14:40:00", "end_date_time": "2023-06-10 14:40:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. Trees downed near Highway 1226.", "ts_dict_index": [12723, 12724, 12725]}
+{"event_id": 834627, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2019-06-29 18:46:00", "end_date_time": "2019-06-29 18:46:00", "narrative": "Scattered thunderstorms formed in an unstable air mass on the 28th.  The storms took advantage of dry air aloft to create downburst conditions in a few cases, producing reports of wind damage in Allegheny, Lawrence, and Westmoreland Counties. Also, one to two inches of rain on already wet ground created flooding issues in portions of western Lawrence County. ||A lull in activity occurred during the night and into the following morning.  Later in the day, renewed instability, plus residual outflow boundaries from previous convection, helped to expand thunderstorm coverage during the evening of the 29th and into the early morning hours of the 30th ahead of a sagging cold front.   Steep lapse rates and dry air aloft supported many instances of thunderstorms with damaging wind.  Damage was mainly to trees, but there were a few instances of roof damage in Washington County.  Hail was much less widespread, but a few reports of dime to quarter sized hail were received. A social media user stated that trees were downed between Stahlstown and Ligonier.", "ts_dict_index": [12696, 12697, 12698]}
+{"event_id": 834155, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-06-19 20:46:00", "end_date_time": "2019-06-19 20:46:00", "narrative": "Severe weather returned on the 19th, and one of the largest severe weather events in Arkansas of 2019 unfolded. The event began with softball size hail or larger around Vandervoort and Cove (both in Polk County) between 630 pm and 700 pm CDT. Evidence from photos showed that some hailstones were close to five inches in diameter, potentially tying the state record set on January 21, 1999 and April 2, 2006. Records go back to the 1950s.||As the evening progressed, two clusters of storms evolved across the central and southern counties. They moved quickly to the east at 50 to more than 60 mph. This usually increases the chances of wind damage.||Trees and/or power lines were downed at many locations including Camden (Ouachita County), Harrell (Calhoun County), Little Rock (Pulaski County), Mount Ida and Norman (both in Montgomery County), Cabot and Lonoke (both in Lonoke County), Florence and Montongo (both in Drew County), and McGehee (Desha County). Trees were blown down along Jim Hall Rd. near Old Tom Box Rd.", "ts_dict_index": [12768, 12769, 12770]}
+{"event_id": 834145, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-06-19 20:11:00", "end_date_time": "2019-06-19 20:11:00", "narrative": "Severe weather returned on the 19th, and one of the largest severe weather events in Arkansas of 2019 unfolded. The event began with softball size hail or larger around Vandervoort and Cove (both in Polk County) between 630 pm and 700 pm CDT. Evidence from photos showed that some hailstones were close to five inches in diameter, potentially tying the state record set on January 21, 1999 and April 2, 2006. Records go back to the 1950s.||As the evening progressed, two clusters of storms evolved across the central and southern counties. They moved quickly to the east at 50 to more than 60 mph. This usually increases the chances of wind damage.||Trees and/or power lines were downed at many locations including Camden (Ouachita County), Harrell (Calhoun County), Little Rock (Pulaski County), Mount Ida and Norman (both in Montgomery County), Cabot and Lonoke (both in Lonoke County), Florence and Montongo (both in Drew County), and McGehee (Desha County). A 60 MPH wind gust was measured on Pinnacle Valley Rd.", "ts_dict_index": [12771, 12772, 12773]}
+{"event_id": 834151, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-06-19 20:38:00", "end_date_time": "2019-06-19 20:38:00", "narrative": "Severe weather returned on the 19th, and one of the largest severe weather events in Arkansas of 2019 unfolded. The event began with softball size hail or larger around Vandervoort and Cove (both in Polk County) between 630 pm and 700 pm CDT. Evidence from photos showed that some hailstones were close to five inches in diameter, potentially tying the state record set on January 21, 1999 and April 2, 2006. Records go back to the 1950s.||As the evening progressed, two clusters of storms evolved across the central and southern counties. They moved quickly to the east at 50 to more than 60 mph. This usually increases the chances of wind damage.||Trees and/or power lines were downed at many locations including Camden (Ouachita County), Harrell (Calhoun County), Little Rock (Pulaski County), Mount Ida and Norman (both in Montgomery County), Cabot and Lonoke (both in Lonoke County), Florence and Montongo (both in Drew County), and McGehee (Desha County). Tree limbs were blown down in Argenta.", "ts_dict_index": [12765, 12766, 12767]}
+{"event_id": 834156, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-06-19 20:48:00", "end_date_time": "2019-06-19 20:48:00", "narrative": "Severe weather returned on the 19th, and one of the largest severe weather events in Arkansas of 2019 unfolded. The event began with softball size hail or larger around Vandervoort and Cove (both in Polk County) between 630 pm and 700 pm CDT. Evidence from photos showed that some hailstones were close to five inches in diameter, potentially tying the state record set on January 21, 1999 and April 2, 2006. Records go back to the 1950s.||As the evening progressed, two clusters of storms evolved across the central and southern counties. They moved quickly to the east at 50 to more than 60 mph. This usually increases the chances of wind damage.||Trees and/or power lines were downed at many locations including Camden (Ouachita County), Harrell (Calhoun County), Little Rock (Pulaski County), Mount Ida and Norman (both in Montgomery County), Cabot and Lonoke (both in Lonoke County), Florence and Montongo (both in Drew County), and McGehee (Desha County). A trained spotter reported 70 mph thunderstorm wind gust.", "ts_dict_index": [12762, 12763, 12764]}
+{"event_id": 834152, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-06-19 20:41:00", "end_date_time": "2019-06-19 20:41:00", "narrative": "Severe weather returned on the 19th, and one of the largest severe weather events in Arkansas of 2019 unfolded. The event began with softball size hail or larger around Vandervoort and Cove (both in Polk County) between 630 pm and 700 pm CDT. Evidence from photos showed that some hailstones were close to five inches in diameter, potentially tying the state record set on January 21, 1999 and April 2, 2006. Records go back to the 1950s.||As the evening progressed, two clusters of storms evolved across the central and southern counties. They moved quickly to the east at 50 to more than 60 mph. This usually increases the chances of wind damage.||Trees and/or power lines were downed at many locations including Camden (Ouachita County), Harrell (Calhoun County), Little Rock (Pulaski County), Mount Ida and Norman (both in Montgomery County), Cabot and Lonoke (both in Lonoke County), Florence and Montongo (both in Drew County), and McGehee (Desha County). Numerous trees and power lines were down.", "ts_dict_index": [12759, 12760, 12761]}
+{"event_id": 834143, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-06-19 20:03:00", "end_date_time": "2019-06-19 20:03:00", "narrative": "Severe weather returned on the 19th, and one of the largest severe weather events in Arkansas of 2019 unfolded. The event began with softball size hail or larger around Vandervoort and Cove (both in Polk County) between 630 pm and 700 pm CDT. Evidence from photos showed that some hailstones were close to five inches in diameter, potentially tying the state record set on January 21, 1999 and April 2, 2006. Records go back to the 1950s.||As the evening progressed, two clusters of storms evolved across the central and southern counties. They moved quickly to the east at 50 to more than 60 mph. This usually increases the chances of wind damage.||Trees and/or power lines were downed at many locations including Camden (Ouachita County), Harrell (Calhoun County), Little Rock (Pulaski County), Mount Ida and Norman (both in Montgomery County), Cabot and Lonoke (both in Lonoke County), Florence and Montongo (both in Drew County), and McGehee (Desha County). Trees were blown down. Some were down on power lines and one fell on a shed.", "ts_dict_index": [12774, 12775, 12776]}
+{"event_id": 1113489, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-23 18:25:00", "end_date_time": "2023-06-23 18:25:00", "narrative": "Scattered strong to severe thunderstorms developed across parts of East Texas on the afternoon of June 23rd, aided by forcing for ascent from weak warm air advection and downstream of a significant but weakening cluster of storms shifting southeast from the middle Red River Valley. This was also focused along the eastern periphery of a plume of warm, capping elevated mixed-layer air, which supported instability up to 4000 J/kg for boundary layer moisture characterized by mid 70s dew points. Under 25-30 knots of northwesterly flow around 500 millibars, deep-layer shear was marginally supportive for the evolution of supercells, and an upscale growing organized cluster as convective inhibition weakened in the peak late afternoon heating. The environment was at least conditionally supportive of large hail and increasing damaging winds, which ultimately occurred across parts of Rusk County and adjacent Panola County with multiple local storm reports. Multiple trees downed along State Highway 323, making it impassable between Henderson and New London.", "ts_dict_index": [12783, 12784, 12785]}
+{"event_id": 1113488, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-23 16:09:00", "end_date_time": "2023-06-23 16:09:00", "narrative": "Scattered strong to severe thunderstorms developed across parts of East Texas on the afternoon of June 23rd, aided by forcing for ascent from weak warm air advection and downstream of a significant but weakening cluster of storms shifting southeast from the middle Red River Valley. This was also focused along the eastern periphery of a plume of warm, capping elevated mixed-layer air, which supported instability up to 4000 J/kg for boundary layer moisture characterized by mid 70s dew points. Under 25-30 knots of northwesterly flow around 500 millibars, deep-layer shear was marginally supportive for the evolution of supercells, and an upscale growing organized cluster as convective inhibition weakened in the peak late afternoon heating. The environment was at least conditionally supportive of large hail and increasing damaging winds, which ultimately occurred across parts of Rusk County and adjacent Panola County with multiple local storm reports. Tree downed onto a home on Forrest Street.", "ts_dict_index": [12786, 12787, 12788]}
+{"event_id": 1113494, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-23 18:33:00", "end_date_time": "2023-06-23 18:33:00", "narrative": "Scattered strong to severe thunderstorms developed across parts of East Texas on the afternoon of June 23rd, aided by forcing for ascent from weak warm air advection and downstream of a significant but weakening cluster of storms shifting southeast from the middle Red River Valley. This was also focused along the eastern periphery of a plume of warm, capping elevated mixed-layer air, which supported instability up to 4000 J/kg for boundary layer moisture characterized by mid 70s dew points. Under 25-30 knots of northwesterly flow around 500 millibars, deep-layer shear was marginally supportive for the evolution of supercells, and an upscale growing organized cluster as convective inhibition weakened in the peak late afternoon heating. The environment was at least conditionally supportive of large hail and increasing damaging winds, which ultimately occurred across parts of Rusk County and adjacent Panola County with multiple local storm reports. Significant roof damage to a home, and a tree downed onto an RV on adjacent property along County Road 382.", "ts_dict_index": [12777, 12778, 12779]}
+{"event_id": 1113492, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-23 18:45:00", "end_date_time": "2023-06-23 18:45:00", "narrative": "Scattered strong to severe thunderstorms developed across parts of East Texas on the afternoon of June 23rd, aided by forcing for ascent from weak warm air advection and downstream of a significant but weakening cluster of storms shifting southeast from the middle Red River Valley. This was also focused along the eastern periphery of a plume of warm, capping elevated mixed-layer air, which supported instability up to 4000 J/kg for boundary layer moisture characterized by mid 70s dew points. Under 25-30 knots of northwesterly flow around 500 millibars, deep-layer shear was marginally supportive for the evolution of supercells, and an upscale growing organized cluster as convective inhibition weakened in the peak late afternoon heating. The environment was at least conditionally supportive of large hail and increasing damaging winds, which ultimately occurred across parts of Rusk County and adjacent Panola County with multiple local storm reports. Roofs removed from several carports and sheds in Mount Enterprise.", "ts_dict_index": [12780, 12781, 12782]}
+{"event_id": 1111488, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:19:00", "end_date_time": "2023-06-14 20:19:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down onto Thomasville Road near Horseshoe Plantation Road in the southbound lane.", "ts_dict_index": [12804, 12805, 12806]}
+{"event_id": 1112011, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-21 09:14:00", "end_date_time": "2023-06-21 09:14:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down near Chaires Cross Road and Hill N Barnes Lane.", "ts_dict_index": [12798, 12799, 12800]}
+{"event_id": 1111609, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-17 17:20:00", "end_date_time": "2023-06-17 17:20:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. Trees were blown down across the intersection of Old St Augustine Road and Miners Road.", "ts_dict_index": [12795, 12796, 12797]}
+{"event_id": 1111501, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:20:00", "end_date_time": "2023-06-14 20:20:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down onto a house on Pimlico Dr.", "ts_dict_index": [12816, 12817, 12818]}
+{"event_id": 1111486, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:15:00", "end_date_time": "2023-06-14 20:15:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down onto a house on Caracus Ct.", "ts_dict_index": [12810, 12811, 12812]}
+{"event_id": 1112009, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-21 08:11:00", "end_date_time": "2023-06-21 08:11:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A large tree was blown down and blocking Meridian Road at Sinclair Road.", "ts_dict_index": [12819, 12820, 12821]}
+{"event_id": 1111616, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-17 17:30:00", "end_date_time": "2023-06-17 17:30:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. Multiple trees were blown down on Miccosukee Road causing several cars to be trapped on the roadway.", "ts_dict_index": [12807, 12808, 12809]}
+{"event_id": 1111649, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-22 20:58:00", "end_date_time": "2023-06-22 20:58:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A power line was blown down along County Road 12.", "ts_dict_index": [12801, 12802, 12803]}
+{"event_id": 1113491, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-06-23 18:27:00", "end_date_time": "2023-06-23 18:27:00", "narrative": "Scattered strong to severe thunderstorms developed across parts of East Texas on the afternoon of June 23rd, aided by forcing for ascent from weak warm air advection and downstream of a significant but weakening cluster of storms shifting southeast from the middle Red River Valley. This was also focused along the eastern periphery of a plume of warm, capping elevated mixed-layer air, which supported instability up to 4000 J/kg for boundary layer moisture characterized by mid 70s dew points. Under 25-30 knots of northwesterly flow around 500 millibars, deep-layer shear was marginally supportive for the evolution of supercells, and an upscale growing organized cluster as convective inhibition weakened in the peak late afternoon heating. The environment was at least conditionally supportive of large hail and increasing damaging winds, which ultimately occurred across parts of Rusk County and adjacent Panola County with multiple local storm reports. Power lines and large tree limbs downed in Henderson.", "ts_dict_index": [12792, 12793, 12794]}
+{"event_id": 1113493, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2023-06-23 18:43:00", "end_date_time": "2023-06-23 18:43:00", "narrative": "Scattered strong to severe thunderstorms developed across parts of East Texas on the afternoon of June 23rd, aided by forcing for ascent from weak warm air advection and downstream of a significant but weakening cluster of storms shifting southeast from the middle Red River Valley. This was also focused along the eastern periphery of a plume of warm, capping elevated mixed-layer air, which supported instability up to 4000 J/kg for boundary layer moisture characterized by mid 70s dew points. Under 25-30 knots of northwesterly flow around 500 millibars, deep-layer shear was marginally supportive for the evolution of supercells, and an upscale growing organized cluster as convective inhibition weakened in the peak late afternoon heating. The environment was at least conditionally supportive of large hail and increasing damaging winds, which ultimately occurred across parts of Rusk County and adjacent Panola County with multiple local storm reports. Trees and power lines downed on County Road 186.", "ts_dict_index": [12789, 12790, 12791]}
+{"event_id": 1104311, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2023-06-10 14:10:00", "end_date_time": "2023-06-10 14:10:00", "narrative": "A Mesoscale Convective System (MCS) developed during the late afternoon and early evening hours on June 9th over Western and Central Kansas, near a shortwave trough that drifted east-southeast into the Southern Plains that evening. While this complex of storms weakened as it moved through Oklahoma during the overnight hours, showers and thunderstorms associated with the remnants of these storms re-intensified by mid and late morning on the 10th across extreme Southeast Oklahoma and Northeast Texas as moderate instability developed with the onset of daytime heating ahead of the trough. Despite the weak shear in place, these storms were able to organize into another MCS as it moved through East Texas and North Louisiana during the afternoon hours, producing multiple reports of damaging winds which downed trees and power lines, as well as isolated instances of large hail before exiting the region into Southeast Texas and Central Louisiana by early evening. Tree downed northwest of Sterlington.", "ts_dict_index": [12726, 12727, 12728]}
+{"event_id": 1111652, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-23 18:50:00", "end_date_time": "2023-06-23 18:50:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down near Centerville Road and Pimlico Dr.", "ts_dict_index": [12822, 12823, 12824]}
+{"event_id": 834149, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-06-19 20:25:00", "end_date_time": "2019-06-19 20:25:00", "narrative": "Severe weather returned on the 19th, and one of the largest severe weather events in Arkansas of 2019 unfolded. The event began with softball size hail or larger around Vandervoort and Cove (both in Polk County) between 630 pm and 700 pm CDT. Evidence from photos showed that some hailstones were close to five inches in diameter, potentially tying the state record set on January 21, 1999 and April 2, 2006. Records go back to the 1950s.||As the evening progressed, two clusters of storms evolved across the central and southern counties. They moved quickly to the east at 50 to more than 60 mph. This usually increases the chances of wind damage.||Trees and/or power lines were downed at many locations including Camden (Ouachita County), Harrell (Calhoun County), Little Rock (Pulaski County), Mount Ida and Norman (both in Montgomery County), Cabot and Lonoke (both in Lonoke County), Florence and Montongo (both in Drew County), and McGehee (Desha County). A tree was snapped along Shelby Rd. in Sherwood.", "ts_dict_index": [12756, 12757, 12758]}
+{"event_id": 1112008, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-21 08:03:00", "end_date_time": "2023-06-21 08:03:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A large tree was blown down and blocking Meridian Road at Waverly Road.", "ts_dict_index": [12861, 12862, 12863]}
+{"event_id": 1111618, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-17 17:40:00", "end_date_time": "2023-06-17 17:40:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down at 15978 Mahan Drive.", "ts_dict_index": [12855, 12856, 12857]}
+{"event_id": 1111491, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:20:00", "end_date_time": "2023-06-14 20:20:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down onto Old Bainbridge Road near Homewood Road.", "ts_dict_index": [12828, 12829, 12830]}
+{"event_id": 1111502, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:23:00", "end_date_time": "2023-06-14 20:23:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. Trees were blown onto power lines along E Call St and Belmont Road.", "ts_dict_index": [12840, 12841, 12842]}
+{"event_id": 1111489, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:19:00", "end_date_time": "2023-06-14 20:19:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down near Swatts Road and N Monroe St.", "ts_dict_index": [12834, 12835, 12836]}
+{"event_id": 1111653, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-23 18:50:00", "end_date_time": "2023-06-23 18:50:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down near Centerville Road and McLaughlin Dr.", "ts_dict_index": [12870, 12871, 12872]}
+{"event_id": 1111517, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:37:00", "end_date_time": "2023-06-14 20:37:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down onto power lines along Old Plank Road near Natural Bridge Road.", "ts_dict_index": [12825, 12826, 12827]}
+{"event_id": 1111621, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-17 17:54:00", "end_date_time": "2023-06-17 17:54:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. Delete.", "ts_dict_index": [12864, 12865, 12866]}
+{"event_id": 1111635, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-19 09:00:00", "end_date_time": "2023-06-19 09:00:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. Tree debris was in the roadway at the 2300 block of Centerville Road.", "ts_dict_index": [12858, 12859, 12860]}
+{"event_id": 1111615, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-17 17:25:00", "end_date_time": "2023-06-17 17:25:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down at the intersection of Baum Road and Wadesboro Rd.", "ts_dict_index": [12843, 12844, 12845]}
+{"event_id": 1111507, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:32:00", "end_date_time": "2023-06-14 20:32:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down onto the road near Southern Park Dr and Oak Ridge Rd.", "ts_dict_index": [12852, 12853, 12854]}
+{"event_id": 1111613, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-17 17:25:00", "end_date_time": "2023-06-17 17:25:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down at the intersection of Veterans Memorial Drive and Mahan Drive.", "ts_dict_index": [12837, 12838, 12839]}
+{"event_id": 1111636, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-19 09:00:00", "end_date_time": "2023-06-19 09:00:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down onto power lines along Buck Lake Road just east of Walden Road.", "ts_dict_index": [12831, 12832, 12833]}
+{"event_id": 1111503, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:25:00", "end_date_time": "2023-06-14 20:25:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down onto Woodville Highway near Longevity Ln.", "ts_dict_index": [12867, 12868, 12869]}
+{"event_id": 1111608, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-17 17:15:00", "end_date_time": "2023-06-17 17:15:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. Six trees were blown down.", "ts_dict_index": [12873, 12874, 12875]}
+{"event_id": 1111617, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-17 17:30:00", "end_date_time": "2023-06-17 17:30:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down at the intersection of Miccosukee Road and Wiley Road.", "ts_dict_index": [12813, 12814, 12815]}
+{"event_id": 1111487, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:16:00", "end_date_time": "2023-06-14 20:16:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down onto Old Bainbridge Road near Westbury Dr.", "ts_dict_index": [12882, 12883, 12884]}
+{"event_id": 1111614, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-17 17:25:00", "end_date_time": "2023-06-17 17:25:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down at 15978 Mahan Dr.", "ts_dict_index": [12885, 12886, 12887]}
+{"event_id": 1111492, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:20:00", "end_date_time": "2023-06-14 20:20:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down onto Jackson Bluff Rd near Jacqueline Ln.", "ts_dict_index": [12888, 12889, 12890]}
+{"event_id": 1111499, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-14 20:20:00", "end_date_time": "2023-06-14 20:20:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down with power line onto the roadway at Springhill Road near Cox Road.", "ts_dict_index": [12876, 12877, 12878]}
+{"event_id": 1111654, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-23 19:00:00", "end_date_time": "2023-06-23 19:00:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down near Mahan and Baum Road.", "ts_dict_index": [12879, 12880, 12881]}
+{"event_id": 1111632, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-19 08:50:00", "end_date_time": "2023-06-19 08:50:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down across Mahan at Phillips.", "ts_dict_index": [12849, 12850, 12851]}
+{"event_id": 1111612, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-17 17:25:00", "end_date_time": "2023-06-17 17:25:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down at the intersection of Baum Road and Mahan Drive.", "ts_dict_index": [12891, 12892, 12893]}
+{"event_id": 927640, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-11-15 15:03:00", "end_date_time": "2020-11-15 15:03:00", "narrative": "A shortwave trough axis lifted quickly across the Great Lakes and the Upper Ohio Valley on November 15th, taking on a negative tilt as it did so. Deepening surface low pressure tracked across Michigan and into Ontario during the day, whipping a cold front across the region during the late morning and early afternoon. Some of the classic ingredients for a widespread wind event were present, including a negatively- tilted trough, jet positioning over the region, and a favorable Great Lakes surface low track. Strong post-frontal 3 hour pressure rises of 5-7 mb were observed, and a low-topped mostly lightning-free convective line accompanied the boundary. Widespread wind gusts of at least 45-55 MPH were observed, with several higher measured gusts seen. Along the convective line, gusts of 55-65 MPH likely occurred. This resulted in widespread reports of wind damage to trees and power lines, with a few instances of mostly minor structural damage. Trees were reported to be uprooted.", "ts_dict_index": [12912, 12913, 12914]}
+{"event_id": 927622, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-11-15 14:52:00", "end_date_time": "2020-11-15 14:52:00", "narrative": "A shortwave trough axis lifted quickly across the Great Lakes and the Upper Ohio Valley on November 15th, taking on a negative tilt as it did so. Deepening surface low pressure tracked across Michigan and into Ontario during the day, whipping a cold front across the region during the late morning and early afternoon. Some of the classic ingredients for a widespread wind event were present, including a negatively- tilted trough, jet positioning over the region, and a favorable Great Lakes surface low track. Strong post-frontal 3 hour pressure rises of 5-7 mb were observed, and a low-topped mostly lightning-free convective line accompanied the boundary. Widespread wind gusts of at least 45-55 MPH were observed, with several higher measured gusts seen. Along the convective line, gusts of 55-65 MPH likely occurred. This resulted in widespread reports of wind damage to trees and power lines, with a few instances of mostly minor structural damage. In Mount Lebanon and South Park, trees and wires were blown down.  A tree hit a fire hydrant on Beadling Road and caused damage to it.", "ts_dict_index": [12894, 12895, 12896]}
+{"event_id": 927656, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-11-15 15:34:00", "end_date_time": "2020-11-15 15:34:00", "narrative": "A shortwave trough axis lifted quickly across the Great Lakes and the Upper Ohio Valley on November 15th, taking on a negative tilt as it did so. Deepening surface low pressure tracked across Michigan and into Ontario during the day, whipping a cold front across the region during the late morning and early afternoon. Some of the classic ingredients for a widespread wind event were present, including a negatively- tilted trough, jet positioning over the region, and a favorable Great Lakes surface low track. Strong post-frontal 3 hour pressure rises of 5-7 mb were observed, and a low-topped mostly lightning-free convective line accompanied the boundary. Widespread wind gusts of at least 45-55 MPH were observed, with several higher measured gusts seen. Along the convective line, gusts of 55-65 MPH likely occurred. This resulted in widespread reports of wind damage to trees and power lines, with a few instances of mostly minor structural damage. Widespread wind damage, along with trees and wires down, was reported across Westmoreland County.", "ts_dict_index": [12906, 12907, 12908]}
+{"event_id": 927621, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2020-11-15 14:45:00", "end_date_time": "2020-11-15 14:45:00", "narrative": "A shortwave trough axis lifted quickly across the Great Lakes and the Upper Ohio Valley on November 15th, taking on a negative tilt as it did so. Deepening surface low pressure tracked across Michigan and into Ontario during the day, whipping a cold front across the region during the late morning and early afternoon. Some of the classic ingredients for a widespread wind event were present, including a negatively- tilted trough, jet positioning over the region, and a favorable Great Lakes surface low track. Strong post-frontal 3 hour pressure rises of 5-7 mb were observed, and a low-topped mostly lightning-free convective line accompanied the boundary. Widespread wind gusts of at least 45-55 MPH were observed, with several higher measured gusts seen. Along the convective line, gusts of 55-65 MPH likely occurred. This resulted in widespread reports of wind damage to trees and power lines, with a few instances of mostly minor structural damage. Power lines were blown down on Washington Pike.", "ts_dict_index": [12897, 12898, 12899]}
+{"event_id": 927643, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-11-15 15:16:00", "end_date_time": "2020-11-15 15:16:00", "narrative": "A shortwave trough axis lifted quickly across the Great Lakes and the Upper Ohio Valley on November 15th, taking on a negative tilt as it did so. Deepening surface low pressure tracked across Michigan and into Ontario during the day, whipping a cold front across the region during the late morning and early afternoon. Some of the classic ingredients for a widespread wind event were present, including a negatively- tilted trough, jet positioning over the region, and a favorable Great Lakes surface low track. Strong post-frontal 3 hour pressure rises of 5-7 mb were observed, and a low-topped mostly lightning-free convective line accompanied the boundary. Widespread wind gusts of at least 45-55 MPH were observed, with several higher measured gusts seen. Along the convective line, gusts of 55-65 MPH likely occurred. This resulted in widespread reports of wind damage to trees and power lines, with a few instances of mostly minor structural damage. Damage to a building created debris that blew on to Route 30.", "ts_dict_index": [12900, 12901, 12902]}
+{"event_id": 927672, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-11-15 15:45:00", "end_date_time": "2020-11-15 15:45:00", "narrative": "A shortwave trough axis lifted quickly across the Great Lakes and the Upper Ohio Valley on November 15th, taking on a negative tilt as it did so. Deepening surface low pressure tracked across Michigan and into Ontario during the day, whipping a cold front across the region during the late morning and early afternoon. Some of the classic ingredients for a widespread wind event were present, including a negatively- tilted trough, jet positioning over the region, and a favorable Great Lakes surface low track. Strong post-frontal 3 hour pressure rises of 5-7 mb were observed, and a low-topped mostly lightning-free convective line accompanied the boundary. Widespread wind gusts of at least 45-55 MPH were observed, with several higher measured gusts seen. Along the convective line, gusts of 55-65 MPH likely occurred. This resulted in widespread reports of wind damage to trees and power lines, with a few instances of mostly minor structural damage. A tree was blown on to a home on Quarry Road.", "ts_dict_index": [12921, 12922, 12923]}
+{"event_id": 983846, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 16:58:00", "end_date_time": "2021-08-18 16:58:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Pictures on social media show multiple snapped tree due to strong downburst winds. Wind speeds estimated around 55 to 60 mph. Timing based on radar. No injuries were reported.", "ts_dict_index": [12918, 12919, 12920]}
+{"event_id": 983840, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 13:38:00", "end_date_time": "2021-08-18 13:38:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. A portion of the roof of an apartment complex near 7th Avenue and Hatcher Road was torn of in strong winds and landed on an unoccupied parked car, causing damage. Nearby, multiple photos on social media showed several downed saguaros with one of them causing some damage to the front of a home near 12th Street and Northern Avenue. Winds estimated around 60 to 65 mph. No injuries were reported.", "ts_dict_index": [12924, 12925, 12926]}
+{"event_id": 983843, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 13:40:00", "end_date_time": "2021-08-18 13:40:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Multiple reports of wind damage from a microburst along Peoria Avenue between 35th and 43rd Avenues. A couple large pine trees fell on an apartment complex, causing damage to the edge of the roof. A tree fell on 2 unoccupied parked cars at another apartment complex, causing major damage. A 1-foot diameter tree fell on an unoccupied parked car at a business plaza. There was also a partial roof torn off reported in the area. Winds were estimated around 60 to 65 mph. Timing based on radar. No injuries were reported.", "ts_dict_index": [12909, 12910, 12911]}
+{"event_id": 983844, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 15:11:00", "end_date_time": "2021-08-18 15:11:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. A large tree, possibly a palm tree, was blown down onto power lines along Extension Road between 2nd Street and 2nd Place, causing a power outage to approximately 600 customers. Winds estimated around 55 to 65 mph. Timing based on radar. No injuries were reported.", "ts_dict_index": [12915, 12916, 12917]}
+{"event_id": 1111633, "event_type": "Thunderstorm Wind", "state": "FLORIDA", "cz_name": "LEON", "begin_date_time": "2023-06-19 08:51:00", "end_date_time": "2023-06-19 08:51:00", "narrative": "The middle part of June was unusually stormy across the area. Numerous rounds of strong to severe storms impacted the region with multiple squall lines that produced severe winds as well as supercells that produced large hail and tornadoes.  Heavy rain also occurred over a multi-day period, which saturated the ground and led to some instances of flash flooding.  ||The synoptic pattern featured well above average 250 mb zonal wind anomalies, which were traceable back to an active subtropical jet stream.  Greater than average instability was also present, in part due to anomalously warm Gulf of Mexico SSTs.  This combination of above average shear from the active subtropical jet and above average instability from the warmer than average SSTs provided a synoptic environment favorable for severe weather as upper level shortwaves moving through the area.  This pattern persisted for many days, leading to an unusually large amount of severe weather. A tree was blown down with power lines at Mahan and James Ct.", "ts_dict_index": [12846, 12847, 12848]}
+{"event_id": 983849, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 17:45:00", "end_date_time": "2021-08-18 17:55:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Numerous trees down across Ahwatukee with many along Desert Foothills Parkway and Chandler Boulevard over to Ray Road. Many of the trees were palo verdes and several fell into roads and impeded traffic. Winds estimated around 50 to 60 mph. Time based on radar. No injuries were reported.", "ts_dict_index": [12927, 12928, 12929]}
+{"event_id": 972495, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-08-18 13:20:00", "end_date_time": "2021-08-18 13:20:00", "narrative": "An upper level trough and lead-on shortwave trough moved through Arizona during the day on the 18th. Moderate to high instability and high moisture content supported scattered strong thunderstorms. With deep south to southwest upslope flow, storms favored the foothills and mountainous areas of Maricopa and Gila counties. Most storms were producing at least 1 to 2 inch per hour rain rates, with several storms producing 2 to 3 inch rates and at times higher. Back-building and training of storms over the same areas resulted in significant to catastrophic flash flooding. A few burn scars experienced flash flooding, including the recent Telegraph burn area which had catastrophic flooding of the Russell Gulch drainage. There were also 2 fatalities on this day with off-roaders recreating near Camp Creek in northeast Maricopa County. The strong to severe storms also produced damaging winds from microbursts and small hail over lower desert locations. Multiple large trees uprooted in the area of 19th Ave between Missouri Ave and Maryland with some trees falling into and blocking streets. One tree was 30 feet tall and had a 12-18 inch diameter trunk. A large tree also reportedly fell at Palo Verde golf course. Timing was based on radar and wind gusts were estimated up to 50-60 mph with downburst signatures evident on radar. No injuries were reported.", "ts_dict_index": [12930, 12931, 12932]}
+{"event_id": 972953, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-13 02:58:00", "end_date_time": "2021-07-13 02:58:00", "narrative": "Two waves of severe storms entered the Ohio River Valley on July 13th. The first, was in the early morning hours. Despite the lack of day time heating, instability was available due to warm, moist advection under southwest flow. Vertical wind shear was also available as a trough approached an area of high pressure and a created a pressure gradient.||During the afternoon, warm and unstable conditions prevailed; dew points stayed in the lower 70s.  Mean-layer CAPE of 1500-2000 J/kg was able to develop.  Due to a gradient between upper high pressure off the east coast and a shortwave trough moving northeast through the Ohio Valley, moderate mid-level flow characterized by 30-40 knots of 0-6km shear prevailed.  This allowed storms to organize into multicellular storm clusters and short line segments.  Many wind damage reports were received, mainly to trees and power lines, although a few reports of structural damage were also noted. Trees and power lines were blown down on Bausman Street.", "ts_dict_index": [12984, 12985, 12986]}
+{"event_id": 971676, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2021-07-14 13:54:00", "end_date_time": "2021-07-14 13:54:00", "narrative": "Slow-moving thunderstorms trained over Rensselaer County during the afternoon of the 14th, resulting in a bullseye of 2-5 of rainfall over two to three hours over central and southern portions of the county. The runoff from the rainfall washed out or destroyed numerous roads and bridges, some of which would take weeks to months to reconstruct. Damages to roads and bridges totaled around $3 million, according to county officials. The Rensselaer County Executive declared a state of emergency and urged no unnecessary travel after the storms. Governor Hochul requested a Physical Disaster Declaration from the Small Business Administration, citing major damage to 18 homes and 9 businesses totaling $1.895 million, and minor damage to 281 homes and 14 businesses totaling $2.3 million. Some flash flooding extended into the northern portion of Columbia County as well. Some of the storms also produced wind damage with reports of trees and wires down. There was a report of trees down blocking Coila Road.", "ts_dict_index": [12969, 12970, 12971]}
+{"event_id": 972959, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-13 03:30:00", "end_date_time": "2021-07-13 03:30:00", "narrative": "Two waves of severe storms entered the Ohio River Valley on July 13th. The first, was in the early morning hours. Despite the lack of day time heating, instability was available due to warm, moist advection under southwest flow. Vertical wind shear was also available as a trough approached an area of high pressure and a created a pressure gradient.||During the afternoon, warm and unstable conditions prevailed; dew points stayed in the lower 70s.  Mean-layer CAPE of 1500-2000 J/kg was able to develop.  Due to a gradient between upper high pressure off the east coast and a shortwave trough moving northeast through the Ohio Valley, moderate mid-level flow characterized by 30-40 knots of 0-6km shear prevailed.  This allowed storms to organize into multicellular storm clusters and short line segments.  Many wind damage reports were received, mainly to trees and power lines, although a few reports of structural damage were also noted. Trees and wires were blown down along Bausman Street.", "ts_dict_index": [12990, 12991, 12992]}
+{"event_id": 972955, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-13 03:00:00", "end_date_time": "2021-07-13 03:00:00", "narrative": "Two waves of severe storms entered the Ohio River Valley on July 13th. The first, was in the early morning hours. Despite the lack of day time heating, instability was available due to warm, moist advection under southwest flow. Vertical wind shear was also available as a trough approached an area of high pressure and a created a pressure gradient.||During the afternoon, warm and unstable conditions prevailed; dew points stayed in the lower 70s.  Mean-layer CAPE of 1500-2000 J/kg was able to develop.  Due to a gradient between upper high pressure off the east coast and a shortwave trough moving northeast through the Ohio Valley, moderate mid-level flow characterized by 30-40 knots of 0-6km shear prevailed.  This allowed storms to organize into multicellular storm clusters and short line segments.  Many wind damage reports were received, mainly to trees and power lines, although a few reports of structural damage were also noted. Numerous trees were snapped or uprooted, bringing down power lines as well.", "ts_dict_index": [12996, 12997, 12998]}
+{"event_id": 972988, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-07-13 16:27:00", "end_date_time": "2021-07-13 16:27:00", "narrative": "Two waves of severe storms entered the Ohio River Valley on July 13th. The first, was in the early morning hours. Despite the lack of day time heating, instability was available due to warm, moist advection under southwest flow. Vertical wind shear was also available as a trough approached an area of high pressure and a created a pressure gradient.||During the afternoon, warm and unstable conditions prevailed; dew points stayed in the lower 70s.  Mean-layer CAPE of 1500-2000 J/kg was able to develop.  Due to a gradient between upper high pressure off the east coast and a shortwave trough moving northeast through the Ohio Valley, moderate mid-level flow characterized by 30-40 knots of 0-6km shear prevailed.  This allowed storms to organize into multicellular storm clusters and short line segments.  Many wind damage reports were received, mainly to trees and power lines, although a few reports of structural damage were also noted. Thunderstorm wind threw bricks on to a roof, blew a hot tub cover through a sliding glass door, and knocked down numerous trees along Stiffler Road.", "ts_dict_index": [12978, 12979, 12980]}
+{"event_id": 972952, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-13 02:48:00", "end_date_time": "2021-07-13 02:48:00", "narrative": "Two waves of severe storms entered the Ohio River Valley on July 13th. The first, was in the early morning hours. Despite the lack of day time heating, instability was available due to warm, moist advection under southwest flow. Vertical wind shear was also available as a trough approached an area of high pressure and a created a pressure gradient.||During the afternoon, warm and unstable conditions prevailed; dew points stayed in the lower 70s.  Mean-layer CAPE of 1500-2000 J/kg was able to develop.  Due to a gradient between upper high pressure off the east coast and a shortwave trough moving northeast through the Ohio Valley, moderate mid-level flow characterized by 30-40 knots of 0-6km shear prevailed.  This allowed storms to organize into multicellular storm clusters and short line segments.  Many wind damage reports were received, mainly to trees and power lines, although a few reports of structural damage were also noted. Trees and power lines were downed on Wible Run Road at Hillwood Road.", "ts_dict_index": [12981, 12982, 12983]}
+{"event_id": 974587, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-09 22:32:00", "end_date_time": "2021-07-09 22:32:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. Damaging wind gusts from severe thunderstorms resulted in a large uprooted tree on a playground in a park near Greenfield Road and Warner Road. No injuries were reported.", "ts_dict_index": [12942, 12943, 12944]}
+{"event_id": 975810, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-09 22:15:00", "end_date_time": "2021-07-09 22:15:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. At least 30-40 large trees were knocked down due to severe thunderstorms at Schnepf Farms in Queen Creek. Five of the eight greenhouses received damage with damage occurring to crops such as tomatoes, squash, and peppers. A wedding was ongoing at the farm as the severe thunderstorms hit. No injuries were reported. Estimates for the crop damage that occurred are unavailable. Timing was estimated from radar and nearby observations.", "ts_dict_index": [12936, 12937, 12938]}
+{"event_id": 974576, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-09 22:32:00", "end_date_time": "2021-07-09 22:32:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. A trained weather spotter reported a roughly 60ft by 20ft metal sheeted roof blew off a port structure and landed across the street, taking out a couple street signs and a chain link fence, at Riggs and Val Vista. Additionally, 8 inch diameter branches snapped from a palo verde tree and fell onto the roof of a house near Lindsay Road and Chandler Heights Road. No injuries were reported.", "ts_dict_index": [12948, 12949, 12950]}
+{"event_id": 974561, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-09 22:20:00", "end_date_time": "2021-07-09 22:20:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. The Rittenhouse SRP mesonet station in Queen Creek recorded a peak gust of 61 mph as severe thunderstorms moved through the area.", "ts_dict_index": [12933, 12934, 12935]}
+{"event_id": 974552, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-09 22:15:00", "end_date_time": "2021-07-09 22:15:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. An emergency management official reported damaging wind gusts ripped swamp coolers off of a couple of buildings at the Queen Creek Field Operations Facility and also bent some rolled up garage doors. A fire sprinkler was also damaged in a building causing the sprinkler to go off. No injuries were reported.", "ts_dict_index": [12951, 12952, 12953]}
+{"event_id": 1137052, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-08-25 15:55:00", "end_date_time": "2023-08-25 15:55:00", "narrative": "Despite a dominant upper-level ridge in place, a few isolated severe thunderstorms were able to develop across parts of Northwest Louisiana on the afternoon of August 25th. Strong diurnal heating allowed for mean-layer instability around 1500-2000 J/kg while deep-layer shear was rather weak and generally less than 10-15 knots. Despite the shear limitations, pulse convection resulted in a few isolated severe thunderstorms across parts of Sabine and Natchitoches Parish around mid-afternoon. Downdraft instability values around 1000 J/kg and fairly steep low-level lapse rates, resulting from very hot temperatures at the surface, also likely supported stronger outflow winds with some sporadic damaging wind gusts. Therefore, isolated reports of damaging wind gusts in Sabine and Natchitoches Parish were likely a result of individual pulse downdrafts as these thunderstorms collapsed within a layer of drier air beneath their cloud bases. Tree downed on Bellwood Street near Highway 117 in Provencal, along with some minor shingle damage to homes.", "ts_dict_index": [12987, 12988, 12989]}
+{"event_id": 974560, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2021-07-09 22:10:00", "end_date_time": "2021-07-09 22:10:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. The Phoenix-Mesa Gateway Airport AWOS station (KIWA) recorded a peak gust of 60 mph as severe thunderstorms moved through the area.", "ts_dict_index": [12957, 12958, 12959]}
+{"event_id": 974591, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-09 22:32:00", "end_date_time": "2021-07-09 22:32:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. The Casa Grande Municipal Airport AWOS station (KCGZ) recorded a peak gust of 58 mph as severe thunderstorms moved through the area.", "ts_dict_index": [12960, 12961, 12962]}
+{"event_id": 974544, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-09 22:14:00", "end_date_time": "2021-07-09 22:14:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. The Quail SRP mesonet station recorded a peak gust of 65 mph as severe thunderstorms ripped through the San Tan Valley area.", "ts_dict_index": [12945, 12946, 12947]}
+{"event_id": 835203, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 20:30:00", "end_date_time": "2019-06-22 20:30:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. A tree was down at the Iowa State Fairgrounds, it fell on a part of a building.", "ts_dict_index": [12972, 12973, 12974]}
+{"event_id": 974543, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-09 22:10:00", "end_date_time": "2021-07-09 22:20:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. Severe thunderstorms with measured winds upwards of 65 mph led to multiple reports of damage across San Tan Valley. At 2210MST, a trained weather spotter reported that numerous large trees 1-2 feet in diameter had been uprooted near Amira Park and in Johnson Ranch. Multiple downed trees were also reported in the Circle Cross Ranch and the Morning Sun Farms areas. Multiple power poles were reported down as well along Skyline Drive. No injuries were reported.", "ts_dict_index": [12954, 12955, 12956]}
+{"event_id": 835202, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-06-22 20:20:00", "end_date_time": "2019-06-22 20:20:00", "narrative": "Strong to severe storms and heavy rainfall moved up into Iowa from northern Missouri during the late afternoon and evening hours of the 22nd of June. Ahead of the storms, a warm front lifted into and through much of the state, bringing with it temperatures into the low to mid 80s and dew points in the low to mid 70s. Support for storms was decent with MUCAPE values of 2000+ J/kg reaching roughly the Interstate 80 corridor, effective bulk shear in the 30 to 40 kt range, and strong low level moisture transport boosting precipitable water values in excess of 1.5 to 1.75 inches.  ||All in all, a handful of severe storm reports (hail and wind) were seen as storms moved into the state from the south and eventually transitioned more into a rain threat that came to fruition over the eastern half of the Des Moines metro. A number of heavy rainfall amounts in excess of 2 to 4 inches were received, producing multiple flash flooding reports. Dispatch reported that a tree landed on a car, and nearby another tree was down in the street with some power lines down as well.", "ts_dict_index": [12975, 12976, 12977]}
+{"event_id": 975809, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-09 22:15:00", "end_date_time": "2021-07-09 22:15:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. The roof of a mobile home was ripped off as severe thunderstorms moved through the Queen Creek area while a family of 4 were inside. Much of the interior property was destroyed from the wind and the rainwater that entered the home. The home suffered additional damage the following night when more severe winds blew through the area. The home is a total loss. No injuries were reported.", "ts_dict_index": [12939, 12940, 12941]}
+{"event_id": 974538, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-09 21:57:00", "end_date_time": "2021-07-09 22:04:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. Severe thunderstorms moving off the higher terrain and into the lower deserts led to damaging wind gusts upwards of 60-65 mph around the Gold Canyon area. The damaging winds resulted in 28 distribution poles being knocked down along Highway 60 at MP 206. No injuries were reported.", "ts_dict_index": [12966, 12967, 12968]}
+{"event_id": 927644, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-11-15 15:16:00", "end_date_time": "2020-11-15 15:16:00", "narrative": "A shortwave trough axis lifted quickly across the Great Lakes and the Upper Ohio Valley on November 15th, taking on a negative tilt as it did so. Deepening surface low pressure tracked across Michigan and into Ontario during the day, whipping a cold front across the region during the late morning and early afternoon. Some of the classic ingredients for a widespread wind event were present, including a negatively- tilted trough, jet positioning over the region, and a favorable Great Lakes surface low track. Strong post-frontal 3 hour pressure rises of 5-7 mb were observed, and a low-topped mostly lightning-free convective line accompanied the boundary. Widespread wind gusts of at least 45-55 MPH were observed, with several higher measured gusts seen. Along the convective line, gusts of 55-65 MPH likely occurred. This resulted in widespread reports of wind damage to trees and power lines, with a few instances of mostly minor structural damage. A tree fell on to a home in Penn Heights Mobile Park.", "ts_dict_index": [12903, 12904, 12905]}
+{"event_id": 972960, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-07-13 03:35:00", "end_date_time": "2021-07-13 03:35:00", "narrative": "Two waves of severe storms entered the Ohio River Valley on July 13th. The first, was in the early morning hours. Despite the lack of day time heating, instability was available due to warm, moist advection under southwest flow. Vertical wind shear was also available as a trough approached an area of high pressure and a created a pressure gradient.||During the afternoon, warm and unstable conditions prevailed; dew points stayed in the lower 70s.  Mean-layer CAPE of 1500-2000 J/kg was able to develop.  Due to a gradient between upper high pressure off the east coast and a shortwave trough moving northeast through the Ohio Valley, moderate mid-level flow characterized by 30-40 knots of 0-6km shear prevailed.  This allowed storms to organize into multicellular storm clusters and short line segments.  Many wind damage reports were received, mainly to trees and power lines, although a few reports of structural damage were also noted. Multiple trees were blown down in the area of Export.", "ts_dict_index": [13002, 13003, 13004]}
+{"event_id": 972998, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2021-07-13 17:15:00", "end_date_time": "2021-07-13 17:15:00", "narrative": "Two waves of severe storms entered the Ohio River Valley on July 13th. The first, was in the early morning hours. Despite the lack of day time heating, instability was available due to warm, moist advection under southwest flow. Vertical wind shear was also available as a trough approached an area of high pressure and a created a pressure gradient.||During the afternoon, warm and unstable conditions prevailed; dew points stayed in the lower 70s.  Mean-layer CAPE of 1500-2000 J/kg was able to develop.  Due to a gradient between upper high pressure off the east coast and a shortwave trough moving northeast through the Ohio Valley, moderate mid-level flow characterized by 30-40 knots of 0-6km shear prevailed.  This allowed storms to organize into multicellular storm clusters and short line segments.  Many wind damage reports were received, mainly to trees and power lines, although a few reports of structural damage were also noted. A tree was downed at Exit 46B of I-70.", "ts_dict_index": [12999, 13000, 13001]}
+{"event_id": 1141672, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-09-24 21:35:00", "end_date_time": "2023-09-24 21:35:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of extreme Northeast Texas with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of East and Northeast Texas. Numerous trees downed across the city of Tyler and Smith County.", "ts_dict_index": [13017, 13018, 13019]}
+{"event_id": 1141670, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-09-24 20:30:00", "end_date_time": "2023-09-24 20:30:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of extreme Northeast Texas with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of East and Northeast Texas. Several trees downed near Highway 110 and FM Road 16.", "ts_dict_index": [13020, 13021, 13022]}
+{"event_id": 1141680, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-09-24 22:33:00", "end_date_time": "2023-09-24 22:33:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of extreme Northeast Texas with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of East and Northeast Texas. A tree was downed across FM Road 225 just north of Laneville. A vehicle struck the tree, but the driver was not injured.", "ts_dict_index": [13011, 13012, 13013]}
+{"event_id": 1141678, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-09-24 22:25:00", "end_date_time": "2023-09-24 22:25:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of extreme Northeast Texas with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of East and Northeast Texas. A roof was removed from an outbuilding, and one exterior wall was blown out of another outbuilding near the intersection of FM Road 1798 and FM Road 839.", "ts_dict_index": [13005, 13006, 13007]}
+{"event_id": 1141679, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-09-24 22:30:00", "end_date_time": "2023-09-24 22:30:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of extreme Northeast Texas with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of East and Northeast Texas. A roof was ripped off of a house on County Road 4256 on the Rusk County side of Lake Striker.", "ts_dict_index": [13008, 13009, 13010]}
+{"event_id": 972954, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "ALLEGHENY", "begin_date_time": "2021-07-13 03:00:00", "end_date_time": "2021-07-13 03:00:00", "narrative": "Two waves of severe storms entered the Ohio River Valley on July 13th. The first, was in the early morning hours. Despite the lack of day time heating, instability was available due to warm, moist advection under southwest flow. Vertical wind shear was also available as a trough approached an area of high pressure and a created a pressure gradient.||During the afternoon, warm and unstable conditions prevailed; dew points stayed in the lower 70s.  Mean-layer CAPE of 1500-2000 J/kg was able to develop.  Due to a gradient between upper high pressure off the east coast and a shortwave trough moving northeast through the Ohio Valley, moderate mid-level flow characterized by 30-40 knots of 0-6km shear prevailed.  This allowed storms to organize into multicellular storm clusters and short line segments.  Many wind damage reports were received, mainly to trees and power lines, although a few reports of structural damage were also noted. Power lines were blown down on Banksville Road.", "ts_dict_index": [12993, 12994, 12995]}
+{"event_id": 1141671, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-09-24 20:50:00", "end_date_time": "2023-09-24 20:50:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of extreme Northeast Texas with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of East and Northeast Texas. Tree downed in Whitehouse.", "ts_dict_index": [13023, 13024, 13025]}
+{"event_id": 1009753, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-03-30 09:27:00", "end_date_time": "2022-03-30 09:27:00", "narrative": "A closed upper low pressure system entered the Four Corners Region on March 29th, before opening up into a trough which lifted through the Southern Rockies during the evening through the early morning hours of the 30th. A very strong southerly low level jet developed during the afternoon and evening of the 29th over the Southern Plains ahead of this ejecting trough, with large scale forcing along and east of the West Texas dryline contributing to the development of scattered to numerous showers and thunderstorms, which marched east into East Texas during the pre-dawn hours of the 30th, and North Louisiana from the mid-morning through the early afternoon. Diurnal heating contributed to increased instability by mid and late morning over North Louisiana, which resulted in scattered severe thunderstorms producing damaging winds and isolated tornadoes. These storms eventually exited North Louisiana to the east by mid-afternoon. Large pine trees were snapped and fencing around a batting area was damaged at Ford Park.", "ts_dict_index": [13029, 13030, 13031]}
+{"event_id": 815842, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2019-05-29 13:39:00", "end_date_time": "2019-05-29 13:40:00", "narrative": "The combination of an upper level impulse and southward sagging frontal boundary out of the Ohio Valley brought a line of strong to severe thunderstorms across eastern Kentucky. The most intense of these storms moved through far eastern Kentucky, including Prestonsburg where a 70-80 mph downburst blew half the roof off of a hock shop building.||A man driving on West Court Street was crushed by this roof, resulting in his death. Damage stretched for about 1 mile through the city. Severe winds blew out a few of the windows of a 2 story building on West Court Street, while a large healthy poplar tree was uprooted.||Elsewhere, from West Liberty and Jackson eastward through Pike County, mainly tree damage was sustained. In Letcher County, a rotating supercell produced quarter to golf ball sized hail near Jenkins, while Somerset experienced isolated damage from a thunderstorm wind gust on the southwest flank of the line of storms. Local Emergency Management reported trees were blown down and onto Kentucky Highway 80 between Nancy and Somerset. A pontoon boat was blown off of Lake Cumberland at Pulaski County Park.", "ts_dict_index": [13026, 13027, 13028]}
+{"event_id": 974594, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2021-07-09 22:35:00", "end_date_time": "2021-07-09 22:35:00", "narrative": "Thunderstorms developed along the Mogollon Rim during the early part of the afternoon on the 9th. Relatively strong easterly mid level anticyclonic flow associated with the upper level ridge centered near the Arizona/Utah state line helped allow strong to severe thunderstorms to propagate westward into the lower deserts. The severe thunderstorms led to damaging winds gusts upwards of 60-65 mph across southeast portions of the Phoenix metro. Thee severe winds ahead of the thunderstorms also produced a dust storm that led to widespread reports of dense blowing dust across central and southeastern Phoenix and as far south as Casa Grande. A few isolated instances of flash flooding occurred as well, including the recent Telegraph burn scar where over 0.75 of rain fell. There were numerous reports of damage across eastern parts of the Valley, including numerous power poles and large trees down. No injuries were reported with these thunderstorms. The Desert Basin SRP mesonet station in Casa Grande recorded a peak gust of 63 mph as severe thunderstorms moved through the area.", "ts_dict_index": [12963, 12964, 12965]}
+{"event_id": 1009751, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-03-30 09:28:00", "end_date_time": "2022-03-30 09:28:00", "narrative": "A closed upper low pressure system entered the Four Corners Region on March 29th, before opening up into a trough which lifted through the Southern Rockies during the evening through the early morning hours of the 30th. A very strong southerly low level jet developed during the afternoon and evening of the 29th over the Southern Plains ahead of this ejecting trough, with large scale forcing along and east of the West Texas dryline contributing to the development of scattered to numerous showers and thunderstorms, which marched east into East Texas during the pre-dawn hours of the 30th, and North Louisiana from the mid-morning through the early afternoon. Diurnal heating contributed to increased instability by mid and late morning over North Louisiana, which resulted in scattered severe thunderstorms producing damaging winds and isolated tornadoes. These storms eventually exited North Louisiana to the east by mid-afternoon. The 5500 block of Greenwood Road was down to one lane due to a tree falling in the westbound lane.", "ts_dict_index": [13035, 13036, 13037]}
+{"event_id": 1141633, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-09-24 21:05:00", "end_date_time": "2023-09-24 21:05:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. Multiple trees were blown down in the Dogwood South subdivision with some trees downed onto homes.", "ts_dict_index": [13059, 13060, 13061]}
+{"event_id": 1009749, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-03-30 09:53:00", "end_date_time": "2022-03-30 09:53:00", "narrative": "A closed upper low pressure system entered the Four Corners Region on March 29th, before opening up into a trough which lifted through the Southern Rockies during the evening through the early morning hours of the 30th. A very strong southerly low level jet developed during the afternoon and evening of the 29th over the Southern Plains ahead of this ejecting trough, with large scale forcing along and east of the West Texas dryline contributing to the development of scattered to numerous showers and thunderstorms, which marched east into East Texas during the pre-dawn hours of the 30th, and North Louisiana from the mid-morning through the early afternoon. Diurnal heating contributed to increased instability by mid and late morning over North Louisiana, which resulted in scattered severe thunderstorms producing damaging winds and isolated tornadoes. These storms eventually exited North Louisiana to the east by mid-afternoon. A couple of trees were uprooted on Pueblo Lane and also on Lasso Lane in far South Shreveport.", "ts_dict_index": [13050, 13051, 13052]}
+{"event_id": 1141638, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-09-24 23:05:00", "end_date_time": "2023-09-24 23:05:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. Trees downed along Colquitt Road between Scout Drive and Woolworth Road.", "ts_dict_index": [13062, 13063, 13064]}
+{"event_id": 1087619, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-05-04 23:48:00", "end_date_time": "2023-05-04 23:48:00", "narrative": "A flat upper level ridge was anchored over the Four State Region during the afternoon through the early morning hours of May 4th-5th, which maintained very warm and dry conditions over the area. However, an upper level disturbance ejected northeast atop the dryline across West Texas and Western Oklahoma, with this forcing interacting with daytime heating and resultant instability to initiate a complex of showers and thunderstorms over West-Central and Central Texas during the afternoon and evening. This complex organized into a large thunderstorm complex, with numerous severe thunderstorms advancing across the Hill Country east into Deep East Texas during the early morning hours of the 5th. These storms remained severe as they entered Deep East Texas, downing multiple trees and power lines across Cherokee, Rusk, and Nacogdoches Counties before weakening as they reached the Sabine Valley closest to the center of the ridge. A tree was blown down in the Brachfield community.", "ts_dict_index": [13053, 13054, 13055]}
+{"event_id": 1009758, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2022-03-30 10:16:00", "end_date_time": "2022-03-30 10:16:00", "narrative": "A closed upper low pressure system entered the Four Corners Region on March 29th, before opening up into a trough which lifted through the Southern Rockies during the evening through the early morning hours of the 30th. A very strong southerly low level jet developed during the afternoon and evening of the 29th over the Southern Plains ahead of this ejecting trough, with large scale forcing along and east of the West Texas dryline contributing to the development of scattered to numerous showers and thunderstorms, which marched east into East Texas during the pre-dawn hours of the 30th, and North Louisiana from the mid-morning through the early afternoon. Diurnal heating contributed to increased instability by mid and late morning over North Louisiana, which resulted in scattered severe thunderstorms producing damaging winds and isolated tornadoes. These storms eventually exited North Louisiana to the east by mid-afternoon. A large tree was blown down blocking Pilgrim Rest Road in Doyline.", "ts_dict_index": [13044, 13045, 13046]}
+{"event_id": 1087618, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-05-04 23:25:00", "end_date_time": "2023-05-04 23:25:00", "narrative": "A flat upper level ridge was anchored over the Four State Region during the afternoon through the early morning hours of May 4th-5th, which maintained very warm and dry conditions over the area. However, an upper level disturbance ejected northeast atop the dryline across West Texas and Western Oklahoma, with this forcing interacting with daytime heating and resultant instability to initiate a complex of showers and thunderstorms over West-Central and Central Texas during the afternoon and evening. This complex organized into a large thunderstorm complex, with numerous severe thunderstorms advancing across the Hill Country east into Deep East Texas during the early morning hours of the 5th. These storms remained severe as they entered Deep East Texas, downing multiple trees and power lines across Cherokee, Rusk, and Nacogdoches Counties before weakening as they reached the Sabine Valley closest to the center of the ridge. A tree was blown down in Reklaw.", "ts_dict_index": [13056, 13057, 13058]}
+{"event_id": 1009757, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2022-03-30 10:40:00", "end_date_time": "2022-03-30 10:40:00", "narrative": "A closed upper low pressure system entered the Four Corners Region on March 29th, before opening up into a trough which lifted through the Southern Rockies during the evening through the early morning hours of the 30th. A very strong southerly low level jet developed during the afternoon and evening of the 29th over the Southern Plains ahead of this ejecting trough, with large scale forcing along and east of the West Texas dryline contributing to the development of scattered to numerous showers and thunderstorms, which marched east into East Texas during the pre-dawn hours of the 30th, and North Louisiana from the mid-morning through the early afternoon. Diurnal heating contributed to increased instability by mid and late morning over North Louisiana, which resulted in scattered severe thunderstorms producing damaging winds and isolated tornadoes. These storms eventually exited North Louisiana to the east by mid-afternoon. A tree fell onto a home on the 100 block of Highway 485 in Powhatan, trapping the family in the home for a brief period. No injuries.", "ts_dict_index": [13041, 13042, 13043]}
+{"event_id": 1009759, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2022-03-30 10:59:00", "end_date_time": "2022-03-30 10:59:00", "narrative": "A closed upper low pressure system entered the Four Corners Region on March 29th, before opening up into a trough which lifted through the Southern Rockies during the evening through the early morning hours of the 30th. A very strong southerly low level jet developed during the afternoon and evening of the 29th over the Southern Plains ahead of this ejecting trough, with large scale forcing along and east of the West Texas dryline contributing to the development of scattered to numerous showers and thunderstorms, which marched east into East Texas during the pre-dawn hours of the 30th, and North Louisiana from the mid-morning through the early afternoon. Diurnal heating contributed to increased instability by mid and late morning over North Louisiana, which resulted in scattered severe thunderstorms producing damaging winds and isolated tornadoes. These storms eventually exited North Louisiana to the east by mid-afternoon. Several trees were snapped and uprooted in Campti. A metal shed was destroyed.", "ts_dict_index": [13047, 13048, 13049]}
+{"event_id": 1009780, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2022-03-30 11:15:00", "end_date_time": "2022-03-30 11:15:00", "narrative": "A closed upper low pressure system entered the Four Corners Region on March 29th, before opening up into a trough which lifted through the Southern Rockies during the evening through the early morning hours of the 30th. A very strong southerly low level jet developed during the afternoon and evening of the 29th over the Southern Plains ahead of this ejecting trough, with large scale forcing along and east of the West Texas dryline contributing to the development of scattered to numerous showers and thunderstorms, which marched east into East Texas during the pre-dawn hours of the 30th, and North Louisiana from the mid-morning through the early afternoon. Diurnal heating contributed to increased instability by mid and late morning over North Louisiana, which resulted in scattered severe thunderstorms producing damaging winds and isolated tornadoes. These storms eventually exited North Louisiana to the east by mid-afternoon. A tree fell onto a utility line on Franklin Lane just southeast of Natchitoches. The road was blocked by the fallen tree and line.", "ts_dict_index": [13038, 13039, 13040]}
+{"event_id": 1141682, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-09-24 22:30:00", "end_date_time": "2023-09-24 22:30:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of extreme Northeast Texas with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of East and Northeast Texas. A 70 mph wind gust was recorded at a Texas Water Development Board Mesonet station on the Rusk County side of Lake Striker.", "ts_dict_index": [13014, 13015, 13016]}
+{"event_id": 1141635, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-09-24 22:59:00", "end_date_time": "2023-09-24 22:59:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. A tree was downed on Woolworth Road between Sagewood Drive and Shirley Francis Road.", "ts_dict_index": [13071, 13072, 13073]}
+{"event_id": 1141636, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-09-24 23:00:00", "end_date_time": "2023-09-24 23:00:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. A tree was downed on Buncombe Road near Bert Kouns Industrial Loop, and another tree was also downed on Bert Kouns near Pines Road.", "ts_dict_index": [13083, 13084, 13085]}
+{"event_id": 1141639, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-09-24 23:13:00", "end_date_time": "2023-09-24 23:13:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. Trees and power lines were downed on Jewella Avenue between Dollarway Drive and Red Bud Lane.", "ts_dict_index": [13080, 13081, 13082]}
+{"event_id": 1141642, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-09-24 23:15:00", "end_date_time": "2023-09-24 23:15:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. Numerous trees and power lines were downed across the South Highlands neighborhood in Shreveport, including near Pierremont Road and Gilbert Drive, and Ockley Drive between Fairfield Avenue and Maryland Avenue.", "ts_dict_index": [13089, 13090, 13091]}
+{"event_id": 1141648, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-09-24 23:13:00", "end_date_time": "2023-09-24 23:13:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. A 66 mph wind gust was recorded at the Shreveport Regional Airport ASOS.", "ts_dict_index": [13068, 13069, 13070]}
+{"event_id": 1082245, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-21 15:40:00", "end_date_time": "2023-04-21 15:45:00", "narrative": "A couple of intense thunderstorms raked the western portion of southern Hidalgo County the afternoon of April 21st. The storm produced hail up to the size of tennis balls for more than an hour, drove that hail with 60 to 65 mph winds, and produced frequent cloud to ground lightning. Initial storms developed along a cold front over the Brush Country of eastern Zapata and northwestern Jim Hogg Counties around 2 PM CDT on April 21st and spread into northern Starr and Southern Hidalgo Counties by 3:30PM CDT to 4:00PM CDT and continued until 5:00PM CDT when it moved into northern Mexico. Additional storms developed along the sea breeze in eastern southern Hidalgo County and northwestern Cameron County around 3:45PM CDT and continued until 4:45PM CDT before moving into Mexico. Those storms split and ultimately produced hail between Lyford, western Harlingen, and La Feria in northwestern Cameron and southern Willacy Counties. The ASOS station at McAllen-Miller International Airport (KMFE) recorded a wind gust of 62 mph at 4:40PM CDT the afternoon of April 21st. There was also some damage to a warehouse a few miles south of the airport with a garage door blown inward.", "ts_dict_index": [13092, 13093, 13094]}
+{"event_id": 1141630, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-09-24 05:48:00", "end_date_time": "2023-09-24 05:48:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. Trees downed near Harrell Street off of Vivian Airport Road.", "ts_dict_index": [13086, 13087, 13088]}
+{"event_id": 1141631, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-09-24 05:53:00", "end_date_time": "2023-09-24 05:53:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. Tree downed near Pelican Lodge Road and Bonham Landing Road near Caddo Lake.", "ts_dict_index": [13095, 13096, 13097]}
+{"event_id": 1084574, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-21 15:45:00", "end_date_time": "2023-04-21 15:45:00", "narrative": "A couple of intense thunderstorms raked the western portion of southern Hidalgo County the afternoon of April 21st. The storm produced hail up to the size of tennis balls for more than an hour, drove that hail with 60 to 65 mph winds, and produced frequent cloud to ground lightning. Initial storms developed along a cold front over the Brush Country of eastern Zapata and northwestern Jim Hogg Counties around 2 PM CDT on April 21st and spread into northern Starr and Southern Hidalgo Counties by 3:30PM CDT to 4:00PM CDT and continued until 5:00PM CDT when it moved into northern Mexico. Additional storms developed along the sea breeze in eastern southern Hidalgo County and northwestern Cameron County around 3:45PM CDT and continued until 4:45PM CDT before moving into Mexico. Those storms split and ultimately produced hail between Lyford, western Harlingen, and La Feria in northwestern Cameron and southern Willacy Counties. Members of the public reported large tree limbs knocked down along Ware Road in McAllen. Timing estimated by radar and wind gust estimated by using the McAllen-Miller International Airport (KMFE) ASOS.", "ts_dict_index": [13074, 13075, 13076]}
+{"event_id": 1084571, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2023-04-21 15:45:00", "end_date_time": "2023-04-21 15:45:00", "narrative": "A couple of intense thunderstorms raked the western portion of southern Hidalgo County the afternoon of April 21st. The storm produced hail up to the size of tennis balls for more than an hour, drove that hail with 60 to 65 mph winds, and produced frequent cloud to ground lightning. Initial storms developed along a cold front over the Brush Country of eastern Zapata and northwestern Jim Hogg Counties around 2 PM CDT on April 21st and spread into northern Starr and Southern Hidalgo Counties by 3:30PM CDT to 4:00PM CDT and continued until 5:00PM CDT when it moved into northern Mexico. Additional storms developed along the sea breeze in eastern southern Hidalgo County and northwestern Cameron County around 3:45PM CDT and continued until 4:45PM CDT before moving into Mexico. Those storms split and ultimately produced hail between Lyford, western Harlingen, and La Feria in northwestern Cameron and southern Willacy Counties. A member of the public shared a picture of a warehouse garage door blown in by a thunderstorm wind gust. Timing estimated by radar and wind gust estimated by using the McAllen-Miller International Airport ASOS, which recorded a gust to 54 knots.", "ts_dict_index": [13077, 13078, 13079]}
+{"event_id": 1009754, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-03-30 09:41:00", "end_date_time": "2022-03-30 09:41:00", "narrative": "A closed upper low pressure system entered the Four Corners Region on March 29th, before opening up into a trough which lifted through the Southern Rockies during the evening through the early morning hours of the 30th. A very strong southerly low level jet developed during the afternoon and evening of the 29th over the Southern Plains ahead of this ejecting trough, with large scale forcing along and east of the West Texas dryline contributing to the development of scattered to numerous showers and thunderstorms, which marched east into East Texas during the pre-dawn hours of the 30th, and North Louisiana from the mid-morning through the early afternoon. Diurnal heating contributed to increased instability by mid and late morning over North Louisiana, which resulted in scattered severe thunderstorms producing damaging winds and isolated tornadoes. These storms eventually exited North Louisiana to the east by mid-afternoon. Large tree limbs were snapped off of a large oak tree at the LA State Building at the corner of Fairfield Ave and Jordan Street.", "ts_dict_index": [13032, 13033, 13034]}
+{"event_id": 1141632, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-09-24 06:22:00", "end_date_time": "2023-09-24 06:22:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. Trees downed near Shreveport Blanchard Road and North Industry Road.", "ts_dict_index": [13098, 13099, 13100]}
+{"event_id": 916305, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 15:29:00", "end_date_time": "2020-08-25 15:29:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. Several trees were reported down in Mount Pleasant Township.", "ts_dict_index": [13110, 13111, 13112]}
+{"event_id": 916296, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 14:16:00", "end_date_time": "2020-08-25 14:16:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. Trees were reported to be blown down on power lines in Derry Township near the intersection of Route 981 and Shortcut Road.", "ts_dict_index": [13122, 13123, 13124]}
+{"event_id": 916294, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 14:15:00", "end_date_time": "2020-08-25 14:15:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. In Fairfield Township, multiple trees were reported to be blown down.", "ts_dict_index": [13125, 13126, 13127]}
+{"event_id": 916302, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 14:38:00", "end_date_time": "2020-08-25 14:38:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. A tree was reported down near the intersection of Wilpen Road and Ramsey Road.", "ts_dict_index": [13119, 13120, 13121]}
+{"event_id": 915585, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 07:40:00", "end_date_time": "2020-08-25 07:40:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. Power lines were reported to be blown down.", "ts_dict_index": [13113, 13114, 13115]}
+{"event_id": 1015182, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-04-30 22:32:00", "end_date_time": "2022-04-30 22:32:00", "narrative": "A weak upper trough shifted southeast from Western Iowa and Eastern Nebraska into Oklahoma and Arkansas during the afternoon and evening of April 30th, reinforcing a weak cold front southeast into Northeast Texas, Southwest Arkansas, and North Louisiana during the evening through the early morning hours of May 1st. A warm, moist, and unstable air mass was in place ahead of the front, with increasing large scale forcing along and ahead of the front and approaching trough resulting in scattered shower and thunderstorm development over portions of Southwest Arkansas and North Louisiana. An isolated severe thunderstorm developed over Northeast Lincoln and Southwest Union Parishes in North-central Louisiana, where damaging winds downed a tree several miles northwest of Downsville along the Lincoln/Union Parish line. These storms weakened and moved out of the region during the early morning hours of May 1st. A tree was blown down on Highway 151 west of Highway 33 near the Lincoln/Union Parish line.", "ts_dict_index": [13116, 13117, 13118]}
+{"event_id": 799408, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2019-02-21 12:45:00", "end_date_time": "2019-02-21 12:45:00", "narrative": "A powerful winter storm moved into Arizona on February 21st, and in addition to heavy rainfall and high elevation snowfall, it generated unstable conditions during the afternoon hours over the greater Phoenix metropolitan area. Elevated wind shear combined with partial sunshine and instability to kick off isolated thunderstorms. One of the stronger storms developed over western portions of the Phoenix area and impacted the town of Tolleson. At 1245MST gusty outflow winds 2 miles west of the town snapped multiple Palo Verde trees in half and uprooted one of the larger trees. The winds also bent over a street sign, and damaged a sign at a local Honda dealership. At the same time, strong winds blew down multiple Salt River Project power poles near the intersection of Interstate 10 and the loop 101 freeway. No injuries were reported, and a Severe Thunderstorm Warning was not in effect at the time of the damage. A slow moving, and very strong winter storm moved through south-central Arizona starting on February 21st, and in addition to heavy desert rain and mountain snow, the storm produced conditions favorable for thunderstorms during the afternoon hours. Isolated strong storms formed in the early afternoon over portions of the greater Phoenix area and one of the stronger ones impacted the town of Tolleson. According to a report from the public, at 1245MST gusty thunderstorm winds up to 65 mph snapped several Palo Verde trees in half and uprooted one of the larger trees. This occurred about 2 miles to the northwest of Tolleson. In addition, the winds bent over a street sign and  damaged a sign at the local Honda dealership. At the same time, about 1 mile northwest of the town, the strong winds downed multiple Salt River Project power poles. No injuries were reported due to the damage. A Severe Thunderstorm Warning was not in effect at the time of the damage.", "ts_dict_index": [13104, 13105, 13106]}
+{"event_id": 954123, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2021-06-13 23:24:00", "end_date_time": "2021-06-13 23:24:00", "narrative": "Scattered showers and thunderstorms developed during the mid-afternoon hours across Northcentral Louisiana on June 13th, near a weak surface trough extending from Southeast Oklahoma, extreme Southwest Arkansas, and North Louisiana. Compressional warming and low level moisture pooling near this boundary resulted in a very unstable air mass developing across much of the region, with a weak upper level disturbance sliding southwest across North Louisiana and East Texas during the afternoon and evening contributing to increasing large scale ascent. These storms continued to redevelop and shift west-southwest across North Louisiana through the evening and into East Texas after midnight. Some of these storms re-intensified and became severe over Harrison and Upshur Counties, with trees downed east of Hallsville and quarter size hail falling in Gilmer. These storms finally diminished between 3-4 am on the 14th. Trees were blown down near FM 968 and I-20.", "ts_dict_index": [13107, 13108, 13109]}
+{"event_id": 822161, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-05-16 20:08:00", "end_date_time": "2019-05-16 20:08:00", "narrative": "The state found itself under broad upper level ridging to zonal flow, allowing for a weak cold front to slide into the state and stall around the Interstate 80 corridor during the evening and overnight hours. The environment was fairly ripe for thunderstorm activity, including 2000-3000+ J/kg SBCAPE and hail CAPE values around 500 J/kg, but lacked supportive effective bulk shear with values generally around 30 kts or less.  With the front stalling across central Iowa, and the thermodynamic environment what it was, thunderstorms predominantly lingered across central Iowa through the evening and overnight hours, producing periods of severe hail during the first couple of hours and transitioning to sub-severe storms and a predominant heavy rainfall threat. In the end, there were a number of reports of quarter to near golf ball sized hail, followed by heavy rainfall amounts of 2 to 3+ inches by the morning of the 17th. Tree damage reported near 42nd and Forest Ave in Des Moines.", "ts_dict_index": [13101, 13102, 13103]}
+{"event_id": 1141634, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-09-24 22:51:00", "end_date_time": "2023-09-24 22:51:00", "narrative": "Intense nocturnal convection early on September 24th became focused across eastern Oklahoma and western Arkansas within an area of strong low-level warm advection, in the vicinity of a 30+ knot southwesterly low-level jet. This convection continued to shift east southeast ahead of an advancing cold front across the Southern Plains through the early morning hours with a gradual veering of the low-level jet. Convection intensified toward the Middle Red River Valley of Southeast Oklahoma and Southwest Arkansas, within a modestly unstable area of inflow. Although gradual weakening was observed, a few severe thunderstorms continued south into parts of northern Caddo Parish with a few reports of isolated damaging wind gusts shortly before daybreak. Additional severe convection developed along and just ahead of the cold front later in the evening with numerous reports of damaging wind gusts across much of Northwest Louisiana. Trees were downed across Highway 169 between Lindsay Road and Carrera Street west of Blanchard.", "ts_dict_index": [13065, 13066, 13067]}
+{"event_id": 1137057, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-08-27 19:57:00", "end_date_time": "2023-08-27 19:57:00", "narrative": "Thunderstorms were observed developing along a nearly stalled frontal boundary and remnant outflows across parts of Southwest Arkansas, Northeast Texas, and Northern Louisiana on the afternoon of August 27th. Very strong diurnal heating was sufficient to erode a capping inversion aloft with around 1500-2000 J/kg of mean-layer instability supporting occasional stronger updrafts. Deep-layer vertical shear across much of the region was weak at generally less than 10-15 knots. This was still enough to support multi-cellular, pulse convection as the primary storm mode. Weak surface flow was also insufficient to support much cold pool propagation. Therefore, the primary severe risk was tied to individual pulse downdrafts as thunderstorms collapsed. This resulted in numerous damaging wind reports across parts of the region, including several reports in parts of Caddo Parish and one in Natchitoches Parish. Trees and power lines downed at multiple locations along Ellerbe Road.", "ts_dict_index": [13155, 13156, 13157]}
+{"event_id": 915581, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 07:25:00", "end_date_time": "2020-08-25 07:25:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. A tree was reported to be down along Route 119 near the Country Farms garden center.", "ts_dict_index": [13140, 13141, 13142]}
+{"event_id": 916303, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 15:15:00", "end_date_time": "2020-08-25 15:15:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. Trees and power lines were blown down in Cook Township off of Linn Run Road.", "ts_dict_index": [13131, 13132, 13133]}
+{"event_id": 915579, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 07:17:00", "end_date_time": "2020-08-25 07:17:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. Trees were reported to be blown down at a residence.", "ts_dict_index": [13143, 13144, 13145]}
+{"event_id": 916293, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 14:05:00", "end_date_time": "2020-08-25 14:05:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. A tree was reported to be blown down on the 200 block of Garrigan Hill Road.", "ts_dict_index": [13134, 13135, 13136]}
+{"event_id": 1056763, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-10-24 22:55:00", "end_date_time": "2022-10-24 22:55:00", "narrative": "A potent upper level low pressure system over New Mexico shifted east across Western and North Texas south of the Red River during the afternoon and evening hours of October 24th, which allowed for a dry line to mix east across Texas. A cold front extended east of this upper low over Eastern Oklahoma and Northeast Texas, with the dry line eventually overtaking the front but provided strong forcing for a linear line of showers and thunderstorms to develop during the evening and overnight hours as they entered East Texas. Although instability was limited given cooler conditions during the latter evening hours, strong shear resulted in a well-organized line of strong to severe thunderstorms along these surface features, producing damaging winds which downed trees across portions of East Texas before the storms weakened further upon entering Western Louisiana during the early morning hours on the 25th. Power lines were downed in Reklaw.", "ts_dict_index": [13149, 13150, 13151]}
+{"event_id": 1056767, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-10-24 23:24:00", "end_date_time": "2022-10-24 23:24:00", "narrative": "A potent upper level low pressure system over New Mexico shifted east across Western and North Texas south of the Red River during the afternoon and evening hours of October 24th, which allowed for a dry line to mix east across Texas. A cold front extended east of this upper low over Eastern Oklahoma and Northeast Texas, with the dry line eventually overtaking the front but provided strong forcing for a linear line of showers and thunderstorms to develop during the evening and overnight hours as they entered East Texas. Although instability was limited given cooler conditions during the latter evening hours, strong shear resulted in a well-organized line of strong to severe thunderstorms along these surface features, producing damaging winds which downed trees across portions of East Texas before the storms weakened further upon entering Western Louisiana during the early morning hours on the 25th. Multiple trees were blown down on Highway 315 several miles northeast of Mount Enterprise.", "ts_dict_index": [13146, 13147, 13148]}
+{"event_id": 1056764, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2022-10-24 23:25:00", "end_date_time": "2022-10-24 23:25:00", "narrative": "A potent upper level low pressure system over New Mexico shifted east across Western and North Texas south of the Red River during the afternoon and evening hours of October 24th, which allowed for a dry line to mix east across Texas. A cold front extended east of this upper low over Eastern Oklahoma and Northeast Texas, with the dry line eventually overtaking the front but provided strong forcing for a linear line of showers and thunderstorms to develop during the evening and overnight hours as they entered East Texas. Although instability was limited given cooler conditions during the latter evening hours, strong shear resulted in a well-organized line of strong to severe thunderstorms along these surface features, producing damaging winds which downed trees across portions of East Texas before the storms weakened further upon entering Western Louisiana during the early morning hours on the 25th. Trees were blown down on I-20 at Exit 604 near Hallsville.", "ts_dict_index": [13158, 13159, 13160]}
+{"event_id": 1056766, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2022-10-24 23:41:00", "end_date_time": "2022-10-24 23:41:00", "narrative": "A potent upper level low pressure system over New Mexico shifted east across Western and North Texas south of the Red River during the afternoon and evening hours of October 24th, which allowed for a dry line to mix east across Texas. A cold front extended east of this upper low over Eastern Oklahoma and Northeast Texas, with the dry line eventually overtaking the front but provided strong forcing for a linear line of showers and thunderstorms to develop during the evening and overnight hours as they entered East Texas. Although instability was limited given cooler conditions during the latter evening hours, strong shear resulted in a well-organized line of strong to severe thunderstorms along these surface features, producing damaging winds which downed trees across portions of East Texas before the storms weakened further upon entering Western Louisiana during the early morning hours on the 25th. Several trees and large limbs were blown down near Highway 43/Pinecrest Drive on Rosborough Springs Road in Marshall.", "ts_dict_index": [13152, 13153, 13154]}
+{"event_id": 1056762, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-10-24 22:54:00", "end_date_time": "2022-10-24 22:54:00", "narrative": "A potent upper level low pressure system over New Mexico shifted east across Western and North Texas south of the Red River during the afternoon and evening hours of October 24th, which allowed for a dry line to mix east across Texas. A cold front extended east of this upper low over Eastern Oklahoma and Northeast Texas, with the dry line eventually overtaking the front but provided strong forcing for a linear line of showers and thunderstorms to develop during the evening and overnight hours as they entered East Texas. Although instability was limited given cooler conditions during the latter evening hours, strong shear resulted in a well-organized line of strong to severe thunderstorms along these surface features, producing damaging winds which downed trees across portions of East Texas before the storms weakened further upon entering Western Louisiana during the early morning hours on the 25th. Trees were blown down on Highway 476.", "ts_dict_index": [13161, 13162, 13163]}
+{"event_id": 916315, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 16:08:00", "end_date_time": "2020-08-25 16:08:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. A large tree was reported to be down on the 200 black of Porter Road in Rostraver Township.", "ts_dict_index": [13128, 13129, 13130]}
+{"event_id": 1137058, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-08-27 19:58:00", "end_date_time": "2023-08-27 19:58:00", "narrative": "Thunderstorms were observed developing along a nearly stalled frontal boundary and remnant outflows across parts of Southwest Arkansas, Northeast Texas, and Northern Louisiana on the afternoon of August 27th. Very strong diurnal heating was sufficient to erode a capping inversion aloft with around 1500-2000 J/kg of mean-layer instability supporting occasional stronger updrafts. Deep-layer vertical shear across much of the region was weak at generally less than 10-15 knots. This was still enough to support multi-cellular, pulse convection as the primary storm mode. Weak surface flow was also insufficient to support much cold pool propagation. Therefore, the primary severe risk was tied to individual pulse downdrafts as thunderstorms collapsed. This resulted in numerous damaging wind reports across parts of the region, including several reports in parts of Caddo Parish and one in Natchitoches Parish. Trees downed, power poles snapped and power lines downed along the 10000 block of East Kings Highway.", "ts_dict_index": [13167, 13168, 13169]}
+{"event_id": 1137056, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-08-27 19:55:00", "end_date_time": "2023-08-27 19:55:00", "narrative": "Thunderstorms were observed developing along a nearly stalled frontal boundary and remnant outflows across parts of Southwest Arkansas, Northeast Texas, and Northern Louisiana on the afternoon of August 27th. Very strong diurnal heating was sufficient to erode a capping inversion aloft with around 1500-2000 J/kg of mean-layer instability supporting occasional stronger updrafts. Deep-layer vertical shear across much of the region was weak at generally less than 10-15 knots. This was still enough to support multi-cellular, pulse convection as the primary storm mode. Weak surface flow was also insufficient to support much cold pool propagation. Therefore, the primary severe risk was tied to individual pulse downdrafts as thunderstorms collapsed. This resulted in numerous damaging wind reports across parts of the region, including several reports in parts of Caddo Parish and one in Natchitoches Parish. Trees and power lines downed along Dixie Garden Drive.", "ts_dict_index": [13173, 13174, 13175]}
+{"event_id": 1137059, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-08-27 20:25:00", "end_date_time": "2023-08-27 20:25:00", "narrative": "Thunderstorms were observed developing along a nearly stalled frontal boundary and remnant outflows across parts of Southwest Arkansas, Northeast Texas, and Northern Louisiana on the afternoon of August 27th. Very strong diurnal heating was sufficient to erode a capping inversion aloft with around 1500-2000 J/kg of mean-layer instability supporting occasional stronger updrafts. Deep-layer vertical shear across much of the region was weak at generally less than 10-15 knots. This was still enough to support multi-cellular, pulse convection as the primary storm mode. Weak surface flow was also insufficient to support much cold pool propagation. Therefore, the primary severe risk was tied to individual pulse downdrafts as thunderstorms collapsed. This resulted in numerous damaging wind reports across parts of the region, including several reports in parts of Caddo Parish and one in Natchitoches Parish. Trees and power lines downed along Ellerbe Road just north of the intersection with State Highway 175.", "ts_dict_index": [13170, 13171, 13172]}
+{"event_id": 947042, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-05-03 21:12:00", "end_date_time": "2021-05-03 21:12:00", "narrative": "Very warm, moist, and humid air spread back north across East Texas, North Louisiana, Southwest Arkansas, and Southeast Oklahoma during the afternoon hours of May 3rd, along a strong southerly low level jet. This resulted in a moderately unstable air mass across the region, which lingered during the evening hours across Southeast Oklahoma, ahead of a upper trough that moved across the Southern Plains. This trough enhanced large scale forcing along the dryline across Central Oklahoma and North Texas, with scattered strong to severe thunderstorms developing over these areas, which shifted east northeast into the unstable air across portions of Northeast Texas, Southeast Oklahoma, and Southwest Arkansas during the late evening and early morning hours of the 14th. Numerous reports of damaging winds were received across these areas before the storms diminished during the early morning hours of the 4th. Several trees were blown down on Highway 259.", "ts_dict_index": [13179, 13180, 13181]}
+{"event_id": 808948, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2019-04-07 14:30:00", "end_date_time": "2019-04-07 14:30:00", "narrative": "A warm front mixed north across portions of Deep East Texas to near the Louisiana/Arkansas border during the early morning hours of April 7th, but steep lapse rates aloft and a shortwave trough which ejected northeast over Northeast Texas, North Louisiana, and Southern Arkansas enhanced the development of scattered elevated strong to severe thunderstorms across portions of North Louisiana near and north of the front. Several reports of large hail were received from these storms during the early morning hours prior to daybreak, with additional strong to severe thunderstorms developing later in the afternoon ahead of the primary upper level trough that lifted east out of Southwest New Mexico and across much of Central Texas and Louisiana. These storms eventually diminished during the late afternoon hours once the upper trough shifted east of the region into the Lower Mississippi Valley. Several trees were blown down in and near the Oakland community.", "ts_dict_index": [13188, 13189, 13190]}
+{"event_id": 1137053, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-08-27 16:00:00", "end_date_time": "2023-08-27 16:00:00", "narrative": "Thunderstorms were observed developing along a nearly stalled frontal boundary and remnant outflows across parts of Southwest Arkansas, Northeast Texas, and Northern Louisiana on the afternoon of August 27th. Very strong diurnal heating was sufficient to erode a capping inversion aloft with around 1500-2000 J/kg of mean-layer instability supporting occasional stronger updrafts. Deep-layer vertical shear across much of the region was weak at generally less than 10-15 knots. This was still enough to support multi-cellular, pulse convection as the primary storm mode. Weak surface flow was also insufficient to support much cold pool propagation. Therefore, the primary severe risk was tied to individual pulse downdrafts as thunderstorms collapsed. This resulted in numerous damaging wind reports across parts of the region, including several reports in parts of Caddo Parish and one in Natchitoches Parish. Tin roofing was peeled back and removed from a structure near Highway 486 and U.S. Highway 71 between Clarence and Campti.", "ts_dict_index": [13164, 13165, 13166]}
+{"event_id": 990878, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2021-12-11 00:45:00", "end_date_time": "2021-12-11 00:45:00", "narrative": "A strong upper trough advanced east out of the Rockies and into the Central and Southern Plains during the afternoon and evening of December 10th, which reinforced a strong cold front southeast into the Ozarks and Southern Plains. An expansive area of very warm and moist air had spread north into all of the Four State Region into Southeast Oklahoma and Central Arkansas, with afternoon heating contributing to moderate instability within a strongly sheared air mass. Scattered strong to severe thunderstorms developed during the evening over portions of Northeast Texas and Southwest Arkansas ahead of the approaching cold front, before organizing into a narrow squall line and shifting southeast into North Louisiana during the late evening and early morning hours on the 11th. These storms produced a couple reports of damaging winds across portions of North Louisiana before diminishing. A tree was blown down onto Henry Williams Road.", "ts_dict_index": [13191, 13192, 13193]}
+{"event_id": 1124678, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-07-29 15:27:00", "end_date_time": "2023-07-29 15:27:00", "narrative": "A cold front approached Kentucky from the northwest overnight, and passed through the state during the afternoon and evening hours. An MCS that had developed along the front the previous day dropped southeastward overnight, with a defined outflow boundary on the WPC surface maps. These initial storms led to four warnings, and one report of wind damage from an NWS employee. The main action occurred later in the day, as eastern Kentucky found itself in a moist and unstable airmass just ahead of the incoming cold front. Most the the Jackson, KY warning forecast area was warned at some point, with the main impact being damaging winds as most of the storms formed into bowing segments with strongest winds along the front edge. Numerous reports of trees down were made across multiple counties through the early and mid-afternoon hours, before the quick-moving system pushed southeast out of the state. Dispatch reported a tree down and onto powerlines along KY-1643 near the community of Meece.", "ts_dict_index": [13182, 13183, 13184]}
+{"event_id": 1083324, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2023-02-16 16:10:00", "end_date_time": "2023-02-16 16:10:00", "narrative": "A low pressure center was slowly tracking into western Kentucky during the first part of the day on Wedensday, with a stationary front positioned along the Ohio River, and keeping much of eastern Kentucky in a warm, moist, and unstable airmass. Showers and thunderstorms were ongoing through much of the morning, leading to multiple flooding reports across the region. Then by the afternoon, the low pressure center had moved into Indiana, allowing the stationary front to lift north as a warm front, and a cold front to begin traversing the western half of the state. A more progressive line of strong showers and thunderstorms moved through eastern Kentucky ahead of this cold front, finally coming to an end after the cold front had passed through overnight. Multiple reports of downed trees and additional flooding were reported as heavy rain and strong winds complimented some of these storms. A powerline was reported down on West Hwy-80 near the town of Nancy.", "ts_dict_index": [13185, 13186, 13187]}
+{"event_id": 916291, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "WESTMORELAND", "begin_date_time": "2020-08-25 14:03:00", "end_date_time": "2020-08-25 14:03:00", "narrative": "The latest shortwave in a series of such disturbances passed across the region during the afternoon of August 25th.  The Storm Prediction Center painted the Upper Ohio Valley with a risk for scattered severe storms. The storms began to develop in the lee of Lake Erie around midday.  The storms were able to take advantage of a frontal boundary sagging towards I-70. Shear and increasing instability favored multicells and short bowing segments initially.  Activity was eventually able to congeal into a linear MCS as it crossed the Mason-Dixon Line during the evening hours.||Most of the severe activity in southwest Pennsylvania occurred to the north and east of Pittsburgh, running from Butler County southeastward to Westemoreland County.  Many instances of tree damage were reported from thunderstorm wind gusts, with a few instances of minor structural damage.  Isolated large hail reports were also received. A tree was reported to be blown down off of Deep Hollow Road.", "ts_dict_index": [13137, 13138, 13139]}
+{"event_id": 990879, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-12-11 01:00:00", "end_date_time": "2021-12-11 01:00:00", "narrative": "A strong upper trough advanced east out of the Rockies and into the Central and Southern Plains during the afternoon and evening of December 10th, which reinforced a strong cold front southeast into the Ozarks and Southern Plains. An expansive area of very warm and moist air had spread north into all of the Four State Region into Southeast Oklahoma and Central Arkansas, with afternoon heating contributing to moderate instability within a strongly sheared air mass. Scattered strong to severe thunderstorms developed during the evening over portions of Northeast Texas and Southwest Arkansas ahead of the approaching cold front, before organizing into a narrow squall line and shifting southeast into North Louisiana during the late evening and early morning hours on the 11th. These storms produced a couple reports of damaging winds across portions of North Louisiana before diminishing. Two trees, a flag pole, and large limbs were blown down along Barron Road in far Southern Caddo Parish.", "ts_dict_index": [13194, 13195, 13196]}
+{"event_id": 1056477, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-11 20:58:00", "end_date_time": "2022-09-11 20:58:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. The Phoenix-Mesa Gateway Airport measured a wind gust of 75 mph.", "ts_dict_index": [13203, 13204, 13205]}
+{"event_id": 1056484, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-11 21:10:00", "end_date_time": "2022-09-11 21:10:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. Social media pictures showed multiple large tree downed across East Mesa, including one tree falling onto a house. Winds were estimated at around 70 mph. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [13200, 13201, 13202]}
+{"event_id": 1056478, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-11 21:15:00", "end_date_time": "2022-09-11 21:15:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. The Mesa Falcon Field Airport measured a wind gust of 58 mph.", "ts_dict_index": [13212, 13213, 13214]}
+{"event_id": 1056482, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-11 21:18:00", "end_date_time": "2022-09-11 21:18:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. Social media picture showed large tree uprooted against a 3 three story apartment complex in the area of North 16th street and Camelback Road. Winds were estimated at around 70 mph. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [13215, 13216, 13217]}
+{"event_id": 1056483, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-11 21:10:00", "end_date_time": "2022-09-11 21:10:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. A large uprooted tree fell onto a couple of cars along South Ellsworth Road between East Southern Avenue and East Broadway Road in East Mesa. There were also reports of many damaged or destroyed sheet metal car ports in the area. A small metal shed was also thrown and destroyed. Winds were estimated at around 70 mph. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [13218, 13219, 13220]}
+{"event_id": 1056470, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-11 19:55:00", "end_date_time": "2022-09-11 19:55:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. The AK-Chin Regional Airport, located northwest of Casa Grande, measured a wind gust of 58 mph.", "ts_dict_index": [13224, 13225, 13226]}
+{"event_id": 1056476, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-11 20:53:00", "end_date_time": "2022-09-11 20:53:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. Phoenix Sky Harbor Airport ASOS measured a wind gust of 86 mph. This wind gust speed was investigated further as it was considered suspect, however NWS meteorologists determined there was not enough evidence to disprove this measurement. Centerfield winds, a 30 meter wind sensor located just over half a mile north of the ASOS, measured a 76 mph wind gust around the same time as the ASOS. The City of Phoenix Aviation Department shared a report with images that mentioned/showed more than a dozen downed trees, damage to some fencing, cargo containers that were damaged after nearly being blown into a building, at least one downed light pole, and a baggage cart that was blown into and damaged a blast fence. There was also damage to the 24th Street Sky Train station with some broken glass windows at one of the entrances and a small section of outer side paneling that was peeled off. Sky Harbor Airport was in a Ground Stop from 2125MST to 2154MST. No injuries were reported.", "ts_dict_index": [13221, 13222, 13223]}
+{"event_id": 1057817, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-11 20:46:00", "end_date_time": "2022-09-11 20:46:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. The City of Queen Creek posted on social media saying to avoid the area of Barnes Parkway and 212th Street due to a tree blown down across the road. Time and wind speed estimated from radar.", "ts_dict_index": [13209, 13210, 13211]}
+{"event_id": 1058651, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-11 19:57:00", "end_date_time": "2022-09-11 20:00:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. A local utility company reported 2 downed power poles in 2 locations east of Maricopa. Winds were estimated around 60 mph. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [13197, 13198, 13199]}
+{"event_id": 1137054, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-08-27 19:35:00", "end_date_time": "2023-08-27 19:35:00", "narrative": "Thunderstorms were observed developing along a nearly stalled frontal boundary and remnant outflows across parts of Southwest Arkansas, Northeast Texas, and Northern Louisiana on the afternoon of August 27th. Very strong diurnal heating was sufficient to erode a capping inversion aloft with around 1500-2000 J/kg of mean-layer instability supporting occasional stronger updrafts. Deep-layer vertical shear across much of the region was weak at generally less than 10-15 knots. This was still enough to support multi-cellular, pulse convection as the primary storm mode. Weak surface flow was also insufficient to support much cold pool propagation. Therefore, the primary severe risk was tied to individual pulse downdrafts as thunderstorms collapsed. This resulted in numerous damaging wind reports across parts of the region, including several reports in parts of Caddo Parish and one in Natchitoches Parish. Tree downed between Blanchard and Latex.", "ts_dict_index": [13176, 13177, 13178]}
+{"event_id": 975369, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2021-09-01 18:25:00", "end_date_time": "2021-09-01 18:25:00", "narrative": "A weak surface trough backdoored southwest into North Central Louisiana during the late afternoon and evening hours of September 1st, which was reinforced by a weakness aloft over the Lower Mississippi Valley rounding the upper ridge anchored over the Central and Southern Plains. Compressional warming ahead of this surface trough resulted in temperatures climbing into the upper 90s to near 100 degrees across North Central Louisiana, contributing to moderate to strong instability over this area. This instability, and the weakness aloft, resulted in strong vertical forcing such that scattered strong to severe thunderstorms developed just ahead of the surface trough across Southwest Arkansas and North Central Louisiana, producing damaging winds which downed trees across portions of Union and Ouachita Parishes before weakening during the evening with the gradual loss of instability. A tree fell onto a house in the Rocky Branch community.", "ts_dict_index": [13236, 13237, 13238]}
+{"event_id": 1056486, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-11 20:30:00", "end_date_time": "2022-09-11 20:30:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. Trained spotter measured a 60 mph gust along South Halsted Drive in Sun Lakes.", "ts_dict_index": [13233, 13234, 13235]}
+{"event_id": 1056471, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-09-11 20:24:00", "end_date_time": "2022-09-11 20:24:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. Chandler Municipal Airport measured a wind gust of 60 mph.", "ts_dict_index": [13230, 13231, 13232]}
+{"event_id": 823331, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-05-18 12:20:00", "end_date_time": "2019-05-18 12:20:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas and Southeast Oklahoma during the afternoon. As a result, trees were downed across portions of Western and Southern McCurtain County Oklahoma before spreading east into Southwest Arkansas. Trees were downed near Pine Creek Lake.", "ts_dict_index": [13260, 13261, 13262]}
+{"event_id": 1119597, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2023-08-25 21:40:00", "end_date_time": "2023-08-25 21:55:00", "narrative": "Scattered instances of strong to marginally severe thunderstorms occurred along the Nebraska-Kansas state line during the afternoon and evening hours of August 25th. Thunderstorms initiated along a southward moving cold front that stalled near the state line during the mid to late afternoon. A brief, transient supercell produced marginally severe hail in Nuckolls County around 5 PM CDT, but the main area of severe weather transpired in Thayer County from a complex of thunderstorms that developed in northwest Kansas then moved eastward along the state line. This activity was sub-severe from 8-10 PM CDT, but then briefly reintensified around 10:30 PM CDT and produced a swath of severe wind. Wind gusts in the 60-65 MPH range were reported, along with crop damage and roof damage to a hotel. The severe portion of the thunderstorm complex exited Thayer County shortly after 11 PM CDT. A wind gust of 63 MPH was measured by a mesonet station located three miles south-southeast of Gilead. Emergency management reported crop damage from Hubbell to Gilead, and minor roof damage to a hotel in Gilead.", "ts_dict_index": [13245, 13246, 13247]}
+{"event_id": 823332, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2019-05-18 12:43:00", "end_date_time": "2019-05-18 12:43:00", "narrative": "A shortwave trough entered the Southern Plains during the morning hours of May 18th, and began to take on a negative tilt as it approached East Texas during the afternoon and evening. Meanwhile, an associated cold front began to shift southeast across Central Oklahoma and portions of North Texas, with the dry line having mixed east ahead of the front into Central Texas. Warm, moist, and unstable air surged north across the warm sector of Northern and Eastern Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana, with large scale forcing spreading east across this area ahead of the trough such that numerous severe thunderstorms with damaging winds developed across East Texas and Southeast Oklahoma during the afternoon. As a result, trees were downed across portions of Western and Southern McCurtain County Oklahoma before spreading east into Southwest Arkansas. A tree was downed in Wright City.", "ts_dict_index": [13257, 13258, 13259]}
+{"event_id": 1057816, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-11 21:03:00", "end_date_time": "2022-09-11 21:03:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. Social media photo shows a sheet metal car port, that was torn off of a home, wrapped around a tree near Ironwood Drive and Superstition Boulevard. Timing and wind speed estimated based on radar.", "ts_dict_index": [13227, 13228, 13229]}
+{"event_id": 1119594, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2023-08-25 22:00:00", "end_date_time": "2023-08-25 22:00:00", "narrative": "Scattered instances of strong to marginally severe thunderstorms occurred along the Nebraska-Kansas state line during the afternoon and evening hours of August 25th. Thunderstorms initiated along a southward moving cold front that stalled near the state line during the mid to late afternoon. A brief, transient supercell produced marginally severe hail in Nuckolls County around 5 PM CDT, but the main area of severe weather transpired in Thayer County from a complex of thunderstorms that developed in northwest Kansas then moved eastward along the state line. This activity was sub-severe from 8-10 PM CDT, but then briefly reintensified around 10:30 PM CDT and produced a swath of severe wind. Wind gusts in the 60-65 MPH range were reported, along with crop damage and roof damage to a hotel. The severe portion of the thunderstorm complex exited Thayer County shortly after 11 PM CDT. A wind gust of 62 MPH was measured by a mesonet station located four miles south-southeast of Deshler.", "ts_dict_index": [13251, 13252, 13253]}
+{"event_id": 1119593, "event_type": "Thunderstorm Wind", "state": "NEBRASKA", "cz_name": "THAYER", "begin_date_time": "2023-08-25 21:55:00", "end_date_time": "2023-08-25 21:55:00", "narrative": "Scattered instances of strong to marginally severe thunderstorms occurred along the Nebraska-Kansas state line during the afternoon and evening hours of August 25th. Thunderstorms initiated along a southward moving cold front that stalled near the state line during the mid to late afternoon. A brief, transient supercell produced marginally severe hail in Nuckolls County around 5 PM CDT, but the main area of severe weather transpired in Thayer County from a complex of thunderstorms that developed in northwest Kansas then moved eastward along the state line. This activity was sub-severe from 8-10 PM CDT, but then briefly reintensified around 10:30 PM CDT and produced a swath of severe wind. Wind gusts in the 60-65 MPH range were reported, along with crop damage and roof damage to a hotel. The severe portion of the thunderstorm complex exited Thayer County shortly after 11 PM CDT. A wind gust of 62 MPH was measured by a mesonet station located three miles north of Chester.", "ts_dict_index": [13254, 13255, 13256]}
+{"event_id": 1137065, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-08-27 19:05:00", "end_date_time": "2023-08-27 19:05:00", "narrative": "Thunderstorms were observed developing along a nearly stalled frontal boundary and remnant outflows across parts of Southwest Arkansas, Northeast Texas, and Northern Louisiana on the afternoon of August 27th. Very strong diurnal heating was sufficient to erode a capping inversion aloft with around 1500-2000 J/kg of mean-layer instability supporting occasional stronger updrafts. Deep-layer vertical shear across much of the region was weak at generally less than 10-15 knots. This was still enough to support multi-cellular, pulse convection as the primary storm mode. Weak surface flow was also insufficient to support much cold pool propagation. Therefore, the primary severe risk was tied to individual pulse downdrafts as thunderstorms collapsed. This resulted in numerous damaging wind reports across parts of the region, including a few isolated reports in Rusk and Harrison County. Tree downed along Cypress Drive in the Uncertain community.", "ts_dict_index": [13248, 13249, 13250]}
+{"event_id": 1141566, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-09-06 15:36:00", "end_date_time": "2023-09-06 15:36:00", "narrative": "Convection developed along a quasi-stationary surface front extending from Central and Southwest Arkansas into Southeast Oklahoma on September 6th. Ahead of this activity, low-level lapse rates continued to steepen with rich pre-frontal boundary-layer moisture (mid to upper 70s surface dew points) in place. While large-scale ascent was generally lacking across the region, strong surface heating and destabilization amid the low-level frontal circulation further supported additional convective initiation along the front with a belt of moderate northwesterly mid-level flow over the frontal zone (around 30 knots of bulk shear). This resulted in some weakly organized thunderstorms after updrafts became established and sustained with the threat of isolated large hail and damaging wind gusts. One report of damaging wind gusts was reported at Beavers Bend State Park in McCurtain County. Trees downed along Highway 259A in Beavers Bend State Park.", "ts_dict_index": [13206, 13207, 13208]}
+{"event_id": 955784, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-06-14 20:15:00", "end_date_time": "2021-06-14 20:15:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. Wires were downed in Florence on 6th Ave. Time estimated from radar.", "ts_dict_index": [13263, 13264, 13265]}
+{"event_id": 955783, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-06-14 20:15:00", "end_date_time": "2021-06-14 20:15:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. Wires were downed at the Pointe Breeze Apartment Complex in Bordentown. Time estimated from radar.", "ts_dict_index": [13272, 13273, 13274]}
+{"event_id": 955773, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-06-14 17:47:00", "end_date_time": "2021-06-14 17:47:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. Trees and wires were downed near Apple Ln. Time estimated from radar.", "ts_dict_index": [13287, 13288, 13289]}
+{"event_id": 955775, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-06-14 19:16:00", "end_date_time": "2021-06-14 19:16:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. Tree limbs were downed near Depot St. Time estimated from radar.", "ts_dict_index": [13269, 13270, 13271]}
+{"event_id": 955776, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-06-14 19:39:00", "end_date_time": "2021-06-14 19:39:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. Downed tree limbs blocked Haverford Rd near Remington Rd. Time estimated from radar.", "ts_dict_index": [13284, 13285, 13286]}
+{"event_id": 955777, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-06-14 19:55:00", "end_date_time": "2021-06-14 19:55:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. A tree was downed on Byberry Rd. Time estimated from radar.", "ts_dict_index": [13266, 13267, 13268]}
+{"event_id": 955774, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-14 18:55:00", "end_date_time": "2021-06-14 18:55:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. A tree was downed on Old Kings Hwy. Time estimated from radar.", "ts_dict_index": [13281, 13282, 13283]}
+{"event_id": 955770, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-14 19:12:00", "end_date_time": "2021-06-14 19:12:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. Trees and wires were downed near Route 202 in Malvern. Time estimated from radar.", "ts_dict_index": [13275, 13276, 13277]}
+{"event_id": 955769, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-06-14 19:25:00", "end_date_time": "2021-06-14 19:25:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. Trees and wires were downed on Montgomery Ave. Time estimated from radar.", "ts_dict_index": [13290, 13291, 13292]}
+{"event_id": 1137064, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-08-27 13:48:00", "end_date_time": "2023-08-27 13:48:00", "narrative": "Thunderstorms were observed developing along a nearly stalled frontal boundary and remnant outflows across parts of Southwest Arkansas, Northeast Texas, and Northern Louisiana on the afternoon of August 27th. Very strong diurnal heating was sufficient to erode a capping inversion aloft with around 1500-2000 J/kg of mean-layer instability supporting occasional stronger updrafts. Deep-layer vertical shear across much of the region was weak at generally less than 10-15 knots. This was still enough to support multi-cellular, pulse convection as the primary storm mode. Weak surface flow was also insufficient to support much cold pool propagation. Therefore, the primary severe risk was tied to individual pulse downdrafts as thunderstorms collapsed. This resulted in numerous damaging wind reports across parts of the region, including a few isolated reports in Rusk and Harrison County. A large tree downed near the intersection of County Road 3206 and County Road 3155 just west of Mount Enterprise.", "ts_dict_index": [13242, 13243, 13244]}
+{"event_id": 925241, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-11-15 21:22:00", "end_date_time": "2020-11-15 21:22:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Measured by a Weatherflow gauge.", "ts_dict_index": [13311, 13312, 13313]}
+{"event_id": 925238, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-11-15 21:26:00", "end_date_time": "2020-11-15 21:26:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. ", "ts_dict_index": [13314, 13315, 13316]}
+{"event_id": 925118, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:40:00", "end_date_time": "2020-11-15 18:40:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A utility pole and wires were downed near Spirit Ct and Park Rd. Time estimated from radar.", "ts_dict_index": [13320, 13321, 13322]}
+{"event_id": 925117, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:39:00", "end_date_time": "2020-11-15 18:39:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree and wires were downed near Church Rd and New Holland Rd. Time estimated from radar.", "ts_dict_index": [13317, 13318, 13319]}
+{"event_id": 925140, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:54:00", "end_date_time": "2020-11-15 18:54:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Sunset Hill Rd. Time estimated from radar.", "ts_dict_index": [13305, 13306, 13307]}
+{"event_id": 955786, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-06-14 22:21:00", "end_date_time": "2021-06-14 22:21:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. Several reports of power lines down in the Bass River area. Time estimated from radar.", "ts_dict_index": [13293, 13294, 13295]}
+{"event_id": 925269, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-11-15 20:20:00", "end_date_time": "2020-11-15 20:20:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on the US-130 southbound ramp from NJ-90. Time estimated from radar.", "ts_dict_index": [13296, 13297, 13298]}
+{"event_id": 925138, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:53:00", "end_date_time": "2020-11-15 18:53:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree and wires were downed near Covered Bridge Rd and Memorial Hwy in Oley Twp. Time estimated from radar.", "ts_dict_index": [13308, 13309, 13310]}
+{"event_id": 925193, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-15 19:40:00", "end_date_time": "2020-11-15 19:40:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Bearhill Rd near East Central Ave. Time estimated from radar.", "ts_dict_index": [13323, 13324, 13325]}
+{"event_id": 925173, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-15 19:14:00", "end_date_time": "2020-11-15 19:14:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Little Conestoga Rd near Mapleflower Rd. Time estimated from radar.", "ts_dict_index": [13299, 13300, 13301]}
+{"event_id": 1056495, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2022-09-11 19:42:00", "end_date_time": "2022-09-11 19:45:00", "narrative": "The remnant mid-level circulation of what was Tropical Cyclone Kay was located over southern California. This led to southerly flow across Arizona, which helped increased moisture and instability with moisture values peaking at around 1.5 and MLCAPE values peaking at around 1000 J/KG. Strong to severe thunderstorms developed across southeast Arizona, near the Tucson area, during the late afternoon hours of the 11th and then progressed northward towards the Phoenix metro during the evening hours, resulting in widespread severe downburst winds and blowing dust as well as isolated flash flooding. The Phoenix Sky Harbor Airport reported a peak wind gust of 86 mph at 2053 MST. Additional storms then developed across western Maricopa County, extending into La Paz County, during the early morning hours of the 12th with heavy rainfall leading to flash flooding become the biggest threat. A local utility company reported 4 power poles were downed in a couple locations north of Stanfield. Winds were estimated at around 60 mph. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [13239, 13240, 13241]}
+{"event_id": 925143, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:56:00", "end_date_time": "2020-11-15 18:56:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed near the intersection of Laurel Rd and Pine Rd. Time estimated from radar.", "ts_dict_index": [13326, 13327, 13328]}
+{"event_id": 955772, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-14 19:00:00", "end_date_time": "2021-06-14 19:00:00", "narrative": "A cold front and associated weak area of surface low pressure approached the mid-Atlantic on June 14. A seasonably warm air mass was present ahead of the front, allowing a moderate amount of instability to build over the mid-Atlantic. Moderate to strong wind shear was also present thanks to the presence of a robust upper level disturbance approaching the region. This disturbance, along with the front, provided sufficient forcing for scattered to widespread convection to develop in the interior mid-Atlantic and propagate towards the coast. Some storms became strong to severe in the rather favorable convective environment, posing a primary risk of damaging winds along with some hail. Convection also continued well into the overnight over portions of the area thanks to the good shear and forcing, with convection eventually moving offshore in the pre-dawn hours of the 15th. A tree was downed on Sugars Bridge Rd near Alton. Time estimated from radar.", "ts_dict_index": [13278, 13279, 13280]}
+{"event_id": 925237, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-11-15 21:24:00", "end_date_time": "2020-11-15 21:24:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Measured at Weather Underground site knjlongb59.", "ts_dict_index": [13332, 13333, 13334]}
+{"event_id": 925111, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:33:00", "end_date_time": "2020-11-15 18:33:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Measured in a Lowe's parking lot with a Kestrel 5000. Power flashes were observed.", "ts_dict_index": [13368, 13369, 13370]}
+{"event_id": 925132, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:46:00", "end_date_time": "2020-11-15 18:46:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. An mPing report of trees and wires down in this area. Time estimated from radar.", "ts_dict_index": [13344, 13345, 13346]}
+{"event_id": 925212, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-15 20:00:00", "end_date_time": "2020-11-15 20:00:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Several trees were downed in the area. Time estimated from radar.", "ts_dict_index": [13347, 13348, 13349]}
+{"event_id": 925136, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:52:00", "end_date_time": "2020-11-15 18:52:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed near West Philadelphia Ave and School House Rd. Time estimated from radar.", "ts_dict_index": [13338, 13339, 13340]}
+{"event_id": 925113, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:35:00", "end_date_time": "2020-11-15 18:35:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A spotter estimated wind gusts of 60 mph with downed tree limbs in the area.", "ts_dict_index": [13365, 13366, 13367]}
+{"event_id": 925194, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-15 19:41:00", "end_date_time": "2020-11-15 19:41:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. The roof was partially blown off of a building in Norristown. Time estimated.", "ts_dict_index": [13329, 13330, 13331]}
+{"event_id": 925189, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-15 19:36:00", "end_date_time": "2020-11-15 19:36:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Eagleville Rd. Time estimated from radar.", "ts_dict_index": [13359, 13360, 13361]}
+{"event_id": 925177, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-15 19:15:00", "end_date_time": "2020-11-15 19:15:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Power poles and lines were downed near West Branch Rd and Wild Run Rd. Time estimated from radar.", "ts_dict_index": [13350, 13351, 13352]}
+{"event_id": 925180, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-15 19:18:00", "end_date_time": "2020-11-15 19:18:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed near Culbertson Run Rd. Time estimated from radar.", "ts_dict_index": [13335, 13336, 13337]}
+{"event_id": 925115, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:30:00", "end_date_time": "2020-11-15 18:30:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Irish Creek Rd near Bellemans Church Rd. Time estimated from radar.", "ts_dict_index": [13362, 13363, 13364]}
+{"event_id": 925186, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-15 19:26:00", "end_date_time": "2020-11-15 19:26:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Longfields Way near Dorian Mill Rd. Time estimated from radar.", "ts_dict_index": [13374, 13375, 13376]}
+{"event_id": 925187, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-15 19:36:00", "end_date_time": "2020-11-15 19:36:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Frazer Rd near King Rd. Time estimated from radar.", "ts_dict_index": [13371, 13372, 13373]}
+{"event_id": 925184, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-15 19:24:00", "end_date_time": "2020-11-15 19:24:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Trees and wires were downed near the Route 30 Bypass near Route 340 and Bondsville Rd. Time estimated from radar.", "ts_dict_index": [13353, 13354, 13355]}
+{"event_id": 925133, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-11-15 18:46:00", "end_date_time": "2020-11-15 18:46:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed into wires near Furnace Rd. Time estimated from radar.", "ts_dict_index": [13356, 13357, 13358]}
+{"event_id": 925190, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-11-15 19:40:00", "end_date_time": "2020-11-15 19:40:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed in wires near Keystone Dr. Time estimated from radar.", "ts_dict_index": [13302, 13303, 13304]}
+{"event_id": 925234, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-11-15 21:14:00", "end_date_time": "2020-11-15 21:14:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Measured at Weather Underground site knjlongb85.", "ts_dict_index": [13383, 13384, 13385]}
+{"event_id": 925232, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-11-15 21:09:00", "end_date_time": "2020-11-15 21:09:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Measured at a Weatherflow gauge.", "ts_dict_index": [13380, 13381, 13382]}
+{"event_id": 925185, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-15 19:24:00", "end_date_time": "2020-11-15 19:24:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Schuykill Rd near Reitnour Rd. Time estimated from radar.", "ts_dict_index": [13377, 13378, 13379]}
+{"event_id": 925211, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-15 20:00:00", "end_date_time": "2020-11-15 20:00:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A large falling tree limb brought down wires onto Terwood Rd. Time estimated from radar.", "ts_dict_index": [13341, 13342, 13343]}
+{"event_id": 925278, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-11-15 21:06:00", "end_date_time": "2020-11-15 21:06:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Tree limbs and wires were downed in the area. Time estimated from radar.", "ts_dict_index": [13425, 13426, 13427]}
+{"event_id": 925227, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-11-15 20:30:00", "end_date_time": "2020-11-15 20:30:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Measured at Moorestown NJ Weathernet gauge.", "ts_dict_index": [13398, 13399, 13400]}
+{"event_id": 925279, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-11-15 21:18:00", "end_date_time": "2020-11-15 21:18:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on the Garden State Parkway near Exit 74. Time estimated from radar.", "ts_dict_index": [13431, 13432, 13433]}
+{"event_id": 925124, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:44:00", "end_date_time": "2020-11-15 18:44:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Seyfert Dr. Time estimated from radar.", "ts_dict_index": [13440, 13441, 13442]}
+{"event_id": 925224, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2020-11-15 20:10:00", "end_date_time": "2020-11-15 20:10:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Measured at Pennsauken NJ Weathernet gauge.", "ts_dict_index": [13392, 13393, 13394]}
+{"event_id": 925126, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:44:00", "end_date_time": "2020-11-15 18:44:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed onto a car on Madison St. No injuries. Time estimated from radar.", "ts_dict_index": [13437, 13438, 13439]}
+{"event_id": 925120, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:42:00", "end_date_time": "2020-11-15 18:42:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree and wires were downed near Memorial Highway and Erhardt Rd. Time estimated from radar.", "ts_dict_index": [13407, 13408, 13409]}
+{"event_id": 925129, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:45:00", "end_date_time": "2020-11-15 18:45:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree and wires were downed near Morgantown Rd. Time estimated from radar.", "ts_dict_index": [13416, 13417, 13418]}
+{"event_id": 925127, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:44:00", "end_date_time": "2020-11-15 18:44:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Friedensberg Rd. Time estimated from radar.", "ts_dict_index": [13434, 13435, 13436]}
+{"event_id": 925202, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-15 19:52:00", "end_date_time": "2020-11-15 19:52:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Several reports of downed tree limbs in Lower Merion Twp. Time estimated from radar.", "ts_dict_index": [13428, 13429, 13430]}
+{"event_id": 925226, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-11-15 20:24:00", "end_date_time": "2020-11-15 20:24:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. NWS meteorologists estimated 60 mph wind gusts at the Weather Forecast Office with the squall line passage.", "ts_dict_index": [13395, 13396, 13397]}
+{"event_id": 925196, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-15 19:44:00", "end_date_time": "2020-11-15 19:44:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Berkshire Dr near Pugh Rd. Time estimated from radar.", "ts_dict_index": [13404, 13405, 13406]}
+{"event_id": 925198, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-15 19:44:00", "end_date_time": "2020-11-15 19:44:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Richards Rd near Thomas Rd. Time estimated from radar.", "ts_dict_index": [13401, 13402, 13403]}
+{"event_id": 925156, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-11-15 19:04:00", "end_date_time": "2020-11-15 19:04:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed into a vehicle. No injuries or entrapments occurred. Time estimated.", "ts_dict_index": [13389, 13390, 13391]}
+{"event_id": 925119, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-11-15 18:41:00", "end_date_time": "2020-11-15 18:41:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed in the area along with a power outage. Time estimated.", "ts_dict_index": [13410, 13411, 13412]}
+{"event_id": 925131, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-11-15 18:45:00", "end_date_time": "2020-11-15 18:45:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A 13 inch diameter tree limb was downed. Time estimated from radar.", "ts_dict_index": [13422, 13423, 13424]}
+{"event_id": 925157, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-11-15 19:05:00", "end_date_time": "2020-11-15 19:05:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed into wires, which were still energized as of the report. Time estimated.", "ts_dict_index": [13413, 13414, 13415]}
+{"event_id": 925281, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-11-15 21:20:00", "end_date_time": "2020-11-15 21:20:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was uprooted in West Creek. Report via social media with a photo. Time estimated from radar.", "ts_dict_index": [13386, 13387, 13388]}
+{"event_id": 925275, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-11-15 21:00:00", "end_date_time": "2020-11-15 21:00:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Several reports of downed tree limbs and power lines in this area. Time estimated from radar.", "ts_dict_index": [13446, 13447, 13448]}
+{"event_id": 925231, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-11-15 20:54:00", "end_date_time": "2020-11-15 20:54:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Measured at a HADS gauge.", "ts_dict_index": [13470, 13471, 13472]}
+{"event_id": 925135, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:48:00", "end_date_time": "2020-11-15 18:48:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. An NWS storm survey was conducted on a severe straight-line wind |event which occurred on Sunday evening in Maxatawny Township in |Berks County PA about 4 miles ENE of Kutztown. A severe surge of |winds began along Kunkel Road where substantial damage occurred |to a single family home and the surrounding property. Several |trees were snapped or uprooted and yard toys were tossed up to 200|yards away from the property. The winds partially lifted the |front porch roof, but did not completely blow it off the house. |The winds swept across nearby fields and struck a large barn, |uprooting and snapping a few more trees along the way. The barn |was almost completely destroyed, suffering outer wall collapse and|partial roof removal. A few trees around the barn were also |uprooted or snapped and a nearby shed was tossed off its |foundation and completely destroyed. Some minor cosmetic damage |occurred to the adjacent farm home. Nearby fields were strewn with|tree and structural debris as well as debris from the yard toys.||The winds continued across a rural area for about another 1.5|miles sweeping across fields and snapping trees along the way.|Most notably, a line of trees near Grim Road over 100 yards in |width were all snapped. Some unharvested, dead corn fields along|Albright Road suffered large swaths of blown over corn stalks. A|home near the downed field of corn stalks suffered some minor|cosmetic damage. The surge of winds ended near a farm on Route |863 where a barn roof was partially removed and a tree was |snapped.", "ts_dict_index": [13458, 13459, 13460]}
+{"event_id": 925210, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-15 19:54:00", "end_date_time": "2020-11-15 19:54:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree and wires were downed on Ambler Rd near Ellerslie Ave. Time estimated from radar.", "ts_dict_index": [13449, 13450, 13451]}
+{"event_id": 925159, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-11-15 19:06:00", "end_date_time": "2020-11-15 19:06:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Layfield Rd near Deep Creek Rd. Time estimated from radar.", "ts_dict_index": [13467, 13468, 13469]}
+{"event_id": 925228, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2020-11-15 20:30:00", "end_date_time": "2020-11-15 20:30:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Measured at Columbus NJ Weathernet gauge.", "ts_dict_index": [13461, 13462, 13463]}
+{"event_id": 925166, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-11-15 19:12:00", "end_date_time": "2020-11-15 19:12:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed on Scholl Rd near West Schuylkill Rd. Time estimated from radar.", "ts_dict_index": [13455, 13456, 13457]}
+{"event_id": 925163, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-11-15 19:10:00", "end_date_time": "2020-11-15 19:10:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. An mPing report of trees uprooted or snapped. Time estimated from radar.", "ts_dict_index": [13452, 13453, 13454]}
+{"event_id": 925130, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-11-15 18:45:00", "end_date_time": "2020-11-15 18:45:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree and wires were downed on Stonehenge Dr. Time estimated from radar.", "ts_dict_index": [13419, 13420, 13421]}
+{"event_id": 1090216, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-03-31 15:25:00", "end_date_time": "2023-03-31 15:25:00", "narrative": "Elevated convection initially developed early in the day on March 31st within a plume of rich low-level moisture and along the periphery of a lead shortwave moving across the Southern Plains. By early afternoon, more widespread severe convection developed and expanded farther along an eastward advancing dryline and associated cold front from Northeast Texas into Southeast Oklahoma and eventually Southwest Arkansas into Northern Louisiana. Strong surface heating within a moist low-level environment resulted in MLCAPE values of 1500-2500 J/kg across the region along with deep layer shear of 50-70 knots, more than sufficient for organized thunderstorms. In this type environment, strong large-scale ascent also promoted some supercell thunderstorms as well with numerous reports of large hail and damaging wind gusts across East Texas during the afternoon and evening hours. Tree limbs downed near Grove Club Lake just south of Whitehouse.", "ts_dict_index": [13476, 13477, 13478]}
+{"event_id": 1090214, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2023-03-31 15:07:00", "end_date_time": "2023-03-31 15:07:00", "narrative": "Elevated convection initially developed early in the day on March 31st within a plume of rich low-level moisture and along the periphery of a lead shortwave moving across the Southern Plains. By early afternoon, more widespread severe convection developed and expanded farther along an eastward advancing dryline and associated cold front from Northeast Texas into Southeast Oklahoma and eventually Southwest Arkansas into Northern Louisiana. Strong surface heating within a moist low-level environment resulted in MLCAPE values of 1500-2500 J/kg across the region along with deep layer shear of 50-70 knots, more than sufficient for organized thunderstorms. In this type environment, strong large-scale ascent also promoted some supercell thunderstorms as well with numerous reports of large hail and damaging wind gusts across East Texas during the afternoon and evening hours. Trees damaged and limbs down on Copeland Road and Paluxy Drive in south Tyler.", "ts_dict_index": [13473, 13474, 13475]}
+{"event_id": 959405, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-08 17:07:00", "end_date_time": "2021-07-08 17:07:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. A downed tree blocked E Prospect Ave at 10th St. Time estimated from radar.", "ts_dict_index": [13488, 13489, 13490]}
+{"event_id": 1090217, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-03-31 16:20:00", "end_date_time": "2023-03-31 16:20:00", "narrative": "Elevated convection initially developed early in the day on March 31st within a plume of rich low-level moisture and along the periphery of a lead shortwave moving across the Southern Plains. By early afternoon, more widespread severe convection developed and expanded farther along an eastward advancing dryline and associated cold front from Northeast Texas into Southeast Oklahoma and eventually Southwest Arkansas into Northern Louisiana. Strong surface heating within a moist low-level environment resulted in MLCAPE values of 1500-2500 J/kg across the region along with deep layer shear of 50-70 knots, more than sufficient for organized thunderstorms. In this type environment, strong large-scale ascent also promoted some supercell thunderstorms as well with numerous reports of large hail and damaging wind gusts across East Texas during the afternoon and evening hours. Trees downed on Hendricks Lake Road and North Hill Street.", "ts_dict_index": [13482, 13483, 13484]}
+{"event_id": 1090218, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2023-03-31 17:06:00", "end_date_time": "2023-03-31 17:06:00", "narrative": "Elevated convection initially developed early in the day on March 31st within a plume of rich low-level moisture and along the periphery of a lead shortwave moving across the Southern Plains. By early afternoon, more widespread severe convection developed and expanded farther along an eastward advancing dryline and associated cold front from Northeast Texas into Southeast Oklahoma and eventually Southwest Arkansas into Northern Louisiana. Strong surface heating within a moist low-level environment resulted in MLCAPE values of 1500-2500 J/kg across the region along with deep layer shear of 50-70 knots, more than sufficient for organized thunderstorms. In this type environment, strong large-scale ascent also promoted some supercell thunderstorms as well with numerous reports of large hail and damaging wind gusts across East Texas during the afternoon and evening hours. Trees reported down just east of Laneville near FM Road 2496 at County Road 3162, FM Road 2496 near FM Road 1798, and along County Road 3163.", "ts_dict_index": [13479, 13480, 13481]}
+{"event_id": 959404, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-07-08 15:55:00", "end_date_time": "2021-07-08 15:55:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. Wires were downed in Upper Milford Twp. Time estimated from radar.", "ts_dict_index": [13485, 13486, 13487]}
+{"event_id": 925151, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-11-15 18:58:00", "end_date_time": "2020-11-15 18:58:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. Trees and wires were downed near Lindberg Ave. Time estimated from radar.", "ts_dict_index": [13443, 13444, 13445]}
+{"event_id": 959413, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-07-08 16:47:00", "end_date_time": "2021-07-08 16:47:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. A tree was downed onto wires on Bernville Rd. Time estimated from radar.", "ts_dict_index": [13521, 13522, 13523]}
+{"event_id": 959406, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-08 17:10:00", "end_date_time": "2021-07-08 17:10:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. Tree limbs and wires were downed in Doylestown.", "ts_dict_index": [13491, 13492, 13493]}
+{"event_id": 959407, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-08 16:50:00", "end_date_time": "2021-07-08 16:50:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. A downed tree partially blocked Avignon Dr at Club House Rd. Time estimated from radar.", "ts_dict_index": [13503, 13504, 13505]}
+{"event_id": 959392, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-07-08 15:40:00", "end_date_time": "2021-07-08 15:40:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. Trees were downed in Washington Twp. Time estimated from radar.", "ts_dict_index": [13497, 13498, 13499]}
+{"event_id": 959408, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-08 16:56:00", "end_date_time": "2021-07-08 16:56:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. A tree down on wires blocked Jolly Rd at Beacon Hill Circle. Time estimated from radar.", "ts_dict_index": [13509, 13510, 13511]}
+{"event_id": 959393, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-07-08 15:06:00", "end_date_time": "2021-07-08 15:06:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. Trees were downed in Robeson Twp. Time estimated from radar.", "ts_dict_index": [13500, 13501, 13502]}
+{"event_id": 859809, "event_type": "Thunderstorm Wind", "state": "ARKANSAS", "cz_name": "PULASKI", "begin_date_time": "2019-10-21 02:55:00", "end_date_time": "2019-10-21 02:55:00", "narrative": "Up to this point, there was plenty of rain to talk about, but severe weather was limited. That changed late on the 20th/early on the 21st. Hit and miss thunderstorms popped up quickly in central and eastern Oklahoma. Storms eventually gelled into a line that rapidly crossed Arkansas.||As the line of storms tore through the region, a roof was removed from a building in Subiaco (Logan County). A carport was blown over at Conway (Faulkner County). Trees and/or powerlines were downed northwest of Benton (Saline County), at Bergman (Boone County), Bismarck (Hot Spring County), Coal Hill (Johnson County), Danville (Yell County), Hollis (Perry County), Little Rock (Pulaski County), and Pine Bluff (Jefferson County). Winds gusted to 58 mph at Carlisle (Lonoke County), 55 mph at Newport (Jackson County), and 53 mph at Flippin (Marion County) and Harrison (Boone County). A tree was downed in a yard on Tyler Street.", "ts_dict_index": [13518, 13519, 13520]}
+{"event_id": 959400, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-08 16:35:00", "end_date_time": "2021-07-08 16:35:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. A tree was downed on Ash Rd at Airport Rd. Time estimated from radar.", "ts_dict_index": [13515, 13516, 13517]}
+{"event_id": 959399, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-08 16:45:00", "end_date_time": "2021-07-08 16:45:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. Wires were downed on Deepdale Rd, blocking the road. Time estimated from radar.", "ts_dict_index": [13512, 13513, 13514]}
+{"event_id": 959394, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-07-08 16:09:00", "end_date_time": "2021-07-08 16:09:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. Numerous 911 calls were received for downed trees in Upper Saucon. Based on radar, a strong downburst likely occurred in the area. Time estimated from radar.", "ts_dict_index": [13494, 13495, 13496]}
+{"event_id": 925162, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-11-15 19:08:00", "end_date_time": "2020-11-15 19:08:00", "narrative": "Strong low pressure moved through the Great Lakes on November 15, 2020. As it did so, it pushed a warm front through the mid-Atlantic during the late morning and early afternoon hours, causing unseasonably warm conditions to develop. Strong mid and upper level dynamics associated with this low pressure caused linear convection to develop ahead of its associated cold front early in the day. While instability ahead of the front was very limited, the strong frontal forcing combined with extreme wind fields allowed two primary lines of convection to form and produce severe convective wind gusts as they moved east. One of these lines tracked into the eastern mid-Atlantic and towards the coast during the evening hours. It produced widespread wind gusts of around 60 mph, with a number of reports of downed trees and power lines and localized property damage across the region. A tree was downed in wires near Grant Rd. Time estimated from radar.", "ts_dict_index": [13464, 13465, 13466]}
+{"event_id": 959412, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-08 17:12:00", "end_date_time": "2021-07-08 17:12:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. A video showed multiple large trees down on power lines along Almshouse Rd in Doylestown. Time estimated from radar.", "ts_dict_index": [13524, 13525, 13526]}
+{"event_id": 959410, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-08 16:50:00", "end_date_time": "2021-07-08 16:50:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. A downed tree blocked Gawain Rd at Camelot Dr. Time estimated from radar.", "ts_dict_index": [13530, 13531, 13532]}
+{"event_id": 961895, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2021-07-12 17:46:00", "end_date_time": "2021-07-12 17:46:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Several reports of downed wires and power outages in the  Collingswood area. Time estimated from radar.", "ts_dict_index": [13536, 13537, 13538]}
+{"event_id": 959398, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-07-08 16:47:00", "end_date_time": "2021-07-08 16:47:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. A tree and wires were downed on Seaton Ross Rd at Ivywood Ln. Time estimated from radar.", "ts_dict_index": [13533, 13534, 13535]}
+{"event_id": 959403, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-08 16:38:00", "end_date_time": "2021-07-08 16:38:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. Downed tree limbs blocked Cedar Grove Rd. Time estimated from radar.", "ts_dict_index": [13506, 13507, 13508]}
+{"event_id": 961887, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-07-12 15:55:00", "end_date_time": "2021-07-12 15:55:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Several trees were downed in Brick Twp. Time estimated from radar.", "ts_dict_index": [13566, 13567, 13568]}
+{"event_id": 961898, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-07-12 15:45:00", "end_date_time": "2021-07-12 15:45:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Power lines were downed near Oak Ave. Time estimated from radar.", "ts_dict_index": [13542, 13543, 13544]}
+{"event_id": 961897, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-07-12 16:13:00", "end_date_time": "2021-07-12 16:13:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Trees and wires were downed near Brookdale Park Dr. Time estimated from radar.", "ts_dict_index": [13545, 13546, 13547]}
+{"event_id": 961885, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-07-12 15:56:00", "end_date_time": "2021-07-12 15:56:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Numerous reports of downed wires in Brick Twp. Time estimated from radar and scanner reports.", "ts_dict_index": [13590, 13591, 13592]}
+{"event_id": 961904, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 14:16:00", "end_date_time": "2021-07-12 14:16:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed near Millenium Dr. Time estimated from radar.", "ts_dict_index": [13551, 13552, 13553]}
+{"event_id": 961871, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-12 15:57:00", "end_date_time": "2021-07-12 15:57:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. A few reports of downed wires west of Levittown. Time estimated from radar.", "ts_dict_index": [13581, 13582, 13583]}
+{"event_id": 961889, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 16:29:00", "end_date_time": "2021-07-12 16:29:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed on Hamilton Ave. Time estimated from radar.", "ts_dict_index": [13557, 13558, 13559]}
+{"event_id": 961880, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 14:15:00", "end_date_time": "2021-07-12 14:15:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Scanner report of downed wires in Florence. Time estimated from radar and dispatch report.", "ts_dict_index": [13548, 13549, 13550]}
+{"event_id": 961905, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 17:12:00", "end_date_time": "2021-07-12 17:12:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed near Springhouse Ln. Time estimated from radar.", "ts_dict_index": [13584, 13585, 13586]}
+{"event_id": 961876, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-12 16:11:00", "end_date_time": "2021-07-12 16:11:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Tree limbs and wires were downed near Bridge St. Time estimated from radar.", "ts_dict_index": [13569, 13570, 13571]}
+{"event_id": 961903, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 16:35:00", "end_date_time": "2021-07-12 16:35:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Tree limbs and wires were downed near New Castle Ln. Time estimated from radar.", "ts_dict_index": [13554, 13555, 13556]}
+{"event_id": 961869, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-12 16:11:00", "end_date_time": "2021-07-12 16:11:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Several reports of downed power lines in the Croydon and Bristol areas. Time estimated from radar.", "ts_dict_index": [13572, 13573, 13574]}
+{"event_id": 961888, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 16:18:00", "end_date_time": "2021-07-12 16:18:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed on Lincoln Ave. Time estimated from radar and scanner report.", "ts_dict_index": [13560, 13561, 13562]}
+{"event_id": 961873, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-12 16:11:00", "end_date_time": "2021-07-12 16:11:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Multiple reports of downed trees and wires in Fairless Hills, especially near Beaumont Rd. Time estimated from radar.", "ts_dict_index": [13587, 13588, 13589]}
+{"event_id": 961902, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 16:40:00", "end_date_time": "2021-07-12 16:40:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed near Warner Rd. Time estimated from radar.", "ts_dict_index": [13563, 13564, 13565]}
+{"event_id": 961881, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 14:10:00", "end_date_time": "2021-07-12 14:10:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed in Cinnaminson. Time estimated from radar and dispatch report.", "ts_dict_index": [13575, 13576, 13577]}
+{"event_id": 961872, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-12 16:08:00", "end_date_time": "2021-07-12 16:08:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed in several locations near Levittown. Time estimated from radar.", "ts_dict_index": [13578, 13579, 13580]}
+{"event_id": 961883, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 14:16:00", "end_date_time": "2021-07-12 14:16:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed near Old York Rd. Time estimated from radar.", "ts_dict_index": [13593, 13594, 13595]}
+{"event_id": 959411, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-07-08 16:47:00", "end_date_time": "2021-07-08 16:47:00", "narrative": "Tropical Storm Elsa approached the mid-Atlantic states from the south on July 8. Downstream of Elsa, a warm and moist environment was present. A slow moving frontal boundary also resided over northern New Jersey, northern Pennsylvania, and into New York. This frontal system provided forcing for convective development over the mid-Atlantic, in fairly close proximity but unrelated to Tropical Storm Elsa. With strong instability and weak to moderate wind shear, some of the storms became severe as they organized into linear and multi-cellular clusters. Deep layer southerly flow in advance of Elsa caused storms to move northward as opposed to a more typical eastward motion. Damaging wind was the main hazard associated with these storms, with several strong downbursts noted. Storm activity eventually weakened and moved north of the region by evening as Elsa moved in. A downed tree blocked Wood St at 12th Ave. Time estimated from radar.", "ts_dict_index": [13527, 13528, 13529]}
+{"event_id": 961892, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-07-12 15:45:00", "end_date_time": "2021-07-12 15:45:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Several reports of downed wires and power outages in the Island Heights area. Time estimated from radar.", "ts_dict_index": [13599, 13600, 13601]}
+{"event_id": 961884, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-07-12 15:55:00", "end_date_time": "2021-07-12 15:55:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Numerous reports of downed wires between Lakewood and Toms River. Time estimated from radar and scanner reports.", "ts_dict_index": [13605, 13606, 13607]}
+{"event_id": 961886, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-07-12 15:52:00", "end_date_time": "2021-07-12 15:52:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed on Ocean Ave in Lakewood. Time estimated from radar.", "ts_dict_index": [13602, 13603, 13604]}
+{"event_id": 961894, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 17:09:00", "end_date_time": "2021-07-12 17:09:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed near Kings Hwy. Time estimated from radar.", "ts_dict_index": [13611, 13612, 13613]}
+{"event_id": 961874, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-12 16:24:00", "end_date_time": "2021-07-12 16:24:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Power lines were downed near State Rd. Time estimated from radar.", "ts_dict_index": [13608, 13609, 13610]}
+{"event_id": 960736, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2021-05-11 23:59:00", "end_date_time": "2021-05-12 00:20:00", "narrative": "Tuesday night through Wednesday morning of May 11th into May 12th, a 500 mb shortwave trough worked from northwest to southeast from the Texas Big Bend through Deep South Texas and the Rio Grande Valley, bringing a late-season cold front through the region. The Storm Prediction Center (SPC) forecasted a Marginal Risk of severe weather for the Rio Grande Plains/Brush Country and parts of the Lower Rio Grande Valley for this time period. While large hail was a potential threat, damaging winds took center stage as the squall line at the leading edge of the front tore through the Rio Grande Valley. Even more impressive was the strong, damaging winds behind the squall line associated with a ���wake low��� that lasted for several hours on the morning of May 12th. Later on during this event, some street flooding was observed in the San Benito area due to heavy rain. As thunderstorms moved through the area, the ASOS station at the McAllen airport measured a gust to 63 mph, or 55 knots. Gusts of 54 knots or higher lasted for about 20 minutes, based on the station reports.", "ts_dict_index": [13617, 13618, 13619]}
+{"event_id": 960735, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2021-05-12 00:05:00", "end_date_time": "2021-05-12 00:25:00", "narrative": "Tuesday night through Wednesday morning of May 11th into May 12th, a 500 mb shortwave trough worked from northwest to southeast from the Texas Big Bend through Deep South Texas and the Rio Grande Valley, bringing a late-season cold front through the region. The Storm Prediction Center (SPC) forecasted a Marginal Risk of severe weather for the Rio Grande Plains/Brush Country and parts of the Lower Rio Grande Valley for this time period. While large hail was a potential threat, damaging winds took center stage as the squall line at the leading edge of the front tore through the Rio Grande Valley. Even more impressive was the strong, damaging winds behind the squall line associated with a ���wake low��� that lasted for several hours on the morning of May 12th. Later on during this event, some street flooding was observed in the San Benito area due to heavy rain. As thunderstorms moved through the area, an anemometer at the Pharr Emergency Operations Center measured a wind gust to 73 mph, or 63 knots.  The anemometer is situated 90 feet (27 meters) above the ground, nearly three times higher than standard NWS measuring equipment and more than four times higher than eye level; wind speed listed here (56 knots) was reduced to account for near-ground friction.", "ts_dict_index": [13614, 13615, 13616]}
+{"event_id": 961893, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-07-12 16:00:00", "end_date_time": "2021-07-12 16:00:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Several reports of downed wires in the Bay Head area. Time estimated from radar.", "ts_dict_index": [13596, 13597, 13598]}
+{"event_id": 961343, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2021-05-11 23:40:00", "end_date_time": "2021-05-12 00:00:00", "narrative": "Tuesday night through Wednesday morning of May 11th into May 12th, a 500 mb shortwave trough worked from northwest to southeast from the Texas Big Bend through Deep South Texas and the Rio Grande Valley, bringing a late-season cold front through the region. The Storm Prediction Center (SPC) forecasted a Marginal Risk of severe weather for the Rio Grande Plains/Brush Country and parts of the Lower Rio Grande Valley for this time period. While large hail was a potential threat, damaging winds took center stage as the squall line at the leading edge of the front tore through the Rio Grande Valley. Even more impressive was the strong, damaging winds behind the squall line associated with a ���wake low��� that lasted for several hours on the morning of May 12th. Later on during this event, some street flooding was observed in the San Benito area due to heavy rain. Social media report of a damaged carport and a barn roof torn off in the Linn area. Time was estimated via radar.", "ts_dict_index": [13623, 13624, 13625]}
+{"event_id": 961341, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2021-05-11 23:40:00", "end_date_time": "2021-05-12 00:00:00", "narrative": "Tuesday night through Wednesday morning of May 11th into May 12th, a 500 mb shortwave trough worked from northwest to southeast from the Texas Big Bend through Deep South Texas and the Rio Grande Valley, bringing a late-season cold front through the region. The Storm Prediction Center (SPC) forecasted a Marginal Risk of severe weather for the Rio Grande Plains/Brush Country and parts of the Lower Rio Grande Valley for this time period. While large hail was a potential threat, damaging winds took center stage as the squall line at the leading edge of the front tore through the Rio Grande Valley. Even more impressive was the strong, damaging winds behind the squall line associated with a ���wake low��� that lasted for several hours on the morning of May 12th. Later on during this event, some street flooding was observed in the San Benito area due to heavy rain. Numerous reports on social media of trees damaged or uprooted near the Linn-San Manuel area.", "ts_dict_index": [13620, 13621, 13622]}
+{"event_id": 960734, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2021-05-11 23:46:00", "end_date_time": "2021-05-12 00:05:00", "narrative": "Tuesday night through Wednesday morning of May 11th into May 12th, a 500 mb shortwave trough worked from northwest to southeast from the Texas Big Bend through Deep South Texas and the Rio Grande Valley, bringing a late-season cold front through the region. The Storm Prediction Center (SPC) forecasted a Marginal Risk of severe weather for the Rio Grande Plains/Brush Country and parts of the Lower Rio Grande Valley for this time period. While large hail was a potential threat, damaging winds took center stage as the squall line at the leading edge of the front tore through the Rio Grande Valley. Even more impressive was the strong, damaging winds behind the squall line associated with a ���wake low��� that lasted for several hours on the morning of May 12th. Later on during this event, some street flooding was observed in the San Benito area due to heavy rain. As thunderstorms moved through the area, the RAWS site at Linn-San Manuel measured a wind gust to 60 mph or 52 knots.", "ts_dict_index": [13629, 13630, 13631]}
+{"event_id": 963651, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2021-05-12 00:11:00", "end_date_time": "2021-05-12 00:20:00", "narrative": "Tuesday night through Wednesday morning of May 11th into May 12th, a 500 mb shortwave trough worked from northwest to southeast from the Texas Big Bend through Deep South Texas and the Rio Grande Valley, bringing a late-season cold front through the region. The Storm Prediction Center (SPC) forecasted a Marginal Risk of severe weather for the Rio Grande Plains/Brush Country and parts of the Lower Rio Grande Valley for this time period. While large hail was a potential threat, damaging winds took center stage as the squall line at the leading edge of the front tore through the Rio Grande Valley. Even more impressive was the strong, damaging winds behind the squall line associated with a ���wake low��� that lasted for several hours on the morning of May 12th. Later on during this event, some street flooding was observed in the San Benito area due to heavy rain. At least a half dozen manufactured homes sustained|damage, mainly from peeled-back or blown off tin roofs, and car ports|knocked down, in portions of Donna and Weslaco along and near the |Interstate 2 corridor. One home slid off its foundation midway between|the cities. Several mesquite and ash trees were uprooted,|split, or lost large limbs. One uprooted large tree damaged a car|in Donna.  Several parts of fences were blown down, and unanchored road|signs were also blown down.", "ts_dict_index": [13626, 13627, 13628]}
+{"event_id": 1084775, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-04-02 18:32:00", "end_date_time": "2023-04-02 18:32:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Large tree limbs were snapped in Waskom.", "ts_dict_index": [13635, 13636, 13637]}
+{"event_id": 1084773, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-04-02 18:01:00", "end_date_time": "2023-04-02 18:01:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Trees were snapped and uprooted just northwest of Scottsville.", "ts_dict_index": [13638, 13639, 13640]}
+{"event_id": 961896, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-07-12 14:13:00", "end_date_time": "2021-07-12 14:13:00", "narrative": "A warm front was draped across northern Pennsylvania and far northern New Jersey on July 12. South of the front, a very warm and unstable air mass was present. An approaching trough also helped spur the development of a weak wave of low pressure, which tracked along the front during the afternoon and evening hours. This helped add some forcing and shear to an already unstable air mass. The result was scattered to widespread thunderstorm development along and south of the front during the peak heating hours. Some of the storms became severe, with a number of instances of damaging wind across the region. This event was also better known for producing prolific flash flooding near the Delaware River just northeast of Philadelphia, along the Pennsylvania and New Jersey border. Storm coverage gradually decreased in the evening hours as heating and forcing were lost. Wires were downed in the Fieldsboro area and near Dunns Mill Rd. Time estimated from radar.", "ts_dict_index": [13539, 13540, 13541]}
+{"event_id": 1084939, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-02 18:36:00", "end_date_time": "2023-04-02 18:36:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Trees were downed on the north side of Blanchard.", "ts_dict_index": [13650, 13651, 13652]}
+{"event_id": 1084941, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-02 18:49:00", "end_date_time": "2023-04-02 18:49:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. A tree was blown down into the kitchen of a home in the Willow Ridge subdivision on the south side of Cross Lake.", "ts_dict_index": [13656, 13657, 13658]}
+{"event_id": 1084942, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-02 18:49:00", "end_date_time": "2023-04-02 18:49:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. A 73 mph wind gust was measured at the Shreveport Regional Airport.", "ts_dict_index": [13659, 13660, 13661]}
+{"event_id": 1084940, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-02 18:25:00", "end_date_time": "2023-04-02 18:25:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Trees were blown down near Old Mooringsport-Latex Road and Highway 169 south of Mooringsport.", "ts_dict_index": [13653, 13654, 13655]}
+{"event_id": 1084937, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-02 18:38:00", "end_date_time": "2023-04-02 18:39:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. A NWS Storm Survey confirmed straight line wind damage from an intense thunderstorm bowing arc that moved through the city of Blanchard during the evening of April 2nd. These winds were estimated to range from 65-85 mph, with a vast majority of the damage due to uprooted trees with any structural damage to buildings and infrastructure overwhelmingly due to trees falling. Trees were blown down along West Phelps Avenue, North Olney Street, West Warriner Avenue, as well as near Katie Circle and Pine Hill Road in Blanchard. There were also few cases of wind that caused minor damage to structures. In addition, the majority of the trees fell to the east and did not exhibit a convergent damage pattern typical of tornadoes.", "ts_dict_index": [13644, 13645, 13646]}
+{"event_id": 1084944, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-02 18:50:00", "end_date_time": "2023-04-02 18:50:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. A tree was blown down near Quinton Street, Orla Avenue, and Velva Avenue in Shreveport.", "ts_dict_index": [13647, 13648, 13649]}
+{"event_id": 1084943, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-02 18:50:00", "end_date_time": "2023-04-02 18:50:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Trees were blown down on Dixie Shreveport Road and George Road.", "ts_dict_index": [13662, 13663, 13664]}
+{"event_id": 1084767, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-04-02 17:52:00", "end_date_time": "2023-04-02 17:57:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. An NWS Storm Survey concluded that an intense and short thunderstorm line segment bowing arc moved through the northern half of the city of Marshall, and produced a damaging downburst of straight-line winds. These winds were estimated to range from roughly 65-85 mph, although there were a few locations where peak wind estimates were between 90-95 mph. A vast majority of the damage was due to uprooted trees with most structural damage to buildings and infrastructure due to trees falling. There were a few cases of wind doing damage to structures, such as at the East Texas Baptist University where the wind did minor roof damage and also removed the facade from a west-facing wall. In addition, there were a few outbuildings in the wind damage swath which were heavily damaged which were heavily damaged or destroyed by the force of the wind. The most concentrated damage extended from the university northeast through Sledge Street were numerous snapped trees garnered the peak wind estimate of 90-95 mph. But even in this area, the overwhelming majority of the trees fell to the east and did not exhibit a convergent damage pattern typical of tornadoes. The pattern of tree fall in an easterly direction was repeated in a vast majority of instances throughout the damage swath.", "ts_dict_index": [13641, 13642, 13643]}
+{"event_id": 961342, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HIDALGO", "begin_date_time": "2021-05-12 00:25:00", "end_date_time": "2021-05-12 00:35:00", "narrative": "Tuesday night through Wednesday morning of May 11th into May 12th, a 500 mb shortwave trough worked from northwest to southeast from the Texas Big Bend through Deep South Texas and the Rio Grande Valley, bringing a late-season cold front through the region. The Storm Prediction Center (SPC) forecasted a Marginal Risk of severe weather for the Rio Grande Plains/Brush Country and parts of the Lower Rio Grande Valley for this time period. While large hail was a potential threat, damaging winds took center stage as the squall line at the leading edge of the front tore through the Rio Grande Valley. Even more impressive was the strong, damaging winds behind the squall line associated with a ���wake low��� that lasted for several hours on the morning of May 12th. Later on during this event, some street flooding was observed in the San Benito area due to heavy rain. Numerous reports received via social media of tree damage and tree branches down on vehicles near Mercedes. Time was estimated via radar and based on NWS Storm Survey on damage from Donna to just east of Weslaco.", "ts_dict_index": [13632, 13633, 13634]}
+{"event_id": 1084946, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-02 18:52:00", "end_date_time": "2023-04-02 18:52:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Trees were blown down near Dillingham Avenue and Mitchell Lane in Shreveport.", "ts_dict_index": [13668, 13669, 13670]}
+{"event_id": 1084947, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-02 19:10:00", "end_date_time": "2023-04-02 19:10:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Multiple trees were blown down on Sligo Road south of Bossier City.", "ts_dict_index": [13671, 13672, 13673]}
+{"event_id": 878108, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2020-02-12 18:22:00", "end_date_time": "2020-02-12 18:22:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. A tree was knocked down at mile marker 49 on Highway 157. Time estimated by radar.", "ts_dict_index": [13698, 13699, 13700]}
+{"event_id": 1084948, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-04-02 19:20:00", "end_date_time": "2023-04-02 19:20:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. A tree was blown down near the 8500 block of Barksdale Blvd near the Taylortown community. A vehicle collided with this tree, but no injuries were reported.", "ts_dict_index": [13674, 13675, 13676]}
+{"event_id": 878092, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 16:43:00", "end_date_time": "2020-02-12 16:43:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. A tree was knocked down at the intersection of CR 131 and CR 8.", "ts_dict_index": [13710, 13711, 13712]}
+{"event_id": 878100, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 17:12:00", "end_date_time": "2020-02-12 17:12:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. A home was damaged near Center Hill Market at the intersection of CR 623 and Highway 64.", "ts_dict_index": [13701, 13702, 13703]}
+{"event_id": 878097, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 17:09:00", "end_date_time": "2020-02-12 17:09:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. ", "ts_dict_index": [13707, 13708, 13709]}
+{"event_id": 878104, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 17:18:00", "end_date_time": "2020-02-12 17:18:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. The roof of a garage was ripped apart. Time estimated by radar. Report obtained by social media.", "ts_dict_index": [13692, 13693, 13694]}
+{"event_id": 878102, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 17:17:00", "end_date_time": "2020-02-12 17:17:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. A tree was knocked down on CR 171.", "ts_dict_index": [13689, 13690, 13691]}
+{"event_id": 878093, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 17:00:00", "end_date_time": "2020-02-12 17:00:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. A tree was knocked down on CR 61 north of CR 24.", "ts_dict_index": [13713, 13714, 13715]}
+{"event_id": 878094, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 17:02:00", "end_date_time": "2020-02-12 17:02:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. Trees were knocked down on power lines near a residence on Cove Springs Road.", "ts_dict_index": [13683, 13684, 13685]}
+{"event_id": 878098, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 17:10:00", "end_date_time": "2020-02-12 17:10:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. Multiple trees and power lines were knocked down near CR 33 and CR 39. Time estimated.", "ts_dict_index": [13686, 13687, 13688]}
+{"event_id": 878099, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2020-02-12 17:12:00", "end_date_time": "2020-02-12 17:12:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. A tree was knocked down at Bowen Street and Lynwood Avenue. Time estimated by radar.", "ts_dict_index": [13704, 13705, 13706]}
+{"event_id": 1084949, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2023-04-02 19:32:00", "end_date_time": "2023-04-02 19:32:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Several trees and power lines were down throughout the southern third of Webster Parish.", "ts_dict_index": [13677, 13678, 13679]}
+{"event_id": 1089975, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2023-03-26 18:51:00", "end_date_time": "2023-03-26 18:51:00", "narrative": "A shortwave trough moving across Central Texas on the morning of March 26th made its way into Ark-La-Tex region by the afternoon. Meanwhile, a surface warm front was lifting back northward from the coast, providing the leading edge of near 70 degree dewpoints and ample surface-based instability. Strengthening southeasterly low-level winds ahead of the upper trough, combined with the favorable thermodynamic environment, resulted in the potential for supercell thunderstorms capable of large hail and damaging winds across much of the Ark-La-Tex. By early in the afternoon, increasing lift and moisture associated with these synoptic features led to scattered thunderstorm development with a cluster of supercells resulting in numerous reports of severe hail and damaging wind gusts across North Louisiana, but more isolated across East Texas and Southwest Arkansas. Tree downed on power lines along Highway 117.", "ts_dict_index": [13680, 13681, 13682]}
+{"event_id": 878095, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 17:08:00", "end_date_time": "2020-02-12 17:08:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. Trees were knocked down on CR 144. Relayed via social media. Time estimated by radar.", "ts_dict_index": [13719, 13720, 13721]}
+{"event_id": 905560, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-22 16:22:00", "end_date_time": "2020-07-22 16:22:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Tree or wires down on College Ave at 3rd Ave. Time estimated from radar.", "ts_dict_index": [13731, 13732, 13733]}
+{"event_id": 878090, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 16:31:00", "end_date_time": "2020-02-12 16:31:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. A power line was knocked down in the Rock Wall area in Waterloo.", "ts_dict_index": [13725, 13726, 13727]}
+{"event_id": 878089, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 16:29:00", "end_date_time": "2020-02-12 16:29:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. A tree was knocked down on CR 1 at Second Creek Recreation Campgrounds.", "ts_dict_index": [13728, 13729, 13730]}
+{"event_id": 878091, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 16:41:00", "end_date_time": "2020-02-12 16:41:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. Power lines were knocked down on Waterloo Road. Time and location estimated.", "ts_dict_index": [13722, 13723, 13724]}
+{"event_id": 878096, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 17:09:00", "end_date_time": "2020-02-12 17:09:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. Trees and power lines were knocked down. Time estimated by radar.", "ts_dict_index": [13716, 13717, 13718]}
+{"event_id": 878101, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-02-12 17:12:00", "end_date_time": "2020-02-12 17:12:00", "narrative": "A solid line of mostly low-topped showers with a few embedded thunderstorms pushed east from Mississippi and western Tennessee across north Alabama and southern middle Tennessee during the late afternoon through mid evening hours. A tornado developed along the line in Lauderdale County near Green Hill, producing a measured wind gust of 76 mph on an Amateur Radio weather station, also knocked down the two 40 foot radio towers the equipment was attached to. The tornado tracked east-northeast crossing into Lawrence County in Tennessee, knocking down trees, power lines, and damaging a few homes.  In addition, the line of showers produced wind gusts of 35 to 50 mph, with a few pockets of 60 mph winds or higher. Due to saturated soils, even sub-severe winds were able to knock down larger limbs and a few trees.  Power lines were also knocked down in some areas. A barn was destroyed on CR 375. Time estimated.", "ts_dict_index": [13695, 13696, 13697]}
+{"event_id": 905333, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-07-22 19:06:00", "end_date_time": "2020-07-22 19:06:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Measured by a HADS gauge.", "ts_dict_index": [13758, 13759, 13760]}
+{"event_id": 905566, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-07-22 16:32:00", "end_date_time": "2020-07-22 16:32:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. An 8 inch diameter maple branch snapped off of a tree in Chalfont.", "ts_dict_index": [13764, 13765, 13766]}
+{"event_id": 905335, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-07-22 19:08:00", "end_date_time": "2020-07-22 19:08:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Measured by a Weatherflow gauge.", "ts_dict_index": [13746, 13747, 13748]}
+{"event_id": 905572, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-22 16:37:00", "end_date_time": "2020-07-22 16:37:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A tree or wires were downed on McLaughlin Rd at Country Club Dr near the Pinecrest Golf Club. Time estimated from radar.", "ts_dict_index": [13755, 13756, 13757]}
+{"event_id": 905565, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-07-22 16:28:00", "end_date_time": "2020-07-22 16:28:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Several reports of downed wires between White Horse and Perkasie. Time estimated from radar.", "ts_dict_index": [13767, 13768, 13769]}
+{"event_id": 905569, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-07-22 16:34:00", "end_date_time": "2020-07-22 16:34:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Downed tree limbs and wires were reported near Mountain View Dr near Quakertown. Time estimated from radar.", "ts_dict_index": [13761, 13762, 13763]}
+{"event_id": 905509, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-22 15:34:00", "end_date_time": "2020-07-22 15:34:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Wires were downed on Ledge Rock Rd east of Mohnton. Time estimated from radar.", "ts_dict_index": [13770, 13771, 13772]}
+{"event_id": 905575, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-07-22 16:57:00", "end_date_time": "2020-07-22 16:57:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Several reports of downed wires were received from the Jamison area. Time estimated from radar.", "ts_dict_index": [13749, 13750, 13751]}
+{"event_id": 905562, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2020-07-22 16:25:00", "end_date_time": "2020-07-22 16:25:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Trees and wires were downed near Schukraft Rd in West Rockhill Twp. Time estimated from radar.", "ts_dict_index": [13734, 13735, 13736]}
+{"event_id": 905574, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-22 16:54:00", "end_date_time": "2020-07-22 16:54:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A tree or wires were downed on W Pennsylvania Ave. Time estimated from radar.", "ts_dict_index": [13752, 13753, 13754]}
+{"event_id": 870417, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "LAUDERDALE", "begin_date_time": "2020-01-11 07:50:00", "end_date_time": "2020-01-11 07:50:00", "narrative": "A long-lived quasi-linear convective system moved into northwest Alabama between 6 and 9 AM, and gradually tracked east across the remainder of north Alabama through the midday and early afternoon hours.  In advance of the line, strong southerly winds of 30 to 40 mph with gusts over 45 mph were reported.  In some cases, trees and power lines were knocked down with these non-thunderstorm winds.  The line of thunderstorms yielded numerous reports of thunderstorm wind damage, including trees and power lines being knocked down, along with some structural damage.  A few weather stations measured wind gusts of 58 mph or higher as well.  Storm surveys revealed 3 separate tornadoes: 1 EF0 and 1 EF1 in Cullman County,  and 1 EF2 in Marshall County.  Intense rainfall in a short period of time resulted in a few reports of brief flash flooding in northwest Alabama. A tree was knocked down along CR 45 with live wires across the road.", "ts_dict_index": [13737, 13738, 13739]}
+{"event_id": 905563, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-22 16:25:00", "end_date_time": "2020-07-22 16:25:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Wires were downed near Leon Dr in Hatfield. Time estimated from radar.", "ts_dict_index": [13743, 13744, 13745]}
+{"event_id": 1084945, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-04-02 18:51:00", "end_date_time": "2023-04-02 18:51:00", "narrative": "A strong upper level trough ejected east-northeast across the Southern Plains during the afternoon and evening hours on April 2nd, with strong southerly low level winds ahead of the trough allowing for a warm front to mix north across East Texas and North Louisiana. Very warm, humid, and unstable air spread north along and south of this front, with the approaching trough reinforcing a dry line into Southeast Oklahoma and East Texas during the late afternoon and evening, and across the remainder of the region during the early morning hours on the 3rd. Given the increased forcing along these boundaries and the approaching upper trough, scattered severe thunderstorms developed across East Texas and North Louisiana, which produced numerous instances of large hail and damaging winds before weakening during the late evening into the early morning hours on the 3rd. Trees were blown down near Fairview Street and Line Avenue in Shreveport.", "ts_dict_index": [13665, 13666, 13667]}
+{"event_id": 905524, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-22 15:53:00", "end_date_time": "2020-07-22 15:53:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A tree was downed onto wires with a transformer blown on Anthony's Mill Rd. Time estimated from radar.", "ts_dict_index": [13785, 13786, 13787]}
+{"event_id": 905512, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-22 15:51:00", "end_date_time": "2020-07-22 15:51:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A tree was downed on Shed Rd in Union Twp. Time estimated from radar.", "ts_dict_index": [13779, 13780, 13781]}
+{"event_id": 905534, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-22 16:01:00", "end_date_time": "2020-07-22 16:01:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Wires were downed near Hopewell Rd near the border of Berks and Chester Counties. Time estimated from radar.", "ts_dict_index": [13791, 13792, 13793]}
+{"event_id": 905514, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-22 15:51:00", "end_date_time": "2020-07-22 15:51:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Trees and wires were downed near West Philadelphia Ave in Earl Twp. Time estimated from radar.", "ts_dict_index": [13773, 13774, 13775]}
+{"event_id": 905557, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-22 16:22:00", "end_date_time": "2020-07-22 16:22:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A tree and wires were downed on Valley Creek Rd at Harmony Hill Rd. Time estimated from radar.", "ts_dict_index": [13800, 13801, 13802]}
+{"event_id": 905540, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-22 16:11:00", "end_date_time": "2020-07-22 16:11:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Wires were downed near Walnut St in Emmaus. Time estimated from radar.", "ts_dict_index": [13797, 13798, 13799]}
+{"event_id": 905510, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-22 15:49:00", "end_date_time": "2020-07-22 15:49:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Wires were downed on Seipstown Rd in Seipstown. Time estimated from radar.", "ts_dict_index": [13776, 13777, 13778]}
+{"event_id": 905544, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-22 16:11:00", "end_date_time": "2020-07-22 16:11:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Wires were downed near Court St in Allentown. Time estimated from radar.", "ts_dict_index": [13794, 13795, 13796]}
+{"event_id": 905527, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-22 15:54:00", "end_date_time": "2020-07-22 15:54:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A tree and wires were downed near Arrowhead Ln near Breinigsville. Time estimated from radar.", "ts_dict_index": [13788, 13789, 13790]}
+{"event_id": 870418, "event_type": "Thunderstorm Wind", "state": "ALABAMA", "cz_name": "COLBERT", "begin_date_time": "2020-01-11 08:50:00", "end_date_time": "2020-01-11 08:50:00", "narrative": "A long-lived quasi-linear convective system moved into northwest Alabama between 6 and 9 AM, and gradually tracked east across the remainder of north Alabama through the midday and early afternoon hours.  In advance of the line, strong southerly winds of 30 to 40 mph with gusts over 45 mph were reported.  In some cases, trees and power lines were knocked down with these non-thunderstorm winds.  The line of thunderstorms yielded numerous reports of thunderstorm wind damage, including trees and power lines being knocked down, along with some structural damage.  A few weather stations measured wind gusts of 58 mph or higher as well.  Storm surveys revealed 3 separate tornadoes: 1 EF0 and 1 EF1 in Cullman County,  and 1 EF2 in Marshall County.  Intense rainfall in a short period of time resulted in a few reports of brief flash flooding in northwest Alabama. Trees were knocked down onto a row of telephone poles, pushing them down to the ground.", "ts_dict_index": [13740, 13741, 13742]}
+{"event_id": 905492, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-22 15:01:00", "end_date_time": "2020-07-22 15:01:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Several reports of trees and wires down in Stouchsburg. Time estimated from radar.", "ts_dict_index": [13833, 13834, 13835]}
+{"event_id": 905505, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-22 15:30:00", "end_date_time": "2020-07-22 15:30:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A tree was downed on Moselem Springs Rd. Time estimated from radar.", "ts_dict_index": [13818, 13819, 13820]}
+{"event_id": 905553, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2020-07-22 16:21:00", "end_date_time": "2020-07-22 16:21:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A utility was downed on US-30 near Planebrook Rd. Time estimated from radar.", "ts_dict_index": [13803, 13804, 13805]}
+{"event_id": 905497, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-22 15:17:00", "end_date_time": "2020-07-22 15:17:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Wires were downed near State St in West Hamburg. Time estimated from radar.", "ts_dict_index": [13827, 13828, 13829]}
+{"event_id": 905507, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-22 15:32:00", "end_date_time": "2020-07-22 15:32:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Wires were downed on Wyomissing Ave in Mohnton. Time estimated from radar.", "ts_dict_index": [13815, 13816, 13817]}
+{"event_id": 905577, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2020-07-22 17:11:00", "end_date_time": "2020-07-22 17:11:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A tree or wires was downed on Moredon Rd at Old Ford Rd. Time estimated from radar.", "ts_dict_index": [13812, 13813, 13814]}
+{"event_id": 905508, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-22 15:33:00", "end_date_time": "2020-07-22 15:33:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A tree was downed into wires on Hollywood Dr. Time estimated from radar.", "ts_dict_index": [13836, 13837, 13838]}
+{"event_id": 905494, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2020-07-22 15:03:00", "end_date_time": "2020-07-22 15:03:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Several reports of trees and wires down in the Host and North Heidelberg areas. Time estimated from radar.", "ts_dict_index": [13830, 13831, 13832]}
+{"event_id": 905499, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-22 15:26:00", "end_date_time": "2020-07-22 15:26:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. A tree was downed on Route 863 near Kistler Valley Rd. Time estimated from radar.", "ts_dict_index": [13821, 13822, 13823]}
+{"event_id": 905502, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-22 15:29:00", "end_date_time": "2020-07-22 15:29:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Trees and wires were downed near Swamp Hollow Rd in Washington Twp. Time estimated from radar.", "ts_dict_index": [13824, 13825, 13826]}
+{"event_id": 1121441, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 21:50:00", "end_date_time": "2023-07-26 21:50:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Large tree branch down in the area of East Boston Street and South Santan Village Parkway in Gilbert. Tree branch is estimated to be three inches in diameter, breaking the windows of parked car. Wind gusts were estimated to be 55-60 mph. No injuries were reported.", "ts_dict_index": [13842, 13843, 13844]}
+{"event_id": 1056605, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-09-25 14:00:00", "end_date_time": "2022-09-25 14:00:00", "narrative": "Northwesterly flow aloft aided in pushing a cold front southward into the region on the afternoon of September 25th. Despite only weak upper-level support, frontal forcing was sufficient to generate scattered convection along the frontal boundary during the afternoon. The atmosphere was relatively uncapped, and with afternoon temperatures climbing into the mid 90s, moderate surface-based instability developed. However, a lack of deep layer moisture appeared to be a limiting factor for any severe weather although classic inverted-V forecast soundings indicated the potential for isolated damaging wind gusts from thunderstorm downbursts in the afternoon. Moisture proved to be sufficient for storms to rapidly develop by mid to late afternoon, quickly accelerating southward and producing sporadic damaging wind gusts across parts of McCurtain County Oklahoma. A few trees downed and a power pole snapped along Highway 3.", "ts_dict_index": [13806, 13807, 13808]}
+{"event_id": 905535, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2020-07-22 16:01:00", "end_date_time": "2020-07-22 16:01:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Trees and wires were downed near Lapp Rd in Stetlersville. Time estimated from radar.", "ts_dict_index": [13782, 13783, 13784]}
+{"event_id": 1121085, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:20:00", "end_date_time": "2023-07-26 22:20:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A large uprooted was reported in the area of 64th street and Osborn Road in Scottsdale. Wind gusts were estimated between 55-60 mph. No injuries were reported.", "ts_dict_index": [13863, 13864, 13865]}
+{"event_id": 1121081, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:29:00", "end_date_time": "2023-07-26 22:29:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A mesonet station located in the Sunnyslope neighbor of Phoenix measured a 61 mph gust.", "ts_dict_index": [13848, 13849, 13850]}
+{"event_id": 1121077, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:09:00", "end_date_time": "2023-07-26 22:09:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A house located in the area of East Lehi Road and North Pioneer in Mesa sustained roof damage to the garage. Winds were estimated between 55-60 mph. No injuries were reported.", "ts_dict_index": [13845, 13846, 13847]}
+{"event_id": 1121444, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:10:00", "end_date_time": "2023-07-26 22:10:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A couple of large trees down in the area of Lehi Road between North Mesa Drive and North Horne in Mesa. One of the tree toppled over a fence. Wind gusts were estimated at 55-60 mph. No injuries were reported.", "ts_dict_index": [13860, 13861, 13862]}
+{"event_id": 1121073, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-07-26 21:50:00", "end_date_time": "2023-07-26 21:50:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Broken roof tiles were observed near the area of US-60 in Gold Canyon. Wind gusts were estimated between 55-60 mph. No injuries were reported.", "ts_dict_index": [13866, 13867, 13868]}
+{"event_id": 1120680, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-07-26 20:43:00", "end_date_time": "2023-07-26 20:43:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A Union Pacific Railroad Mesonet observing site located just northwest of Eloy measured a 60 mph wind gust.", "ts_dict_index": [13851, 13852, 13853]}
+{"event_id": 1121076, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:08:00", "end_date_time": "2023-07-26 22:08:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Large tree limbs down in the area of East Lehi Road and North Terrace Circle in Mesa. Wind gusts were estimated at between 55-60 mph. No injuries were reported.", "ts_dict_index": [13875, 13876, 13877]}
+{"event_id": 1121088, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:29:00", "end_date_time": "2023-07-26 22:29:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Multiple trees down along the area of North Frank Lloyd Wright Boulevard and North 90th street in Scottsdale. One tree snapped in half with the largest tree diameter estimated to be a foot. Winds were estimated near 60 mph. No injuries were reported.", "ts_dict_index": [13854, 13855, 13856]}
+{"event_id": 1121079, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:10:00", "end_date_time": "2023-07-26 22:10:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Large tree limbs down in the area of East Nance Street and North Horne in Mesa. Wind gusts were estimated between 55-60 mph. No injuries were reported.", "ts_dict_index": [13857, 13858, 13859]}
+{"event_id": 1121078, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:10:00", "end_date_time": "2023-07-26 22:10:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Significant wind damage centered around West Ingram and North Center Streets in Mesa. Five apartment complexes sustained roof damage. A large number of trees, block walls and other structures sustained damage. Wind gusts were estimated between 55-60 mph. No injuries were reported.", "ts_dict_index": [13872, 13873, 13874]}
+{"event_id": 905336, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2020-07-22 19:11:00", "end_date_time": "2020-07-22 19:11:00", "narrative": "A slow moving frontal boundary was draped across upstate New York and southern New England on July 22 with multiple waves of low pressure tracking along it. The mid-Atlantic was left in a warm sector air mass south of this front. This led to a very hot and humid day on July 22 with air temperatures rising into the 90s and dew point values near 70. This caused strong instability to develop. Shear values were not overly impressive, but an approaching shortwave disturbance from the Midwest did help to increase shear late in the day. This disturbance also served as forcing for convection to develop in the warm and unstable air mass. Widespread thunderstorm development occurred, with storms eventually developing into a mostly solid squall line. This line of storms produced numerous reports of wind damage across eastern Pennsylvania, New Jersey, and Delmarva. Measured by a CWOP station.", "ts_dict_index": [13809, 13810, 13811]}
+{"event_id": 1121096, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:05:00", "end_date_time": "2023-07-26 22:05:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Video showed multiple homes along the area of East Juniper Street and Pasadena in Mesa suffered roof damage. One home suffered damage to the garage door. Wind gusts were estimated at 55-60 mph. No injuries were reported.", "ts_dict_index": [13884, 13885, 13886]}
+{"event_id": 1121084, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:45:00", "end_date_time": "2023-07-26 22:45:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A large tree was knocked over in Sun City near 108th Ave and Thunderbird Road. Diameter of trunk estimated to be 2-3 ft. Wind gusts were estimated between 55-60 mph. No injuries were reported.", "ts_dict_index": [13878, 13879, 13880]}
+{"event_id": 1120685, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-07-26 21:15:00", "end_date_time": "2023-07-26 21:15:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A 61 mph wind gust was measured at the Ak-Chin Regional Airport.", "ts_dict_index": [13881, 13882, 13883]}
+{"event_id": 1121116, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:05:00", "end_date_time": "2023-07-26 22:05:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Several homes along the area of North Mesa Drive and East McKellips Road in Mesa suffered roof damage. In addition to the damaged homes, a block wall was damaged and a downed tree estimated at two feet in diameter. Wind gusts were estimated at 55-60 mph. No injuries were reported.", "ts_dict_index": [13890, 13891, 13892]}
+{"event_id": 1121082, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:29:00", "end_date_time": "2023-07-26 22:29:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A 63 mph gust was measured at the Scottsdale Municipal Airport.", "ts_dict_index": [13839, 13840, 13841]}
+{"event_id": 1121080, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:30:00", "end_date_time": "2023-07-26 22:30:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A large pine tree with an estimated trunk diameter of 2-3 feet was knocked over in an apartment complex located in the are West Thunderbird Road in Phoenix. Wind gusts were estimated at 55-60 mph. No injuries were reported.", "ts_dict_index": [13899, 13900, 13901]}
+{"event_id": 1121440, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:30:00", "end_date_time": "2023-07-26 22:30:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Large tree down in the area of 7th Street and Bell Road in Phoenix. Diameter of tree estimated to be about a foot. Wind gusts were estimated at 55-60 mph. No injuries were reported.", "ts_dict_index": [13896, 13897, 13898]}
+{"event_id": 880022, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2020-04-19 14:49:00", "end_date_time": "2020-04-19 14:49:00", "narrative": "A warm front lifted north into Deep East Texas and the southern sections of North Central Louisiana by afternoon on April 19th, ahead of a vigorous upper level trough that ejected east from New Mexico across Texas. Large scale forcing increased by afternoon ahead of the trough as it approached the expanding warm sector, characteristic of moderate instability and strong wind shear. Areas of showers and thunderstorms developed and became widespread near and north of the warm front, and limited the northward progress of the front, but severe thunderstorms still developed within the warm sector across Deep East Texas and Northcentral Louisiana, resulting in areas of damaging winds across these areas, and even an isolated tornado in Grant Parish. These storms eventually weakened during the mid evening hours with the passage of the trough through the area. A tree was downed at the 2100 block of Highway 155 southwest of Ashland.", "ts_dict_index": [13914, 13915, 13916]}
+{"event_id": 1121083, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:30:00", "end_date_time": "2023-07-26 22:30:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Multiple downed trees with estimated diameter of 6-8 inches as well as a downed saguaro tree were reported in the area of I-17 and Happy Valley Road in Phoenix. Wind gusts were estimated between 55-60 mph. No injuries were reported.", "ts_dict_index": [13908, 13909, 13910]}
+{"event_id": 1121101, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:30:00", "end_date_time": "2023-07-26 22:30:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A large tree was down in the area of West Jomax Road and I-17. The tree toppled on top of a car. Diameter of the tree estimated at two feet. Wind gusts were estimated at 55-60 mph. No injuries were reported.", "ts_dict_index": [13902, 13903, 13904]}
+{"event_id": 1121093, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:05:00", "end_date_time": "2023-07-26 22:05:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A mobile home park located in the area of North Mesa Drive and East McKellips Road in Mesa suffered widespread damage with the awnings from roofs and carports ripped apart. Wind gusts were estimated at 55-60 mph. No injuries were reported.", "ts_dict_index": [13905, 13906, 13907]}
+{"event_id": 1121119, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2023-07-26 22:45:00", "end_date_time": "2023-07-26 22:45:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. Large tree down estimated to be 1.5 feet in diameter at the area of West Lakeview Road and North 93rd Avenue in Peoria. Wind gusts were estimated at 55-60 mph. No injuries were reported.", "ts_dict_index": [13893, 13894, 13895]}
+{"event_id": 880007, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2020-04-19 12:23:00", "end_date_time": "2020-04-19 12:23:00", "narrative": "A warm front lifted north into Deep East Texas and the southern sections of North Central Louisiana by afternoon on April 19th, ahead of a vigorous upper level trough that ejected east from New Mexico across Texas. Large scale forcing increased by afternoon ahead of the trough as it approached the expanding warm sector, characteristic of moderate instability and strong wind shear. Areas of showers and thunderstorms developed and became widespread near and north of the warm front, and limited the northward progress of the front, but severe thunderstorms still developed within the warm sector across Deep East Texas and Northcentral Louisiana, resulting in areas of damaging winds across these areas, and even an isolated tornado in Grant Parish. These storms eventually weakened during the mid evening hours with the passage of the trough through the area. A couple of trees were snapped/uprooted along Highway 478 just southwest of Pump Station Road south of Flora.", "ts_dict_index": [13911, 13912, 13913]}
+{"event_id": 1121442, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-07-26 21:15:00", "end_date_time": "2023-07-26 21:15:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. An overhead street sign was blown down in the area of Pinal Avenue and Florence Boulevard in Casa Grande. Wind gusts were estimated around 55 mph. No injuries were reported.", "ts_dict_index": [13869, 13870, 13871]}
+{"event_id": 951565, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-05-26 21:40:00", "end_date_time": "2021-05-26 21:40:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Nottingham Dr. Time estimated from radar.", "ts_dict_index": [13926, 13927, 13928]}
+{"event_id": 951566, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-05-26 21:37:00", "end_date_time": "2021-05-26 21:37:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Globe Ln. Time estimated from radar.", "ts_dict_index": [13929, 13930, 13931]}
+{"event_id": 951520, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-05-26 16:21:00", "end_date_time": "2021-05-26 16:21:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Park Rd. Time estimated from radar and utility company reports.", "ts_dict_index": [13932, 13933, 13934]}
+{"event_id": 951567, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-05-26 21:42:00", "end_date_time": "2021-05-26 21:42:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Shreve St. Time estimated from radar.", "ts_dict_index": [13935, 13936, 13937]}
+{"event_id": 951559, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-05-26 21:23:00", "end_date_time": "2021-05-26 21:23:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees were downed in Palmyra.", "ts_dict_index": [13938, 13939, 13940]}
+{"event_id": 951568, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2021-05-26 21:22:00", "end_date_time": "2021-05-26 21:22:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Several reports of downed tree limbs and wires in the Pennsauken area. Time estimated from radar.", "ts_dict_index": [13941, 13942, 13943]}
+{"event_id": 880004, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2020-04-19 12:24:00", "end_date_time": "2020-04-19 12:24:00", "narrative": "A warm front lifted north into Deep East Texas and the southern sections of North Central Louisiana by afternoon on April 19th, ahead of a vigorous upper level trough that ejected east from New Mexico across Texas. Large scale forcing increased by afternoon ahead of the trough as it approached the expanding warm sector, characteristic of moderate instability and strong wind shear. Areas of showers and thunderstorms developed and became widespread near and north of the warm front, and limited the northward progress of the front, but severe thunderstorms still developed within the warm sector across Deep East Texas and Northcentral Louisiana, resulting in areas of damaging winds across these areas, and even an isolated tornado in Grant Parish. These storms eventually weakened during the mid evening hours with the passage of the trough through the area. A tree was downed onto a power line near the intersection of Highway 120 and 478 in Flora.", "ts_dict_index": [13920, 13921, 13922]}
+{"event_id": 879998, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2020-04-19 12:22:00", "end_date_time": "2020-04-19 12:22:00", "narrative": "A warm front lifted north into Deep East Texas and the southern sections of North Central Louisiana by afternoon on April 19th, ahead of a vigorous upper level trough that ejected east from New Mexico across Texas. Large scale forcing increased by afternoon ahead of the trough as it approached the expanding warm sector, characteristic of moderate instability and strong wind shear. Areas of showers and thunderstorms developed and became widespread near and north of the warm front, and limited the northward progress of the front, but severe thunderstorms still developed within the warm sector across Deep East Texas and Northcentral Louisiana, resulting in areas of damaging winds across these areas, and even an isolated tornado in Grant Parish. These storms eventually weakened during the mid evening hours with the passage of the trough through the area. A tree was downed on Highway 153 near Creston.", "ts_dict_index": [13917, 13918, 13919]}
+{"event_id": 1121443, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "PINAL", "begin_date_time": "2023-07-26 21:00:00", "end_date_time": "2023-07-26 21:00:00", "narrative": "With the subtropical high pressure situated across central New Mexico, a southeasterly wind flow was established across Arizona. Thunderstorm activity developed across portions of southeast AZ during the afternoon hours. MLCAPE between 500-1000 J/KG as well as Downdraft CAPE near 2000 J/KG aided in creating a favorable environment for the thunderstorm activity to result in strong downburst winds. The first thunderstorm activity to develop across portions of southeast AZ resulted in the development of a strong outflow boundary, responsible for dense blowing dust conditions across Pinal and southern Maricopa Counties as well as sparking additional storms that affected portions of the Phoenix metro area. With the thunderstorms that moved across the Phoenix metro area, there were several reports of tree damage as well as structural damage to several homes. A tree, with three separate trunks estimated to be 1-2 feet in diameter toppled and damaged a cinderblock wall along the area of West Loma Verde Avenue and West Acacia Drive in Eloy. Wind gusts were estimated at 55-60 mph. No injuries were reported.", "ts_dict_index": [13887, 13888, 13889]}
+{"event_id": 951572, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-05-26 22:20:00", "end_date_time": "2021-05-26 22:20:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Sea Breeze Dr. Time estimated from radar.", "ts_dict_index": [13944, 13945, 13946]}
+{"event_id": 951427, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:27:00", "end_date_time": "2021-05-26 15:27:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Chapel Hill Rd. Time estimated from radar.", "ts_dict_index": [13950, 13951, 13952]}
+{"event_id": 951429, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:27:00", "end_date_time": "2021-05-26 15:27:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near River Rd. Time estimated from radar.", "ts_dict_index": [13956, 13957, 13958]}
+{"event_id": 951426, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:25:00", "end_date_time": "2021-05-26 15:25:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed on US-222 near Bernville Rd. Time estimated from radar.", "ts_dict_index": [13974, 13975, 13976]}
+{"event_id": 951526, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 18:26:00", "end_date_time": "2021-05-26 18:26:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. An mPing report of large tree limbs or power lines down.", "ts_dict_index": [13947, 13948, 13949]}
+{"event_id": 951522, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-05-26 16:25:00", "end_date_time": "2021-05-26 16:25:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Route 212 in Durham Twp. Time estimated from radar.", "ts_dict_index": [13962, 13963, 13964]}
+{"event_id": 951514, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-05-26 15:58:00", "end_date_time": "2021-05-26 15:58:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed in wires on Kutztown Rd near Township Woods Rd. Time estimated from radar.", "ts_dict_index": [13971, 13972, 13973]}
+{"event_id": 951431, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:27:00", "end_date_time": "2021-05-26 15:27:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Christman Rd. Time estimated from radar.", "ts_dict_index": [13959, 13960, 13961]}
+{"event_id": 951571, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-05-26 21:42:00", "end_date_time": "2021-05-26 21:42:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Wires were downed near Lambert Dr. Time estimated from radar.", "ts_dict_index": [13968, 13969, 13970]}
+{"event_id": 951523, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-05-26 15:58:00", "end_date_time": "2021-05-26 15:58:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Downed trees and wires near Farmington Ave on the Berks/Montgomery County border. Time estimated from radar.", "ts_dict_index": [13965, 13966, 13967]}
+{"event_id": 951518, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-05-26 16:05:00", "end_date_time": "2021-05-26 16:05:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed near the intersection of Limeport Pike and Chestnut Hill Church Rd. Time estimated from radar.", "ts_dict_index": [13923, 13924, 13925]}
+{"event_id": 951476, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-05-26 16:07:00", "end_date_time": "2021-05-26 16:07:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Several reports of downed trees and wires near and west of Sellersville. Time estimated from radar.", "ts_dict_index": [14004, 14005, 14006]}
+{"event_id": 951435, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:30:00", "end_date_time": "2021-05-26 15:30:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Social media video of a tree blowing down from strong thunderstorm winds, which appeared to be about 60 mph.", "ts_dict_index": [13983, 13984, 13985]}
+{"event_id": 951424, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:11:00", "end_date_time": "2021-05-26 15:11:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A power pole snapped on Holly Rd. Time estimated from radar.", "ts_dict_index": [13989, 13990, 13991]}
+{"event_id": 951425, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:13:00", "end_date_time": "2021-05-26 15:13:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Garfield Rd. Time estimated from radar.", "ts_dict_index": [13986, 13987, 13988]}
+{"event_id": 951434, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:29:00", "end_date_time": "2021-05-26 15:29:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. An mPing report of uprooted trees or snapped power poles near Adam Rd. Time estimated from radar.", "ts_dict_index": [13980, 13981, 13982]}
+{"event_id": 951452, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:53:00", "end_date_time": "2021-05-26 15:53:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Mulberry Hill Rd. Time estimated from radar.", "ts_dict_index": [13995, 13996, 13997]}
+{"event_id": 951436, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:33:00", "end_date_time": "2021-05-26 15:33:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed on Basket Rd. Time estimated from radar.", "ts_dict_index": [13998, 13999, 14000]}
+{"event_id": 951477, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-05-26 16:05:00", "end_date_time": "2021-05-26 16:05:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Several downed trees and a downed power pole were reported. Time estimated from radar.", "ts_dict_index": [14001, 14002, 14003]}
+{"event_id": 951473, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-05-26 15:58:00", "end_date_time": "2021-05-26 15:58:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed on Reifsnyder Rd near Swamp Picnic Rd. Time estimated from radar.", "ts_dict_index": [14022, 14023, 14024]}
+{"event_id": 951478, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-05-26 16:05:00", "end_date_time": "2021-05-26 16:05:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed on Ward Rd. Time estimated from radar.", "ts_dict_index": [14025, 14026, 14027]}
+{"event_id": 951474, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-05-26 16:30:00", "end_date_time": "2021-05-26 16:30:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs were downed on Fourth Ave and Lincoln Ave. Time estimated from radar.", "ts_dict_index": [14019, 14020, 14021]}
+{"event_id": 951525, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-05-26 16:54:00", "end_date_time": "2021-05-26 16:54:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Daleville Rd. Time estimated from radar.", "ts_dict_index": [13992, 13993, 13994]}
+{"event_id": 951458, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-05-26 15:55:00", "end_date_time": "2021-05-26 15:55:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A social media photo of a snapped tree in a neighborhood near Allentown. Time estimated from radar.", "ts_dict_index": [14007, 14008, 14009]}
+{"event_id": 951475, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-05-26 15:58:00", "end_date_time": "2021-05-26 15:58:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Several reports of downed trees and wires southwest of Allentown. Time estimated from radar.", "ts_dict_index": [14016, 14017, 14018]}
+{"event_id": 951455, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-05-26 15:55:00", "end_date_time": "2021-05-26 15:55:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Six homes along Oakwood Trail and Dogwood Trail were damaged by strong wind gusts and falling trees.", "ts_dict_index": [14013, 14014, 14015]}
+{"event_id": 951457, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-05-26 15:55:00", "end_date_time": "2021-05-26 15:55:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Wires were downed near Haines Mill Rd. Time estimated from radar.", "ts_dict_index": [14010, 14011, 14012]}
+{"event_id": 951509, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-05-26 16:16:00", "end_date_time": "2021-05-26 16:16:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Kellers Rd and Mine Rd. Time estimated from radar.", "ts_dict_index": [14031, 14032, 14033]}
+{"event_id": 951510, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-05-26 16:23:00", "end_date_time": "2021-05-26 16:23:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A downed tree blocked Overbrook Dr near Gwynedd Valley Dr. Time estimated from radar.", "ts_dict_index": [14028, 14029, 14030]}
+{"event_id": 951507, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-05-26 16:21:00", "end_date_time": "2021-05-26 16:21:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near County Line Rd and Business Route 202. Time estimated from radar.", "ts_dict_index": [14037, 14038, 14039]}
+{"event_id": 951508, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-05-26 15:58:00", "end_date_time": "2021-05-26 15:58:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Kressler Rd. Time estimated from radar.", "ts_dict_index": [14034, 14035, 14036]}
+{"event_id": 951432, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:29:00", "end_date_time": "2021-05-26 15:29:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Westwood Rd. Time estimated from radar.", "ts_dict_index": [13977, 13978, 13979]}
+{"event_id": 951575, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-05-26 22:36:00", "end_date_time": "2021-05-26 22:36:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Wires were downed near Washington Ave. Time estimated from radar.", "ts_dict_index": [14076, 14077, 14078]}
+{"event_id": 951558, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "BURLINGTON", "begin_date_time": "2021-05-26 21:53:00", "end_date_time": "2021-05-26 21:53:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed in Medford. Time estimated from radar.", "ts_dict_index": [14043, 14044, 14045]}
+{"event_id": 951440, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:35:00", "end_date_time": "2021-05-26 15:35:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Lytle Ln. Time estimated from radar.", "ts_dict_index": [14070, 14071, 14072]}
+{"event_id": 951441, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:35:00", "end_date_time": "2021-05-26 15:35:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Multiple trees were downed on Crystal Ridge Rd. Time estimated from radar and dispatch report.", "ts_dict_index": [14067, 14068, 14069]}
+{"event_id": 951471, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:58:00", "end_date_time": "2021-05-26 15:58:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Ridgeway Rd. Time estimated from radar.", "ts_dict_index": [14055, 14056, 14057]}
+{"event_id": 951472, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-05-26 16:05:00", "end_date_time": "2021-05-26 16:05:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed on Salford Station Rd near Cepp Rd. Time estimated from radar.", "ts_dict_index": [14061, 14062, 14063]}
+{"event_id": 951576, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2021-05-26 21:35:00", "end_date_time": "2021-05-26 21:35:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Wires were downed near Hemlock Ln. Time estimated from radar.", "ts_dict_index": [14073, 14074, 14075]}
+{"event_id": 951499, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-05-26 16:09:00", "end_date_time": "2021-05-26 16:09:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Mountain View Rd. Time estimated from radar.", "ts_dict_index": [14046, 14047, 14048]}
+{"event_id": 951480, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-05-26 16:39:00", "end_date_time": "2021-05-26 16:39:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs were downed on Davisville Rd and Danielle Dr. Time estimated from radar.", "ts_dict_index": [14052, 14053, 14054]}
+{"event_id": 951442, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:39:00", "end_date_time": "2021-05-26 15:39:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Several reports of downed trees and wires in the Bowers area. Time estimated from radar.", "ts_dict_index": [14064, 14065, 14066]}
+{"event_id": 951500, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-05-26 16:32:00", "end_date_time": "2021-05-26 16:32:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed on Styer Rd near Meadow Creek Ln. Time estimated from radar.", "ts_dict_index": [14040, 14041, 14042]}
+{"event_id": 951481, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-05-26 16:27:00", "end_date_time": "2021-05-26 16:27:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed on Buck Dr near Rabbit Run Ln. Time estimated from radar.", "ts_dict_index": [14049, 14050, 14051]}
+{"event_id": 951516, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-05-26 16:10:00", "end_date_time": "2021-05-26 16:10:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs were downed near Walnut Ln. Time estimated from radar.", "ts_dict_index": [13953, 13954, 13955]}
+{"event_id": 951449, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:50:00", "end_date_time": "2021-05-26 15:50:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Hillcrest Rd. Time estimated from radar.", "ts_dict_index": [14100, 14101, 14102]}
+{"event_id": 951448, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:48:00", "end_date_time": "2021-05-26 15:48:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Several reports of trees and wires down in the Klines Corner and Maxatawany areas. Time estimated from radar.", "ts_dict_index": [14103, 14104, 14105]}
+{"event_id": 951437, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:33:00", "end_date_time": "2021-05-26 15:33:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. An mPing report of downed tree limbs or wires.", "ts_dict_index": [14085, 14086, 14087]}
+{"event_id": 951450, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:52:00", "end_date_time": "2021-05-26 15:52:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. An mPing report of downed tree limbs or power lines near Lines Valley Rd. Time estimated from radar.", "ts_dict_index": [14097, 14098, 14099]}
+{"event_id": 951438, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:35:00", "end_date_time": "2021-05-26 15:35:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed on Kutztown Rd. Time estimated from radar.", "ts_dict_index": [14082, 14083, 14084]}
+{"event_id": 951451, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:53:00", "end_date_time": "2021-05-26 15:53:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Ironstone Dr. Time estimated from radar.", "ts_dict_index": [14094, 14095, 14096]}
+{"event_id": 951444, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:48:00", "end_date_time": "2021-05-26 15:48:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed on Powder Mill Hollow Rd. Time estimated from radar.", "ts_dict_index": [14112, 14113, 14114]}
+{"event_id": 951445, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:48:00", "end_date_time": "2021-05-26 15:48:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Forgedale Rd. Time estimated from radar.", "ts_dict_index": [14109, 14110, 14111]}
+{"event_id": 951447, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:48:00", "end_date_time": "2021-05-26 15:48:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. An mPing report of downed tree limbs and power lines near Old Topton Rd. Time estimated from radar.", "ts_dict_index": [14106, 14107, 14108]}
+{"event_id": 951454, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-05-26 15:54:00", "end_date_time": "2021-05-26 15:54:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Hickory Circle. Time estimated from radar.", "ts_dict_index": [14088, 14089, 14090]}
+{"event_id": 951529, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "OCEAN", "begin_date_time": "2021-05-26 18:38:00", "end_date_time": "2021-05-26 18:38:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. NJ Weathernet measured gust.", "ts_dict_index": [14079, 14080, 14081]}
+{"event_id": 893823, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:17:00", "end_date_time": "2020-05-15 17:17:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Stump Church Road.", "ts_dict_index": [14133, 14134, 14135]}
+{"event_id": 951422, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-05-26 16:20:00", "end_date_time": "2021-05-26 16:20:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A broadcast meteorologist estimated 60 to 65 mph wind gusts near Allentown Rd and County Line Rd, which was supported by an accompanying video.", "ts_dict_index": [14115, 14116, 14117]}
+{"event_id": 951511, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-05-26 16:44:00", "end_date_time": "2021-05-26 16:44:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Trees and wires were downed near Sixth St and Market St. Time estimated from radar.", "ts_dict_index": [14124, 14125, 14126]}
+{"event_id": 951512, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-05-26 16:49:00", "end_date_time": "2021-05-26 16:49:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Wires were downed near Loop Rd. Time estimated from radar.", "ts_dict_index": [14127, 14128, 14129]}
+{"event_id": 893821, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:24:00", "end_date_time": "2020-05-15 17:24:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees were downed and a barn collapsed.", "ts_dict_index": [14136, 14137, 14138]}
+{"event_id": 951501, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-05-26 16:27:00", "end_date_time": "2021-05-26 16:27:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Wires were downed on Wistar Rd near Chetwynd Rd. Time estimated from radar.", "ts_dict_index": [14118, 14119, 14120]}
+{"event_id": 951515, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-05-26 16:52:00", "end_date_time": "2021-05-26 16:52:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. Tree limbs and wires were downed near Mindy Dr. Time estimated from radar.", "ts_dict_index": [14121, 14122, 14123]}
+{"event_id": 1100452, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-07-03 17:05:00", "end_date_time": "2023-07-03 17:05:00", "narrative": "A broad positively tilted upper trough continued to extend from the Great Lakes Region and Mid-Mississippi Valley southwest into North Texas during the afternoon of July 3rd, while an associated weak surface front lifted back north before becoming stationary across Southeast Oklahoma and Western/Central Arkansas. Strong heating within a moist air mass resulted in strong instability developing during the afternoon, with large scale forcing ahead of the trough adequate enough for the development of scattered showers and thunderstorms across portions of Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and Northwest Louisiana during the afternoon. One isolated severe thunderstorm developed over Northeast McCurtain County Oklahoma, producing damaging winds which downed multiple trees near Smithville. Large hail was also observed from this storm. Multiple trees were downed near Smithville.", "ts_dict_index": [14130, 14131, 14132]}
+{"event_id": 893826, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:26:00", "end_date_time": "2020-05-15 17:26:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Perry Hill Road.", "ts_dict_index": [14139, 14140, 14141]}
+{"event_id": 893825, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:22:00", "end_date_time": "2020-05-15 17:22:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on County Route 64.", "ts_dict_index": [14148, 14149, 14150]}
+{"event_id": 893822, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:23:00", "end_date_time": "2020-05-15 17:23:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed at West Main Street and Gilmore Avenue.", "ts_dict_index": [14142, 14143, 14144]}
+{"event_id": 893767, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:15:00", "end_date_time": "2020-05-15 17:15:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Coon Road.", "ts_dict_index": [14157, 14158, 14159]}
+{"event_id": 893771, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:08:00", "end_date_time": "2020-05-15 17:08:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Three large trees were downed in Fort Edward.", "ts_dict_index": [14151, 14152, 14153]}
+{"event_id": 893817, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:22:00", "end_date_time": "2020-05-15 17:22:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on McDougal Lake Road.", "ts_dict_index": [14145, 14146, 14147]}
+{"event_id": 893724, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:15:00", "end_date_time": "2020-05-15 17:15:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Colonel Baume Road.", "ts_dict_index": [14154, 14155, 14156]}
+{"event_id": 893769, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:15:00", "end_date_time": "2020-05-15 17:15:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on County Route 49.", "ts_dict_index": [14160, 14161, 14162]}
+{"event_id": 893811, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:18:00", "end_date_time": "2020-05-15 17:18:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on County Route 48.", "ts_dict_index": [14166, 14167, 14168]}
+{"event_id": 893770, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:11:00", "end_date_time": "2020-05-15 17:11:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. A pole and wires were downed on Route 4 at Cary Road.", "ts_dict_index": [14169, 14170, 14171]}
+{"event_id": 893810, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:18:00", "end_date_time": "2020-05-15 17:18:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Rabbit Road.", "ts_dict_index": [14163, 14164, 14165]}
+{"event_id": 951460, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2021-05-26 15:55:00", "end_date_time": "2021-05-26 15:55:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was downed on Ziegler Rd near Gravel Pike. Time estimated from radar.", "ts_dict_index": [14058, 14059, 14060]}
+{"event_id": 893719, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:13:00", "end_date_time": "2020-05-15 17:13:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Ryan Road, and a shed was blown over nearby.", "ts_dict_index": [14181, 14182, 14183]}
+{"event_id": 893813, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:24:00", "end_date_time": "2020-05-15 17:24:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. There were multiple reports of trees down in the Salem area and the Town of Jackson.", "ts_dict_index": [14178, 14179, 14180]}
+{"event_id": 893720, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:08:00", "end_date_time": "2020-05-15 17:08:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on North River Road.", "ts_dict_index": [14193, 14194, 14195]}
+{"event_id": 893815, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:22:00", "end_date_time": "2020-05-15 17:22:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Dobbin Hill Road.", "ts_dict_index": [14187, 14188, 14189]}
+{"event_id": 893824, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:25:00", "end_date_time": "2020-05-15 17:25:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Juniper Swamp Road.", "ts_dict_index": [14175, 14176, 14177]}
+{"event_id": 893809, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:18:00", "end_date_time": "2020-05-15 17:18:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Derby Road.", "ts_dict_index": [14172, 14173, 14174]}
+{"event_id": 893814, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:22:00", "end_date_time": "2020-05-15 17:22:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Dunbar Road.", "ts_dict_index": [14184, 14185, 14186]}
+{"event_id": 893816, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:22:00", "end_date_time": "2020-05-15 17:22:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Ackley Road.", "ts_dict_index": [14190, 14191, 14192]}
+{"event_id": 893709, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:09:00", "end_date_time": "2020-05-15 17:09:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on County Road 113.", "ts_dict_index": [14205, 14206, 14207]}
+{"event_id": 893820, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:24:00", "end_date_time": "2020-05-15 17:24:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on State Route 22.", "ts_dict_index": [14196, 14197, 14198]}
+{"event_id": 893716, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:12:00", "end_date_time": "2020-05-15 17:12:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on State Route 40.", "ts_dict_index": [14214, 14215, 14216]}
+{"event_id": 893712, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:11:00", "end_date_time": "2020-05-15 17:11:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Ashdown Way.", "ts_dict_index": [14208, 14209, 14210]}
+{"event_id": 893812, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:19:00", "end_date_time": "2020-05-15 17:19:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Reafield Farm Road.", "ts_dict_index": [14199, 14200, 14201]}
+{"event_id": 893714, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:12:00", "end_date_time": "2020-05-15 17:12:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Hegeman Bridge Road.", "ts_dict_index": [14211, 14212, 14213]}
+{"event_id": 954122, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2021-06-13 15:13:00", "end_date_time": "2021-06-13 15:13:00", "narrative": "Scattered showers and thunderstorms developed during the mid-afternoon hours across Northcentral Louisiana on June 13th, near a weak surface trough extending from Southeast Oklahoma, extreme Southwest Arkansas, and North Louisiana. Compressional warming and low level moisture pooling near this boundary resulted in a very unstable air mass developing across much of the region, with a weak upper level disturbance sliding southwest across North Louisiana and East Texas during the afternoon and evening contributing to increasing large scale ascent. As a result, one of these storms became severe over Eastern Union Parish Louisiana, producing damaging winds which downed a large tree on a home west of Sterlington. These storms continued to redevelop and shift west-southwest across North Louisiana through the evening and into East Texas after midnight. A very large oak tree fell down onto a home near the Rocky Branch community.", "ts_dict_index": [14217, 14218, 14219]}
+{"event_id": 1054618, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-08-21 18:11:00", "end_date_time": "2022-08-21 18:11:00", "narrative": "Similar to the 20th, thunderstorms once again initiated across the northern Arizona high terrain during the afternoon of the 21st, though more focused along the Mogollon Rim compared to the day prior. Increased steering flow allowed for thunderstorms to move off of the Rim and toward the lower elevations. High instability (MUCAPE 2,000-2,500 J/kg) helped thunderstorms maintain intensity as they travelled toward the lower deserts. Given the greater steering flow, faster thunderstorm motion helped abate flash flood impacts. Greater shear across northwest Arizona allowed an organized complex of thunderstorms to develop during the evening hours before progressing through southwest Arizona and the Lower Colorado River Valley area, producing severe wind gusts and dense blowing dust into the early morning hours on the 22nd. No injuries were reported. A large tree fell between two parked vehicles at a condominium at Roosevelt Street and Granite Reef Road. Timing estimated from radar. No injuries were reported.", "ts_dict_index": [14220, 14221, 14222]}
+{"event_id": 951443, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-05-26 15:40:00", "end_date_time": "2021-05-26 15:40:00", "narrative": "Following a more than two week stretch of dry weather, a cold front approached the mid-Atlantic on May 26. Ahead of the front, an unseasonably hot and humid air mass developed, with high temperatures near to above 90 degrees in much of the region. This contributed to strong instability, while wind shear was more moderate. Multiple rounds of convection affected the region, triggered by a pre-frontal trough and a couple of upper level impulses ahead of the front. A fairly widespread severe weather event resulted, with damaging winds by far the most widespread hazard. Numerous instances of downed trees and power lines and some property damage were reported. Thunderstorms during the evening hours were also prolific lightning producers. The final round of storms finally moved offshore close to midnight after several hours of severe weather in the region. A tree was reported down from high winds, along with pea size hail.", "ts_dict_index": [14091, 14092, 14093]}
+{"event_id": 1056602, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2022-09-25 15:43:00", "end_date_time": "2022-09-25 15:43:00", "narrative": "Northwesterly flow aloft aided in pushing a cold front southward into the region on the afternoon of September 25th. Despite only weak upper-level support, frontal forcing was sufficient to generate scattered convection along the frontal boundary during the afternoon. The atmosphere was relatively uncapped, and with afternoon temperatures climbing into the mid 90s, moderate surface-based instability developed. However, a lack of deep layer moisture appeared to be a limiting factor for any severe weather although classic inverted-V forecast soundings indicated the potential for isolated damaging wind gusts from thunderstorm downbursts in the afternoon. Moisture proved to be sufficient for storms to rapidly develop by mid to late afternoon, quickly accelerating southward and producing sporadic damaging wind gusts across parts of Union Parish. Tree downed near New Hope and River Road near Spearsville.", "ts_dict_index": [14241, 14242, 14243]}
+{"event_id": 1029539, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-06-17 11:24:00", "end_date_time": "2022-06-17 11:24:00", "narrative": "A stationary front was located north of the state heading into the day on June 17th, before transitioning to a slow moving cold front that continued to near the state throughout the day. Eastern KY's placement in the warm sector, combined with ample moisture advection from the Gulf of Mexico, set the stage for shower and thunderstorm development. Storms developed to our west, over western and central Kentucky, and began to impact eastern Kentucky by just after noon. Strong winds aloft resulted in wind damage at the surface, as well as decent storm motions. Most of the storms had exited the state just 2 to 3 hours later. Some of the strongest storms brought widespread downed trees and power lines and caused damage to buildings and home around eastern Kentucky. In total, 121 storm reports of damage were sent out as a result of this storm system. Trees were blown down along Bourbon Road near Somerset.", "ts_dict_index": [14238, 14239, 14240]}
+{"event_id": 939789, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2021-03-17 07:58:00", "end_date_time": "2021-03-17 07:58:00", "narrative": "A strong closed upper low pressure system ejected northeast through the Oklahoma/Texas Panhandle region during the afternoon and evening hours of March 16th, which helped mix a dry line east across Oklahoma and Texas. Ahead of this dry line, a broad warm and moist sector spread north across the Ark-La-Tex, which allowed for greater instability to overspread into the area ahead of this surface feature. A complex of showers and thunderstorms developed over West Texas during the late afternoon through the evening hours on the 16th, before advancing east across the state during the overnight and early morning hours of the 17th. Some of these storms remained severe as they moved through East Texas around and shortly after daybreak, where damaging winds downed trees and power lines before gradually weakening as they moved into Western Louisiana. Several trees were blown down just west of Carthage.", "ts_dict_index": [14247, 14248, 14249]}
+{"event_id": 1029550, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-06-17 11:33:00", "end_date_time": "2022-06-17 11:33:00", "narrative": "A stationary front was located north of the state heading into the day on June 17th, before transitioning to a slow moving cold front that continued to near the state throughout the day. Eastern KY's placement in the warm sector, combined with ample moisture advection from the Gulf of Mexico, set the stage for shower and thunderstorm development. Storms developed to our west, over western and central Kentucky, and began to impact eastern Kentucky by just after noon. Strong winds aloft resulted in wind damage at the surface, as well as decent storm motions. Most of the storms had exited the state just 2 to 3 hours later. Some of the strongest storms brought widespread downed trees and power lines and caused damage to buildings and home around eastern Kentucky. In total, 121 storm reports of damage were sent out as a result of this storm system. Trees were blown down along Hickory Nut Road in Pointer.", "ts_dict_index": [14235, 14236, 14237]}
+{"event_id": 1029843, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-06-17 11:42:00", "end_date_time": "2022-06-17 11:42:00", "narrative": "A stationary front was located north of the state heading into the day on June 17th, before transitioning to a slow moving cold front that continued to near the state throughout the day. Eastern KY's placement in the warm sector, combined with ample moisture advection from the Gulf of Mexico, set the stage for shower and thunderstorm development. Storms developed to our west, over western and central Kentucky, and began to impact eastern Kentucky by just after noon. Strong winds aloft resulted in wind damage at the surface, as well as decent storm motions. Most of the storms had exited the state just 2 to 3 hours later. Some of the strongest storms brought widespread downed trees and power lines and caused damage to buildings and home around eastern Kentucky. In total, 121 storm reports of damage were sent out as a result of this storm system. Trees were blown down and onto KY-192 near Rockcastle Spring.", "ts_dict_index": [14232, 14233, 14234]}
+{"event_id": 1029553, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-06-17 11:35:00", "end_date_time": "2022-06-17 11:35:00", "narrative": "A stationary front was located north of the state heading into the day on June 17th, before transitioning to a slow moving cold front that continued to near the state throughout the day. Eastern KY's placement in the warm sector, combined with ample moisture advection from the Gulf of Mexico, set the stage for shower and thunderstorm development. Storms developed to our west, over western and central Kentucky, and began to impact eastern Kentucky by just after noon. Strong winds aloft resulted in wind damage at the surface, as well as decent storm motions. Most of the storms had exited the state just 2 to 3 hours later. Some of the strongest storms brought widespread downed trees and power lines and caused damage to buildings and home around eastern Kentucky. In total, 121 storm reports of damage were sent out as a result of this storm system. Trees were blown down along Hall Ridge Road.", "ts_dict_index": [14226, 14227, 14228]}
+{"event_id": 1029552, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-06-17 11:35:00", "end_date_time": "2022-06-17 11:35:00", "narrative": "A stationary front was located north of the state heading into the day on June 17th, before transitioning to a slow moving cold front that continued to near the state throughout the day. Eastern KY's placement in the warm sector, combined with ample moisture advection from the Gulf of Mexico, set the stage for shower and thunderstorm development. Storms developed to our west, over western and central Kentucky, and began to impact eastern Kentucky by just after noon. Strong winds aloft resulted in wind damage at the surface, as well as decent storm motions. Most of the storms had exited the state just 2 to 3 hours later. Some of the strongest storms brought widespread downed trees and power lines and caused damage to buildings and home around eastern Kentucky. In total, 121 storm reports of damage were sent out as a result of this storm system. Trees were blown down along Slate Branch Road near Bronston.", "ts_dict_index": [14229, 14230, 14231]}
+{"event_id": 939787, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2021-03-17 07:58:00", "end_date_time": "2021-03-17 07:58:00", "narrative": "A strong closed upper low pressure system ejected northeast through the Oklahoma/Texas Panhandle region during the afternoon and evening hours of March 16th, which helped mix a dry line east across Oklahoma and Texas. Ahead of this dry line, a broad warm and moist sector spread north across the Ark-La-Tex, which allowed for greater instability to overspread into the area ahead of this surface feature. A complex of showers and thunderstorms developed over West Texas during the late afternoon through the evening hours on the 16th, before advancing east across the state during the overnight and early morning hours of the 17th. Some of these storms remained severe as they moved through East Texas around and shortly after daybreak, where damaging winds downed trees and power lines before gradually weakening as they moved into Western Louisiana. Trees were blown down in Karnack. A Texas State Trooper's vehicle was damaged by a falling tree.", "ts_dict_index": [14244, 14245, 14246]}
+{"event_id": 893713, "event_type": "Thunderstorm Wind", "state": "NEW YORK", "cz_name": "WASHINGTON", "begin_date_time": "2020-05-15 17:12:00", "end_date_time": "2020-05-15 17:12:00", "narrative": "On Friday, May 15, 2020, an intense line of thunderstorms quickly developed near Lake Ontario and raced eastward into eastern New York. A segment of particularly strong and long-lasting thunderstorms impacted the region from just north of the Mohawk Valley in Herkimer County into Saratoga and Washington counties, producing damaging winds throughout its path. Notable areas of damage include a confirmed macroburst near Russia and Cold Brook, NY where wind estimates ranged from 80 to 100 mph, an EF-1 tornado in Wilton, NY, and numerous trees snapped or uprooted in Saratoga and Washington counties. A supercell that developed in the eastern Catskills produced a microburst in Cottekill, NY. Around 71,000 customers were without power at the height of the storm, and the American Red Cross provided emergency aid to 10 people after their homes were damaged. Trees and wires were downed on Cheese Factory Road.", "ts_dict_index": [14202, 14203, 14204]}
+{"event_id": 956574, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-06-21 18:19:00", "end_date_time": "2021-06-21 18:19:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. Trees and wires were downed near Blue Rocks Rd. Time estimated from radar.", "ts_dict_index": [14280, 14281, 14282]}
+{"event_id": 956590, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 17:58:00", "end_date_time": "2021-06-21 17:58:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A tree, wires, and a power pole were downed on a residence near Forge Ln. Time estimated from radar.", "ts_dict_index": [14262, 14263, 14264]}
+{"event_id": 939785, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "SMITH", "begin_date_time": "2021-03-17 06:35:00", "end_date_time": "2021-03-17 06:35:00", "narrative": "A strong closed upper low pressure system ejected northeast through the Oklahoma/Texas Panhandle region during the afternoon and evening hours of March 16th, which helped mix a dry line east across Oklahoma and Texas. Ahead of this dry line, a broad warm and moist sector spread north across the Ark-La-Tex, which allowed for greater instability to overspread into the area ahead of this surface feature. A complex of showers and thunderstorms developed over West Texas during the late afternoon through the evening hours on the 16th, before advancing east across the state during the overnight and early morning hours of the 17th. Some of these storms remained severe as they moved through East Texas around and shortly after daybreak, where damaging winds downed trees and power lines before gradually weakening as they moved into Western Louisiana. Numerous trees were blown down in the southeast part of Smith County.", "ts_dict_index": [14253, 14254, 14255]}
+{"event_id": 956553, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 17:45:00", "end_date_time": "2021-06-21 17:45:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A tree and wires were downed. Time estimated from radar.", "ts_dict_index": [14268, 14269, 14270]}
+{"event_id": 956582, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 18:02:00", "end_date_time": "2021-06-21 18:02:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. Tree limbs were down on Edge Ln. Time estimated from radar.", "ts_dict_index": [14265, 14266, 14267]}
+{"event_id": 956589, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 18:07:00", "end_date_time": "2021-06-21 18:07:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A tree was downed on Mill Ln. Time estimated from radar.", "ts_dict_index": [14283, 14284, 14285]}
+{"event_id": 956576, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 18:02:00", "end_date_time": "2021-06-21 18:02:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. Outflow winds downed trees and wires near Hill Rd. Time estimated from radar.", "ts_dict_index": [14274, 14275, 14276]}
+{"event_id": 956584, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 17:58:00", "end_date_time": "2021-06-21 17:58:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A tree was downed on Boot Rd. Time estimated from radar.", "ts_dict_index": [14271, 14272, 14273]}
+{"event_id": 939788, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2021-03-17 08:00:00", "end_date_time": "2021-03-17 08:00:00", "narrative": "A strong closed upper low pressure system ejected northeast through the Oklahoma/Texas Panhandle region during the afternoon and evening hours of March 16th, which helped mix a dry line east across Oklahoma and Texas. Ahead of this dry line, a broad warm and moist sector spread north across the Ark-La-Tex, which allowed for greater instability to overspread into the area ahead of this surface feature. A complex of showers and thunderstorms developed over West Texas during the late afternoon through the evening hours on the 16th, before advancing east across the state during the overnight and early morning hours of the 17th. Some of these storms remained severe as they moved through East Texas around and shortly after daybreak, where damaging winds downed trees and power lines before gradually weakening as they moved into Western Louisiana. Trees were blown down in Elysian Fields.", "ts_dict_index": [14250, 14251, 14252]}
+{"event_id": 827974, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "NATCHITOCHES", "begin_date_time": "2019-06-02 13:38:00", "end_date_time": "2019-06-02 13:38:00", "narrative": "The remnants of a mesoscale convective system (MCS) that originated over the Texas Panhandle and Northwest Texas during the early morning hours of June 2nd drifted east southeast into portions of East Texas and Northwest Louisiana during the daytime hours. An associated outflow boundary from this system focused scattered thunderstorm development during the afternoon across the southern half of Deep East Texas into Northwest Louisiana, where moderate instability developed once temperatures climbed into the lower 90s. As a result, a couple of these storms became severe along and near this residual outflow boundary, which downed trees in Desoto and Natchitoches Parishes, and also produced large hail in Northwest Natchitoches Parish. These storms eventually weakened during the evening with the loss of heating and diminished instability. A large tree was blown down on Highway 487 near Johnnie Birdwell Road in the Ajax community.", "ts_dict_index": [14259, 14260, 14261]}
+{"event_id": 932015, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-01-25 07:48:00", "end_date_time": "2021-01-25 07:48:00", "narrative": "A narrow line of showers and thunderstorms developed during the pre-dawn hours of January 25th across Northcentral Texas, along and just ahead of a cold front and associated upper trough that progressed east across the Central and Southern Plains. A strong southwesterly low level jet helped to organize these storms into a line along the front, with steep mid level instability helping to enhance large scale ascent to fuel strong thunderstorms along the line, which produced consistent 40-45 mph wind gusts. However, an isolated severe thunderstorm did develop within this line over Western Red River County Texas, which lifted northeast into Southern McCurtain County Oklahoma, where it blew the roof off of a porch at a home just east of Idabel shortly after daybreak. These storms weakened as they pushed into adjacent sections of Southwest Arkansas. A roof was ripped off of a porch at a home on Opal Valley Road east of Idabel.", "ts_dict_index": [14223, 14224, 14225]}
+{"event_id": 956587, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 17:41:00", "end_date_time": "2021-06-21 17:41:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A tree was downed on Limestone Rd. Time estimated from radar.", "ts_dict_index": [14292, 14293, 14294]}
+{"event_id": 956572, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-06-21 17:26:00", "end_date_time": "2021-06-21 17:26:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. Trees and wires were downed near Hawk Mountain Rd. Time estimated from radar.", "ts_dict_index": [14301, 14302, 14303]}
+{"event_id": 956571, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-06-21 17:46:00", "end_date_time": "2021-06-21 17:46:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. Several reports of downed power lines in the area. Time estimated from radar.", "ts_dict_index": [14304, 14305, 14306]}
+{"event_id": 956542, "event_type": "Thunderstorm Wind", "state": "NEW JERSEY", "cz_name": "CAMDEN", "begin_date_time": "2021-06-21 18:50:00", "end_date_time": "2021-06-21 18:50:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A personal weather station measured a 61 kt with gust. The actual value of the gust is estimated to be slightly lower. Time estimated.", "ts_dict_index": [14298, 14299, 14300]}
+{"event_id": 956583, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 17:54:00", "end_date_time": "2021-06-21 17:54:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A tree was downed on Newark Rd. Time estimated from radar.", "ts_dict_index": [14286, 14287, 14288]}
+{"event_id": 956588, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 17:58:00", "end_date_time": "2021-06-21 17:58:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. Trees were downed on Creek Rd. Time estimated from radar.", "ts_dict_index": [14295, 14296, 14297]}
+{"event_id": 956585, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 18:13:00", "end_date_time": "2021-06-21 18:13:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A tree was downed on Goshen Rd. Time estimated from radar.", "ts_dict_index": [14289, 14290, 14291]}
+{"event_id": 956561, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-06-21 18:30:00", "end_date_time": "2021-06-21 18:30:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A tree and wires were reported down. Time estimated from radar.", "ts_dict_index": [14307, 14308, 14309]}
+{"event_id": 956575, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2021-06-21 18:05:00", "end_date_time": "2021-06-21 18:05:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. Trees and wires were downed near Kegerise Dr. Time estimated from radar.", "ts_dict_index": [14277, 14278, 14279]}
+{"event_id": 1062554, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2022-11-05 11:15:00", "end_date_time": "2022-11-05 11:15:00", "narrative": "A strong cold front moved across northern Illinois during the late morning and early afternoon of November 5th with convective showers which produced thunderstorm wind damage and one tornado.  Wind damage from the convection was described as countywide across Ogle, Boone and McHenry Counties.  DuPage Airport measured a peak wind gust to 77 mph.  A handheld anemometer measured a wind gust to 80 mph near Roselle.||High winds caused tree damage both in the early morning of November 5th and then again in the afternoon of November 5th.  A large portion of a roof was blown off an apartment building in Elk Grove Village.  Some trees fell onto vehicles in Chicago.  Peak wind gusts included 62 mph at DuPage Airport; 61 mph at Aurora Municipal Airport; 59 mph at Chicago Midway and Chicago Executive Airports and 58 mph at Waukegan Airport. Several tree limbs 4 to 6 inches in diameter were blown down in the 2600 block of West Wilson Avenue.", "ts_dict_index": [14322, 14323, 14324]}
+{"event_id": 1062540, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2022-11-05 10:50:00", "end_date_time": "2022-11-05 10:50:00", "narrative": "A strong cold front moved across northern Illinois during the late morning and early afternoon of November 5th with convective showers which produced thunderstorm wind damage and one tornado.  Wind damage from the convection was described as countywide across Ogle, Boone and McHenry Counties.  DuPage Airport measured a peak wind gust to 77 mph.  A handheld anemometer measured a wind gust to 80 mph near Roselle.||High winds caused tree damage both in the early morning of November 5th and then again in the afternoon of November 5th.  A large portion of a roof was blown off an apartment building in Elk Grove Village.  Some trees fell onto vehicles in Chicago.  Peak wind gusts included 62 mph at DuPage Airport; 61 mph at Aurora Municipal Airport; 59 mph at Chicago Midway and Chicago Executive Airports and 58 mph at Waukegan Airport. A wind gust to 80 mph was measured with a handheld anemometer near Roselle.", "ts_dict_index": [14316, 14317, 14318]}
+{"event_id": 1062557, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2022-11-05 11:15:00", "end_date_time": "2022-11-05 11:15:00", "narrative": "A strong cold front moved across northern Illinois during the late morning and early afternoon of November 5th with convective showers which produced thunderstorm wind damage and one tornado.  Wind damage from the convection was described as countywide across Ogle, Boone and McHenry Counties.  DuPage Airport measured a peak wind gust to 77 mph.  A handheld anemometer measured a wind gust to 80 mph near Roselle.||High winds caused tree damage both in the early morning of November 5th and then again in the afternoon of November 5th.  A large portion of a roof was blown off an apartment building in Elk Grove Village.  Some trees fell onto vehicles in Chicago.  Peak wind gusts included 62 mph at DuPage Airport; 61 mph at Aurora Municipal Airport; 59 mph at Chicago Midway and Chicago Executive Airports and 58 mph at Waukegan Airport. A three foot diameter tree was blown down in the 1500 block of West Wilson Avenue.", "ts_dict_index": [14331, 14332, 14333]}
+{"event_id": 1062541, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2022-11-05 10:59:00", "end_date_time": "2022-11-05 10:59:00", "narrative": "A strong cold front moved across northern Illinois during the late morning and early afternoon of November 5th with convective showers which produced thunderstorm wind damage and one tornado.  Wind damage from the convection was described as countywide across Ogle, Boone and McHenry Counties.  DuPage Airport measured a peak wind gust to 77 mph.  A handheld anemometer measured a wind gust to 80 mph near Roselle.||High winds caused tree damage both in the early morning of November 5th and then again in the afternoon of November 5th.  A large portion of a roof was blown off an apartment building in Elk Grove Village.  Some trees fell onto vehicles in Chicago.  Peak wind gusts included 62 mph at DuPage Airport; 61 mph at Aurora Municipal Airport; 59 mph at Chicago Midway and Chicago Executive Airports and 58 mph at Waukegan Airport. ", "ts_dict_index": [14319, 14320, 14321]}
+{"event_id": 1062551, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2022-11-05 11:20:00", "end_date_time": "2022-11-05 11:20:00", "narrative": "A strong cold front moved across northern Illinois during the late morning and early afternoon of November 5th with convective showers which produced thunderstorm wind damage and one tornado.  Wind damage from the convection was described as countywide across Ogle, Boone and McHenry Counties.  DuPage Airport measured a peak wind gust to 77 mph.  A handheld anemometer measured a wind gust to 80 mph near Roselle.||High winds caused tree damage both in the early morning of November 5th and then again in the afternoon of November 5th.  A large portion of a roof was blown off an apartment building in Elk Grove Village.  Some trees fell onto vehicles in Chicago.  Peak wind gusts included 62 mph at DuPage Airport; 61 mph at Aurora Municipal Airport; 59 mph at Chicago Midway and Chicago Executive Airports and 58 mph at Waukegan Airport. A wind gust to 60 mph was measured at the Montrose Harbor Light.", "ts_dict_index": [14328, 14329, 14330]}
+{"event_id": 956555, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 18:00:00", "end_date_time": "2021-06-21 18:00:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. Multiple reports of downed trees and wires in East Brandywine Twp. Time estimated from radar.", "ts_dict_index": [14325, 14326, 14327]}
+{"event_id": 1062558, "event_type": "Thunderstorm Wind", "state": "ILLINOIS", "cz_name": "COOK", "begin_date_time": "2022-11-05 11:16:00", "end_date_time": "2022-11-05 11:16:00", "narrative": "A strong cold front moved across northern Illinois during the late morning and early afternoon of November 5th with convective showers which produced thunderstorm wind damage and one tornado.  Wind damage from the convection was described as countywide across Ogle, Boone and McHenry Counties.  DuPage Airport measured a peak wind gust to 77 mph.  A handheld anemometer measured a wind gust to 80 mph near Roselle.||High winds caused tree damage both in the early morning of November 5th and then again in the afternoon of November 5th.  A large portion of a roof was blown off an apartment building in Elk Grove Village.  Some trees fell onto vehicles in Chicago.  Peak wind gusts included 62 mph at DuPage Airport; 61 mph at Aurora Municipal Airport; 59 mph at Chicago Midway and Chicago Executive Airports and 58 mph at Waukegan Airport. A tree two to three feet in diameter was blown down onto two cars in the 3700 block of Clifton Avenue.", "ts_dict_index": [14334, 14335, 14336]}
+{"event_id": 956554, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 17:54:00", "end_date_time": "2021-06-21 17:54:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A few reports of trees and wires down in New Garden Twp. Time estimated from radar.", "ts_dict_index": [14340, 14341, 14342]}
+{"event_id": 956563, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-06-21 18:45:00", "end_date_time": "2021-06-21 18:45:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A few reports of downed wires were received from in and near Allentown. Time estimated from radar.", "ts_dict_index": [14337, 14338, 14339]}
+{"event_id": 956565, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-06-21 18:45:00", "end_date_time": "2021-06-21 18:45:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. Trees and wires were downed near Grant St. Time estimated from radar.", "ts_dict_index": [14313, 14314, 14315]}
+{"event_id": 952540, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-05-20 19:15:00", "end_date_time": "2021-05-20 19:15:00", "narrative": "A deep longwave trough remained anchored over the Central and Southern Rockies on May 20th, with a deep southerly fetch of low level moisture continuing to maintain an ample moisture-rich environment over the Four State Region. Diurnal heating contributed to air mass destabilization during the afternoon, with disturbances aloft contributing to scattered shower and isolated thunderstorm development across the area. Low level shear increased during the afternoon, and helped foster the development of isolated severe thunderstorms across portions of East Texas and McCurtain County Oklahoma, with trees blown down in the community of Plunketville. Locally heavy rainfall also fell from these storms for several hours, contributing to flash flooding across McCurtain County as well. These storms eventually diminished during the late evening hours. Trees were downed on Welcome Home Road in the community of Plunketville. A tree also fell onto a home in this same area.", "ts_dict_index": [14256, 14257, 14258]}
+{"event_id": 1072946, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-01-18 12:41:00", "end_date_time": "2023-01-18 12:41:00", "narrative": "An upper level low moved into the Southern Plains during the evening of January 17th, before lifting northeast into the Central Plains during the daytime hours of the 18th. Warm, moist, and unstable air had spread north across East Texas, North Louisiana, and Southwest Arkansas during the 17th-18th, east of a surface low that ejected northeast from North Texas into Eastern Oklahoma. The instability was maximized with daytime heating across the extreme Eastern Texas, North Louisiana, and Southern Arkansas on the 18th, as large scale forcing ahead of the ejecting low increased across these areas from the mid-morning through the afternoon hours. This resulted in scattered to numerous strong to severe thunderstorms, with damaging winds downing trees across various locations before the storms weakened by the mid-afternoon hours. A tree was downed near the Southern Trace Country Club in extreme Southeast Shreveport.", "ts_dict_index": [14364, 14365, 14366]}
+{"event_id": 953802, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-06-07 14:07:00", "end_date_time": "2021-06-07 14:07:00", "narrative": "A complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of a shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms across North Louisiana, before they exited the region during the late afternoon. A large tree was blown down across power lines and a fence on South Brookwood Drive in the Southern Hills neighborhood of South Shreveport.", "ts_dict_index": [14361, 14362, 14363]}
+{"event_id": 953801, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-06-07 14:07:00", "end_date_time": "2021-06-07 14:07:00", "narrative": "A complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of a shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms across North Louisiana, before they exited the region during the late afternoon. Numerous large trees were downed on several homes on South Brookwood Drive in the Southern Hills neighborhood in South Shreveport, including an oak and an 80 foot pine tree.", "ts_dict_index": [14349, 14350, 14351]}
+{"event_id": 953804, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-06-07 14:07:00", "end_date_time": "2021-06-07 14:07:00", "narrative": "A complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of a shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms across North Louisiana, before they exited the region during the late afternoon. A large tree was blown down on two homes on Flournoy Lucas near Francais Drive.", "ts_dict_index": [14352, 14353, 14354]}
+{"event_id": 953806, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2021-06-07 14:22:00", "end_date_time": "2021-06-07 14:22:00", "narrative": "A complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of a shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms across North Louisiana, before they exited the region during the late afternoon. A tree was blown down in Sarepta.", "ts_dict_index": [14358, 14359, 14360]}
+{"event_id": 953807, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2021-06-07 14:43:00", "end_date_time": "2021-06-07 14:43:00", "narrative": "A complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of a shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms across North Louisiana, before they exited the region during the late afternoon. A tree was blown down in Minden.", "ts_dict_index": [14355, 14356, 14357]}
+{"event_id": 956569, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "LEHIGH", "begin_date_time": "2021-06-21 18:45:00", "end_date_time": "2021-06-21 18:45:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. Power lines were downed near Neffs Laurys Rd. Time estimated from radar.", "ts_dict_index": [14343, 14344, 14345]}
+{"event_id": 820378, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2019-06-21 21:30:00", "end_date_time": "2019-06-21 21:33:00", "narrative": "A long-lived complex of thunderstorms, originating across the central Plains and Midwest, moved through Kentucky late this afternoon and evening. A tight instability gradient kept the strongest portions of this line of storms confined to the Lake Cumberland region and southeast parts of Kentucky locally. ||The most significant damage occurred across portions of Pulaski and Wayne Counties, including over 4,000 power outages due to downed trees and powerlines. A fireworks tent and utility pole at the Cumberland Crossing Shopping Center in Monticello were blown down by severe wind gusts, while a few tin roofs were also blown down in and north of Monticello. This led to the declaration of a State of Emergency to assist with cleanup efforts. South of Somerset, a large oak tree was blown down onto a house, causing extensive damage. Dispatch reported that a tree was blown down on Danny Drive south of Burnside, while a large oak tree was blown down onto a house south of Somerset.", "ts_dict_index": [14346, 14347, 14348]}
+{"event_id": 956586, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "CHESTER", "begin_date_time": "2021-06-21 18:13:00", "end_date_time": "2021-06-21 18:13:00", "narrative": "A cold front moved through the Great Lakes region on June 21, while Tropical Storm Claudette passed offshore of New Jersey and the Delmarva region. Ahead of the cold front, a hot, humid, and unstable air mass developed in the mid-Atlantic. A pre-frontal trough then served as a focus for widespread convection across the Northeast and mid-Atlantic during the afternoon and evening hours. With the strong instability and good forcing, much of the convection became strong to severe, taking the form of both linear and semi-discrete activity. Damaging winds were by far the primary hazard with these storms, with numerous reports of downed trees and power lines across the region. Convection weakened as it approached the coast owing to loss of daytime heating, weakening shear, and large scale subsidence on the northwest flank of Claudette. A tree was downed on Valley Rd. Time estimated from radar.", "ts_dict_index": [14310, 14311, 14312]}
+{"event_id": 953805, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-06-07 14:07:00", "end_date_time": "2021-06-07 14:07:00", "narrative": "A complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of a shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms across North Louisiana, before they exited the region during the late afternoon. Numerous trees and power lines were blown down across Bossier Parish.", "ts_dict_index": [14379, 14380, 14381]}
+{"event_id": 953803, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-06-07 14:07:00", "end_date_time": "2021-06-07 14:07:00", "narrative": "A complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of a shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms across North Louisiana, before they exited the region during the late afternoon. A large tree fell across Kingston Road just north of Shady Lane, blocking the road in both directions.", "ts_dict_index": [14370, 14371, 14372]}
+{"event_id": 954695, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-06-07 14:07:00", "end_date_time": "2021-06-07 14:07:00", "narrative": "A complex of showers and thunderstorms developed during the early morning hours of June 7th across Northwest Texas, and shifted east-southeast across North Texas throughout the morning, ahead of a shortwave trough that ejected east beneath an upper low pressure system that had begun to lift north across Southeast Oklahoma and Western Arkansas. The air mass ahead of this complex of storms across the Ark-La-Tex warmed considerably throughout the day, resulting in moderately unstable conditions within a marginally sheared environment. Thus, the storms intensified as they entered East Texas and remained severe and they progressed east across Southern Arkansas and North Louisiana. Trees and power lines were downed throughout the path of these storms across North Louisiana, before they exited the region during the late afternoon. A large tree fell through a home at the corner of Crooked Creek Drive and Flournoy Lucas Road in South Shreveport.", "ts_dict_index": [14376, 14377, 14378]}
+{"event_id": 1072957, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2023-01-18 12:43:00", "end_date_time": "2023-01-18 12:43:00", "narrative": "An upper level low moved into the Southern Plains during the evening of January 17th, before lifting northeast into the Central Plains during the daytime hours of the 18th. Warm, moist, and unstable air had spread north across East Texas, North Louisiana, and Southwest Arkansas during the 17th-18th, east of a surface low that ejected northeast from North Texas into Eastern Oklahoma. The instability was maximized with daytime heating across the extreme Eastern Texas, North Louisiana, and Southern Arkansas on the 18th, as large scale forcing ahead of the ejecting low increased across these areas from the mid-morning through the afternoon hours. This resulted in scattered to numerous strong to severe thunderstorms, with damaging winds downing trees across various locations before the storms weakened by the mid-afternoon hours. Several trees were uprooted along Alfred and Oliver Roads just southeast of Haughton.", "ts_dict_index": [14367, 14368, 14369]}
+{"event_id": 1088132, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-03-31 16:40:00", "end_date_time": "2023-03-31 16:50:00", "narrative": "A very strong system developed on the morning of March 31st and tracked across the state of Iowa. This system pulled unseasonably warm and moist air into the Midwest, which combined with a very favorable wind profile to create a volatile environment for severe thunderstorms.  Discrete supercell thunderstorms occurred initially, but quickly transitioned into a QLCS mode. This system produced a historic tornado outbreak for the area, with a record 29 tornadoes on the day, including 13 rated EF-2, 1 rated EF-3, and 1 rated EF-4. This was the first EF-4 tornado in the NWS Quad Cities service area since 1995. 11 injuries were reported, with no known fatalities. In addition to the numerous tornadoes, there were many large hail and damaging wind reports. Maximum straight line thunderstorm winds were estimated at 80 to 90 mph. Pea sized hail also fell with the strong winds.", "ts_dict_index": [14388, 14389, 14390]}
+{"event_id": 1017157, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2022-05-20 13:00:00", "end_date_time": "2022-05-20 13:00:00", "narrative": "A remnant mesoscale convective vortex (MCV) moved through the mid-Atlantic on the afternoon of May 20. This feature formed in association with a strong convective complex over the southern Plains on May 18, and proceeded to track northeast across the eastern half of the US, producing multiple additional rounds of severe weather as it did so. This included over the mid-Atlantic on May 20. As the MCV moved into the region, a warm and moderately unstable air mass was present over the region. Shear and forcing associated with the MCV caused multiple rounds of thunderstorms to develop during the afternoon. Some storms became severe, with a mixed convective mode leading to instances of damaging winds, hail, and one brief tornado in New Jersey. As the MCV moved offshore, convection diminished during the evening hours. Severe large tree branches were downed. Time estimated from radar.", "ts_dict_index": [14418, 14419, 14420]}
+{"event_id": 1087365, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-03-31 16:20:00", "end_date_time": "2023-03-31 16:20:00", "narrative": "A very strong system developed on the morning of March 31st and tracked across the state of Iowa. This system pulled unseasonably warm and moist air into the Midwest, which combined with a very favorable wind profile to create a volatile environment for severe thunderstorms.  Discrete supercell thunderstorms occurred initially, but quickly transitioned into a QLCS mode. This system produced a historic tornado outbreak for the area, with a record 29 tornadoes on the day, including 13 rated EF-2, 1 rated EF-3, and 1 rated EF-4. This was the first EF-4 tornado in the NWS Quad Cities service area since 1995. 11 injuries were reported, with no known fatalities. In addition to the numerous tornadoes, there were many large hail and damaging wind reports. Maximum straight line thunderstorm winds were estimated at 80 to 90 mph. A trained spotter reported 6 inch diameter trees down at this location.", "ts_dict_index": [14391, 14392, 14393]}
+{"event_id": 1016858, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-05-18 22:05:00", "end_date_time": "2022-05-18 22:05:00", "narrative": "A surface low was situated over Iowa/Illinois/Missouri during the day of the 18th, with a  warm front extended eastward and across and just north of the Bluegrass State. SPC had placed much of our area in a marginal risk of severe weather early in the day, before upgrading to a slight category during a morning update. A secondary low also developed and moved into the state for the afternoon, creating a secondary warm front boundary - along which lift and all modes of severe weather were possible, with the best chances for wind and hail. There was enough low level sheer that an isolated tornado couldn't be ruled out. As a shortwave trough also approached eastern KY throughout the day, along with an MCS to our west, the atmosphere was primed for severe weather to occur across the southeastern portions of the CWA. Multiple trees were downed along Lakeview Ave near Quinton, Kentucky.", "ts_dict_index": [14412, 14413, 14414]}
+{"event_id": 881334, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-05-08 02:36:00", "end_date_time": "2020-05-08 02:36:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. These storms exited Southeast Oklahoma prior to daybreak on the 8th. A picture was posted to social media by a trained spotter of a large outdoor light post that was broken off and splintered at the baseball field at Valliant High School.", "ts_dict_index": [14397, 14398, 14399]}
+{"event_id": 1072961, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2023-01-18 13:02:00", "end_date_time": "2023-01-18 13:02:00", "narrative": "An upper level low moved into the Southern Plains during the evening of January 17th, before lifting northeast into the Central Plains during the daytime hours of the 18th. Warm, moist, and unstable air had spread north across East Texas, North Louisiana, and Southwest Arkansas during the 17th-18th, east of a surface low that ejected northeast from North Texas into Eastern Oklahoma. The instability was maximized with daytime heating across the extreme Eastern Texas, North Louisiana, and Southern Arkansas on the 18th, as large scale forcing ahead of the ejecting low increased across these areas from the mid-morning through the afternoon hours. This resulted in scattered to numerous strong to severe thunderstorms, with damaging winds downing trees across various locations before the storms weakened by the mid-afternoon hours. A tree was blown down onto Carter Road south of Doyline.", "ts_dict_index": [14373, 14374, 14375]}
+{"event_id": 881338, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-05-08 03:05:00", "end_date_time": "2020-05-08 03:05:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. These storms exited Southeast Oklahoma prior to daybreak on the 8th. A pole was snapped in half with a power line down on Highway 3 east of Pipe Springs Road. A tree was also blown down on Living Land Road between Idabel and Haworth.", "ts_dict_index": [14394, 14395, 14396]}
+{"event_id": 881337, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-05-08 02:50:00", "end_date_time": "2020-05-08 02:50:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. These storms exited Southeast Oklahoma prior to daybreak on the 8th. Trees were blown down in the Lukfata community northwest of Broken Bow, as well as in the Golden community.", "ts_dict_index": [14403, 14404, 14405]}
+{"event_id": 881335, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-05-08 02:51:00", "end_date_time": "2020-05-08 02:51:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. These storms exited Southeast Oklahoma prior to daybreak on the 8th. Trees were blown down just south of Idabel.", "ts_dict_index": [14400, 14401, 14402]}
+{"event_id": 881333, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-05-08 02:36:00", "end_date_time": "2020-05-08 02:36:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. These storms exited Southeast Oklahoma prior to daybreak on the 8th. Trees were downed in Valliant.", "ts_dict_index": [14409, 14410, 14411]}
+{"event_id": 1016846, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-05-18 19:42:00", "end_date_time": "2022-05-18 19:42:00", "narrative": "A surface low was situated over Iowa/Illinois/Missouri during the day of the 18th, with a  warm front extended eastward and across and just north of the Bluegrass State. SPC had placed much of our area in a marginal risk of severe weather early in the day, before upgrading to a slight category during a morning update. A secondary low also developed and moved into the state for the afternoon, creating a secondary warm front boundary - along which lift and all modes of severe weather were possible, with the best chances for wind and hail. There was enough low level sheer that an isolated tornado couldn't be ruled out. As a shortwave trough also approached eastern KY throughout the day, along with an MCS to our west, the atmosphere was primed for severe weather to occur across the southeastern portions of the CWA. A tree was reported down on Stanford Street in Science Hill, Kentucky.", "ts_dict_index": [14421, 14422, 14423]}
+{"event_id": 881336, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-05-08 02:56:00", "end_date_time": "2020-05-08 02:56:00", "narrative": "A shortwave trough diving southeast across Eastern Oklahoma and Western Arkansas in the northwest flow aloft during the evening through the early morning hours of May 7th-8th, enhanced large scale forcing ahead of an attendant cold front, resulting in a complex of showers and thunderstorms to develop near and ahead of the front. This mesoscale convective system, or MCS, quickly shifted southeast into Southeast Oklahoma, Southwest Arkansas, Northeast Texas, and North Louisiana during the early morning hours of May 8th, strengthening as it encountered greater instability and a strong southerly low level jet. This resulted in the development of severe thunderstorms containing damaging winds, triggering numerous reports of wind damage across these areas. These storms exited Southeast Oklahoma prior to daybreak on the 8th. Trees and power lines were downed from Broken Bow to the Red River. Numerous roadways were blocked by fallen trees and power lines.", "ts_dict_index": [14406, 14407, 14408]}
+{"event_id": 1017158, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2022-05-20 15:18:00", "end_date_time": "2022-05-20 15:18:00", "narrative": "A remnant mesoscale convective vortex (MCV) moved through the mid-Atlantic on the afternoon of May 20. This feature formed in association with a strong convective complex over the southern Plains on May 18, and proceeded to track northeast across the eastern half of the US, producing multiple additional rounds of severe weather as it did so. This included over the mid-Atlantic on May 20. As the MCV moved into the region, a warm and moderately unstable air mass was present over the region. Shear and forcing associated with the MCV caused multiple rounds of thunderstorms to develop during the afternoon. Some storms became severe, with a mixed convective mode leading to instances of damaging winds, hail, and one brief tornado in New Jersey. As the MCV moved offshore, convection diminished during the evening hours. A couple of trees reported down.", "ts_dict_index": [14415, 14416, 14417]}
+{"event_id": 952839, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-05-28 01:45:00", "end_date_time": "2021-05-28 01:45:00", "narrative": "An upper low dove southeast across the Central Plains during the early morning hours of May 28th, with the associated upper trough axis quickly shifting southeast into the Southern Plains, along an attendant cold front. A southerly low level jet quickly spread low level moisture north ahead of the front, while also enhancing convergence along the front to allow for a complex of showers and thunderstorms to develop over portions of Oklahoma and North Texas. These storms produced a strong cold pool resulting in very strong to occasionally severe winds across East Texas, which downed sporadic trees before re-intensifying as they entered Northwest Louisiana during the pre-dawn hours. As a result, additional trees and power lines were downed, with an isolated tornado also touching down in Minden (Webster Parish). A 59 mph wind gust was measured at the Shreveport Downtown Airport.", "ts_dict_index": [14454, 14455, 14456]}
+{"event_id": 1017154, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2022-05-20 14:03:00", "end_date_time": "2022-05-20 14:03:00", "narrative": "A remnant mesoscale convective vortex (MCV) moved through the mid-Atlantic on the afternoon of May 20. This feature formed in association with a strong convective complex over the southern Plains on May 18, and proceeded to track northeast across the eastern half of the US, producing multiple additional rounds of severe weather as it did so. This included over the mid-Atlantic on May 20. As the MCV moved into the region, a warm and moderately unstable air mass was present over the region. Shear and forcing associated with the MCV caused multiple rounds of thunderstorms to develop during the afternoon. Some storms became severe, with a mixed convective mode leading to instances of damaging winds, hail, and one brief tornado in New Jersey. As the MCV moved offshore, convection diminished during the evening hours. A damage report from near Oley via social media showed numerous trees down. Radar data indicates a strong downburst likely occurred in the area. Time estimated from radar.", "ts_dict_index": [14430, 14431, 14432]}
+{"event_id": 1017153, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "MONTGOMERY", "begin_date_time": "2022-05-20 14:00:00", "end_date_time": "2022-05-20 14:00:00", "narrative": "A remnant mesoscale convective vortex (MCV) moved through the mid-Atlantic on the afternoon of May 20. This feature formed in association with a strong convective complex over the southern Plains on May 18, and proceeded to track northeast across the eastern half of the US, producing multiple additional rounds of severe weather as it did so. This included over the mid-Atlantic on May 20. As the MCV moved into the region, a warm and moderately unstable air mass was present over the region. Shear and forcing associated with the MCV caused multiple rounds of thunderstorms to develop during the afternoon. Some storms became severe, with a mixed convective mode leading to instances of damaging winds, hail, and one brief tornado in New Jersey. As the MCV moved offshore, convection diminished during the evening hours. A large tree limbs estimated at over 8 inches in diameter took down power lines along the southbound side of Allentown Rd near Green Hill Rd and Rising Sun Rd. Time estimated from radar.", "ts_dict_index": [14433, 14434, 14435]}
+{"event_id": 952842, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-05-28 01:48:00", "end_date_time": "2021-05-28 01:48:00", "narrative": "An upper low dove southeast across the Central Plains during the early morning hours of May 28th, with the associated upper trough axis quickly shifting southeast into the Southern Plains, along an attendant cold front. A southerly low level jet quickly spread low level moisture north ahead of the front, while also enhancing convergence along the front to allow for a complex of showers and thunderstorms to develop over portions of Oklahoma and North Texas. These storms produced a strong cold pool resulting in very strong to occasionally severe winds across East Texas, which downed sporadic trees before re-intensifying as they entered Northwest Louisiana during the pre-dawn hours. As a result, additional trees and power lines were downed, with an isolated tornado also touching down in Minden (Webster Parish). A large tree was blown down onto power lines on West Canal Blvd near Sunset Circle in the Sunset Acres neighborhood. Several other trees were blown down across roads in the area as well.", "ts_dict_index": [14445, 14446, 14447]}
+{"event_id": 952841, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "WEBSTER", "begin_date_time": "2021-05-28 01:46:00", "end_date_time": "2021-05-28 01:46:00", "narrative": "An upper low dove southeast across the Central Plains during the early morning hours of May 28th, with the associated upper trough axis quickly shifting southeast into the Southern Plains, along an attendant cold front. A southerly low level jet quickly spread low level moisture north ahead of the front, while also enhancing convergence along the front to allow for a complex of showers and thunderstorms to develop over portions of Oklahoma and North Texas. These storms produced a strong cold pool resulting in very strong to occasionally severe winds across East Texas, which downed sporadic trees before re-intensifying as they entered Northwest Louisiana during the pre-dawn hours. As a result, additional trees and power lines were downed, with an isolated tornado also touching down in Minden (Webster Parish). Trees and power lines were downed across Highway 79 east of Highway 159 in Minden, forcing the closure of the road in both directions.", "ts_dict_index": [14451, 14452, 14453]}
+{"event_id": 952846, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2021-05-28 03:20:00", "end_date_time": "2021-05-28 03:20:00", "narrative": "An upper low dove southeast across the Central Plains during the early morning hours of May 28th, with the associated upper trough axis quickly shifting southeast into the Southern Plains, along an attendant cold front. A southerly low level jet quickly spread low level moisture north ahead of the front, while also enhancing convergence along the front to allow for a complex of showers and thunderstorms to develop over portions of Oklahoma and North Texas. These storms produced a strong cold pool resulting in very strong to occasionally severe winds across East Texas, which downed sporadic trees before re-intensifying as they entered Northwest Louisiana during the pre-dawn hours. As a result, additional trees and power lines were downed, with an isolated tornado also touching down in Minden (Webster Parish). Large pieces of a metal roof were ripped off of a mobile home.", "ts_dict_index": [14457, 14458, 14459]}
+{"event_id": 1016850, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-05-18 19:54:00", "end_date_time": "2022-05-18 19:54:00", "narrative": "A surface low was situated over Iowa/Illinois/Missouri during the day of the 18th, with a  warm front extended eastward and across and just north of the Bluegrass State. SPC had placed much of our area in a marginal risk of severe weather early in the day, before upgrading to a slight category during a morning update. A secondary low also developed and moved into the state for the afternoon, creating a secondary warm front boundary - along which lift and all modes of severe weather were possible, with the best chances for wind and hail. There was enough low level sheer that an isolated tornado couldn't be ruled out. As a shortwave trough also approached eastern KY throughout the day, along with an MCS to our west, the atmosphere was primed for severe weather to occur across the southeastern portions of the CWA. The Department of Highways reported a tree down on Puncheon Creek Rd. between Science Hill and Eubank, Kentucky.", "ts_dict_index": [14424, 14425, 14426]}
+{"event_id": 1102857, "event_type": "Thunderstorm Wind", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2023-07-16 12:48:00", "end_date_time": "2023-07-16 12:48:00", "narrative": "A mesoscale convective system (MCS) developed during the early morning hours of July 16th across North Texas, along a stationary front that extended from North Texas east to along the Southern Arkansas/North Louisiana border. Large scale forcing just ahead a weak upper level disturbance traversing atop upper ridging in place across Westcentral Texas maintained this complex of thunderstorms through the morning, with strong diurnal heating contributing to ample instability to intensify these thunderstorms as they entered East Texas, Southern Arkansas, and North Louisiana. Thus, this line of thunderstorms became severe, producing damaging winds which resulted in numerous reports of downed trees and power lines across East Texas  during the afternoon before they spread into Southern Arkansas and North Louisiana. Scattered trees and power lines were downed across mainly Northern and Eastern Harrison County.", "ts_dict_index": [14448, 14449, 14450]}
+{"event_id": 1016841, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-05-18 19:37:00", "end_date_time": "2022-05-18 19:37:00", "narrative": "A surface low was situated over Iowa/Illinois/Missouri during the day of the 18th, with a  warm front extended eastward and across and just north of the Bluegrass State. SPC had placed much of our area in a marginal risk of severe weather early in the day, before upgrading to a slight category during a morning update. A secondary low also developed and moved into the state for the afternoon, creating a secondary warm front boundary - along which lift and all modes of severe weather were possible, with the best chances for wind and hail. There was enough low level sheer that an isolated tornado couldn't be ruled out. As a shortwave trough also approached eastern KY throughout the day, along with an MCS to our west, the atmosphere was primed for severe weather to occur across the southeastern portions of the CWA. Several powerlines reported down near 461 Shopville Rd. in Shopville, Kentucky.", "ts_dict_index": [14439, 14440, 14441]}
+{"event_id": 1016847, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-05-18 19:44:00", "end_date_time": "2022-05-18 19:44:00", "narrative": "A surface low was situated over Iowa/Illinois/Missouri during the day of the 18th, with a  warm front extended eastward and across and just north of the Bluegrass State. SPC had placed much of our area in a marginal risk of severe weather early in the day, before upgrading to a slight category during a morning update. A secondary low also developed and moved into the state for the afternoon, creating a secondary warm front boundary - along which lift and all modes of severe weather were possible, with the best chances for wind and hail. There was enough low level sheer that an isolated tornado couldn't be ruled out. As a shortwave trough also approached eastern KY throughout the day, along with an MCS to our west, the atmosphere was primed for severe weather to occur across the southeastern portions of the CWA. The Department of Highways reported a tree down on East Todd Road near Pulaski, Kentucky.", "ts_dict_index": [14442, 14443, 14444]}
+{"event_id": 1016835, "event_type": "Thunderstorm Wind", "state": "KENTUCKY", "cz_name": "PULASKI", "begin_date_time": "2022-05-18 19:34:00", "end_date_time": "2022-05-18 19:34:00", "narrative": "A surface low was situated over Iowa/Illinois/Missouri during the day of the 18th, with a  warm front extended eastward and across and just north of the Bluegrass State. SPC had placed much of our area in a marginal risk of severe weather early in the day, before upgrading to a slight category during a morning update. A secondary low also developed and moved into the state for the afternoon, creating a secondary warm front boundary - along which lift and all modes of severe weather were possible, with the best chances for wind and hail. There was enough low level sheer that an isolated tornado couldn't be ruled out. As a shortwave trough also approached eastern KY throughout the day, along with an MCS to our west, the atmosphere was primed for severe weather to occur across the southeastern portions of the CWA. Powerlines were reported down in Science Hill, Kentucky.", "ts_dict_index": [14436, 14437, 14438]}
+{"event_id": 1087366, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "LINN", "begin_date_time": "2023-03-31 16:36:00", "end_date_time": "2023-03-31 16:36:00", "narrative": "A very strong system developed on the morning of March 31st and tracked across the state of Iowa. This system pulled unseasonably warm and moist air into the Midwest, which combined with a very favorable wind profile to create a volatile environment for severe thunderstorms.  Discrete supercell thunderstorms occurred initially, but quickly transitioned into a QLCS mode. This system produced a historic tornado outbreak for the area, with a record 29 tornadoes on the day, including 13 rated EF-2, 1 rated EF-3, and 1 rated EF-4. This was the first EF-4 tornado in the NWS Quad Cities service area since 1995. 11 injuries were reported, with no known fatalities. In addition to the numerous tornadoes, there were many large hail and damaging wind reports. Maximum straight line thunderstorm winds were estimated at 80 to 90 mph. A 60 knot gust measured by the ASOS at the Cedar Rapids Airport.", "ts_dict_index": [14385, 14386, 14387]}
+{"event_id": 952844, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2021-05-28 02:52:00", "end_date_time": "2021-05-28 02:52:00", "narrative": "An upper low dove southeast across the Central Plains during the early morning hours of May 28th, with the associated upper trough axis quickly shifting southeast into the Southern Plains, along an attendant cold front. A southerly low level jet quickly spread low level moisture north ahead of the front, while also enhancing convergence along the front to allow for a complex of showers and thunderstorms to develop over portions of Oklahoma and North Texas. These storms produced a strong cold pool resulting in very strong to occasionally severe winds across East Texas, which downed sporadic trees before re-intensifying as they entered Northwest Louisiana during the pre-dawn hours. As a result, additional trees and power lines were downed, with an isolated tornado also touching down in Minden (Webster Parish). A tree fell onto a vehicle severe miles east of Farmerville.", "ts_dict_index": [14463, 14464, 14465]}
+{"event_id": 952845, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "UNION", "begin_date_time": "2021-05-28 03:15:00", "end_date_time": "2021-05-28 03:15:00", "narrative": "An upper low dove southeast across the Central Plains during the early morning hours of May 28th, with the associated upper trough axis quickly shifting southeast into the Southern Plains, along an attendant cold front. A southerly low level jet quickly spread low level moisture north ahead of the front, while also enhancing convergence along the front to allow for a complex of showers and thunderstorms to develop over portions of Oklahoma and North Texas. These storms produced a strong cold pool resulting in very strong to occasionally severe winds across East Texas, which downed sporadic trees before re-intensifying as they entered Northwest Louisiana during the pre-dawn hours. As a result, additional trees and power lines were downed, with an isolated tornado also touching down in Minden (Webster Parish). A large oak tree was blown down onto Highway 143.", "ts_dict_index": [14460, 14461, 14462]}
+{"event_id": 952847, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2021-05-28 01:45:00", "end_date_time": "2021-05-28 01:45:00", "narrative": "An upper low dove southeast across the Central Plains during the early morning hours of May 28th, with the associated upper trough axis quickly shifting southeast into the Southern Plains, along an attendant cold front. A southerly low level jet quickly spread low level moisture north ahead of the front, while also enhancing convergence along the front to allow for a complex of showers and thunderstorms to develop over portions of Oklahoma and North Texas. These storms produced a strong cold pool resulting in very strong to occasionally severe winds across East Texas, which downed sporadic trees before re-intensifying as they entered Northwest Louisiana during the pre-dawn hours. As a result, additional trees and power lines were downed, with an isolated tornado also touching down in Minden (Webster Parish). A concentrated but significant area of wind damage occurred from along and just east of Benton Road in Bossier City near Riverwood Drive, which continued to just south of East Texas Street just west of Pierre Bossier Mall. Across this area, there were various levels of mainly roof damage to apartments, outbuildings, and metal building systems, including a fast food restaurant on East Texas Street. A 2 year old girl suffered a head injury after a large tree limb crashed through a living room window of a home in the 2300 block of Broadway Drive off of Benton Road in Bossier City. Wind speeds in this straight line damage swath were generally estimated to be in the 70-80 mph range, although damage indicators did suggest some isolated peak speeds up to 90 mph just east of Benton Road.", "ts_dict_index": [14469, 14470, 14471]}
+{"event_id": 952843, "event_type": "Thunderstorm Wind", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-05-28 01:49:00", "end_date_time": "2021-05-28 01:49:00", "narrative": "An upper low dove southeast across the Central Plains during the early morning hours of May 28th, with the associated upper trough axis quickly shifting southeast into the Southern Plains, along an attendant cold front. A southerly low level jet quickly spread low level moisture north ahead of the front, while also enhancing convergence along the front to allow for a complex of showers and thunderstorms to develop over portions of Oklahoma and North Texas. These storms produced a strong cold pool resulting in very strong to occasionally severe winds across East Texas, which downed sporadic trees before re-intensifying as they entered Northwest Louisiana during the pre-dawn hours. As a result, additional trees and power lines were downed, with an isolated tornado also touching down in Minden (Webster Parish). A couple of trees were downed onto power lines in the Anderson Island area of Shreveport. One of the trees also fell onto a nearby home. No injuries were reported.", "ts_dict_index": [14466, 14467, 14468]}
+{"event_id": 991392, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "HAMILTON", "begin_date_time": "2021-12-15 14:26:00", "end_date_time": "2021-12-15 14:34:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. This tornado touched down in northeast Hamilton County near Kronborg and moved northeast into southwest Polk County. This tornado was one of the more classic-looking tornadoes of the day, based on photos reviewed. The estimated maximum wind speed of 100 MPH was based primarily upon snapped power poles, but a hog facility was also heavily damages about 2 miles into the path of this tornado. The tornado crossed Highway 66 about two miles west of Polk. Just before it lifted north of Polk, the tornado took down a large metal building.", "ts_dict_index": [14496, 14497, 14498]}
+{"event_id": 1112859, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-17 23:32:00", "end_date_time": "2023-06-17 23:32:00", "narrative": "Areas of deep convection began to develop late in the afternoon and through the evening of June 17th across Southeast Oklahoma into the Ark-La-Tex region. A stationary front was draped from west-northwest to east-southeast through the region, with temperatures generally in the mid to upper 90s and dew points around 80 degrees. These conditions contributed to extreme instability with around 5500-6000 J/kg. As a result, very vigorous updraft development occurred over the next several hours, eventually maturing into some supercell structures given 45-55 knots of bulk shear. The threat for damaging wind gusts quickly materialized with several reports of damaging wind gusts across McCurtain County in Southeast Oklahoma prior to midnight, resulting in one fatality from a fallen tree at Beavers Bend State Park. A tree was downed onto an RV at Beavers Bend State Park, resulting in the fatality of a female occupant inside.", "ts_dict_index": [14493, 14494, 14495]}
+{"event_id": 1112857, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-17 23:21:00", "end_date_time": "2023-06-17 23:21:00", "narrative": "Areas of deep convection began to develop late in the afternoon and through the evening of June 17th across Southeast Oklahoma into the Ark-La-Tex region. A stationary front was draped from west-northwest to east-southeast through the region, with temperatures generally in the mid to upper 90s and dew points around 80 degrees. These conditions contributed to extreme instability with around 5500-6000 J/kg. As a result, very vigorous updraft development occurred over the next several hours, eventually maturing into some supercell structures given 45-55 knots of bulk shear. The threat for damaging wind gusts quickly materialized with several reports of damaging wind gusts across McCurtain County in Southeast Oklahoma prior to midnight, resulting in one fatality from a fallen tree at Beavers Bend State Park. Trees downed on Old 98 from Valliant to Wright City and on State Highway 98 north of Highway 70.", "ts_dict_index": [14484, 14485, 14486]}
+{"event_id": 1054440, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-08-20 20:30:00", "end_date_time": "2022-08-20 20:30:00", "narrative": "Isolated showers and thunderstorms initially began across parts of southern Gila County, along with eastern Maricopa County and northeast Pinal County, producing locally heavy rainfall leading to isolated flash flooding. By the late afternoon and early evening hours on the 20th, new thunderstorms initiated over the high terrain of northern Arizona. High instability (MUCAPE 2,000-2,500 J/kg) aided in maintaining strong to severe thunderstorms into the Phoenix area as thunderstorms pushed toward the south and into the lower deserts during the evening. DCAPE around 1,000-1,200 J/kg promoted strong to severe downbursts with the strongest thunderstorms. Meanwhile, PWATs around 1.7-1.9 aided in thunderstorms being heavy rainfall producers, leading to several reports of flash flooding. No injuries were reported. Images showed multiple snapped and uprooted trees in the Sun City Festival area. Some trees knocked down road signs and also fell onto walls and a pergola. No injuries were reported.", "ts_dict_index": [14475, 14476, 14477]}
+{"event_id": 1112856, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-17 23:20:00", "end_date_time": "2023-06-17 23:20:00", "narrative": "Areas of deep convection began to develop late in the afternoon and through the evening of June 17th across Southeast Oklahoma into the Ark-La-Tex region. A stationary front was draped from west-northwest to east-southeast through the region, with temperatures generally in the mid to upper 90s and dew points around 80 degrees. These conditions contributed to extreme instability with around 5500-6000 J/kg. As a result, very vigorous updraft development occurred over the next several hours, eventually maturing into some supercell structures given 45-55 knots of bulk shear. The threat for damaging wind gusts quickly materialized with several reports of damaging wind gusts across McCurtain County in Southeast Oklahoma prior to midnight, resulting in one fatality from a fallen tree at Beavers Bend State Park. Several RVs at Pine Creek Lake were flipped over by severe thunderstorm wind gusts.", "ts_dict_index": [14481, 14482, 14483]}
+{"event_id": 1054445, "event_type": "Thunderstorm Wind", "state": "ARIZONA", "cz_name": "MARICOPA", "begin_date_time": "2022-08-20 20:45:00", "end_date_time": "2022-08-20 20:45:00", "narrative": "Isolated showers and thunderstorms initially began across parts of southern Gila County, along with eastern Maricopa County and northeast Pinal County, producing locally heavy rainfall leading to isolated flash flooding. By the late afternoon and early evening hours on the 20th, new thunderstorms initiated over the high terrain of northern Arizona. High instability (MUCAPE 2,000-2,500 J/kg) aided in maintaining strong to severe thunderstorms into the Phoenix area as thunderstorms pushed toward the south and into the lower deserts during the evening. DCAPE around 1,000-1,200 J/kg promoted strong to severe downbursts with the strongest thunderstorms. Meanwhile, PWATs around 1.7-1.9 aided in thunderstorms being heavy rainfall producers, leading to several reports of flash flooding. No injuries were reported. A large tree was uprooted near 91st Avenue and Beardsley Road. No injuries were reported.", "ts_dict_index": [14478, 14479, 14480]}
+{"event_id": 1112860, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-17 23:45:00", "end_date_time": "2023-06-17 23:45:00", "narrative": "Areas of deep convection began to develop late in the afternoon and through the evening of June 17th across Southeast Oklahoma into the Ark-La-Tex region. A stationary front was draped from west-northwest to east-southeast through the region, with temperatures generally in the mid to upper 90s and dew points around 80 degrees. These conditions contributed to extreme instability with around 5500-6000 J/kg. As a result, very vigorous updraft development occurred over the next several hours, eventually maturing into some supercell structures given 45-55 knots of bulk shear. The threat for damaging wind gusts quickly materialized with several reports of damaging wind gusts across McCurtain County in Southeast Oklahoma prior to midnight, resulting in one fatality from a fallen tree at Beavers Bend State Park. A 61 mph wind gust was recorded at the Oklahoma Mesonet site in Idabel.", "ts_dict_index": [14490, 14491, 14492]}
+{"event_id": 954694, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2021-06-17 16:47:00", "end_date_time": "2021-06-17 16:47:00", "narrative": "A broad ridge of high pressure aloft was anchored from the Four Corners Region east into the Southern Plains on June 17th. Meanwhile, an upper level disturbance rounded the ridge and drifted southwest across Western Arkansas and Southeast Oklahoma during the afternoon, over an area where moderate instability developed once temperatures climbed into the lower and mid 90s. Given the higher terrain over this area, orographic ascent helped to increase large scale forcing beneath this disturbance such that isolated showers and thunderstorms developed during the mid and late afternoon, and became severe as they entered Northern McCurtain County Oklahoma. Reports of quarter size hail and damaging winds which downed trees were received from this storm as it spread west, before entering Southern Pushmataha County. A picture was posted to social media of a large hardwood tree that was snapped from its trunk near Battiest. Other trees were downed near Battiest as well.", "ts_dict_index": [14472, 14473, 14474]}
+{"event_id": 1017155, "event_type": "Thunderstorm Wind", "state": "PENNSYLVANIA", "cz_name": "BERKS", "begin_date_time": "2022-05-20 13:57:00", "end_date_time": "2022-05-20 13:57:00", "narrative": "A remnant mesoscale convective vortex (MCV) moved through the mid-Atlantic on the afternoon of May 20. This feature formed in association with a strong convective complex over the southern Plains on May 18, and proceeded to track northeast across the eastern half of the US, producing multiple additional rounds of severe weather as it did so. This included over the mid-Atlantic on May 20. As the MCV moved into the region, a warm and moderately unstable air mass was present over the region. Shear and forcing associated with the MCV caused multiple rounds of thunderstorms to develop during the afternoon. Some storms became severe, with a mixed convective mode leading to instances of damaging winds, hail, and one brief tornado in New Jersey. As the MCV moved offshore, convection diminished during the evening hours. Trees were downed on Link Rd in Fleetwood from a possible microburst. Ping pong ball size hail was also reported in the area. Time estimated from radar.", "ts_dict_index": [14427, 14428, 14429]}
+{"event_id": 1099407, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "HAMILTON", "begin_date_time": "2023-06-02 15:09:00", "end_date_time": "2023-06-02 15:13:00", "narrative": "For the vast majority of South Central Nebraska, this Friday simply featured varying amounts of much-needed rain from scattered-to-widespread showers and weak thunderstorms streaming across the area from south-southeast to north-northwest. However, one particular storm had other ideas during the mid-late afternoon, as it intensified and ended up spawning a few weaker tornadoes and localized, severe straight-line winds while tracking through the hearts of Hamilton and Merrick counties, causing some damage in rural areas but fortunately no human injuries. Although the finer details of the exact tornado touchdowns/locations proved a bit murky given that ground circulations were primarily intermittent/weak���along with a lack of reported damage (Hamilton County) and a lack of concrete photographic evidence of a tornado (Merrick County)���officially three tornadoes were declared (chronological order): 1) an EF-unknown with a nearly five-mile, south-to-north path from a few miles west of the Interstate 80 Aurora exit to just northwest of Aurora itself (no known damage)...2) a brief EF-unknown with a roughly one-mile, south-to-north track through fields near Highway 14 east of Marquette (no known damage)...3) an EF-0 with a four-mile, southeast-to-northwest path through rural areas four to eight miles northwest of Central City. This Merrick County EF-0 was the only one that produced confirmed damage, although some of it was likely also associated with an accompanying/nearby swath of straight line winds estimated up to around 80 MPH. Most notably, a large cattle feedlot four miles north-northwest of Central City sustained a variety of damage, including a portion of a large confinement building destroyed along with some outdoor pens and livestock shade structures. In addition, four head of cattle were reportedly injured, including two that had to be euthanized. Although this was the only known occurrence of concentrated structural damage, several irrigation pivots and a few trees were toppled, and an unoccupied tractor windshield was blown out. Turning to the Hamilton County tornado paths, there were no confirmed damage reports and the Emergency Manager characterized them as mainly broad/weak ground circulations (visually more resembling landspouts). That being said, the community of Aurora narrowly avoided a direct hit, as a KLKN-TV web cam captured a dusty circulation passing over Highway 34 on the extreme west side of town. ||Digging into the timing and meteorological background behind this rogue severe/tornadic storm, and starting from a forecast perspective, especially the tornadic aspect was largely an unanticipated surprise. All convection prior to this storm's development had been quite weak, and instability/shear parameters offered little hint of severe weather in the immediate area. The 20 UTC (3 p.m. CDT) Day 1 Convective Outlook from SPC called for only ���general thunder��� in the Hamilton/Merrick area, with the eastern fringes of a categorical Marginal Risk category (level 1 of 5) residing a good 100 miles off to the west. In the mid-upper levels, a large-scale (but weak/unprogressive) upper trough was positioned along a northwest-southeast axis over the western United States, while an upper ridge was centered over the Upper Great Lakes, and the net influence of these features placing South Central Nebraska under modest south-southeasterly flow aloft. At the surface, there was also an absence of noteworthy features, with fairly light south-southeast breezes supporting a seasonably-moist airmass with dewpoints into the low-60s (F). On the finer mesoscale level, there was likely at least a subtle boundary in the area prior to storm development...perhaps an outflow boundary kicked out from earlier/ongoing showers and weak storms, and perhaps also augmented by a differential-heating boundary (the latter evidenced by a modest surface temperature difference at 4 p.m. CDT between a rain-cooled 68 degrees at Hastings versus 81 at Aurora). No matter what ultimately caused this mesoscale accident to unfold, the storm made its presence known during its 1 hour, 45-minute lifespan, first gaining strength over the Clay/Hamilton County line around 3:45 p.m. CDT, crossing into Merrick County around 4:30 p.m. CDT, and rapidly weakening around 5:30 p.m. CDT while entering southwestern Nance County. Emergency management confirmed report of a tornado. Location was based on their information along with media/social media photos and videos showing the tornado developing near Interstate 80 and then moving passing just west of Aurora before dissipating. No damage was reported.", "ts_dict_index": [14502, 14503, 14504]}
+{"event_id": 1099403, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "HAMILTON", "begin_date_time": "2023-06-02 15:29:00", "end_date_time": "2023-06-02 15:31:00", "narrative": "For the vast majority of South Central Nebraska, this Friday simply featured varying amounts of much-needed rain from scattered-to-widespread showers and weak thunderstorms streaming across the area from south-southeast to north-northwest. However, one particular storm had other ideas during the mid-late afternoon, as it intensified and ended up spawning a few weaker tornadoes and localized, severe straight-line winds while tracking through the hearts of Hamilton and Merrick counties, causing some damage in rural areas but fortunately no human injuries. Although the finer details of the exact tornado touchdowns/locations proved a bit murky given that ground circulations were primarily intermittent/weak���along with a lack of reported damage (Hamilton County) and a lack of concrete photographic evidence of a tornado (Merrick County)���officially three tornadoes were declared (chronological order): 1) an EF-unknown with a nearly five-mile, south-to-north path from a few miles west of the Interstate 80 Aurora exit to just northwest of Aurora itself (no known damage)...2) a brief EF-unknown with a roughly one-mile, south-to-north track through fields near Highway 14 east of Marquette (no known damage)...3) an EF-0 with a four-mile, southeast-to-northwest path through rural areas four to eight miles northwest of Central City. This Merrick County EF-0 was the only one that produced confirmed damage, although some of it was likely also associated with an accompanying/nearby swath of straight line winds estimated up to around 80 MPH. Most notably, a large cattle feedlot four miles north-northwest of Central City sustained a variety of damage, including a portion of a large confinement building destroyed along with some outdoor pens and livestock shade structures. In addition, four head of cattle were reportedly injured, including two that had to be euthanized. Although this was the only known occurrence of concentrated structural damage, several irrigation pivots and a few trees were toppled, and an unoccupied tractor windshield was blown out. Turning to the Hamilton County tornado paths, there were no confirmed damage reports and the Emergency Manager characterized them as mainly broad/weak ground circulations (visually more resembling landspouts). That being said, the community of Aurora narrowly avoided a direct hit, as a KLKN-TV web cam captured a dusty circulation passing over Highway 34 on the extreme west side of town. ||Digging into the timing and meteorological background behind this rogue severe/tornadic storm, and starting from a forecast perspective, especially the tornadic aspect was largely an unanticipated surprise. All convection prior to this storm's development had been quite weak, and instability/shear parameters offered little hint of severe weather in the immediate area. The 20 UTC (3 p.m. CDT) Day 1 Convective Outlook from SPC called for only ���general thunder��� in the Hamilton/Merrick area, with the eastern fringes of a categorical Marginal Risk category (level 1 of 5) residing a good 100 miles off to the west. In the mid-upper levels, a large-scale (but weak/unprogressive) upper trough was positioned along a northwest-southeast axis over the western United States, while an upper ridge was centered over the Upper Great Lakes, and the net influence of these features placing South Central Nebraska under modest south-southeasterly flow aloft. At the surface, there was also an absence of noteworthy features, with fairly light south-southeast breezes supporting a seasonably-moist airmass with dewpoints into the low-60s (F). On the finer mesoscale level, there was likely at least a subtle boundary in the area prior to storm development...perhaps an outflow boundary kicked out from earlier/ongoing showers and weak storms, and perhaps also augmented by a differential-heating boundary (the latter evidenced by a modest surface temperature difference at 4 p.m. CDT between a rain-cooled 68 degrees at Hastings versus 81 at Aurora). No matter what ultimately caused this mesoscale accident to unfold, the storm made its presence known during its 1 hour, 45-minute lifespan, first gaining strength over the Clay/Hamilton County line around 3:45 p.m. CDT, crossing into Merrick County around 4:30 p.m. CDT, and rapidly weakening around 5:30 p.m. CDT while entering southwestern Nance County. Emergency Manager witnessed and followed this brief tornado, with location approximated based upon their information. No damage was reported.", "ts_dict_index": [14505, 14506, 14507]}
+{"event_id": 901999, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "HAMILTON", "begin_date_time": "2020-08-14 16:12:00", "end_date_time": "2020-08-14 16:16:00", "narrative": "Although it only impacted a small percentage of the 24-county South Central Nebraska area, the large and intense supercell storm that marched south-southwestward for over 90 miles through several eastern counties on this Friday afternoon/early evening was likely the local area's most noteworthy individual storm of the 2020 convective season. In addition to dropping three fairly brief EF-0 tornadoes in southeastern Hamilton and northeastern Clay counties, its main calling card was large hail, with several reports of golf ball to slightly larger than baseball size stones in Clay/Nuckolls counties, and smaller hail to around quarter size as far north as Osceola. Interestingly, damaging winds were not a major player, with no ground-truth gusts in excess of 50 MPH. Focusing on specific storm reports, and starting with the three EF-0 tornadoes, they all occurred between 5-6 p.m. CDT, touching down briefly along a roughly 15-mile long corridor from near Interstate 80 a few miles south of Hampton, down to the Saronville area. Per storm surveys, the first two tornadoes were each on the ground for roughly 2 miles. While the majority of minor damage was confined to crops and trees, a lean-to shed was destroyed and a pivot overturned. As for the hail, the largest reported was 3 diameter between Clay Center and Harvard, but towns including Sutton and Nelson endured stones to at least tennis ball size. Flooding was not much of an issue, as the storm was progressive enough to keep rainfall amounts largely under one inch. ||Breaking down the meteorological background and event timing, this was actually a fairly conditional severe weather setup for South Central Nebraska, with various pros and cons for/against robust activity. In the mid-upper levels, the local area resided a fair distance south of a vigorous shortwave trough swinging across the Dakotas towards northern MN, resulting in fairly limited forcing aloft. Also working against convection (especially widespread severe) was a plume of warm mid level temperatures, with 700 millibar values of 12-14C providing a healthy cap. On the other hand, low-level forcing was seasonably-strong, as a well-defined cold front slid southeastward into the area during the afternoon. Ahead of this boundary, a significantly-unstable airmass awaited, featuring temperatures in the upper 80s-low 90s F/dewpoints upper 60s-mid 70s F, yielding formidable mixed-layer CAPE around 4000 J/kg. This extreme instability, in the presence of sufficient deep-layer wind shear around 35 knots, clearly fostered a mesoscale environment capable of stout convection. As for what actually transpired, the main show was preceded by a broken line of non-severe, likely elevated storms that passed primarily through counties south of Interstate 80 and east of Highway 281 between 12:30-3:30 p.m. CDT. About the time this innocuous early afternoon activity was departing the local area to the southeast, a broken line of true, surface-based storms got going along the front in northeast Nebraska, with the southwestern-most cell building down into the far northeast corner of South Central Nebraska (eastern Nance/northeast Merrick/northern Polk counties) between 3-4 p.m. CDT. Within an hour thereafter, this tail end Charlie storm rapidly grew into a full-blown supercell over Polk/northern York counties, producing its first marginally-severe hail reports. During the following two hours (5-7 p.m. CDT), the storm anchored itself firmly to the surface front, with new updraft generation along its western edge promoting more of a southwestward propagation and causing it to grow larger in both intensity/size, becoming more of a supercell cluster. It was during this time that the brief tornadoes occurred along the storm's far western flank, likely driven by pronounced low-level vorticity stretching along the surface front. While the sporadic tornado touchdowns were brief, the storm continued to be a prolific hail-producer as it gradually exited the local area out of Nuckolls County into northern Kansas between 7-8 p.m. CDT, ending all South Central Nebraska convection for the night. Minor crop and tree damage occurred. Debris was found in nearby powerlines. An old lean-to shed was destroyed.", "ts_dict_index": [14511, 14512, 14513]}
+{"event_id": 991391, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "HAMILTON", "begin_date_time": "2021-12-15 14:11:00", "end_date_time": "2021-12-15 14:19:00", "narrative": "A historic onslaught of swift moving severe thunderstorms with embedded tornadoes, followed by several hours of severe gradient winds and areas of blowing dust/smoke (and even a touch of wind-whipped snow) unfolded within South Central Nebraska on this Wednesday afternoon-evening, with the local area serving as the initiation zone of what would not only end up being the most impactful convective event on record during the month of December for the state of Nebraska (far eclipsing Christmas Day 2016), but also for other nearby states including IA/MN. In fact, the nearly continuous swath of damaging winds that stretched from south central NE/north central KS northeastward into southeast MN/western WI was officially declared a serial derecho...the first December derecho on record in the United States. Including nine confirmed tornadoes in South Central Nebraska (and 19 others that occurred in eastern NE), there were 28 confirmed tornadoes within the state...a remarkable fact considering that prior to this day only five Nebraska tornadoes had occurred in December since 1950! Focusing exclusively on the local South Central NE area going forward, the nine tornadoes consisted of five rated EF-1 and four rated EF-0. There were also dozens of measured reports of damaging winds in the 60-80+ MPH range (both thunderstorm/non-thunderstorm), including a peak thunderstorm gust of 85 MPH at Central Nebraska Regional Airport in Grand Island and a peak non-thunderstorm gust of 77 MPH by an unofficial mesonet in southwestern Clay County. Fortunately, there were no reported injuries, despite countless instances of damage primarily to irrigation pivots, outbuildings, power lines/poles and trees. ||Breaking down event evolution/timing for the local area, first of all, even before convection flared up it was already an unusual/noteworthy December weather day given unseasonable warmth/humidity being pumped into the area on strong south winds. By late morning-early afternoon, southerly gusts were commonly 35-50 MPH as temperatures soared into the mid-60s to low-70s F (setting new Dec. 15th records in Grand Island/Hastings), accompanied by dewpoints surging at least briefly into the 50s F (mainly near/east of Highway 281). This set the stage for severe convection/tornadoes during the early-mid afternoon, as the squall line that eventually impacted all but a few far western local counties raced through South Central NE at an incredible average forward motion of 65-75 MPH. The squall line, which was still in its infant stages as it entered Harlan County out of Kansas shortly before 1 p.m., rapidly intensified/expanded in scope while reaching the Highway 281 corridor by 2 p.m., and then in the blink of an eye had all-but-exited the extreme eastern fringes of the local area (Highway 81 counties) by 3 p.m....wrapping up a brief-but-wild two hours of weather. As for the nine confirmed South Central NE tornadoes, they all occurred between 1:27-2:43 p.m. and had at-times-intermittent path lengths between 7-15 miles. The tornadoes concentrated within counties mainly situated between the Highway 92 and Highway 6 corridors, touching down as far west as eastern Kearney/Franklin counties and as far east-northeast as Hamilton/Polk counties. The circulations were firmly embedded within the aforementioned squall line, making these quasi linear convective system (QLCS) tornadoes with often-intermittent damage paths. As is typical of such tornadoes, there was little in the way of clear cut photographic/video evidence, with the main exception consisting of a more classic looking photo of an EF-1 near Marquette. Although specific details regarding each of the nine tornadoes can be found in their respective event narratives, the vast majority of damage occurred to irrigation pivots, power poles/lines and a handful of outbuildings/grain bins, including a few fairly large metal outbuildings that were partially or completely demolished within only a few miles of communities such as Hastings, Marquette and Polk. Fortunately, no homes suffered major damage, although a few sustained relatively minor roof/siding issues. And although there were no reported injuries, one family north of Hastings had a fairly close call as their sport utility vehicle had several windows blown out of it only about one minute after they arrived home and sought shelter. Although straight-line thunderstorm winds along the surging line took a publicity backseat to the tornadoes, there were dozens of reported measured/estimated gusts of at least 60-70 MPH, and a handful of measured gusts as high as 75-85 MPH, highlighted by 85 MPH at Central Nebraska Regional Airport (official) and unofficial mesonet gusts of 84 MPH near Shickley, 83 MPH near Davenport and 81 MPH near Oxford. As just a sampling of damage attributed to convective winds: a blown-over semi truck on Highway 6 near Hastings; an overturned pickup truck and trailer along I-80 near Grand Island; significant roof and siding damage to a brick building in downtown Giltner; a metal outbuilding largely destroyed near Fullerton; a carport lofted into power lines in Bruning. Lastly in the convective department, hail was a minimal issue for the vast majority of South Central Nebraska. However, stones up to golf ball size significantly damaged a home near Marquette, while slightly smaller, wind-driven hail up to quarter size was reported in the Grand Island and Hastings areas, including a report of considerable damage to siding, fences and shingles in the Lake Hastings area.||Turning to non-convective severe winds, for the majority of South Central Nebraska they peaked in intensity a few hours after the passage of the squall line (and also impacted those few far western counties that were spared by convection), ramping up initially from the southwest and eventually west-northwest behind a surging composite cold front/dryline. Generally speaking, roughly the southwestern half of the local area observed its strongest non-convective winds between 2-7 p.m., while the northeastern half of the area peaked more so 4-9 p.m. However, the entire area endured at least a few hours of sustained speeds commonly 30-45 MPH and sporadic gusts of 50-70 MPH, including official peak gusts of 73 MPH at Hastings and Ord airports, and unofficial peak mesonet gusts of 77 MPH near Glenvil, 76 MPH near Davenport and 75 MPH near Norman. Although these non-convective winds undoubtedly caused considerable minor damage and/or exacerbated damage already done by earlier convective winds, specific reports were actually quite limited. However, one unique highlight of these southwesterly-turning-westerly winds is that they shrouded much of the local area a under an eerie pall for a few hours during the mid-late afternoon...a combination of blowing dust (emanating off the western High Plains) and also smoke (from large wildfires in northern KS) that reduced visibility to under a mile in some spots. Fortunately, no wildfires were sparked within South Central NE itself, despite favorable conditions for large fire growth behind the dryline (especially in southwestern counties). The final severe-criteria gust of the evening (59 MPH) occurred in Nance County shortly after 7 p.m., and gusts eased down to only 30-40 MPH within most of South Central NE by 10 p.m.||The last weather element of this multi-faceted event (and ironically of least-overall impact for December) was snow, as far western/northwest portions of the local area observed roughly a one-hour period of wind-whipped snow between 3:30-5:30 p.m. as a weakening deformation zone on the backside of the system clipped parts of mainly Dawson, Sherman, Valley and far western Buffalo counties. Although total accumulations were mainly at-or-below one-half inch and there were no reports of significant travel impacts, the fact that this snow band prompted brief, greatly-reduced visibility reductions along Interstate 80 prompted the first-ever Snow Squall Warning issuance within South Central NE.||Examining the meteorology behind this event, this would have been considered a powerhouse setup for severe convection/high winds during the more typical spring season usually associated with this type of system, let alone in mid-December. In the mid-upper levels, not only was the parent, negatively-tilted shortwave trough notably intense as it slammed across the central United States, but it was also notably fast. At daybreak, its vorticity maximum was just passing by the Four Corners, but by mid-day it had already reached the NE/CO/KS border area and by sunset had advanced into far northeast NE. At the 500-millibar level, a stout jet streak of 100+ knots nosed into South Central NE from the south-southwest during the afternoon, while lower in the column a potent southerly low level jet (evident at 850 millibars) ramped up to 40-60 knots. At the surface, a vigorous low pressure center sliced across the heart of Nebraska from southwest-to-northeast during the afternoon, deepening to around 984 millibars along the way and driving a sharp dryline/cold frontal combo eastward through the area. As mentioned, surface dewpoints climbed into the 50s F across much of the area prior to convective initiation, fostering a corridor of mixed-layer CAPE up to 500-1000 J/kg. Although somewhat modest instability values by warmer-season standards, in this case it was more than enough to promote robust severe convection in the presence of extreme wind fields, with embedded QLCS tornadoes no surprise given 0-1 kilometer bulk shear around 40 knots and effective storm-relative helicity (SRH) around 200-300 m2/s2. In the wake of the squall line, the ensuing non-convective wind event corresponded to a zone of deep subsidence (likely associated with a sting jet) and a pronounced surface pressure gradient on the backside of the departing low, with a 16-millibar gradient noted across South Central NE at 6 p.m. (ranging from 988 mb at Columbus to 1004 mb at McCook).||Closing with some comments about official NWS forecasts leading up to this historic event, there was excellent awareness several days in advance regarding the likelihood of powerful non-convective winds both ahead of (southerlies) and behind (westerlies) the intense surface low pressure system. An area-wide High Wind Watch was issued early on the 13th (48-60 hours in advance) and was subsequently upgraded to a High Wind Warning early on the 14th. However, what was not as well anticipated (both at the local and national forecast level) was how great of a convective/tornado threat South Central NE would face, as the fast-tracking squall line ended up forming slightly earlier and several counties farther west than most model data suggested (especially 12+ hours out). As a result, there was a noticeable ramp-up of convective threat categories within South Central NE on Dec. 15th SPC Day 1 Outlooks, progressing from the initial 06Z outlook that barely brushed the far eastern fringes of the area with a Marginal Risk (level 1 of 5), to the 1630Z outlook that correctly shifted Slight (level 2) and Enhanced (level 3) categories westward into several counties along/east of Highway 281. This Hamilton County tornado touched down four miles southeast of Giltner and traveled northeast into Aurora. The estimated maximum wind gust of 100 MPH was based mainly upon snapped power poles. There were numerous irrigation pivots damaged along and near this path. The tornado crossed Interstate 80 approximately two miles west of the Aurora interchange. The tornado entered the southwest side of Aurora near the fairgrounds. Metal cladding was peeled from storage facilities nearby and there were several spots of tree damage. The tornado lifted around 12th and E Streets just south of the railroad tracks.", "ts_dict_index": [14499, 14500, 14501]}
+{"event_id": 913264, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "HAMILTON", "begin_date_time": "2020-08-14 16:34:00", "end_date_time": "2020-08-14 16:36:00", "narrative": "Although it only impacted a small percentage of the 24-county South Central Nebraska area, the large and intense supercell storm that marched south-southwestward for over 90 miles through several eastern counties on this Friday afternoon/early evening was likely the local area's most noteworthy individual storm of the 2020 convective season. In addition to dropping three fairly brief EF-0 tornadoes in southeastern Hamilton and northeastern Clay counties, its main calling card was large hail, with several reports of golf ball to slightly larger than baseball size stones in Clay/Nuckolls counties, and smaller hail to around quarter size as far north as Osceola. Interestingly, damaging winds were not a major player, with no ground-truth gusts in excess of 50 MPH. Focusing on specific storm reports, and starting with the three EF-0 tornadoes, they all occurred between 5-6 p.m. CDT, touching down briefly along a roughly 15-mile long corridor from near Interstate 80 a few miles south of Hampton, down to the Saronville area. Per storm surveys, the first two tornadoes were each on the ground for roughly 2 miles. While the majority of minor damage was confined to crops and trees, a lean-to shed was destroyed and a pivot overturned. As for the hail, the largest reported was 3 diameter between Clay Center and Harvard, but towns including Sutton and Nelson endured stones to at least tennis ball size. Flooding was not much of an issue, as the storm was progressive enough to keep rainfall amounts largely under one inch. ||Breaking down the meteorological background and event timing, this was actually a fairly conditional severe weather setup for South Central Nebraska, with various pros and cons for/against robust activity. In the mid-upper levels, the local area resided a fair distance south of a vigorous shortwave trough swinging across the Dakotas towards northern MN, resulting in fairly limited forcing aloft. Also working against convection (especially widespread severe) was a plume of warm mid level temperatures, with 700 millibar values of 12-14C providing a healthy cap. On the other hand, low-level forcing was seasonably-strong, as a well-defined cold front slid southeastward into the area during the afternoon. Ahead of this boundary, a significantly-unstable airmass awaited, featuring temperatures in the upper 80s-low 90s F/dewpoints upper 60s-mid 70s F, yielding formidable mixed-layer CAPE around 4000 J/kg. This extreme instability, in the presence of sufficient deep-layer wind shear around 35 knots, clearly fostered a mesoscale environment capable of stout convection. As for what actually transpired, the main show was preceded by a broken line of non-severe, likely elevated storms that passed primarily through counties south of Interstate 80 and east of Highway 281 between 12:30-3:30 p.m. CDT. About the time this innocuous early afternoon activity was departing the local area to the southeast, a broken line of true, surface-based storms got going along the front in northeast Nebraska, with the southwestern-most cell building down into the far northeast corner of South Central Nebraska (eastern Nance/northeast Merrick/northern Polk counties) between 3-4 p.m. CDT. Within an hour thereafter, this tail end Charlie storm rapidly grew into a full-blown supercell over Polk/northern York counties, producing its first marginally-severe hail reports. During the following two hours (5-7 p.m. CDT), the storm anchored itself firmly to the surface front, with new updraft generation along its western edge promoting more of a southwestward propagation and causing it to grow larger in both intensity/size, becoming more of a supercell cluster. It was during this time that the brief tornadoes occurred along the storm's far western flank, likely driven by pronounced low-level vorticity stretching along the surface front. While the sporadic tornado touchdowns were brief, the storm continued to be a prolific hail-producer as it gradually exited the local area out of Nuckolls County into northern Kansas between 7-8 p.m. CDT, ending all South Central Nebraska convection for the night. Crop damage and scouring occurred. The tornado started in Hamilton County and continued into Clay County.", "ts_dict_index": [14508, 14509, 14510]}
+{"event_id": 997125, "event_type": "Tornado", "state": "TENNESSEE", "cz_name": "OBION", "begin_date_time": "2021-12-10 20:43:00", "end_date_time": "2021-12-10 20:44:00", "narrative": "December 10, 2021, was unseasonably warm over the region. Temperatures broke several long-standing records. Memphis hit 80��F which broke a 103-year-old high-temperature record. ||A strong upper-level trough was approaching from the west, providing strong lift within the unseasonably warm and unstable air mass.  MLCAPE reached the 1500-2000 J/kg range by 6 PM. The wind field was impressive with plenty of vertical wind shear needed for organized thunderstorms. Effective 0-1 km storm-relative helicity values ranged from 300-400 m2/s2 with effective bulk shear values of 70 knots - more than sufficient to support discrete supercells in the warm sector ahead of the cold front.||The first supercell developed in central Arkansas and tracked into northeast Arkansas producing a few weak tornadoes initially before intensifying across eastern Craighead and Mississippi Counties and killing two people. The tornado eventually strengthened into an EF-4 while moving through the Missouri Bootheel, resulting in 2 direct and one indirect fatality in Pemiscot County. The tornado then tracked across the Mississippi River into northwest Tennessee, producing an additional 4 fatalities near Reelfoot Lake. This tornado lifted for a brief time in Obion County, reorganized, and then moved into Kentucky. All told, the mesocyclone tracked for over 300 miles and was producing tornadoes for over 250 miles. This storm was responsible for at least 9 fatalities and many injuries in the NWS Memphis CWA along with millions of dollars of damage. ||As the initial supercell was crossing the state line into Kentucky, a string of supercells was moving into eastern Arkansas. A few brief tornadoes produced minor damage near Cash in western Craighead County and in the Fisher area of western Poinsett County. As the dominant supercell moved into eastern Poinsett County, the mesocyclone quickly intensified and the storm produced an EF-2 tornado in Trumann with several injuries and widespread damage. ||A new supercell developed in Mississippi County causing straight-line wind damage initially. This supercell intensified as it crossed the Mississippi River and produced another long-track tornado starting in Dyer County,  Tennessee. This tornado tracked east-northeast across northwest Tennessee into Henry County, and eventually into Kentucky. This tornado was rated EF-3 and resulted in several injuries with Kenton and Dresden, Tennessee being the hardest hit. ||The convection eventually evolved into a QLCS as it moved east. A mesovortex developed south of I-40 near Jackson that resulted in 3 tornadoes across eastern Madison, Henderson, and Decatur Counties including an EF-2. Non-tornadic storms moved across the Memphis metropolitan area, producing straight-line wind damage as a mesovortex moved through the city. A fatality was reported in Shelby County after a large tree fell on a home in South Memphis. Later that night, an EF-1 tornado occurred in Prentiss County before the severe weather threat began to wind down around 6 AM on December 11, 2021. ||In total, there were 18 tornadoes across the NWS Memphis CWA.  Along with tornadoes, several incidents of wind damage and minor flash flooding also occurred. A brief tornado damaged trees along Highway 22 west of Union City. Peak winds were estimated at 70 mph.", "ts_dict_index": [14514, 14515, 14516]}
+{"event_id": 815854, "event_type": "Thunderstorm Wind", "state": "IOWA", "cz_name": "POLK", "begin_date_time": "2019-04-17 15:00:00", "end_date_time": "2019-04-17 15:00:00", "narrative": "A surface low pressure system developed in the southern Colorado front range area on April 16th and slid east northeast through Kansas, Nebraska, and into Iowa through the 17th of April. By mid afternoon on the 17th, the surface low was situated over north central Iowa/south central Minnesota and the accompanying surface low extending back south southwest through the state. In the warm sector, SBCAPE values were in the 1000-2000 J/kg range, effective bulk shear around 30 to 40 kts, nominal hail CAPE values in the 200 to 300 J/kg range, and nearly negligible DCAPE. Storms were driven by the cold front and were pulse storms in nature in most cases. Storms were predominantly sub-severe with gusty winds and small hail, though two instances of severe reports were seen in the form of a destroyed farm shed and quarter inch hail. Public reported a destroyed farm shed, via social media.", "ts_dict_index": [14382, 14383, 14384]}
+{"event_id": 993706, "event_type": "Tornado", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2021-12-15 18:01:00", "end_date_time": "2021-12-15 18:03:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado was discovered using high resolution satellite imagery.  The tornado started just east of the Brushy Creek State Preserve with a short path in rural Webster County before crossing into Hamilton County.  No damage was reported in Webster County, hence the EFU rating for this segment.", "ts_dict_index": [14550, 14551, 14552]}
+{"event_id": 993698, "event_type": "Tornado", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2021-12-15 17:55:00", "end_date_time": "2021-12-15 17:56:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado travelled through both Webster and Hamilton Counties.  This short section in Webster County produced no reportable damage but was observed via high resolution satellite imagery.   The tornado moved into Hamilton County south of Stratford.", "ts_dict_index": [14535, 14536, 14537]}
+{"event_id": 993683, "event_type": "Tornado", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2021-12-15 17:49:00", "end_date_time": "2021-12-15 17:52:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado moved into Webster County from Boone County.  It remained in rural areas of southeast Webster County producing tree and utility pole damage.  EF2 damage was incurred to the southeast of Dayton along State Highway 175 where 8 utility poles were snapped.  The tornado then moved into the Des Moines River  east of Dayton valley where it dissipated.", "ts_dict_index": [14544, 14545, 14546]}
+{"event_id": 993704, "event_type": "Tornado", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2021-12-15 18:00:00", "end_date_time": "2021-12-15 18:04:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado started on the east side of the Des Moines River valley southwest of Duncombe and moved quickly northeast.  The tornado snapped several power poles near the intersection of Taylor Avenue and 220th Street west of Duncombe. Another outbuilding was destroyed northwest of Duncombe near the intersection of 210th Street and the Canadian National Railway.  The tornado lifted not long afterwards.", "ts_dict_index": [14538, 14539, 14540]}
+{"event_id": 997124, "event_type": "Tornado", "state": "TENNESSEE", "cz_name": "OBION", "begin_date_time": "2021-12-10 20:39:00", "end_date_time": "2021-12-10 20:40:00", "narrative": "December 10, 2021, was unseasonably warm over the region. Temperatures broke several long-standing records. Memphis hit 80��F which broke a 103-year-old high-temperature record. ||A strong upper-level trough was approaching from the west, providing strong lift within the unseasonably warm and unstable air mass.  MLCAPE reached the 1500-2000 J/kg range by 6 PM. The wind field was impressive with plenty of vertical wind shear needed for organized thunderstorms. Effective 0-1 km storm-relative helicity values ranged from 300-400 m2/s2 with effective bulk shear values of 70 knots - more than sufficient to support discrete supercells in the warm sector ahead of the cold front.||The first supercell developed in central Arkansas and tracked into northeast Arkansas producing a few weak tornadoes initially before intensifying across eastern Craighead and Mississippi Counties and killing two people. The tornado eventually strengthened into an EF-4 while moving through the Missouri Bootheel, resulting in 2 direct and one indirect fatality in Pemiscot County. The tornado then tracked across the Mississippi River into northwest Tennessee, producing an additional 4 fatalities near Reelfoot Lake. This tornado lifted for a brief time in Obion County, reorganized, and then moved into Kentucky. All told, the mesocyclone tracked for over 300 miles and was producing tornadoes for over 250 miles. This storm was responsible for at least 9 fatalities and many injuries in the NWS Memphis CWA along with millions of dollars of damage. ||As the initial supercell was crossing the state line into Kentucky, a string of supercells was moving into eastern Arkansas. A few brief tornadoes produced minor damage near Cash in western Craighead County and in the Fisher area of western Poinsett County. As the dominant supercell moved into eastern Poinsett County, the mesocyclone quickly intensified and the storm produced an EF-2 tornado in Trumann with several injuries and widespread damage. ||A new supercell developed in Mississippi County causing straight-line wind damage initially. This supercell intensified as it crossed the Mississippi River and produced another long-track tornado starting in Dyer County,  Tennessee. This tornado tracked east-northeast across northwest Tennessee into Henry County, and eventually into Kentucky. This tornado was rated EF-3 and resulted in several injuries with Kenton and Dresden, Tennessee being the hardest hit. ||The convection eventually evolved into a QLCS as it moved east. A mesovortex developed south of I-40 near Jackson that resulted in 3 tornadoes across eastern Madison, Henderson, and Decatur Counties including an EF-2. Non-tornadic storms moved across the Memphis metropolitan area, producing straight-line wind damage as a mesovortex moved through the city. A fatality was reported in Shelby County after a large tree fell on a home in South Memphis. Later that night, an EF-1 tornado occurred in Prentiss County before the severe weather threat began to wind down around 6 AM on December 11, 2021. ||In total, there were 18 tornadoes across the NWS Memphis CWA.  Along with tornadoes, several incidents of wind damage and minor flash flooding also occurred. A brief tornado uprooted trees along Marvin Vaught Road northeast of Samburg. Peak winds were estimated at 90 mph.", "ts_dict_index": [14517, 14518, 14519]}
+{"event_id": 997135, "event_type": "Tornado", "state": "TENNESSEE", "cz_name": "OBION", "begin_date_time": "2021-12-10 20:30:00", "end_date_time": "2021-12-10 20:36:00", "narrative": "December 10, 2021, was unseasonably warm over the region. Temperatures broke several long-standing records. Memphis hit 80��F which broke a 103-year-old high-temperature record. ||A strong upper-level trough was approaching from the west, providing strong lift within the unseasonably warm and unstable air mass.  MLCAPE reached the 1500-2000 J/kg range by 6 PM. The wind field was impressive with plenty of vertical wind shear needed for organized thunderstorms. Effective 0-1 km storm-relative helicity values ranged from 300-400 m2/s2 with effective bulk shear values of 70 knots - more than sufficient to support discrete supercells in the warm sector ahead of the cold front.||The first supercell developed in central Arkansas and tracked into northeast Arkansas producing a few weak tornadoes initially before intensifying across eastern Craighead and Mississippi Counties and killing two people. The tornado eventually strengthened into an EF-4 while moving through the Missouri Bootheel, resulting in 2 direct and one indirect fatality in Pemiscot County. The tornado then tracked across the Mississippi River into northwest Tennessee, producing an additional 4 fatalities near Reelfoot Lake. This tornado lifted for a brief time in Obion County, reorganized, and then moved into Kentucky. All told, the mesocyclone tracked for over 300 miles and was producing tornadoes for over 250 miles. This storm was responsible for at least 9 fatalities and many injuries in the NWS Memphis CWA along with millions of dollars of damage. ||As the initial supercell was crossing the state line into Kentucky, a string of supercells was moving into eastern Arkansas. A few brief tornadoes produced minor damage near Cash in western Craighead County and in the Fisher area of western Poinsett County. As the dominant supercell moved into eastern Poinsett County, the mesocyclone quickly intensified and the storm produced an EF-2 tornado in Trumann with several injuries and widespread damage. ||A new supercell developed in Mississippi County causing straight-line wind damage initially. This supercell intensified as it crossed the Mississippi River and produced another long-track tornado starting in Dyer County,  Tennessee. This tornado tracked east-northeast across northwest Tennessee into Henry County, and eventually into Kentucky. This tornado was rated EF-3 and resulted in several injuries with Kenton and Dresden, Tennessee being the hardest hit. ||The convection eventually evolved into a QLCS as it moved east. A mesovortex developed south of I-40 near Jackson that resulted in 3 tornadoes across eastern Madison, Henderson, and Decatur Counties including an EF-2. Non-tornadic storms moved across the Memphis metropolitan area, producing straight-line wind damage as a mesovortex moved through the city. A fatality was reported in Shelby County after a large tree fell on a home in South Memphis. Later that night, an EF-1 tornado occurred in Prentiss County before the severe weather threat began to wind down around 6 AM on December 11, 2021. ||In total, there were 18 tornadoes across the NWS Memphis CWA.  Along with tornadoes, several incidents of wind damage and minor flash flooding also occurred. The tornado crossed from Lake County to Obion County. The tornado's width was shrinking as it approached Samburg, however, it was still strong enough to damage homes, businesses, and city buildings in Samburg. Many homes suffered partial roof loss, and several mobile homes were separated from their undercarriages. A recreational vehicle in a mobile home park along Lake Drive in Samburg was destroyed, resulting in one fatality. The tornado continued northeast from Samburg, damaging several homes along Old Samburg Road. The last observed damage was west of Treece Road. Peak winds in Obion County were estimated at 130 mph.", "ts_dict_index": [14523, 14524, 14525]}
+{"event_id": 997426, "event_type": "Tornado", "state": "TENNESSEE", "cz_name": "OBION", "begin_date_time": "2021-12-10 20:54:00", "end_date_time": "2021-12-10 20:56:00", "narrative": "December 10, 2021, was unseasonably warm over the region. Temperatures broke several long-standing records. Memphis hit 80��F which broke a 103-year-old high-temperature record. ||A strong upper-level trough was approaching from the west, providing strong lift within the unseasonably warm and unstable air mass.  MLCAPE reached the 1500-2000 J/kg range by 6 PM. The wind field was impressive with plenty of vertical wind shear needed for organized thunderstorms. Effective 0-1 km storm-relative helicity values ranged from 300-400 m2/s2 with effective bulk shear values of 70 knots - more than sufficient to support discrete supercells in the warm sector ahead of the cold front.||The first supercell developed in central Arkansas and tracked into northeast Arkansas producing a few weak tornadoes initially before intensifying across eastern Craighead and Mississippi Counties and killing two people. The tornado eventually strengthened into an EF-4 while moving through the Missouri Bootheel, resulting in 2 direct and one indirect fatality in Pemiscot County. The tornado then tracked across the Mississippi River into northwest Tennessee, producing an additional 4 fatalities near Reelfoot Lake. This tornado lifted for a brief time in Obion County, reorganized, and then moved into Kentucky. All told, the mesocyclone tracked for over 300 miles and was producing tornadoes for over 250 miles. This storm was responsible for at least 9 fatalities and many injuries in the NWS Memphis CWA along with millions of dollars of damage. ||As the initial supercell was crossing the state line into Kentucky, a string of supercells was moving into eastern Arkansas. A few brief tornadoes produced minor damage near Cash in western Craighead County and in the Fisher area of western Poinsett County. As the dominant supercell moved into eastern Poinsett County, the mesocyclone quickly intensified and the storm produced an EF-2 tornado in Trumann with several injuries and widespread damage. ||A new supercell developed in Mississippi County causing straight-line wind damage initially. This supercell intensified as it crossed the Mississippi River and produced another long-track tornado starting in Dyer County,  Tennessee. This tornado tracked east-northeast across northwest Tennessee into Henry County, and eventually into Kentucky. This tornado was rated EF-3 and resulted in several injuries with Kenton and Dresden, Tennessee being the hardest hit. ||The convection eventually evolved into a QLCS as it moved east. A mesovortex developed south of I-40 near Jackson that resulted in 3 tornadoes across eastern Madison, Henderson, and Decatur Counties including an EF-2. Non-tornadic storms moved across the Memphis metropolitan area, producing straight-line wind damage as a mesovortex moved through the city. A fatality was reported in Shelby County after a large tree fell on a home in South Memphis. Later that night, an EF-1 tornado occurred in Prentiss County before the severe weather threat began to wind down around 6 AM on December 11, 2021. ||In total, there were 18 tornadoes across the NWS Memphis CWA.  Along with tornadoes, several incidents of wind damage and minor flash flooding also occurred. The supercell that produced the long track EF-4 tornado from Craighead County, Arkansas into western Obion County, Tennessee reintensified and formed another tornado in northern Obion County near Woodland Mills. A home suffered roof damage on Woodland Mills Road and trees were uprooted north of Woodland Mills. The tornado then crossed into Fulton County and eventually intensified into an EF-4 as it approached Mayfield, Kentucky. Peak winds in Obion County were estimated at 75 mph.", "ts_dict_index": [14520, 14521, 14522]}
+{"event_id": 993680, "event_type": "Tornado", "state": "IOWA", "cz_name": "GREENE", "begin_date_time": "2021-12-15 17:39:00", "end_date_time": "2021-12-15 17:42:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado traveled through three counties and initially touched down in Greene county to the east northeast of Grand Junction.  This tornado remained in rural areas of Greene county with no damage reports received.  The tornado path was observed using high resolution satellite imagery as well.  The tornado moved into Boone County between 190th and 180th Streets.", "ts_dict_index": [14532, 14533, 14534]}
+{"event_id": 997126, "event_type": "Tornado", "state": "TENNESSEE", "cz_name": "OBION", "begin_date_time": "2021-12-10 20:41:00", "end_date_time": "2021-12-10 20:44:00", "narrative": "December 10, 2021, was unseasonably warm over the region. Temperatures broke several long-standing records. Memphis hit 80��F which broke a 103-year-old high-temperature record. ||A strong upper-level trough was approaching from the west, providing strong lift within the unseasonably warm and unstable air mass.  MLCAPE reached the 1500-2000 J/kg range by 6 PM. The wind field was impressive with plenty of vertical wind shear needed for organized thunderstorms. Effective 0-1 km storm-relative helicity values ranged from 300-400 m2/s2 with effective bulk shear values of 70 knots - more than sufficient to support discrete supercells in the warm sector ahead of the cold front.||The first supercell developed in central Arkansas and tracked into northeast Arkansas producing a few weak tornadoes initially before intensifying across eastern Craighead and Mississippi Counties and killing two people. The tornado eventually strengthened into an EF-4 while moving through the Missouri Bootheel, resulting in 2 direct and one indirect fatality in Pemiscot County. The tornado then tracked across the Mississippi River into northwest Tennessee, producing an additional 4 fatalities near Reelfoot Lake. This tornado lifted for a brief time in Obion County, reorganized, and then moved into Kentucky. All told, the mesocyclone tracked for over 300 miles and was producing tornadoes for over 250 miles. This storm was responsible for at least 9 fatalities and many injuries in the NWS Memphis CWA along with millions of dollars of damage. ||As the initial supercell was crossing the state line into Kentucky, a string of supercells was moving into eastern Arkansas. A few brief tornadoes produced minor damage near Cash in western Craighead County and in the Fisher area of western Poinsett County. As the dominant supercell moved into eastern Poinsett County, the mesocyclone quickly intensified and the storm produced an EF-2 tornado in Trumann with several injuries and widespread damage. ||A new supercell developed in Mississippi County causing straight-line wind damage initially. This supercell intensified as it crossed the Mississippi River and produced another long-track tornado starting in Dyer County,  Tennessee. This tornado tracked east-northeast across northwest Tennessee into Henry County, and eventually into Kentucky. This tornado was rated EF-3 and resulted in several injuries with Kenton and Dresden, Tennessee being the hardest hit. ||The convection eventually evolved into a QLCS as it moved east. A mesovortex developed south of I-40 near Jackson that resulted in 3 tornadoes across eastern Madison, Henderson, and Decatur Counties including an EF-2. Non-tornadic storms moved across the Memphis metropolitan area, producing straight-line wind damage as a mesovortex moved through the city. A fatality was reported in Shelby County after a large tree fell on a home in South Memphis. Later that night, an EF-1 tornado occurred in Prentiss County before the severe weather threat began to wind down around 6 AM on December 11, 2021. ||In total, there were 18 tornadoes across the NWS Memphis CWA.  Along with tornadoes, several incidents of wind damage and minor flash flooding also occurred. A tornado damaged trees and storage buildings along Shawtown Road. Peak winds were estimated at 80 mph.", "ts_dict_index": [14526, 14527, 14528]}
+{"event_id": 993711, "event_type": "Tornado", "state": "IOWA", "cz_name": "FRANKLIN", "begin_date_time": "2021-12-15 18:30:00", "end_date_time": "2021-12-15 18:34:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado continued into Franklin County from Wright County.  The tornado continued on a northeast track through the far northwest corner of Franklin County with no reports of damage, hence the EFU rating.  This tornado moved into Cerro Gordo County about a mile east of Meservey.", "ts_dict_index": [14541, 14542, 14543]}
+{"event_id": 1112858, "event_type": "Thunderstorm Wind", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-06-17 23:27:00", "end_date_time": "2023-06-17 23:27:00", "narrative": "Areas of deep convection began to develop late in the afternoon and through the evening of June 17th across Southeast Oklahoma into the Ark-La-Tex region. A stationary front was draped from west-northwest to east-southeast through the region, with temperatures generally in the mid to upper 90s and dew points around 80 degrees. These conditions contributed to extreme instability with around 5500-6000 J/kg. As a result, very vigorous updraft development occurred over the next several hours, eventually maturing into some supercell structures given 45-55 knots of bulk shear. The threat for damaging wind gusts quickly materialized with several reports of damaging wind gusts across McCurtain County in Southeast Oklahoma prior to midnight, resulting in one fatality from a fallen tree at Beavers Bend State Park. Numerous trees and power lines downed throughout McCurtain County.", "ts_dict_index": [14487, 14488, 14489]}
+{"event_id": 993690, "event_type": "Tornado", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2021-12-15 17:46:00", "end_date_time": "2021-12-15 17:57:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado moved into Webster County from Greene County.  The tornado entered the county southwest of Lanyon and passed just west of Harcourt continuing northeast before dissipating between Lehigh and Otho.   This tornado snapped several large utility poles on its path across the county along with destroying a few outbuildings.", "ts_dict_index": [14562, 14563, 14564]}
+{"event_id": 993694, "event_type": "Tornado", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2021-12-15 17:54:00", "end_date_time": "2021-12-15 17:55:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This portion of the path just clipped the far southeast corner of Webster county without producing any damage, hence the EFU rating.  The tornado moved from Boone County into Webster County, then from Webster County into Hamilton County.", "ts_dict_index": [14559, 14560, 14561]}
+{"event_id": 993617, "event_type": "Tornado", "state": "IOWA", "cz_name": "GREENE", "begin_date_time": "2021-12-15 17:27:00", "end_date_time": "2021-12-15 17:42:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. Tornado continued into Greene County from Guthrie County.  The path through Greene County was long but remained in rural portions of the county.  Damage to rural outbuildings occurred in southern Greene county with more intense damage south of Jefferson.  Utility poles were snapped along 280th Street near where N Avenue intersects the road.   The tornado then impacted a farmstead on the west side of Highway 4 destroying several outbuildings and producing minor damage to the home.  The tornado proceeded northeast crossing US Highway 30 east of Jefferson and then continued in rural areas before lifting north of Dana.", "ts_dict_index": [14571, 14572, 14573]}
+{"event_id": 993719, "event_type": "Tornado", "state": "IOWA", "cz_name": "FRANKLIN", "begin_date_time": "2021-12-15 18:28:00", "end_date_time": "2021-12-15 18:35:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado moved into Franklin County from Hardin County.  Much of the path through Franklin County was found using high resolution satellite imagery.  However, the emergency manager did supply some damage points on the northeast end of the track to the northeast of Bradford, Iowa.  The damage was to trees with tree trunks being snapped along several different roads.  The tornado lifted a few miles west southwest of Geneva.", "ts_dict_index": [14553, 14554, 14555]}
+{"event_id": 993721, "event_type": "Tornado", "state": "IOWA", "cz_name": "FRANKLIN", "begin_date_time": "2021-12-15 18:32:00", "end_date_time": "2021-12-15 18:43:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado continued into Franklin County from Hardin County.  This path was determined using high resolution satellite imagery.  There was damage to trees and some outbuildings as the tornado moved northeast.   The tornado lifted just south of Highway 3 near the Handorf Roadside Park.", "ts_dict_index": [14565, 14566, 14567]}
+{"event_id": 993619, "event_type": "Tornado", "state": "IOWA", "cz_name": "GREENE", "begin_date_time": "2021-12-15 17:29:00", "end_date_time": "2021-12-15 17:45:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. Tornado moved into Greene County from Guthrie County.  This tornado produced damage through rural south and east portions of the county.  The tornado passed just southeast of the hamlet of Cooper and through Grand Junction.  Most of the damage was EF0 to EF1 with tree and minor house damage.  However, the tornado strengthened north of Grand Junction with power pole damage and then toppling an industrial wind mill along W Avenue with an EF2 rating at that location.  The circulation then destroyed a confinement building before dissipating several miles northeast of Dana.", "ts_dict_index": [14574, 14575, 14576]}
+{"event_id": 993687, "event_type": "Tornado", "state": "IOWA", "cz_name": "GREENE", "begin_date_time": "2021-12-15 17:42:00", "end_date_time": "2021-12-15 17:46:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado moved through both Greene and Webster Counties.  The tornado developed southwest of Paton in Greene County and blew apart an old shed.  It continued to strengthen and snapped several large utility poles along 110th Street west of U Avenue.  The tornado then exited the county into Webster County north of Paton.", "ts_dict_index": [14556, 14557, 14558]}
+{"event_id": 993614, "event_type": "Tornado", "state": "IOWA", "cz_name": "GREENE", "begin_date_time": "2021-12-15 17:24:00", "end_date_time": "2021-12-15 17:28:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado moved from Guthrie into Greene County.  The tornado destroyed several grain bins shortly after entering the county and then snapped several large power poles along 330th Street between F and G Avenues.   The tornado continued northeast producing sporadic damage in rural southern Greene County before dissipating north of 300th Street between H and I Avenues.", "ts_dict_index": [14568, 14569, 14570]}
+{"event_id": 993621, "event_type": "Tornado", "state": "IOWA", "cz_name": "GREENE", "begin_date_time": "2021-12-15 17:29:00", "end_date_time": "2021-12-15 17:33:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado occurred southwest of Jefferson and remained in rural Greene County during its entire path.   The tornado damaged a confinement building and farther northeast destroyed an outbuilding.  However, the most intense damage was a series of high voltage utility dual pole towers which were snapped by the tornado.  At least 8 towers were snapped over J Avenue between 250th and 260th Streets.  Additional utility poles were snapped along 250th Street as well.   The tornado lifted in the vicinity of an apple orchard located southwest of Jefferson.", "ts_dict_index": [14577, 14578, 14579]}
+{"event_id": 993685, "event_type": "Tornado", "state": "IOWA", "cz_name": "WEBSTER", "begin_date_time": "2021-12-15 17:49:00", "end_date_time": "2021-12-15 17:54:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado continued into Webster County from Calhoun County.  This tornado entered the county near US Highway 20 and continued northeast through the east side of Barnum.  Most minor damage to houses occurred along with tree damage.  The tornado dissipated to the northeast of Barnum near Lizard Creek.", "ts_dict_index": [14547, 14548, 14549]}
+{"event_id": 877525, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "DE SOTO", "begin_date_time": "2020-04-12 08:57:00", "end_date_time": "2020-04-12 09:02:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. An EF-1 tornado with estimated maximum winds near 110 mph touched down near Red Lick Road, where it snapped large limbs and uprooted several hardwood and softwood trees. The tornado then weakened as it continued to snap limbs before crossing over the International Paper Mill. The tornado re-strengthened and widened to nearly 300 yards as it snapped and uprooted hundreds of trees before crossing Bayou Pierre into Northwest Red River Parish.", "ts_dict_index": [14601, 14602, 14603]}
+{"event_id": 877521, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-04-12 08:52:00", "end_date_time": "2020-04-12 08:53:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. An EF-1 tornado with estimated maximum winds near 105 mph touched down near Caddo Avenue south of 5th Street in the town of Benton. After initially touching down as an EF-0, this tornado strengthened as it crossed 5th Street between Sibley and Bossier Streets, before lifting east of Pine Street. Several buildings in town had roof damage, the feed store had its flat roof covering removed, and a single family home had a large porch dislodged with portions of its roof removed from the residence. The bay doors at Fire Station District 4 were also blown in.", "ts_dict_index": [14607, 14608, 14609]}
+{"event_id": 993726, "event_type": "Tornado", "state": "IOWA", "cz_name": "FRANKLIN", "begin_date_time": "2021-12-15 18:38:00", "end_date_time": "2021-12-15 18:43:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado produced EF1 damage on the east side of Sheffield nearly destroying a business outbuilding.  The track farther to the southwest was found in high resolution satellite imagery and also confirmed through a private weather station which recorded a wind gust to 108 mph as the tornado passed its location.", "ts_dict_index": [14589, 14590, 14591]}
+{"event_id": 993622, "event_type": "Tornado", "state": "IOWA", "cz_name": "GREENE", "begin_date_time": "2021-12-15 17:32:00", "end_date_time": "2021-12-15 17:36:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. Another QLCS tornado which began west southwest of Jefferson and ended to the northwest of town.  This tornado began in rural areas but toppled several large single pole utility poles along I Avenue south of 250th Street and moved northeast with tree and minor house damage on 240th Street near the intersection with K Avenue.   The tornado ended up crossing US Highway 30 about 1.5 miles west of the intersection with State Highway 4 and severely leaned high voltage poles along the highway.  The tornado dissipated not long afterwards near M Avenue north of Highway 30.", "ts_dict_index": [14580, 14581, 14582]}
+{"event_id": 877563, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "BIENVILLE", "begin_date_time": "2020-04-12 09:30:00", "end_date_time": "2020-04-12 09:31:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. An EF-1 tornado with estimated maximum winds near 105 mph briefly touched down just north of the Bienville/Natchitoches Parish line along Foster Arbor Road, and tracked northeast for nearly 2 miles, crossing Highway 153, New Ramah Road, Cloud Road, and Thompson Road. This tornado snapped and uprooted trees along its path, but a few structures did sustain minor roof damage from the wind, but not from falling branches or trees. The most considerable damage occurred as the tornado crossed Thompson Road, where numerous large pine trees had their trunks snapped. Radar data suggested the tornado likely continued on for another mile or two east of Thompson Road, but there was no access to those areas for the survey team to confirm.", "ts_dict_index": [14604, 14605, 14606]}
+{"event_id": 823484, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "DAWSON", "begin_date_time": "2019-05-17 18:15:00", "end_date_time": "2019-05-17 18:33:00", "narrative": "A long-lived supercell produced 3 weak tornadoes over Dawson county on this Friday evening. Around 2 PM CST, a north-northwest to south-southeast broken line of showers and thunderstorms developed from near Lexington to Alma and into north central Kansas. Between 2 and 430 PM CST, this line moved northeast across south central Nebraska. The strongest storms developed over Gosper and Dawson counties and moved north-northeast across Sherman and Valley counties. These storms produced some low-end severe hail (nickel to quarter size) over eastern Dawson and western Buffalo counties, and downburst winds were strong enough to knock a tree onto a lean-to south of Ord. Storms in the rest of the line rapidly weakened. Meanwhile, a lone supercell had formed over northwest Kansas. This storm moved north-northeast and crossed western Dawson county between 545 and 745 PM CST, producing three tornadoes. Two tornadoes had a maximum damage intensity of EF-1. These tornadoes were near Farnam and Cozad. The third tornado was an EF-0 west of Eddyville. The Cozad tornado was the longest with a 10-mile path. This supercell also produced severe hail from Farnam north to Gothenburg, the largest of which was the size of tennis balls in Farnam.||This was a much-anticipated day for storm chasers as the setup was classic. Deepening low pressure was over northeast Colorado, and by 6 PM CST, the pressure was down to 990 mb. This low was located along a stationary front that extended east-northeast across Nebraska. A dryline extended south from the low and a cold front was approaching from the west. The area was in the warm sector with the triple point over southwest Nebraska. As the evening progressed, the low and cold front moved into central Nebraska, with the front merging with the dryline. The flow aloft was moderately-amplified with a low over Utah, embedded within a longwave trough over the West, while a ridge was over the eastern United States. In the wake of the earlier showers and storms, within the inflow of the supercell, temperatures were in the middle 70s, with dewpoints in the middle 60s. With mid-level lapse rates 7.5-8.0 C/km, this resulted in MLCAPE around 3000 J/kg. Deep layer shear was around 40 kt. Low-level winds were strong and veered significantly with height, resulting in 0-1 km SRH between 250 and 300 m2/s2. The Supercell Composite Parameter was about 18 and the Significant Tornado Parameter was around 4. This tornado uprooted some trees, caused minor damage to some homes and completely destroyed at least one storage building. The tornado crossed Highway 23 east of Farnam, then Highway 47 northeast of Farnam before dissipating. The path became indiscernible as the storm approached rougher terrain and the road network was not viable for surveying. The estimated maximum wind speed was 100 MPH.", "ts_dict_index": [14598, 14599, 14600]}
+{"event_id": 823486, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "DAWSON", "begin_date_time": "2019-05-17 19:15:00", "end_date_time": "2019-05-17 19:17:00", "narrative": "A long-lived supercell produced 3 weak tornadoes over Dawson county on this Friday evening. Around 2 PM CST, a north-northwest to south-southeast broken line of showers and thunderstorms developed from near Lexington to Alma and into north central Kansas. Between 2 and 430 PM CST, this line moved northeast across south central Nebraska. The strongest storms developed over Gosper and Dawson counties and moved north-northeast across Sherman and Valley counties. These storms produced some low-end severe hail (nickel to quarter size) over eastern Dawson and western Buffalo counties, and downburst winds were strong enough to knock a tree onto a lean-to south of Ord. Storms in the rest of the line rapidly weakened. Meanwhile, a lone supercell had formed over northwest Kansas. This storm moved north-northeast and crossed western Dawson county between 545 and 745 PM CST, producing three tornadoes. Two tornadoes had a maximum damage intensity of EF-1. These tornadoes were near Farnam and Cozad. The third tornado was an EF-0 west of Eddyville. The Cozad tornado was the longest with a 10-mile path. This supercell also produced severe hail from Farnam north to Gothenburg, the largest of which was the size of tennis balls in Farnam.||This was a much-anticipated day for storm chasers as the setup was classic. Deepening low pressure was over northeast Colorado, and by 6 PM CST, the pressure was down to 990 mb. This low was located along a stationary front that extended east-northeast across Nebraska. A dryline extended south from the low and a cold front was approaching from the west. The area was in the warm sector with the triple point over southwest Nebraska. As the evening progressed, the low and cold front moved into central Nebraska, with the front merging with the dryline. The flow aloft was moderately-amplified with a low over Utah, embedded within a longwave trough over the West, while a ridge was over the eastern United States. In the wake of the earlier showers and storms, within the inflow of the supercell, temperatures were in the middle 70s, with dewpoints in the middle 60s. With mid-level lapse rates 7.5-8.0 C/km, this resulted in MLCAPE around 3000 J/kg. Deep layer shear was around 40 kt. Low-level winds were strong and veered significantly with height, resulting in 0-1 km SRH between 250 and 300 m2/s2. The Supercell Composite Parameter was about 18 and the Significant Tornado Parameter was around 4. This tornado touched down west of Eddyville, and was reported to be rain wrapped as it crossed Highway 21. The path, wind speed and other information were estimated from eyewitness reports and radar data, as there are few damage indicators in the area. The estimated maximum wind speed was 85 MPH.", "ts_dict_index": [14595, 14596, 14597]}
+{"event_id": 823485, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "DAWSON", "begin_date_time": "2019-05-17 18:54:00", "end_date_time": "2019-05-17 19:10:00", "narrative": "A long-lived supercell produced 3 weak tornadoes over Dawson county on this Friday evening. Around 2 PM CST, a north-northwest to south-southeast broken line of showers and thunderstorms developed from near Lexington to Alma and into north central Kansas. Between 2 and 430 PM CST, this line moved northeast across south central Nebraska. The strongest storms developed over Gosper and Dawson counties and moved north-northeast across Sherman and Valley counties. These storms produced some low-end severe hail (nickel to quarter size) over eastern Dawson and western Buffalo counties, and downburst winds were strong enough to knock a tree onto a lean-to south of Ord. Storms in the rest of the line rapidly weakened. Meanwhile, a lone supercell had formed over northwest Kansas. This storm moved north-northeast and crossed western Dawson county between 545 and 745 PM CST, producing three tornadoes. Two tornadoes had a maximum damage intensity of EF-1. These tornadoes were near Farnam and Cozad. The third tornado was an EF-0 west of Eddyville. The Cozad tornado was the longest with a 10-mile path. This supercell also produced severe hail from Farnam north to Gothenburg, the largest of which was the size of tennis balls in Farnam.||This was a much-anticipated day for storm chasers as the setup was classic. Deepening low pressure was over northeast Colorado, and by 6 PM CST, the pressure was down to 990 mb. This low was located along a stationary front that extended east-northeast across Nebraska. A dryline extended south from the low and a cold front was approaching from the west. The area was in the warm sector with the triple point over southwest Nebraska. As the evening progressed, the low and cold front moved into central Nebraska, with the front merging with the dryline. The flow aloft was moderately-amplified with a low over Utah, embedded within a longwave trough over the West, while a ridge was over the eastern United States. In the wake of the earlier showers and storms, within the inflow of the supercell, temperatures were in the middle 70s, with dewpoints in the middle 60s. With mid-level lapse rates 7.5-8.0 C/km, this resulted in MLCAPE around 3000 J/kg. Deep layer shear was around 40 kt. Low-level winds were strong and veered significantly with height, resulting in 0-1 km SRH between 250 and 300 m2/s2. The Supercell Composite Parameter was about 18 and the Significant Tornado Parameter was around 4. This tornado was witnessed by many as it formed on the east side of Cozad, where some tree damage and power poles were broken. The nearly 10-mile path weaved to the northeast across a rural landscape. One-half of a large farm machinery shed was complete destroyed and several irrigation pivots were upset, helping delineate the path. Grain bins were destroyed and tree damage was sporadic along the path. The tornado was reported to be rain-wrapped at times. The path become indiscernible as the tornado moved into the hills north of Cozad and the road network became more sparse. The estimated maximum wind speed was 100 MPH.", "ts_dict_index": [14592, 14593, 14594]}
+{"event_id": 993727, "event_type": "Tornado", "state": "IOWA", "cz_name": "FRANKLIN", "begin_date_time": "2021-12-15 18:40:00", "end_date_time": "2021-12-15 18:46:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This tornado began a few miles north of Geneva and moved northeast producing plenty of tree damage as well as extensive outbuilding damage on two farmsteads.  Additional damage to a home with missing roofing and siding occurred along 170th Street west of Yarrow Avenue.  The tornado continue producing tree and power pole damage to the northeast before lifting on the north side of 190th Street near the West Fork Wildlife Area.", "ts_dict_index": [14586, 14587, 14588]}
+{"event_id": 997142, "event_type": "Tornado", "state": "TENNESSEE", "cz_name": "OBION", "begin_date_time": "2021-12-10 22:48:00", "end_date_time": "2021-12-10 22:50:00", "narrative": "December 10, 2021, was unseasonably warm over the region. Temperatures broke several long-standing records. Memphis hit 80��F which broke a 103-year-old high-temperature record. ||A strong upper-level trough was approaching from the west, providing strong lift within the unseasonably warm and unstable air mass.  MLCAPE reached the 1500-2000 J/kg range by 6 PM. The wind field was impressive with plenty of vertical wind shear needed for organized thunderstorms. Effective 0-1 km storm-relative helicity values ranged from 300-400 m2/s2 with effective bulk shear values of 70 knots - more than sufficient to support discrete supercells in the warm sector ahead of the cold front.||The first supercell developed in central Arkansas and tracked into northeast Arkansas producing a few weak tornadoes initially before intensifying across eastern Craighead and Mississippi Counties and killing two people. The tornado eventually strengthened into an EF-4 while moving through the Missouri Bootheel, resulting in 2 direct and one indirect fatality in Pemiscot County. The tornado then tracked across the Mississippi River into northwest Tennessee, producing an additional 4 fatalities near Reelfoot Lake. This tornado lifted for a brief time in Obion County, reorganized, and then moved into Kentucky. All told, the mesocyclone tracked for over 300 miles and was producing tornadoes for over 250 miles. This storm was responsible for at least 9 fatalities and many injuries in the NWS Memphis CWA along with millions of dollars of damage. ||As the initial supercell was crossing the state line into Kentucky, a string of supercells was moving into eastern Arkansas. A few brief tornadoes produced minor damage near Cash in western Craighead County and in the Fisher area of western Poinsett County. As the dominant supercell moved into eastern Poinsett County, the mesocyclone quickly intensified and the storm produced an EF-2 tornado in Trumann with several injuries and widespread damage. ||A new supercell developed in Mississippi County causing straight-line wind damage initially. This supercell intensified as it crossed the Mississippi River and produced another long-track tornado starting in Dyer County,  Tennessee. This tornado tracked east-northeast across northwest Tennessee into Henry County, and eventually into Kentucky. This tornado was rated EF-3 and resulted in several injuries with Kenton and Dresden, Tennessee being the hardest hit. ||The convection eventually evolved into a QLCS as it moved east. A mesovortex developed south of I-40 near Jackson that resulted in 3 tornadoes across eastern Madison, Henderson, and Decatur Counties including an EF-2. Non-tornadic storms moved across the Memphis metropolitan area, producing straight-line wind damage as a mesovortex moved through the city. A fatality was reported in Shelby County after a large tree fell on a home in South Memphis. Later that night, an EF-1 tornado occurred in Prentiss County before the severe weather threat began to wind down around 6 AM on December 11, 2021. ||In total, there were 18 tornadoes across the NWS Memphis CWA.  Along with tornadoes, several incidents of wind damage and minor flash flooding also occurred. The tornado moved from Gibson County into the southeast corner of Obion County. The tornado uprooted and snapped trees along its path and heavily damaged a couple of homes on Sidonia Kenton Road. The tornado then crossed back into Gibson County. Peak winds were estimated at 125 mph in Obion County.", "ts_dict_index": [14529, 14530, 14531]}
+{"event_id": 879880, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "OUACHITA", "begin_date_time": "2020-04-12 10:36:00", "end_date_time": "2020-04-12 10:45:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. An EF-3 tornado with estimated maximum winds near 140 mph touched down at the corner of Fern Street and Brown Street in the Brownsville-Bawcomville community. As it moved through this area, it downed and snapped hundreds of trees, many of which fell onto homes. As the tornado crossed Sandal Street, it caused minor structural damage to several single-wide manufactured homes before tipping over a trailer as it crossed Jonesboro Road. The tornado then proceeded onward to break the metal trusses and bring down a wood chip conveyor belt onto a train at the Graphic Packaging International Paper Mill. As the tornado continued, it crossed the Ouachita River twice where it bends sharply before increasing intensity along Riverbend Drive. This increase in intensity was most notable from the many tree trunks snapped, the roof ripped off of a single family home, and the collapsed wall of another single family home. ||The tornado then crossed the Ouachita River again and partially damaged the roof of the Masur Museum of Art, missing Downtown Monroe by roughly a mile. As it crossed South Grand Street, it then ripped the roof off of a two story home and continued on to damage the roofs of several homes and downed trees until it crossed the intersection of Highway 165 and Interstate 20. There, it damaged a metal building structure and snapped a wooden power pole and steel light assembly as it crossed Millhaven Road. Numerous other power poles were snapped and blown over across Millhaven Road. Two semi trucks were also blown over near the Highway 165/Interstate 20 intersection as well. ||The worst damage from the tornado then occurred along Orchid Drive where it ripped the roof off of three homes and collapsed much of the exterior walls of one of the homes. It is believed that a mesovortex within the tornado led to this narrow corridor of more intense damage. After the tornado moved out of this subdivision, damage became more sporadic and the tornado touch down several more times before it destroyed a metal hangar housing several airplanes at the Monroe Regional Airport. The tornado then lifted as it crossed a runway at the airport. ||Initial estimates from the Ouachita Parish Office of Homeland Security and Emergency Preparedness indicate that a total of 458 homes across the parish were impacted by this tornado and the two other tornadoes which also touched down near the Sterlington community in Northern Ouachita Parish that same morning of April 12th. Of these homes, 23 homes were destroyed, 108 had major damage, 243 with minor damage, and another 84 homes were affected across the parish. Damage at the Monroe Regional Airport alone was estimated at $25-30 million. According to Entergy, South Monroe lost seven distribution lines and one substation as a result of this tornado. Several other circuits and transmission structures were also damaged.", "ts_dict_index": [14622, 14623, 14624]}
+{"event_id": 877511, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "DE SOTO", "begin_date_time": "2020-04-12 08:41:00", "end_date_time": "2020-04-12 08:53:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. An EF-2 tornado with estimated maximum winds around 125 mph touched down along Adams Road and downed hundreds of trees as it crossed Simpton Road, Myrtle Hill Road, and Willie X Road. Along Willie X Road, it damaged the shingles of three single family homes and a church. As the tornado crossed Highway 5, it strengthened and completely destroyed three single wide manufactured homes, ripped the roof off and collapsed the walls of two homes, shifted a portion of a home off its foundation while ripping its roof off, and then damaged an exterior wall and a carport in addition to ripping portions of the roof off of a fourth home. One of the manufactured homes destroyed had five residents inside when the tornado struck, and all five survived, with only one of the five injured while the others only experienced minor bumps and bruises. The tornado went on to destroy the fourth single wide manufactured home and damage the roofs of two additional homes along Fuller Lane. The tornado continued to snap and uproot several trees just off of Scott Road and damaged shingles to homes off of Pin Oak Flat Road and Berry Lane. The tornado went on to uproot and snap trees as it crossed Highway 175 and Interstate 49 just south of the Frierson exit. After downing additional trees, the tornado lifted near Friendship Road.", "ts_dict_index": [14610, 14611, 14612]}
+{"event_id": 965631, "event_type": "Tornado", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-29 16:40:00", "end_date_time": "2021-07-29 16:45:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. Tree damage began in the area of Bradshaw Rd in Plumstead Twp in |Bucks County, where a few sizable limbs were downed and a couple |of larger but weakened trees were snapped. The tornado then |entered a cornfield near the intersection of Ferry Rd and Point |Pleasant Pike. Some degree of convergence was noted in a narrow |path of downed corn, though it was not overly strong. In addition,|some trees adjacent to and southeast of the cornfield were also |damaged. The damage became more substantial with a clearer |rotation signature observed in the area of Ridgeview Dr, where a |number of trees were snapped, favoring higher elevation areas |along a ridge line. The snapping and shearing of trees in that |area and the nature of the debris field strongly indicated |tornadic damage, with the magnitude of damage meriting an EF1 |rating. The tornado continued southeastward through Carversville |Rd and to the area of Long Ln in Buckingham Twp. Several |residences along and near Long Ln sustained tree damage. The |tornado impacted Maximuck's Farm Market on Long Ln, where |greenhouses sustained roof damage and some uplift of their frames.|Some convergence was also noted in crop fields on the property. |Just southeast of the greenhouses, a barn on the property was |heavily damaged with a partial collapse of its walls. However, |just beyond the barn, a large stretch of cornfields and a tree |line beyond the cornfields were left untouched, indicating the |tornado lifted near the damaged barn.", "ts_dict_index": [14625, 14626, 14627]}
+{"event_id": 879881, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "OUACHITA", "begin_date_time": "2020-04-12 10:39:00", "end_date_time": "2020-04-12 10:43:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. An EF-3 tornado with estimated maximum winds near 140 mph touched down in a forested area near Horseshoe Lake Road, uprooting hundreds of trees. Winds increased and tree damage became more widespread as trees were uprooted and snapped, and several trees were debarked in a forested area before the tornado reached End of Line Road. This widespread tree damage was confirmed from drone video from the Ouachita Parish Office of Homeland Security and Emergency Preparedness (OHSEP) and photos from the University of Louisiana Monroe. This forested area is where the tornado is believed to be strongest based on tree damage and radar imagery, but there were not sufficient damage indicators available to rate winds any higher than 140 mph (EF-3). ||After passing through the forested area, the tornado ripped the roof off of two single family homes and destroyed an outbuilding along End of Line Road. It then damaged shingles from approximately ten houses as it tracked along Lonewa Lane and Rose Plantation Lane. Along Lonewa Lane, the tornado snapped four concrete poles (also indicative of EF-3 damage) before lifting just before it crossed Keystone Road about 1/2 mile northwest of Sterlington High School.", "ts_dict_index": [14613, 14614, 14615]}
+{"event_id": 877565, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "BIENVILLE", "begin_date_time": "2020-04-12 09:39:00", "end_date_time": "2020-04-12 09:44:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. An EF-1 tornado with estimated maximum winds near 110 mph touched down just west of the city of Arcadia, near Highway 9 south of Interstate 20. The tornado moved to the east-northeast uprooting and snapping trees and power lines. It completely destroyed a small outbuilding on Sapp Street west of Smith Avenue, and a single family home lost about 20% of its metal roof in this area as well. A mobile home was rolled off of its foundation along Crawford Road south of I-20. As the tornado crossed the interstate, it uprooted several trees before dissipating just north of I-20.", "ts_dict_index": [14619, 14620, 14621]}
+{"event_id": 993623, "event_type": "Tornado", "state": "IOWA", "cz_name": "GREENE", "begin_date_time": "2021-12-15 17:34:00", "end_date_time": "2021-12-15 17:36:00", "narrative": "December 15, 2021 was an unprecedented and historic event for the state of Iowa and the central US.  It featured the first-ever December derecho observed anywhere in the United States and the first Moderate Risk of severe thunderstorms issued by the NWS Storm Prediction Center in December for Iowa. Unofficially, it set the new single-day Iowa records for the most tornadoes and the most EF-2/F-2 or stronger tornadoes since 1950.  Finally, it will break the all-time December record high temperature for Iowa. ||Tornadoes: There were 63 confirmed tornadoes that occurred in Iowa, 21 of which were rated EF-2. Sixty three is unofficially the most tornadoes in Iowa in a single day with the previous being 35 tornadoes on August 31, 2014. Further, 21 EF-2 tornadoes is unofficially the most EF-2/F-2 or stronger tornadoes in a single day with the previous being 16 tornadoes on June 7, 1984. Prior to this event, a total of 5 tornadoes had occurred in Iowa in December since 1950 with all of them in southeastern Iowa.  | |Thunderstorm Wind: Numerous straight line wind gusts were also associated with these thunderstorms, some in excess of 80 mph.  During the event, nearly the entire state of Iowa was under a Severe Thunderstorm Warning at some point.  Audubon reported the highest gust in Iowa at 88 mph. This storm also met the criteria for a ���derecho'', which makes it the first derecho on record in the month of December anywhere in the United States.  Finally, we had an unofficial gust of 108 mph recorded by a mesonet station near Sheffield, Iowa associated with one of the tornadic circulations. ||Environmental Wind: After the line of storms had passed, numerous strong, non-thunderstorm wind gusts over 70 mph occurred overnight. The top three non-thunderstorm wind gusts were 83 mph in Decatur City, 81 mph in Marshalltown, and 80 mph in Johnston. The Des Moines International Airport recorded a 74 mph non-thunderstorm wind gust, which is the highest non-thunderstorm wind gust at this location since 1970.| |Temperatures: In addition to the severe weather and strong non-thunderstorm winds, the temperatures were remarkable and record setting. Numerous record daily highs were broken by many degrees. In addition and preliminarily, the all-time December record high temperature for Iowa of 74 degrees that was set in Thurman, IA on December 6, 1939 was broken with four sites reaching 75 degrees (Oskaloosa, Muscatine, Iowa City, and Ottumwa).||For detailed environmental analysis, including soundings, please view the various local NWS office event review pages: NWS Des Moines, NWS Sioux Falls, NWS Omaha, NWS Wichita, NWS Pueblo, NWS Twin Cities, NWS Quad Cities, NWS Hastings, NWS La Crosse, NWS Green Bay, or NWS Milwaukee. This was a relatively brief tornado but none the less strong as it snapped power poles along I Avenue south of 180th Street to the northwest of Farlin.  Otherwise, the tornado remained in rural areas of Greene County with no other reports of damage.", "ts_dict_index": [14583, 14584, 14585]}
+{"event_id": 965632, "event_type": "Tornado", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-29 16:59:00", "end_date_time": "2021-07-29 17:01:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. The supercell storm which produced a tornado in Plumstead Twp in Bucks County|cycled and produced another tornado beginning in New Hope in |Bucks County, Pennsylvania. Tree damage began near River Rd just |west of the Delaware River, with a portion of River Rd closed and |impassable due to downed trees. The tornado then began to cross the Delaware River enroute to Mercer County, New Jersey.", "ts_dict_index": [14628, 14629, 14630]}
+{"event_id": 971958, "event_type": "Tornado", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-07-29 18:06:00", "end_date_time": "2021-07-29 18:12:00", "narrative": "A strong shortwave trough moved east-southeastward out of the Great Lakes region on July 29. An associated, strengthening surface low also tracked out of the Great Lakes and into upstate New York. A warm front associated with this low moved through most of New Jersey and eastern Pennsylvania during the late morning and early afternoon hours. This front, combined with the remains of widespread convection to the west from the previous overnight and morning hours, brought significant cloud cover to the eastern mid-Atlantic for much of the day on the 29th. This was mainly in the form of mid and high level cloud cover, however, and temperatures still warmed to near seasonal levels behind the warm front, allowing moderate to strong instability to build. Meanwhile, the robust surface and upper level disturbances approaching the region brought both strong forcing and unseasonably strong wind shear. By mid-afternoon, an unusually favorable convective environment existed over eastern Pennsylvania and New Jersey.||The result of this environment was a rare tornado outbreak across the area. Initially, during the mid-afternoon hours, mixed convective modes over east-central Pennsylvania produced a couple instances of damaging wind and brief tornadoes as storms attempted to overcome cloud cover and some light stratiform rain in the area. With time, as storms moved into better instability and a less contaminated environment over far eastern Pennsylvania and New Jersey, they took on more supercellular structures. Multiple cyclic supercells would go on to produce several tornadoes, three of them strong (EF2+) over eastern Pennsylvania and New Jersey. Convection persisted past the sunset hour with little to no loss in intensity due to the strong forcing. The only thing that put an end to the outbreak was the coastline, as storms moved offshore towards 9 to 10PM local time. Even offshore, one supercell continued to exhibit strong rotation and likely produced a strong waterspout for tens of miles over the Atlantic.||Fortunately, and miraculously, no serious injuries or loss of life occurred as a result of this outbreak. With the passage of a cold front late on the evening of the 29th, cooler, drier, and much less active weather would grace the region for several days as clean-up efforts began. The tornado which began in Philadelphia County crossed into Bucks County, where it would produce the majority of its impacts. After crossing the county line, the tornado continued between Trevose Road and Peyton Street |where additional tree damage occurred before crossing Lukens |Street. The tornado then very briefly crossed back into |Philadelphia County at the northern tip of Poquessing Valley Park |where a few trees were uprooted. The tornado then crossed back |into Trevose in Bucks County where it caused some minor cosmetic |damage to some homes in the Beechwood Estates neighborhood and |blew down several sections of vinyl fencing. Several small trees |were also snapped or uprooted in and just south and east of the |residential neighborhood.||As the tornado approached Somerton Road, it began intensifying |and widening substantially as it moved into the Metropolitan |Industrial Center. Numerous softwood and hardwood trees were |snapped or uprooted in the SUEZ Water Company property southwest |of and along Somerton Road. Five wooden power poles were snapped |near the ground along Somerton Road as well at the northern end of|the SUEZ property. All seven warehouse buildings in the |industrial complex northeast of Somerton Road sustained at least |minor damage, with the most significant occurring to the Northtec |building. Numerous roof mounted HVAC units were shifted or blown |off of a few of the buildings in the industrial complex. Open bay |doors in the western- most building caused a non-load bearing |interior wall to collapse. A sedan was lifted and flipped over in |the Northtec parking lot and a steel flag pole bearing a flag |flattened completely to the ground. The Northtec building |sustained substantial structural damage where large sections of |roofing material were removed. Additionally, numerous exterior |paneling was blown off, garage bay doors were blown out, a few |windows were blown out, and at least two large HVAC units were |blown off of the building. Numerous softwood and hardwood trees |were uprooted or snapped in the industrial complex and immediately|adjacent areas.||A cellphone tower adjacent to the industrial complex had all of |the antennas blown off, but the tower itself did not collapse. |Southeast of the industrial complex, minor cosmetic damage |occurred to some homes along Carter Road in a residential |neighborhood. Tree damage associated with the tornado occurred |along Carter Road and Sussex Road north of Buckfield Terrace. This|was the area where the tornado circulation reached its widest |extent of around three tenths of a mile. As the tornado neared and|crossed the Pennsylvania Turnpike (I- 276), an overhead roadway |information sign was blown off and a portion of it landed |downstream nearly a half mile away. Just north of the turnpike, |minor cosmetic damage occurred to a hotel building where a tree |was also uprooted in the parking lot. A large billboard was blown |over just north of the turnpike and south of Street Road. A small |utility building nearby had its roof blown off. The northern- most|extent of the damage occurred on the Toscana 52 restaurant |property where the tornado blew down some chain link fencing and |uprooted a few small trees in the parking lot.||The tornado continued east-northeastward across Street Road |toward the Faulkner car dealership complex where it began |intensifying and somewhat narrowing its path of damage. The four |dealership showrooms sustained significant damage where most |windows were blown out and at least some roofing material was |blown off. The most significant damage occurred to the Buick/GMC |showroom where most of the roofing material was blown off, all |windows and doors were blown out, and exterior walls exhibited |fracturing due to stress from the wind. Roof HVAC units of this |building were tossed into the parking lot behind the building. All|of the dealership signs near the main road were destroyed. Scores|of new and used vehicles sustained significant damage from flying|debris or from being pushed or tossed trough the air.||The tornado continued toward the dealership's main service garage|where the most significant damage occurred. The southwestern |portion of the building was destroyed with most exterior walls |collapsing completely and all roofing material blown off. Interior|walls mostly remained standing. Roof HVAC units were tossed off |of the building with one unit landing nearly 200 yards downstream |of the building. Damage sustained to the building decreased |somewhat toward the eastern end of it where portions of the |exterior walls were damaged and almost all garage bay doors were |blown out. The wind rushing through the garage area carried |debris, car parts, and tools well away from the structure |downstream. Some vehicles near the main garage building were |completely destroyed from large pieces of flying debris or from |being tossed and dropped back onto the ground. A small pickup |truck was crushed from a collapsed exterior wall. Five people |reportedly sustained minor injuries at the dealership complex.||The tornado continued east-northeast toward the Weisser Homes |mobile home park and into an area of trees which sustained |significant damage. Most tree canopies and limbs were completely |stripped from the still standing or snapped trunks of hardwood |trees in this area. A large storage container filled with car |parts from the service garage parking lot upstream was lofted into|the air and dropped into this area of trees. An uninhabited |mobile home model was lifted and completely destroyed at the |mobile home park. Another double-wide mobile home had a large |portion of its roof blown off. Several other mobile home sustained|varying degrees of damage as well. A large amount of various |debris from the dealership complex landed in this mobile home |park. Numerous softwood and hardwood trees near and just |downstream of this area were snapped or uprooted along Old Lincoln|Highway.||At this stage, the tornado damage path narrowed considerably and |intensity weakened significantly as it crossed Old Lincoln Highway|and moved toward the Lowe's and Walmart shopping centers on Route|1. The tornado passed over these shopping centers, but no |structural damage was noted to these structures. Numerous small |trees were snapped and uprooted in the large parking lot area and |line of trees just north of the Bensalem turnpike interchange. |Some exit ramp signs were blown down in the interchange area.||The tornado damage became somewhat discontinuous as it continued |east-southeast into Bensalem across Route 1 and toward a |residential neighborhood. Several homes in the neighborhood |sustained loss of some roofing material and other cosmetic damage |in addition to some tree damage. The tornado continued across |Rockhill Road and along Richlieu Road toward the Christian Life |Center where several trees were snapped or uprooted. The church's |steeple had some paneling blown off, but the steeple itself was |not damaged otherwise. The tornado continued weakening as it |crossed Galloway Road then dissipated in the Bensalem Township |Community Park where some minor tree damage occurred.||No known serious injuries or fatalities occurred from this |tornado.", "ts_dict_index": [14631, 14632, 14633]}
+{"event_id": 1033988, "event_type": "Tornado", "state": "IOWA", "cz_name": "WOODBURY", "begin_date_time": "2022-05-12 18:01:00", "end_date_time": "2022-05-12 18:02:00", "narrative": "A volatile environment featured a warm front from parts of east central South Dakota into western Minnesota, with a dryline extending to the southwest into Nebraska. With a very strong wave moving northeast through Nebraska into a highly unstable and highly sheared environment, scattered storms initiated and quickly grew upscale to a broad linear structure with damaging winds. With crop development well behind schedule and many fields yet to be planted, there was ample dirt available to be lofted into the leading edge of the storms, which took on the characteristics of a haboob reducing visibility to near zero at the onset of high winds.||A broad swath of winds from 70 to 100 mph devastated much of southeast South Dakota, and portions of southwest Minnesota, northeast Nebraska and northwest Iowa, causing extensive tree and structural damage and scores of injuries. The highest observed wind gust was 107 mph near Tripp, SD. In addition, vehicles and high profile vehicles were blown off several roads, shutting down traffic on Interstates 29 and 90. Two (direct) fatalities occurred in vehicles impacted by debris as the storms moved into the Sioux Falls area. Power was disrupted in a widespread area, with estimates of over 45,000 customers impacted at one time. Many schools were closed due to damage and power issues. The South Dakota Governor requested and was granted a Presidential Disaster Declaration for damage to public infrastructure at an estimated cost of 6.7 million dollars across 20 counties and two reservations. Private losses were a much higher toll, and just one of the impacted counties (McCook) estimated at least 150 to 175 million dollars in damage. Presidential Disaster Declarations were also granted in Dixon County, Nebraska and Lincoln County, Minnesota.||Following the afternoon line of storms, a secondary band of storms developed near the core of the upper level jet across eastern Nebraska in the early evening hours. These storms also quickly become severe, with a mix of large hail, damaging wind, and even an isolated tornado near Sioux City. This cluster of storms moved through far southeast South Dakota, northwest Iowa and southwest Minnesota during the evening. A video showed a brief tornado crossing Interstate 29 between Sergeant Bluff and Port Neal. The tornado caused no damage from which the NWS could assign an EF-scale rating.", "ts_dict_index": [14637, 14638, 14639]}
+{"event_id": 952383, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "HAMILTON", "begin_date_time": "2021-05-02 18:51:00", "end_date_time": "2021-05-02 18:52:00", "narrative": "Slow moving front brought severe thunderstorms, including landspouts, and heavy rain to portions of south central Nebraska during the evening of May 2nd. A line of thunderstorms blossomed along a stationary front between 6-8PM CDT from southern Gosper County E to Adams County, then NE to Polk County. Once this activity developed, it remained nearly stationary until around 10PM CDT when an upper level disturbance arrived from the W and began to nudge convection to the E and SE. The primary hazard with the initial convection was landspout tornadoes. A total of four landspout tornadoes were observed: one in Kearney County, two in Hamilton County, and one in Polk County. Landspout tornadoes are often very weak and cause little to no damage. These landspouts generally fall into that category, but two of them did cause at least minor damage. Most notable was the landspout that occurred near Hwy 14 just S of Aurora. Not only was it very photogenic, but it also caused damage to a storage building and downed a power line. Other severe reports were limited to severe wind gust in Furnas County, and a large hail report in Kearney County. By late evening and into the overnight, the main threat turned to flash flooding due to the stationary/nearly-stationary nature of the thunderstorms. The heaviest rainfall amounts ranged from 3 to 6 inches and flash flooding was reported in Kearney, Adams, and Hamilton Counties. Impacts ranged from flooded streets, underpasses, and rural roads, to water in some basements in Aurora. Thunderstorms weakened considerably by midnight and lingering rain showers ended by dawn on the morning of the 3rd.||The landspout tornadoes developed within a zone of favorable juxtaposition of steep low level lapse rates, moderate low level instability, weak deep layer shear, and high ambient surface vorticity associated with the stalled surface boundary. Heavy rainfall was supported by aforementioned extremely slow storm motions, as well as seasonably high deep layer moisture. This landspout was rated an unknown EF scale and unknown wind speed because of the lack of observable damage. The location was estimated based on pictures and videos.", "ts_dict_index": [14655, 14656, 14657]}
+{"event_id": 1107644, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 15:28:00", "end_date_time": "2023-06-21 15:29:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A tornado briefly touched down in open country. No damage was observed.", "ts_dict_index": [14673, 14674, 14675]}
+{"event_id": 1107618, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 15:10:00", "end_date_time": "2023-06-21 15:11:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A tornado touched down briefly in an open field.  No damage was observed.", "ts_dict_index": [14670, 14671, 14672]}
+{"event_id": 824304, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HOCKLEY", "begin_date_time": "2019-05-25 15:59:00", "end_date_time": "2019-05-25 16:01:00", "narrative": "Another consecutive day of severe weather unfolded across the South Plains of West Texas and the extreme southern Texas Panhandle. An upper level trough remained in place over the Intermountain West with a weak short wave moving over the South Plains during the afternoon hours. Convection initially developed late in the morning in eastern New Mexico while rapidly expanding in coverage as convection moved east. Storms quickly became severe as they took advantage of ample instability. A few reports of large hail and severe wind gusts were received from thunderstorms on the 25th. ||The most significant weather from these storms were flooding and tornadoes. A NWS storm survey revealed that four tornadoes occurred on the 25th with one EF-2 and three EF-U ratings. The first was approximately eight miles west-southwest of Anton in Hockley County but flooded roads prevented a survey from taking place. The second tornado, rated EF-2, occurred for only six minutes but caused significant damage near Plainview (Hale County). The most significant damage from this tornado was the destruction of a trussed cell phone tower. Several other areas of damage were noted from this tornado along Interstate 27 just north of Plainview. The third tornado was on the ground for approximately 4.7 miles but no damage indicators prevented a rating to be assigned to this tornado. The fourth and final tornado was observed in Hall County near the ghost town of Eli.||Very high precipitable water values relative to the time of year were observed on nearby RAOBs. Furthermore, many of the storms were slow moving. Exacerbating the flooding were the very wet grounds from previous days precipitation. A NWS cooperative weather observer's home near Littlefield flooded on both the 24th and 25th due to torrential rainfall. The supercell storm that produced a tornado near Plainview also developed major flooding in and around Plainview. Storm chasers reported a brief tornado in Hockley County. A storm survey was unable to be completed to due flooded roads.", "ts_dict_index": [14661, 14662, 14663]}
+{"event_id": 1108827, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 17:45:00", "end_date_time": "2023-06-21 18:00:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A tornado touched down in open country.  No damage was observed.", "ts_dict_index": [14667, 14668, 14669]}
+{"event_id": 1107962, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 15:45:00", "end_date_time": "2023-06-21 15:46:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A tornado touched down briefly in open country. No damage was observed.", "ts_dict_index": [14664, 14665, 14666]}
+{"event_id": 952382, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "HAMILTON", "begin_date_time": "2021-05-02 18:51:00", "end_date_time": "2021-05-02 18:56:00", "narrative": "Slow moving front brought severe thunderstorms, including landspouts, and heavy rain to portions of south central Nebraska during the evening of May 2nd. A line of thunderstorms blossomed along a stationary front between 6-8PM CDT from southern Gosper County E to Adams County, then NE to Polk County. Once this activity developed, it remained nearly stationary until around 10PM CDT when an upper level disturbance arrived from the W and began to nudge convection to the E and SE. The primary hazard with the initial convection was landspout tornadoes. A total of four landspout tornadoes were observed: one in Kearney County, two in Hamilton County, and one in Polk County. Landspout tornadoes are often very weak and cause little to no damage. These landspouts generally fall into that category, but two of them did cause at least minor damage. Most notable was the landspout that occurred near Hwy 14 just S of Aurora. Not only was it very photogenic, but it also caused damage to a storage building and downed a power line. Other severe reports were limited to severe wind gust in Furnas County, and a large hail report in Kearney County. By late evening and into the overnight, the main threat turned to flash flooding due to the stationary/nearly-stationary nature of the thunderstorms. The heaviest rainfall amounts ranged from 3 to 6 inches and flash flooding was reported in Kearney, Adams, and Hamilton Counties. Impacts ranged from flooded streets, underpasses, and rural roads, to water in some basements in Aurora. Thunderstorms weakened considerably by midnight and lingering rain showers ended by dawn on the morning of the 3rd.||The landspout tornadoes developed within a zone of favorable juxtaposition of steep low level lapse rates, moderate low level instability, weak deep layer shear, and high ambient surface vorticity associated with the stalled surface boundary. Heavy rainfall was supported by aforementioned extremely slow storm motions, as well as seasonably high deep layer moisture. This landspout moved north-northwest for approximately 1 mile before diminishing roughly as it crossed Highway 14 just south of Aurora. The main observable damage was damage to storage building roll-up doors, a couple of larger overhead doors and a downed power line. The treeline near the start of the tornado had evidence of cornstalks lofted up into the trees and power lines.", "ts_dict_index": [14658, 14659, 14660]}
+{"event_id": 1107686, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 15:36:00", "end_date_time": "2023-06-21 15:37:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A tornado touched down briefly in open country.  No damage was observed.", "ts_dict_index": [14679, 14680, 14681]}
+{"event_id": 866649, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2020-01-10 23:43:00", "end_date_time": "2020-01-10 23:50:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. An EF-1 tornado with estimated maximum winds near 110 mph touched down along Highway 84 near the intersection of County Road 4234 west of Mount Enterprise, snapping and uprooting a few trees. The tornado continued eastward roughly along Highway 84, intensifying and snapping numerous trees in the Reagan Branch bottom, just west of the Farm to Market Road 225 intersection. It continued east-northeast snapping and uprooting trees as it crossed County Roads 3223, 3226, and 3206. Several farm outbuildings were tossed and completely destroyed along County Road 3206, with two residences sustaining roof damage, before the tornado lifted just northeast of the intersection of County Road 3206 and 3166.", "ts_dict_index": [14649, 14650, 14651]}
+{"event_id": 866662, "event_type": "Tornado", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2020-01-11 00:18:00", "end_date_time": "2020-01-11 00:19:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. An EF-1 tornado with estimated maximum winds near 110 mph touched down on a hillside just southwest of Farm to Market Road 959 just northeast of Tatum. The damage was limited to trees, as a majority of the few hundred pine trees in a confined area had their trunks snapped. The tornado tracked northeast off the hill doing only sporadic tree damage before crossing Farm to Market Road 959, resulting in roof damage to several residences and outbuildings. The tornado lifted shortly thereafter prior to crossing the Sabine River bordering Southern Harrison County.", "ts_dict_index": [14643, 14644, 14645]}
+{"event_id": 877438, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-04-12 08:08:00", "end_date_time": "2020-04-12 08:20:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and locally heavy rainfall which resulted in isolated flash flooding. Two isolated tornadoes also touched down in Shelby and Southern Harrison Counties. ||While there was a lull in the thunderstorms from late morning through much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds exited East Texas into Western Louisiana by early evening before gradually weakening. An EF-1 tornado with estimated maximum winds near 105 mph touched down just southwest of the Crossroads community near the intersection of Mercer and Eddington Roads, where several trees were snapped. The tornado continued northeast across FM 31 near Hays Road, where multiple trees were snapped and uprooted. A tree also fell on a home, but fortunately, the residents inside were not injured. The tornado tracked northeast, crossing FM 2525, Webb Rogers Road near Sneed Road, and Ireland Williams Road, snapping numerous large limbs and trees. The tornado crossed Interstate 20 and Highway 80, snapping additional large limbs, before lifting near Bellview Road.", "ts_dict_index": [14634, 14635, 14636]}
+{"event_id": 866665, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2020-01-11 00:30:00", "end_date_time": "2020-01-11 00:33:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. An EF-0 tornado with estimated maximum winds near 85 mph touched down off of County Road 2108 and snapped small and large branches along its path. The tornado crossed Highway 43 where it tore off a wooden front porch and gutters off of a home. It then crossed County Road 2600 before lifting near Farm to Market Road 134 before entering the Longhorn Army Ammunition Plant.", "ts_dict_index": [14652, 14653, 14654]}
+{"event_id": 1096954, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "DAWSON", "begin_date_time": "2023-05-05 21:54:00", "end_date_time": "2023-05-05 22:00:00", "narrative": "Large hail, damaging wind gusts, and an isolated tornado occurred over portions of south central Nebraska, mainly west of Highway 281, during the afternoon through late evening hours. Initial development occurred roughly along the NE/KS state line between 1600-1700CDT, and was mainly in the form of supercells. By around 2200CDT, nearly a half-dozen supercells affected portions of south central Nebraska roughly along and south of Interstate 80 (I-80) and west of Highway 281 and produced scattered instances of large to very large hail. The largest hail reported was tennis ball in Franklin County, which was associated with one of the first supercells to form in the late afternoon. After the initial round of supercells, which weakened mostly below severe limits by 2230CDT, a squall line of thunderstorms moved into far western portions of the CWA between 2230-2300CDT. The primary severe threat with this activity was damaging wind gusts of 60-65MPH. However, embedded within the squall line was a brief EF-1 tornado that impacted the Johnson Lake area around 2300. A bow echo developed within the squall line between 2300-2400CDT over Dawson County then raced northeast and affected areas north of the Platte River over the next 60-90 minutes. This activity weakened as it exited NE portions of the CWA during the early morning hours of May 6th.||While there were no significant synoptic scale fronts or low pressure systems in the area of this event, the first round of scattered supercells developed along a remnant outflow boundary that was stalled near the NE/KS state line. The second round was a result of thunderstorms that developed over the High Plains which was then supported by an increasing low level jet as activity shifted east overnight. Through the entire event, there was moderately strong instability (2000-3000 J/kg of CAPE), strong deep layer shear around 40-45kt, and steep mid level lapse rates of 7-8C/km. 0-3km shear was also strong during this event, around 30kt, which supported the bow echo development across northern portions of the CWA during the evening hours. A tornado developed within a line of thunderstorms northwest of Johnson Lake in far southern Dawson county just before 11:00 PM on Friday, May 5th. The tornado appeared to begin a couple miles northwest of the toppled three irrigation pivots before hitting the Lakeview Acres area on the northwest side of the lake. At least two large storage sheds were totally destroyed in that area. There were several instances of damage in the area, such as trees, smaller buildings, windows and some roof damage,|including two 2x4 stud driven into the roof of one home. The tornado traversed east across the lake and did significant damage to several homes on the east side of the lake right along the Gosper county line. Along the shore line, at least three homes in a row had all or part of a covered porch blown apart, and one home had a large section of its roof torn off. Another flat roof cabin had its entire roof torn off. A few power poles were snapped. Tree damage was common in this general area. The tornado moved east and upset an irrigation pivot and peeled back some metal roofing from a large building just east of the lake. The tornado likely dissipated east of County Road 428. The |maximum wind speed was estimated to be 95 MPH based upon the residential roof damage and the storage building being destroyed. The path was just under 5 miles long and the width was estimated to be 80 yards.", "ts_dict_index": [14640, 14641, 14642]}
+{"event_id": 879885, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "OUACHITA", "begin_date_time": "2020-04-12 10:46:00", "end_date_time": "2020-04-12 10:48:00", "narrative": "Warm, moist, and unstable air surged north into East Texas, North Louisiana, and Southern Arkansas during the evening through the early morning hours of April 11th-12th, along a warm front that lifted north across much of East Texas into North Louisiana. Meanwhile, a strong upper level low opened up into a trough as it entered the Southern Plains during the evening of the 11th, with large scale forcing ahead of the trough enhancing shower and thunderstorm development across much of West-central, Central, East and Southeast Texas during the evening through the early morning hours. Given the extent of shear, instability, and upper level forcing in place across the warm sector, numerous showers and thunderstorms developed over these areas, which quickly spread east northeast into East Texas around and shortly after daybreak on the 12th, and into North Louisiana during the mid and late morning hours. Some of these storms were severe, producing numerous reports of damaging winds, large hail, and tornadoes. In all, nine tornadoes touched down across North Louisiana, including two EF-3 tornadoes with estimated maximum winds near 140 mph which tore through the southern sections of West Monroe through Central and Eastern Monroe, as well as just southwest of Sterlington in Northern Ouachita Parish. ||While there was a lull in the thunderstorms during much of the afternoon, additional strong to severe thunderstorms developed across portions of Northeast Texas well behind the dry line which had mixed east to near Texarkana into Western Louisiana, and near the center of the upper level trough. Steep lapse rates aloft and the drier low level air mass contributed to areas of damaging winds and isolated instances of large hail, with the majority of the wind damage from a collapsing thunderstorm which originated just east of Dallas, and quickly moved east along the I-20 corridor in East Texas into Western Louisiana. Aided by strong pressure rises behind an associated cold front, a large swath of damaging winds were noted with the severe gust front, with gusts ranging from 50-70 mph well ahead of the collapsed storm. This resulted in numerous reports of downed trees and power lines across East Texas and Western Louisiana, with AEP Swepco noting that over 64,000 customers were without power at one time in the aftermath of the storms. These damaging winds diminished across Western Louisiana by mid-evening. An EF-1 tornado with estimated maximum winds near 105 mph briefly touched down in the Fairbanks community along the corner of John Turner Road and Highway 134. It continued on to cross Highway 134 again and Curtis Road before lifting. Approximately 30 trees were uprooted and snapped in a convergent pattern along its path.", "ts_dict_index": [14616, 14617, 14618]}
+{"event_id": 1107666, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 15:29:00", "end_date_time": "2023-06-21 15:30:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A second weaker satellite tornado, formed in close proximity to the EF2 tornado, briefly touched down in open country.  No damage was observed.", "ts_dict_index": [14685, 14686, 14687]}
+{"event_id": 1107655, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 15:28:00", "end_date_time": "2023-06-21 15:35:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A large tornado with estimated peak winds to 118 mph, snapped power poles as it crossed Highway 63.", "ts_dict_index": [14697, 14698, 14699]}
+{"event_id": 1108819, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 15:57:00", "end_date_time": "2023-06-21 16:10:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A tornado touched down in open country. No damage was observed.", "ts_dict_index": [14691, 14692, 14693]}
+{"event_id": 1108822, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 16:30:00", "end_date_time": "2023-06-21 16:40:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A tornado touched down and damaged a house.", "ts_dict_index": [14688, 14689, 14690]}
+{"event_id": 1107678, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 15:31:00", "end_date_time": "2023-06-21 15:34:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. Another satellite tornado, formed in open country near the EF2 tornado, and eventually wrapped into it.  No damage was observed.", "ts_dict_index": [14694, 14695, 14696]}
+{"event_id": 1108821, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 16:20:00", "end_date_time": "2023-06-21 16:36:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A large tornado damaged a farm with a large barn destroyed along with grain bins.  A few power poles snapped near this area as well.", "ts_dict_index": [14682, 14683, 14684]}
+{"event_id": 1107627, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 15:25:00", "end_date_time": "2023-06-21 15:26:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A tornado briefly touched down in open country.  No damage was observed.", "ts_dict_index": [14700, 14701, 14702]}
+{"event_id": 1107958, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 15:43:00", "end_date_time": "2023-06-21 15:45:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A larger tornado touched down briefly in open country. No damage was observed.", "ts_dict_index": [14676, 14677, 14678]}
+{"event_id": 1018628, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HOCKLEY", "begin_date_time": "2022-05-23 19:06:00", "end_date_time": "2022-05-23 19:11:00", "narrative": "Returning Gulf of Mexico moisture into the South Plains of West Texas fueled widespread severe thunderstorm development across the region on the afternoon and evening of the 23rd. Moderate to strong instability developed across the western South Plains and eastern New Mexico Monday afternoon and evening as the improving low-level moisture and temperatures warming into the 80s developed beneath an approaching upper level storm system. Relatively strong wind shear caused several of the thunderstorms to rotate as they moved into the western South Plains and western Texas Panhandle. A cluster of thunderstorms moving northeast out of southeastern New Mexico interacted with an outflow boundary moving northwest out of the Permian Basin. This caused a storm on the southern flank of the cluster to begin to rotate and become supercellular and take a more easterly, then southeasterly track. As the storm intensified, it became cyclic in behavior and its forward speed varied from about 5 mph to 20 mph. An NWS storm survey revealed that this supercell produced nine separate tornadoes over an approximately two hour period. The tornadoes occurred over rural areas which limited the overall impacts. Spotty damage did occur including two oil pumpjacks that were toppled by the intense tornadic winds. This damage, along with snapped power poles and flipped center pivots earned a peak damage rating of EF-2. The thunderstorms eventually evolved into a larger complex that brought widespread rain to most of the South Plains, Rolling Plains, and southern Texas Panhandle. The heaviest rain was associated with the slow-moving tornadic storm and was concentrated over Bailey County, where three to as much as seven inches of rain fell. A cyclic tornadic supercell produced several tornadoes over a period of approximately two hours. An NWS storm survey revealed that this supercell produced nine separate tornadoes. This tornado was the fifth tornado. Numerous storm chasers documented a brief, small tornado in an open field. Wooden power poles were blown down at the intersection of Farm to Market Roads 597 and 303, approximately two miles south of Pep. Maximum winds were estimated at 85 mph.", "ts_dict_index": [14721, 14722, 14723]}
+{"event_id": 1018629, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HOCKLEY", "begin_date_time": "2022-05-23 19:28:00", "end_date_time": "2022-05-23 19:32:00", "narrative": "Returning Gulf of Mexico moisture into the South Plains of West Texas fueled widespread severe thunderstorm development across the region on the afternoon and evening of the 23rd. Moderate to strong instability developed across the western South Plains and eastern New Mexico Monday afternoon and evening as the improving low-level moisture and temperatures warming into the 80s developed beneath an approaching upper level storm system. Relatively strong wind shear caused several of the thunderstorms to rotate as they moved into the western South Plains and western Texas Panhandle. A cluster of thunderstorms moving northeast out of southeastern New Mexico interacted with an outflow boundary moving northwest out of the Permian Basin. This caused a storm on the southern flank of the cluster to begin to rotate and become supercellular and take a more easterly, then southeasterly track. As the storm intensified, it became cyclic in behavior and its forward speed varied from about 5 mph to 20 mph. An NWS storm survey revealed that this supercell produced nine separate tornadoes over an approximately two hour period. The tornadoes occurred over rural areas which limited the overall impacts. Spotty damage did occur including two oil pumpjacks that were toppled by the intense tornadic winds. This damage, along with snapped power poles and flipped center pivots earned a peak damage rating of EF-2. The thunderstorms eventually evolved into a larger complex that brought widespread rain to most of the South Plains, Rolling Plains, and southern Texas Panhandle. The heaviest rain was associated with the slow-moving tornadic storm and was concentrated over Bailey County, where three to as much as seven inches of rain fell. A cyclic tornadic supercell produced several tornadoes over a period of approximately two hours. An NWS storm survey revealed that this supercell produced nine separate tornadoes. This tornado was the seventh tornado. No damage was observed or reported from this short lived, small tornado. The instantaneous center of the tornado was estimated from TTU-Kal radar data.", "ts_dict_index": [14724, 14725, 14726]}
+{"event_id": 1018631, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HOCKLEY", "begin_date_time": "2022-05-23 19:40:00", "end_date_time": "2022-05-23 19:58:00", "narrative": "Returning Gulf of Mexico moisture into the South Plains of West Texas fueled widespread severe thunderstorm development across the region on the afternoon and evening of the 23rd. Moderate to strong instability developed across the western South Plains and eastern New Mexico Monday afternoon and evening as the improving low-level moisture and temperatures warming into the 80s developed beneath an approaching upper level storm system. Relatively strong wind shear caused several of the thunderstorms to rotate as they moved into the western South Plains and western Texas Panhandle. A cluster of thunderstorms moving northeast out of southeastern New Mexico interacted with an outflow boundary moving northwest out of the Permian Basin. This caused a storm on the southern flank of the cluster to begin to rotate and become supercellular and take a more easterly, then southeasterly track. As the storm intensified, it became cyclic in behavior and its forward speed varied from about 5 mph to 20 mph. An NWS storm survey revealed that this supercell produced nine separate tornadoes over an approximately two hour period. The tornadoes occurred over rural areas which limited the overall impacts. Spotty damage did occur including two oil pumpjacks that were toppled by the intense tornadic winds. This damage, along with snapped power poles and flipped center pivots earned a peak damage rating of EF-2. The thunderstorms eventually evolved into a larger complex that brought widespread rain to most of the South Plains, Rolling Plains, and southern Texas Panhandle. The heaviest rain was associated with the slow-moving tornadic storm and was concentrated over Bailey County, where three to as much as seven inches of rain fell. A cyclic tornadic supercell produced several tornadoes over a period of approximately two hours. An NWS storm survey revealed that this supercell produced nine separate tornadoes. This tornado was the ninth and final tornado. The NWS storm survey team discovered several locations along Farm to Market Road 303 with wooden power poles snapped at the base and two pump jacks overturned. Maximum winds were estimated at 120 mph. The instantaneous width and center of the tornado was estimated from TTU-Kal radar data.", "ts_dict_index": [14727, 14728, 14729]}
+{"event_id": 866960, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2020-01-11 01:24:00", "end_date_time": "2020-01-11 01:32:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Widespread damaging winds downed trees and power lines across much of Northwest and Northcentral Louisiana, with even a long track tornado developing along the line of severe thunderstorms across Central Bossier, Southern Webster, and Southern Claiborne Parishes. Another isolated tornado touched down in Western Union Parish, before these storms exited the region shortly before daybreak on the 11th. Unfortunately, these storms resulted in four fatalities  across Northwest Louisiana, three of which occurred from the Haughton tornado. A long track 40+ mile long EF-2 tornado with estimated maximum winds near 135 mph first touched down just south of Barksdale Air Force Base off of Sligo Road in Central Bossier Parish, where it snapped and uprooted hundreds of softwood and hardwood trees and damaged several carports and outbuildings. The tornado then crossed the far southeast corner of Barksdale Air Force Base where at least one hundred trees were snapped or uprooted. After the tornado exited the corner of Barksdale Air Force Base, it strengthened south of Haughton to produce its most significant damage, completely destroying a single-wide manufactured home and a double-wide manufactured home off of Davis Road. Two fatalities (a 79 year old male and his 65 year old wife) occurred in the double-wide with an additional fatality (an 87 year old male) occurring in the single-wide. The tornado continued to produce roof damage and uproot and snap trees which fell into homes in Eastern Bossier Parish, concentrated most along James Lane. The tornado continued moving northeast across Oliver Road and Camp Zion Road, where numerous trees were snapped and uprooted, while also removing siding off of a single-wide manufactured home, and ripping a portion of the metal exterior and doors off of the Bossier Parish Fire District 1 Station 6 building, as well as tearing off some vinyl siding to a mobile home living quarters located next door, before crossing over into Webster Parish.", "ts_dict_index": [14712, 14713, 14714]}
+{"event_id": 1018630, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HOCKLEY", "begin_date_time": "2022-05-23 19:37:00", "end_date_time": "2022-05-23 19:39:00", "narrative": "Returning Gulf of Mexico moisture into the South Plains of West Texas fueled widespread severe thunderstorm development across the region on the afternoon and evening of the 23rd. Moderate to strong instability developed across the western South Plains and eastern New Mexico Monday afternoon and evening as the improving low-level moisture and temperatures warming into the 80s developed beneath an approaching upper level storm system. Relatively strong wind shear caused several of the thunderstorms to rotate as they moved into the western South Plains and western Texas Panhandle. A cluster of thunderstorms moving northeast out of southeastern New Mexico interacted with an outflow boundary moving northwest out of the Permian Basin. This caused a storm on the southern flank of the cluster to begin to rotate and become supercellular and take a more easterly, then southeasterly track. As the storm intensified, it became cyclic in behavior and its forward speed varied from about 5 mph to 20 mph. An NWS storm survey revealed that this supercell produced nine separate tornadoes over an approximately two hour period. The tornadoes occurred over rural areas which limited the overall impacts. Spotty damage did occur including two oil pumpjacks that were toppled by the intense tornadic winds. This damage, along with snapped power poles and flipped center pivots earned a peak damage rating of EF-2. The thunderstorms eventually evolved into a larger complex that brought widespread rain to most of the South Plains, Rolling Plains, and southern Texas Panhandle. The heaviest rain was associated with the slow-moving tornadic storm and was concentrated over Bailey County, where three to as much as seven inches of rain fell. A cyclic tornadic supercell produced several tornadoes over a period of approximately two hours. An NWS storm survey revealed that this supercell produced nine separate tornadoes. This tornado was the eighth tornado. No damage was observed or reported with this short lived, small tornado. The instantaneous center of the tornado was estimated from TTU-Kal radar data.", "ts_dict_index": [14718, 14719, 14720]}
+{"event_id": 818899, "event_type": "Tornado", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-05-08 14:19:00", "end_date_time": "2019-05-08 14:20:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in several reports of tornadoes, with two separate tracks found across Northern Harrison and extreme Northeast Panola Counties, before the storms moved into North Louisiana by mid-afternoon. Locally heavy rainfall from the stronger storms within a short period of time also resulted in localized flash flooding across portions of Cass County, with flash flooding also reported across Eastern Harrison and Panola Counties during the early morning hours on May 9th as additional showers and thunderstorms redeveloped and moved repeatedly over the same areas. During the evening hours on the 9th, isolated severe thunderstorms developed over portions of Deep East Texas along old outflow boundaries from the storms earlier in the day. These storms produced large hail in extreme Southern Sabine County and Central Nacogdoches County before diminishing by midnight. An EF-1 tornado with maximum estimated winds near 100 mph touched down along Highway 79 in Bethany, Texas in the far northeast section of Panola County, where it snapped and uprooted several trees and removed the roofing of a service station along Highway 79 before crossing over into Caddo Parish in Northwest Louisiana. The estimated winds of the tornado shortly after it touched down in Panola County was near 90 mph before the winds increased as it moved into the Louisiana side of Bethany in Caddo Parish.", "ts_dict_index": [14706, 14707, 14708]}
+{"event_id": 818896, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-05-08 13:36:00", "end_date_time": "2019-05-08 13:45:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in several reports of tornadoes, with two separate tracks found across Northern Harrison and extreme Northeast Panola Counties, before the storms moved into North Louisiana by mid-afternoon. Locally heavy rainfall from the stronger storms within a short period of time also resulted in localized flash flooding across portions of Cass County, with flash flooding also reported across Eastern Harrison and Panola Counties during the early morning hours on May 9th as additional showers and thunderstorms redeveloped and moved repeatedly over the same areas. During the evening hours on the 9th, isolated severe thunderstorms developed over portions of Deep East Texas along old outflow boundaries from the storms earlier in the day. These storms produced large hail in extreme Southern Sabine County and Central Nacogdoches County before diminishing by midnight. An EF-1 tornado with maximum estimated winds around 105 mph developed within a squall line of thunderstorms that produced sporadic straight line wind damage mainly to trees across Northern Harrison County. The tornado touched down a few miles west of Highway 59 on FM 1997, tracking east across County Road 4000 where several trees were snapped and uprooted.  As the tornado crossed Highway 59 along the north side of Suburban Acres Road, numerous hardwood trees were snapped with a few homes receiving roof damage due to trees or large limbs falling on the structures. The tornado continued to uproot and snap several more trees before crossing County Road 2012, and lifting shortly thereafter.", "ts_dict_index": [14709, 14710, 14711]}
+{"event_id": 1064054, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "JACKSON", "begin_date_time": "2023-01-02 16:46:00", "end_date_time": "2023-01-02 17:09:00", "narrative": "A vigorous upper level trough traversed east through the Desert Southwest and into the Southern Rockies January 1st, before ejecting northeast across the Texas/Oklahoma Panhandles into Western Kansas on the 2nd. In advance of this trough, rich low level moisture quickly spread northward from the Gulf of Mexico across East Texas, North Louisiana, and Southern Arkansas, along a strong southerly low level jet that developed ahead of a deepening surface low over Southeast Colorado and Western Kansas. With the trough taking on a more negative tilt as it ejected northeast across the Panhandle region, a dryline mixed east to the I-35 corridor of North-central Texas by early evening, and into East Texas and Eastern Oklahoma during the evening and overnight hours. Large scale forcing increased well ahead of the approaching upper trough across the expanding moist sector from the late morning through the afternoon and evening hours of the 2nd, with scattered to numerous showers and thunderstorms developing across portions of Deep East Texas, North Louisiana, and Southern Arkansas. Increasing instability due to diurnal heating within a strongly sheared and moist air mass resulted in the gradual development of strong to severe thunderstorms across these areas, with locally heavy rain falling over areas where the storms moved repeatedly over the same areas. Rainfall amounts ranged from 1-3 inches across much of North Louisiana, with isolated higher totals of 5-6+ inches observed Eastern Bienville, much of Jackson, Western Ouachita, and Eastern Union Parishes. This resulted in areas of flash flooding across portions of North Louisiana from the mid-afternoon through the early morning hours on the 3rd, with sporadic reports of damaging winds and isolated tornadoes across the region as well. An EF-2 tornado with estimated maximum winds near 120 mph touched down just north of the Jackson/Winn Parish line along Highway 167 and moved northeast across Firetower Section Road and Highway 147/Walker Road, where numerous trees were snapped. On Walker Road, the tornado caused roof damage to a chicken house and some manufactured homes. The most significant damage on Walker Road occurred just north of its intersection with Whitman Road where a single-wide manufactured home, which was anchored into the ground, was flipped and rolled off of its foundation, destroying most of its roof and walls, but leaving the undercarriage attached. The tornado snapped and uprooted more trees and broke a wooden electrical pole as it crossed Rome Road, Highway 4, and Strain Allen Road. On Strain Allen Road, a very large hardwood tree was snapped and a home suffered the partial loss of its metal roof. More broken limbs and snapped trunks were observed as the tornado crossed Halfway Creek and travelled north-northeast along Kelley Road. The most significant damage along the entire tornado track occurred as it crossed Highway 811/Gladway Road near its intersection with Kelley Road. Here, a brick single-family home lost most of its roof. This caused the partial failure of the walls of the garage of the home, but the majority of the home remained standing and intact. A metal garage building on this property suffered a complete loss of its walls, but most of its roof and the metal frame poles remained standing. About 150 yards to the northwest, another brick single-family home suffered almost a total loss of its roof covering. The damage in this area was rated as EF-2 based mainly on the roof loss to the two homes. On the north side of Gladway Road, a double-wide manufactured home suffered the loss of most of its roof, but the walls remained standing. An attached carport on another single-family brick residence was destroyed as the tornado continued north of Gladway Road and west of Kelley Road. This tornado continued to snap numerous trees on Kelley Road as it continued northward crossing Slash Pine Road and again crossing Kelley Road and Parish Barn Road. More tree damage was observed along Lucy-Leonard Road and Highway 155. Two brick single-family homes on Highway 155 just west of Sugar Creek suffered some loss of shingles from the roof. The tornado began to weaken rapidly and caused more minor roof damage to a single-family home and snapped some large tree branches along Stonewall Road before finally lifting. Three minor injuries were reported from this tornado, but their exact locations were not available to the survey team.", "ts_dict_index": [14715, 14716, 14717]}
+{"event_id": 994712, "event_type": "Tornado", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2021-12-15 19:03:00", "end_date_time": "2021-12-15 19:05:00", "narrative": "A low pressure system of historic strength led to a variety of high-end weather impacts from the central plains to the Upper Midwest and Great Lakes December 15-16. An unprecedented December severe weather unfolded over portions of Minnesota and Wisconsin Wednesday evening, with the Storm Prediction Center issuing their farthest-north Moderate Risk for the Month of December. A serial derecho moving at 60-70 mph tracked from Kansas to Wisconsin, resulting in over 400 reports of damaging wind and numerous tornadoes. Most of the damage across our area occurred from south-central Minnesota through west-central Wisconsin. The strongest tornado damage occurred in Hartland.||Before the thunderstorms, strong southerly winds led to record high temperature at many sites across the Upper Midwest. Temperatures warmed into the mid to upper 50s across much of central Minnesota and western Wisconsin, and even exceeded 60 degrees across southern Minnesota. The warm temperatures melted what was left of the snowpack from the December 10 winter storm, which led to widespread dense fog through much of the morning and afternoon.||After the thunderstorms, strong gradient winds and widespread wind gusts in excess of 50 mph developed for several hours late Wednesday night and into the overnight hours. The Redwood Falls airport measured a gust of 78 mph at 11:30 PM.||Temperatures quickly fell below freezing across western and central Minnesota Wednesday night, causing rain to change over to a wintry mix of freezing drizzle and snow. Snowfall accumulations of 1-4 inches, along with the strong gusty winds, led to low visibility and travel hazards late Wednesday night into Thursday morning. This tornado developed to the east of Alden, damaging trees and a large building that housed farm equipment. It then continued to the northeast, damaging additional trees before dissipating in a field.", "ts_dict_index": [14730, 14731, 14732]}
+{"event_id": 866536, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CHEROKEE", "begin_date_time": "2020-01-10 23:21:00", "end_date_time": "2020-01-10 23:22:00", "narrative": "An upper level longwave trough emerged out of the Intermountain West and into the Central and Southern Plains during the daytime and evening hours of January 10th. A strong southerly return flow commenced out ahead of the trough during the 8th-9th, allowing for unseasonably warm and humid conditions to advance northward across Southern Oklahoma, much of Central and Eastern Texas, as well as Louisiana, Arkansas, and the Lower Mississippi Valley. Meanwhile, an intensifying surface low pressure system and associated dry line developed along the Red River of North Texas into Southern Oklahoma during the afternoon hours, which spread east northeast across the Ark-La-Tex during the early morning hours on January 11th. With afternoon temperatures climbing into the mid 70s ahead of this trough, moderate instability developed across the broad warm sector, with very strong wind shear in place as large scale forcing increased ahead of the trough axis across East Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana. Thus, an axis of strong to severe showers and thunderstorms developed during the evening hours across Southeast Oklahoma, adjacent sections of Southwest Arkansas and East Texas, which advanced east into North Louisiana during the early morning hours of the 11th. Damaging winds downed trees and power lines across portions of East Texas, with even multiple tornadoes touching down along the line of severe thunderstorms. Unfortunately, a man  was killed when a tornado touched down west of Nacogdoches and a tree fell on his mobile home. These storms also produced locally heavy rainfall, with amounts of one to three inches, with isolated higher amounts up to four inches recorded across much of this area, resulting in isolated instances of flash flooding. These storms continued to intensify during the late evening and early morning hours as they moved into extreme Eastern Texas and Western Louisiana, producing more in the way of widespread wind damage and isolated tornadoes. An EF-1 tornado, with estimated maximum winds near 105 mph, touched down on a farm off of County Road 1619, uprooting several trees. It also broke windows and partially damaged the roof of a home before it destroyed a shed and damaged the roofs of two more homes. The tornado crossed Highway 69 and continued to uproot trees and damage the roofs of two homes before lifting along County Road 1501.", "ts_dict_index": [14646, 14647, 14648]}
+{"event_id": 1115322, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2023-06-16 00:20:00", "end_date_time": "2023-06-16 00:25:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. A strong line of thunderstorms moved through East Texas and Northwest Louisiana during the early morning hours on June 16th. As it moved through East Texas and into the Shreveport metro area, the storm begin to take on a bow shape, indicating that the system would likely produce strong straight line winds. As the storm reached near the Texas/Louisiana state line from Panola County into southwest Caddo Parish, it produced a brief EF-1 tornado with maximum wind gusts of 110 mph, a path width of nearly 850 yards, and path length of nearly six miles in far southwest Caddo Parish. ||With a storm already producing widespread straight-line wind damage, it became difficult to determine what was tornadic and what was straight-line winds. It was determined that the tornado touched down to the west of County Road 322 in Panola County where a large tree fell onto a single family home. The tornado then moved to the southeast across the Texas/Louisiana state line towards Johns Gin Road where it produced widespread tree damage all along Johns Gin Road north of Keatchie Marshall Road. From there, the tornado moved through a neighborhood to the west of Four |Forks Road just north of Keatchie Marshall Road where a number of trees were either uprooted or snapped. This same area was just struck by a tragic tornado in December 2022. The tornado then tracked to the southeast along Keatchie Marshall Road where damage became more sparse and then lifted just to the west of Preston Road.", "ts_dict_index": [14763, 14764, 14765]}
+{"event_id": 953091, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HOCKLEY", "begin_date_time": "2021-05-17 18:50:00", "end_date_time": "2021-05-17 18:51:00", "narrative": "A widespread severe thunderstorm event occurred on the afternoon and evening of the 17th. Thunderstorms initially formed along a dryline near the Texas/New Mexico state line and along an outflow boundary from previous day storms. The ample instability was complemented by large scale lift moving overhead from an upper level jet moving into the southern High Plains. Very intense supercells developed across the entirety of the South Plains, Rolling Plains, and extreme southern Texas Panhandle due to the abundant amount of unstable air. Several supercells produced hail up to baseball size as they slowly moved across the region. One particularly robust rotating storm developed over Hockley County and moved eastward into Lubbock County and through the city of Lubbock. This storm developed several funnel clouds and a brief tornado in far eastern Hockley County. The low level circulation moved directly over the southern portion of the city of Lubbock but did not produce any additional tornadoes. Decaying thunderstorms also produced two high wind gusts. These high wind gusts were measured by the Texas Tech University West Texas mesonet at Friona (Parmer County) 64 mph and Lesley (Hall County) 59 mph. Lastly, thunderstorms repeatedly formed over central Bailey County causing flash flooding along Farm to Market Road 746 west of Texas Highway 214.||In the early morning hours of the 18th, stratiform precipitation from decaying thunderstorms produced two high wind gusts. One near Graham of 62 mph and the other near Hackberry (Cottle County) of 59 mph. Both of these reports came from the Texas Tech University West Texas mesonet. Numerous reports of a funnel cloud and a brief touchdown were received on a supercell just west of Wolfforth. The tornado briefly touched down in an open field in Hockley County just west of the Lubbock/Hockley County line. No damage was known from this tornado, therefore, a rating of EF-Unknown was assigned.", "ts_dict_index": [14757, 14758, 14759]}
+{"event_id": 1084582, "event_type": "Tornado", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2023-03-02 21:05:00", "end_date_time": "2023-03-02 21:11:00", "narrative": "A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 1st and through March 2nd. Strong warm and moist air advection was ongoing in advance of the trough preceding the event. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. This environment produced an isolated strong thunderstorm that produced nickel size hail just south of Haworth on the 1st. A potent upper-level trough progressed from the Four-Corners Region into the Texas Panhandle by late in the afternoon on March 2nd. Strong warm and moist air advection was ongoing in advance of the trough earlier in the morning. This resulted in scattered convection, but this had little effect on increasing instability through the afternoon as temperatures warmed into the mid and upper 70s to lower and mid 80s. Additionally, backing surface winds also promoted increasing low-level shear as well as deep-layer shear with a 50-60 knot low-level jet surging east ahead of the trough and advancing cold front. This environment was supportive of several supercells that developed by late afternoon into the early evening hours, producing an isolated tornado in addition to large hail and damaging wind gusts Across McCurtain County Oklahoma. As the cold front surged east of I-35 by early in the evening, the storm mode eventually became more linear with an increasing threat of more widespread damaging winds along the complex of storms while the threat of large hail also continued through the end of the event. An EF1 tornado embedded within a quasi-linear convective system, or squall line, began west of Broken Bow along Poppy Road and proceeded to advance nearly 5 miles northwest and then north of the city before lifting as it crossed Highway 259. Most the damage was in the form of uprooted trees lying to the north or northeast, but some trees were lying to the northwest. This fact, in combination with signs of convergence in the damage pattern, was enough to give confidence in categorizing this as a tornado. The highest winds estimated in the 90 to 100 mph range, and the maximum width of nearly 400 yards, was in the vicinity of where the tornado crossed Highway 3. A few structures were damaged in this tornado, but mainly due to falling trees.", "ts_dict_index": [14754, 14755, 14756]}
+{"event_id": 1115312, "event_type": "Tornado", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2023-06-16 00:15:00", "end_date_time": "2023-06-16 00:20:00", "narrative": "Late during the evening of June 15th, regional radar analysis showed several clusters of severe thunderstorms ongoing along the middle Red River Valley into Northeast Texas. The eastern-most cluster displayed signs of cold pool intensification and developed a bowing structure. Observational trends farther downstream favored a continued motion along the instability gradient to the southeast through midnight into the early morning hours on June 16th. Given that the background wind fields and buoyancy were still quite strong, the threat of damaging winds upwards of 75+ mph and large hail increased as the complex moved into far Northeast Texas and Northwest Louisiana just after midnight.||Farther west near the Red River, additional storm development occurred along the trailing outflow. Less organized than the eastern cluster, individual storms, including a few supercells, eventually evolved and remained semi-discrete for a few hours. Given the more cellular nature, large hail was a threat initially with the amount of instability upwards of 5000 J/kg and 60 knots of effective shear. A greater risk of damaging winds gradually evolved as storms remained organized and grew upscale overnight.||As a result, large hail up to 2+ inches in diameter eventually occurred in some storms followed by an intense bow echo, resulting in widespread severe winds and even some hurricane-force gusts, setting the stage for initiating a derecho-type event across much of Northeast Texas and North Louisiana. In addition, an isolated tornado also occurred near the Texas/Louisiana state line on the south flank of the extreme derecho winds. A strong line of thunderstorms moved through East Texas and Northwest Louisiana during the early morning hours on June 16th. As it moved through East Texas and into the Shreveport metro area, the storm begin to take on a bow shape, indicating that the system would likely produce strong straight line winds. As the storm reached near the Texas/Louisiana state line from Panola County into southwest Caddo Parish, it produced a brief EF-1 tornado with maximum wind gusts of 110 mph, a path width of nearly 850 yards, and path length of nearly two miles in far eastern Panola County. ||With a storm already producing widespread straight-line wind damage, it became difficult to determine what was tornadic and what was straight-line winds. It was determined that the tornado touched down to the west of County Road 322 in Panola County where a large tree fell onto a single family home. The tornado then moved to the southeast across the Texas/Louisiana state line into extreme Southwest Caddo Parish.", "ts_dict_index": [14760, 14761, 14762]}
+{"event_id": 994717, "event_type": "Tornado", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2021-12-15 19:10:00", "end_date_time": "2021-12-15 19:13:00", "narrative": "A low pressure system of historic strength led to a variety of high-end weather impacts from the central plains to the Upper Midwest and Great Lakes December 15-16. An unprecedented December severe weather unfolded over portions of Minnesota and Wisconsin Wednesday evening, with the Storm Prediction Center issuing their farthest-north Moderate Risk for the Month of December. A serial derecho moving at 60-70 mph tracked from Kansas to Wisconsin, resulting in over 400 reports of damaging wind and numerous tornadoes. Most of the damage across our area occurred from south-central Minnesota through west-central Wisconsin. The strongest tornado damage occurred in Hartland.||Before the thunderstorms, strong southerly winds led to record high temperature at many sites across the Upper Midwest. Temperatures warmed into the mid to upper 50s across much of central Minnesota and western Wisconsin, and even exceeded 60 degrees across southern Minnesota. The warm temperatures melted what was left of the snowpack from the December 10 winter storm, which led to widespread dense fog through much of the morning and afternoon.||After the thunderstorms, strong gradient winds and widespread wind gusts in excess of 50 mph developed for several hours late Wednesday night and into the overnight hours. The Redwood Falls airport measured a gust of 78 mph at 11:30 PM.||Temperatures quickly fell below freezing across western and central Minnesota Wednesday night, causing rain to change over to a wintry mix of freezing drizzle and snow. Snowfall accumulations of 1-4 inches, along with the strong gusty winds, led to low visibility and travel hazards late Wednesday night into Thursday morning. A brief tornado occurred south of Glenville. It spun up around 782nd Ave and tracked northeast producing some tree damage until it reached 795th Ave. There, it damaged farm buildings and tossed hay bales across the road.", "ts_dict_index": [14739, 14740, 14741]}
+{"event_id": 994718, "event_type": "Tornado", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2021-12-15 19:15:00", "end_date_time": "2021-12-15 19:21:00", "narrative": "A low pressure system of historic strength led to a variety of high-end weather impacts from the central plains to the Upper Midwest and Great Lakes December 15-16. An unprecedented December severe weather unfolded over portions of Minnesota and Wisconsin Wednesday evening, with the Storm Prediction Center issuing their farthest-north Moderate Risk for the Month of December. A serial derecho moving at 60-70 mph tracked from Kansas to Wisconsin, resulting in over 400 reports of damaging wind and numerous tornadoes. Most of the damage across our area occurred from south-central Minnesota through west-central Wisconsin. The strongest tornado damage occurred in Hartland.||Before the thunderstorms, strong southerly winds led to record high temperature at many sites across the Upper Midwest. Temperatures warmed into the mid to upper 50s across much of central Minnesota and western Wisconsin, and even exceeded 60 degrees across southern Minnesota. The warm temperatures melted what was left of the snowpack from the December 10 winter storm, which led to widespread dense fog through much of the morning and afternoon.||After the thunderstorms, strong gradient winds and widespread wind gusts in excess of 50 mph developed for several hours late Wednesday night and into the overnight hours. The Redwood Falls airport measured a gust of 78 mph at 11:30 PM.||Temperatures quickly fell below freezing across western and central Minnesota Wednesday night, causing rain to change over to a wintry mix of freezing drizzle and snow. Snowfall accumulations of 1-4 inches, along with the strong gusty winds, led to low visibility and travel hazards late Wednesday night into Thursday morning. This tornado hit several farmsteads, partially removing the roofs of several outbuildings and a turkey barn. It dented a silo. Trees fell on a number of sheds and vehicles.", "ts_dict_index": [14736, 14737, 14738]}
+{"event_id": 994716, "event_type": "Tornado", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2021-12-15 19:10:00", "end_date_time": "2021-12-15 19:11:00", "narrative": "A low pressure system of historic strength led to a variety of high-end weather impacts from the central plains to the Upper Midwest and Great Lakes December 15-16. An unprecedented December severe weather unfolded over portions of Minnesota and Wisconsin Wednesday evening, with the Storm Prediction Center issuing their farthest-north Moderate Risk for the Month of December. A serial derecho moving at 60-70 mph tracked from Kansas to Wisconsin, resulting in over 400 reports of damaging wind and numerous tornadoes. Most of the damage across our area occurred from south-central Minnesota through west-central Wisconsin. The strongest tornado damage occurred in Hartland.||Before the thunderstorms, strong southerly winds led to record high temperature at many sites across the Upper Midwest. Temperatures warmed into the mid to upper 50s across much of central Minnesota and western Wisconsin, and even exceeded 60 degrees across southern Minnesota. The warm temperatures melted what was left of the snowpack from the December 10 winter storm, which led to widespread dense fog through much of the morning and afternoon.||After the thunderstorms, strong gradient winds and widespread wind gusts in excess of 50 mph developed for several hours late Wednesday night and into the overnight hours. The Redwood Falls airport measured a gust of 78 mph at 11:30 PM.||Temperatures quickly fell below freezing across western and central Minnesota Wednesday night, causing rain to change over to a wintry mix of freezing drizzle and snow. Snowfall accumulations of 1-4 inches, along with the strong gusty winds, led to low visibility and travel hazards late Wednesday night into Thursday morning. This tornado developed in Worth County Iowa along 500th Street, initially producing some tree damage (see separate entry from NWS Des Moines).  As it crossed into Freeborn County Minnesota, it displaced and destroyed an empty silo on State Line Road. It then destroyed a cattle barn and a pole crashed through a car. The tornado then continued to produce mostly minor tree damage and moved northeast into southwestern Mower County (see separate entry from NWS La Crosse).", "ts_dict_index": [14742, 14743, 14744]}
+{"event_id": 994711, "event_type": "Tornado", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2021-12-15 18:58:00", "end_date_time": "2021-12-15 19:01:00", "narrative": "A low pressure system of historic strength led to a variety of high-end weather impacts from the central plains to the Upper Midwest and Great Lakes December 15-16. An unprecedented December severe weather unfolded over portions of Minnesota and Wisconsin Wednesday evening, with the Storm Prediction Center issuing their farthest-north Moderate Risk for the Month of December. A serial derecho moving at 60-70 mph tracked from Kansas to Wisconsin, resulting in over 400 reports of damaging wind and numerous tornadoes. Most of the damage across our area occurred from south-central Minnesota through west-central Wisconsin. The strongest tornado damage occurred in Hartland.||Before the thunderstorms, strong southerly winds led to record high temperature at many sites across the Upper Midwest. Temperatures warmed into the mid to upper 50s across much of central Minnesota and western Wisconsin, and even exceeded 60 degrees across southern Minnesota. The warm temperatures melted what was left of the snowpack from the December 10 winter storm, which led to widespread dense fog through much of the morning and afternoon.||After the thunderstorms, strong gradient winds and widespread wind gusts in excess of 50 mph developed for several hours late Wednesday night and into the overnight hours. The Redwood Falls airport measured a gust of 78 mph at 11:30 PM.||Temperatures quickly fell below freezing across western and central Minnesota Wednesday night, causing rain to change over to a wintry mix of freezing drizzle and snow. Snowfall accumulations of 1-4 inches, along with the strong gusty winds, led to low visibility and travel hazards late Wednesday night into Thursday morning. The first damage observed was a bent road sign near the tornado origin point. A path of tree and utility pole damage continued to the northeast before ending just south of I-90. Several trees were uprooted.", "ts_dict_index": [14751, 14752, 14753]}
+{"event_id": 994714, "event_type": "Tornado", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2021-12-15 19:10:00", "end_date_time": "2021-12-15 19:15:00", "narrative": "A low pressure system of historic strength led to a variety of high-end weather impacts from the central plains to the Upper Midwest and Great Lakes December 15-16. An unprecedented December severe weather unfolded over portions of Minnesota and Wisconsin Wednesday evening, with the Storm Prediction Center issuing their farthest-north Moderate Risk for the Month of December. A serial derecho moving at 60-70 mph tracked from Kansas to Wisconsin, resulting in over 400 reports of damaging wind and numerous tornadoes. Most of the damage across our area occurred from south-central Minnesota through west-central Wisconsin. The strongest tornado damage occurred in Hartland.||Before the thunderstorms, strong southerly winds led to record high temperature at many sites across the Upper Midwest. Temperatures warmed into the mid to upper 50s across much of central Minnesota and western Wisconsin, and even exceeded 60 degrees across southern Minnesota. The warm temperatures melted what was left of the snowpack from the December 10 winter storm, which led to widespread dense fog through much of the morning and afternoon.||After the thunderstorms, strong gradient winds and widespread wind gusts in excess of 50 mph developed for several hours late Wednesday night and into the overnight hours. The Redwood Falls airport measured a gust of 78 mph at 11:30 PM.||Temperatures quickly fell below freezing across western and central Minnesota Wednesday night, causing rain to change over to a wintry mix of freezing drizzle and snow. Snowfall accumulations of 1-4 inches, along with the strong gusty winds, led to low visibility and travel hazards late Wednesday night into Thursday morning. This tornado hit several farms, including one where seven buildings had enough damage so they will be totaled. Several windows of a house were blown out. A machine shed at another farm had several pillars of a large machine shed pulled out of the ground. At the end of the tornado, a home had many shingles removed.", "ts_dict_index": [14748, 14749, 14750]}
+{"event_id": 1108825, "event_type": "Tornado", "state": "COLORADO", "cz_name": "WASHINGTON", "begin_date_time": "2023-06-21 17:16:00", "end_date_time": "2023-06-21 17:22:00", "narrative": "Long duration severe weather event across the northeast plains, and most of the Denver metropolitan area beginning during the early afternoon hours.   Scores of  tornadoes occurred across Washington and Logan counties.  Several rounds of hail across the Denver metro, with ping pong ball sized hail in downtown, larger hail up to 2 inches in diameter at concert in Red Rocks Amphitheatre.  In all, seven patrons were hospitalized,  with 83 treated on scene.   A substantial number of attendees suffered welts, bruises and broken fingers trying to protect themselves.  Several suffered concussions as well.  A total of 33 tornadoes touched down in Washington County, with 3 reported in Logan County.  There were reports of at least one home damaged west of Sterling and one commercial building collapse in Sterling. The home was damaged by one of the tornadoes.||Significant flooding and flash flooding also occurred in portions of the plains, including Elbert, Arapahoe, Adams, Logan, Washington and Morgan counties. There were likely several rural roads that flooded due to the heavy rainfall.  There was a flood fatality just south of I-70 along Watkins Rd.  First responders found two stranded cars swept into a field, but its occupants had either gotten out or had been rescued. The third vehicle ended up west of Watkins and 6th Ave. in what is normally a dry creek bed. South Metro���s water rescue team was then called out to do a water rescue but that operation turned into a recovery by the following morning.  Due to flooding, Watkins Road was closed between Interstate 70 and Jewell Ave.  Interstate 70 was also closed for several hours until water could recede from flooded underpasses. Minor flooding also occurred in portions of the Denver and the surrounding metro area.  Baseball size hail was observed in Washington County.  In Clear Creek County, a thunderstorm wind gusts to 68 mph was recorded. A large multi-vortex tornado snapped power poles.", "ts_dict_index": [14703, 14704, 14705]}
+{"event_id": 1007735, "event_type": "Tornado", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2022-03-31 20:48:00", "end_date_time": "2022-03-31 20:52:00", "narrative": "A warm front moved through the mid-Atlantic on the morning hours of March 31. This was associated with a strong area of low pressure moving through the Great Lakes, which had brought widespread severe weather to the Southeast US in prior days. Behind the warm front, widespread cloud cover and scattered showers lingered for most of the day over the eastern mid-Atlantic. Despite temperatures that still warmed to above average values, this greatly limited instability. However, more sunshine and subsequent instability developed further west over central Pennsylvania and northern Maryland. As a cold front approached by late afternoon, forcing for ascent increased, and strong wind fields were in place across the region in the warm sector of the Great Lakes low. Widespread convection developed over the interior mid-Atlantic, some of which became strong to severe. Convection generally favored a linear evolution with some embedded supercell structures. Because of the orientation of mid and upper level winds and the decreasing instability to the east, thunderstorms were very slow to move east and gradually lost intensity with time. In the local area, reports of severe weather were mostly isolated and confined to eastern Pennsylvania. However, a short-lived EF1 tornado did touch down over Bucks County, producing a 2 mile path of tree, utility, and some structural damage. Shower and thunderstorm activity continued through much of the night, slowly making its way to the coast, but was well below severe limits over New Jersey and Delmarva in the later hours of the night. A tornado began in Hilltown Township along Souderton Road about a |half mile west of Route 313/Dublin Pike. The tornado continued to |the northeast along Souderton Road where it uprooted and snapped |numerous trees and also caused primarily cosmetic damage to a few |homes. The CVS Pharmacy at the intersection of Souderton Road and |Route 313 also sustained minor cosmetic damage, including the front |door being blown out. Also near this intersection, a home sustained |minor cosmetic damage and a number of trees were uprooted and |snapped where the tornado crossed into Bedminster Township. The |tornado continued northeast along Bedminster Road weakening |somewhat, but still uprooting and snapping several trees and causing |cosmetic damage to some homes, especially near the intersection of |Bucks Road.||The tornado continued northeast toward Elephant Road while |continuing to cause mainly sporadic tree damage, including uprooting |several trees in front of a home. The tornado passed over the |Bedminster Municipal Authority complex, where it blew off roof |shingles from several well constructed buildings and uprooted a few |small trees nearby. The tornado crossed Elephant Road about 700 feet |south of Irish Meetinghouse Road where it caused some more |substantial tree damage. At least a dozen or more healthy trees were |uprooted or snapped along a driveway, one of which fell onto a |parked vehicle. The home on this property sustained minor cosmetic |damage and had some roof shingles blown off. The tornado then |continued into a wooded area with homes paralleling Irish |Meetinghouse Road where the tree damage became more sporadic once |again, and no additional structural damage was noted. The tornado |then crossed just north of Irish Meetinghouse Road where it uprooted |a few small trees in an open field then dissipated.||No known injuries or fatalities occurred from this tornado.", "ts_dict_index": [14787, 14788, 14789]}
+{"event_id": 1014828, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-12 20:55:00", "end_date_time": "2022-04-12 20:56:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. An EF-0 tornado with estimated maximum winds near 85 mph embedded within a quasi-linear convective system (QLCS) touched down along Sophia Lane and Brunswick Drive in Southeast Shreveport. There, large branches of hardwood and softwood trees were broken and twisted off. The tornado then damaged a food stand as it crossed Youree Drive, while also damaging large branches and uprooting a couple of trees. Minor shingle damage to single family homes adjacent to LSU-Shreveport also resulted from this tornado, before tracking across the LSU-S campus, uprooting trees and downing large branches. The tornado also damaged the soccer and baseball fields at LSU-S before crossing East Kings Highway and the Red River into Western Bossier Parish.", "ts_dict_index": [14784, 14785, 14786]}
+{"event_id": 1014823, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-12 20:54:00", "end_date_time": "2022-04-12 20:55:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. An EF-0 tornado with estimated maximum winds around 80 mph which was embedded in a quasi-linear convective system (QLCS) touched down on a farm to the northwest of Blanchard in Caddo Parish. A center pivot irrigation system was flipped by the tornado as it crossed an open field. The tornado then snapped tree limbs before partially removing the roofs of four metal farm buildings along Sentell Road. The tornado then crossed the Red River into Bossier Parish. It should be noted that while the tornado was an EF-0 in Caddo Parish, it did intensify into an EF-1 with estimated maximum winds around 110 mph after it entered Bossier Parish.", "ts_dict_index": [14775, 14776, 14777]}
+{"event_id": 1014825, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2022-04-12 20:55:00", "end_date_time": "2022-04-12 20:57:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. This is a continuation of the Caddo Parish tornado. This tornado intensified to an EF-1 with estimated maximum winds near 110 mph as it moved over a heavily wooded area near and just south of Willow Bend Road northwest of Benton, where it snapped and uprooted hardwood and softwood trees. The most intense damage was to a guest house which was shifted off of its foundation and destroyed. The tornado continued on to remove a large portion of the roof of a two-story single family home. Two children on the second story of the home were saved by their father who got the Tornado Warning via a Wireless Emergency Alert (WEA) on his wireless phone, and then moved them to a tornado shelter in the center of the home on the first floor. The tornado continued on to damage another single family home and then cross Old Plain Dealing Road. After crossing Old Plain Dealing Road, the tornado removed the roof of a small metal outbuilding and snapped/uprooted several more hardwood and softwood trees before moving into a forested area and lifting.", "ts_dict_index": [14778, 14779, 14780]}
+{"event_id": 1014836, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-04-12 20:57:00", "end_date_time": "2022-04-12 20:58:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. An EF-0 tornado with estimated maximum winds near 80 mph that was embedded within a quasi-linear convective system (QLCS), briefly touched down along Hosston Rodessa Road just north of the Hosston city limits, where it twisted and broke off small and large hardwood tree branches. The tornado continued to down additional tree branches along Christian Street, before lifting as it crossed Highway 71.", "ts_dict_index": [14766, 14767, 14768]}
+{"event_id": 1014835, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2022-04-12 20:56:00", "end_date_time": "2022-04-12 21:04:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. The is a continuation of the Eastern Caddo Parish (Southeast Shreveport) EF-0 tornado. This tornado maintained its intensity with estimated maximum winds near 85 mph as it crossed over into South Bossier City in Bossier Parish, where it continued to uproot trees and down/twist large tree branches. It also uprooted trees which split at least three manufactured homes off of Alfred Lane as they fell and damaged several others. The tornado continued on to General Ewell Drive, and then moved over a forested area on Barksdale Air Force Base. Personnel from Barksdale Air Force Base relayed that trees were uprooted and that large tree branches were broken via pictures as the tornado crossed the southern and eastern forested portions of the base. Beyond Barksdale Air Force Base, only thunderstorm wind damage was found off of Union Texas Road and Academy Lane by Haughton Elementary School in Haughton.", "ts_dict_index": [14781, 14782, 14783]}
+{"event_id": 1014596, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "OUACHITA", "begin_date_time": "2022-04-12 17:34:00", "end_date_time": "2022-04-12 17:39:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. A brief EF-1 tornado with estimated maximum winds near 110 mph touched down in the Swartz community near Woodmont Drive, where it tracked just east of due north for around two and a half miles over a largely residential area. Direct damage was primarily to trees, although many structures and homes were damaged due to falling trees and tree limbs. The tree damage was near the EF-0 to EF-1 threshold for most of the track, with many more uproots and trunk snaps. However, near the end of the tornado along and north of Highway 139, the level of tree damage indicated a strengthening of the tornado, in particular along Trichel Lane. It was near the end of this road that approximately one hundred trees were snapped and uprooted, warranting a peak wind speed estimate of 110 mph, which is a high-end EF-1 on the Enhanced Fujita Scale. Unfortunately, one of these trees destroyed a mobile home and a resident inside was injured, but not critically.", "ts_dict_index": [14772, 14773, 14774]}
+{"event_id": 1014843, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "BIENVILLE", "begin_date_time": "2022-04-12 21:23:00", "end_date_time": "2022-04-12 21:34:00", "narrative": "A large upper trough dug through the Southern Plains during the afternoon and overnight hours on April 12th-13th, allowing the dry line to mix east into Central Texas. Large scale forcing increased along the dry line across Central Texas during the late afternoon through the evening, as these storms tapped moderate instability and increasing wind shear ahead of this system. In fact, isolated showers and a few thunderstorms developed during the mid and late afternoon across portions of Northeast Louisiana, with one storm spawning a brief tornado over Northeast Ouachita Parish near the Swartz community. These storms over Central Texas eventually developed in a quasi-linear convection system (QLCS), as they became severe and accelerated east across much of East Texas and North Louisiana during the evening through the early morning hours of the 12th-13th. Instances of damaging winds were reported from these storms, downing numerous trees and power lines, and even spawning isolated tornadoes as well. While these storms exited the region prior to daybreak on the 13th, additional showers and thunderstorms developed along the associated cold front across East Texas during the mid and late morning of the 13th, before spreading into North Louisiana during the peak heating of the afternoon. Thus, adequate instability developed such that some of these storms again became severe, producing instances of damaging winds over portions of North Louisiana and an isolated tornado over Eastern Winn/Western Caldwell Parishes. These storms finally exited North Louisiana during the late afternoon hours of the 13th. An EF-1 tornado with estimated maximum winds near 100 mph touched down in a wooded area west of Layfield Road west of Castor, and tracked northeast across Highway 4, snapping and uprooting numerous trees along its path. One area of maximum winds was found in an open field just west of Layfield Road where 10-11 wooden power poles were snapped just west of Highway 4. The tornado continued northeast across Highway 792 north of Castor, where it tracked along and just north of Ayers Road and across a logging camp, where a second area of maximum winds were found on Kepler Road just north of Ayers Road. The tornado continued to track northeast over a heavily wooded area inaccessible by vehicle, but dopplar radar indicated a tornadic debris signature north of Highway 4 and west of Highway 9. The tornado lifted prior to reaching Highway 9 and the community of Bienville, although straight line winds estimated to be near 90 mph were found here as numerous trees were snapped and uprooted, but all lying in a northeasterly direction.", "ts_dict_index": [14769, 14770, 14771]}
+{"event_id": 994713, "event_type": "Tornado", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2021-12-15 19:11:00", "end_date_time": "2021-12-15 19:13:00", "narrative": "A low pressure system of historic strength led to a variety of high-end weather impacts from the central plains to the Upper Midwest and Great Lakes December 15-16. An unprecedented December severe weather unfolded over portions of Minnesota and Wisconsin Wednesday evening, with the Storm Prediction Center issuing their farthest-north Moderate Risk for the Month of December. A serial derecho moving at 60-70 mph tracked from Kansas to Wisconsin, resulting in over 400 reports of damaging wind and numerous tornadoes. Most of the damage across our area occurred from south-central Minnesota through west-central Wisconsin. The strongest tornado damage occurred in Hartland.||Before the thunderstorms, strong southerly winds led to record high temperature at many sites across the Upper Midwest. Temperatures warmed into the mid to upper 50s across much of central Minnesota and western Wisconsin, and even exceeded 60 degrees across southern Minnesota. The warm temperatures melted what was left of the snowpack from the December 10 winter storm, which led to widespread dense fog through much of the morning and afternoon.||After the thunderstorms, strong gradient winds and widespread wind gusts in excess of 50 mph developed for several hours late Wednesday night and into the overnight hours. The Redwood Falls airport measured a gust of 78 mph at 11:30 PM.||Temperatures quickly fell below freezing across western and central Minnesota Wednesday night, causing rain to change over to a wintry mix of freezing drizzle and snow. Snowfall accumulations of 1-4 inches, along with the strong gusty winds, led to low visibility and travel hazards late Wednesday night into Thursday morning. A fast-moving tornado touched down to the southwest of Hartland and moved into town, damaging numerous buildings, trees, and utility poles. The damage in the southern residential part of town was mainly tree and roof damage. As the tornado tracked into the center of town, more significant damage was observed to buildings along Broadway Street. The most significant damage was to two buildings along Broadway and Johnson in the center of town with significant damage to the walls of low-rise commercial buildings. More tree and roof damage was observed to the northeast with some branches observed along State Highway 13. The tornado dissipated to the northeast in a field with no further damage observed.", "ts_dict_index": [14733, 14734, 14735]}
+{"event_id": 1098967, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "SCOTTS BLUFF", "begin_date_time": "2023-06-23 18:44:00", "end_date_time": "2023-06-23 18:47:00", "narrative": "The most notable storm of the day was an intense, long-lived, cyclic tornadic supercell which significantly impacted Scotts Bluff and Morrill Counties during the early evening hours. This storm originated in the central Laramie Range of Wyoming approximately 50 miles to the west around 3 to 4 hours prior to reaching western Nebraska, producing several confirmed tornadoes along its path. Environmental conditions across Scotts Bluff County continued to support the potential for tornadoes, with abundant moisture pooling in the Platte River Valley and favorable east-to-southeast winds near the surface with a strong southwesterly jet stream aloft. The supercell produced 7 additional confirmed tornadoes (6 in Scotts Bluff County and 1 in Morrill County), most notably including an EF-2 tornado which tracked approximately 1-3 miles ENE of Gering between 7:38 PM and 7:45 PM MDT. A Tornado Emergency was in effect for Gering and Scottsbluff from 7:31 PM until 8:00 PM MDT, which was the first ever issuance of this product from the NWS in Cheyenne. Numerous instances of baseball to softball sized hail occurred across Scotts Bluff County including the city of Scottsbluff. A second intense supercell developed and tracked across Scotts Bluff County in the wake of the first tornadic storm, producing a second swath of very large (baseball sized) hail over the same area. In addition to this primary focus area for intense storms, other isolated storms also brought quarter sized hail, 60 MPH wind gusts to portions of the western Nebraska Panhandle. A confirmed tornado produced a broad, diffuse area of damage along CR 24 and Highway 92 from a secondary tornadic circulation just east of the main Gering tornado. An EF-1 rating was based on a quonset collapse and broken power poles.", "ts_dict_index": [14805, 14806, 14807]}
+{"event_id": 815575, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "DE SOTO", "begin_date_time": "2019-04-24 23:11:00", "end_date_time": "2019-04-24 23:28:00", "narrative": "A strong closed upper level low pressure system advanced east across Central Texas during the evening hours of April 24th, which helped to mix a warm front north into portions of Deep East Texas and Northcentral Louisiana. As a result, warm, moist, and unstable air began to build north along and south of the front, as steepening lapse rates aloft spread east along the axis of increasing large scale forcing ahead of the low. This resulted in an increase in scattered to numerous showers and thunderstorms near and south of the warm front from the late evening hours of the 24th through the early morning hours of the 25th across East Texas and North Louisiana. Coupled with the strong wind shear present across the expanding warm sector, several supercell thunderstorms developed, with one supercell spawning six separate tornadoes from San Augustine Texas northeast to Eastern Union Parish Louisiana, directly impacting the cities of San Augustine Texas and Ruston Louisiana along its 150+ mile track across the NWS Shreveport County Warning Area. In fact, this supercell spawned another tornado across Northwest Morehouse and Southern Ashley County Arkansas, to complete its nearly 180 mile track before dissipating. Other isolated supercells developed near and south of the warm front which spawned tornadoes across Northern Caddo Parish and Central La Salle Parish in Northern Louisiana, with other severe thunderstorms producing damaging winds across portions of Northcentral Louisiana as well, before the storms exited the region around daybreak on the 25th. This is a continuation of the Northwest Sabine Parish tornado. This EF-1 tornado began to weaken as it entered Southeast Desoto Parish, with maximum estimated winds around 95 mph. It snapped and uprooted several trees near the Pelican community, where a tree fell on a vehicle on Highway 175 just south of the Highway 483 intersection, resulting in an injury to the female driver in the vehicle. The tornado continued its northeast movement to Highway 177 north of Parish Road 507 snapping and uprooting several more trees before finally lifting. In all, this long track tornado from Eastern Shelby County Texas through Northwest Sabine and Southeast Desoto Parishes in Northwest Louisiana remained on the ground for 32.1 miles before finally lifting.", "ts_dict_index": [14796, 14797, 14798]}
+{"event_id": 815576, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-04-24 22:51:00", "end_date_time": "2019-04-24 22:53:00", "narrative": "A strong closed upper level low pressure system advanced east across Central Texas during the evening hours of April 24th, which helped to mix a warm front north into portions of Deep East Texas and Northcentral Louisiana. As a result, warm, moist, and unstable air began to build north along and south of the front, as steepening lapse rates aloft spread east along the axis of increasing large scale forcing ahead of the low. This resulted in an increase in scattered to numerous showers and thunderstorms near and south of the warm front from the late evening hours of the 24th through the early morning hours of the 25th across East Texas and North Louisiana. Coupled with the strong wind shear present across the expanding warm sector, several supercell thunderstorms developed, with one supercell spawning six separate tornadoes from San Augustine Texas northeast to Eastern Union Parish Louisiana, directly impacting the cities of San Augustine Texas and Ruston Louisiana along its 150+ mile track across the NWS Shreveport County Warning Area. In fact, this supercell spawned another tornado across Northwest Morehouse and Southern Ashley County Arkansas, to complete its nearly 180 mile track before dissipating. Other isolated supercells developed near and south of the warm front which spawned tornadoes across Northern Caddo Parish and Central La Salle Parish in Northern Louisiana, with other severe thunderstorms producing damaging winds across portions of Northcentral Louisiana as well, before the storms exited the region around daybreak on the 25th. An EF-1 tornado with maximum estimated winds around 105 mph touched down just south of Dixie-Mooringsport Road (Highway 169), where it ripped through roof off of a small outbuilding and damaged a fence. The tornado then crossed Highway 169 where it snapped and uprooted around 10 trees and downed power lines before crossing the highway where its path was observed being the widest at about 100 yards. The tornado then went on to partially damage a roof of a single family home, ripping off shingles, and uprooting and snapping 10-20 more trees along Sundown Drive before lifting near Sunset Lane as it approached the southern shore of Caddo Lake.||In all, four homes were damaged from this tornado near Mooringsport.", "ts_dict_index": [14802, 14803, 14804]}
+{"event_id": 1098736, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "SCOTTS BLUFF", "begin_date_time": "2023-06-23 18:38:00", "end_date_time": "2023-06-23 18:45:00", "narrative": "The most notable storm of the day was an intense, long-lived, cyclic tornadic supercell which significantly impacted Scotts Bluff and Morrill Counties during the early evening hours. This storm originated in the central Laramie Range of Wyoming approximately 50 miles to the west around 3 to 4 hours prior to reaching western Nebraska, producing several confirmed tornadoes along its path. Environmental conditions across Scotts Bluff County continued to support the potential for tornadoes, with abundant moisture pooling in the Platte River Valley and favorable east-to-southeast winds near the surface with a strong southwesterly jet stream aloft. The supercell produced 7 additional confirmed tornadoes (6 in Scotts Bluff County and 1 in Morrill County), most notably including an EF-2 tornado which tracked approximately 1-3 miles ENE of Gering between 7:38 PM and 7:45 PM MDT. A Tornado Emergency was in effect for Gering and Scottsbluff from 7:31 PM until 8:00 PM MDT, which was the first ever issuance of this product from the NWS in Cheyenne. Numerous instances of baseball to softball sized hail occurred across Scotts Bluff County including the city of Scottsbluff. A second intense supercell developed and tracked across Scotts Bluff County in the wake of the first tornadic storm, producing a second swath of very large (baseball sized) hail over the same area. In addition to this primary focus area for intense storms, other isolated storms also brought quarter sized hail, 60 MPH wind gusts to portions of the western Nebraska Panhandle. A tornado tracked approximately 1 to 3 miles ENE of Gering, causing significant damage to a structure with debris scattered up to 1/2 mile to the west, including hazardous material. Vehicles on the property were thrown 50 feet. A small wooden trailer was thrown 1/4 mile away. Additionally, irrigation pivots were rolled numerous times and power lines were broken along Highway 26. Damage was consistent with an EF-2 tornado. Confirmed by official NWS Storm Survey.", "ts_dict_index": [14811, 14812, 14813]}
+{"event_id": 1098735, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "SCOTTS BLUFF", "begin_date_time": "2023-06-23 18:22:00", "end_date_time": "2023-06-23 18:27:00", "narrative": "The most notable storm of the day was an intense, long-lived, cyclic tornadic supercell which significantly impacted Scotts Bluff and Morrill Counties during the early evening hours. This storm originated in the central Laramie Range of Wyoming approximately 50 miles to the west around 3 to 4 hours prior to reaching western Nebraska, producing several confirmed tornadoes along its path. Environmental conditions across Scotts Bluff County continued to support the potential for tornadoes, with abundant moisture pooling in the Platte River Valley and favorable east-to-southeast winds near the surface with a strong southwesterly jet stream aloft. The supercell produced 7 additional confirmed tornadoes (6 in Scotts Bluff County and 1 in Morrill County), most notably including an EF-2 tornado which tracked approximately 1-3 miles ENE of Gering between 7:38 PM and 7:45 PM MDT. A Tornado Emergency was in effect for Gering and Scottsbluff from 7:31 PM until 8:00 PM MDT, which was the first ever issuance of this product from the NWS in Cheyenne. Numerous instances of baseball to softball sized hail occurred across Scotts Bluff County including the city of Scottsbluff. A second intense supercell developed and tracked across Scotts Bluff County in the wake of the first tornadic storm, producing a second swath of very large (baseball sized) hail over the same area. In addition to this primary focus area for intense storms, other isolated storms also brought quarter sized hail, 60 MPH wind gusts to portions of the western Nebraska Panhandle. A tornado occurred in open country west of Gering with no damage reported. Confirmed by official NWS Storm Survey.", "ts_dict_index": [14817, 14818, 14819]}
+{"event_id": 1098733, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "SCOTTS BLUFF", "begin_date_time": "2023-06-23 18:04:00", "end_date_time": "2023-06-23 18:11:00", "narrative": "The most notable storm of the day was an intense, long-lived, cyclic tornadic supercell which significantly impacted Scotts Bluff and Morrill Counties during the early evening hours. This storm originated in the central Laramie Range of Wyoming approximately 50 miles to the west around 3 to 4 hours prior to reaching western Nebraska, producing several confirmed tornadoes along its path. Environmental conditions across Scotts Bluff County continued to support the potential for tornadoes, with abundant moisture pooling in the Platte River Valley and favorable east-to-southeast winds near the surface with a strong southwesterly jet stream aloft. The supercell produced 7 additional confirmed tornadoes (6 in Scotts Bluff County and 1 in Morrill County), most notably including an EF-2 tornado which tracked approximately 1-3 miles ENE of Gering between 7:38 PM and 7:45 PM MDT. A Tornado Emergency was in effect for Gering and Scottsbluff from 7:31 PM until 8:00 PM MDT, which was the first ever issuance of this product from the NWS in Cheyenne. Numerous instances of baseball to softball sized hail occurred across Scotts Bluff County including the city of Scottsbluff. A second intense supercell developed and tracked across Scotts Bluff County in the wake of the first tornadic storm, producing a second swath of very large (baseball sized) hail over the same area. In addition to this primary focus area for intense storms, other isolated storms also brought quarter sized hail, 60 MPH wind gusts to portions of the western Nebraska Panhandle. A brief tornado touchdown occurred over open country west of Gering with no damage reported. Confirmed by official NWS Damage Survey.", "ts_dict_index": [14808, 14809, 14810]}
+{"event_id": 1098740, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "SCOTTS BLUFF", "begin_date_time": "2023-06-23 18:50:00", "end_date_time": "2023-06-23 18:50:00", "narrative": "The most notable storm of the day was an intense, long-lived, cyclic tornadic supercell which significantly impacted Scotts Bluff and Morrill Counties during the early evening hours. This storm originated in the central Laramie Range of Wyoming approximately 50 miles to the west around 3 to 4 hours prior to reaching western Nebraska, producing several confirmed tornadoes along its path. Environmental conditions across Scotts Bluff County continued to support the potential for tornadoes, with abundant moisture pooling in the Platte River Valley and favorable east-to-southeast winds near the surface with a strong southwesterly jet stream aloft. The supercell produced 7 additional confirmed tornadoes (6 in Scotts Bluff County and 1 in Morrill County), most notably including an EF-2 tornado which tracked approximately 1-3 miles ENE of Gering between 7:38 PM and 7:45 PM MDT. A Tornado Emergency was in effect for Gering and Scottsbluff from 7:31 PM until 8:00 PM MDT, which was the first ever issuance of this product from the NWS in Cheyenne. Numerous instances of baseball to softball sized hail occurred across Scotts Bluff County including the city of Scottsbluff. A second intense supercell developed and tracked across Scotts Bluff County in the wake of the first tornadic storm, producing a second swath of very large (baseball sized) hail over the same area. In addition to this primary focus area for intense storms, other isolated storms also brought quarter sized hail, 60 MPH wind gusts to portions of the western Nebraska Panhandle. A trained spotter reported a rain-wrapped tornado with lofted debris near the intersection of CR 26 and Highway 92.", "ts_dict_index": [14814, 14815, 14816]}
+{"event_id": 815581, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "BIENVILLE", "begin_date_time": "2019-04-25 00:25:00", "end_date_time": "2019-04-25 00:26:00", "narrative": "A strong closed upper level low pressure system advanced east across Central Texas during the evening hours of April 24th, which helped to mix a warm front north into portions of Deep East Texas and Northcentral Louisiana. As a result, warm, moist, and unstable air began to build north along and south of the front, as steepening lapse rates aloft spread east along the axis of increasing large scale forcing ahead of the low. This resulted in an increase in scattered to numerous showers and thunderstorms near and south of the warm front from the late evening hours of the 24th through the early morning hours of the 25th across East Texas and North Louisiana. Coupled with the strong wind shear present across the expanding warm sector, several supercell thunderstorms developed, with one supercell spawning six separate tornadoes from San Augustine Texas northeast to Eastern Union Parish Louisiana, directly impacting the cities of San Augustine Texas and Ruston Louisiana along its 150+ mile track across the NWS Shreveport County Warning Area. In fact, this supercell spawned another tornado across Northwest Morehouse and Southern Ashley County Arkansas, to complete its nearly 180 mile track before dissipating. Other isolated supercells developed near and south of the warm front which spawned tornadoes across Northern Caddo Parish and Central La Salle Parish in Northern Louisiana, with other severe thunderstorms producing damaging winds across portions of Northcentral Louisiana as well, before the storms exited the region around daybreak on the 25th. An EF-1 tornado with maximum estimated winds around 105 mph briefly touched down as it crossed Highway 508 and Raspberry Road near the Walsh community. The most significant damage was where it snapped multiple power poles and snapped/uprooted 20-30 trees on Highway 508.", "ts_dict_index": [14799, 14800, 14801]}
+{"event_id": 815578, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "BIENVILLE", "begin_date_time": "2019-04-25 00:12:00", "end_date_time": "2019-04-25 00:15:00", "narrative": "A strong closed upper level low pressure system advanced east across Central Texas during the evening hours of April 24th, which helped to mix a warm front north into portions of Deep East Texas and Northcentral Louisiana. As a result, warm, moist, and unstable air began to build north along and south of the front, as steepening lapse rates aloft spread east along the axis of increasing large scale forcing ahead of the low. This resulted in an increase in scattered to numerous showers and thunderstorms near and south of the warm front from the late evening hours of the 24th through the early morning hours of the 25th across East Texas and North Louisiana. Coupled with the strong wind shear present across the expanding warm sector, several supercell thunderstorms developed, with one supercell spawning six separate tornadoes from San Augustine Texas northeast to Eastern Union Parish Louisiana, directly impacting the cities of San Augustine Texas and Ruston Louisiana along its 150+ mile track across the NWS Shreveport County Warning Area. In fact, this supercell spawned another tornado across Northwest Morehouse and Southern Ashley County Arkansas, to complete its nearly 180 mile track before dissipating. Other isolated supercells developed near and south of the warm front which spawned tornadoes across Northern Caddo Parish and Central La Salle Parish in Northern Louisiana, with other severe thunderstorms producing damaging winds across portions of Northcentral Louisiana as well, before the storms exited the region around daybreak on the 25th. An EF-1 tornado with maximum estimated winds near 110 mph touched down on Brooks Loop in the Lucky community where it snapped large branches before crossing Highway 4. The tornado continued northeast across Highway 9 where it broke power poles and snapped/uprooted approximately 20 trees before lifting.", "ts_dict_index": [14793, 14794, 14795]}
+{"event_id": 1141337, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "DAWSON", "begin_date_time": "2023-10-03 14:59:00", "end_date_time": "2023-10-03 15:01:00", "narrative": "A deep upper trough moved over the Central Plains. A shortwave moved over east central Colorado during the afternoon and CAPE values were highest just to the east of this feature. Low-level moisture was limited and instability was marginal across south central and central Nebraska but high enough for storms to produce severe updrafts.  Wind shear values were around 40 to 50 knots, and a cold front was moving toward the area. Low-level storm relative helicity was increasing which lead to a greater tornado threat. ||Thunderstorms developed during the afternoon ahead of the shortwave and became severe across portions of western Kansas and portions of southern Nebraska. These storms continued to develop and move eastward as the afternoon progressed. The storms began by producing nickel sized hail in Furnas County around 3 pm CDT. The hail got up to the size of golf balls in Dawson, Harlan, Phelps, and Adams Counties. A few of the storms produced tornadoes in Dawson and Sherman Counties. These tornadoes resulted in some damage and were rated EF-0. These storms eventually developed into a line as they moved across portions of Nebraska and Kansas. Aside from an estimated 70 mph wind causing some damage a farmstead near Marquette in Hamilton county, the strongest wind gust reported from the line of storms was 86 mph in Polk County. This wind gust along with other wind gusts resulted in wind damage across portions of south central and central Nebraska. The last severe report of the day was just before 7 pm CDT in Polk County with a wind gust near 60 mph. A short-lived tornado occurred about 3 miles northeast of Overton. This tornado upset at least two center irrigation pivots, and the associated rear flank downdraft damaged three more pivots. One farmstead reported tree damage. One helpful nugget of information was video from a nearby home showing the condensation funnel as it formed. The tornado likely dissipated in a pasture after a couple minutes.", "ts_dict_index": [14790, 14791, 14792]}
+{"event_id": 817405, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "DE SOTO", "begin_date_time": "2019-05-02 05:40:00", "end_date_time": "2019-05-02 05:42:00", "narrative": "A deep southerly flow increased across much of the Ark-La-Tex during the daytime hours of April 30th through May 1st, ahead of a slow moving upper level trough that drifted east into the Southern Plains from the Four Corners Region. A complex of showers and thunderstorms that developed over Western and Central Oklahoma during the evening of April 30th ahead of a stalled surface frontal boundary sent a cold pool southeast into portions of extreme Northeast Texas and Southwest Arkansas which eventually stalled out during the early morning hours on May 1st. Weak upper level disturbances in the southwest flow aloft ahead of the approaching trough triggered additional showers and thunderstorms across Northcentral Texas, which spread east northeast across East Texas, Southwest Arkansas, and North Louisiana during the evening hours of the 1st, and continued throughout the morning hours of the 2nd. The earlier stalled boundary over Northeast Texas and Southwest Arkansas helped to enhance the showers and thunderstorms, and coupled with the instability and deep moisture in place, some of the showers and thunderstorms became severe, producing large hail, damaging winds, and locally heavy rainfall. Isolated strong to severe storms eventually moved into portions of Western Louisiana just prior to daybreak on the 2nd, where trees were downed in Sabine Parish, and even a couple of confirmed isolated tornadoes briefly spinning up over portions of Western and Central Desoto Parish, before finally weakening by mid-morning. An EF-1 tornado with maximum estimated winds between 85-95 mph touched down along Duck Lane and continued northwest snapping and uprooting numerous hardwood trees along Highway 191. A metal awning was lifted off of the roof of a mobile home on Roberts Road. The tornado continued northwest snapping a few more trees along Straus and Roberts Roads before lifting.", "ts_dict_index": [14823, 14824, 14825]}
+{"event_id": 1098741, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "SCOTTS BLUFF", "begin_date_time": "2023-06-23 19:05:00", "end_date_time": "2023-06-23 19:05:00", "narrative": "The most notable storm of the day was an intense, long-lived, cyclic tornadic supercell which significantly impacted Scotts Bluff and Morrill Counties during the early evening hours. This storm originated in the central Laramie Range of Wyoming approximately 50 miles to the west around 3 to 4 hours prior to reaching western Nebraska, producing several confirmed tornadoes along its path. Environmental conditions across Scotts Bluff County continued to support the potential for tornadoes, with abundant moisture pooling in the Platte River Valley and favorable east-to-southeast winds near the surface with a strong southwesterly jet stream aloft. The supercell produced 7 additional confirmed tornadoes (6 in Scotts Bluff County and 1 in Morrill County), most notably including an EF-2 tornado which tracked approximately 1-3 miles ENE of Gering between 7:38 PM and 7:45 PM MDT. A Tornado Emergency was in effect for Gering and Scottsbluff from 7:31 PM until 8:00 PM MDT, which was the first ever issuance of this product from the NWS in Cheyenne. Numerous instances of baseball to softball sized hail occurred across Scotts Bluff County including the city of Scottsbluff. A second intense supercell developed and tracked across Scotts Bluff County in the wake of the first tornadic storm, producing a second swath of very large (baseball sized) hail over the same area. In addition to this primary focus area for intense storms, other isolated storms also brought quarter sized hail, 60 MPH wind gusts to portions of the western Nebraska Panhandle. A trained spotter reported a tornado 2 miles WNW of Minatare.", "ts_dict_index": [14820, 14821, 14822]}
+{"event_id": 941491, "event_type": "Tornado", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2021-03-27 18:12:00", "end_date_time": "2021-03-27 18:31:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track from Cherokee County northeast into Northwest Nacogdoches, Southern Rusk, and Southern Panola Counties, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area during the early morning hours of the 28th. This is a continuation of the Southern Rusk County tornado. This tornado continued northeast towards Lake Murvaul, where it maintained EF1 intensity while snapping and uprooting numerous trees as it paralleled FM 1971. Upon reaching the lake, the tornado reached several residences along the shoreline where it increased in intensity as it snapped and uprooted more trees and damaged the shingles of many homes. By this time, the tornado had strengthened to an EF2, with estimated maximum winds of 115 mph. One person was injured at their residence on the shore of Lake Murvaul, while video of the tornado was recorded by a storm chaser as it crossed the lake. After downing trees which damaged several structures on the east shore of the lake, it weakened and produced more sporadic damage before lifting north-northwest of Gary City. A review of video, TDEM ground survey data, and Sentinel satellite data indicate that the tornado lifted for approximately 5 miles before it touched down again in Southern Panola County.", "ts_dict_index": [14832, 14833, 14834]}
+{"event_id": 941309, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2021-03-27 17:58:00", "end_date_time": "2021-03-27 18:12:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track from Cherokee County northeast into Northwest Nacogdoches, Southern Rusk, and Southern Panola Counties, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area during the early morning hours of the 28th. An EF1 tornado with estimated maximum winds around 110 mph touched down about 1 mile west of Mount Enterprise where it uprooted trees in an open field southwest of town. The tornado then tracked northeast into the Mount Enterprise where it caused shingle damage on several single family homes. One home had its roof mostly removed near the intersection of Highway 84 and West 5th Street, while also damaging a church steeple as it crossed Highway 84. Multiple trees were snapped and uprooted and additional homes suffered shingle damage as the tornado tore through the northeast side of Mount Enterprise. The tornado continued northeast as it crossed County Roads 3195 and 3185, before moving into a heavily wooded area east of County Road 3122 in extreme Southeast Rusk County, snapping and uprooting numerous trees, before crossing over into Southwest Panola County and intensifying into an EF2 tornado just southwest of Lake Murvaul.", "ts_dict_index": [14829, 14830, 14831]}
+{"event_id": 994715, "event_type": "Tornado", "state": "MINNESOTA", "cz_name": "FREEBORN", "begin_date_time": "2021-12-15 19:11:00", "end_date_time": "2021-12-15 19:15:00", "narrative": "A low pressure system of historic strength led to a variety of high-end weather impacts from the central plains to the Upper Midwest and Great Lakes December 15-16. An unprecedented December severe weather unfolded over portions of Minnesota and Wisconsin Wednesday evening, with the Storm Prediction Center issuing their farthest-north Moderate Risk for the Month of December. A serial derecho moving at 60-70 mph tracked from Kansas to Wisconsin, resulting in over 400 reports of damaging wind and numerous tornadoes. Most of the damage across our area occurred from south-central Minnesota through west-central Wisconsin. The strongest tornado damage occurred in Hartland.||Before the thunderstorms, strong southerly winds led to record high temperature at many sites across the Upper Midwest. Temperatures warmed into the mid to upper 50s across much of central Minnesota and western Wisconsin, and even exceeded 60 degrees across southern Minnesota. The warm temperatures melted what was left of the snowpack from the December 10 winter storm, which led to widespread dense fog through much of the morning and afternoon.||After the thunderstorms, strong gradient winds and widespread wind gusts in excess of 50 mph developed for several hours late Wednesday night and into the overnight hours. The Redwood Falls airport measured a gust of 78 mph at 11:30 PM.||Temperatures quickly fell below freezing across western and central Minnesota Wednesday night, causing rain to change over to a wintry mix of freezing drizzle and snow. Snowfall accumulations of 1-4 inches, along with the strong gusty winds, led to low visibility and travel hazards late Wednesday night into Thursday morning. The tornado hit one farmstead, knocking down trees and causing some damage to outbuildings. At the next farmstead, it destroyed a machine shed. A nearly full grain bin was dented at the top. The house had part of its roof taken off. Near the end of its path, two irrigation pivots were blown over. It was uncertain whether the tornado moved into Mower County, and so the path was not extended into Mower County.", "ts_dict_index": [14745, 14746, 14747]}
+{"event_id": 941501, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-03-27 19:40:00", "end_date_time": "2021-03-27 19:41:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track across East Texas, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area through the early morning hours of the 28th. This is a continuation of the Northern Desoto Parish tornado. This EF1 tornado, which had weakened slightly with estimated maximum winds near 90 mph, tracked across the extreme southeast sections of Wallace Lake over Wallace Lake Dam where additional hardwood and softwood trees were snapped and uprooted, with minor roof damage occurring to a home along Ellerbe Road. The tornado lifted in a pecan orchard shortly after crossing Ellerbe Road.", "ts_dict_index": [14871, 14872, 14873]}
+{"event_id": 855002, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-10-20 19:42:00", "end_date_time": "2019-10-20 19:49:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over the east side of Bossier City in Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, before diminishing shortly after daybreak with the departure of this system. An EF-1 tornado with estimated maximum winds around 105 mph touched down along Mount Olive Church Road where it broke large branches off of a hardwood tree. It then continued on to cross State Highway 169 (Glenwood Springridge Road), breaking branches off of several hardwood trees. The worst of the damage associated with the tornado occurred as it crossed Buncombe Road where approximately 20 hardwood and softwood trees were either uprooted or had their trunks snapped. The tornado also destroyed a greenhouse and ripped the singles off of the roofs of two single family homes. The tornado then moved on to roll an RV trailer on Kimberly Road and snapped the tops off of trees on Simpson Road and Brossette Road before lifting just shy of the Shreveport city limits.", "ts_dict_index": [14868, 14869, 14870]}
+{"event_id": 1061294, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-12-13 16:36:00", "end_date_time": "2022-12-13 16:41:00", "narrative": "A strong upper level low pressure system shifted northeast out of the Central Rockies across Eastern Colorado and Northwest Kansas during the day on December 13th, which allowed for surface low pressure to develop along an attendant cold front that extended south across Western Kansas into Western Oklahoma and Northwest Texas. Meanwhile, a tightening pressure gradient ahead of the front resulted in strong southerly low level winds across the Southern Plains and Lower Mississippi Valley, with an increase in warmer, more humid and unstable air spreading back north into East Texas and the Lower Mississippi Valley. Large scale forcing increased during the afternoon across East Texas ahead of the approaching upper trough, along a dry line that had mixed east ahead of the cold front. Thus, scattered showers and thunderstorms developed across much of East Texas and Western Louisiana, before becoming more numerous as they spread east across North-central Louisiana. Some of these storms became severe across North Louisiana as they tapped the strongly sheared air mass in place and the better instability contributed from daytime heating. A couple of isolated strong tornadoes were spawned across extreme Southwest Caddo Parish near the Four Forks community, as well as near Farmerville in Central Union Parish. These storms exited the region into Northeast Louisiana by late evening. An EF-2 tornado with estimated maximum winds near 130 mph touched down in extreme Southwest Caddo Parish near the Four Forks community, where it initially produced minor tree damage along Johns Road just to the south of Keatchie Marshall Road. As the tornado crossed Keatchie Marshall Road, it quickly began to strengthen, producing damage to a number of hardwood and softwood trees. The tornado continued its northeast track across Rita and Laurie Ann Streets, where additional trees were snapped and uprooted, and minor damage to a few homes occurred. The tornado then approached a number of manufactured homes as it moved across Pecan Road, producing EF-2 damage with winds estimated at 130 mph. A single-wide mobile home was completely destroyed, with similar damage occurring to three additional single-wide homes on Pecan Road as it moved across Lareta Street. Two other single-wide mobile homes were completely destroyed on both sides of Pecan Road just south of Lareta Street. ||As the tornado crossed Lareta Street, it lifted a double-wide manufactured home and tossed it to the north and east. Two residents inside the home were killed, with an 8 year old boy thrown an estimated 500-600 yards to the north, and his 30 year old mother thrown an estimated 200 yards before being found on Paula Road. In addition to these two fatalities, two other individuals on Pecan Road were injured from this tornado. Upon crossing Paula Street, the tornado continued to move northeast, snapping and uprooting additional trees to the west of Four Forks Road before crossing Highway 169 just south of Small Road and lifting.", "ts_dict_index": [14883, 14884, 14885]}
+{"event_id": 941559, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2021-03-27 19:11:00", "end_date_time": "2021-03-27 19:13:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track across East Texas, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area through the early morning hours of the 28th. This is a continuation of the Northwest Desoto Parish EF1 tornado northwest of Keachi. This tornado, with estimated maximum winds near 90 mph, continued to track northeast along the Caddo/Desoto Parish line across an open field just south of Majestic Road, before lifting in a heavily wooded area just beyond the triple intersection of Majestic Road, Pluto Road, and Keatchie-Marshall Road. The damage consisted entirely of snapped and uprooted trees. During the survey, it was found that tree damage was found on both the Caddo and Desoto Parish sides of the parish line. The end point was determined to be in Caddo Parish as the damage indicators depicted stronger winds on the Caddo Parish side of the parish line on Keatchie-Marshall Road.", "ts_dict_index": [14874, 14875, 14876]}
+{"event_id": 941557, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "DE SOTO", "begin_date_time": "2021-03-27 19:08:00", "end_date_time": "2021-03-27 19:11:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track across East Texas, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area through the early morning hours of the 28th. An EF1 tornado with estimated maximum winds near 90 mph touched down on Holmes Road between Highway 168 and Highway 172, and tracked northeast across a heavily wooded area into extreme Southwest Caddo Parish northwest of Keachi near the end of Majestic Road. The damage consisted entirely of snapped and uprooted trees.", "ts_dict_index": [14880, 14881, 14882]}
+{"event_id": 1000140, "event_type": "Tornado", "state": "IOWA", "cz_name": "WOODBURY", "begin_date_time": "2021-12-15 16:35:00", "end_date_time": "2021-12-15 16:39:00", "narrative": "An unprecedented storm system lifted across the central Plains from December 15 into the early hours of December 16. Kinematic fields were at the top of the climatological distributions, leading to extreme wind shear in the lowest levels. Ahead of the system, record high temperatures with surface dew point values into the 50s and lower 60s surged toward northwest Iowa and resulted in instability not typically found in December.||A serial derecho developed across Nebraska and Kansas during the early afternoon and raced to the northeast toward Iowa and Minnesota, with widespread damaging wind and a few tornadoes. The first Storm Prediction Center moderate risk, as well as severe thunderstorm and tornado warnings during December, were issued for the Sioux Falls warning area. There was even remaining snow cover in parts of northwest Iowa north of Highway 18 and into southwest Minnesota as the severe storms evolved during the afternoon and evening hours.||As the cold front swung through the area behind the convective line, 60 to 75 mph winds aloft were mixed to the surface and resulted in a few synoptic wind gusts up to hurricane force.  Some light wintry precipitation also fell during the transition toward the much colder air, which led to flash freezing as temperatures fell as much as 40 degrees during the overnight hours. This tornado formed around 4 miles east-northeast of Moville, one-quarter mile east of the intersection of Jasper Avenue and 140th Street. The tornado traveled north-northeast for slightly over 4 and one quarter miles before exiting Woodbury County two miles south of Kingsley, just east of the intersection of Knox Avenue and 100th Street.  The tornado continued in Plymouth County for somewhat less than 4 miles before dissipating at 1642CST.  In Woodbury County near the touchdown point, a barn roof was collapsed.  The tornado continued northeast for around a mile and a half before removing most roof panels from another barn. Near the Plymouth County line, the tornado encountered another farmstead which suffered total destruction of a garage and outbuilding. Numerous larger trees were snapped, and debris from damaged buildings was deposited in the trees. The tornado was rated EF1 while in both Woodbury and Plymouth Counties. The average path width in Woodbury County was 50 yards and the maximum estimated wind speed was 110 mph. Property damage costs are a rough estimate.", "ts_dict_index": [14907, 14908, 14909]}
+{"event_id": 1027142, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-05-21 23:12:00", "end_date_time": "2022-05-21 23:15:00", "narrative": "A weak upper level trough moved into much of Arkansas, Northeast and Central Texas, and North Louisiana during the afternoon and evening hours of May 21st, which helped to reinforce a weak cold front southeast into the region during the evening and overnight hours. The air mass ahead of the front was very unstable, with steep lapse rates present along the trough once large scale forcing was adequate enough to initiate shower and thunderstorm development. As a result, showers and thunderstorms quickly developed during the early to mid evening hours along and just ahead of the front, with many of these storms becoming severe across East Texas, Southwest Arkansas, and extreme Northwest Louisiana. Damaging winds and isolated instances of large hail accompanied these storms, with an isolated tornado briefly touching down just northwest of Hosston in Northern Caddo Parish. A second complex of severe thunderstorms developed over Central Texas near Waco, which quickly moved east into East Texas south of I-20. Damaging winds were widespread with the convective complex across Central and East texas, before the winds weakened as they reached extreme Northwest Louisiana around midnight. However, one isolated tornado did briefly touch down in Northern Caddo Parish near Hosston, before weakening during the early morning hours of the 22nd. An EF-1 tornado with estimated maximum winds near 110 mph touched down as a waterspout over Black Bayou Lake along Ed Road, causing significant damaged to a number of trees which fell onto a few mobile homes. The tornado tracked northeast, crossing Nichols Road where a few more trees were snapped and uprooted before lifting after it crossed Hosston Rodessa Road S. The path length of this tornado was around 1.5 miles.", "ts_dict_index": [14904, 14905, 14906]}
+{"event_id": 941500, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "DE SOTO", "begin_date_time": "2021-03-27 19:22:00", "end_date_time": "2021-03-27 19:40:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track across East Texas, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area through the early morning hours of the 28th. An EF1 tornado with estimated maximum winds near 105 mph touched down in the North Desoto Estates subdivision in Stonewall, where two homes sustained moderate roof damage. The tornado continued northeast while crossing Highway 171 just north of the North Desoto Elementary/Middle/High School campus, where it crossed Ann Francis Drive. At this location, an attached garage of a home was completely destroyed after the tornadic winds compromised the garage door, removed the roof, and caused the collapse of the exterior brick walls, which were lightly mortared to the foundation. The roof was lifted nearly 30 feet into the air and thrown over a set of trees and into a field to the northeast. The remainder of the home was left relatively undamaged. The tornado continued east-northeast over open country snapping and uprooting numerous trees. It turned more to the northeast after crossing Interstate 49 and produced more consistent tree damage along Rodeo Drive just north of Stonewall-Frierson Road. Roofing was also peeled back from a small outbuilding at the north end of Rodeo Drive. The tornado continued to track northeast across a heavily wooded area before crossing the extreme southeast sections of Wallace Lake into extreme Southeast Caddo Parish.", "ts_dict_index": [14877, 14878, 14879]}
+{"event_id": 828454, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RANDALL", "begin_date_time": "2019-05-23 16:01:00", "end_date_time": "2019-05-23 16:04:00", "narrative": "A vigorous upper level low pressure system developed across southern Nevada.  Significant wind shear and instability developed as moisture was drawn north into the Panhandles setting the stage for a very long duration and higher end severe episode.  Initially, elevated supercell storms developed in the NW Texas Panhandles on the cold side of a nearly stationary frontal boundary and moved northeast into the central Oklahoma Panhandle as the first of multiple disturbances moved across the area.  Hail up to golf ball size and wind damage was reported with these storms. ||During the afternoon hours, upper level disturbances, daytime heating and the very pronounced frontal boundary stretching from near Amarillo northeast into Beaver County, Oklahoma became the main catalyst for surface based supercells, which produced very large hail up to baseball size and several tornadoes.  Two very large and long tracked tornadoes produced damage across the northeast Panhandles.  Both were rated EF-2s based on the damage, but they remained in very rural areas throughout their life-cycle.  A total of eight tornadoes occurred during this event, however three of these were landspouts that developed along an outflow produced by storms early in the event.  With the loss of daytime heating, supercells congealed into a line which produced gusty winds and hail across the eastern Texas Panhandle before finally moving east and exiting the region in the early morning hours on May 24th. Local deputy called in landspout.", "ts_dict_index": [14862, 14863, 14864]}
+{"event_id": 941492, "event_type": "Tornado", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2021-03-27 18:38:00", "end_date_time": "2021-03-27 19:05:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track from Cherokee County northeast into Northwest Nacogdoches, Southern Rusk, and Southern Panola Counties, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area during the early morning hours of the 28th. An EF2 tornado with estimated maximum winds near 125 mph touched down again from the same supercell thunderstorm that produced the tornado near and over Lake Murvaul in Southwest Panola County, with this tornado downing and uprooting about 10 hardwood and softwood trees along Highway 59 several miles south of Carthage. The tornado intensified as it tracked parallel to FM 2517 and ripped the roof off of a single family home. The tornado's damage path widened considerably as it moved between FM 2517 and County Road 405. Security footage from a local meat processing center in the Antioch community indicates that a multiple-vortex tornado developed as the storm continued and produced a wide swath of snapped trees north and south of FM 2517. ||Along County Road 405, the multiple-vortex tornado continued to completely destroy 3 metal outbuildings and shift another single family home off of its foundation. At this same location, the tornado tossed an antique vehicle 50 yards and wrapped sheet metal around approximately 10 trees. The tornado continued to snap large softwood trees along County Road 407, and as it crossed FM 699, it caused major roof damage to a brick home near the intersection of County Road 407 and County Road 408. A single-wide manufactured home utilizing a pan anchorage system was pulled free from the anchors and destroyed, with some of the debris blown a couple of hundred yards into a field to the east. ||Hundreds of trees were downed in an area along County Road 448. As the tornado crossed FM 31, a large outbuilding was destroyed, but portions of the wooden frame were anchored by bolts to the foundation and remained in place. In this same area, a large pine tree was uprooted and fell onto a single-wide manufactured home, killing a 46 year old woman with her husband suffering a head injury. Another tree fell onto a vehicle nearby and injured two additional people. The tornado continued northeast snapping and uprooting additional trees and it travelled north of FM 2517. It crossed County Road 470, County Road 471, and finally lifted just east of County Road 332.", "ts_dict_index": [14835, 14836, 14837]}
+{"event_id": 854764, "event_type": "Tornado", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2019-10-20 18:36:00", "end_date_time": "2019-10-20 18:38:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. An EF-0 tornado with estimated maximum winds near 85 mph touched down along the south side of Highway 79 just west of County Road 280 in Western Panola County, where it snapped some large branches out of trees and uprooted a few more. Then, the tornado traveled east-northeast along the north side of Highway 79 where it uprooted and snapped a few trees and damaged a roof to a residential home. It continued on to the east-northeast where it snapped more branches out of a few more trees before lifting near the intersection of County Road 1251 and County Road 124 in the Fair Play community.", "ts_dict_index": [14847, 14848, 14849]}
+{"event_id": 813790, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2019-04-13 12:54:00", "end_date_time": "2019-04-13 13:00:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing numerous reports of damaging winds with several tornadoes across portions of East Texas. These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. This is a continuation of the Cherokee and Northwest Nacogdoches County tornado that tore through the Alto and Sacul communities. This tornado crossed County Roads 4265 and 4238 in extreme Southern Rusk County, where numerous trees were snapped and uprooted. The tornado continued northeast across the East Fork Angelina River, Highway 84, and County Road 4233, where it began to weaken as much of the damage over these areas consisted of snapped large limbs. The tornado finally lifted on County Road 4233 near the intersection of FM 2753. The maximum estimated winds in Southern Rusk County was near 105 mph primarily in the area of County Roads 4265 and 4238.", "ts_dict_index": [14859, 14860, 14861]}
+{"event_id": 854862, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CASS", "begin_date_time": "2019-10-21 02:08:00", "end_date_time": "2019-10-21 02:21:00", "narrative": "A longwave trough dug south into the Southern Plains during the daytime hours of October 20th, with southerly winds increasing ahead of the trough helping to return low level moisture north from the Gulf of Mexico. Above normal temperatures were seen across much of the region as readings climbed into the mid 80s to near 90 degrees, which enhanced instability during the late afternoon through the evening hours across much of the Ark-La-Tex area. Wind shear increased during the evening, with an isolated supercell thunderstorm developing over Central Cherokee County Texas, which tracked northeast across Central Rusk, Western and Northern Panola Counties, and into the Shreveport/Bossier City areas of Northwest Louisiana before weakening. This supercell produced a tornado across Western Panola County Texas, with numerous reports of damaging winds which downed trees and power lines, as well as hail before diminishing over Northwest Louisiana. Additional strong to severe thunderstorms developed during the late evening through the early morning hours on October 21st across Northeast Texas, Southeast Oklahoma, Southwest Arkansas, and North Louisiana ahead of this trough and associated strong cold front, as wind shear increased within a still unstable environment. These storms produced numerous reports of damaging winds across these areas, with even another isolated tornado touching down in Central Cass County before diminishing shortly after daybreak with the departure of this system. An EF-1 tornado, with estimated maximum winds around 100 mph, first touched down on County Road 2617 and tracked almost due east through rural portions of Central Cass County for nearly 10 miles. Almost all of the damage was confined to trees along the entire path. There were a few spots where small amounts of tin roofing material were wrapped in amongst the tree debris, but the sources of the roofing material were never located. In addition, at the surveyed ending point of the tornado on County Road 1145, there was a very small shed structure whose roof was removed.", "ts_dict_index": [14844, 14845, 14846]}
+{"event_id": 813798, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CHEROKEE", "begin_date_time": "2019-04-13 10:52:00", "end_date_time": "2019-04-13 11:00:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing numerous reports of damaging winds with several tornadoes across portions of East Texas. These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. The same storm that produced an EF-2 tornado over Southern Cherokee County about 6 miles south southwest of Alto produced another EF-2 tornado with maximum estimated winds near 120 mph across the southern and western sections of the city of Alto, where it damaged structures along Highway 21, Blaton Street, and Putnam Avenue. Damage included shifting a single family home off of its foundation and significant roof damage to another home on Quincy Avenue. Several other homes sustained structural damage as the tornado tracked across the west side of Alto and then crossed Highway 69. The tornado then moved across the Alto Independent School District (ISD) and damaged its gymnasium and roofs to structures on the campus. It was near the Alto ISD where a second stronger tornado crossed paths with this tornado as it tore through the western and northern sections of Alto just over an hour later.", "ts_dict_index": [14850, 14851, 14852]}
+{"event_id": 941297, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CHEROKEE", "begin_date_time": "2021-03-27 17:06:00", "end_date_time": "2021-03-27 17:37:00", "narrative": "A longwave trough shifted east out of the Rockies and into the Central and Southern Plains during the day on March 27th, with the southwest flow ahead of the trough ejecting a series of upper level disturbances northeast across Northeast Texas, Southwest Arkansas, and Northwest Louisiana during the afternoon and evening. Meanwhile, a broad warm and moist sector had spread north across all of the Ark-La-Tex into Eastern Oklahoma and much of Arkansas ahead of this trough, with temperatures warming into the upper 70s and lower 80s areawide. This resulted in moderate instability developing as large scale forcing increased during the late afternoon through the evening hours, resulting in scattered to numerous shower and thunderstorm development across much of these areas. Increasing wind shear late in the afternoon also promoted the development of scattered severe thunderstorms over East Texas, Southwest Arkansas, and Northwest Louisiana, with various reports of damaging winds and large hail received. However, one lone supercell developed over Eastern Anderson County Texas, which produced multiple tornadoes along its track from Cherokee County northeast into Northwest Nacogdoches, Southern Rusk, and Southern Panola Counties, before eventually moving into Northern Desoto and Southeast Caddo Parishes in Northwest Louisiana. These storms eventually organized along a broken line as it pushed into North Louisiana, ahead of a cold front that shifted southeast into the area during the early morning hours of the 28th. An EF2 tornado with estimated maximum winds near 120 mph touched down just southwest of Russell Cemetery off of FM 23 south-southwest of the city of Rusk in Cherokee County. The tornado tracked northeast where it crossed Highway 69 with intermittent damage along County Road 1101. The tornado crossed FM 343 and intensified and widened significantly to approximately 500 yards, where several hundred trees were snapped continuously along County Road 1211 and County Road 1209. The tornado then weakened and produced more intermittent damage as it crossed over into extreme Northwest Nacogdoches County just west of the Sacul community.", "ts_dict_index": [14838, 14839, 14840]}
+{"event_id": 916389, "event_type": "Tornado", "state": "NORTH CAROLINA", "cz_name": "BRUNSWICK", "begin_date_time": "2020-08-03 18:55:00", "end_date_time": "2020-08-03 19:05:00", "narrative": "Hurricane Isaias came off the African coast as a tropical wave on July 23, 2020. It became Tropical Storm Isaias on July 30th, further strengthening to a hurricane on the 31st. After crossing the Bahamas, it weakened to a tropical storm. Isaias strengthened again to a hurricane as it approached the coast of North Carolina. Hurricane Isaias made landfall at Ocean Isle Beach as a strong Category 1 around 11 pm on August 3rd, with an 87 mph recorded gust. It pushed inland to Goldsboro NC, where it weakened and accelerated northward. ||The hurricane spawned six tornadoes, ranging from EF-0 to EF-2. Most of the tornadoes occurred in Brunswick County.||Rainfall was heaviest along the coast of Georgetown County, topping out at nearly seven inches. Most areas along the coast of North and South Carolina received around three to four inches on average, with lesser amounts inland. The Wilmington ASOS reported a gust to 74 mph. Storm surge was significant in Brunswick County, where many docks were damage, and homes and businesses were inundated with three feet of water.  Downtown Wilmington also received a record surge that came up the Cape Fear River. Over 80,000 residences lost power in New Hanover county, with widespread outages along the coast of Pender County, as they were in the eastern eyewall. Total damage was at least 300 million dollars. The survey team found significant damage to swaths of vegetation which|started near the East Beach area of Bald Head Island where a|strong waterspout moved onshore. The tornado also caused damage|to homes including roof loss and blown in windows as it moved |toward the northwest. The tornado moved across Bald Head Creek |into the Dogwood Ridge Trail area where some of the most extensive |damage was found. The tornado then crossed portions of Cape Creek |and across the Cape Fear River coming ashore again near West Bay St.  |The tornado caused damage to homes and especially trees from W. West |St. to W. 9th St., Robet Ruak Dr., and  Bonner Bussells Dr. SE, prior to |lifting near Dutchman Creek Outlet Channel.", "ts_dict_index": [14895, 14896, 14897]}
+{"event_id": 916387, "event_type": "Tornado", "state": "NORTH CAROLINA", "cz_name": "BRUNSWICK", "begin_date_time": "2020-08-03 20:59:00", "end_date_time": "2020-08-03 21:01:00", "narrative": "Hurricane Isaias came off the African coast as a tropical wave on July 23, 2020. It became Tropical Storm Isaias on July 30th, further strengthening to a hurricane on the 31st. After crossing the Bahamas, it weakened to a tropical storm. Isaias strengthened again to a hurricane as it approached the coast of North Carolina. Hurricane Isaias made landfall at Ocean Isle Beach as a strong Category 1 around 11 pm on August 3rd, with an 87 mph recorded gust. It pushed inland to Goldsboro NC, where it weakened and accelerated northward. ||The hurricane spawned six tornadoes, ranging from EF-0 to EF-2. Most of the tornadoes occurred in Brunswick County.||Rainfall was heaviest along the coast of Georgetown County, topping out at nearly seven inches. Most areas along the coast of North and South Carolina received around three to four inches on average, with lesser amounts inland. The Wilmington ASOS reported a gust to 74 mph. Storm surge was significant in Brunswick County, where many docks were damage, and homes and businesses were inundated with three feet of water.  Downtown Wilmington also received a record surge that came up the Cape Fear River. Over 80,000 residences lost power in New Hanover county, with widespread outages along the coast of Pender County, as they were in the eastern eyewall. Total damage was at least 300 million dollars. A tornado touched down just southwest of Highland Shores subdivision |near the Brunswick River before tracking northwest across River Road |and across Jackey's Creek Lane, producing mostly scattered tree damage. |More significant damage was observed as the tornado moved through the |Olde Towne subdivision, including roof damage, a partially collapsed |garage door, and chimney damage. A considerable amount of trees were |also snapped and uprooted along both South Olde Towne Wynd SE and North |Olde Towne Wynd SE. This included multiple large pine trees up to two |feet in diameter. The tornado then appeared to produce spotty tree and |roof damage as it crossed Kingsworth Lane, before ultimately lifting |just north of Chappell Loop Road SE.", "ts_dict_index": [14889, 14890, 14891]}
+{"event_id": 916393, "event_type": "Tornado", "state": "NORTH CAROLINA", "cz_name": "BRUNSWICK", "begin_date_time": "2020-08-03 19:43:00", "end_date_time": "2020-08-03 19:46:00", "narrative": "Hurricane Isaias came off the African coast as a tropical wave on July 23, 2020. It became Tropical Storm Isaias on July 30th, further strengthening to a hurricane on the 31st. After crossing the Bahamas, it weakened to a tropical storm. Isaias strengthened again to a hurricane as it approached the coast of North Carolina. Hurricane Isaias made landfall at Ocean Isle Beach as a strong Category 1 around 11 pm on August 3rd, with an 87 mph recorded gust. It pushed inland to Goldsboro NC, where it weakened and accelerated northward. ||The hurricane spawned six tornadoes, ranging from EF-0 to EF-2. Most of the tornadoes occurred in Brunswick County.||Rainfall was heaviest along the coast of Georgetown County, topping out at nearly seven inches. Most areas along the coast of North and South Carolina received around three to four inches on average, with lesser amounts inland. The Wilmington ASOS reported a gust to 74 mph. Storm surge was significant in Brunswick County, where many docks were damage, and homes and businesses were inundated with three feet of water.  Downtown Wilmington also received a record surge that came up the Cape Fear River. Over 80,000 residences lost power in New Hanover county, with widespread outages along the coast of Pender County, as they were in the eastern eyewall. Total damage was at least 300 million dollars. A tornado associated with Hurricane Isaias appeared to touch down |near the intersection of Andrew Jackson Highway (Highway 74) and |Ocean Highway East (Highway 17). This was characterized by a few |snapped pine trees. Additional trees were snapped along the path |near Old Fayetteville Road, Wayne Street NE, Village Road NE, and |Old Mill Road NE, although tree damage was spotty in nature.", "ts_dict_index": [14901, 14902, 14903]}
+{"event_id": 916388, "event_type": "Tornado", "state": "NORTH CAROLINA", "cz_name": "BRUNSWICK", "begin_date_time": "2020-08-03 19:15:00", "end_date_time": "2020-08-03 19:17:00", "narrative": "Hurricane Isaias came off the African coast as a tropical wave on July 23, 2020. It became Tropical Storm Isaias on July 30th, further strengthening to a hurricane on the 31st. After crossing the Bahamas, it weakened to a tropical storm. Isaias strengthened again to a hurricane as it approached the coast of North Carolina. Hurricane Isaias made landfall at Ocean Isle Beach as a strong Category 1 around 11 pm on August 3rd, with an 87 mph recorded gust. It pushed inland to Goldsboro NC, where it weakened and accelerated northward. ||The hurricane spawned six tornadoes, ranging from EF-0 to EF-2. Most of the tornadoes occurred in Brunswick County.||Rainfall was heaviest along the coast of Georgetown County, topping out at nearly seven inches. Most areas along the coast of North and South Carolina received around three to four inches on average, with lesser amounts inland. The Wilmington ASOS reported a gust to 74 mph. Storm surge was significant in Brunswick County, where many docks were damage, and homes and businesses were inundated with three feet of water.  Downtown Wilmington also received a record surge that came up the Cape Fear River. Over 80,000 residences lost power in New Hanover county, with widespread outages along the coast of Pender County, as they were in the eastern eyewall. Total damage was at least 300 million dollars. Weak tornado impacted a small area near Law Road |SE and Old Ocean Highway East near the Brunswick |County Government Complex.  The tornado mainly |caused damage to trees and lifted after crossing |Old Ocean Highway East.", "ts_dict_index": [14898, 14899, 14900]}
+{"event_id": 916392, "event_type": "Tornado", "state": "NORTH CAROLINA", "cz_name": "BRUNSWICK", "begin_date_time": "2020-08-03 19:15:00", "end_date_time": "2020-08-03 19:16:00", "narrative": "Hurricane Isaias came off the African coast as a tropical wave on July 23, 2020. It became Tropical Storm Isaias on July 30th, further strengthening to a hurricane on the 31st. After crossing the Bahamas, it weakened to a tropical storm. Isaias strengthened again to a hurricane as it approached the coast of North Carolina. Hurricane Isaias made landfall at Ocean Isle Beach as a strong Category 1 around 11 pm on August 3rd, with an 87 mph recorded gust. It pushed inland to Goldsboro NC, where it weakened and accelerated northward. ||The hurricane spawned six tornadoes, ranging from EF-0 to EF-2. Most of the tornadoes occurred in Brunswick County.||Rainfall was heaviest along the coast of Georgetown County, topping out at nearly seven inches. Most areas along the coast of North and South Carolina received around three to four inches on average, with lesser amounts inland. The Wilmington ASOS reported a gust to 74 mph. Storm surge was significant in Brunswick County, where many docks were damage, and homes and businesses were inundated with three feet of water.  Downtown Wilmington also received a record surge that came up the Cape Fear River. Over 80,000 residences lost power in New Hanover county, with widespread outages along the coast of Pender County, as they were in the eastern eyewall. Total damage was at least 300 million dollars. The tornado touched down along Green Swamp Road and snapped|approximately 20 large pine trees on the west side, up to|20 inches in diameter. A lower degree of tree damage was |observed on the east side of the road. It is suspected that |additional damage extended further into the Green Swamp, |however the area was inaccessible.", "ts_dict_index": [14892, 14893, 14894]}
+{"event_id": 811397, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CHEROKEE", "begin_date_time": "2019-04-13 12:20:00", "end_date_time": "2019-04-13 12:47:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing numerous reports of damaging winds with several tornadoes across portions of East Texas. These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. An EF-3 tornado with maximum estimated winds near 160 mph that originally touched down in Houston County about 9 miles northeast of Crockett crossed the Neches River into Southwest Cherokee County, where it snapped and uprooted thousands of trees along its path. The tornado paralleled Highway 21 before reaching the city of Alto, where it severely damaged or destroyed approximately 20 homes. Included along the damage path southwest of Alto was the Caddo Mounds Sate Historic Site building, which had its roof torn off, nearly all of its exterior walls removed, and was left to only a few interior rooms in the building. Several people were outside running to get inside for safety when the building was destroyed, resulting in one fatality and a number of serious injuries. Multiple cars in the parking lot were thrown 150 yards into trees and across Highway 21. The tornado then went on to lift and destroy a double wide mobile home, throwing it 50 yards. As the tornado continued along Highway 21, its most significant damage was at a single family home and the St. Thomas Chapel which saw their roofs and exterior walls collapsed. Winds were estimated at 150 mph at this point. ||As the tornado neared Alto, it destroyed three homes along Highway 294 and Singletary Street, recording high end EF-3 damage as it wiped the lower level of a two story home off of its foundation and left the top story of the home 20 yards away from the foundation. This damage was reviewed by tornado damage experts from the National Weather Service (NWS) Southern Region Headquarters, NWS Norman, and the Warning Decision Training Division who all agreed it was high end EF-3 damage (with maximum estimated winds near 160 mph) based off how the home walls were separated from the bolts which anchored them to the foundation. Surrounding damage indicators also validated the EF-3 tornado determination. ||The storm then went on to destroy several homes and mobile homes at nearby Alto Elementary School and Alto High School. It also snapped a metal power pole before crossing Highway 69, where it went on to snap and debark several trees in rural Cherokee County north of Alto before crossing FM 343 and into extreme Northwest Nacogdoches County.", "ts_dict_index": [14853, 14854, 14855]}
+{"event_id": 1140298, "event_type": "Tornado", "state": "NEBRASKA", "cz_name": "DAWSON", "begin_date_time": "2023-10-12 13:20:00", "end_date_time": "2023-10-12 13:20:00", "narrative": "Southerly upper level winds moved across Nebraska and brought in a thick layer of low-level stratus clouds during the early morning hours. These clouds limited surface heating during the day; however, cooler air aloft moved over the area during midday. These conditions resulted in more instability. This instability combined with a low-pressure system, forcing from a strong 500 mb jet, and strong low-level wind shear. There was locally enhanced 0 ��� 1 km helicity near a surface low. There was an intersection of a surface warm front with a dryline and cold front near the center of the surface low. The cold front moved across the area during the overnight hours. These conditions resulted in severe weather during the afternoon hours. ||Thunderstorms were present across Nebraska during the early afternoon hours and moved northeastward. These storms began in south central Nebraska by producing a tornado in Phelps County at 1:05 PM CDT. This tornado was rated as an EF-0 and did some damage. These storms moved eastward and developed into line segments and went on to produce 5 more tornadoes. The additional tornadoes were in Dawson, Franklin, Kearney, Adams, and Hall Counties. The tornadoes in Franklin and Kearney Counties were rated EF-1 while the others were rated EF-0. These storms also produced hail and severe wind gusts. The biggest hail was half dollar size in Phelps County. There was a 63 mph wind gust in Adams County. The storms ended by producing nickel sized hail in Hamilton County at 5:05 PM CDT. This tornado was reported by the public to the NWS via pictures and video. No rating nor wind speed was assigned due to the lack of quality damage indicators in the area. The location is estimated.", "ts_dict_index": [14841, 14842, 14843]}
+{"event_id": 916394, "event_type": "Tornado", "state": "NORTH CAROLINA", "cz_name": "BRUNSWICK", "begin_date_time": "2020-08-03 19:15:00", "end_date_time": "2020-08-03 19:19:00", "narrative": "Hurricane Isaias came off the African coast as a tropical wave on July 23, 2020. It became Tropical Storm Isaias on July 30th, further strengthening to a hurricane on the 31st. After crossing the Bahamas, it weakened to a tropical storm. Isaias strengthened again to a hurricane as it approached the coast of North Carolina. Hurricane Isaias made landfall at Ocean Isle Beach as a strong Category 1 around 11 pm on August 3rd, with an 87 mph recorded gust. It pushed inland to Goldsboro NC, where it weakened and accelerated northward. ||The hurricane spawned seven tornadoes, ranging from EF-0 to EF-2. Most of the tornadoes occurred in Brunswick County.||Rainfall was heaviest along the coast of Georgetown County, topping out at nearly seven inches. Most areas along the coast of North and South Carolina received around three to four inches on average, with lesser amounts inland. The Wilmington ASOS reported a gust to 74 mph. Storm surge was significant in Brunswick County, where many docks were damage, and homes and businesses were inundated with three feet of water.  Downtown Wilmington also received a record surge that came up the Cape Fear River. Over 80,000 residences lost power in New Hanover county, with widespread outages along the coast of Pender County, as they were in the eastern eyewall. Total damage was at least 300 million dollars. Weak tornado impacted a small area near Law Road |SE and Old Ocean Highway East near the Brunswick |County Government Complex.  The tornado mainly |caused damage to trees and lifted after crossing |Ocean Highway East (Highway 17).", "ts_dict_index": [14886, 14887, 14888]}
+{"event_id": 817411, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "DE SOTO", "begin_date_time": "2019-05-02 06:08:00", "end_date_time": "2019-05-02 06:09:00", "narrative": "A deep southerly flow increased across much of the Ark-La-Tex during the daytime hours of April 30th through May 1st, ahead of a slow moving upper level trough that drifted east into the Southern Plains from the Four Corners Region. A complex of showers and thunderstorms that developed over Western and Central Oklahoma during the evening of April 30th ahead of a stalled surface frontal boundary sent a cold pool southeast into portions of extreme Northeast Texas and Southwest Arkansas which eventually stalled out during the early morning hours on May 1st. Weak upper level disturbances in the southwest flow aloft ahead of the approaching trough triggered additional showers and thunderstorms across Northcentral Texas, which spread east northeast across East Texas, Southwest Arkansas, and North Louisiana during the evening hours of the 1st, and continued throughout the morning hours of the 2nd. The earlier stalled boundary over Northeast Texas and Southwest Arkansas helped to enhance the showers and thunderstorms, and coupled with the instability and deep moisture in place, some of the showers and thunderstorms became severe, producing large hail, damaging winds, and locally heavy rainfall. Isolated strong to severe storms eventually moved into portions of Western Louisiana just prior to daybreak on the 2nd, where trees were downed in Sabine Parish, and even a couple of confirmed isolated tornadoes briefly spinning up over portions of Western and Central Desoto Parish, before finally weakening by mid-morning. An EF-1 tornado with maximum estimated winds between 95-100 mph briefly touched down just southwest of the intersection of Highway 84 ad Oak Hill Road on the west side of Mansfield, snapping several trees and destroying several small sheds. The tornado also ripped the roof off of a metal awning and snapped a light pole off the concrete base, before lifting along Kings Highway prior to reaching Mansfield High School.", "ts_dict_index": [14826, 14827, 14828]}
+{"event_id": 999589, "event_type": "Tornado", "state": "IOWA", "cz_name": "WOODBURY", "begin_date_time": "2021-12-15 16:20:00", "end_date_time": "2021-12-15 16:24:00", "narrative": "An unprecedented storm system lifted across the central Plains from December 15 into the early hours of December 16. Kinematic fields were at the top of the climatological distributions, leading to extreme wind shear in the lowest levels. Ahead of the system, record high temperatures with surface dew point values into the 50s and lower 60s surged toward northwest Iowa and resulted in instability not typically found in December.||A serial derecho developed across Nebraska and Kansas during the early afternoon and raced to the northeast toward Iowa and Minnesota, with widespread damaging wind and a few tornadoes. The first Storm Prediction Center moderate risk, as well as severe thunderstorm and tornado warnings during December, were issued for the Sioux Falls warning area. There was even remaining snow cover in parts of northwest Iowa north of Highway 18 and into southwest Minnesota as the severe storms evolved during the afternoon and evening hours.||As the cold front swung through the area behind the convective line, 60 to 75 mph winds aloft were mixed to the surface and resulted in a few synoptic wind gusts up to hurricane force.  Some light wintry precipitation also fell during the transition toward the much colder air, which led to flash freezing as temperatures fell as much as 40 degrees during the overnight hours. The tornado touched down near Buchanan Avenue between 230th and 240th streets and moved north northeast, impacting four farmsteads. One machine shed was completely destroyed with debris deposited about 1 mile downstream in an open field. Several other outbuildings were damaged along the track along with a few trees. The tornado lifted just east of the intersection of Old Highway 141 and County Home Road. The average path width was 50 yards and the maximum estimated wind speed was 105 mph. Property damage costs are a rough estimate.", "ts_dict_index": [14913, 14914, 14915]}
+{"event_id": 999598, "event_type": "Tornado", "state": "IOWA", "cz_name": "WOODBURY", "begin_date_time": "2021-12-15 16:25:00", "end_date_time": "2021-12-15 16:32:00", "narrative": "An unprecedented storm system lifted across the central Plains from December 15 into the early hours of December 16. Kinematic fields were at the top of the climatological distributions, leading to extreme wind shear in the lowest levels. Ahead of the system, record high temperatures with surface dew point values into the 50s and lower 60s surged toward northwest Iowa and resulted in instability not typically found in December.||A serial derecho developed across Nebraska and Kansas during the early afternoon and raced to the northeast toward Iowa and Minnesota, with widespread damaging wind and a few tornadoes. The first Storm Prediction Center moderate risk, as well as severe thunderstorm and tornado warnings during December, were issued for the Sioux Falls warning area. There was even remaining snow cover in parts of northwest Iowa north of Highway 18 and into southwest Minnesota as the severe storms evolved during the afternoon and evening hours.||As the cold front swung through the area behind the convective line, 60 to 75 mph winds aloft were mixed to the surface and resulted in a few synoptic wind gusts up to hurricane force.  Some light wintry precipitation also fell during the transition toward the much colder air, which led to flash freezing as temperatures fell as much as 40 degrees during the overnight hours. The tornado spun up two miles northeast of Bronson along 190th Street, around one mile west of the intersection with Emmett Ave, where it ripped a portion of the roof off a single family home and damaged an outbuilding, with debris sent 100 yards to the north into a field.  The tornado continued northeast across open fields until it hit two large metal utility transmission towers, and deposited the electric lines across U.S. Highway 20, resulting in the closure of U.S. Highway 20 east of Lawton for two days. The tornado crossed U.S. Highway 20 less than a mile east of Lawton, then made a more northward turn. As the tornado approached Fayette Avenue, it impacted multiple farmsteads with damage to a few barns and sheds, as well as broken and snapped tree limbs.  A machine shed at one farmstead was completely destroyed along with a concrete silo and lean-to shed. Multiple power poles were snapped along 140th Street. Minor damage was also noted to shingles on a couple single family homes.|The tornado eventually lifted near the intersection of 110th Street and Fayette Avenue.  The average path width was 75 yards and the maximum estimated wind speed was 130 mph. Property damage costs are a rough estimate.", "ts_dict_index": [14910, 14911, 14912]}
+{"event_id": 951816, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RANDALL", "begin_date_time": "2021-03-13 15:31:00", "end_date_time": "2021-03-13 15:36:00", "narrative": "A very potent upper level system produced widespread hazards from heavy snow across the front range/Rockies to severe weather across the Southern High Plains. The vigorous closed upper low was approached the Four Corners region from the west. A warm front lifted north and northwest across all but the Oklahoma Panhandle and the northwest Texas Panhandle while a sharpening dryline was located over eastern New Mexico. The dryline preceded a Pacific cold front which was also located in eastern New Mexico and swept eastward later in the evening. A broken line of thunderstorms developed ahead of the dryline in eastern New Mexico and tracked north and east into the western and southwestern Texas Panhandle before continuing to move east across the remainder of the eastern Panhandles during the evening hours, growing upscale as the Pacific cold front swept eastward and overtook the dryline. Nine confirmed tornadoes occurred early in the event during the afternoon hours and some of these were large, violent and were on the ground for long periods of time. Three separate instances occurred where two tornadoes were in progress from the same parent thunderstorm at the same time. While traveling across mostly rural areas, the tornadoes did impact several farm homes as well as Palo Duro State Park and Greenbelt Lake. A brief secondary tornado was documented by storm chasers and|residents in the area with video and photographs. This tornado|was just north of the main tornado and appears to have been quickly|absorbed by the larger circulation. The tornado damaged a barn and|several power lines along its short track.", "ts_dict_index": [14919, 14920, 14921]}
+{"event_id": 1000137, "event_type": "Tornado", "state": "IOWA", "cz_name": "WOODBURY", "begin_date_time": "2021-12-15 16:15:00", "end_date_time": "2021-12-15 16:16:00", "narrative": "An unprecedented storm system lifted across the central Plains from December 15 into the early hours of December 16. Kinematic fields were at the top of the climatological distributions, leading to extreme wind shear in the lowest levels. Ahead of the system, record high temperatures with surface dew point values into the 50s and lower 60s surged toward northwest Iowa and resulted in instability not typically found in December.||A serial derecho developed across Nebraska and Kansas during the early afternoon and raced to the northeast toward Iowa and Minnesota, with widespread damaging wind and a few tornadoes. The first Storm Prediction Center moderate risk, as well as severe thunderstorm and tornado warnings during December, were issued for the Sioux Falls warning area. There was even remaining snow cover in parts of northwest Iowa north of Highway 18 and into southwest Minnesota as the severe storms evolved during the afternoon and evening hours.||As the cold front swung through the area behind the convective line, 60 to 75 mph winds aloft were mixed to the surface and resulted in a few synoptic wind gusts up to hurricane force.  Some light wintry precipitation also fell during the transition toward the much colder air, which led to flash freezing as temperatures fell as much as 40 degrees during the overnight hours. A public video revealed that a tornado briefly spun up in an open field southwest of Salix between Benton Avenue and Interstate 29 north of 290th Street. The tornado traveled north northeast and lifted just south of 280th Street. The average path width was estimated at 20 yards.", "ts_dict_index": [14916, 14917, 14918]}
+{"event_id": 979253, "event_type": "Tornado", "state": "MISSISSIPPI", "cz_name": "HARRISON", "begin_date_time": "2021-08-29 05:23:00", "end_date_time": "2021-08-29 05:25:00", "narrative": "The ninth named storm, fourth hurricane, and second major hurricane of the 2021 Atlantic hurricane season, Ida originated from a tropical wave in the Caribbean Sea on August 23rd. On August 26th, the wave developed into a tropical depression, which organized further and became Tropical Storm Ida later that day, near Grand Cayman. On a northwestward track, Ida intensified into a hurricane on August 27, just before moving over western Cuba. A day later, the hurricane underwent rapid intensification over the Gulf of Mexico as it passed over a warm core eddy and reached major hurricane strength. It was just under 72 hours from tropical depression formation to category 4 strength with 150 mph winds. Ida remained at its peak intensity of 150 mph winds and a minimum central pressure of 929 millibars as it made landfall near Port Fourchon midday on August 29th. It didn���t weaken to a tropical storm until it reached near the Louisiana/Mississippi border.||Ida produced over a dozen tornadoes and light to moderate wind damage across southwestern and coastal Mississippi. Around 100,000 residents were without power. Around 100 homes were damaged, 6 destroyed. Storm surge inundation ranged from a few feet in Jackson County to 7 feet in Harrison County. Hurricane Ida caused approximately $10 million worth of damage. A waterspout moved onshore near Railroad St and Henderson Ave where it caused minor roof damage to several houses. The most significant damage occurred near Witman Ave where a house sustained extensive roof damage and numerous trees were snapped or uprooted. The tornado tracked to the northwest, causing additional minor roof damage and snapped trees near Blue Lake Cove. It continued to move northwest where a roof was damaged near Prentiss Rd and Hillcrest Drive. Estimated peak winds of 90 mph.", "ts_dict_index": [14937, 14938, 14939]}
+{"event_id": 951825, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RANDALL", "begin_date_time": "2021-03-13 15:48:00", "end_date_time": "2021-03-13 16:04:00", "narrative": "A very potent upper level system produced widespread hazards from heavy snow across the front range/Rockies to severe weather across the Southern High Plains. The vigorous closed upper low was approached the Four Corners region from the west. A warm front lifted north and northwest across all but the Oklahoma Panhandle and the northwest Texas Panhandle while a sharpening dryline was located over eastern New Mexico. The dryline preceded a Pacific cold front which was also located in eastern New Mexico and swept eastward later in the evening. A broken line of thunderstorms developed ahead of the dryline in eastern New Mexico and tracked north and east into the western and southwestern Texas Panhandle before continuing to move east across the remainder of the eastern Panhandles during the evening hours, growing upscale as the Pacific cold front swept eastward and overtook the dryline. Nine confirmed tornadoes occurred early in the event during the afternoon hours and some of these were large, violent and were on the ground for long periods of time. Three separate instances occurred where two tornadoes were in progress from the same parent thunderstorm at the same time. While traveling across mostly rural areas, the tornadoes did impact several farm homes as well as Palo Duro State Park and Greenbelt Lake. The original tornado - Happy to Palo Duro Canyon - associated with this tornado's parent supercell handed off to this second major tornado. Storm chaser video and damage patterns suggest the tornado was either multi-vortex or that multiple satellites may have occurred. Both the original and newly developing tornadoes were briefly on the ground simultaneously. This tornado was narrow initially and possibly consisted of multiple cones as it damaged camp grounds around the rim of Palo Duro State Park. One cabin sustained EF1 damage as its roof was completely removed. A porch likely caught the wind and aided in the damage of the roof, which is why this tornado was not rated higher. Several travel trailers were flipped and one was destroyed at another campground, but none of these trailers were anchored. Minor damage occurred to weaker structures at the state park entrance and there was notable tree damage as well. The tornado crossed the canyon and grew large on the east side, but remained in very rural country. Another rapid and complicated tornado handoff to the Palo Duro Canyon to Washburn tornado occurred east of the canyon around the Randall/Armstrong County line near the intersection of 1258 and Goathead Road as a new circulation took over.", "ts_dict_index": [14931, 14932, 14933]}
+{"event_id": 979257, "event_type": "Tornado", "state": "MISSISSIPPI", "cz_name": "HARRISON", "begin_date_time": "2021-08-29 16:15:00", "end_date_time": "2021-08-29 16:19:00", "narrative": "The ninth named storm, fourth hurricane, and second major hurricane of the 2021 Atlantic hurricane season, Ida originated from a tropical wave in the Caribbean Sea on August 23rd. On August 26th, the wave developed into a tropical depression, which organized further and became Tropical Storm Ida later that day, near Grand Cayman. On a northwestward track, Ida intensified into a hurricane on August 27, just before moving over western Cuba. A day later, the hurricane underwent rapid intensification over the Gulf of Mexico as it passed over a warm core eddy and reached major hurricane strength. It was just under 72 hours from tropical depression formation to category 4 strength with 150 mph winds. Ida remained at its peak intensity of 150 mph winds and a minimum central pressure of 929 millibars as it made landfall near Port Fourchon midday on August 29th. It didn���t weaken to a tropical storm until it reached near the Louisiana/Mississippi border.||Ida produced over a dozen tornadoes and light to moderate wind damage across southwestern and coastal Mississippi. Around 100,000 residents were without power. Around 100 homes were damaged, 6 destroyed. Storm surge inundation ranged from a few feet in Jackson County to 7 feet in Harrison County. Hurricane Ida caused approximately $10 million worth of damage. The tornado developed just to the north of East Railroad Street along Gulf Ave where several large tree limbs were snapped. It continued northwest producing sporadic tree damage. The most significant damage was noted as it crossed 27th Street where numerous large limbs were snapped and a large oak tree was uprooted onto two houses. An older house lost part of its roof as the tornado crossed Broadmoore Pl. The tornado weakened as it crossed 28th Street and dissipated north of Pass Rd where some minor siding damage was noted to an older strip mall. Estimated peak winds of 85 mph.", "ts_dict_index": [14922, 14923, 14924]}
+{"event_id": 951827, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RANDALL", "begin_date_time": "2021-03-13 16:06:00", "end_date_time": "2021-03-13 16:12:00", "narrative": "A very potent upper level system produced widespread hazards from heavy snow across the front range/Rockies to severe weather across the Southern High Plains. The vigorous closed upper low was approached the Four Corners region from the west. A warm front lifted north and northwest across all but the Oklahoma Panhandle and the northwest Texas Panhandle while a sharpening dryline was located over eastern New Mexico. The dryline preceded a Pacific cold front which was also located in eastern New Mexico and swept eastward later in the evening. A broken line of thunderstorms developed ahead of the dryline in eastern New Mexico and tracked north and east into the western and southwestern Texas Panhandle before continuing to move east across the remainder of the eastern Panhandles during the evening hours, growing upscale as the Pacific cold front swept eastward and overtook the dryline. Nine confirmed tornadoes occurred early in the event during the afternoon hours and some of these were large, violent and were on the ground for long periods of time. Three separate instances occurred where two tornadoes were in progress from the same parent thunderstorm at the same time. While traveling across mostly rural areas, the tornadoes did impact several farm homes as well as Palo Duro State Park and Greenbelt Lake. The supercell underwent another odd handoff from the Palo Duro Canyon tornado near Highway 1258 which was documented by storm chasers in the area. Again, both the initial and new developing tornado co-existed for a period of time creating a wide damage path Near County Road 1 in Armstrong County. This tornado path remained in very rural country with few damage indicators and was likely stronger than suggested by the very limited rating. Along the path the tornado snapped a few small diameter power poles and destroyed a couple out buildings. It also pushed over a semi before it dissipated just north of Highway 287.", "ts_dict_index": [14934, 14935, 14936]}
+{"event_id": 951821, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RANDALL", "begin_date_time": "2021-03-13 15:37:00", "end_date_time": "2021-03-13 15:42:00", "narrative": "A very potent upper level system produced widespread hazards from heavy snow across the front range/Rockies to severe weather across the Southern High Plains. The vigorous closed upper low was approached the Four Corners region from the west. A warm front lifted north and northwest across all but the Oklahoma Panhandle and the northwest Texas Panhandle while a sharpening dryline was located over eastern New Mexico. The dryline preceded a Pacific cold front which was also located in eastern New Mexico and swept eastward later in the evening. A broken line of thunderstorms developed ahead of the dryline in eastern New Mexico and tracked north and east into the western and southwestern Texas Panhandle before continuing to move east across the remainder of the eastern Panhandles during the evening hours, growing upscale as the Pacific cold front swept eastward and overtook the dryline. Nine confirmed tornadoes occurred early in the event during the afternoon hours and some of these were large, violent and were on the ground for long periods of time. Three separate instances occurred where two tornadoes were in progress from the same parent thunderstorm at the same time. While traveling across mostly rural areas, the tornadoes did impact several farm homes as well as Palo Duro State Park and Greenbelt Lake. This satellite tornado occurred south of the main large tornado that was ongoing at the time. Radar and chaser reports/video suggest it was an anticyclonic tornado that occurred on the southern edge of the storms rear flank downdraft. A brief radar debris signature was noted after the tornado crossed he interstate. The tornado snapped power poles along I-27, south of the main tornado track, but no other notable damage occurred as it remained in open ranch and grassland  country otherwise.", "ts_dict_index": [14925, 14926, 14927]}
+{"event_id": 951937, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RANDALL", "begin_date_time": "2021-03-13 16:08:00", "end_date_time": "2021-03-13 16:11:00", "narrative": "A very potent upper level system produced widespread hazards from heavy snow across the front range/Rockies to severe weather across the Southern High Plains. The vigorous closed upper low was approached the Four Corners region from the west. A warm front lifted north and northwest across all but the Oklahoma Panhandle and the northwest Texas Panhandle while a sharpening dryline was located over eastern New Mexico. The dryline preceded a Pacific cold front which was also located in eastern New Mexico and swept eastward later in the evening. A broken line of thunderstorms developed ahead of the dryline in eastern New Mexico and tracked north and east into the western and southwestern Texas Panhandle before continuing to move east across the remainder of the eastern Panhandles during the evening hours, growing upscale as the Pacific cold front swept eastward and overtook the dryline. Nine confirmed tornadoes occurred early in the event during the afternoon hours and some of these were large, violent and were on the ground for long periods of time. Three separate instances occurred where two tornadoes were in progress from the same parent thunderstorm at the same time. While traveling across mostly rural areas, the tornadoes did impact several farm homes as well as Palo Duro State Park and Greenbelt Lake. This tornado was photographed by storm chasers positioned east of the area as it crossed the Swisher county line into Randall County. No damaged was observed and the tornado lifted relatively quickly.", "ts_dict_index": [14928, 14929, 14930]}
+{"event_id": 813797, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CHEROKEE", "begin_date_time": "2019-04-13 10:46:00", "end_date_time": "2019-04-13 10:48:00", "narrative": "A strong upper level trough entered the Southern Plains during the afternoon hours of April 12th, which allowed southerly low level winds to gradually return warm and moist air from the Gulf of Mexico north into East Texas and North Louisiana. An upper level disturbance ejecting northeast ahead of the trough across portions of East Texas and North Louisiana during the early morning hours of April 13th carried enough elevated instability, shear, and forcing north of an advancing warm front over Southeast Texas and South Louisiana, such that scattered strong to severe thunderstorms developed, with numerous reports of large hail and occasional damaging winds received. The warm front continued to gradually mix north northwest into East Texas and Northcentral Louisiana by late morning and early afternoon hours, with a very warm, moist, and unstable air mass noted over Deep East Texas and portions of Northcentral Louisiana south of the front. Coupled with even stronger forcing and low level shear ahead of the approaching upper trough, additional strong to severe thunderstorms developed near and south of the front from late morning through the afternoon, producing numerous reports of damaging winds with several tornadoes across portions of East Texas. These showers and thunderstorms diminished by early evening with the departure of the trough, and the arrival of an associated cold front which brought about cooler, drier, and more stable air southeast into the region. An EF-2 tornado with maximum estimated winds near 120 mph touched down in a rural field approximately 2 miles north of the Neches River. It initially snapped several hundred hardwood and softwood trees at their trunks before destroying two single wide mobile homes and ripping the roof off of a single family home at the end of FM 220 near County Road 2806. There, winds were estimated to be at their strongest at approximately 120 mph. The tornado also tossed several antique vehicles near the home and then went on to snap another 20 trees before lifting along FM 220.", "ts_dict_index": [14856, 14857, 14858]}
+{"event_id": 980449, "event_type": "Tornado", "state": "MISSISSIPPI", "cz_name": "HARRISON", "begin_date_time": "2021-08-30 04:55:00", "end_date_time": "2021-08-30 04:56:00", "narrative": "The ninth named storm, fourth hurricane, and second major hurricane of the 2021 Atlantic hurricane season, Ida originated from a tropical wave in the Caribbean Sea on August 23rd. On August 26th, the wave developed into a tropical depression, which organized further and became Tropical Storm Ida later that day, near Grand Cayman. On a northwestward track, Ida intensified into a hurricane on August 27, just before moving over western Cuba. A day later, the hurricane underwent rapid intensification over the Gulf of Mexico as it passed over a warm core eddy and reached major hurricane strength. It was just under 72 hours from tropical depression formation to category 4 strength with 150 mph winds. Ida remained at its peak intensity of 150 mph winds and a minimum central pressure of 929 millibars as it made landfall near Port Fourchon midday on August 29th. It didn���t weaken to a tropical storm until it reached near the Louisiana/Mississippi border.||Ida produced over a dozen tornadoes and light to moderate wind damage across southwestern and coastal Mississippi. Around 100,000 residents were without power. Around 100 homes were damaged, 6 destroyed. Storm surge inundation ranged from a few feet in Jackson County to 7 feet in Harrison County. Hurricane Ida caused approximately $10 million worth of damage. A brief tornado tracked north for approximately a half mile in Biloxi, downing trees and snapping large branches, and causing roof damage to several homes along Howard Ave., Peyton Dr., Keller Ave., and Esters Blvd. Roof damage to a small office complex at the corner of Division St. and Keller Ave. and several nearby houses was also noted. Survey conducted remotely via high-res aerial photography.", "ts_dict_index": [14949, 14950, 14951]}
+{"event_id": 980451, "event_type": "Tornado", "state": "MISSISSIPPI", "cz_name": "HARRISON", "begin_date_time": "2021-08-30 07:49:00", "end_date_time": "2021-08-30 07:51:00", "narrative": "The ninth named storm, fourth hurricane, and second major hurricane of the 2021 Atlantic hurricane season, Ida originated from a tropical wave in the Caribbean Sea on August 23rd. On August 26th, the wave developed into a tropical depression, which organized further and became Tropical Storm Ida later that day, near Grand Cayman. On a northwestward track, Ida intensified into a hurricane on August 27, just before moving over western Cuba. A day later, the hurricane underwent rapid intensification over the Gulf of Mexico as it passed over a warm core eddy and reached major hurricane strength. It was just under 72 hours from tropical depression formation to category 4 strength with 150 mph winds. Ida remained at its peak intensity of 150 mph winds and a minimum central pressure of 929 millibars as it made landfall near Port Fourchon midday on August 29th. It didn���t weaken to a tropical storm until it reached near the Louisiana/Mississippi border.||Ida produced over a dozen tornadoes and light to moderate wind damage across southwestern and coastal Mississippi. Around 100,000 residents were without power. Around 100 homes were damaged, 6 destroyed. Storm surge inundation ranged from a few feet in Jackson County to 7 feet in Harrison County. Hurricane Ida caused approximately $10 million worth of damage. A waterspout moved onshore near the Great Southern Golf Club. Several snapped and uprooted trees were noted in this area and in a wooded area to the northeast of the club. The tornado tracked to the north-northeast, causing damage to several homes along Palmer Dr near Magazine Cir, Oakridge Cir, Hayden Dri, and Lipscomb Ct. A path of downed trees was noted just north of Oakridge Cir. Roof panels were missing from a storage facility building on E Pass Rd. The tornado crossed Debuys Rd and ripped siding off a house on Rainbow Dr. A fence, trees, and large branches were also downed on Rainbow Dr. The tornado lifted shortly thereafter. Survey conducted remotely via high-res aerial photography.", "ts_dict_index": [14943, 14944, 14945]}
+{"event_id": 980447, "event_type": "Tornado", "state": "MISSISSIPPI", "cz_name": "HARRISON", "begin_date_time": "2021-08-29 21:37:00", "end_date_time": "2021-08-29 21:38:00", "narrative": "The ninth named storm, fourth hurricane, and second major hurricane of the 2021 Atlantic hurricane season, Ida originated from a tropical wave in the Caribbean Sea on August 23rd. On August 26th, the wave developed into a tropical depression, which organized further and became Tropical Storm Ida later that day, near Grand Cayman. On a northwestward track, Ida intensified into a hurricane on August 27, just before moving over western Cuba. A day later, the hurricane underwent rapid intensification over the Gulf of Mexico as it passed over a warm core eddy and reached major hurricane strength. It was just under 72 hours from tropical depression formation to category 4 strength with 150 mph winds. Ida remained at its peak intensity of 150 mph winds and a minimum central pressure of 929 millibars as it made landfall near Port Fourchon midday on August 29th. It didn���t weaken to a tropical storm until it reached near the Louisiana/Mississippi border.||Ida produced over a dozen tornadoes and light to moderate wind damage across southwestern and coastal Mississippi. Around 100,000 residents were without power. Around 100 homes were damaged, 6 destroyed. Storm surge inundation ranged from a few feet in Jackson County to 7 feet in Harrison County. Hurricane Ida caused approximately $10 million worth of damage. A likely waterspout moved onshore near Hwy 90 and Fort Henry Ave. It caused damage to trees and a detached garage on Fort Henry Ave. The tornado then moved north-northwest, damaging several roofs in a subdivision near Bayview St, and snapping trees and power lines. The tornado continued on its north-northwestward track, downing trees and causing additional damage to houses on Louisiana Ave. It lifted near Livingston Drive. Survey conducted remotely via high-res satellite imagery.", "ts_dict_index": [14955, 14956, 14957]}
+{"event_id": 980453, "event_type": "Tornado", "state": "MISSISSIPPI", "cz_name": "HARRISON", "begin_date_time": "2021-08-30 07:56:00", "end_date_time": "2021-08-30 07:58:00", "narrative": "The ninth named storm, fourth hurricane, and second major hurricane of the 2021 Atlantic hurricane season, Ida originated from a tropical wave in the Caribbean Sea on August 23rd. On August 26th, the wave developed into a tropical depression, which organized further and became Tropical Storm Ida later that day, near Grand Cayman. On a northwestward track, Ida intensified into a hurricane on August 27, just before moving over western Cuba. A day later, the hurricane underwent rapid intensification over the Gulf of Mexico as it passed over a warm core eddy and reached major hurricane strength. It was just under 72 hours from tropical depression formation to category 4 strength with 150 mph winds. Ida remained at its peak intensity of 150 mph winds and a minimum central pressure of 929 millibars as it made landfall near Port Fourchon midday on August 29th. It didn���t weaken to a tropical storm until it reached near the Louisiana/Mississippi border.||Ida produced over a dozen tornadoes and light to moderate wind damage across southwestern and coastal Mississippi. Around 100,000 residents were without power. Around 100 homes were damaged, 6 destroyed. Storm surge inundation ranged from a few feet in Jackson County to 7 feet in Harrison County. Hurricane Ida caused approximately $10 million worth of damage. A tornado touched down just north of the Mississippi Coast Coliseum. A half dozen houses along Pinewood Dr and Arbor Dr sustained minor roof damage. An air conditioner was blown off its pad and several trees and large branches were snapped. The tornado tracked north across Pass Rd where a portion of the roof was torn off a restaurant and bank, and several trees were downed in an adjoining parking lot. The tornado then tracked to the north-northwest, eventually crossing Popps Ferry Rd toward Carter Rd, Martin Rd, and Old Bay Rd. Numerous houses with shingle damage, downed fences and a few downed trees were noted in the tornado's path. The tornado tracked along Carmargue Ln and either dissipated shortly thereafter or continued as waterspout in Big Lake. Survey conducted remotely via high-res aerial photography. Estimated peak winds of 80 mph.", "ts_dict_index": [14946, 14947, 14948]}
+{"event_id": 980448, "event_type": "Tornado", "state": "MISSISSIPPI", "cz_name": "HARRISON", "begin_date_time": "2021-08-30 03:18:00", "end_date_time": "2021-08-30 03:19:00", "narrative": "The ninth named storm, fourth hurricane, and second major hurricane of the 2021 Atlantic hurricane season, Ida originated from a tropical wave in the Caribbean Sea on August 23rd. On August 26th, the wave developed into a tropical depression, which organized further and became Tropical Storm Ida later that day, near Grand Cayman. On a northwestward track, Ida intensified into a hurricane on August 27, just before moving over western Cuba. A day later, the hurricane underwent rapid intensification over the Gulf of Mexico as it passed over a warm core eddy and reached major hurricane strength. It was just under 72 hours from tropical depression formation to category 4 strength with 150 mph winds. Ida remained at its peak intensity of 150 mph winds and a minimum central pressure of 929 millibars as it made landfall near Port Fourchon midday on August 29th. It didn���t weaken to a tropical storm until it reached near the Louisiana/Mississippi border.||Ida produced over a dozen tornadoes and light to moderate wind damage across southwestern and coastal Mississippi. Around 100,000 residents were without power. Around 100 homes were damaged, 6 destroyed. Storm surge inundation ranged from a few feet in Jackson County to 7 feet in Harrison County. Hurricane Ida caused approximately $10 million worth of damage. A brief tornado touched down about one-quarter mile southwest of Keesler Air Force Base in Biloxi, MS. Several houses sustained minor wind damage along Miramar Ave and Clower St. Large branches were also snapped in this area. The tornado lifted quickly but not before producing more damage farther northwest along its path, including minor roof damage to several apartment buildings along Iberville Dr. A few hardwood trees fell in a wooded area just to the west of the apartment complex. Survey conducted remotely via high-res aerial photography.", "ts_dict_index": [14958, 14959, 14960]}
+{"event_id": 980452, "event_type": "Tornado", "state": "MISSISSIPPI", "cz_name": "HARRISON", "begin_date_time": "2021-08-30 07:50:00", "end_date_time": "2021-08-30 07:55:00", "narrative": "The ninth named storm, fourth hurricane, and second major hurricane of the 2021 Atlantic hurricane season, Ida originated from a tropical wave in the Caribbean Sea on August 23rd. On August 26th, the wave developed into a tropical depression, which organized further and became Tropical Storm Ida later that day, near Grand Cayman. On a northwestward track, Ida intensified into a hurricane on August 27, just before moving over western Cuba. A day later, the hurricane underwent rapid intensification over the Gulf of Mexico as it passed over a warm core eddy and reached major hurricane strength. It was just under 72 hours from tropical depression formation to category 4 strength with 150 mph winds. Ida remained at its peak intensity of 150 mph winds and a minimum central pressure of 929 millibars as it made landfall near Port Fourchon midday on August 29th. It didn���t weaken to a tropical storm until it reached near the Louisiana/Mississippi border.||Ida produced over a dozen tornadoes and light to moderate wind damage across southwestern and coastal Mississippi. Around 100,000 residents were without power. Around 100 homes were damaged, 6 destroyed. Storm surge inundation ranged from a few feet in Jackson County to 7 feet in Harrison County. Hurricane Ida caused approximately $10 million worth of damage. A tornado touched down just north of the Edgewater Mall near Rue Petit Bois where it uprooted a tree and caused minor roof damage. Numerous shingles were missing from a bank on Pass Road and a portion of a roof was torn off a Dunkin Donuts. The tornado tracked north-northeast and produced minor roof damage and downed trees along Lakeview Drive and Fairview Drive. Shingles were missing from an apartment complex on Big Lake Road. A convergent pattern was evident in the tall marshy grass along the south shore of Big Lake. The tornado crossed Big Lake and caused minor damage to several homes near the Sunkist Country Club, including along Barrett Road, Rue Maison, Lackland Drive, and Club Moss Drive. Survey conducted remotely via high-res aerial photography. Peak estimated winds of 85 mph.", "ts_dict_index": [14961, 14962, 14963]}
+{"event_id": 980450, "event_type": "Tornado", "state": "MISSISSIPPI", "cz_name": "HARRISON", "begin_date_time": "2021-08-30 07:44:00", "end_date_time": "2021-08-30 07:45:00", "narrative": "The ninth named storm, fourth hurricane, and second major hurricane of the 2021 Atlantic hurricane season, Ida originated from a tropical wave in the Caribbean Sea on August 23rd. On August 26th, the wave developed into a tropical depression, which organized further and became Tropical Storm Ida later that day, near Grand Cayman. On a northwestward track, Ida intensified into a hurricane on August 27, just before moving over western Cuba. A day later, the hurricane underwent rapid intensification over the Gulf of Mexico as it passed over a warm core eddy and reached major hurricane strength. It was just under 72 hours from tropical depression formation to category 4 strength with 150 mph winds. Ida remained at its peak intensity of 150 mph winds and a minimum central pressure of 929 millibars as it made landfall near Port Fourchon midday on August 29th. It didn���t weaken to a tropical storm until it reached near the Louisiana/Mississippi border.||Ida produced over a dozen tornadoes and light to moderate wind damage across southwestern and coastal Mississippi. Around 100,000 residents were without power. Around 100 homes were damaged, 6 destroyed. Storm surge inundation ranged from a few feet in Jackson County to 7 feet in Harrison County. Hurricane Ida caused approximately $10 million worth of damage. An EF-0 tornado snapped numerous trees and damaged several roofs in the neighborhood between 26th and 28th Streets and Roberts and Hewes Avenues. It then tracked northeast for at least a half mile, producing minor roof damage and uprooting several trees on 30th Street and D Avenue. Survey conducted remotely via high-res aerial photography. The track may have continued briefly beyond this point, but imagery was unavailable.", "ts_dict_index": [14952, 14953, 14954]}
+{"event_id": 951814, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RANDALL", "begin_date_time": "2021-03-13 15:26:00", "end_date_time": "2021-03-13 16:00:00", "narrative": "A very potent upper level system produced widespread hazards from heavy snow across the front range/Rockies to severe weather across the Southern High Plains. The vigorous closed upper low was approached the Four Corners region from the west. A warm front lifted north and northwest across all but the Oklahoma Panhandle and the northwest Texas Panhandle while a sharpening dryline was located over eastern New Mexico. The dryline preceded a Pacific cold front which was also located in eastern New Mexico and swept eastward later in the evening. A broken line of thunderstorms developed ahead of the dryline in eastern New Mexico and tracked north and east into the western and southwestern Texas Panhandle before continuing to move east across the remainder of the eastern Panhandles during the evening hours, growing upscale as the Pacific cold front swept eastward and overtook the dryline. Nine confirmed tornadoes occurred early in the event during the afternoon hours and some of these were large, violent and were on the ground for long periods of time. Three separate instances occurred where two tornadoes were in progress from the same parent thunderstorm at the same time. While traveling across mostly rural areas, the tornadoes did impact several farm homes as well as Palo Duro State Park and Greenbelt Lake. This tornado was a continuation from Swisher County. The tornado damaged numerous electrical transmission lines with power poles snapped along the path. Several homes sustained significant roof damage. One home lost large sections of roof |decking material and this together with a collapsed cell phone |tower led to an EF2 rating. Otherwise, damage to power poles, out |buildings, trees, and fencing suggested EF0 to EF1 ratings along |the tornado path. This tornado handed off to a new tornado - the |Palo Duro Canyon to Washburn tornado - just east of its path and |both tornadoes occurred simultaneously for several minutes before |the first tornado dissipated.", "ts_dict_index": [14940, 14941, 14942]}
+{"event_id": 828460, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RANDALL", "begin_date_time": "2019-05-23 16:15:00", "end_date_time": "2019-05-23 16:17:00", "narrative": "A vigorous upper level low pressure system developed across southern Nevada.  Significant wind shear and instability developed as moisture was drawn north into the Panhandles setting the stage for a very long duration and higher end severe episode.  Initially, elevated supercell storms developed in the NW Texas Panhandles on the cold side of a nearly stationary frontal boundary and moved northeast into the central Oklahoma Panhandle as the first of multiple disturbances moved across the area.  Hail up to golf ball size and wind damage was reported with these storms. ||During the afternoon hours, upper level disturbances, daytime heating and the very pronounced frontal boundary stretching from near Amarillo northeast into Beaver County, Oklahoma became the main catalyst for surface based supercells, which produced very large hail up to baseball size and several tornadoes.  Two very large and long tracked tornadoes produced damage across the northeast Panhandles.  Both were rated EF-2s based on the damage, but they remained in very rural areas throughout their life-cycle.  A total of eight tornadoes occurred during this event, however three of these were landspouts that developed along an outflow produced by storms early in the event.  With the loss of daytime heating, supercells congealed into a line which produced gusty winds and hail across the eastern Texas Panhandle before finally moving east and exiting the region in the early morning hours on May 24th. Landspout reported.", "ts_dict_index": [14865, 14866, 14867]}
+{"event_id": 1057183, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2022-11-04 21:57:00", "end_date_time": "2022-11-04 21:59:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours into the 5th. An EF-0 tornado with estimated maximum winds near 85 mph briefly touched down in the Spring Ridge community just east of Adams Road in a heavily wooded area, where it snapped the top off of a couple of trees. The tornado continued east across Greenwood-Springridge Road and along Godfrey Road, where it snapped several trees and large limbs, and ripped some shingles off of a home. The tornado lifted in a heavily wooded area just east-northeast of Godfrey Road.", "ts_dict_index": [14967, 14968, 14969]}
+{"event_id": 1103147, "event_type": "Tornado", "state": "INDIANA", "cz_name": "FLOYD", "begin_date_time": "2023-05-07 07:42:00", "end_date_time": "2023-05-07 07:43:00", "narrative": "During the early morning hours of May 7th, a cluster of strong and occasionally severe thunderstorms over central Illinois gradually grew upscale into a bowing line of storms as it moved southeast into central and southern Indiana toward dawn. Ahead of the developing quasi-linear convective system, a moderately unstable environment was present across southern Indiana, with MLCAPE ranging from around 500 J/kg in the east to around 1500 J/kg in the west. The line of thunderstorms generally produced sub-severe wind gusts across southern Indiana, as the strongest winds remained aloft thanks to a residual nocturnal stable layer. However, as storms approached the Ohio River, a few discrete cells moving from west to east were overtaken by the line which was moving from north-northwest to south-southeast. In the fifteen minutes or so after these cell mergers took place, five brief spin-up tornadoes occurred in Floyd County, producing pockets of structural and tree damage across the county. All of the tornadoes produced either EF0 or EF1 damage, with estimated wind speeds generally between 75 and 105 mph. Minor straight-line wind damage was also observed as this line of storms moved through. The severe threat ended by 10 a.m. as storms pushed southward into central Kentucky. At 3424 Hamby Road, several trees were snapped and uprooted. Trees were facing from the east northeast to a southeasterly direction. Branches from the trees were scattered from the northeast to the southeast direction. An outbuilding had some siding and gutter damage. Of particular note was a large, healthy red oak tree that was uprooted with a significant root ball, which hit the far corner of the neighbor's house, doing structural damage to the roof and gutters. |     The vast majority of the damage was to the trees, and just off the ground. The tornado topped a few trees at the edge of their property by the forested area, before lifting. Wind speeds of 90 mph were estimated, with a width of 100 yards, across this very short tornado track.", "ts_dict_index": [14979, 14980, 14981]}
+{"event_id": 1103151, "event_type": "Tornado", "state": "INDIANA", "cz_name": "FLOYD", "begin_date_time": "2023-05-07 07:48:00", "end_date_time": "2023-05-07 07:49:00", "narrative": "During the early morning hours of May 7th, a cluster of strong and occasionally severe thunderstorms over central Illinois gradually grew upscale into a bowing line of storms as it moved southeast into central and southern Indiana toward dawn. Ahead of the developing quasi-linear convective system, a moderately unstable environment was present across southern Indiana, with MLCAPE ranging from around 500 J/kg in the east to around 1500 J/kg in the west. The line of thunderstorms generally produced sub-severe wind gusts across southern Indiana, as the strongest winds remained aloft thanks to a residual nocturnal stable layer. However, as storms approached the Ohio River, a few discrete cells moving from west to east were overtaken by the line which was moving from north-northwest to south-southeast. In the fifteen minutes or so after these cell mergers took place, five brief spin-up tornadoes occurred in Floyd County, producing pockets of structural and tree damage across the county. All of the tornadoes produced either EF0 or EF1 damage, with estimated wind speeds generally between 75 and 105 mph. Minor straight-line wind damage was also observed as this line of storms moved through. The severe threat ended by 10 a.m. as storms pushed southward into central Kentucky. The tornado first touched down on the Indiana University Southeast campus, on the west side of the Natural Science and Nursing building. There was roof and siding damage to the building. Trees between the parking lot and Grenadier Drive were |facing east, north, and to the northwest. |     Power poles were snapped along Highway 111 (Grant Line Road). Apartments along Countryside Drive had shingle, gutter and downspout damage. However, one of the apartments had a large section of its roof removed with debris being thrown in all |directions. Two people in the apartment building were injured with head lacerations. Shingles were thrown several hundred yards. Trees were uprooted, snapped and twisted along Countryside Drive and Melvyn Drive. Trees were facing from the northwest to the southeasterly direction. Wind speeds in this area were 100 mph |with a width of 125 yards. One house on Melvyn Drive had no damage except for a piece of gutter that was thrown as a missile in a northerly direction through a window into their living room. Thankfully no one was injured at this location. |     One outbuilding was thrown to the south, while another outbuilding was thrown to the north, three houses apart. Powerlines were snapped, and one large piece of roofing material from the apartment was impaled into the ground. There was numerous wooden and metal fence damage between Melvyn Drive and Preswick Square. A |very big, healthy oak tree was uprooted and was facing an east northeasterly direction. Wind damage in this area was consistent with an EF1 tornado, winds of 105 miles per hour, and a width of 100 yards. |     The last damage was just on the other side of Klerner Lane, which was some low-end EF1 90 mph topped tree damage. In addition to a ground survey, drone photography was used, and there were several videos of a funnel on social media.", "ts_dict_index": [14976, 14977, 14978]}
+{"event_id": 829357, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "BOSSIER", "begin_date_time": "2019-06-19 21:47:00", "end_date_time": "2019-06-19 21:49:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon and evening hours across East Texas, which eventually spread into Northwest Louisiana by late evening just prior to midnight. The storms produced damaging winds across Caddo and Bossier Parishes, and even a brief tornado touchdown in Northern Bossier Parish, before finally weakening during the early morning hours of June 20th. An EF-2 tornado with maximum estimated winds near 130 mph was embedded in a line of severe thunderstorms, and touched down across a forested area northeast of Benton near Butler Hill Road. Based off of drone video, the tornado downed at least a couple hundred trees before it ripped most of the roof off of a two-story single family home, leaving only a small portion of the roof on the second story and the brick exterior walls on the first story standing. This was the worst damage from the tornado, resulting in a high end EF-2 rating. As the tornado continued on to cross Butler Hill Road, it downed and uprooted another couple hundred trees, with several falling on two separate single family homes. The tornado also damaged the roof of an outbuilding before moving on to uproot and snap several additional hardwood and softwood trees. ||This was the strongest tornado to occur between the months of June and September in Bossier Parish. This was only the second tornado to ever occur in the month of June in Bossier Parish, with an F-1 tornado recorded in 1992.", "ts_dict_index": [14988, 14989, 14990]}
+{"event_id": 1103149, "event_type": "Tornado", "state": "INDIANA", "cz_name": "FLOYD", "begin_date_time": "2023-05-07 07:46:00", "end_date_time": "2023-05-07 07:47:00", "narrative": "During the early morning hours of May 7th, a cluster of strong and occasionally severe thunderstorms over central Illinois gradually grew upscale into a bowing line of storms as it moved southeast into central and southern Indiana toward dawn. Ahead of the developing quasi-linear convective system, a moderately unstable environment was present across southern Indiana, with MLCAPE ranging from around 500 J/kg in the east to around 1500 J/kg in the west. The line of thunderstorms generally produced sub-severe wind gusts across southern Indiana, as the strongest winds remained aloft thanks to a residual nocturnal stable layer. However, as storms approached the Ohio River, a few discrete cells moving from west to east were overtaken by the line which was moving from north-northwest to south-southeast. In the fifteen minutes or so after these cell mergers took place, five brief spin-up tornadoes occurred in Floyd County, producing pockets of structural and tree damage across the county. All of the tornadoes produced either EF0 or EF1 damage, with estimated wind speeds generally between 75 and 105 mph. Minor straight-line wind damage was also observed as this line of storms moved through. The severe threat ended by 10 a.m. as storms pushed southward into central Kentucky. The tornado first touched down on the northwest portion of the Brookside subdivision (near the eastern portion of Georgetown Lake), with a couple larger branches of two older compromised trees twisted off. The Brookside subdivision is located just south of Indiana Route 64 and just east of Baylor Wissman Rd. There were over a dozen homes sustaining shingle, soffit, gutter, and fascia damage with many tarps on roofs. Shingles were thrown from an east northeasterly direction to a east southeasterly direction. There was little if any tree damage inside the subdivision, with one playground lifted and thrown into a fence. Drone photography showed the vast majority of the damage was to shingles and to soffits. The damage was estimated to be EF0 with 80 mph winds. The last damage point was in a wooded area just east of Zachary Trail before interstate 64. One tree was topped in that grove of trees.", "ts_dict_index": [14973, 14974, 14975]}
+{"event_id": 1103181, "event_type": "Tornado", "state": "INDIANA", "cz_name": "FLOYD", "begin_date_time": "2023-05-07 07:57:00", "end_date_time": "2023-05-07 07:58:00", "narrative": "During the early morning hours of May 7th, a cluster of strong and occasionally severe thunderstorms over central Illinois gradually grew upscale into a bowing line of storms as it moved southeast into central and southern Indiana toward dawn. Ahead of the developing quasi-linear convective system, a moderately unstable environment was present across southern Indiana, with MLCAPE ranging from around 500 J/kg in the east to around 1500 J/kg in the west. The line of thunderstorms generally produced sub-severe wind gusts across southern Indiana, as the strongest winds remained aloft thanks to a residual nocturnal stable layer. However, as storms approached the Ohio River, a few discrete cells moving from west to east were overtaken by the line which was moving from north-northwest to south-southeast. In the fifteen minutes or so after these cell mergers took place, five brief spin-up tornadoes occurred in Floyd County, producing pockets of structural and tree damage across the county. All of the tornadoes produced either EF0 or EF1 damage, with estimated wind speeds generally between 75 and 105 mph. Minor straight-line wind damage was also observed as this line of storms moved through. The severe threat ended by 10 a.m. as storms pushed southward into central Kentucky. The first area of damage was at The Sporting Club at the Farm on Indiana State Road 111. Two large barns had significant roof damage and there was shingle and soffit damage to a large, well-built house. Of significance, a 110-pound storm cellar door was sucked out and thrown almost 100 yards to the east. There were 3 trees uprooted |and facing from north to an easterly direction. |     The 600-pound sign for the sporting club was lifted up and moved to the north several feet. The tornado crossed Highway 111 and snapped and twisted over a dozen trees along the west side of the Ohio River. Because of the 110-pound bolted tornado shelter door being sucked out, the tornado rating increased from 95 to 100 mph. The |width was 100 yards wide. |     The tornado continued near Five Mile Lane and River Road in Floyd County along the Ohio River where shingles were lost on a residence and a barn garage received significant roof damage where the metal panels were peeled off. The tornado then crossed the Ohio River into Kentucky in the Lake Dreamland area of West Louisville in western Jefferson County.", "ts_dict_index": [14982, 14983, 14984]}
+{"event_id": 1103153, "event_type": "Tornado", "state": "INDIANA", "cz_name": "FLOYD", "begin_date_time": "2023-05-07 07:52:00", "end_date_time": "2023-05-07 07:53:00", "narrative": "During the early morning hours of May 7th, a cluster of strong and occasionally severe thunderstorms over central Illinois gradually grew upscale into a bowing line of storms as it moved southeast into central and southern Indiana toward dawn. Ahead of the developing quasi-linear convective system, a moderately unstable environment was present across southern Indiana, with MLCAPE ranging from around 500 J/kg in the east to around 1500 J/kg in the west. The line of thunderstorms generally produced sub-severe wind gusts across southern Indiana, as the strongest winds remained aloft thanks to a residual nocturnal stable layer. However, as storms approached the Ohio River, a few discrete cells moving from west to east were overtaken by the line which was moving from north-northwest to south-southeast. In the fifteen minutes or so after these cell mergers took place, five brief spin-up tornadoes occurred in Floyd County, producing pockets of structural and tree damage across the county. All of the tornadoes produced either EF0 or EF1 damage, with estimated wind speeds generally between 75 and 105 mph. Minor straight-line wind damage was also observed as this line of storms moved through. The severe threat ended by 10 a.m. as storms pushed southward into central Kentucky. The first damage point towards the western end of McCarthy Knob Road was some straight-line wind damage of some cedars and maple trees of 75 mph. Shortly east of there was more widespread tree damage on the west side of the road and up the hill. There were softwood and hardwood trees twisted, snapped, topped, and uprooted for almost a half a mile which ended near the intersection of Budd Road. |     A tree fell on the back side of the house, causing some gutter and fascia damage. There were several power lines down and two power poles pushed over. The maximum tornado winds were 90 mph.", "ts_dict_index": [14985, 14986, 14987]}
+{"event_id": 1061291, "event_type": "Tornado", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2022-12-13 15:38:00", "end_date_time": "2022-12-13 15:44:00", "narrative": "A strong upper level low pressure system shifted northeast out of the Central Rockies across Eastern Colorado and Northwest Kansas during the day on December 13th, which allowed for surface low pressure to develop along an attendant cold front that extended south across Western Kansas into Western Oklahoma and Northwest Texas. Meanwhile, a tightening pressure gradient ahead of the front resulted in strong southerly low level winds across the Southern Plains and Lower Mississippi Valley, with an increase in warmer, more humid and unstable air spreading back north into East Texas and the Lower Mississippi Valley. Large scale forcing increased during the afternoon across East Texas ahead of the approaching upper trough, along a dry line that had mixed east ahead of the cold front. Thus, scattered showers and thunderstorms developed across much of East Texas, some of which became severe as they tapped the strongly sheared air mass in place and the better instability contributed from daytime heating. Several reports of damaging winds which downed trees were received across East Texas, and spawned an isolated tornado over Northern Panola and Southern Harrison Counties near the Elysian Fields community, before lifting prior to reaching Caddo Parish in Northwest Louisiana. An EF-2 tornado with estimated maximum winds around 115 mph touched down in a forested area in Northern Panola County just west of County Road 3123, where approximately a couple hundred softwood trees were snapped and uprooted across an area around 460 yards wide. The tornado damage swath narrowed as it damaged a roof of a single family home off of County Road 312 and County Road 3123. The tornado continued to snap and uproot trees as it tracked across FM 31 and into Southern Harrison County near the Elysian Fields community.", "ts_dict_index": [14994, 14995, 14996]}
+{"event_id": 828152, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2019-06-19 05:03:00", "end_date_time": "2019-06-19 05:04:00", "narrative": "A weakening complex of showers and thunderstorms entered portions of Northeast Texas during the pre-dawn hours of June 19th, but a strong southwesterly low level jet feeding into these storms interacted with adequate instability still in place for these storms to re-intensify over portions of East Texas, such that they became severe producing damaging winds that downed trees and power lines, which eventually spread into portions of Northwest Louisiana before weakening again shortly after daybreak. These storms also spawned a brief, weak tornado over Harrison County just northwest of the Nesbitt community. ||This complex of thunderstorms left behind a surface boundary which lifted north across Northeast Texas, Southeast Oklahoma, and Southwest Arkansas ahead of an approaching upper level shortwave trough. Strong heating near this surface boundary resulted in the development of moderate instability, with large scale forcing ahead of the approaching trough contributing to the development of a second round of severe thunderstorms during the late afternoon through the evening hours across East Texas. The storms produced damaging winds and large hail, with localized flash flooding in Northeast Wood County before finally weakening during the early morning hours of June 20th. An EF-0 tornado with maximum estimated winds near 85 mph briefly touched down along Highway 450 along Little Cypress Bayou. Trees were uprooted and large branches were snapped in a convergent pattern which, when paired with radar data, led to the confirmation of a tornado.", "ts_dict_index": [14970, 14971, 14972]}
+{"event_id": 1063556, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CASS", "begin_date_time": "2022-11-04 18:03:00", "end_date_time": "2022-11-04 18:06:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours. This is a continuation of an EF-3 tornado that occurred in Morris County and tracked into extreme northwestern Cass County. This tornado produced mainly EF-1 damage with estimated maximum winds near 105 mph to a mix of trees and structures as it crossed CR-2888 and CR-2738, before lifting shortly after crossing Texas Highway 77.", "ts_dict_index": [14997, 14998, 14999]}
+{"event_id": 1061292, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2022-12-13 15:44:00", "end_date_time": "2022-12-13 15:52:00", "narrative": "A strong upper level low pressure system shifted northeast out of the Central Rockies across Eastern Colorado and Northwest Kansas during the day on December 13th, which allowed for surface low pressure to develop along an attendant cold front that extended south across Western Kansas into Western Oklahoma and Northwest Texas. Meanwhile, a tightening pressure gradient ahead of the front resulted in strong southerly low level winds across the Southern Plains and Lower Mississippi Valley, with an increase in warmer, more humid and unstable air spreading back north into East Texas and the Lower Mississippi Valley. Large scale forcing increased during the afternoon across East Texas ahead of the approaching upper trough, along a dry line that had mixed east ahead of the cold front. Thus, scattered showers and thunderstorms developed across much of East Texas, some of which became severe as they tapped the strongly sheared air mass in place and the better instability contributed from daytime heating. Several reports of damaging winds which downed trees were received across East Texas, and spawned an isolated tornado over Northern Panola and Southern Harrison Counties near the Elysian Fields community, before lifting prior to reaching Caddo Parish in Northwest Louisiana. This is a continuation of the Northern Panola County EF-2 tornado. This tornado weakened slightly to a strong EF-1 with estimated maximum winds near 110 mph as it entered Southern Harrison County near the Elysian Fields community, where it continued to snap and uproot trees before crossing Old Town Road south of FM 451. A few shingles were torn off of a roof of a single family home along Old Town Road, before the tornado crossed FM 451 near CR 1212 just west of Elysian Fields High School, where it paralleled CR 1214 as it continued to snap and uproot trees, and damaged the roof of an outbuilding and destroyed another. The tornado then crossed FM 9 where it damaged a two story home, removing large portions of the roof before lifting shortly thereafter upon crossing a private road just southeast of FM 9.", "ts_dict_index": [14991, 14992, 14993]}
+{"event_id": 1084989, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CASS", "begin_date_time": "2023-04-05 07:44:00", "end_date_time": "2023-04-05 07:45:00", "narrative": "An upper low pressure system over the Four Corners Region ejected northeast through the Southern Rockies into the Central Plains by the afternoon of April 5th, which reinforced a cold front southeast into East Texas, Southwest Arkansas, and North Louisiana before stalling out late in the day. Large scale ascent increased along and ahead of the front and the ejecting upper low, which had tapped into a warm and moderately unstable air mass that had pooled north from the Gulf of Mexico ahead of the front. This resulted in numerous shower and thunderstorm development during the morning around and after daybreak over Northeast Texas and Southwest Arkansas, which eventually moved into portions of extreme Northwest Louisiana by late morning/early afternoon. Some of these storms became severe, with damaging winds observed and even an isolated tornado briefly touching down just west of Linden in Cass County Texas. While these storms eventually weakened by mid-afternoon, additional redevelopment occurred along the slowing front farther south of I-20 in East Texas by late afternoon and early evening as they tapped stronger instability, with isolated severe thunderstorms producing large hail affecting portions of Cherokee and Panola Counties before moving into extreme Northwest Louisiana. A NWS Storm Survey concluded that a brief EF-0 tornado with estimated maximum winds near 85 mph briefly touched down along Farm Road 130, where it uprooted approximately 10 trees in a convergent pattern while also downing several small and large tree limbs.", "ts_dict_index": [14964, 14965, 14966]}
+{"event_id": 819402, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "DE SOTO", "begin_date_time": "2019-05-08 14:53:00", "end_date_time": "2019-05-08 15:00:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. An EF-1 tornado with maximum estimated winds near 90 mph was associated with the parent mesocyclone which produced a tornado just south and east of Stonewall, before tracking into extreme Southeast Caddo Parish. This second tornado snapped and uprooted several trees on Bethel Road, before moving northeast snapping and uprooting several more trees on Wallace Lake Road and Old Church Road before lifting. A metal farm outbuilding was also lifted and destroyed on Old Church Road before the tornado lifted.", "ts_dict_index": [15024, 15025, 15026]}
+{"event_id": 819121, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "DE SOTO", "begin_date_time": "2019-05-08 14:44:00", "end_date_time": "2019-05-08 15:01:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. An EF-1 tornado with maximum estimated winds near 110 mph touched down along Highway 171 just south of the Stonewall city limits where it snapped numerous large hardwood trees and some power poles between Red Bluff Road and Dixie Swim Club Road. The tornado continued east-northeast along or just south of Red Bluff Road, eventually crossing Bethel Road, Stonewall Frierson Road, and White Springs Road, snapping and uprooting numerous trees along its path. One home sustained heavy damage after several large trees fell on it. From White Springs Road, the tornado crossed over into extreme Southeast Caddo Parish before lifting shortly thereafter.", "ts_dict_index": [15015, 15016, 15017]}
+{"event_id": 819122, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-05-08 15:01:00", "end_date_time": "2019-05-08 15:02:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. The is a continuation of the Desoto Parish EF-1 tornado. This tornado weakened slightly as it entered extreme Southeast Caddo Parish near Ellerbe Road, with maximum estimated winds around 90 mph. Several trees were snapped along Ellerbe Road before the tornado lifted just along Highway 175 just north of its intersection of Ellerbe Road.", "ts_dict_index": [15027, 15028, 15029]}
+{"event_id": 819595, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "OUACHITA", "begin_date_time": "2019-05-08 17:36:00", "end_date_time": "2019-05-08 17:41:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. An EF-1 tornado with maximum estimated winds near 90 mph touched down just south of Interstate 20 east of Ruby Road just southeast of the Monroe city limits, and tracked northeast across Russell Sage Road and Interstate 20, where multiple tree branches were snapped. As the tornado crossed Interstate 20, a few softwood tree trunks were snapped on the south side of the interstate, continuing northeast and lifting near Highway 80 in an area under construction near the Richland Parish line. This damage was collaborated by small tornadic debris signatures as observed from the University of Louisiana-Monroe dopplar radar.", "ts_dict_index": [15039, 15040, 15041]}
+{"event_id": 819111, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "CADDO", "begin_date_time": "2019-05-08 14:20:00", "end_date_time": "2019-05-08 14:24:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. This is a continuation of the extreme Northeast Panola County tornado. This EF-1 tornado strengthened as it entered Western Caddo Parish, with maximum estimated winds near 100 mph. It continued east from the Texas/Louisiana state line in the Bethany community along Highway 79, where it uprooted and snapped several trees, before paralleling Buncombe Road. Along this nearly two mile stretch of Buncombe Road, numerous trees were snapped and uprooted before the tornado lifted near the intersection of Cook Road.", "ts_dict_index": [15036, 15037, 15038]}
+{"event_id": 819114, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "DE SOTO", "begin_date_time": "2019-05-08 14:33:00", "end_date_time": "2019-05-08 14:36:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. An EF-1 tornado with maximum estimated winds near 95 mph touched down along Highway 172 just west of Keachi, snapping and uprooting several trees and destroying a large metal farm canopy. The tornado continued east into the community of Keachi, snapping and uprooting numerous trees along Highway 789 before lifting.", "ts_dict_index": [15033, 15034, 15035]}
+{"event_id": 819589, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "JACKSON", "begin_date_time": "2019-05-08 16:52:00", "end_date_time": "2019-05-08 16:55:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. This is a continuation of the Lincoln Parish EF-1 tornado. This tornado weakened slightly as it crossed Riser Road back into Jackson Parish, with maximum estimated winds around 105 mph as it continued northeast across extreme Northwest Jackson Parish. Numerous trees were snapped and uprooted as the tornado tracked northeast across and along Edmiston Road before lifting on Countyline Road near its intersection of Edmiston Road.", "ts_dict_index": [15012, 15013, 15014]}
+{"event_id": 819436, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "JACKSON", "begin_date_time": "2019-05-08 16:35:00", "end_date_time": "2019-05-08 16:41:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. An EF-1 tornado with maximum estimated winds near 110 mph touched down near the Charles H. Garrett Community Center in the extreme southern portions of the city of Jonesboro where it damaged a small portion of the roof. It then crossed Highway 167 and snapped/uprooted trees along the highway and damaged a metal building where the column anchorage failed. Several more trees were snapped and uprooted along the path as it crossed Firetower Road, Highway 147, Rome Road, and Holiday Lane. The tornado then lifted after crossing Highway 4.", "ts_dict_index": [15030, 15031, 15032]}
+{"event_id": 1057269, "event_type": "Tornado", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-11-04 16:51:00", "end_date_time": "2022-11-04 16:56:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours. An EF-1 tornado with estimated maximum winds near 105 mph touched down in a heavily wooded area in far Northwest McCurtain County northwest of Second Mountain. Numerous trees were snapped or uprooted as it crossed Dog Creek northeast into Southern Le Flore County just southeast of the Honobia community. This is part of an overall 11+ mile track from Northwest McCurtain County into Southwest Le Flore County.", "ts_dict_index": [15006, 15007, 15008]}
+{"event_id": 819441, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "JACKSON", "begin_date_time": "2019-05-08 16:35:00", "end_date_time": "2019-05-08 16:36:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. An EF-1 tornado with maximum estimated winds near 100 mph briefly touched down just west of Highway 167, where it snapped and uprooted approximately 15 trees as it crossed Highway 167 and then quickly lifted.", "ts_dict_index": [15021, 15022, 15023]}
+{"event_id": 819451, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "JACKSON", "begin_date_time": "2019-05-08 16:47:00", "end_date_time": "2019-05-08 16:50:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. An EF-1 tornado with maximum estimated winds near 110 mph touched down in the community of Clay near Homer Sisemore Road, where it snapped and uprooted numerous trees, ripped the roof off of a small outbuilding, completely destroyed a shed, and ripped shingles off of the roof of a single family home. The tornado continued northeast, crossing Bonnie Blue Lane and tracking along Highway 167, snapping additional trees before entering extreme Southeast Lincoln Parish.", "ts_dict_index": [15018, 15019, 15020]}
+{"event_id": 1009248, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CHEROKEE", "begin_date_time": "2022-03-21 22:16:00", "end_date_time": "2022-03-21 22:20:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. An EF-2 tornado with estimated maximum winds near 125 mph touched down in a field just north of Highway 21 in Southern Cherokee County a couple miles east-northeast of Alto, where it downed large limbs in a convergent pattern. As the tornado crossed Highway 241, it uprooted trees, and damaged two metal outbuildings just off of County Road 2525. The tornado continued to uproot and snap trees in more rural areas unreachable by vehicles, before crossing over into Northwest Nacogdoches County. The damage across Southern Cherokee County was consistent with EF-1 tornado winds up to 100 mph, although the tornado strengthened to an EF-2 shortly after crossing over into Northwest Nacogdoches County.", "ts_dict_index": [15045, 15046, 15047]}
+{"event_id": 819446, "event_type": "Tornado", "state": "LOUISIANA", "cz_name": "JACKSON", "begin_date_time": "2019-05-08 16:42:00", "end_date_time": "2019-05-08 16:48:00", "narrative": "A strong upper level trough of low pressure extending from the Intermountain West into the Four Corners Region energized the southwest flow aloft across the Southern Plains during much of the day on May 8th, with a strong low level jet sustaining a mesoscale convective complex (MCS) across much of Oklahoma into Northcentral Texas south into the Texas Hill Country. While these storms gradually weakened after daybreak as a cold pool from these storms propagated southeast into the region, additional upper level disturbances ahead of this trough interacted with ample moisture and instability near this cold pool to intensify these showers and thunderstorms, some of which became severe with damaging winds as they moved across portions of East Texas, Southwest Arkansas, and North Louisiana. Strong low level shear was also present within the moderately unstable air mass, with discrete supercell thunderstorms developing across extreme East Texas and North Louisiana. This resulted in eleven reports of tornadoes across Northern Louisiana before the storms gradually weakened during the evening. However, locally heavy rainfall from the stronger storms persisted across portions of North Louisiana during the evening through the overnight/early morning hours of the 9th. An EF-1 tornado with maximum estimated winds near 110 mph that was embedded within a squall line touched down on Poda Road where several trees were snapped. The tornado continued east, crossing Dewberry Road and Northstar Lane where numerous trees were snapped and uprooted. The tornado then crossed Caney Lake Reservoir and into Jimmie Davis State Park, where it snapped and uprooted numerous hardwood and softwood trees. Some of the trees fell into multiple campers and approximately three-fourths of the cabins in the park. The tornado lifted as it exited the north end of the State Park.", "ts_dict_index": [15042, 15043, 15044]}
+{"event_id": 1009226, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CASS", "begin_date_time": "2022-03-21 22:29:00", "end_date_time": "2022-03-21 22:32:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. An EF-1 tornado with estimated maximum winds near 100 mph embedded within a quasi-linear convective system (QLCS) briefly touched down on County Road 3658, before crossing Highway 59 between the Queen City and Domino communities. The tornado continued to track northeast, crossing County Road 3664 before lifting near County Road 3665. Numerous trees were uprooted along the tornado's path, and destroyed several metal outbuildings while damaging the roofs of manufactured homes along County Roads 3658 and 3664 before lifting.", "ts_dict_index": [15048, 15049, 15050]}
+{"event_id": 1063565, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CASS", "begin_date_time": "2022-11-04 18:37:00", "end_date_time": "2022-11-04 19:00:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours. The tornado first touched down just to the southwest of Hughes Springs and then moved northeast into the city limits, where EF-1 damage was noted. Two single family residences sustained damage to the roofs with partial roof removal. The forest station on Pine Street also sustained damage to the roof and walls. Additionally, numerous large trees were downed along the path. Damage continued along CR-2994, just northeast of Hughes Springs, where two well-built homes sustained substantial roof damage consistent with an EF-2 rating. As the tornado continued on its path, it continued to cause EF-1 damage through more rural areas of Cass County, with a consistent path of snapped and uprooted softwood and hardwood trees. The tornado began to intensify near Cusseta, with a tornado debris signature appearing on radar. Here, the tornado caused widespread EF-2 damage to countless hardwood and softwood trees. Trees were snapped and twisted over an extensive area of ground, with the tornado causing EF-1 damage to an old structure located on a small hill. The tornado began to weaken on the north side of Texas Highway 77 west of Douglassville, but not before snapping more hardwood and softwood trees on both sides of the highway. Through the use of high resolution satellite imagery, the track was found to be continuous in areas that originally could not be surveyed by ground.", "ts_dict_index": [15003, 15004, 15005]}
+{"event_id": 1009240, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CASS", "begin_date_time": "2022-03-21 21:49:00", "end_date_time": "2022-03-21 22:08:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. This is a continuation of the Upshur/Western Marion/Southeast Morris County EF-2 tornado. This tornado, which maintained an EF-1 rating with estimated maximum winds around 105 mph, continued to uproot and snap trees and Southwest and Central Cass County with damage becoming more sporadic and narrow as it tracked northeast across FM 161, County Road 1599, Highway 49, County Road 1577, Highway 11, before finally lifting just east of Highway 130. The most significant damage occurred off of Highway 11 where a metal roof of a home was damaged. The total path length of this tornado which originated in Central Upshur County was 40.15 miles.", "ts_dict_index": [15051, 15052, 15053]}
+{"event_id": 1057264, "event_type": "Tornado", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-11-04 16:46:00", "end_date_time": "2022-11-04 16:49:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours. An EF-2 tornado with estimated maximum winds near 125 mph touched down in extreme Northwest McCurtain County near the Pickens community. The tornado touched down off of Pickens Road where it completed destroyed a chicken house, removed large sections of a roof of a home, and snapped multiple hardwood trees. The tornado then impacted a double-wide mobile home that was tied down with straps, which were snapped or footings pulled out of the ground. The mobile home was vaulted to the northwest and led to a fatality of a 90 year old male inside. A vehicle was also tossed and rolled at this location as well. The tornado continued moving northeast and uprooted multiple hardwood and softwood trees as it crossed Mount Zion Church Road, Glover Road, and Cedarwood Lane, before lifting near Coleman Road.", "ts_dict_index": [15000, 15001, 15002]}
+{"event_id": 1031944, "event_type": "Tornado", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2022-05-05 13:08:00", "end_date_time": "2022-05-05 13:21:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms also produced a few isolated tornadoes across portions of Rusk and Western Panola Counties, with localized flash flooding observed across portions of Upshur and Panola Counties. This is a continuation of the Eastern Rusk County tornado. This EF-1 tornado, with estimated maximum winds near 104 mph, moved over Martin Creek Lake into western Panola County, where most of the damage consisted of snapped and uprooted trees with the strongest tree damage indicators and the widest path being near County Road 257. The tornado continued up to and just east of Highway 149 before lifting. The tornado tracked just over six miles in western Panola County for a total path length of nearly 8.5 miles.", "ts_dict_index": [15078, 15079, 15080]}
+{"event_id": 1031937, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-05-05 12:45:00", "end_date_time": "2022-05-05 12:59:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms also produced a few isolated tornadoes across portions of Rusk and Western Panola Counties, with localized flash flooding observed across portions of Upshur and Panola Counties. An EF-2 tornado with estimated maximum winds of 115 mph developed just west of County Road 222 on the east side of Henderson and continued northeast for just over eight miles, uprooting and snapping thousands of trees and causing damage to some structures. The tornado was at its widest and strongest crossing County Road 262, FM 1251 East, County Road 324, and County Road 327 where extensive snapping of pine and hardwood trees warranted an estimated peak wind speed of 115 mph, a low EF-2 rating on the Enhanced Fujita Scale. The one injury occurred along County Road 262 where a male outside was struck by a falling tree. Several residences received various levels of roof damage, mostly due to falling trees. The tornado weakened as it lifted west of Martin Lake, with the same storm spawning another tornado just to the east near Martin Lake.", "ts_dict_index": [15075, 15076, 15077]}
+{"event_id": 1009331, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-03-21 22:37:00", "end_date_time": "2022-03-21 23:08:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. This is a continuation of the Northwest Nacogdoches County EF-2 tornado. The tornado maintained its high end EF-1/low end EF-2 intensity as it moved through Southern and Eastern Rusk County, with estimated maximum winds near 125 mph. Upon departing FM 225 just inside the Southern Rusk County line, the tornado tracked northeast and crossed County Roads 3238 and 3227 before reaching Highway 84. Numerous trees were snapped and uprooted along the tornado's path through Highway 84, with the tornado tearing down a large metal electrical transmission tower off of County Road 3206 northeast of the Sulphur Springs community, while also ripping the roof off of a nearby single family home. The tornado continued northeast snapping and uprooting additional trees, while also damaging the roofs off of several homes as it crossed County Road 3167, FM 2496, County Roads 3155 and 3146. As the tornado crossed Highway 259 and County Road 317, it damaged or destroyed several metal buildings, while also destroying a single-wide mobile home. The tornado also destroyed another single-wide mobile home on FM 95 in the Minden community, while also significantly damaging a nearby single family home. The tornado then crossed FM 1798 and County Road 3125, snapping and uprooting additional trees before crossing FM 840. Here, several metal buildings were destroyed, with damage to roofs and walls on a couple of homes. The tornado crossed County Road 366 before finally lifting just east of County Road 364 about 10 miles east-southeast of Henderson. ||In Rusk County, around 50 structures were damaged. The total path length of this tornado from Southern Cherokee, Northwest Nacogdoches, and through Southern and Eastern Rusk Counties was 37.57 miles.", "ts_dict_index": [15063, 15064, 15065]}
+{"event_id": 1009340, "event_type": "Tornado", "state": "TEXAS", "cz_name": "PANOLA", "begin_date_time": "2022-03-21 23:09:00", "end_date_time": "2022-03-21 23:25:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. This is a continuation of the Eastern Rusk County tornado. Although this tornado entered Western Panola County with estimated winds around 90 mph, it strengthened to a strong EF-2 with estimated maximum winds around 130 mph, as it lifted northeast through Western Panola County. It crossed FM 348 and County Roads 881, 188, and 189, snapping and uprooting numerous trees before reaching Highway 79. In this area, several homes were significantly damaged, and one well-built residence lost most of its roof with several walls collapsed. One injury occurred in this home, although the injury was not deemed critical. The damage rating on this structure was a strong EF-2, and near this location, the tornado achieved its maximum width of approximately 500 yards. Near this location, the high level of tree damage and damage to at least one other structure also warranted a rating of EF-2. A home on County Road 293 and a metal building on County Road 237 were also damaged from this tornado, before it lifted along County Road 241 several miles southwest of Beckville.", "ts_dict_index": [15066, 15067, 15068]}
+{"event_id": 1009223, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CASS", "begin_date_time": "2022-03-21 22:21:00", "end_date_time": "2022-03-21 22:23:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. An EF-1 tornado with estimated maximum winds around 90 mph embedded within a quasi-linear convective system (QLCS) briefly touched down and uprooted approximately 10 hardwood and softwood trees along Highway 77 just southeast of Douglassville. The tornado lifted north of Highway 77 and east of FM 2791.", "ts_dict_index": [15060, 15061, 15062]}
+{"event_id": 1031941, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-05-05 13:25:00", "end_date_time": "2022-05-05 13:31:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms also produced a few isolated tornadoes across portions of Rusk and Western Panola Counties, with localized flash flooding observed across portions of Upshur and Panola Counties. An EF-1 tornado with estimated maximum winds of 110 mph first touched down near Highway 259, causing damage at the Whispering Pines RV Park. This damage consisted of numerous trees being uprooted or snapped along with the complete destruction of a towable RV trailer. In addition, a food truck was tossed around 50 feet along with a number of canopies being tossed up to 500 feet. The tornado tracked to the east northeast and crossed County Road 3145 and uprooted/snapped numerous trees, before crossing FM 95 South toward County Road 3153, leaving behind a trail of uprooted and snapped trees. The tornado lifted near County Road 3144, with a path length of just over 3 miles.", "ts_dict_index": [15072, 15073, 15074]}
+{"event_id": 881225, "event_type": "Tornado", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-04-28 21:05:00", "end_date_time": "2020-04-28 21:10:00", "narrative": "A deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region during the afternoon and evening hours on April 28th, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Southeast Oklahoma into Northeast Texas, Southwest Arkansas, and North Louisiana just prior to midnight on the 29th. An EF-1 tornado with estimated maximum winds near 110 mph touched down along Johnny Beavers Trail Road, snapping and uprooting numerous trees. Several RVs and vehicles were significantly damaged by the snapped and uprooted trees. The tornado then crossed the Northern sections of Broken Bow Lake, snapping and uprooting several more trees before lifting along the eastern shore of the lake.", "ts_dict_index": [15081, 15082, 15083]}
+{"event_id": 1009351, "event_type": "Tornado", "state": "TEXAS", "cz_name": "HARRISON", "begin_date_time": "2022-03-21 23:49:00", "end_date_time": "2022-03-22 00:00:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. A weak EF-1 tornado with estimated maximum winds near 90 mph touched down on Blocker Road and snapped/uprooted several softwood trees. The tornado then crossed County Roads 1320, 1312, and 1202 (Old Town Road) before lifting. Multiple trees were snapped and uprooted in a convergent pattern along its path.", "ts_dict_index": [15057, 15058, 15059]}
+{"event_id": 1060587, "event_type": "Tornado", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2022-11-04 17:44:00", "end_date_time": "2022-11-04 18:21:00", "narrative": "A strong upper level trough progressed through the Rockies and into the Central and Southern Plains during the day on November 4th, enhancing strong surface low development over the Upper Red River Valley into Oklahoma. This produced a strong pressure gradient over the Southern Plains and Lower Mississippi Valley, allowing for very rich Gulf moisture to surge north across the Ark-La-Tex area into Eastern Oklahoma and much of Arkansas. This generated moderate instability across these areas during the afternoon, as temperatures rose into the lower to mid 80s. Very strong wind shear was also in place over these areas, with the upper trough reinforcing a cold front southeast into Southeast Oklahoma, Western Arkansas, and East Texas. This trough enhanced large scale forcing along the front, with discrete supercell development also occurring ahead of the main line of storms over portions of East Texas, Southeast Oklahoma, and Southwest Arkansas. Multiple tornadoes, some strong, touched down across these areas, with additional instances of damaging winds also reported before the line of storms overtook these discrete supercells and shifted east across the remainder of East Texas, Southwest Arkansas, and into North Louisiana during the evening and overnight hours. This is the continuation of the Red River County Texas EF-4 tornado. This tornado had weakened upon entering Southern McCurtain County Oklahoma, producing EF-2 damage in rural areas southwest of Idabel, ripping the roofs off of several single family homes. Shortly before entering Idabel, the outer edge of this tornado hit the Oklahoma Mesonet observing platform located about 5 miles to the southwest off of Ravens Nest Road. An anemometer located 10 meters above the platform measured a wind gust of 108 mph, with a nearby single family home sustaining roof damage where EF-2 winds estimated near 125 mph removed a large section of the roof structure with a wall collapsing on another single family home off of Osprey Road. The tornado continued on to snap several hundred trees before hitting a single family home off of Boss Road which had a wall collapse and partial roof damage that could not be rated due to trees falling into the home. More EF-2 damage was observed as the tornado approached Highway 259 when the tornado removed the roof and much of the second story off of a single family home. The two people in the home took shelter on the first floor under the stairs, preventing injury as winds estimated at 125 mph damaged the home. As the tornado moved northeast across Stone Haven Road, a Davis weather station recorded a gust of approximately 130 mph. ||Upon entering Idabel, the tornado damaged additional roofs of homes in several neighborhoods on the southeast side of town. One of the most hard hit subdivisions was Country Club Estates. None of the homes in the Country Club Estates were rated due to tree damage which resulted in much of the structural damage from trees falling into homes. Nearby at the Idabel Country Club, nearly every tree sustained damage on approximately six holes, with mostly snaps observed. There was also some debarking of trees in this area, where an EF-3 swath of damage had begun. Behind the golf course, a single family home was destroyed with most of its walls collapsed except for a small interior room. ||The tornado continued to move northeast, hitting the Kiamichi Family Medical Center where EF-2 damage (near 115 mph) was estimated due to the facade components that were torn from the structure. As the tornado approached Highway 259 and East Washington Street, it damaged the sign of a McDonald's and a swath of EF-3 winds completely destroyed the Donut Crossing and Express Tire stores. A sign from the Donut Crossing store was lofted by the tornado and carried 14.3 miles where it was found on the west side of Eagletown. After crossing East Washington Street, the tornado completely destroyed the Trinity Baptist Church. Winds at this location were estimated to be near 155 mph with the total destruction of the metal building system which was surrounded by a brick wall that collapsed with concrete anchors pulled up from the ground. The tornado moved on to produce narrow EF-2 damage in the more broader EF-1 damage swath with small vorticies likely extending down to the ground from the elevated large funnel cloud at this point. ||After moving northeast of Idabel, the tornado crossed mainly rural areas and completely destroyed chicken houses while snapping hardwood and softwood trees for approximately the next ten miles. An areal survey indicates that the tornado briefly lifted near the Little River and then touched down again in a forested area before damaging a metal structure atop a chicken plant off of Craig Road. A survey team from the National Weather Service Little Rock office found EF-2 damage with 135 mph winds between Eagletown and Broken Bow just south of Highway 70, where numerous trees and several wooden utility poles were snapped near the base near the Tyson Craig Feed Mill, a large elevator structure on top of a silo collapsed with a portion of a metal roof and walls ripped off of an adjacent metal building, and a doublewide manufactured home at the eastern end of Box Turtle Road was thrown off of its concrete pad, nearly pulling out an underground shelter, rolling over it, and landing about 30 feet to the north. Over half of the house was stripped of the undercarriage. Only about one-third of the walls/roof were left with the remainder of the structure removed and scattered well to the north. ||As the tornado crossed Highway 70 just west of Eagletown, many additional pines and hardwoods were snapped and uprooted. Nearly all utility poles within the path were also snapped or pushed over. The tornado then moved into a heavily forested area north of Eagletown with more specific damage noted from Old Winship Road to Pero Creek through the use of high-resolution satellite imagery before the tornado finally lifted a few miles before reaching the border with Northwestern Sevier County in Southwest Arkansas. ||Remarkedly, only 6 injuries and no fatalities were reported from this long track tornado throughout Southern and Eastern McCurtain County Oklahoma. In total, 220 homes were estimated to had been affected by this tornado, with 10-20 businesses damaged or destroyed. Of the total homes affected, 65 of them were destroyed.", "ts_dict_index": [15009, 15010, 15011]}
+{"event_id": 972359, "event_type": "Tornado", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-09-01 16:59:00", "end_date_time": "2021-09-01 17:06:00", "narrative": "The remnants of Hurricane Ida impacted the mid-Atlantic on September 1, 2021. As it moved northward, Ida began transitioning to a strong mid-latitude cyclone with pronounced frontal features, but with continued tropical moisture. On a regional level, the remnants of Ida became one of the most severe natural disasters in US history, due to a combination of several tornadoes, some of them strong, as well as catastrophic flooding over a large and densely populated area. The severe weather threat unfolded as the system's developing warm front lifted northward from the Delmarva region into Pennsylvania and New Jersey. South of the warm front, partial clearing and moderate to strong instability developed. Meanwhile, very strong shear and forcing, along with tropical moisture, were present within the warm sector. The result was widespread convection in the form of both supercell and quasi-linear thunderstorms. A number of storms became severe across the region, producing several tornadoes and other instances of wind damage. This continued an exceptionally active stretch of high end severe weather in the region, coming barely a month after the tornado outbreak of July 29. The storm which produced a strong tornado in Montgomery County, |PA, cycled and produced another tornado in Bucks County, PA. |Damage began near in the area of Neshaminy Creek between Valley Rd|and Pebble Hill Rd in Doylestown. The tornado tracked north- |northeast from there, producing a consistent path of damage. |Damage was mainly confined to trees and was fairly extensive at |times, with much of the path length being heavily wooded. Numerous|hardwood and softwood trees were snapped and uprooted along the |path. Damage was strongly suggestive of tornadic winds, and a |tornado debris signature was also evident on radar. The heaviest |damage occurred near and along a stretch of Edison- Furlong Rd. |Extensive tree damage occurred along that road and a number of its|cross streets. Several utility poles were snapped in this area. |Tree damage along nearby Swamp Rd was also significant. The |tornado continued but began to lose intensity as it approached |Route 202, with sporadic tree damage observed on Mill Rd. Gradual |weakening continued and the tornado appeared to lift entirely in |the area of Burnt House Hill Rd. The extent of tree damage |suggested maximum winds of around 100 mph. No injuries were |reported as a result of this tornado.", "ts_dict_index": [15108, 15109, 15110]}
+{"event_id": 972364, "event_type": "Tornado", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-09-01 17:30:00", "end_date_time": "2021-09-01 17:35:00", "narrative": "The remnants of Hurricane Ida impacted the mid-Atlantic on September 1, 2021. As it moved northward, Ida began transitioning to a strong mid-latitude cyclone with pronounced frontal features, but with continued tropical moisture. On a regional level, the remnants of Ida became one of the most severe natural disasters in US history, due to a combination of several tornadoes, some of them strong, as well as catastrophic flooding over a large and densely populated area. The severe weather threat unfolded as the system's developing warm front lifted northward from the Delmarva region into Pennsylvania and New Jersey. South of the warm front, partial clearing and moderate to strong instability developed. Meanwhile, very strong shear and forcing, along with tropical moisture, were present within the warm sector. The result was widespread convection in the form of both supercell and quasi-linear thunderstorms. A number of storms became severe across the region, producing several tornadoes and other instances of wind damage. This continued an exceptionally active stretch of high end severe weather in the region, coming barely a month after the tornado outbreak of July 29. A tornado embedded within a squall line developed several miles |southeast of the storm which produced a tornado in Buckingham |Township. Tornadic damage was first observed in the vicinity of |Stoneybrook Rd at Eagle Rd, near Jericho Creek. The tornado |tracked northeastward from there. It passed over the Jericho |National Golf Club, and sporadic tree damage mainly consisting of |uproots and large limbs snapped was observed in a path throughout |the golf course. It then moved over the adjacent Brownsburg Park, |where additional tree damage was observed and several soccer goals|were observed flipped in various directions. The tornado then |began to approach the Delaware River. Some minor tree damage was |observed along River Rd. However, the tornado appeared to lift |just slightly before reaching the Delaware River, with no apparent|damage on Pebbletown Rd just prior to the river. Throughout its |path, the tree damage produced by this tornado was fairly |sporadic, and it may have been discontinuous. Noticeable wind |damage was also observed for at least a mile east of the tornado |track, especially near its endpoint close to the Delaware River. |This is believed to be straight line wind damage, which is |corroborated by radar data, occurring around the rear flank |downdraft region of the tornadic circulation. However, the exact |length and width of the tornadic circulation is somewhat uncertain|due to the surrounding areas of straight line wind damage.", "ts_dict_index": [15111, 15112, 15113]}
+{"event_id": 972397, "event_type": "Tornado", "state": "PENNSYLVANIA", "cz_name": "BUCKS", "begin_date_time": "2021-09-01 18:03:00", "end_date_time": "2021-09-01 18:04:00", "narrative": "The remnants of Hurricane Ida impacted the mid-Atlantic on September 1, 2021. As it moved northward, Ida began transitioning to a strong mid-latitude cyclone with pronounced frontal features, but with continued tropical moisture. On a regional level, the remnants of Ida became one of the most severe natural disasters in US history, due to a combination of several tornadoes, some of them strong, as well as catastrophic flooding over a large and densely populated area. The severe weather threat unfolded as the system's developing warm front lifted northward from the Delmarva region into Pennsylvania and New Jersey. South of the warm front, partial clearing and moderate to strong instability developed. Meanwhile, very strong shear and forcing, along with tropical moisture, were present within the warm sector. The result was widespread convection in the form of both supercell and quasi-linear thunderstorms. A number of storms became severe across the region, producing several tornadoes and other instances of wind damage. This continued an exceptionally active stretch of high end severe weather in the region, coming barely a month after the tornado outbreak of July 29. The tornado which began in Burlington County, New Jersey crossed the Burlington-Bristol Bridge and moved into Bucks County, Pennsylvania. As the tornado passed through a wooded floodplain along |the banks of the Delaware River, no visible damage was noted |either. The tornado then lifted just before reaching downtown |Bristol, PA, with several trees being snapped along the Bristol |Wharf.", "ts_dict_index": [15114, 15115, 15116]}
+{"event_id": 866156, "event_type": "Tornado", "state": "KENTUCKY", "cz_name": "CHRISTIAN", "begin_date_time": "2020-01-11 07:19:00", "end_date_time": "2020-01-11 07:23:00", "narrative": "An unseasonably strong storm system impacted the region January 10-11. Heavy rainfall, flooding, scattered damaging winds, tornadoes, and gusty non-thunderstorm winds impacted western Kentucky during this time. The bulk of the event occurred overnight and into the morning hours on the 11th. Rainfall totals ranged from 2 to 5 inches, which resulted in pockets of flash flooding across the region, as well as minor flooding of the Green River. Strong to severe convection over the Ozark Mountains moved east into an environment of very strong wind shear over southeast Missouri, with 850 mb winds near 60 knots. The convection maintained intensity after it crossed the Mississippi River during the early morning hours. Tremendous wind shear (winds of 50 knots down to 1500 feet above ground) and strong forcing associated with a potent 500 mb shortwave compensated for weak instability. Some of the strong winds aloft reached the surface in the form of gradient wind gusts from 40 to around 50 mph. A weak surface low formed along a cold front over southwest Arkansas, then deepened as it tracked northeast across the Missouri Bootheel and into the lower Ohio Valley on the morning of the 11th. The tornado touched down in the Pennyrile Forest State Resort Park. Over half of its path was in the park. After leaving the park, the tornado crossed Highway 109. A few barns were damaged or blown down. A couple houses sustained loss of shingles. At least dozens of trees were uprooted or snapped. Peak winds were estimated near 95 mph.", "ts_dict_index": [15105, 15106, 15107]}
+{"event_id": 866161, "event_type": "Tornado", "state": "KENTUCKY", "cz_name": "CHRISTIAN", "begin_date_time": "2020-01-11 07:16:00", "end_date_time": "2020-01-11 07:20:00", "narrative": "An unseasonably strong storm system impacted the region January 10-11. Heavy rainfall, flooding, scattered damaging winds, tornadoes, and gusty non-thunderstorm winds impacted western Kentucky during this time. The bulk of the event occurred overnight and into the morning hours on the 11th. Rainfall totals ranged from 2 to 5 inches, which resulted in pockets of flash flooding across the region, as well as minor flooding of the Green River. Strong to severe convection over the Ozark Mountains moved east into an environment of very strong wind shear over southeast Missouri, with 850 mb winds near 60 knots. The convection maintained intensity after it crossed the Mississippi River during the early morning hours. Tremendous wind shear (winds of 50 knots down to 1500 feet above ground) and strong forcing associated with a potent 500 mb shortwave compensated for weak instability. Some of the strong winds aloft reached the surface in the form of gradient wind gusts from 40 to around 50 mph. A weak surface low formed along a cold front over southwest Arkansas, then deepened as it tracked northeast across the Missouri Bootheel and into the lower Ohio Valley on the morning of the 11th. The tornado crossed over from Caldwell County. Most of the Christian County portion of the path was in the Pennyrile Forest State Resort Park, where hundreds of trees were snapped or uprooted. Peak winds were estimated near 95 mph.", "ts_dict_index": [15099, 15100, 15101]}
+{"event_id": 866151, "event_type": "Tornado", "state": "KENTUCKY", "cz_name": "CHRISTIAN", "begin_date_time": "2020-01-11 07:40:00", "end_date_time": "2020-01-11 07:43:00", "narrative": "An unseasonably strong storm system impacted the region January 10-11. Heavy rainfall, flooding, scattered damaging winds, tornadoes, and gusty non-thunderstorm winds impacted western Kentucky during this time. The bulk of the event occurred overnight and into the morning hours on the 11th. Rainfall totals ranged from 2 to 5 inches, which resulted in pockets of flash flooding across the region, as well as minor flooding of the Green River. Strong to severe convection over the Ozark Mountains moved east into an environment of very strong wind shear over southeast Missouri, with 850 mb winds near 60 knots. The convection maintained intensity after it crossed the Mississippi River during the early morning hours. Tremendous wind shear (winds of 50 knots down to 1500 feet above ground) and strong forcing associated with a potent 500 mb shortwave compensated for weak instability. Some of the strong winds aloft reached the surface in the form of gradient wind gusts from 40 to around 50 mph. A weak surface low formed along a cold front over southwest Arkansas, then deepened as it tracked northeast across the Missouri Bootheel and into the lower Ohio Valley on the morning of the 11th. This tornado crossed U.S. Highway 41 about four miles southeast of Hopkinsville. Several trees were snapped along the path. One barn received some partial damage to its roof. Peak winds were estimated near 95 mph.", "ts_dict_index": [15093, 15094, 15095]}
+{"event_id": 866223, "event_type": "Tornado", "state": "KENTUCKY", "cz_name": "CHRISTIAN", "begin_date_time": "2020-01-11 07:14:00", "end_date_time": "2020-01-11 07:19:00", "narrative": "An unseasonably strong storm system impacted the region January 10-11. Heavy rainfall, flooding, scattered damaging winds, tornadoes, and gusty non-thunderstorm winds impacted western Kentucky during this time. The bulk of the event occurred overnight and into the morning hours on the 11th. Rainfall totals ranged from 2 to 5 inches, which resulted in pockets of flash flooding across the region, as well as minor flooding of the Green River. Strong to severe convection over the Ozark Mountains moved east into an environment of very strong wind shear over southeast Missouri, with 850 mb winds near 60 knots. The convection maintained intensity after it crossed the Mississippi River during the early morning hours. Tremendous wind shear (winds of 50 knots down to 1500 feet above ground) and strong forcing associated with a potent 500 mb shortwave compensated for weak instability. Some of the strong winds aloft reached the surface in the form of gradient wind gusts from 40 to around 50 mph. A weak surface low formed along a cold front over southwest Arkansas, then deepened as it tracked northeast across the Missouri Bootheel and into the lower Ohio Valley on the morning of the 11th. The tornado entered Christian County from Caldwell County just south of Highway 91. At least a half dozen barns or outbuildings were damaged or destroyed, mostly in the Caldwell County portion of the track. At least dozens of trees were snapped or uprooted. The tornado path ended at the southern boundary of the Pennyrile Forest State Resort Park. Peak winds were estimated near 100 mph.", "ts_dict_index": [15102, 15103, 15104]}
+{"event_id": 866150, "event_type": "Tornado", "state": "KENTUCKY", "cz_name": "CHRISTIAN", "begin_date_time": "2020-01-11 07:34:00", "end_date_time": "2020-01-11 07:44:00", "narrative": "An unseasonably strong storm system impacted the region January 10-11. Heavy rainfall, flooding, scattered damaging winds, tornadoes, and gusty non-thunderstorm winds impacted western Kentucky during this time. The bulk of the event occurred overnight and into the morning hours on the 11th. Rainfall totals ranged from 2 to 5 inches, which resulted in pockets of flash flooding across the region, as well as minor flooding of the Green River. Strong to severe convection over the Ozark Mountains moved east into an environment of very strong wind shear over southeast Missouri, with 850 mb winds near 60 knots. The convection maintained intensity after it crossed the Mississippi River during the early morning hours. Tremendous wind shear (winds of 50 knots down to 1500 feet above ground) and strong forcing associated with a potent 500 mb shortwave compensated for weak instability. Some of the strong winds aloft reached the surface in the form of gradient wind gusts from 40 to around 50 mph. A weak surface low formed along a cold front over southwest Arkansas, then deepened as it tracked northeast across the Missouri Bootheel and into the lower Ohio Valley on the morning of the 11th. The tornado touched down on the northern perimeter of the Fort Campbell military base and proceeded northeast across U.S. Highway 41. Trees were uprooted and snapped along the path. Several barns were damaged or destroyed, including one that had its roof thrown several hundred yards into trees. Power lines were downed, and 13 empty rail cars were tipped over along the path. A couple of homes received some minor damage. The tornado lifted just northwest of Pembroke. Peak winds were estimated near 100 mph.", "ts_dict_index": [15096, 15097, 15098]}
+{"event_id": 954103, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CHEROKEE", "begin_date_time": "2021-06-08 09:23:00", "end_date_time": "2021-06-08 09:24:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, moving over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. ||Additional scattered severe thunderstorms developed later in the morning farther south across East Texas, which resulted in downed trees and even a few weak, short-lived tornadoes. These storms progressed into North Louisiana around midday, downing additional trees before exiting the region by mid-afternoon. An EF-0 tornado with estimated maximum winds near 80 mph briefly touched down at the Ramey Plant Farm. It collapsed the metal lining structure of two greenhouses before breaking several large branches on a mature hardwood tree. The tornado lifted as it crossed Highway 204. At the Reklaw City Hall, intense ear pressure was experienced by one of the city workers as the tornado passed nearby.", "ts_dict_index": [15090, 15091, 15092]}
+{"event_id": 954102, "event_type": "Tornado", "state": "TEXAS", "cz_name": "CHEROKEE", "begin_date_time": "2021-06-08 09:02:00", "end_date_time": "2021-06-08 09:03:00", "narrative": "Another shortwave trough ejected east across the Ark-La-Tex from the morning through the afternoon hours on June 8th, beneath an upper low pressure system that lifted north from Eastern Oklahoma and Western Arkansas into Southeast Kansas and Western Missouri. Showers and thunderstorms redeveloped during the pre-dawn hours across Southeast Oklahoma and adjacent sections of Southwest Arkansas along a remnant surface boundary from earlier storms ahead of this next approaching trough, moving over already saturated grounds from heavy rainfall that fell a day prior across these areas. A warm, very moist, and unstable air mass was in place, with these storms very efficient rain producers, moving repeatedly over the same areas across Western and Central McCurtain County Oklahoma. Widespread rainfall amounts of 3-8 inches fell across this area, resulting in significant flash flooding. ||Additional scattered severe thunderstorms developed later in the morning farther south across East Texas, which resulted in downed trees and even a few weak, short-lived tornadoes. These storms progressed into North Louisiana around midday, downing additional trees before exiting the region by mid-afternoon. An EF-0 tornado with estimated maximum winds near 70 mph briefly touched down as it was crossing Highway 84 northeast of Rusk. The tornado broke small limbs on a couple of hardwood and softwood trees and also left two power poles leaning before lifting near the intersection of Highway 84 and Highway 110.", "ts_dict_index": [15087, 15088, 15089]}
+{"event_id": 1009338, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-03-21 23:08:00", "end_date_time": "2022-03-21 23:09:00", "narrative": "A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma. Strong southerly low level winds allowed for the rapid return of warm, moist, and unstable north behind a warm front which lifted north through East Texas and North Louisiana. Large scale forcing began to increase across Northern and Central Texas during the evening, with showers and thunderstorms becoming numerous across this area which spread into East Texas and North Louisiana during the late evening through the early morning hours of the 22nd. Given the extent of forcing within the unstable air mass in place, severe thunderstorms developed over North-central Texas and spread into East Texas, resulting in numerous reports of damaging winds, large hail, and even isolated tornadoes. Redevelopment of these storms continued overnight as well over the same areas of East Texas and Northwest Louisiana, which resulted in instances of flash flooding as well, as widespread rainfall amounts of 3-6 inches fell over these areas. These storms diminished during the early morning hours of the 22nd with the passage of a cold front through the region. An EF-2 tornado with estimated maximum winds near 130 mph, touched down along County Road 3124 in extreme Eastern Rusk County, snapping and uprooting several trees before crossing County Road 3121 into Western Panola County. While the stronger winds were noted in Panola County, maximum winds were estimated to be near 90 mph (low EF-1 strength) in extreme Eastern Rusk County.", "ts_dict_index": [15054, 15055, 15056]}
+{"event_id": 1031943, "event_type": "Tornado", "state": "TEXAS", "cz_name": "RUSK", "begin_date_time": "2022-05-05 13:04:00", "end_date_time": "2022-05-05 13:08:00", "narrative": "A surface low was centered over the southern Texas Panhandle with a stationary front extending through southern Oklahoma into southern Arkansas eastward into northern Mississippi. A dry line extended southward from the surface low through west Texas into the Big Bend Country along with a cold front draped southwest from the surface low into southeast New Mexico. Aloft, an upper-level low was initially centered just east of the Rockies in eastern Colorado before tracking into eastern Kansas and eventually into the Ozarks on the morning of May 6th. Meanwhile, the surface low shifted along the Red River Valley with the cold front trailing along the I-35 corridor, shifting farther east into the Ark-La-Tex region on the afternoon and evening of May 5th. As a result, an ongoing complex of showers and thunderstorms over Oklahoma strengthened as they moved into a more unstable environment during the afternoon ahead of the cold front and upper low, becoming strong to severe across portions of Southwest Arkansas, East Texas, and Northwest Louisiana. These storms also produced a few isolated tornadoes across portions of Rusk and Western Panola Counties, with localized flash flooding observed across portions of Upshur and Panola Counties. This was the second tornado of an east to northeast moving supercell thunderstorm. This EF-1 tornado, with estimated maximum winds of 104 mph, moved over Martin Creek Lake and eventually into western Panola County. Most of the damage consisted of snapped and uprooted trees. The total path length in Rusk County was approximately two miles before entering Western Panola County.", "ts_dict_index": [15069, 15070, 15071]}
+{"event_id": 881231, "event_type": "Tornado", "state": "OKLAHOMA", "cz_name": "MCCURTAIN", "begin_date_time": "2020-04-28 21:20:00", "end_date_time": "2020-04-28 21:24:00", "narrative": "A deepening upper level trough sweeping southeast across Oklahoma and Arkansas reinforced a cold front southeast across the Southern Plains and Ozarks region during the afternoon and evening hours on April 28th, where a complex of showers and thunderstorms developed by mid and late afternoon over these areas and quickly progressed southeast into the Four State Region. Despite the showers and thunderstorms that affected the area earlier in the day, instability remained adequate especially over East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas. As large scale forcing increased ahead of the trough, thus tapping into this unstable air, a squall line progressed southeast through all of the region during the late evening through the early morning hours on April 29th, producing widespread reports of damaging winds and large hail. A couple of isolated tornadoes also touched down across McCurtain County Oklahoma, one associated with the supercell that developed ahead of the line, and another associated within the squall line itself. These storms exited Southeast Oklahoma into Northeast Texas, Southwest Arkansas, and North Louisiana just prior to midnight on the 29th. An EF-2 tornado with estimated maximum winds near 125 mph touched down in a heavily wooded area along Union Valley Road, snapping and uprooting numerous trees. The tornado moved south southeast, tossing two barges over 100 yards and lifting a large portion of the roof deck of a home, causing it to collapse. The tornado then completely destroyed a single-wide manufactured home, with the base frame of the home twisted and tossed 100 yards to the east. Further to the south, another home sustained significant roof and structural damage when large gas tanks were tossed into it. The tornado then continued to snap numerous trees along Cascade Creek Road and along Wyr 20000 Road, as well as removing roofing material from another home on Union Valley Road. The tornado continued to track southeast across a heavily wooded area before crossing into Sevier County Arkansas.", "ts_dict_index": [15084, 15085, 15086]}